<?xml version="1.0" encoding="UTF-8"?><!DOCTYPE article  PUBLIC "-//NLM//DTD Journal Publishing DTD v3.0 20080202//EN" "http://dtd.nlm.nih.gov/publishing/3.0/journalpublishing3.dtd"><article xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink" dtd-version="3.0" xml:lang="en" article-type="research article"><front><journal-meta><journal-id journal-id-type="publisher-id">JAMP</journal-id><journal-title-group><journal-title>Journal of Applied Mathematics and Physics</journal-title></journal-title-group><issn pub-type="epub">2327-4352</issn><publisher><publisher-name>Scientific Research Publishing</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.4236/jamp.2022.102043</article-id><article-id pub-id-type="publisher-id">JAMP-115519</article-id><article-categories><subj-group subj-group-type="heading"><subject>Articles</subject></subj-group><subj-group subj-group-type="Discipline-v2"><subject>Physics&amp;Mathematics</subject></subj-group></article-categories><title-group><article-title>
 
 
  On the Paradox of the Duality of Autoregressive and Moving Average Processes
 
</article-title></title-group><contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Elechi</surname><given-names>Onyemachi</given-names></name><xref ref-type="aff" rid="aff1"><sup>1</sup></xref><xref ref-type="corresp" rid="cor1"><sup>*</sup></xref></contrib><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Iheanyi</surname><given-names>Sylvester Iwueze</given-names></name><xref ref-type="aff" rid="aff1"><sup>1</sup></xref></contrib><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Eleazar</surname><given-names>Chukwunenye Nwogu</given-names></name><xref ref-type="aff" rid="aff1"><sup>1</sup></xref></contrib></contrib-group><aff id="aff1"><addr-line>Department of Statistics, Federal University of Technology, Owerri, Nigeria</addr-line></aff><pub-date pub-type="epub"><day>28</day><month>01</month><year>2022</year></pub-date><volume>10</volume><issue>02</issue><fpage>589</fpage><lpage>609</lpage><history><date date-type="received"><day>18,</day>	<month>March</month>	<year>2021</year></date><date date-type="rev-recd"><day>25,</day>	<month>February</month>	<year>2022</year>	</date><date date-type="accepted"><day>28,</day>	<month>February</month>	<year>2022</year></date></history><permissions><copyright-statement>&#169; Copyright  2014 by authors and Scientific Research Publishing Inc. </copyright-statement><copyright-year>2014</copyright-year><license><license-p>This work is licensed under the Creative Commons Attribution International License (CC BY). http://creativecommons.org/licenses/by/4.0/</license-p></license></permissions><abstract><p>
 
 
  A widely held view in time series analysis is the concept of duality that a finite order stationary autoregressive process of order 
  <em>p</em> (AR(
  <em>p</em>)) is equivalent to an infinite order moving average (MA) process and a finite order invertible moving average of order 
  <em>q</em> (MA(
  <em>q</em>)) is equivalent to an infinite order autoregressive (AR) process. The purpose of this paper is to demonstrate that the concept is not universally true. Thus, a finite order stationary autoregressive process of order 
  <em>p</em> (AR(
  <em>p</em>)) can be written as an finite order moving average process and a finite order moving average process of order 
  <em>q</em> (MA(
  <em>q</em>)) can be written as a finite order stationary autoregressive process. The regions of breakdown of concept of duality were determined for 
  <em>p</em> = 
  <em>q</em> = 1,2 using method of moments. The method involves equating non-zero autocovariances of the stationary AR(
  <em>p</em>) to the equivalent non-zero autocovariances of the invertible MA(
  <em>p</em>) to determine the region of non-duality. In such region of breakdown in duality, 1) both the Autocorrelation function and the Partial Autocorrelation function of the AR process and MA process cuts off after equal lags 2) a finite AR model can be adequately represented by a finite MA model of equal order and conversely with the same error variance and 3) negative values of the parameters of the AR process are equal in magnitude but opposite in direction to the parameters of the equivalent MA process and conversely. Empirical examples (simulation and real life examples) were used to illustrate these. Therefore, it has been recommended that caution should be exercised in using the concept of duality in time series analysis until future research proves otherwise.
 
</p></abstract><kwd-group><kwd>Duality</kwd><kwd> Non-Duality</kwd><kwd> Method of Moments</kwd><kwd> Quadratic Inequality</kwd><kwd> Stationarity Region</kwd><kwd> Invertibility Region</kwd></kwd-group></article-meta></front><body><sec id="s1"><title>1. Introduction</title><p>The concept of duality is an old topic and a fruitful idea that can be found in many areas of Mathematics and other related disciplines [<xref ref-type="bibr" rid="scirp.115519-ref1">1</xref>] [<xref ref-type="bibr" rid="scirp.115519-ref2">2</xref>] [<xref ref-type="bibr" rid="scirp.115519-ref3">3</xref>]. Duality is a principle that gives two different points of view to the same object [<xref ref-type="bibr" rid="scirp.115519-ref1">1</xref>] [<xref ref-type="bibr" rid="scirp.115519-ref4">4</xref>] [<xref ref-type="bibr" rid="scirp.115519-ref5">5</xref>]. These points of view constitute an instance of opposition or contrast between concepts that are interchangeable, such that all results in one formulation also hold in the dual formulation [<xref ref-type="bibr" rid="scirp.115519-ref6">6</xref>] - [<xref ref-type="bibr" rid="scirp.115519-ref11">11</xref>]. As a consequence, the concept of duality involves symmetry within a system such that a theorem remains valid if certain objects, relations or operations are interchanged [<xref ref-type="bibr" rid="scirp.115519-ref12">12</xref>].</p><p>In a mathematical system, the concept of duality forms bases for describing and identifying the property of algebraic structures, theorems and/or expressions, being dual to each other. In his views, [<xref ref-type="bibr" rid="scirp.115519-ref13">13</xref>] stated that the concept of duality involves two objects plus a relation between them that is symmetric, such that one can get from one object to the other and vice versa. Some examples where the principle of duality applies in Mathematics include the linear duality in plane geometry and linear algebra, duality for Abelian groups and Non-Abelian groups, duality for non-linear geometry and Fourier theory, etc. [<xref ref-type="bibr" rid="scirp.115519-ref1">1</xref>]. Similarly, in Physics, the concept of duality has been applied to describe and identify the properties of variables in space. These include mirror symmetry, position momentum, quantum mechanics and electromagnetism [<xref ref-type="bibr" rid="scirp.115519-ref1">1</xref>] [<xref ref-type="bibr" rid="scirp.115519-ref6">6</xref>] [<xref ref-type="bibr" rid="scirp.115519-ref14">14</xref>].</p><p>Dual Aspect Concept, also known as Duality Principle, is a fundamental convention of accounting that forms basis for double entry accounting system. Under the accounting system, transactions are classified into debit or credit, loss or profit, etc. which enables every transaction to have dual effects [<xref ref-type="bibr" rid="scirp.115519-ref15">15</xref>] [<xref ref-type="bibr" rid="scirp.115519-ref16">16</xref>]. These dual effects ensure that all aspects of a transaction are accounted for in the financial statements.</p><p>In Statistics duality has been used to describe the relationship between models for two classes of stationary time series (the autoregressive and moving average processes). A given stationary autoregressive process of order p (AR(p)) was denoted by [<xref ref-type="bibr" rid="scirp.115519-ref17">17</xref>];</p><p>φ p ( B ) X t = e t (1.1)</p><p>we can write (1.1) as</p><p>X t = ψ ( B ) e t (1.2)</p><p>such that</p><p>φ p ( B ) ψ ( B ) = 1 (1.3)</p><p>In (1.1) and (1.2), e t ~ N ( 0 , σ 2 ) and</p><p>φ p ( B ) = 1 + ϕ   1 B + ϕ   2 B 2 + ⋯ + ϕ p B p (1.4)</p><p>ψ ( B ) = 1 + ψ 1 B 1 + ψ 2 B 2 + ⋯ (1.5)</p><p>That is, a finite order stationary AR process (1.1) is equivalent to an infinite order moving average process (1.2).</p><p>Conversely, for a given invertible moving average process of order q, (MA(q)) denoted by</p><p>X t = θ q ( B ) e t (1.6)</p><p>we can write (1.6) as</p><p>e t = θ q − 1 ( B ) X t = ∏ ( B ) X t (1.7)</p><p>such that</p><p>θ q ( B ) ∏ ( B ) = 1 (1.8)</p><p>In (1.6) and (1.7), e t ~ N ( 0 , σ 2 ) and</p><p>θ q ( B ) = 1 + θ 1 B 1 + θ 2 B 2 + ⋯ + θ q B q (1.9)</p><p>∏ ( B ) = 1 + π 1 B 1 + π 2 B 2 + ⋯ (1.10)</p><p>is an infinite but converging series. That is, a finite order invertible MA process (1.6) is equivalent to an infinite order AR process (1.7).</p><p>The dual relationship also exists in their autocorrelation functions (ACFs) and partial autocorrelation functions (PACFs) [<xref ref-type="bibr" rid="scirp.115519-ref17">17</xref>]. For an AR(p) process, while the ACF tails off, the PACF cuts off after lag p, but for MA(q) process, the ACF cuts off after lag q while the PACF tails off.</p><p>The works of [<xref ref-type="bibr" rid="scirp.115519-ref18">18</xref>] - [<xref ref-type="bibr" rid="scirp.115519-ref27">27</xref>] outlined other properties of the duality principle among these models. Using the duality principle, [<xref ref-type="bibr" rid="scirp.115519-ref28">28</xref>] showed that if AR and MA processes of the same order are simulated from the same sequence of errors using the same parameter values, then to a close approximation, the least squares estimates calculated from the MA series will tend to underestimate the true parameter values while those from AR series will tend to over-estimate them by the same amount. Thus, suggesting that the duality principle between AR(p) is equivalent to an infinite order moving average (MA) process and MA(q) processes is equivalent to an infinite order autoregressive (AR) process may be universally true.</p><p>However, certain real life examples have shown that this principle may not be strictly true. Thereby raising some doubts about the universality of duality in time series analysis. The question that we now ask is, “Is the duality between models for stationary AR(p) and invertible MA(q) processes universally true? If not, under what condition(s) will the principle break down? This question is what this study intends to address. Therefore, the ultimate objective of this study is to determine the parameter region within which the principle of duality between models for stationary AR(p) and invertible MA(q) processes breaks down. This region has been designated as the ‘Non-Duality’ region in this study. For the translation from stationary AR(p) process to invertible MA(p) process and, from invertible MA(p) process to stationary AR(p) process, the method adopted to determine the non-duality region was discussed in Section 2. In Section 3, the study illustrated the breakdown in duality principle between stationary AR(p) and invertible MA(p) processes using empirical examples (real life data and simulated series examples) while Section 4 is the concluding remark.</p></sec><sec id="s2"><title>2. Methodology</title><p>The methodology adopted to determine the Non-Duality region is the method of moments. The method involves equating non-zero autocovariances of the stationary Autoregressive Process of order p (AR(p)), to corresponding non-zero autocovariances of the invertible Moving Average Process of order p (MA(p)). This is because as noted by [<xref ref-type="bibr" rid="scirp.115519-ref17">17</xref>], the dual relationship between models for stationary AR(p) and invertible MA(q) processes also exists between the autocorrelation functions (ACFs) and partial autocorrelation functions (PACFs). For a given sequence of errors, our bases for determining breakdown in duality is to evaluate</p><p>| R ​ AR ( p ) ( k ) − R MA ( p ) ( k ) | = h k ,     k = 0 , 1 , ⋯ , p (2.1)</p><p>where R ​ AR ( p ) ( k ) is the lag k autocovariance of the stationary AR(p) process, R MA ( p ) ( k ) is the lag k autocovariance of the invertible MA(p) process and h k is the degree of precision. The principle of duality is considered to have broken down if h k ≈ 0 ∀ k to some degree of approximation. The parameters of stationary AR(p) process and invertible MA(p) process for which h k ≈ 0 give the region where duality breaks down (Non-duality region). Hence, for various degrees of approximations allowable for h k , the real values of the parameters for the Non-Duality region are determined.</p><sec id="s2_1"><title>2.1. Non-Duality between AR(1) and MA(1) Processes</title><p>For the model and autocovariances of stationary autoregressive process of order one (AR(1)) [<xref ref-type="bibr" rid="scirp.115519-ref20">20</xref>]:</p><p>X ˜ t = ϕ   1 X ˜ t − 1 + e t   ;     e t ~ N ( 0 , σ 2 ) ,         − 1 &lt; ϕ   1 &lt; 1 (2.2)</p><p>R ​ AR ( 1 ) ( k ) = { σ 2 1 − ϕ   1 2 ,     k = 0 ϕ   1 σ 2 1 − ϕ   1 2 ,       k = 1 ϕ   1 R ( k − 1 )   ,     k &gt; 1 (2.3)</p><p>and for invertible moving average process of order one (MA(1)) [<xref ref-type="bibr" rid="scirp.115519-ref20">20</xref>]:</p><p>X ˜ t = e t − θ   1 e t − 1 ;   e t ~ N ( 0 , σ 2 ) ,     X ˜ t = X t − μ ,     − 1 &lt; θ   1 &lt; 1 (2.4)</p><p>R MA ( 1 ) ( k ) = { σ 2 ( 1 + θ   1 2 ) ,     k = 0 − θ   1 σ 2 ,     k = 1 0 ,     k &gt; 1 (2.5)</p><p>where X ˜ t = X t − μ and μ = E ( X t ) . By equating non-zero autocovariances of AR(p) and MA(p) processes: p = 1, we obtain</p><p>σ 2 1 − ϕ   1 2 = σ 2 ( 1 + θ   1 2 ) (2.6)</p><p>ϕ   1 σ 2 1 − ϕ   1 2 = − θ   1 σ 2 (2.7)</p><p>By combining (2.6) and (2.7), we obtain</p><p>ϕ   1 = − θ   1 1 + θ   1 2 ⇒ ϕ   1 θ   1 2 + θ   1 + ϕ   1 = 0 (2.8)</p><p>Note that for invertible MA(1) process, the autocorrelation function of MA(1) process at lag 1 − 0.5 &lt; ρ 1 MA ( 1 ) &lt; 0.5 . This implies that − 0.5 &lt; − θ   1 1 + θ   1 2 &lt; 0.5 . Hence, for Non-duality, it is expected that − 0.5 &lt; ϕ   1 &lt; 0.5 , since ϕ   1 = − θ   1 1 + θ   1 2 .</p><p>In solving Equation (2.4), two cases arise.</p><p>Case I: Non-Duality Region in movement from stationary AR(1) process to invertible MA(1) process.</p><p>The solutions for θ 1 in the resulting quadratic Equation (2.8) are</p><p>θ 1 = − 1 &#177; 1 − 4 ϕ   1 2 2 ϕ   1 (2.9)</p><p>For real values D = 1 − 4 ϕ   1 2 ≥ 0 , ⇒ 4 ϕ   1 2 ≥ 1 , ϕ   1 2 ≥ 1 4 and − 1 2 &lt; ϕ   1 &lt; 1 2 .</p><p>For − 1 &lt; θ 1 &lt; 1 , the acceptable value of θ 1 is</p><p>θ 1 = − 1 + 1 − 4 ϕ   1 2 2 ϕ   1 (2.10)</p><p>Therefore when moving from stationary AR(1) process to invertible MA(1) process, the region of breakdown of duality is determined using (2.1), and illustrated in <xref ref-type="table" rid="table1">Table 1</xref>.</p><p>Case II: Non-Duality Region in movement from invertible MA(1) process to stationary AR(1) process.</p><table-wrap id="table1" ><label><xref ref-type="table" rid="table1">Table 1</xref></label><caption><title> Regions of ϕ   1 and θ 1 for non-duality of AR(1) and MA(1) processes</title></caption><table><tbody><thead><tr><th align="center" valign="middle"  rowspan="3"  >Degree of approximation allowable for h k</th><th align="center" valign="middle"  colspan="2"  >Region of Non-duality</th><th align="center" valign="middle"  rowspan="3"  >Remark</th></tr></thead><tr><td align="center" valign="middle" >AR(1) Process</td><td align="center" valign="middle" >MA(1) Process</td></tr><tr><td align="center" valign="middle" >ϕ   1</td><td align="center" valign="middle" >θ 1</td></tr><tr><td align="center" valign="middle" >1</td><td align="center" valign="middle" >[ − 0.38 , 0.38 ]</td><td align="center" valign="middle" >[ − 0.46 , 0.46 ]</td><td align="center" valign="middle" >Negative values ϕ   1 are mapped into positive values of θ 1 and vice versa</td></tr><tr><td align="center" valign="middle" >2</td><td align="center" valign="middle" >[ − 0.24 , 0.24 ]</td><td align="center" valign="middle" >[ − 0.26 , 0.26 ]</td><td align="center" valign="middle" >Negative values ϕ   1 are mapped into positive values of θ 1 and vice versa</td></tr><tr><td align="center" valign="middle" >3</td><td align="center" valign="middle" >[ − 0.14 , 0.14 ]</td><td align="center" valign="middle" >[ − 0.14 , 0.14 ]</td><td align="center" valign="middle" >Negative values ϕ   1 are mapped into positive values of θ 1 and vice versa</td></tr><tr><td align="center" valign="middle" >4</td><td align="center" valign="middle" >[ − 0.08 , 0.08 ]</td><td align="center" valign="middle" >[ − 0.08 , 0.08 ]</td><td align="center" valign="middle" >Negative values ϕ   1 are mapped into positive values of θ 1 and vice versa</td></tr></tbody></table></table-wrap><p>When it is assumed that the process is invertible MA(1), that is θ 1 is known, and it is required to determine the region of Non-Duality, ϕ   1 is determined in terms of θ 1 subject to − 1 &lt; ϕ   1 &lt; 1 using Equation (2.8). Hence, when moving from invertible MA(1) process to stationary AR(1) process, the region of breakdown of duality is determined using (2.1), and illustrated in <xref ref-type="table" rid="table2">Table 2</xref>.</p><p>Remark 2.1: As shown in <xref ref-type="table" rid="table1">Table 1</xref> and <xref ref-type="table" rid="table2">Table 2</xref>, if we allow beyond two or more decimal places, the intervals of breakdown of duality are the same for AR(1) process and MA(1) process. However, beyond three or more decimal places, the intervals are quite small and whose significance may be questionable. Therefore, we recommend that for breakdown of duality, one to three decimal places of the absolute difference between the lag k corresponding autocovariances of stationary AR(p) process and that for the invertible MA(p) process may be allowed.</p></sec><sec id="s2_2"><title>2.2. Non-Duality between AR(2) and MA(2) Processes</title><p>For the model and autocovariances of stationary autoregressive process of order two (AR(2)) [<xref ref-type="bibr" rid="scirp.115519-ref20">20</xref>]:</p><p>X ˜ t = ϕ   1 X ˜ t − 1 + ϕ   2 X ˜ t − 2 + e t   ;   e t ~ N ( 0 , σ 2 ) ,     ϕ   2 − ϕ   1 &lt; 1 ,   ϕ   2 + ϕ   1 &lt; 1 ,   − 1 &lt; ϕ   2 &lt; 1 (2.11)</p><p>R ​ AR ( 2 ) ( k ) = { ( 1 − ϕ   2 ) σ 2 ( 1 + ϕ   2 ) ( 1 − ϕ   2 + ϕ   1 ) ( 1 − ϕ   2 − ϕ   1 ) ,   k = 0 ϕ   1 σ 2 ( 1 + ϕ   2 ) ( 1 − ϕ   2 + ϕ   1 ) ( 1 − ϕ   2 − ϕ   1 ) ;   k = 1 ( ϕ   1 2 + ϕ   2 ( 1 − ϕ   2 ) ) σ 2 ( 1 + ϕ   2 ) ( 1 − ϕ   2 + ϕ   1 ) ( 1 − ϕ   2 − ϕ   1 ) ;   k = 2 ϕ   1 R ( k − 1 ) + ϕ   2 R ( k − 2 ) ,                               k &gt; 2 (2.12)</p><p>and for invertible moving average process of order one (MA(1)) [<xref ref-type="bibr" rid="scirp.115519-ref20">20</xref>]:</p><table-wrap id="table2" ><label><xref ref-type="table" rid="table2">Table 2</xref></label><caption><title> Regions of θ 1 and ϕ   1 for non-duality of MA(1) and AR(1) Processes</title></caption><table><tbody><thead><tr><th align="center" valign="middle"  rowspan="3"  >Degree of approximation allowable for h k</th><th align="center" valign="middle"  colspan="2"  >Region of Non-duality</th><th align="center" valign="middle"  rowspan="3"  >Remark</th></tr></thead><tr><td align="center" valign="middle" >MA(1) Process</td><td align="center" valign="middle" >AR(1) Process</td></tr><tr><td align="center" valign="middle" >θ 1</td><td align="center" valign="middle" >ϕ   1</td></tr><tr><td align="center" valign="middle" >1</td><td align="center" valign="middle" >[ − 0.47 , 0.47 ]</td><td align="center" valign="middle" >[ − 0.38 , 0.38 ]</td><td align="center" valign="middle" >Negative values θ 1 are mapped into positive values of ϕ   1 and vice versa</td></tr><tr><td align="center" valign="middle" >2</td><td align="center" valign="middle" >[ − 0.26 , 0.26 ]</td><td align="center" valign="middle" >[ − 0.24 , 0.24 ]</td><td align="center" valign="middle" >Negative values θ 1 are mapped into positive values of ϕ   1 and vice versa</td></tr><tr><td align="center" valign="middle" >3</td><td align="center" valign="middle" >[ − 0.14 , 0.14 ]</td><td align="center" valign="middle" >[ − 0.14 , 0.14 ]</td><td align="center" valign="middle" >Negative values θ 1 are mapped into positive values of ϕ   1 and vice versa</td></tr><tr><td align="center" valign="middle" >4</td><td align="center" valign="middle" >[ − 0.08 , 0.08 ]</td><td align="center" valign="middle" >[ − 0.08 , 0.08 ]</td><td align="center" valign="middle" >Negative values θ 1 are mapped into positive values of ϕ   1 and vice versa</td></tr></tbody></table></table-wrap><p>X ˜ t = e t − θ 1 e t − 1 − θ 2 e t − 2   ;     e t ~ N ( 0 , σ 2 ) ,   θ 2 − θ 1 &lt; 1 ,   θ 2 + θ 1 &lt; 1 ,     − 1 &lt; θ 2 &lt; 1 (2.13)</p><p>R MA ( 2 ) ( k ) = { σ 2 ( 1 + θ 1 2 + θ 2 2 ) ,     k = 0 − θ 1 ( 1 − θ 2 ) σ 2 ,     k = 1 − θ 2 σ 2 ,     k = 2 0 ,     k &gt; 2 (2.14)</p><p>By equating corresponding non-zero autocovariances from stationary AR(2) process and invertible MA(2) process respectively, we obtain</p><p>1 − ϕ   2 ( 1 + ϕ   2 ) ( 1 − ϕ   2 + ϕ   1 ) ( 1 − ϕ   2 − ϕ   1 ) = 1 + θ 1 2 + θ 2 2 (2.15)</p><p>ϕ   1 ( 1 + ϕ   2 ) ( 1 − ϕ   2 + ϕ   1 ) ( 1 − ϕ   2 − ϕ   1 ) = − θ 1 ( 1 − θ 2 ) (2.16)</p><p>ϕ   1 2 + ϕ 2 ( 1 − ϕ 2 ) ( 1 + ϕ   2 ) ( 1 − ϕ   2 + ϕ   1 ) ( 1 − ϕ   2 − ϕ   1 ) = − θ 2 (2.17)</p><p>From (2.15), we have</p><p>1 ( 1 + ϕ   2 ) ( 1 − ϕ   2 + ϕ   1 ) ( 1 − ϕ   2 − ϕ   1 ) = 1 + θ 1 2 + θ 2 2 1 − ϕ   2 (2.18)</p><p>From (2.16), we have</p><p>1 ( 1 + ϕ   2 ) ( 1 − ϕ   2 + ϕ   1 ) ( 1 − ϕ   2 − ϕ   1 ) = − θ 1 ( 1 − θ 2 ) ϕ   1 (2.19)</p><p>From (2.17)</p><p>1 ( 1 + ϕ   2 ) ( 1 − ϕ   2 + ϕ   1 ) ( 1 − ϕ   2 − ϕ   1 ) = − θ 2 ϕ   1 2 + ϕ   2 ( 1 − ϕ   2 ) (2.20)</p><p>Equating the right hand sides of (2.18), (2.19) and (2.20), we obtain</p><p>− θ 1 ( 1 − θ 2 ) ϕ   1 = − θ 2 ϕ   1 2 + ϕ   2 ( 1 − ϕ   2 ) = 1 ( 1 + ϕ   2 ) ( 1 − ϕ   2 + ϕ   1 ) ( 1 − ϕ   2 − ϕ   1 ) (2.21)</p><p>Hence, Equation (2.21) is the relational equation connecting ϕ   1 , ϕ   2 , θ 1 and θ 2 . Using transitivity rule, these three equations can be used to obtain the desired solutions. That is</p><p>− θ 1 ( 1 − θ 2 ) ϕ   1 = − θ 2 ϕ   1 2 + ϕ   2 ( 1 − ϕ   2 ) (2.22)</p><p>− θ 1 ( 1 − θ 2 ) ϕ   1 = 1 ( 1 + ϕ   2 ) ( 1 − ϕ   2 + ϕ   1 ) ( 1 − ϕ   2 − ϕ   1 ) (2.23)</p><p>− θ 2 ϕ   1 2 + ϕ   2 ( 1 − ϕ   2 )   =   1 ( 1 + ϕ   2 ) ( 1 − ϕ   2 + ϕ   1 ) ( 1 − ϕ   2 − ϕ   1 ) (2.24)</p><p>In considering the above three equations, two cases arise resulting in the Non-Duality region.</p><p>Case I: Non-Duality Region in movement from stationary AR(2) process to invertible MA(2) process.</p><p>Given the stationary AR(2) process, we determine θ 1 and θ 2 (in terms ϕ   1 and ϕ   2 ) that must satisfy the invertibility conditions explicitly from the relational Equation (2.24) as</p><p>θ 2 = − ( ϕ   1 2 + ϕ   2 ( 1 − ϕ   2 ) ) ( 1 + ϕ   2 ) ( 1 − ϕ   2 + ϕ   1 ) ( 1 − ϕ   2 − ϕ   1 ) = − ϕ   1 2 − ϕ   2 ( 1 − ϕ   2 ) ( 1 + ϕ   2 ) ( 1 − ϕ   2 + ϕ   1 ) ( 1 − ϕ   2 − ϕ   1 )   (2.25)</p><p>Substituting (2.25) into (2.23), we obtain θ 1 as</p><p>θ 1 = − ϕ   1 ( ( 1 + ϕ   2 ) ( 1 − ϕ   2 + ϕ   1 ) ( 1 − ϕ   2 − ϕ   1 ) ) + ( ϕ   1 2 + ϕ   2 ( 1 − ϕ   2 ) ) (2.26)</p><p>From the invertibility conditions of MA(2) process, | θ 2 | &lt; 1 implies that</p><p>| θ 2 | = | − ( ϕ   1 2 + ϕ   2 ( 1 − ϕ   2 ) ) ( 1 + ϕ   2 ) ( 1 − ϕ   2 + ϕ   1 ) ( 1 − ϕ   2 − ϕ   1 ) | &lt; 1 (2.27)</p><p>The expression (2.27) is added to the stationarity conditions to obtain the Non-duality region/conditions for movement from AR(2) to MA(2) processes as</p><p>ϕ   2 − ϕ   1 &lt; 1 ϕ   2 + ϕ   1 &lt; 1 − 1 &lt; ϕ   2 &lt; 1 } stationarity   conditions | − ( ϕ   1 2 + ϕ   2 ( 1 − ϕ   2 ) ) ( 1 + ϕ   2 ) ( 1 − ϕ   2 + ϕ   1 ) ( 1 − ϕ   2 − ϕ   1 ) | &lt; 1 } Non-duality   region (2.28)</p><p>This region (2.28) is illustrated graphically in <xref ref-type="fig" rid="fig1">Figure 1</xref>. Then, using (2.1), the region of breakdown of duality when moving from stationary AR(2) process to invertible MA(2) process is determined. This region determined is shown in <xref ref-type="table" rid="table3">Table 3</xref>.</p><table-wrap id="table3" ><label><xref ref-type="table" rid="table3">Table 3</xref></label><caption><title> Regions of ( ϕ 1 , ϕ 2 ) and ( θ 1 , θ 2 ) for non-duality of AR(2) and MA(2) processes</title></caption><table><tbody><thead><tr><th align="center" valign="middle"  rowspan="3"  >Degree of approximation allowable for h k</th><th align="center" valign="middle"  colspan="4"  >Region of Non-duality</th><th align="center" valign="middle"  rowspan="3"  >Remark</th></tr></thead><tr><td align="center" valign="middle"  colspan="2"  >AR(2) Process</td><td align="center" valign="middle"  colspan="2"  >MA(2) Process</td></tr><tr><td align="center" valign="middle" >ϕ   1</td><td align="center" valign="middle" >ϕ   2</td><td align="center" valign="middle" >θ 1</td><td align="center" valign="middle" >θ 2</td></tr><tr><td align="center" valign="middle" >1</td><td align="center" valign="middle" >[ − 0.30 , 0.30 ]</td><td align="center" valign="middle" >[ − 0.30 , 0.30 ]</td><td align="center" valign="middle" >[ − 0.37 , 0.37 ]</td><td align="center" valign="middle" >[ − 0.43 , 0.32 ]</td><td align="center" valign="middle" >positive values ( ϕ 1 , ϕ 2 ) are mapped into negative values of ( θ 1 , θ 2 ) and vice versa</td></tr><tr><td align="center" valign="middle" >2</td><td align="center" valign="middle" >[ − 0.30 , 0.30 ]</td><td align="center" valign="middle" >[ − 0.20 , 0.20 ]</td><td align="center" valign="middle" >[ − 0.30 , 0.30 ]</td><td align="center" valign="middle" >[ − 0.22 , 0.20 ]</td><td align="center" valign="middle" >positive values ( ϕ 1 , ϕ 2 ) are mapped into negative values of ( θ 1 , θ 2 ) and vice versa</td></tr><tr><td align="center" valign="middle" >3</td><td align="center" valign="middle" >[ − 0.10 , 0.10 ]</td><td align="center" valign="middle" >−0.10</td><td align="center" valign="middle" >[ − 0.10 , 0.10 ]</td><td align="center" valign="middle" >0.09</td><td align="center" valign="middle" >positive values ( ϕ 1 , ϕ 2 ) are mapped into negative values of ( θ 1 , θ 2 ) and vice versa</td></tr></tbody></table></table-wrap><p>Case II: Non-Duality region in movement from invertible MA(2) process to stationary AR(2) process.</p><p>Given the invertible MA(2) process, we determine the values of ( ϕ   1 and ϕ   2 ) that lead to break down in duality from Equation (2.22). Solving for ϕ   1 and ϕ   2 , the expression reduces to the quadratic Equation</p><p>ϕ   1 2 − [ θ   2 θ 1 ( 1 − θ 2 ) ] ϕ   1 + ϕ   2 ( 1 − ϕ   2 ) = 0 (2.29)</p><p>Equation (2.29) is a quadratic equation in both ϕ   1 and ϕ   2 . By either solving for ϕ   1 first in (2.29) or ϕ   2 first in (2.29), Case II breaks into two-sub cases. Case II (a) involves solving for ϕ   1 first in (2.29) and we obtain</p><p>ϕ   1 = θ 2 θ 1 ( 1 − θ 2 ) &#177; [ θ 2 θ 1 ( 1 − θ 2 ) ]   2 − 4 ϕ   2 ( 1 − ϕ   2 ) 2 (2.30)</p><p>for fixed θ 1 and θ 2 with − 1 &lt; ϕ   2 &lt; 1 . For real roots of ϕ   1 , it is requested that the discriminant</p><p>D = 4 ϕ   2 2 − 4 ϕ   2 + [ θ 2 θ 1 ( 1 − θ 2 ) ] 2 ≥ 0 (2.31)</p><p>For fixed values of θ 1 and θ 2 satisfying the invertibility conditions, Equation (2.31) is a quadratic inequality in ϕ   2 . First, we solve for ϕ   2 in</p><p>4 ϕ   2 2 − 4 ϕ   2 + [ θ 2 θ 1 ( 1 − θ 2 ) ] 2 = 0 (2.32)</p><p>to obtain</p><p>ϕ   2 = 1 &#177; 1 − [ θ 2 θ 1 ( 1 − θ 2 ) ] 2 2 (2.33)</p><p>Since (2.26) is a quadratic inequality, the roots of (2.33) split the interval for ϕ   2 , ϕ   2 ∈ ( − 1 , 1 ) , into three intervals [<xref ref-type="bibr" rid="scirp.115519-ref29">29</xref>] [<xref ref-type="bibr" rid="scirp.115519-ref30">30</xref>]. If we define</p><p>W = θ   2 θ 1 ( 1 − θ 2 ) . (2.34)</p><p>then, the intervals are ( − 1 , 1 − 1 − W 2 2 ) , [ 1 − 1 − W 2 2 , 1 + 1 − W 2 2 ] and ( 1 + 1 − W 2 2 , 1 ) .</p><p>From (2.33), it is clear that for two distinct real roots of ϕ   2 ;</p><p>[ θ 2 θ 1 ( 1 − θ 2 ) ] 2 &lt; 1 (2.35)</p><p>⇒ | θ 2 θ 1 ( 1 − θ 2 ) | &lt; 1 (2.36)</p><p>Similarly, Case II (b) involves solving for ϕ   2 first in (2.29) to obtain</p><p>ϕ   2 = 1 &#177; 1 + 4 ϕ   1 [ ϕ   1 − [ θ 2 θ 1 ( 1 − θ 2 ) ] ] 2 (2.37)</p><p>for fixed θ 1 and θ 2 with − 2 &lt; ϕ   1 &lt; 2 . For real roots of ϕ   2 ,</p><p>1 + 4 ϕ   1 [ ϕ   1 − [ θ 2 θ 1 ( 1 − θ 2 ) ] ] ≥ 0 (2.38)</p><p>Equation (2.38) is a quadratic inequality on ϕ   1 . Solving for ϕ   1 , we use</p><p>1 + 4 ϕ   1 [ ϕ   1 − [ θ 2 θ 1 ( 1 − θ 2 ) ] ] = 0 (2.39)</p><p>to obtain</p><p>ϕ   1 = θ 2 θ 1 ( 1 − θ 2 ) &#177; [ θ 2 θ 1 ( 1 − θ 2 ) ] 2 − 1 2 (2.40)</p><p>for fixed θ 1 and θ 2 . Since (2.38) is a quadratic inequality, (2.40) split the interval for ϕ   1 , ϕ   1 ∈ ( − 2 , 2 ) , into three intervals [<xref ref-type="bibr" rid="scirp.115519-ref30">30</xref>]. The intervals are:</p><p>( − 2 , W − W 2 − 1 2 ) , [ W − W 2 − 1 2 , W + W 2 − 1 2 ] and ( W + W 2 − 1 2 , 2 )</p><p>From (2.40), it is clear that for distinct real roots of ϕ   1 ;</p><p>[ θ 2 θ 1 ( 1 − θ 2 ) ] 2 &gt; 1 (2.41)</p><p>⇒ | θ 2 θ 1 ( 1 − θ 2 ) | &gt; 1 (2.42)</p><p>Equation (2.36) and (2.42) combined with the invertibility conditions gives what we call the Non-Duality conditions/region when going from MA(2) to AR(2) processes. The Non-Duality conditions/region when moving from MA(2) to AR(2) processes is given as</p><p>θ 2 − θ 1 &lt; 1 θ 2 + θ 1 &lt; 1 − 1 &lt; θ 2 &lt; 1 } invertibility   conditions | θ 2 θ 1 ( 1 − θ 2 ) | ≠ 1 } Non-duality   region (2.43)</p><p>See <xref ref-type="fig" rid="fig2">Figure 2</xref> for illustration of Equation (2.43). Then, using (2.1), the region of breakdown of duality when moving from invertible MA(2) process to stationary AR(2) process for case IIa and case IIb are determined and illustrated in <xref ref-type="table" rid="table4">Table 4</xref> and <xref ref-type="table" rid="table5">Table 5</xref> respectively.</p><table-wrap id="table4" ><label><xref ref-type="table" rid="table4">Table 4</xref></label><caption><title> Regions of ( θ 1 , θ 2 ) and ( ϕ   1 , ϕ   2 ) for non-duality of MA(2) and AR(2) processes</title></caption><table><tbody><thead><tr><th align="center" valign="middle"  rowspan="3"  >Degree of approximation allowable for h k</th><th align="center" valign="middle"  colspan="4"  >Region of Non-duality</th><th align="center" valign="middle"  rowspan="3"  >Remark</th></tr></thead><tr><td align="center" valign="middle"  colspan="2"  >MA(2) Process</td><td align="center" valign="middle"  colspan="2"  >AR(2) Process</td></tr><tr><td align="center" valign="middle" >θ 1</td><td align="center" valign="middle" >θ 2</td><td align="center" valign="middle" >ϕ   1</td><td align="center" valign="middle" >ϕ   2</td></tr><tr><td align="center" valign="middle" >1</td><td align="center" valign="middle" >0.10</td><td align="center" valign="middle" >−0.11</td><td align="center" valign="middle" >[ − 0.12 , − 0.07 ]</td><td align="center" valign="middle" >[ 0.07 , 0.12 ]</td><td align="center" valign="middle" >positive values ( θ 1 , θ 2 ) are mapped into negative values of ( ϕ   1 , ϕ   2 ) and vice versa</td></tr><tr><td align="center" valign="middle" >2</td><td align="center" valign="middle" >0.10</td><td align="center" valign="middle" >−0.11</td><td align="center" valign="middle" >−0.10</td><td align="center" valign="middle" >0.10</td><td align="center" valign="middle" >positive values ( θ 1 , θ 2 ) are mapped into negative values of ( ϕ   1 , ϕ   2 ) and vice versa</td></tr></tbody></table></table-wrap><table-wrap id="table5" ><label><xref ref-type="table" rid="table5">Table 5</xref></label><caption><title> Regions of ( θ 1 , θ 2 ) and ( ϕ   1 , ϕ   2 ) for non-duality of MA(2) and AR(2) processes</title></caption><table><tbody><thead><tr><th align="center" valign="middle"  rowspan="3"  >Degree of approximation allowable for h k</th><th align="center" valign="middle"  colspan="4"  >Region of Non-duality</th><th align="center" valign="middle"  rowspan="3"  >Remark</th></tr></thead><tr><td align="center" valign="middle"  colspan="2"  >MA(2) Process</td><td align="center" valign="middle"  colspan="2"  >AR(2) Process</td></tr><tr><td align="center" valign="middle" >θ 1</td><td align="center" valign="middle" >θ 2</td><td align="center" valign="middle" >ϕ   1</td><td align="center" valign="middle" >ϕ   2</td></tr><tr><td align="center" valign="middle" >1</td><td align="center" valign="middle" >−0.11</td><td align="center" valign="middle" >−0.22</td><td align="center" valign="middle" >[ 0.09 , 0.11 ]</td><td align="center" valign="middle" >[ 0.17 , 0.21 ]</td><td align="center" valign="middle" >positive values ( θ 1 , θ 2 ) are mapped into negative values of ( ϕ   1 , ϕ   2 ) and vice versa</td></tr><tr><td align="center" valign="middle" >2</td><td align="center" valign="middle" >−0.11</td><td align="center" valign="middle" >−0.22</td><td align="center" valign="middle" >0.10</td><td align="center" valign="middle" >0.20</td><td align="center" valign="middle" >positive values ( θ 1 , θ 2 ) are mapped into negative values of ( ϕ   1 , ϕ   2 ) and vice versa</td></tr></tbody></table></table-wrap></sec></sec><sec id="s3"><title>3. Empirical Examples</title><p>This section presents some empirical examples to illustrate the results obtained in Section 2. Both simulated and real life time series data were used for the illustration. The first set of simulations consist of one thousand (1000) stationary AR(2) series of 120 observations each, simulated using e t ~ N ( 0 , σ 2 ) and ( φ 1 , φ 2 ) = ( − 0.30 , − 0.30 ) which satisfy the non-duality conditions defined in Equation (2.28). The estimates of the autocorrelation function, acf ( ρ k ) and the partial autocorrelation function, pacf ( ϕ k k ) of the simulated series cut off after lag two. These indicate that the patterns in the series may be adequately described by either the stationary AR(2) process or the invertible MA(2) process. Since the series were simulated from stationary AR(2) process, an MA(2) model was fitted to the series. The estimate of the acf and the pacf of the residuals from the fitted MA(2) model all lie within 2 standard deviations from mean (zero) indicating that the fitted model is adequate. The estimates of the means and variances of the residuals are also not significantly different from 0 and 1 respectively. These indicate that the model adequately describes the pattern in the simulated series. The estimates of θ 1 and θ 2 , obtained using MINITAB 17 series software are shown in <xref ref-type="table" rid="table6">Table 6</xref> (for ten simulated series only for want of space). As <xref ref-type="table" rid="table6">Table 6</xref> shows, the estimates also: (i) satisfy the invertibility conditions and (ii) compare favourably well, in absolute terms, with those of stationary AR(2) process but with opposite signs. These indicate that a stationary AR(2) process can be adequately represented by an invertible MA(2) process contrary to the widely held duality concept.</p><p>The second set of simulations consists of one thousand (1000) invertible MA(2) series of 120 observations each, simulated using e t ~ N ( 0 , σ 2 ) and ( θ 1 , θ 2 ) = ( 0.37 , 0.27 ) which satisfy the non-duality conditions defined in Equation (2.43). The estimates of the autocorrelation function, acf ( ρ k ) and the partial autocorrelation function, pacf ( ϕ k k ) of the simulated series cut off after lag two. These indicate that the patterns in the series may be adequately described by either the invertible MA(2) process or the stationary AR(2) process. Since the series were simulated from invertible MA(2) process, the AR(2) model was fitted to the series. The estimates of the mean, variance, acf and the pacf of the residuals from the fitted AR(2) model indicate that the model adequately describes the pattern in the simulated series. The estimates of ϕ   1 and ϕ   2 obtained using MINITAB 17 series software shown in <xref ref-type="table" rid="table7">Table 7</xref> (for ten simulations for want of space) also: (i) satisfy the stationarity conditions and (ii) compare favourably well, in absolute terms, with those of invertible MA(2) process with opposite signs. These indicate that an invertible MA(2) process can be adequately represented by a stationary AR(2) process contrary to the widely held duality concept.</p><p>Furthermore, the breakdown of duality was illustrated using the real life data on the monthly average exchange rate of Naira per unit of CFA currency collected from Central Bank of Nigeria for the period January 2002 to December 2013 [<xref ref-type="bibr" rid="scirp.115519-ref31">31</xref>] [<xref ref-type="bibr" rid="scirp.115519-ref32">32</xref>]. The estimates of ρ k and ϕ k k of the original series ( X t ) shown</p><table-wrap id="table6" ><label><xref ref-type="table" rid="table6">Table 6</xref></label><caption><title> Estimates of parameters of MA(2) model fitted to simulated AR(2) process with ϕ   1 = − 0.30 , ϕ   2 = − 0.30 and e t ~ N ( 0 , 1 ) </title></caption><table><tbody><thead><tr><th align="center" valign="middle"  rowspan="2"  >S/No.</th><th align="center" valign="middle"  rowspan="2"  >i</th><th align="center" valign="middle"  colspan="4"  >AR(2) Model</th><th align="center" valign="middle"  rowspan="2"  >i</th><th align="center" valign="middle"  colspan="4"  >MA(2) Model</th></tr></thead><tr><td align="center" valign="middle" >ϕ ^ i</td><td align="center" valign="middle" >s t d ( ϕ ^ i )</td><td align="center" valign="middle" >t-value</td><td align="center" valign="middle" >σ ^ 2</td><td align="center" valign="middle" >θ ^ i</td><td align="center" valign="middle" >s t d ( θ ^ i )</td><td align="center" valign="middle" >t-value</td><td align="center" valign="middle" >σ ^ 2</td></tr><tr><td align="center" valign="middle"  rowspan="2"  >1</td><td align="center" valign="middle" >1</td><td align="center" valign="middle" >−0.3241</td><td align="center" valign="middle" >0.0943</td><td align="center" valign="middle" >−3.44</td><td align="center" valign="middle"  rowspan="2"  >1.1220</td><td align="center" valign="middle" >1</td><td align="center" valign="middle" >0.3105</td><td align="center" valign="middle" >0.0954</td><td align="center" valign="middle" >3.25</td><td align="center" valign="middle"  rowspan="2"  >1.1020</td></tr><tr><td align="center" valign="middle" >2</td><td align="center" valign="middle" >−0.3612</td><td align="center" valign="middle" >0.0953</td><td align="center" valign="middle" >−3.79</td><td align="center" valign="middle" >2</td><td align="center" valign="middle" >0.3286</td><td align="center" valign="middle" >0.0958</td><td align="center" valign="middle" >3.43</td></tr><tr><td align="center" valign="middle"  rowspan="2"  >2</td><td align="center" valign="middle" >1</td><td align="center" valign="middle" >−0.2162</td><td align="center" valign="middle" >0.0961</td><td align="center" valign="middle" >−2.25</td><td align="center" valign="middle"  rowspan="2"  >1.0890</td><td align="center" valign="middle" >1</td><td align="center" valign="middle" >0.2218</td><td align="center" valign="middle" >0.0974</td><td align="center" valign="middle" >2.28</td><td align="center" valign="middle"  rowspan="2"  >1.0900</td></tr><tr><td align="center" valign="middle" >2</td><td align="center" valign="middle" >−0.3130</td><td align="center" valign="middle" >0.0964</td><td align="center" valign="middle" >−3.25</td><td align="center" valign="middle" >2</td><td align="center" valign="middle" >0.2563</td><td align="center" valign="middle" >0.0975</td><td align="center" valign="middle" >2.63</td></tr><tr><td align="center" valign="middle"  rowspan="2"  >3</td><td align="center" valign="middle" >1</td><td align="center" valign="middle" >−0.2127</td><td align="center" valign="middle" >0.0974</td><td align="center" valign="middle" >−2.18</td><td align="center" valign="middle"  rowspan="2"  >0.8725</td><td align="center" valign="middle" >1</td><td align="center" valign="middle" >0.2718</td><td align="center" valign="middle" >0.0975</td><td align="center" valign="middle" >2.79</td><td align="center" valign="middle"  rowspan="2"  >0.8520</td></tr><tr><td align="center" valign="middle" >2</td><td align="center" valign="middle" >−0.3010</td><td align="center" valign="middle" >0.0973</td><td align="center" valign="middle" >−3.09</td><td align="center" valign="middle" >2</td><td align="center" valign="middle" >0.2762</td><td align="center" valign="middle" >0.0975</td><td align="center" valign="middle" >2.83</td></tr><tr><td align="center" valign="middle"  rowspan="2"  >4</td><td align="center" valign="middle" >1</td><td align="center" valign="middle" >−0.3098</td><td align="center" valign="middle" >0.0944</td><td align="center" valign="middle" >−3.28</td><td align="center" valign="middle"  rowspan="2"  >0.9103</td><td align="center" valign="middle" >1</td><td align="center" valign="middle" >0.3323</td><td align="center" valign="middle" >0.0979</td><td align="center" valign="middle" >3.39</td><td align="center" valign="middle"  rowspan="2"  >0.9220</td></tr><tr><td align="center" valign="middle" >2</td><td align="center" valign="middle" >−0.3606</td><td align="center" valign="middle" >0.0945</td><td align="center" valign="middle" >−3.82</td><td align="center" valign="middle" >2</td><td align="center" valign="middle" >0.2468</td><td align="center" valign="middle" >0.0981</td><td align="center" valign="middle" >2.52</td></tr><tr><td align="center" valign="middle"  rowspan="2"  >5</td><td align="center" valign="middle" >1</td><td align="center" valign="middle" >−0.2619</td><td align="center" valign="middle" >0.0934</td><td align="center" valign="middle" >−2.81</td><td align="center" valign="middle"  rowspan="2"  >1.1780</td><td align="center" valign="middle" >1</td><td align="center" valign="middle" >0.2009</td><td align="center" valign="middle" >0.0960</td><td align="center" valign="middle" >2.09</td><td align="center" valign="middle"  rowspan="2"  >1.2210</td></tr><tr><td align="center" valign="middle" >2</td><td align="center" valign="middle" >−0.3873</td><td align="center" valign="middle" >0.0934</td><td align="center" valign="middle" >−4.15</td><td align="center" valign="middle" >2</td><td align="center" valign="middle" >0.3390</td><td align="center" valign="middle" >0.0963</td><td align="center" valign="middle" >3.52</td></tr><tr><td align="center" valign="middle"  rowspan="2"  >6</td><td align="center" valign="middle" >1</td><td align="center" valign="middle" >−0.2957</td><td align="center" valign="middle" >0.0909</td><td align="center" valign="middle" >−3.25</td><td align="center" valign="middle"  rowspan="2"  >0.8452</td><td align="center" valign="middle" >1</td><td align="center" valign="middle" >0.2356</td><td align="center" valign="middle" >0.0946</td><td align="center" valign="middle" >2.49</td><td align="center" valign="middle"  rowspan="2"  >0.8851</td></tr><tr><td align="center" valign="middle" >2</td><td align="center" valign="middle" >−0.4419</td><td align="center" valign="middle" >0.0916</td><td align="center" valign="middle" >−4.82</td><td align="center" valign="middle" >2</td><td align="center" valign="middle" >0.3531</td><td align="center" valign="middle" >0.0953</td><td align="center" valign="middle" >3.71</td></tr><tr><td align="center" valign="middle"  rowspan="2"  >7</td><td align="center" valign="middle" >1</td><td align="center" valign="middle" >−0.2177</td><td align="center" valign="middle" >0.0961</td><td align="center" valign="middle" >−2.26</td><td align="center" valign="middle"  rowspan="2"  >1.0073</td><td align="center" valign="middle" >1</td><td align="center" valign="middle" >0.2896</td><td align="center" valign="middle" >0.0961</td><td align="center" valign="middle" >3.02</td><td align="center" valign="middle"  rowspan="2"  >0.9750</td></tr><tr><td align="center" valign="middle" >2</td><td align="center" valign="middle" >−0.3064</td><td align="center" valign="middle" >0.0962</td><td align="center" valign="middle" >−3.18</td><td align="center" valign="middle" >2</td><td align="center" valign="middle" >0.3080</td><td align="center" valign="middle" >0.0961</td><td align="center" valign="middle" >3.21</td></tr><tr><td align="center" valign="middle"  rowspan="2"  >8</td><td align="center" valign="middle" >1</td><td align="center" valign="middle" >−0.2970</td><td align="center" valign="middle" >0.0949</td><td align="center" valign="middle" >−3.13</td><td align="center" valign="middle"  rowspan="2"  >0.9185</td><td align="center" valign="middle" >1</td><td align="center" valign="middle" >0.3579</td><td align="center" valign="middle" >0.0972</td><td align="center" valign="middle" >3.68</td><td align="center" valign="middle"  rowspan="2"  >0.9009</td></tr><tr><td align="center" valign="middle" >2</td><td align="center" valign="middle" >−0.3395</td><td align="center" valign="middle" >0.0951</td><td align="center" valign="middle" >−3.57</td><td align="center" valign="middle" >2</td><td align="center" valign="middle" >0.2726</td><td align="center" valign="middle" >0.0972</td><td align="center" valign="middle" >2.80</td></tr><tr><td align="center" valign="middle"  rowspan="2"  >9</td><td align="center" valign="middle" >1</td><td align="center" valign="middle" >−0.2634</td><td align="center" valign="middle" >0.0953</td><td align="center" valign="middle" >−2.76</td><td align="center" valign="middle"  rowspan="2"  >1.092</td><td align="center" valign="middle" >1</td><td align="center" valign="middle" >0.2035</td><td align="center" valign="middle" >0.0983</td><td align="center" valign="middle" >2.07</td><td align="center" valign="middle"  rowspan="2"  >1.1390</td></tr><tr><td align="center" valign="middle" >2</td><td align="center" valign="middle" >−0.3477</td><td align="center" valign="middle" >0.0956</td><td align="center" valign="middle" >−3.64</td><td align="center" valign="middle" >2</td><td align="center" valign="middle" >0.2255</td><td align="center" valign="middle" >0.0983</td><td align="center" valign="middle" >2.29</td></tr><tr><td align="center" valign="middle"  rowspan="2"  >10</td><td align="center" valign="middle" >1</td><td align="center" valign="middle" >−0.3409</td><td align="center" valign="middle" >0.0947</td><td align="center" valign="middle" >−3.60</td><td align="center" valign="middle"  rowspan="2"  >0.9556</td><td align="center" valign="middle" >1</td><td align="center" valign="middle" >0.3399</td><td align="center" valign="middle" >0.0992</td><td align="center" valign="middle" >3.43</td><td align="center" valign="middle"  rowspan="2"  >0.9664</td></tr><tr><td align="center" valign="middle" >2</td><td align="center" valign="middle" >−0.3476</td><td align="center" valign="middle" >0.0949</td><td align="center" valign="middle" >−3.66</td><td align="center" valign="middle" >2</td><td align="center" valign="middle" >0.2084</td><td align="center" valign="middle" >0.1017</td><td align="center" valign="middle" >2.05</td></tr></tbody></table></table-wrap><table-wrap id="table7" ><label><xref ref-type="table" rid="table7">Table 7</xref></label><caption><title> Estimates of parameters of AR(2) model fitted to simulated MA(2) model with θ 1 = 0.37 , θ 2 = 0.27 and e t ~ N ( 0 , 1 ) </title></caption><table><tbody><thead><tr><th align="center" valign="middle"  rowspan="2"  >S/No.</th><th align="center" valign="middle"  rowspan="2"  >i</th><th align="center" valign="middle"  colspan="4"  >MA(2) Model</th><th align="center" valign="middle"  rowspan="2"  >i</th><th align="center" valign="middle"  colspan="4"  >AR(2) Model</th></tr></thead><tr><td align="center" valign="middle" >θ ^ i</td><td align="center" valign="middle" >s t d ( θ ^ i )</td><td align="center" valign="middle" >t-value</td><td align="center" valign="middle" >σ ^ 2</td><td align="center" valign="middle" >ϕ ^ i</td><td align="center" valign="middle" >s t d ( ϕ ^ i )</td><td align="center" valign="middle" >t-value</td><td align="center" valign="middle" >σ ^ 2</td></tr><tr><td align="center" valign="middle"  rowspan="2"  >1</td><td align="center" valign="middle" >1</td><td align="center" valign="middle" >0.3427</td><td align="center" valign="middle" >0.0981</td><td align="center" valign="middle" >3.49</td><td align="center" valign="middle"  rowspan="2"  >1.0136</td><td align="center" valign="middle" >1</td><td align="center" valign="middle" >−0.2615</td><td align="center" valign="middle" >0.0967</td><td align="center" valign="middle" >−2.70</td><td align="center" valign="middle"  rowspan="2"  >1.0450</td></tr><tr><td align="center" valign="middle" >2</td><td align="center" valign="middle" >0.2862</td><td align="center" valign="middle" >0.0984</td><td align="center" valign="middle" >2.91</td><td align="center" valign="middle" >2</td><td align="center" valign="middle" >−0.3528</td><td align="center" valign="middle" >0.0971</td><td align="center" valign="middle" >−3.63</td></tr><tr><td align="center" valign="middle"  rowspan="2"  >2</td><td align="center" valign="middle" >1</td><td align="center" valign="middle" >0.3513</td><td align="center" valign="middle" >0.0943</td><td align="center" valign="middle" >3.72</td><td align="center" valign="middle"  rowspan="2"  >1.0510</td><td align="center" valign="middle" >1</td><td align="center" valign="middle" >−0.2013</td><td align="center" valign="middle" >0.0964</td><td align="center" valign="middle" >−2.09</td><td align="center" valign="middle"  rowspan="2"  >1.1560</td></tr><tr><td align="center" valign="middle" >2</td><td align="center" valign="middle" >0.3412</td><td align="center" valign="middle" >0.0943</td><td align="center" valign="middle" >3.62</td><td align="center" valign="middle" >2</td><td align="center" valign="middle" >−0.3011</td><td align="center" valign="middle" >0.0966</td><td align="center" valign="middle" >−3.12</td></tr><tr><td align="center" valign="middle"  rowspan="2"  >3</td><td align="center" valign="middle" >1</td><td align="center" valign="middle" >0.3902</td><td align="center" valign="middle" >0.0929</td><td align="center" valign="middle" >4.20</td><td align="center" valign="middle"  rowspan="2"  >1.1770</td><td align="center" valign="middle" >1</td><td align="center" valign="middle" >−0.3004</td><td align="center" valign="middle" >0.0953</td><td align="center" valign="middle" >−3.15</td><td align="center" valign="middle"  rowspan="2"  >1.2770</td></tr><tr><td align="center" valign="middle" >2</td><td align="center" valign="middle" >0.3940</td><td align="center" valign="middle" >0.0933</td><td align="center" valign="middle" >4.23</td><td align="center" valign="middle" >2</td><td align="center" valign="middle" >−0.3500</td><td align="center" valign="middle" >0.0953</td><td align="center" valign="middle" >−3.67</td></tr><tr><td align="center" valign="middle"  rowspan="2"  >4</td><td align="center" valign="middle" >1</td><td align="center" valign="middle" >0.3629</td><td align="center" valign="middle" >0.0967</td><td align="center" valign="middle" >3.75</td><td align="center" valign="middle"  rowspan="2"  >1.0590</td><td align="center" valign="middle" >1</td><td align="center" valign="middle" >−0.2879</td><td align="center" valign="middle" >0.0973</td><td align="center" valign="middle" >−2.96</td><td align="center" valign="middle"  rowspan="2"  >1.1230</td></tr><tr><td align="center" valign="middle" >2</td><td align="center" valign="middle" >0.2958</td><td align="center" valign="middle" >0.0970</td><td align="center" valign="middle" >3.05</td><td align="center" valign="middle" >2</td><td align="center" valign="middle" >−0.2709</td><td align="center" valign="middle" >0.0973</td><td align="center" valign="middle" >−2.78</td></tr><tr><td align="center" valign="middle"  rowspan="2"  >5</td><td align="center" valign="middle" >1</td><td align="center" valign="middle" >0.3322</td><td align="center" valign="middle" >0.0977</td><td align="center" valign="middle" >3.40</td><td align="center" valign="middle"  rowspan="2"  >0.9375</td><td align="center" valign="middle" >1</td><td align="center" valign="middle" >−0.2472</td><td align="center" valign="middle" >0.0970</td><td align="center" valign="middle" >−2.55</td><td align="center" valign="middle"  rowspan="2"  >0.9769</td></tr><tr><td align="center" valign="middle" >2</td><td align="center" valign="middle" >0.2830</td><td align="center" valign="middle" >0.0977</td><td align="center" valign="middle" >2.90</td><td align="center" valign="middle" >2</td><td align="center" valign="middle" >−0.2901</td><td align="center" valign="middle" >0.0994</td><td align="center" valign="middle" >−2.92</td></tr><tr><td align="center" valign="middle"  rowspan="2"  >6</td><td align="center" valign="middle" >1</td><td align="center" valign="middle" >0.4133</td><td align="center" valign="middle" >0.0975</td><td align="center" valign="middle" >4.24</td><td align="center" valign="middle"  rowspan="2"  >0.9956</td><td align="center" valign="middle" >1</td><td align="center" valign="middle" >−0.3220</td><td align="center" valign="middle" >0.0963</td><td align="center" valign="middle" >−3.34</td><td align="center" valign="middle"  rowspan="2"  >1.0670</td></tr><tr><td align="center" valign="middle" >2</td><td align="center" valign="middle" >0.2674</td><td align="center" valign="middle" >0.0991</td><td align="center" valign="middle" >2.70</td><td align="center" valign="middle" >2</td><td align="center" valign="middle" >−0.3053</td><td align="center" valign="middle" >0.0962</td><td align="center" valign="middle" >−3.17</td></tr><tr><td align="center" valign="middle"  rowspan="2"  >7</td><td align="center" valign="middle" >1</td><td align="center" valign="middle" >0.2955</td><td align="center" valign="middle" >0.0983</td><td align="center" valign="middle" >3.01</td><td align="center" valign="middle"  rowspan="2"  >0.9634</td><td align="center" valign="middle" >1</td><td align="center" valign="middle" >−0.2575</td><td align="center" valign="middle" >0.0967</td><td align="center" valign="middle" >−2.66</td><td align="center" valign="middle"  rowspan="2"  >0.9719</td></tr><tr><td align="center" valign="middle" >2</td><td align="center" valign="middle" >0.2476</td><td align="center" valign="middle" >0.0990</td><td align="center" valign="middle" >2.50</td><td align="center" valign="middle" >2</td><td align="center" valign="middle" >−0.2996</td><td align="center" valign="middle" >0.0983</td><td align="center" valign="middle" >−3.05</td></tr><tr><td align="center" valign="middle"  rowspan="2"  >8</td><td align="center" valign="middle" >1</td><td align="center" valign="middle" >0.3655</td><td align="center" valign="middle" >0.0987</td><td align="center" valign="middle" >3.70</td><td align="center" valign="middle"  rowspan="2"  >1.0770</td><td align="center" valign="middle" >1</td><td align="center" valign="middle" >−0.3685</td><td align="center" valign="middle" >0.0933</td><td align="center" valign="middle" >−3.95</td><td align="center" valign="middle"  rowspan="2"  >1.0540</td></tr><tr><td align="center" valign="middle" >2</td><td align="center" valign="middle" >0.2279</td><td align="center" valign="middle" >0.0987</td><td align="center" valign="middle" >2.31</td><td align="center" valign="middle" >2</td><td align="center" valign="middle" >−0.3906</td><td align="center" valign="middle" >0.0941</td><td align="center" valign="middle" >−4.15</td></tr><tr><td align="center" valign="middle"  rowspan="2"  >9</td><td align="center" valign="middle" >1</td><td align="center" valign="middle" >0.3554</td><td align="center" valign="middle" >0.0976</td><td align="center" valign="middle" >3.64</td><td align="center" valign="middle"  rowspan="2"  >1.2330</td><td align="center" valign="middle" >1</td><td align="center" valign="middle" >−0.3564</td><td align="center" valign="middle" >0.0954</td><td align="center" valign="middle" >−4.74</td><td align="center" valign="middle"  rowspan="2"  >1.2280</td></tr><tr><td align="center" valign="middle" >2</td><td align="center" valign="middle" >0.2808</td><td align="center" valign="middle" >0.0978</td><td align="center" valign="middle" >2.87</td><td align="center" valign="middle" >2</td><td align="center" valign="middle" >−0.3401</td><td align="center" valign="middle" >0.0961</td><td align="center" valign="middle" >−3.54</td></tr><tr><td align="center" valign="middle"  rowspan="2"  >10</td><td align="center" valign="middle" >1</td><td align="center" valign="middle" >0.2389</td><td align="center" valign="middle" >0.0958</td><td align="center" valign="middle" >2.49</td><td align="center" valign="middle"  rowspan="2"  >1.0290</td><td align="center" valign="middle" >1</td><td align="center" valign="middle" >−0.2598</td><td align="center" valign="middle" >0.0940</td><td align="center" valign="middle" >−2.76</td><td align="center" valign="middle"  rowspan="2"  >1.0260</td></tr><tr><td align="center" valign="middle" >2</td><td align="center" valign="middle" >0.3301</td><td align="center" valign="middle" >0.0963</td><td align="center" valign="middle" >3.43</td><td align="center" valign="middle" >2</td><td align="center" valign="middle" >−0.3869</td><td align="center" valign="middle" >0.0941</td><td align="center" valign="middle" >−4.11</td></tr></tbody></table></table-wrap><p>in <xref ref-type="table" rid="table8">Table 8</xref> suggest that the series requires differencing to remove non-stationarity in mean. The estimates of ρ k and ϕ k k of the first order differenced series ( ( 1 − B ) X t ) shown in <xref ref-type="table" rid="table8">Table 8</xref>, indicates that both ρ k and ϕ k k cut off after lag one. This suggests that the pattern in the differenced series may be adequately described by either AR(1) process or MA(1) process. The estimates ( ρ ^ k and ϕ ^ k k ) of the residuals from the fitted models (AR(1) and MA(1)) also shown in <xref ref-type="table" rid="table8">Table 8</xref>, indicate that both models adequately describe the pattern in the series [<xref ref-type="bibr" rid="scirp.115519-ref33">33</xref>]. The estimate ( ϕ ^   1 = − 0.2369 ) of ϕ   1 in the AR(1) process, shown in <xref ref-type="table" rid="table9">Table 9</xref> satisfies the stationarity condition, while the estimate ( θ ^ 1 = 0 .2581 ) of θ 1 in MA(1) process also shown in <xref ref-type="table" rid="table9">Table 9</xref> satisfy the invertibility condition. In addittion, both estimates ( ϕ ^   1 and θ ^ 1 ) compare favourably well in absolute terms, but with opposite signs. Here again contrary to the widely held duality concept, these indicate that a stationary AR(1) process can be adequately represented by an invertible MA(1) process.</p><p>The second real life data used to illustrate the breakdown of duality is the monthly All Shares Index of the Nigeria Stock Exchange (NSE), for the period January 1, 1985 to December 31, 2007, collected from the CBN Statistical Bulletin [<xref ref-type="bibr" rid="scirp.115519-ref31">31</xref>] [<xref ref-type="bibr" rid="scirp.115519-ref32">32</xref>] [<xref ref-type="bibr" rid="scirp.115519-ref34">34</xref>]. Following the procedure of [<xref ref-type="bibr" rid="scirp.115519-ref35">35</xref>] [<xref ref-type="bibr" rid="scirp.115519-ref36">36</xref>], the original series was shown to require logarithmic transformation to stabilize its variance. The estimates of ρ k and ϕ k k of the transformed series ( Y t ) shown in <xref ref-type="table" rid="table1">Table 1</xref>0, suggest that the series requires differencing to remove non-stationarity in mean. The estimates ( ρ ^ k and ϕ ^ k k ) of acf and pacf of the first order differenced series ( Z t ) also shown in <xref ref-type="table" rid="table1">Table 1</xref>0, indicate that both ρ ^ k and ϕ ^ k k cut off after lag five. These suggest that the pattern in the series may be adequately described by either AR(5) model or MA(5) model. Both models were fitted to the series and the estimates ( ρ ^ k and ϕ ^ k k ) of acf and pacf of the residuals from the fitted models shown in <xref ref-type="table" rid="table1">Table 1</xref>0, indicate that both models adequately describe the pattern in the series. However, some of the estimates of the parameters of the fitted</p><table-wrap id="table8" ><label><xref ref-type="table" rid="table8">Table 8</xref></label><caption><title> The estimates of ρ k and ϕ k k of X t , ( 1 − B ) X t and residuals from the fitted models (AR(1) and MA(1) Models)</title></caption><table><tbody><thead><tr><th align="center" valign="middle"  rowspan="4"  >k</th><th align="center" valign="middle"  colspan="8"  >CFA</th></tr></thead><tr><td align="center" valign="middle"  colspan="2"   rowspan="2"  >X t</td><td align="center" valign="middle"  colspan="2"   rowspan="2"  >( 1 − B ) X t</td><td align="center" valign="middle"  colspan="4"  >Residuals ( e t )</td></tr><tr><td align="center" valign="middle"  colspan="2"  >AR(1)</td><td align="center" valign="middle"  colspan="2"  >MA(1)</td></tr><tr><td align="center" valign="middle" >ρ ^ k</td><td align="center" valign="middle" >ϕ ^ k k</td><td align="center" valign="middle" >ρ ^ k</td><td align="center" valign="middle" >ϕ ^ k k</td><td align="center" valign="middle" >ρ ^ k</td><td align="center" valign="middle" >ϕ ^ k k</td><td align="center" valign="middle" >ρ ^ k</td><td align="center" valign="middle" >ϕ ^ k k</td></tr><tr><td align="center" valign="middle" >1</td><td align="center" valign="middle" >0.94</td><td align="center" valign="middle" >0.94</td><td align="center" valign="middle" >−0.25</td><td align="center" valign="middle" >−0.25</td><td align="center" valign="middle" >−0.03</td><td align="center" valign="middle" >−0.03</td><td align="center" valign="middle" >−0.01</td><td align="center" valign="middle" >−0.01</td></tr><tr><td align="center" valign="middle" >2</td><td align="center" valign="middle" >0.90</td><td align="center" valign="middle" >0.13</td><td align="center" valign="middle" >−0.05</td><td align="center" valign="middle" >−0.11</td><td align="center" valign="middle" >−0.09</td><td align="center" valign="middle" >−0.09</td><td align="center" valign="middle" >−0.03</td><td align="center" valign="middle" >−0.03</td></tr><tr><td align="center" valign="middle" >3</td><td align="center" valign="middle" >0.86</td><td align="center" valign="middle" >0.03</td><td align="center" valign="middle" >0.08</td><td align="center" valign="middle" >0.04</td><td align="center" valign="middle" >0.07</td><td align="center" valign="middle" >0.06</td><td align="center" valign="middle" >0.06</td><td align="center" valign="middle" >0.06</td></tr><tr><td align="center" valign="middle" >4</td><td align="center" valign="middle" >0.82</td><td align="center" valign="middle" >−0.05</td><td align="center" valign="middle" >−0.04</td><td align="center" valign="middle" >−0.01</td><td align="center" valign="middle" >−0.03</td><td align="center" valign="middle" >−0.04</td><td align="center" valign="middle" >−0.03</td><td align="center" valign="middle" >−0.03</td></tr><tr><td align="center" valign="middle" >5</td><td align="center" valign="middle" >0.78</td><td align="center" valign="middle" >−0.01</td><td align="center" valign="middle" >−0.02</td><td align="center" valign="middle" >−0.03</td><td align="center" valign="middle" >−0.02</td><td align="center" valign="middle" >−0.01</td><td align="center" valign="middle" >−0.02</td><td align="center" valign="middle" >−0.02</td></tr><tr><td align="center" valign="middle" >6</td><td align="center" valign="middle" >0.74</td><td align="center" valign="middle" >0.01</td><td align="center" valign="middle" >0.04</td><td align="center" valign="middle" >0.02</td><td align="center" valign="middle" >0.02</td><td align="center" valign="middle" >0.01</td><td align="center" valign="middle" >0.02</td><td align="center" valign="middle" >0.01</td></tr><tr><td align="center" valign="middle" >7</td><td align="center" valign="middle" >0.71</td><td align="center" valign="middle" >0.04</td><td align="center" valign="middle" >−0.07</td><td align="center" valign="middle" >−0.06</td><td align="center" valign="middle" >−0.07</td><td align="center" valign="middle" >−0.07</td><td align="center" valign="middle" >−0.07</td><td align="center" valign="middle" >−0.07</td></tr><tr><td align="center" valign="middle" >8</td><td align="center" valign="middle" >0.68</td><td align="center" valign="middle" >0.07</td><td align="center" valign="middle" >0.01</td><td align="center" valign="middle" >−0.02</td><td align="center" valign="middle" >−0.01</td><td align="center" valign="middle" >−0.01</td><td align="center" valign="middle" >−0.01</td><td align="center" valign="middle" >−0.01</td></tr><tr><td align="center" valign="middle" >9</td><td align="center" valign="middle" >0.66</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >−0.01</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >−0.02</td><td align="center" valign="middle" >−0.01</td><td align="center" valign="middle" >−0.02</td></tr><tr><td align="center" valign="middle" >10</td><td align="center" valign="middle" >0.63</td><td align="center" valign="middle" >−0.02</td><td align="center" valign="middle" >−0.03</td><td align="center" valign="middle" >−0.03</td><td align="center" valign="middle" >−0.04</td><td align="center" valign="middle" >−0.04</td><td align="center" valign="middle" >−0.05</td><td align="center" valign="middle" >−0.05</td></tr><tr><td align="center" valign="middle" >11</td><td align="center" valign="middle" >0.61</td><td align="center" valign="middle" >−0.02</td><td align="center" valign="middle" >−0.03</td><td align="center" valign="middle" >−0.05</td><td align="center" valign="middle" >−0.07</td><td align="center" valign="middle" >−0.08</td><td align="center" valign="middle" >−0.08</td><td align="center" valign="middle" >−0.09</td></tr><tr><td align="center" valign="middle" >12</td><td align="center" valign="middle" >0.59</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >−0.12</td><td align="center" valign="middle" >−0.16</td><td align="center" valign="middle" >−0.15</td><td align="center" valign="middle" >−0.17</td><td align="center" valign="middle" >−0.16</td><td align="center" valign="middle" >−0.18</td></tr><tr><td align="center" valign="middle" >13</td><td align="center" valign="middle" >0.57</td><td align="center" valign="middle" >0.06</td><td align="center" valign="middle" >−0.02</td><td align="center" valign="middle" >−0.10</td><td align="center" valign="middle" >−0.07</td><td align="center" valign="middle" >−0.10</td><td align="center" valign="middle" >−0.09</td><td align="center" valign="middle" >−0.10</td></tr><tr><td align="center" valign="middle" >14</td><td align="center" valign="middle" >0.55</td><td align="center" valign="middle" >0.04</td><td align="center" valign="middle" >−0.08</td><td align="center" valign="middle" >−0.16</td><td align="center" valign="middle" >−0.10</td><td align="center" valign="middle" >−0.15</td><td align="center" valign="middle" >−0.12</td><td align="center" valign="middle" >−0.15</td></tr><tr><td align="center" valign="middle" >15</td><td align="center" valign="middle" >0.54</td><td align="center" valign="middle" >0.06</td><td align="center" valign="middle" >−0.02</td><td align="center" valign="middle" >−0.10</td><td align="center" valign="middle" >−0.04</td><td align="center" valign="middle" >−0.08</td><td align="center" valign="middle" >−0.05</td><td align="center" valign="middle" >−0.07</td></tr><tr><td align="center" valign="middle" >16</td><td align="center" valign="middle" >0.54</td><td align="center" valign="middle" >0.02</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >−0.07</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >−0.06</td><td align="center" valign="middle" >−0.01</td><td align="center" valign="middle" >−0.05</td></tr><tr><td align="center" valign="middle" >17</td><td align="center" valign="middle" >0.53</td><td align="center" valign="middle" >−0.01</td><td align="center" valign="middle" >0.01</td><td align="center" valign="middle" >−0.03</td><td align="center" valign="middle" >−0.01</td><td align="center" valign="middle" >−0.04</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >−0.03</td></tr><tr><td align="center" valign="middle" >18</td><td align="center" valign="middle" >0.52</td><td align="center" valign="middle" >−0.02</td><td align="center" valign="middle" >−0.08</td><td align="center" valign="middle" >−0.12</td><td align="center" valign="middle" >−0.05</td><td align="center" valign="middle" >−0.10</td><td align="center" valign="middle" >−0.04</td><td align="center" valign="middle" >−0.08</td></tr><tr><td align="center" valign="middle" >19</td><td align="center" valign="middle" >0.51</td><td align="center" valign="middle" >0.06</td><td align="center" valign="middle" >0.14</td><td align="center" valign="middle" >0.06</td><td align="center" valign="middle" >0.16</td><td align="center" valign="middle" >0.11</td><td align="center" valign="middle" >0.16</td><td align="center" valign="middle" >0.11</td></tr><tr><td align="center" valign="middle" >20</td><td align="center" valign="middle" >0.49</td><td align="center" valign="middle" >−0.06</td><td align="center" valign="middle" >0.08</td><td align="center" valign="middle" >0.12</td><td align="center" valign="middle" >0.10</td><td align="center" valign="middle" >0.09</td><td align="center" valign="middle" >0.11</td><td align="center" valign="middle" >0.10</td></tr><tr><td align="center" valign="middle" >21</td><td align="center" valign="middle" >0.47</td><td align="center" valign="middle" >−0.09</td><td align="center" valign="middle" >−0.08</td><td align="center" valign="middle" >−0.02</td><td align="center" valign="middle" >−0.04</td><td align="center" valign="middle" >−0.02</td><td align="center" valign="middle" >−0.03</td><td align="center" valign="middle" >−0.03</td></tr><tr><td align="center" valign="middle" >22</td><td align="center" valign="middle" >0.45</td><td align="center" valign="middle" >−0.01</td><td align="center" valign="middle" >0.13</td><td align="center" valign="middle" >0.10</td><td align="center" valign="middle" >0.11</td><td align="center" valign="middle" >0.10</td><td align="center" valign="middle" >0.12</td><td align="center" valign="middle" >0.08</td></tr><tr><td align="center" valign="middle" >23</td><td align="center" valign="middle" >0.42</td><td align="center" valign="middle" >−0.08</td><td align="center" valign="middle" >−0.06</td><td align="center" valign="middle" >−0.04</td><td align="center" valign="middle" >−0.04</td><td align="center" valign="middle" >−0.08</td><td align="center" valign="middle" >−0.04</td><td align="center" valign="middle" >−0.09</td></tr><tr><td align="center" valign="middle" >24</td><td align="center" valign="middle" >0.39</td><td align="center" valign="middle" >−0.01</td><td align="center" valign="middle" >−0.02</td><td align="center" valign="middle" >−0.06</td><td align="center" valign="middle" >−0.04</td><td align="center" valign="middle" >−0.07</td><td align="center" valign="middle" >−0.04</td><td align="center" valign="middle" >−0.08</td></tr><tr><td align="center" valign="middle" >25</td><td align="center" valign="middle" >0.36</td><td align="center" valign="middle" >−0.03</td><td align="center" valign="middle" >−0.01</td><td align="center" valign="middle" >−0.13</td><td align="center" valign="middle" >−0.03</td><td align="center" valign="middle" >−0.14</td><td align="center" valign="middle" >−0.02</td><td align="center" valign="middle" >−0.13</td></tr><tr><td align="center" valign="middle" >26</td><td align="center" valign="middle" >0.35</td><td align="center" valign="middle" >0.09</td><td align="center" valign="middle" >−0.03</td><td align="center" valign="middle" >−0.13</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >−0.08</td><td align="center" valign="middle" >0.01</td><td align="center" valign="middle" >−0.07</td></tr><tr><td align="center" valign="middle" >27</td><td align="center" valign="middle" >0.34</td><td align="center" valign="middle" >0.10</td><td align="center" valign="middle" >0.13</td><td align="center" valign="middle" >0.06</td><td align="center" valign="middle" >0.15</td><td align="center" valign="middle" >0.11</td><td align="center" valign="middle" >0.15</td><td align="center" valign="middle" >0.11</td></tr><tr><td align="center" valign="middle" >28</td><td align="center" valign="middle" >0.31</td><td align="center" valign="middle" >−0.22</td><td align="center" valign="middle" >0.07</td><td align="center" valign="middle" >0.09</td><td align="center" valign="middle" >0.09</td><td align="center" valign="middle" >0.06</td><td align="center" valign="middle" >0.09</td><td align="center" valign="middle" >0.06</td></tr><tr><td align="center" valign="middle" >29</td><td align="center" valign="middle" >0.28</td><td align="center" valign="middle" >−0.01</td><td align="center" valign="middle" >−0.11</td><td align="center" valign="middle" >−0.04</td><td align="center" valign="middle" >−0.09</td><td align="center" valign="middle" >−0.06</td><td align="center" valign="middle" >−0.08</td><td align="center" valign="middle" >−0.06</td></tr><tr><td align="center" valign="middle" >30</td><td align="center" valign="middle" >0.26</td><td align="center" valign="middle" >0.01</td><td align="center" valign="middle" >0.06</td><td align="center" valign="middle" >0.01</td><td align="center" valign="middle" >0.04</td><td align="center" valign="middle" >0.03</td><td align="center" valign="middle" >0.04</td><td align="center" valign="middle" >0.03</td></tr><tr><td align="center" valign="middle" >31</td><td align="center" valign="middle" >0.24</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.01</td><td align="center" valign="middle" >0.05</td><td align="center" valign="middle" >0.01</td><td align="center" valign="middle" >0.05</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.05</td></tr><tr><td align="center" valign="middle" >32</td><td align="center" valign="middle" >0.22</td><td align="center" valign="middle" >−0.04</td><td align="center" valign="middle" >−0.06</td><td align="center" valign="middle" >0.01</td><td align="center" valign="middle" >−0.07</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >−0.07</td><td align="center" valign="middle" >0.00</td></tr><tr><td align="center" valign="middle" >33</td><td align="center" valign="middle" >0.20</td><td align="center" valign="middle" >0.02</td><td align="center" valign="middle" >−0.01</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >−0.04</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >−0.04</td><td align="center" valign="middle" >0.00</td></tr><tr><td align="center" valign="middle" >34</td><td align="center" valign="middle" >0.18</td><td align="center" valign="middle" >0.02</td><td align="center" valign="middle" >−0.04</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >−0.04</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >−0.05</td><td align="center" valign="middle" >0.00</td></tr><tr><td align="center" valign="middle" >35</td><td align="center" valign="middle" >0.18</td><td align="center" valign="middle" >0.03</td><td align="center" valign="middle" >0.01</td><td align="center" valign="middle" >0.01</td><td align="center" valign="middle" >0.01</td><td align="center" valign="middle" >0.01</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.00</td></tr><tr><td align="center" valign="middle" >36</td><td align="center" valign="middle" >0.18</td><td align="center" valign="middle" >0.06</td><td align="center" valign="middle" ></td><td align="center" valign="middle" ></td><td align="center" valign="middle" ></td><td align="center" valign="middle" ></td><td align="center" valign="middle" ></td><td align="center" valign="middle" ></td></tr></tbody></table></table-wrap><table-wrap id="table9" ><label><xref ref-type="table" rid="table9">Table 9</xref></label><caption><title> Estimates of parameters of AR(1) process and MA(1) process fitted to the monthly average exchange rate of Naira per unit of CFA currency</title></caption><table><tbody><thead><tr><th align="center" valign="middle"  colspan="4"  >AR(1) Model</th><th align="center" valign="middle"  colspan="4"  >MA(1) Model</th></tr></thead><tr><td align="center" valign="middle" >Coefficient</td><td align="center" valign="middle" >Estimate</td><td align="center" valign="middle" >Std Error</td><td align="center" valign="middle" >t-value</td><td align="center" valign="middle" >Coefficient</td><td align="center" valign="middle" >Estimate</td><td align="center" valign="middle" >Std Error</td><td align="center" valign="middle" >t-value</td></tr><tr><td align="center" valign="middle" >ϕ   1</td><td align="center" valign="middle" >−0.2369</td><td align="center" valign="middle" >0.0816</td><td align="center" valign="middle" >−2.90</td><td align="center" valign="middle" >θ 1</td><td align="center" valign="middle" >0.2581</td><td align="center" valign="middle" >0.0811</td><td align="center" valign="middle" >3.18</td></tr><tr><td align="center" valign="middle" >σ ^ 2</td><td align="center" valign="middle"  colspan="3"  >0.0002</td><td align="center" valign="middle" >σ ^ 2</td><td align="center" valign="middle"  colspan="3"  >0.0002</td></tr></tbody></table></table-wrap><table-wrap id="table10" ><label><xref ref-type="table" rid="table1">Table 1</xref>0</label><caption><title> The estimates of ρ k and ϕ k k of X t , ( 1 − B ) X t and residuals from the fitted models (AR(5) process and MA(5) process)</title></caption><table><tbody><thead><tr><th align="center" valign="middle"  rowspan="4"  >k</th><th align="center" valign="middle"  colspan="8"  >NSE ALL SHARES INDEX</th></tr></thead><tr><td align="center" valign="middle"  colspan="2"   rowspan="2"  >Y t = log e X t</td><td align="center" valign="middle"  colspan="2"   rowspan="2"  >Z t = ( 1 − B ) Y t</td><td align="center" valign="middle"  colspan="4"  >Residuals ( e t )</td></tr><tr><td align="center" valign="middle"  colspan="2"  >AR(5)</td><td align="center" valign="middle"  colspan="2"  >MA(5)</td></tr><tr><td align="center" valign="middle" >ρ ^ k</td><td align="center" valign="middle" >ϕ ^ k k</td><td align="center" valign="middle" >ρ ^ k</td><td align="center" valign="middle" >ϕ ^ k k</td><td align="center" valign="middle" >ρ ^ k</td><td align="center" valign="middle" >ϕ ^ k k</td><td align="center" valign="middle" >ρ ^ k</td><td align="center" valign="middle" >ϕ ^ k k</td></tr><tr><td align="center" valign="middle" >1</td><td align="center" valign="middle" >0.99</td><td align="center" valign="middle" >0.99</td><td align="center" valign="middle" >0.19</td><td align="center" valign="middle" >0.19</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.00</td></tr><tr><td align="center" valign="middle" >2</td><td align="center" valign="middle" >0.98</td><td align="center" valign="middle" >−0.01</td><td align="center" valign="middle" >0.15</td><td align="center" valign="middle" >0.12</td><td align="center" valign="middle" >0.01</td><td align="center" valign="middle" >0.01</td><td align="center" valign="middle" >−0.01</td><td align="center" valign="middle" >−0.01</td></tr><tr><td align="center" valign="middle" >3</td><td align="center" valign="middle" >0.97</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.06</td><td align="center" valign="middle" >0.01</td><td align="center" valign="middle" >−0.02</td><td align="center" valign="middle" >−0.02</td><td align="center" valign="middle" >0.02</td><td align="center" valign="middle" >0.02</td></tr><tr><td align="center" valign="middle" >4</td><td align="center" valign="middle" >0.96</td><td align="center" valign="middle" >−0.01</td><td align="center" valign="middle" >−0.02</td><td align="center" valign="middle" >−0.06</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.00</td></tr><tr><td align="center" valign="middle" >5</td><td align="center" valign="middle" >0.95</td><td align="center" valign="middle" >−0.01</td><td align="center" valign="middle" >0.18</td><td align="center" valign="middle" >0.19</td><td align="center" valign="middle" >0.01</td><td align="center" valign="middle" >0.01</td><td align="center" valign="middle" >0.01</td><td align="center" valign="middle" >0.01</td></tr><tr><td align="center" valign="middle" >6</td><td align="center" valign="middle" >0.93</td><td align="center" valign="middle" >−0.03</td><td align="center" valign="middle" >0.04</td><td align="center" valign="middle" >−0.02</td><td align="center" valign="middle" >−0.01</td><td align="center" valign="middle" >−0.01</td><td align="center" valign="middle" >0.03</td><td align="center" valign="middle" >0.03</td></tr><tr><td align="center" valign="middle" >7</td><td align="center" valign="middle" >0.92</td><td align="center" valign="middle" >−0.01</td><td align="center" valign="middle" >0.02</td><td align="center" valign="middle" >−0.04</td><td align="center" valign="middle" >−0.05</td><td align="center" valign="middle" >−0.05</td><td align="center" valign="middle" >−0.01</td><td align="center" valign="middle" >−0.01</td></tr><tr><td align="center" valign="middle" >8</td><td align="center" valign="middle" >0.91</td><td align="center" valign="middle" >−0.01</td><td align="center" valign="middle" >0.08</td><td align="center" valign="middle" >0.08</td><td align="center" valign="middle" >0.07</td><td align="center" valign="middle" >0.07</td><td align="center" valign="middle" >0.08</td><td align="center" valign="middle" >0.08</td></tr><tr><td align="center" valign="middle" >9</td><td align="center" valign="middle" >0.90</td><td align="center" valign="middle" >−0.01</td><td align="center" valign="middle" >0.05</td><td align="center" valign="middle" >0.05</td><td align="center" valign="middle" >0.04</td><td align="center" valign="middle" >0.04</td><td align="center" valign="middle" >0.02</td><td align="center" valign="middle" >0.02</td></tr><tr><td align="center" valign="middle" >10</td><td align="center" valign="middle" >0.89</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.06</td><td align="center" valign="middle" >−0.01</td><td align="center" valign="middle" >0.02</td><td align="center" valign="middle" >0.02</td><td align="center" valign="middle" >0.05</td><td align="center" valign="middle" >0.05</td></tr><tr><td align="center" valign="middle" >11</td><td align="center" valign="middle" >0.88</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >−0.01</td><td align="center" valign="middle" >−0.04</td><td align="center" valign="middle" >−0.03</td><td align="center" valign="middle" >−0.03</td><td align="center" valign="middle" >−0.03</td><td align="center" valign="middle" >−0.03</td></tr><tr><td align="center" valign="middle" >12</td><td align="center" valign="middle" >0.87</td><td align="center" valign="middle" >0.01</td><td align="center" valign="middle" >−0.03</td><td align="center" valign="middle" >−0.02</td><td align="center" valign="middle" >−0.02</td><td align="center" valign="middle" >−0.01</td><td align="center" valign="middle" >−0.01</td><td align="center" valign="middle" >−0.01</td></tr><tr><td align="center" valign="middle" >13</td><td align="center" valign="middle" >0.86</td><td align="center" valign="middle" >0.01</td><td align="center" valign="middle" >−0.08</td><td align="center" valign="middle" >−0.10</td><td align="center" valign="middle" >−0.12</td><td align="center" valign="middle" >−0.12</td><td align="center" valign="middle" >−0.10</td><td align="center" valign="middle" >−0.11</td></tr><tr><td align="center" valign="middle" >14</td><td align="center" valign="middle" >0.84</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.04</td><td align="center" valign="middle" >0.07</td><td align="center" valign="middle" >0.03</td><td align="center" valign="middle" >0.02</td><td align="center" valign="middle" >0.03</td><td align="center" valign="middle" >0.02</td></tr><tr><td align="center" valign="middle" >15</td><td align="center" valign="middle" >0.83</td><td align="center" valign="middle" >−0.01</td><td align="center" valign="middle" >0.04</td><td align="center" valign="middle" >0.04</td><td align="center" valign="middle" >0.01</td><td align="center" valign="middle" >0.02</td><td align="center" valign="middle" >0.02</td><td align="center" valign="middle" >0.01</td></tr><tr><td align="center" valign="middle" >16</td><td align="center" valign="middle" >0.82</td><td align="center" valign="middle" >−0.01</td><td align="center" valign="middle" >0.10</td><td align="center" valign="middle" >0.08</td><td align="center" valign="middle" >0.11</td><td align="center" valign="middle" >0.11</td><td align="center" valign="middle" >0.11</td><td align="center" valign="middle" >0.11</td></tr><tr><td align="center" valign="middle" >17</td><td align="center" valign="middle" >0.81</td><td align="center" valign="middle" >−0.02</td><td align="center" valign="middle" >0.02</td><td align="center" valign="middle" >−0.03</td><td align="center" valign="middle" >−0.01</td><td align="center" valign="middle" >−0.02</td><td align="center" valign="middle" >−0.01</td><td align="center" valign="middle" >−0.02</td></tr><tr><td align="center" valign="middle" >18</td><td align="center" valign="middle" >0.80</td><td align="center" valign="middle" >0.02</td><td align="center" valign="middle" >0.02</td><td align="center" valign="middle" >0.03</td><td align="center" valign="middle" >0.02</td><td align="center" valign="middle" >0.01</td><td align="center" valign="middle" >0.01</td><td align="center" valign="middle" >0.00</td></tr><tr><td align="center" valign="middle" >19</td><td align="center" valign="middle" >0.79</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.07</td><td align="center" valign="middle" >0.05</td><td align="center" valign="middle" >0.07</td><td align="center" valign="middle" >0.07</td><td align="center" valign="middle" >0.06</td><td align="center" valign="middle" >0.06</td></tr><tr><td align="center" valign="middle" >20</td><td align="center" valign="middle" >0.78</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.08</td><td align="center" valign="middle" >0.05</td><td align="center" valign="middle" >0.10</td><td align="center" valign="middle" >0.10</td><td align="center" valign="middle" >0.09</td><td align="center" valign="middle" >0.10</td></tr><tr><td align="center" valign="middle" >21</td><td align="center" valign="middle" >0.77</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >−0.02</td><td align="center" valign="middle" >−0.09</td><td align="center" valign="middle" >−0.05</td><td align="center" valign="middle" >−0.03</td><td align="center" valign="middle" >−0.05</td><td align="center" valign="middle" >−0.04</td></tr><tr><td align="center" valign="middle" >22</td><td align="center" valign="middle" >0.76</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >−0.03</td><td align="center" valign="middle" >−0.02</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.01</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >−0.01</td></tr><tr><td align="center" valign="middle" >23</td><td align="center" valign="middle" >0.75</td><td align="center" valign="middle" >−0.01</td><td align="center" valign="middle" >−0.07</td><td align="center" valign="middle" >−0.05</td><td align="center" valign="middle" >−0.04</td><td align="center" valign="middle" >−0.03</td><td align="center" valign="middle" >−0.04</td><td align="center" valign="middle" >−0.04</td></tr><tr><td align="center" valign="middle" >24</td><td align="center" valign="middle" >0.74</td><td align="center" valign="middle" >−0.01</td><td align="center" valign="middle" >−0.09</td><td align="center" valign="middle" >−0.11</td><td align="center" valign="middle" >−0.04</td><td align="center" valign="middle" >−0.07</td><td align="center" valign="middle" >−0.04</td><td align="center" valign="middle" >−0.07</td></tr><tr><td align="center" valign="middle" >25</td><td align="center" valign="middle" >0.73</td><td align="center" valign="middle" >−0.01</td><td align="center" valign="middle" >−0.11</td><td align="center" valign="middle" >−0.13</td><td align="center" valign="middle" >−0.10</td><td align="center" valign="middle" >−0.12</td><td align="center" valign="middle" >−0.10</td><td align="center" valign="middle" >−0.12</td></tr><tr><td align="center" valign="middle" >26</td><td align="center" valign="middle" >0.72</td><td align="center" valign="middle" >−0.01</td><td align="center" valign="middle" >−0.10</td><td align="center" valign="middle" >−0.04</td><td align="center" valign="middle" >−0.07</td><td align="center" valign="middle" >−0.08</td><td align="center" valign="middle" >−0.05</td><td align="center" valign="middle" >−0.08</td></tr><tr><td align="center" valign="middle" >27</td><td align="center" valign="middle" >0.71</td><td align="center" valign="middle" >−0.02</td><td align="center" valign="middle" >−0.13</td><td align="center" valign="middle" >−0.08</td><td align="center" valign="middle" >−0.10</td><td align="center" valign="middle" >−0.10</td><td align="center" valign="middle" >−0.10</td><td align="center" valign="middle" >−0.10</td></tr><tr><td align="center" valign="middle" >28</td><td align="center" valign="middle" >0.70</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >−0.06</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.01</td><td align="center" valign="middle" >−0.02</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >−0.02</td></tr><tr><td align="center" valign="middle" >29</td><td align="center" valign="middle" >0.69</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >−0.11</td><td align="center" valign="middle" >−0.05</td><td align="center" valign="middle" >−0.10</td><td align="center" valign="middle" >−0.09</td><td align="center" valign="middle" >−0.10</td><td align="center" valign="middle" >−0.08</td></tr><tr><td align="center" valign="middle" >30</td><td align="center" valign="middle" >0.68</td><td align="center" valign="middle" >0.04</td><td align="center" valign="middle" >−0.03</td><td align="center" valign="middle" >0.04</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >−0.01</td><td align="center" valign="middle" >0.01</td><td align="center" valign="middle" >0.01</td></tr><tr><td align="center" valign="middle" >31</td><td align="center" valign="middle" >0.67</td><td align="center" valign="middle" >−0.01</td><td align="center" valign="middle" >0.02</td><td align="center" valign="middle" >0.08</td><td align="center" valign="middle" >0.03</td><td align="center" valign="middle" >0.04</td><td align="center" valign="middle" >0.02</td><td align="center" valign="middle" >0.05</td></tr><tr><td align="center" valign="middle" >32</td><td align="center" valign="middle" >0.66</td><td align="center" valign="middle" >−0.01</td><td align="center" valign="middle" >−0.02</td><td align="center" valign="middle" >0.04</td><td align="center" valign="middle" >0.02</td><td align="center" valign="middle" >0.04</td><td align="center" valign="middle" >0.01</td><td align="center" valign="middle" >0.04</td></tr><tr><td align="center" valign="middle" >33</td><td align="center" valign="middle" >0.65</td><td align="center" valign="middle" >−0.01</td><td align="center" valign="middle" >−0.04</td><td align="center" valign="middle" >−0.02</td><td align="center" valign="middle" >−0.03</td><td align="center" valign="middle" >0.01</td><td align="center" valign="middle" >−0.03</td><td align="center" valign="middle" >0.02</td></tr><tr><td align="center" valign="middle" >34</td><td align="center" valign="middle" >0.63</td><td align="center" valign="middle" >−0.04</td><td align="center" valign="middle" >−0.02</td><td align="center" valign="middle" >0.01</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >−0.01</td><td align="center" valign="middle" >0.01</td></tr><tr><td align="center" valign="middle" >35</td><td align="center" valign="middle" >0.62</td><td align="center" valign="middle" >0.01</td><td align="center" valign="middle" >−0.03</td><td align="center" valign="middle" >−0.01</td><td align="center" valign="middle" >−0.05</td><td align="center" valign="middle" >−0.05</td><td align="center" valign="middle" >−0.06</td><td align="center" valign="middle" >−0.05</td></tr><tr><td align="center" valign="middle" >36</td><td align="center" valign="middle" >0.61</td><td align="center" valign="middle" >−0.02</td><td align="center" valign="middle" >0.11</td><td align="center" valign="middle" >0.10</td><td align="center" valign="middle" >0.14</td><td align="center" valign="middle" >0.11</td><td align="center" valign="middle" >0.13</td><td align="center" valign="middle" >0.12</td></tr><tr><td align="center" valign="middle" >37</td><td align="center" valign="middle" >0.60</td><td align="center" valign="middle" >−0.02</td><td align="center" valign="middle" >0.03</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.03</td><td align="center" valign="middle" >0.05</td><td align="center" valign="middle" >0.03</td><td align="center" valign="middle" >0.05</td></tr><tr><td align="center" valign="middle" >38</td><td align="center" valign="middle" >0.59</td><td align="center" valign="middle" >−0.01</td><td align="center" valign="middle" >−0.02</td><td align="center" valign="middle" >−0.07</td><td align="center" valign="middle" >−0.02</td><td align="center" valign="middle" >−0.05</td><td align="center" valign="middle" >−0.03</td><td align="center" valign="middle" >−0.05</td></tr><tr><td align="center" valign="middle" >39</td><td align="center" valign="middle" >0.58</td><td align="center" valign="middle" >−0.01</td><td align="center" valign="middle" >−0.04</td><td align="center" valign="middle" >−0.06</td><td align="center" valign="middle" >−0.04</td><td align="center" valign="middle" >−0.07</td><td align="center" valign="middle" >−0.05</td><td align="center" valign="middle" >−0.08</td></tr><tr><td align="center" valign="middle" >40</td><td align="center" valign="middle" >0.57</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.04</td><td align="center" valign="middle" >0.04</td><td align="center" valign="middle" >0.02</td><td align="center" valign="middle" >0.04</td><td align="center" valign="middle" >0.02</td></tr><tr><td align="center" valign="middle" >41</td><td align="center" valign="middle" >0.56</td><td align="center" valign="middle" >−0.02</td><td align="center" valign="middle" >−0.01</td><td align="center" valign="middle" >−0.01</td><td align="center" valign="middle" >−0.02</td><td align="center" valign="middle" >0.01</td><td align="center" valign="middle" >−0.02</td><td align="center" valign="middle" >0.01</td></tr><tr><td align="center" valign="middle" >42</td><td align="center" valign="middle" >0.54</td><td align="center" valign="middle" >−0.03</td><td align="center" valign="middle" >−0.03</td><td align="center" valign="middle" >−0.04</td><td align="center" valign="middle" >−0.03</td><td align="center" valign="middle" >−0.04</td><td align="center" valign="middle" >−0.04</td><td align="center" valign="middle" >−0.04</td></tr><tr><td align="center" valign="middle" >43</td><td align="center" valign="middle" >0.53</td><td align="center" valign="middle" >−0.02</td><td align="center" valign="middle" >−0.06</td><td align="center" valign="middle" >0.01</td><td align="center" valign="middle" >−0.04</td><td align="center" valign="middle" >0.02</td><td align="center" valign="middle" >−0.04</td><td align="center" valign="middle" >0.00</td></tr><tr><td align="center" valign="middle" >44</td><td align="center" valign="middle" >0.52</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >−0.04</td><td align="center" valign="middle" >0.03</td><td align="center" valign="middle" >−0.01</td><td align="center" valign="middle" >0.03</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.02</td></tr><tr><td align="center" valign="middle" >45</td><td align="center" valign="middle" >0.51</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >−0.05</td><td align="center" valign="middle" >−0.02</td><td align="center" valign="middle" >−0.05</td><td align="center" valign="middle" >−0.02</td><td align="center" valign="middle" >−0.05</td><td align="center" valign="middle" >−0.01</td></tr><tr><td align="center" valign="middle" >46</td><td align="center" valign="middle" >0.50</td><td align="center" valign="middle" >0.01</td><td align="center" valign="middle" >−0.02</td><td align="center" valign="middle" >−0.02</td><td align="center" valign="middle" >−0.02</td><td align="center" valign="middle" >−0.02</td><td align="center" valign="middle" >−0.01</td><td align="center" valign="middle" >−0.02</td></tr><tr><td align="center" valign="middle" >47</td><td align="center" valign="middle" >0.48</td><td align="center" valign="middle" >−0.02</td><td align="center" valign="middle" >0.01</td><td align="center" valign="middle" >0.05</td><td align="center" valign="middle" >0.03</td><td align="center" valign="middle" >0.05</td><td align="center" valign="middle" >0.03</td><td align="center" valign="middle" >0.04</td></tr><tr><td align="center" valign="middle" >48</td><td align="center" valign="middle" >0.47</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >−0.04</td><td align="center" valign="middle" >−0.05</td><td align="center" valign="middle" >−0.01</td><td align="center" valign="middle" >−0.01</td><td align="center" valign="middle" >−0.01</td><td align="center" valign="middle" >−0.02</td></tr><tr><td align="center" valign="middle" >49</td><td align="center" valign="middle" >0.46</td><td align="center" valign="middle" >0.01</td><td align="center" valign="middle" >−0.08</td><td align="center" valign="middle" >−0.08</td><td align="center" valign="middle" >−0.08</td><td align="center" valign="middle" >−0.06</td><td align="center" valign="middle" >−0.09</td><td align="center" valign="middle" >−0.06</td></tr><tr><td align="center" valign="middle" >50</td><td align="center" valign="middle" >0.45</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >−0.01</td><td align="center" valign="middle" >0.01</td><td align="center" valign="middle" >−0.03</td><td align="center" valign="middle" >0.01</td><td align="center" valign="middle" >−0.04</td></tr><tr><td align="center" valign="middle" >51</td><td align="center" valign="middle" >0.44</td><td align="center" valign="middle" >−0.01</td><td align="center" valign="middle" >0.03</td><td align="center" valign="middle" >0.01</td><td align="center" valign="middle" >0.04</td><td align="center" valign="middle" >0.01</td><td align="center" valign="middle" >0.03</td><td align="center" valign="middle" >0.00</td></tr><tr><td align="center" valign="middle" >52</td><td align="center" valign="middle" >0.43</td><td align="center" valign="middle" >0.01</td><td align="center" valign="middle" >0.06</td><td align="center" valign="middle" >−0.02</td><td align="center" valign="middle" >0.09</td><td align="center" valign="middle" >0.01</td><td align="center" valign="middle" >0.08</td><td align="center" valign="middle" >0.02</td></tr><tr><td align="center" valign="middle" >53</td><td align="center" valign="middle" >0.42</td><td align="center" valign="middle" >−0.01</td><td align="center" valign="middle" >−0.03</td><td align="center" valign="middle" >−0.06</td><td align="center" valign="middle" >−0.03</td><td align="center" valign="middle" >−0.05</td><td align="center" valign="middle" >−0.03</td><td align="center" valign="middle" >−0.05</td></tr><tr><td align="center" valign="middle" >54</td><td align="center" valign="middle" >0.41</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >−0.05</td><td align="center" valign="middle" >−0.05</td><td align="center" valign="middle" >−0.05</td><td align="center" valign="middle" >−0.06</td><td align="center" valign="middle" >−0.05</td><td align="center" valign="middle" >−0.06</td></tr><tr><td align="center" valign="middle" >55</td><td align="center" valign="middle" >0.40</td><td align="center" valign="middle" >−0.01</td><td align="center" valign="middle" >−0.05</td><td align="center" valign="middle" >−0.05</td><td align="center" valign="middle" >−0.03</td><td align="center" valign="middle" >−0.07</td><td align="center" valign="middle" >−0.03</td><td align="center" valign="middle" >−0.06</td></tr><tr><td align="center" valign="middle" >56</td><td align="center" valign="middle" >0.38</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >−0.01</td><td align="center" valign="middle" >−0.02</td><td align="center" valign="middle" >0.03</td><td align="center" valign="middle" >−0.04</td><td align="center" valign="middle" >0.02</td><td align="center" valign="middle" >−0.03</td></tr><tr><td align="center" valign="middle" >57</td><td align="center" valign="middle" >0.37</td><td align="center" valign="middle" >−0.01</td><td align="center" valign="middle" >−0.06</td><td align="center" valign="middle" >−0.03</td><td align="center" valign="middle" >−0.07</td><td align="center" valign="middle" >−0.06</td><td align="center" valign="middle" >−0.08</td><td align="center" valign="middle" >−0.06</td></tr><tr><td align="center" valign="middle" >58</td><td align="center" valign="middle" >0.36</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >−0.03</td><td align="center" valign="middle" >0.03</td><td align="center" valign="middle" >−0.03</td><td align="center" valign="middle" >−0.01</td><td align="center" valign="middle" >−0.02</td><td align="center" valign="middle" >−0.01</td></tr><tr><td align="center" valign="middle" >59</td><td align="center" valign="middle" >0.35</td><td align="center" valign="middle" >−0.01</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.05</td><td align="center" valign="middle" >0.02</td><td align="center" valign="middle" >0.03</td><td align="center" valign="middle" >0.02</td><td align="center" valign="middle" >0.04</td></tr><tr><td align="center" valign="middle" >60</td><td align="center" valign="middle" >0.34</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.02</td><td align="center" valign="middle" >0.05</td><td align="center" valign="middle" >0.03</td><td align="center" valign="middle" >0.03</td><td align="center" valign="middle" >0.03</td><td align="center" valign="middle" >0.03</td></tr><tr><td align="center" valign="middle" >61</td><td align="center" valign="middle" >0.33</td><td align="center" valign="middle" >0.01</td><td align="center" valign="middle" >0.03</td><td align="center" valign="middle" >0.05</td><td align="center" valign="middle" >0.01</td><td align="center" valign="middle" >0.05</td><td align="center" valign="middle" >0.01</td><td align="center" valign="middle" >0.05</td></tr><tr><td align="center" valign="middle" >62</td><td align="center" valign="middle" >0.32</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.03</td><td align="center" valign="middle" >0.06</td><td align="center" valign="middle" >0.04</td><td align="center" valign="middle" >0.07</td><td align="center" valign="middle" >0.04</td><td align="center" valign="middle" >0.07</td></tr></tbody></table></table-wrap><p>models shown in <xref ref-type="table" rid="table1">Table 1</xref>1 are not significant. Therefore, the subset models were fitted to the series following the selection of subset time series models by [<xref ref-type="bibr" rid="scirp.115519-ref37">37</xref>]</p><table-wrap id="table11" ><label><xref ref-type="table" rid="table1">Table 1</xref>1</label><caption><title> Estimates of parameters of AR(5) model and MA(5) model fitted to the monthly all shares index of the Nigeria Stock Exchange (NSE)</title></caption><table><tbody><thead><tr><th align="center" valign="middle"  colspan="4"  >AR(5)</th><th align="center" valign="middle"  colspan="4"  >MA(5)</th></tr></thead><tr><td align="center" valign="middle" >Coefficient</td><td align="center" valign="middle" >Estimate</td><td align="center" valign="middle" >Std Error</td><td align="center" valign="middle" >t-value</td><td align="center" valign="middle" >Coefficient</td><td align="center" valign="middle" >Estimate</td><td align="center" valign="middle" >Std Error</td><td align="center" valign="middle" >t-value</td></tr><tr><td align="center" valign="middle" >Constant ϕ   0</td><td align="center" valign="middle" >0.0136</td><td align="center" valign="middle" >0.0029</td><td align="center" valign="middle" >4.75</td><td align="center" valign="middle" >Constant θ 0</td><td align="center" valign="middle" >0.0228</td><td align="center" valign="middle" >0.0042</td><td align="center" valign="middle" >5.42</td></tr><tr><td align="center" valign="middle" >ϕ   1</td><td align="center" valign="middle" >0.1745</td><td align="center" valign="middle" >0.0599</td><td align="center" valign="middle" >2.91</td><td align="center" valign="middle" >θ 1</td><td align="center" valign="middle" >−0.1741</td><td align="center" valign="middle" >0.0602</td><td align="center" valign="middle" >−2.89</td></tr><tr><td align="center" valign="middle" >ϕ   2</td><td align="center" valign="middle" >0.1220</td><td align="center" valign="middle" >0.0607</td><td align="center" valign="middle" >2.01</td><td align="center" valign="middle" >θ 2</td><td align="center" valign="middle" >−0.1756</td><td align="center" valign="middle" >0.0612</td><td align="center" valign="middle" >−2.87</td></tr><tr><td align="center" valign="middle" >ϕ   3</td><td align="center" valign="middle" >−0.0015</td><td align="center" valign="middle" >0.0612</td><td align="center" valign="middle" >−0.02</td><td align="center" valign="middle" >θ 3</td><td align="center" valign="middle" >−0.0156</td><td align="center" valign="middle" >0.0621</td><td align="center" valign="middle" >−0.25</td></tr><tr><td align="center" valign="middle" >ϕ   4</td><td align="center" valign="middle" >−0.0895</td><td align="center" valign="middle" >0.0607</td><td align="center" valign="middle" >−1.47</td><td align="center" valign="middle" >θ 4</td><td align="center" valign="middle" >0.0656</td><td align="center" valign="middle" >0.0612</td><td align="center" valign="middle" >1.07</td></tr><tr><td align="center" valign="middle" >ϕ   5</td><td align="center" valign="middle" >0.1965</td><td align="center" valign="middle" >0.0603</td><td align="center" valign="middle" >3.26</td><td align="center" valign="middle" >θ 5</td><td align="center" valign="middle" >−0.1711</td><td align="center" valign="middle" >0.0606</td><td align="center" valign="middle" >−2.82</td></tr><tr><td align="center" valign="middle" >σ ^ 2</td><td align="center" valign="middle"  colspan="3"  >0.0022</td><td align="center" valign="middle" >σ ^ 2</td><td align="center" valign="middle"  colspan="3"  >0.0022</td></tr></tbody></table></table-wrap><table-wrap id="table12" ><label><xref ref-type="table" rid="table1">Table 1</xref>2</label><caption><title> Estimates of parameters of subset AR(5) model and subset MA(5) model for the models fitted to the monthly all shares index of the Nigeria Stock Exchange (NSE)</title></caption><table><tbody><thead><tr><th align="center" valign="middle"  colspan="4"  >AR(5) SUBSET</th><th align="center" valign="middle"  colspan="4"  >MA(5) SUBSET</th></tr></thead><tr><td align="center" valign="middle" >Coefficient</td><td align="center" valign="middle" >Estimate</td><td align="center" valign="middle" >Std Error</td><td align="center" valign="middle" >t-value</td><td align="center" valign="middle" >Coefficient</td><td align="center" valign="middle" >Estimate</td><td align="center" valign="middle" >Std Error</td><td align="center" valign="middle" >t-value</td></tr><tr><td align="center" valign="middle" >Constant ϕ   0</td><td align="center" valign="middle" >0.0126</td><td align="center" valign="middle" >0.0036</td><td align="center" valign="middle" >3.47</td><td align="center" valign="middle" >Constant θ 0</td><td align="center" valign="middle" >0.0202</td><td align="center" valign="middle" >0.0038</td><td align="center" valign="middle" >5.31</td></tr><tr><td align="center" valign="middle" >ϕ   1</td><td align="center" valign="middle" >0.1697</td><td align="center" valign="middle" >0.0599</td><td align="center" valign="middle" >2.83</td><td align="center" valign="middle" >θ 1</td><td align="center" valign="middle" >−0.1648</td><td align="center" valign="middle" >0.0404</td><td align="center" valign="middle" >−4.07</td></tr><tr><td align="center" valign="middle" >ϕ   2</td><td align="center" valign="middle" >0.1092</td><td align="center" valign="middle" >0.0602</td><td align="center" valign="middle" >1.82</td><td align="center" valign="middle" >θ 2</td><td align="center" valign="middle" >−0.1793</td><td align="center" valign="middle" >0.0454</td><td align="center" valign="middle" >−3.95</td></tr><tr><td align="center" valign="middle" >ϕ   5</td><td align="center" valign="middle" >0.1801</td><td align="center" valign="middle" >0.0594</td><td align="center" valign="middle" >3.03</td><td align="center" valign="middle" >θ 5</td><td align="center" valign="middle" >−0.1774</td><td align="center" valign="middle" >0.0388</td><td align="center" valign="middle" >−4.57</td></tr><tr><td align="center" valign="middle" >σ ^ 2</td><td align="center" valign="middle"  colspan="3"  >0.0022</td><td align="center" valign="middle" >σ ^ 2</td><td align="center" valign="middle"  colspan="3"  >0.0022</td></tr></tbody></table></table-wrap><p>and the non-linear least squares method of estimation of parameters by [<xref ref-type="bibr" rid="scirp.115519-ref38">38</xref>]. The estimates of the parameters of the subset AR(5) model and the subset MA(5) model shown in <xref ref-type="table" rid="table1">Table 1</xref>2 compare favourably well in absolute terms with opposite signs. Contrary to the widely held duality concept, these indicate that an AR(5) series can be adequately represented by an MA(5) model and conversely.</p></sec><sec id="s4"><title>4. Conclusions</title><p>In summary, this study has demonstrated analytically and empirically that the concept of duality that a finite order stationary autoregressive process of order p (AR(p)) stationary is equivalent to an infinite order moving average (MA) process and invertible moving average of order q (MA(q)) is equivalent to an infinite order autoregressive (AR) process is not universally true. Specifically, this study constructed regions of breakdown of duality starting from AR(p) to MA(p) processes and from MA(p) to AR(p) processes for p = 1, 2. These regions, designated as “Non-duality” regions in this study, have been illustrated mathematically and graphically. In these regions (a) both the Autocorrelation function and the Partial Autocorrelation function of the AR process and MA process cuts off after equal lags (b) a finite AR model can be adequately represented by a finite MA model of equal order and conversely with the same error variance and (c) negative values of the parameters of the AR process are mapped into positive values of the parameters of the equivalent MA process and conversely.</p><p>In view of these, it has been recommended that the concept of duality should be treated with caution in analysis of time series data.</p></sec><sec id="s5"><title>Conflicts of Interest</title><p>The authors declare no conflicts of interest regarding the publication of this paper.</p></sec><sec id="s6"><title>Cite this paper</title><p>Onyemachi, E., Iwueze, I.S. and Nwogu, E.C. 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