<?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">OJG</journal-id><journal-title-group><journal-title>Open Journal of Geology</journal-title></journal-title-group><issn pub-type="epub">2161-7570</issn><publisher><publisher-name>Scientific Research Publishing</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.4236/ojg.2015.55021</article-id><article-id pub-id-type="publisher-id">OJG-56133</article-id><article-categories><subj-group subj-group-type="heading"><subject>Articles</subject></subj-group><subj-group subj-group-type="Discipline-v2"><subject>Earth&amp;Environmental Sciences</subject></subj-group></article-categories><title-group><article-title>
 
 
  Presentation of Empirical Equations for Estimating Internal Friction Angle of GW and GC Soils in Mashhad, Iran Using Standard Penetration and Direct Shear Tests and Comparison with Previous Equations
 
</article-title></title-group><contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>ouya</surname><given-names>Salari</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>Gholam</surname><given-names>Reza Lashkaripour</given-names></name><xref ref-type="aff" rid="aff2"><sup>2</sup></xref><xref ref-type="corresp" rid="cor1"><sup>*</sup></xref></contrib><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Mohammad</surname><given-names>Ghafoori</given-names></name><xref ref-type="aff" rid="aff2"><sup>2</sup></xref></contrib></contrib-group><aff id="aff2"><addr-line>Department of Geology, Ferdowsi University of Mashhad, Mashhad, Iran</addr-line></aff><aff id="aff1"><addr-line>Department of Geology, Ferdowsi University of Mashhad, International Branch, Mashhad, Iran</addr-line></aff><author-notes><corresp id="cor1">* E-mail:<email>lashkaripour@um.ac.ir(GRL)</email>;</corresp></author-notes><pub-date pub-type="epub"><day>06</day><month>05</month><year>2015</year></pub-date><volume>05</volume><issue>05</issue><fpage>231</fpage><lpage>238</lpage><history><date date-type="received"><day>17</day>	<month>March</month>	<year>2015</year></date><date date-type="rev-recd"><day>accepted</day>	<month>2</month>	<year>May</year>	</date><date date-type="accepted"><day>6</day>	<month>May</month>	<year>2015</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>
 
 
  Presentation of empirical equations for estimating engineering properties of soils is a simple, low cost and widely-used method. One of the major concerns in using these equations is evaluating their accuracy in different conditions and regions which often lead to doubts about obtained results. Most of these equations were derived in special laboratories, different climate conditions and in soils with different geotechnical and geological engineering properties and were generalized to other conditions. The main question is that whether these methods are also applicable to other conditions. Using local equations and narrowing the usage range of various methods based on each region’s properties are appropriate methods to solve these problems. This leads to simplified and faster analysis and high reliability in the obtained results. In this paper, empirical equations were derived to estimate internal friction angle, based on SPT numbers of Mashhad City’s soils in Iran, using SPT and direct shear tests results from 50 samples (25 GW and 25 GC soil samples). The results showed similar values for predicted 
  φ
   values by SPT test and 
  φ
   values determined by direct shear tests.
 
</p></abstract><kwd-group><kwd>Internal Friction Angle</kwd><kwd> GW and GC Soil</kwd><kwd> Direct Shear Test</kwd><kwd> SPT Test</kwd></kwd-group></article-meta></front><body><sec id="s1"><title>1. Introduction</title><p>Internal friction angle is one of the most important parameters in analyzing soil geotechnical properties and earthwork calculations. It has a wide range of applications such as calculating retaining walls, foundations, friction and end-bearing piles and so on [<xref ref-type="bibr" rid="scirp.56133-ref1">1</xref>] [<xref ref-type="bibr" rid="scirp.56133-ref2">2</xref>] .</p><p>Based on properties of a given soil profile such as fine or coarse grained, various tests such as direct shear and triaxial tests are recommended for obtaining internal friction angle parameter. Although due to the soil disturbance during sampling as well as special laboratory conditions, these results may not completely represent true properties of soils and even in case of special care in doing the tests, they are still highly time-consuming and require using simpler empirical equations. This research aims to obtain internal friction angle of soils using standard penetration test for different types of soils in Mashhad. For this purpose, several equations have already been presented [<xref ref-type="bibr" rid="scirp.56133-ref3">3</xref>] . Internal friction angle for Mashhad city can be estimated using appropriate equations for the city soil conditions, soil types, samples depth and specific unit weight.</p><p>SPT number has been defined in various equations based on specific weight, grading, relative density, internal friction angle and undrained compressive strength [<xref ref-type="bibr" rid="scirp.56133-ref4">4</xref>] [<xref ref-type="bibr" rid="scirp.56133-ref5">5</xref>] . This number is also used for estimating bearing capacity of soil for foundation and elastic modulus calculations [<xref ref-type="bibr" rid="scirp.56133-ref6">6</xref>] . These equations and their approaches are often doubtful due to having a small amount of gathered data, lack of focus on special aspects or incorrect equations generalization [<xref ref-type="bibr" rid="scirp.56133-ref7">7</xref>] -[<xref ref-type="bibr" rid="scirp.56133-ref9">9</xref>] .</p><p>Equations obtained by Shioi and Fukui (1982) are presented below (Equations (1) to (3)). Equation (1) is for roads and bridges, Equation (2) for buildings and Equation (3) is general.</p><disp-formula id="scirp.56133-formula1"><label>(1)</label><graphic position="anchor" xlink:href="http://html.scirp.org/file/1-1210292x6.png"  xlink:type="simple"/></disp-formula><disp-formula id="scirp.56133-formula2"><label>(2)</label><graphic position="anchor" xlink:href="http://html.scirp.org/file/1-1210292x7.png"  xlink:type="simple"/></disp-formula><disp-formula id="scirp.56133-formula3"><label>(3)</label><graphic position="anchor" xlink:href="http://html.scirp.org/file/1-1210292x8.png"  xlink:type="simple"/></disp-formula></sec><sec id="s2"><title>2. FHWA Recommended Tables</title><p>Federal Highway Administration recommend using <xref ref-type="table" rid="table1">Table 1</xref> for correlating approximate SPT number, relative density and internal friction angle parameters with each other [<xref ref-type="bibr" rid="scirp.56133-ref10">10</xref>] . Following information is necessary to use <xref ref-type="table" rid="table1">Table 1</xref>:</p><p>1. Measured SPT numbers were obtained without any correction factors in field tests.</p><p>2. (Pa) is free sea level pressure.</p><p>3. Ranges in column (a) is based on Peck, Hanson, and Thornburn (1974) study.</p><p>4. Ranges in column (b) is based on Meyerhof (1956) study.</p><p>(3) Ranges in column (a) from Peck, Hanson, and Thornburn (1974).</p><p>(4) Ranges in column (b) and for CPT are from Meyerhof (1956).</p><p>Since the values are from field SPT tests, the table can be very useful and widely applicable [<xref ref-type="bibr" rid="scirp.56133-ref11">11</xref>] .</p></sec><sec id="s3"><title>3. Methods of study</title><p>First, SPT tests were carried out on 50 samples (25 GC and 25 GW samples in various depths). Results of direct shear tests (φ values) and also depth and dry unit weight of samples are shown in <xref ref-type="table" rid="table2">Table 2</xref> and <xref ref-type="table" rid="table3">Table 3</xref> [<xref ref-type="bibr" rid="scirp.56133-ref12">12</xref>] . These tables show in situ (SPT) and laboratory (direct shear) tests results. Locations of sampling in the city are shown in <xref ref-type="fig" rid="fig1">Figure 1</xref>.</p><p>Then, based on statistical validations, two equations were derived to estimate internal friction angle, based on SPT number for two soil types (GC, GW).</p><p>In order to use <xref ref-type="table" rid="table2">Table 2</xref> and <xref ref-type="table" rid="table3">Table 3</xref>, some points must be considered.</p><p>1. Narrowing application range was done for special types of soils in order to achieve higher accuracy.</p><p>2. In order to attenuate the effects of some parameters such as weathering, all studied samples were taken from the depths of 4 to 15 meters.</p><p>3. In order to obtain better results, samples with special dry unit weight of 19 to 21 KN/m<sup>3 </sup>were considered.</p><p>4. Internal friction angle in these tables were obtained from direct shear tests.</p><p>5. All data were obtained from soil profiles on Vakilabad area located in the western part of Mashhad city.</p><table-wrap id="table1" ><label><xref ref-type="table" rid="table1">Table 1</xref></label><caption><title> Correlation between SPT and CPT results and friction angle of cohesionless soils (FHWA, 2003)</title></caption><table><tbody><thead><tr><th align="center" valign="middle"  colspan="2"  ><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/1-1210292x9.png" xlink:type="simple"/></inline-formula> (a)<sup>3</sup> (b)<sup>4</sup></th><th align="center" valign="middle" >Relative Density</th><th align="center" valign="middle" >In-Situ Test Results</th><th align="center" valign="middle" ></th></tr></thead><tr><td align="center" valign="middle" >&lt;30</td><td align="center" valign="middle" >&lt; 28</td><td align="center" valign="middle" >Very Loose</td><td align="center" valign="middle" >0 to 4</td><td align="center" valign="middle"  rowspan="5"  >SPT N-Value (blows/300 mm or blows/ft)</td></tr><tr><td align="center" valign="middle" >30 to 35</td><td align="center" valign="middle" >28 to 30</td><td align="center" valign="middle" >Loose</td><td align="center" valign="middle" >4 to 10</td></tr><tr><td align="center" valign="middle" >35 to 40</td><td align="center" valign="middle" >30 to 36</td><td align="center" valign="middle" >Medium</td><td align="center" valign="middle" >10 to 30</td></tr><tr><td align="center" valign="middle" >40 to 45</td><td align="center" valign="middle" >36 to 41</td><td align="center" valign="middle" >Dense</td><td align="center" valign="middle" >30 to 50</td></tr><tr><td align="center" valign="middle" >&gt;45</td><td align="center" valign="middle" >&gt;41</td><td align="center" valign="middle" >Very Dense</td><td align="center" valign="middle" >&gt;50</td></tr><tr><td align="center" valign="middle"  colspan="2"  >&lt;30</td><td align="center" valign="middle" >Very Loose</td><td align="center" valign="middle" >&lt;20</td><td align="center" valign="middle"  rowspan="5"  >Normalized CPT cone bearing resistance (qc/Pa)</td></tr><tr><td align="center" valign="middle"  colspan="2"  >30 to 35</td><td align="center" valign="middle" >Loose</td><td align="center" valign="middle" >20 to 40</td></tr><tr><td align="center" valign="middle"  colspan="2"  >35 to 40</td><td align="center" valign="middle" >Medium</td><td align="center" valign="middle" >40 to 120</td></tr><tr><td align="center" valign="middle"  colspan="2"  >40 to 45</td><td align="center" valign="middle" >Dense</td><td align="center" valign="middle" >120 to 200</td></tr><tr><td align="center" valign="middle"  colspan="2"  >&gt;45</td><td align="center" valign="middle" >Very Dense</td><td align="center" valign="middle" >&gt;200</td></tr></tbody></table></table-wrap><table-wrap id="table2" ><label><xref ref-type="table" rid="table2">Table 2</xref></label><caption><title> GW soils data obtained by laboratory and in-situ tests</title></caption><table><tbody><thead><tr><th align="center" valign="middle" >Internal Friction Angle</th><th align="center" valign="middle" >SPT Number</th><th align="center" valign="middle" >Depth (m)</th><th align="center" valign="middle" >Dry Unit Weight (KN/m<sup>3</sup>)</th><th align="center" valign="middle" >Row</th><th align="center" valign="middle" >Soil Type</th></tr></thead><tr><td align="center" valign="middle" >34</td><td align="center" valign="middle" >38</td><td align="center" valign="middle" >13</td><td align="center" valign="middle" >19.5</td><td align="center" valign="middle" >1</td><td align="center" valign="middle"  rowspan="25"  >GW</td></tr><tr><td align="center" valign="middle" >34.4</td><td align="center" valign="middle" >39</td><td align="center" valign="middle" >11</td><td align="center" valign="middle" >20.1</td><td align="center" valign="middle" >2</td></tr><tr><td align="center" valign="middle" >34.9</td><td align="center" valign="middle" >41</td><td align="center" valign="middle" >10</td><td align="center" valign="middle" >19.6</td><td align="center" valign="middle" >3</td></tr><tr><td align="center" valign="middle" >37.2</td><td align="center" valign="middle" >45</td><td align="center" valign="middle" >14</td><td align="center" valign="middle" >19.9</td><td align="center" valign="middle" >4</td></tr><tr><td align="center" valign="middle" >36.2</td><td align="center" valign="middle" >42</td><td align="center" valign="middle" >6</td><td align="center" valign="middle" >20.8</td><td align="center" valign="middle" >5</td></tr><tr><td align="center" valign="middle" >35.5</td><td align="center" valign="middle" >40</td><td align="center" valign="middle" >9</td><td align="center" valign="middle" >20.1</td><td align="center" valign="middle" >6</td></tr><tr><td align="center" valign="middle" >34.2</td><td align="center" valign="middle" >38</td><td align="center" valign="middle" >13</td><td align="center" valign="middle" >20.0</td><td align="center" valign="middle" >7</td></tr><tr><td align="center" valign="middle" >34.3</td><td align="center" valign="middle" >39</td><td align="center" valign="middle" >4</td><td align="center" valign="middle" >19.2</td><td align="center" valign="middle" >8</td></tr><tr><td align="center" valign="middle" >34.5</td><td align="center" valign="middle" >39</td><td align="center" valign="middle" >14</td><td align="center" valign="middle" >19.6</td><td align="center" valign="middle" >9</td></tr><tr><td align="center" valign="middle" >36.8</td><td align="center" valign="middle" >43</td><td align="center" valign="middle" >9</td><td align="center" valign="middle" >20.6</td><td align="center" valign="middle" >10</td></tr><tr><td align="center" valign="middle" >36.3</td><td align="center" valign="middle" >42</td><td align="center" valign="middle" >5</td><td align="center" valign="middle" >20.3</td><td align="center" valign="middle" >11</td></tr><tr><td align="center" valign="middle" >37.3</td><td align="center" valign="middle" >45</td><td align="center" valign="middle" >6</td><td align="center" valign="middle" >19.1</td><td align="center" valign="middle" >12</td></tr><tr><td align="center" valign="middle" >36.4</td><td align="center" valign="middle" >42</td><td align="center" valign="middle" >8</td><td align="center" valign="middle" >19.8</td><td align="center" valign="middle" >13</td></tr><tr><td align="center" valign="middle" >36.7</td><td align="center" valign="middle" >43</td><td align="center" valign="middle" >11</td><td align="center" valign="middle" >20.4</td><td align="center" valign="middle" >14</td></tr><tr><td align="center" valign="middle" >34.1</td><td align="center" valign="middle" >38</td><td align="center" valign="middle" >10</td><td align="center" valign="middle" >20.9</td><td align="center" valign="middle" >15</td></tr><tr><td align="center" valign="middle" >37.2</td><td align="center" valign="middle" >45</td><td align="center" valign="middle" >14</td><td align="center" valign="middle" >20.1</td><td align="center" valign="middle" >16</td></tr><tr><td align="center" valign="middle" >36.9</td><td align="center" valign="middle" >43</td><td align="center" valign="middle" >13</td><td align="center" valign="middle" >19.3</td><td align="center" valign="middle" >17</td></tr><tr><td align="center" valign="middle" >36</td><td align="center" valign="middle" >41</td><td align="center" valign="middle" >12</td><td align="center" valign="middle" >20.6</td><td align="center" valign="middle" >18</td></tr><tr><td align="center" valign="middle" >36.1</td><td align="center" valign="middle" >42</td><td align="center" valign="middle" >9</td><td align="center" valign="middle" >19.2</td><td align="center" valign="middle" >19</td></tr><tr><td align="center" valign="middle" >36.3</td><td align="center" valign="middle" >42</td><td align="center" valign="middle" >13</td><td align="center" valign="middle" >19.7</td><td align="center" valign="middle" >20</td></tr><tr><td align="center" valign="middle" >36.4</td><td align="center" valign="middle" >43</td><td align="center" valign="middle" >11</td><td align="center" valign="middle" >19.6</td><td align="center" valign="middle" >21</td></tr><tr><td align="center" valign="middle" >37.1</td><td align="center" valign="middle" >44</td><td align="center" valign="middle" >10</td><td align="center" valign="middle" >20.7</td><td align="center" valign="middle" >22</td></tr><tr><td align="center" valign="middle" >35.8</td><td align="center" valign="middle" >40</td><td align="center" valign="middle" >8</td><td align="center" valign="middle" >19.3</td><td align="center" valign="middle" >23</td></tr><tr><td align="center" valign="middle" >34.2</td><td align="center" valign="middle" >38</td><td align="center" valign="middle" >14</td><td align="center" valign="middle" >20.6</td><td align="center" valign="middle" >24</td></tr><tr><td align="center" valign="middle" >37</td><td align="center" valign="middle" >44</td><td align="center" valign="middle" >11</td><td align="center" valign="middle" >20.4</td><td align="center" valign="middle" >25</td></tr></tbody></table></table-wrap><table-wrap id="table3" ><label><xref ref-type="table" rid="table3">Table 3</xref></label><caption><title> GC soils data obtained by laboratory and in-situ tests</title></caption><table><tbody><thead><tr><th align="center" valign="middle" >Internal Friction Angle</th><th align="center" valign="middle" >SPT Number</th><th align="center" valign="middle" >Depth (m)</th><th align="center" valign="middle" >Dry Unit Weight (KN/m<sup>3</sup>)</th><th align="center" valign="middle" >Row</th><th align="center" valign="middle" >Soil Type</th></tr></thead><tr><td align="center" valign="middle" >33</td><td align="center" valign="middle" >35</td><td align="center" valign="middle" >11</td><td align="center" valign="middle" >20.2</td><td align="center" valign="middle" >1</td><td align="center" valign="middle"  rowspan="25"  >GC</td></tr><tr><td align="center" valign="middle" >33.6</td><td align="center" valign="middle" >36</td><td align="center" valign="middle" >6</td><td align="center" valign="middle" >19.9</td><td align="center" valign="middle" >2</td></tr><tr><td align="center" valign="middle" >33.9</td><td align="center" valign="middle" >37</td><td align="center" valign="middle" >13</td><td align="center" valign="middle" >20.2</td><td align="center" valign="middle" >3</td></tr><tr><td align="center" valign="middle" >33.9</td><td align="center" valign="middle" >38</td><td align="center" valign="middle" >12</td><td align="center" valign="middle" >20.7</td><td align="center" valign="middle" >4</td></tr><tr><td align="center" valign="middle" >34.1</td><td align="center" valign="middle" >39</td><td align="center" valign="middle" >6</td><td align="center" valign="middle" >20.1</td><td align="center" valign="middle" >5</td></tr><tr><td align="center" valign="middle" >34.5</td><td align="center" valign="middle" >40</td><td align="center" valign="middle" >9</td><td align="center" valign="middle" >20.4</td><td align="center" valign="middle" >6</td></tr><tr><td align="center" valign="middle" >35</td><td align="center" valign="middle" >41</td><td align="center" valign="middle" >5</td><td align="center" valign="middle" >19.9</td><td align="center" valign="middle" >7</td></tr><tr><td align="center" valign="middle" >35.9</td><td align="center" valign="middle" >42</td><td align="center" valign="middle" >14</td><td align="center" valign="middle" >19.5</td><td align="center" valign="middle" >8</td></tr><tr><td align="center" valign="middle" >34.7</td><td align="center" valign="middle" >40</td><td align="center" valign="middle" >11</td><td align="center" valign="middle" >19.3</td><td align="center" valign="middle" >9</td></tr><tr><td align="center" valign="middle" >33.8</td><td align="center" valign="middle" >36</td><td align="center" valign="middle" >10</td><td align="center" valign="middle" >20.6</td><td align="center" valign="middle" >10</td></tr><tr><td align="center" valign="middle" >33.1</td><td align="center" valign="middle" >35</td><td align="center" valign="middle" >15</td><td align="center" valign="middle" >20.1</td><td align="center" valign="middle" >11</td></tr><tr><td align="center" valign="middle" >35.2</td><td align="center" valign="middle" >41</td><td align="center" valign="middle" >11</td><td align="center" valign="middle" >20.7</td><td align="center" valign="middle" >12</td></tr><tr><td align="center" valign="middle" >34.1</td><td align="center" valign="middle" >37</td><td align="center" valign="middle" >9</td><td align="center" valign="middle" >19.8</td><td align="center" valign="middle" >13</td></tr><tr><td align="center" valign="middle" >34.3</td><td align="center" valign="middle" >39</td><td align="center" valign="middle" >12</td><td align="center" valign="middle" >20.1</td><td align="center" valign="middle" >14</td></tr><tr><td align="center" valign="middle" >34.2</td><td align="center" valign="middle" >38</td><td align="center" valign="middle" >11</td><td align="center" valign="middle" >19.8</td><td align="center" valign="middle" >15</td></tr><tr><td align="center" valign="middle" >35.3</td><td align="center" valign="middle" >41</td><td align="center" valign="middle" >14</td><td align="center" valign="middle" >19.4</td><td align="center" valign="middle" >16</td></tr><tr><td align="center" valign="middle" >36.1</td><td align="center" valign="middle" >42</td><td align="center" valign="middle" >9</td><td align="center" valign="middle" >20.3</td><td align="center" valign="middle" >17</td></tr><tr><td align="center" valign="middle" >34.8</td><td align="center" valign="middle" >40</td><td align="center" valign="middle" >8</td><td align="center" valign="middle" >19.8</td><td align="center" valign="middle" >18</td></tr><tr><td align="center" valign="middle" >34.2</td><td align="center" valign="middle" >39</td><td align="center" valign="middle" >7</td><td align="center" valign="middle" >20.3</td><td align="center" valign="middle" >19</td></tr><tr><td align="center" valign="middle" >33.2</td><td align="center" valign="middle" >35</td><td align="center" valign="middle" >12</td><td align="center" valign="middle" >19.7</td><td align="center" valign="middle" >20</td></tr><tr><td align="center" valign="middle" >33.5</td><td align="center" valign="middle" >36</td><td align="center" valign="middle" >13</td><td align="center" valign="middle" >19.4</td><td align="center" valign="middle" >21</td></tr><tr><td align="center" valign="middle" >36.2</td><td align="center" valign="middle" >42</td><td align="center" valign="middle" >14</td><td align="center" valign="middle" >20.4</td><td align="center" valign="middle" >22</td></tr><tr><td align="center" valign="middle" >34.4</td><td align="center" valign="middle" >37</td><td align="center" valign="middle" >9</td><td align="center" valign="middle" >20.3</td><td align="center" valign="middle" >23</td></tr><tr><td align="center" valign="middle" >34.6</td><td align="center" valign="middle" >38</td><td align="center" valign="middle" >7</td><td align="center" valign="middle" >20.5</td><td align="center" valign="middle" >24</td></tr><tr><td align="center" valign="middle" >34.8</td><td align="center" valign="middle" >40</td><td align="center" valign="middle" >11</td><td align="center" valign="middle" >20.4</td><td align="center" valign="middle" >25</td></tr></tbody></table></table-wrap></sec><sec id="s4"><title>4. Results and Discussion</title><p>Reliability and accuracy of the obtained equations must be measured by statistical reliability ratings. In order to obtain correlations between data, following steps were taken:</p><p>1. Drawing scatter diagram; <xref ref-type="fig" rid="fig2">Figure 2</xref> and <xref ref-type="fig" rid="fig3">Figure 3</xref> show scatter diagrams related to GC and GW soils properties.</p><p>2. Model fitting and obtaining coefficients: the aim of a proper model fitting is to determine correlation among control (x) and response (y) variables (Equations (4)-(6) and <xref ref-type="fig" rid="fig2">Figure 2</xref> and <xref ref-type="fig" rid="fig3">Figure 3</xref>) [<xref ref-type="bibr" rid="scirp.56133-ref13">13</xref>] [<xref ref-type="bibr" rid="scirp.56133-ref14">14</xref>] .</p><disp-formula id="scirp.56133-formula4"><label>(4)</label><graphic position="anchor" xlink:href="http://html.scirp.org/file/1-1210292x10.png"  xlink:type="simple"/></disp-formula><disp-formula id="scirp.56133-formula5"><label>(5)</label><graphic position="anchor" xlink:href="http://html.scirp.org/file/1-1210292x11.png"  xlink:type="simple"/></disp-formula><disp-formula id="scirp.56133-formula6"><label>(6)</label><graphic position="anchor" xlink:href="http://html.scirp.org/file/1-1210292x12.png"  xlink:type="simple"/></disp-formula><p>3. Obtaining numerical value of Sig for comparing correlations.</p><fig id="fig1"  position="float"><label><xref ref-type="fig" rid="fig1">Figure 1</xref></label><caption><title> Locations of sampling and SPT testing in Mashhad city</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/1-1210292x13.png"/></fig><fig id="fig2"  position="float"><label><xref ref-type="fig" rid="fig2">Figure 2</xref></label><caption><title> Correlation between φ and SPT number for GW soils</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/1-1210292x14.png"/></fig><p>Models were studied on 95% reliability level. Thus, for studying meaningfulness of the model, model making and model coefficients evaluation, following statistical hypotheses were considered (Equations (7), (8)).</p><disp-formula id="scirp.56133-formula7"><label>(7)</label><graphic position="anchor" xlink:href="http://html.scirp.org/file/1-1210292x15.png"  xlink:type="simple"/></disp-formula><disp-formula id="scirp.56133-formula8"><label>(8)</label><graphic position="anchor" xlink:href="http://html.scirp.org/file/1-1210292x16.png"  xlink:type="simple"/></disp-formula><p>Sig. (p-value) were obtained from Fisher test (<xref ref-type="table" rid="table4">Table 4</xref>).</p><p>Based on Sig (p-value) that was obtained from Fisher test: meaningful</p><disp-formula id="scirp.56133-formula9"><graphic  xlink:href="http://html.scirp.org/file/1-1210292x17.png"  xlink:type="simple"/></disp-formula><fig id="fig3"  position="float"><label><xref ref-type="fig" rid="fig3">Figure 3</xref></label><caption><title> Correlation between φ and SPT number for GC soils</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/1-1210292x18.png"/></fig><table-wrap id="table4" ><label><xref ref-type="table" rid="table4">Table 4</xref></label><caption><title> ANOVA table for studying the meaningfulness of the model</title></caption><table><tbody><thead><tr><th align="center" valign="middle"  colspan="7"  >ANOVA<sup>a</sup></th></tr></thead><tr><td align="center" valign="middle"  colspan="2"  >Model 1 for GW Soils</td><td align="center" valign="middle" >Sum of Squares</td><td align="center" valign="middle" >df</td><td align="center" valign="middle" >Mean Square</td><td align="center" valign="middle" >F</td><td align="center" valign="middle" >Sig.</td></tr><tr><td align="center" valign="middle"  rowspan="3"  >1</td><td align="center" valign="middle" >Regression</td><td align="center" valign="middle" >29.697</td><td align="center" valign="middle" >1</td><td align="center" valign="middle" >29.697</td><td align="center" valign="middle" >316.619</td><td align="center" valign="middle" >0.000</td></tr><tr><td align="center" valign="middle" >Residual</td><td align="center" valign="middle" >2.157</td><td align="center" valign="middle" >23</td><td align="center" valign="middle" >0.094</td><td align="center" valign="middle" ></td><td align="center" valign="middle" ></td></tr><tr><td align="center" valign="middle" >Total</td><td align="center" valign="middle" >31.854</td><td align="center" valign="middle" >24</td><td align="center" valign="middle" ></td><td align="center" valign="middle" ></td><td align="center" valign="middle" ></td></tr><tr><td align="center" valign="middle"  colspan="2"  >Model 2 for GC Soils</td><td align="center" valign="middle" >Sum of Squares</td><td align="center" valign="middle" >df</td><td align="center" valign="middle" >Mean Square</td><td align="center" valign="middle" >F</td><td align="center" valign="middle" >Sig.</td></tr><tr><td align="center" valign="middle"  rowspan="3"  >2</td><td align="center" valign="middle" >Regression</td><td align="center" valign="middle" >16.208</td><td align="center" valign="middle" >1</td><td align="center" valign="middle" >16.208</td><td align="center" valign="middle" >177.010</td><td align="center" valign="middle" >0.000</td></tr><tr><td align="center" valign="middle" >Residual</td><td align="center" valign="middle" >2.106</td><td align="center" valign="middle" >23</td><td align="center" valign="middle" >0.092</td><td align="center" valign="middle" ></td><td align="center" valign="middle" ></td></tr><tr><td align="center" valign="middle" >Total</td><td align="center" valign="middle" >18.314</td><td align="center" valign="middle" >24</td><td align="center" valign="middle" ></td><td align="center" valign="middle" ></td><td align="center" valign="middle" ></td></tr></tbody></table></table-wrap><p><sup>a</sup>Dependent Variable: PHI; <sup>b</sup>Predictors: (Constant), SPT.</p><p>According to <xref ref-type="table" rid="table4">Table 4</xref>, both models are meaningful (Equations (9) and (10)).</p><p>Presented equation for GW soils:</p><disp-formula id="scirp.56133-formula10"><label>(9)</label><graphic position="anchor" xlink:href="http://html.scirp.org/file/1-1210292x19.png"  xlink:type="simple"/></disp-formula><p>Presented equation for GC soils:</p><disp-formula id="scirp.56133-formula11"><label>(10)</label><graphic position="anchor" xlink:href="http://html.scirp.org/file/1-1210292x20.png"  xlink:type="simple"/></disp-formula><p>In <xref ref-type="fig" rid="fig4">Figure 4</xref> and <xref ref-type="fig" rid="fig5">Figure 5</xref>, observed friction angle (φ<sub>obs</sub>) (based on direct shear test) and predicted friction angle (φ<sub>pre</sub>) (based on the equations obtained in this research) were compared.</p><p>Based on the obtained equations for GC and GW soils, following comparisons with FHWA table values were done:</p><p>The results indicate similarity between predicted φ values calculated using presented equations in this paper and Peck, Hanson and Thornburn (1974) study; they had also predicted the values of φ about 30 to 35 degrees (for this range of SPT numbers). In contrast, the results of this research do not conform to the Meyerhof (1956) study, indicating that he had over-predicted the φ values.</p></sec><sec id="s5"><title>5. Conclusions</title><p>Deriving empirical equations among various geotechnical parameters such as SPT number and internal friction angle can be very effective for different purposes such as fast and simple approximate evaluations and reliability rating of laboratory results. In this paper, these correlations were presented for coarse grained and low cohesive soils profiles of Mashhad city. In order to present the mentioned correlations, GC and GW soils with special dry unit weight of 19 to 21 KN/m<sup>3</sup> were studied. To avoid weathering effect on results, samples with depths between 4 to 15 m were used. By narrowing soil type range, depth of sampling and dry unit weight for predicting internal friction angle based on SPT number, two equations were presented. Based on <xref ref-type="table" rid="table5">Table 5</xref>, FHWA values are similar</p><fig id="fig4"  position="float"><label><xref ref-type="fig" rid="fig4">Figure 4</xref></label><caption><title> Comparison between φ obs and φ pre for GW soils</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/1-1210292x21.png"/></fig><fig id="fig5"  position="float"><label><xref ref-type="fig" rid="fig5">Figure 5</xref></label><caption><title> Comparison between φ obs and φ pre for GC soils</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/1-1210292x22.png"/></fig><table-wrap id="table5" ><label><xref ref-type="table" rid="table5">Table 5</xref></label><caption><title> Predicted values of internal friction angle in this research</title></caption><table><tbody><thead><tr><th align="center" valign="middle" >φ (by using obtained equation)</th><th align="center" valign="middle" >SPT number (in situ test)</th><th align="center" valign="middle" ></th><th align="center" valign="middle" >φ (by using obtained equation)</th><th align="center" valign="middle" >SPT number (in situ test)</th><th align="center" valign="middle" ></th></tr></thead><tr><td align="center" valign="middle" >34.1408</td><td align="center" valign="middle" >38</td><td align="center" valign="middle"  rowspan="8"  >GW soils</td><td align="center" valign="middle" >33.107</td><td align="center" valign="middle" >35</td><td align="center" valign="middle"  rowspan="8"  >GC soils</td></tr><tr><td align="center" valign="middle" >34.6259</td><td align="center" valign="middle" >39</td><td align="center" valign="middle" >33.4558</td><td align="center" valign="middle" >36</td></tr><tr><td align="center" valign="middle" >35.111</td><td align="center" valign="middle" >40</td><td align="center" valign="middle" >33.8046</td><td align="center" valign="middle" >37</td></tr><tr><td align="center" valign="middle" >35.5961</td><td align="center" valign="middle" >41</td><td align="center" valign="middle" >34.1534</td><td align="center" valign="middle" >38</td></tr><tr><td align="center" valign="middle" >36.0812</td><td align="center" valign="middle" >42</td><td align="center" valign="middle" >34.5022</td><td align="center" valign="middle" >39</td></tr><tr><td align="center" valign="middle" >36.5663</td><td align="center" valign="middle" >43</td><td align="center" valign="middle" >34.851</td><td align="center" valign="middle" >40</td></tr><tr><td align="center" valign="middle" >37.0514</td><td align="center" valign="middle" >44</td><td align="center" valign="middle" >35.1998</td><td align="center" valign="middle" >41</td></tr><tr><td align="center" valign="middle" >37.5365</td><td align="center" valign="middle" >45</td><td align="center" valign="middle" >35.5486</td><td align="center" valign="middle" >42</td></tr></tbody></table></table-wrap><p>to the values of internal friction angle obtained from presented equations in this paper and conform to the results of Peck, Hanson and Thornburn (1974) study. However, the obtained values are mainly lower than the values obtained by Meyerhof (1956).</p></sec><sec id="s6"><title>NOTES</title></sec></body><back><ref-list><title>References</title><ref id="scirp.56133-ref1"><label>1</label><mixed-citation publication-type="other" xlink:type="simple">McGregor, J. and Duncan, J.M. (1998) Performance and Use of the Standard Penetration Test in Geotechnical Engineering Practice. Report of CGPR, Virginia Polytechnic Institute, Blacksburg.</mixed-citation></ref><ref id="scirp.56133-ref2"><label>2</label><mixed-citation publication-type="other" xlink:type="simple">Shioi, Y. and Fukui, J. (1982) Application of N-Value to Design of Foundation in Japan. 2nd ESOPT, Vol. 1, 40-93.</mixed-citation></ref><ref id="scirp.56133-ref3"><label>3</label><mixed-citation publication-type="book" xlink:type="simple">Silva, S.D., Wightman, E.N.R. and Kamruzzaman, M. (2010) Geotechnical Ground Investigation for the Padmamain Bridge. In: Amin, Okui, Bhuiyan, Eds., IABCE-JSCE Joint Conference on Advances in Bridge Engineering-II, Dhaka, Bangladesh, 8-10 August 2010, 427-436.</mixed-citation></ref><ref id="scirp.56133-ref4"><label>4</label><mixed-citation publication-type="other" xlink:type="simple">Hettiarachchi, H. and Brown, T. (2009) Use of SPT Blow Counts to Estimate Shear Strength Properties of Soils: Energy Balance Approach, Journal of Geotechnical and Geoenvironmental Engineering, 135, 25-32.  
http://dx.doi.org/10.1061/(ASCE)GT.1943-5606.0000016</mixed-citation></ref><ref id="scirp.56133-ref5"><label>5</label><mixed-citation publication-type="journal" xlink:type="simple"><name name-style="western"><surname>Jianguo</surname><given-names> C. </given-names></name>,<etal>et al</etal>. (<year>2012</year>)<article-title>Correlation Analysis of SPT N Values and Cohesion and Internal Angle of a Clay</article-title><source> Soil Engineering and Foundation</source><volume> 26</volume>,<fpage> 91</fpage>-<lpage>93</lpage>.<pub-id pub-id-type="doi"></pub-id></mixed-citation></ref><ref id="scirp.56133-ref6"><label>6</label><mixed-citation publication-type="other" xlink:type="simple">Kaliniski, M. (2011) Soil Mechanics Lab Manual. 2nd Edition, John Wiley &amp; Sons, Inc., Hoboken.</mixed-citation></ref><ref id="scirp.56133-ref7"><label>7</label><mixed-citation publication-type="journal" xlink:type="simple"><name name-style="western"><surname>Mohammad</surname><given-names> M. </given-names></name>,<etal>et al</etal>. (<year>2013</year>)<article-title>Reliability of Standard Penetration Test (SPT) in Predicting Properties of Silty Clay with Sand Soil</article-title><source> International Journal of Civil and Structural Engineering</source><volume> 3</volume>,<fpage> 85</fpage>-<lpage>94</lpage>.<pub-id pub-id-type="doi"></pub-id></mixed-citation></ref><ref id="scirp.56133-ref8"><label>8</label><mixed-citation publication-type="other" xlink:type="simple">Bowles, J.E. (1988) Foundation Analysis and Design. 4th Edition, McGraw Hill.</mixed-citation></ref><ref id="scirp.56133-ref9"><label>9</label><mixed-citation publication-type="other" xlink:type="simple">Budhu, M. (2011) Soil Mechanics and Foundation. 3rd Edition, John Wiley &amp; Sons, Inc., Hoboken.</mixed-citation></ref><ref id="scirp.56133-ref10"><label>10</label><mixed-citation publication-type="other" xlink:type="simple">FHWAO-IF-03-17 (2003) Geotechnical Engineering Circular, No.3, Soil Nail Walls.</mixed-citation></ref><ref id="scirp.56133-ref11"><label>11</label><mixed-citation publication-type="other" xlink:type="simple">Aggour, M.S. and Radding, W.R. (2001) Standard Penetration Test (SPT) Correction. Research Report, Civil and Environmental Engineering Department, University of Maryland College Park, Maryland, 20742.</mixed-citation></ref><ref id="scirp.56133-ref12"><label>12</label><mixed-citation publication-type="other" xlink:type="simple">Soil and Structure Consulting Engineers Company (2014) Geotechnical Reports of Vakilabad Region Projects.</mixed-citation></ref><ref id="scirp.56133-ref13"><label>13</label><mixed-citation publication-type="other" xlink:type="simple">Rad, M. (2008) Engineering Statistics and Probabilities. Publications of Hafiz and Tafresh University, Tafresh.</mixed-citation></ref><ref id="scirp.56133-ref14"><label>14</label><mixed-citation publication-type="other" xlink:type="simple">Isotalo, J. (2001) Basics of Statistics. University of Tampere, Tampere.</mixed-citation></ref></ref-list></back></article>