<?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">IJAA</journal-id><journal-title-group><journal-title>International Journal of Astronomy and Astrophysics</journal-title></journal-title-group><issn pub-type="epub">2161-4717</issn><publisher><publisher-name>Scientific Research Publishing</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.4236/ijaa.2020.103010</article-id><article-id pub-id-type="publisher-id">IJAA-102258</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>
 
 
  New Probability Distributions in Astrophysics: III. The Truncated Maxwell-Boltzmann Distribution
 
</article-title></title-group><contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Lorenzo</surname><given-names>Zaninetti</given-names></name><xref ref-type="aff" rid="aff1"><sub>1</sub></xref><xref ref-type="corresp" rid="cor1"><sup>*</sup></xref></contrib></contrib-group><aff id="aff1"><label>1</label><addr-line>Physics Department, Turin, Italy</addr-line></aff><pub-date pub-type="epub"><day>18</day><month>08</month><year>2020</year></pub-date><volume>10</volume><issue>03</issue><fpage>191</fpage><lpage>202</lpage><history><date date-type="received"><day>17,</day>	<month>June</month>	<year>2020</year></date><date date-type="rev-recd"><day>16,</day>	<month>August</month>	<year>2020</year>	</date><date date-type="accepted"><day>19,</day>	<month>August</month>	<year>2020</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>
 
 
  The Maxwell-Boltzmann (MB) distribution for velocities in ideal gases is usually defined between zero and infinity. A double truncated MB distribution is here introduced and the probability density function, the distribution function, the average value, the rth moment about the origin, the root-mean-square speed and the variance are evaluated. Two applications are presented: 1) a numerical relationship between root-mean-square speed and temperature, and 2) a modification of the formula for the Jeans escape flux of molecules from an atmosphere.
 
</p></abstract><kwd-group><kwd>05.20.-y Classical Statistical Mechanics</kwd><kwd> 05.20.Dd Kinetic Theory</kwd></kwd-group></article-meta></front><body><sec id="s1"><title>1. Introduction</title><p>The Maxwell-Boltzmann (MB) distribution, see [<xref ref-type="bibr" rid="scirp.102258-ref1">1</xref>] [<xref ref-type="bibr" rid="scirp.102258-ref2">2</xref>], is a powerful tool to explain the kinetic theory of gases. The range in velocity of this distribution spans the interval [ 0, ∞ ] , which produces several problems:</p><p>1) The maximum velocity of a gas cannot be greater than the velocity of light, c.</p><p>2) The kinetic theory is developed in a classical environment, which means that the involved velocities should be smaller than ≈1/10c.</p><p>These items point toward the hypothesis of an upper bound in velocity for the MB. We will now report some approaches, including an upper bound in velocity: the ion velocities parallel to the magnetic field in a low density surface of a ionized plasma [<xref ref-type="bibr" rid="scirp.102258-ref3">3</xref>]; propagation of longitudinal electron waves in a collisionless, homogeneous, isotropic plasma, whose velocity distribution function is a truncated MB [<xref ref-type="bibr" rid="scirp.102258-ref4">4</xref>]; fast ion production in laser plasma [<xref ref-type="bibr" rid="scirp.102258-ref5">5</xref>]; the release of a dust particle from a plasma-facing wall [<xref ref-type="bibr" rid="scirp.102258-ref6">6</xref>]; an explanation of an anomaly in the Dark Matter (DAMA) experiment [<xref ref-type="bibr" rid="scirp.102258-ref7">7</xref>]; a distorted MB distribution of epithermal ions observed associated with the collapse of energetic ions [<xref ref-type="bibr" rid="scirp.102258-ref8">8</xref>]; and deviations to MB distribution that could have observable effects which can be measured trough the vapor spectroscopy at an interface [<xref ref-type="bibr" rid="scirp.102258-ref9">9</xref>]. However, these approaches do not clearly cover the effect of introducing a lower and an upper boundary in the MB distribution, which is the subject that will be analyzed in this paper.</p><p>This paper is structured as follows. Section 2 reviews the basic statistics of the MB distribution and it derives a new approximate expression for the median. Section 3 introduces the double truncated MB and it derives the connected statistics. Section 4 derives the relationship for root-mean-square speed versus temperature in the double truncated MB. Finally, Section 5.2 derives a new formula for Jeans flux in the exosphere.</p></sec><sec id="s2"><title>2. The Maxwell-Boltzmann Distribution</title><p>Let V be a random variable defined in [ 0, ∞ ] ; the MB probability density function (PDF), f ( v ; a ) , is</p><p>f ( v ; a ) = 2 v 2 e − 1 2 v 2 a 2 π a 3 , (1)</p><p>where a is a parameter and v denotes the velocity, see [<xref ref-type="bibr" rid="scirp.102258-ref1">1</xref>] [<xref ref-type="bibr" rid="scirp.102258-ref2">2</xref>]. Conversion to the physics is done by introducing the variable a, which is defined as</p><p>a = k T m , (2)</p><p>where m is the mass of the gas molecules, k is the Boltzmann constant and T is the thermodynamic temperature. With this change of variable, the MB PDF is</p><p>f p ( v ; m , k , T ) = 2 v 2 e − 1 2 v 2 m k T π ( k T m ) 3 2 , (3)</p><p>where the index p stands for physics. The distribution function (DF), F ( x ; a ) , is</p><p>F ( v ; a ) = 2 a 2 ( a π 2   erf ( 1 2 2 v a ) − 2 v e − 1 2 v 2 a 2 ) 2   π a 3 (4)</p><p>F p ( v ) = 2 ( ( k T m ) 3 2 π 2   erf ( 1 2 2 v 1 k T m ) m − 2 v e − 1 2 v 2 m k T k T ) 2 π ( k T m ) 3 2 m . (5)</p><p>The average value or mean, μ , is</p><p>μ ( a ) = 2 2 a π , (6)</p><p>μ ( m , k , T ) p = 2 2 π k T m , (7)</p><p>the variance, σ 2 , is</p><p>σ 2 ( a ) = a 2 ( − 8 + 3   π ) π (8)</p><p>σ 2 ( m , k , T ) p = k T ( − 8 + 3 π ) m π . (9)</p><p>The rth moment about the origin for the MB distribution is, μ ′ r , is</p><p>μ ′ r ( a ) = 2 r / 2 + 1 a r Γ ( r / 2 + 3 2 ) π (10)</p><p>μ ′ r ( m , k , T ) p = 2 r / 2 + 1 ( k T m ) r Γ ( r / 2 + 3 2 ) π , (11)</p><p>where</p><p>Γ ( z ) = ∫ 0 ∞ e − t t z − 1 d t , (12)</p><p>is the gamma function, see [<xref ref-type="bibr" rid="scirp.102258-ref10">10</xref>]. The root-mean-square speed , v r m s , can be obtained from this formula by inserting r = 2</p><p>v r m s ( a ) = 3 a (13)</p><p>v r m s ( m , k , T ) p = 3 k T m , (14)</p><p>see Equations (7-10-16) in [<xref ref-type="bibr" rid="scirp.102258-ref11">11</xref>]. This equation allows us to derive the temperature once the root-mean-square speed is measured</p><p>T = 1 3   v r m s 2 m k . (15)</p><p>The coefficient of variation (CV) is</p><p>C V = σ ( a ) μ ( a ) = 3 8 π − 1 , (16)</p><p>which is constant. The first three rth moments about the mean for the MB distribution, μ r ( a ) , are</p><p>μ 2 ( a ) = a 2 ( − 8 + 3   π ) π (17)</p><p>μ 3 ( a ) = − 2 a 3 2 ( 5 π − 16 ) π 3 / 2 (18)</p><p>μ 4 ( a ) = a 4 ( 15 π 2 + 16 π − 192 ) π 2 . (19)</p><p>The mode is at</p><p>v ( a ) = 2 a (20)</p><p>v ( m , k , T ) p = 2 k T m . (21)</p><p>An approximate expression for the median can be obtained by a Taylor series of the DF around the mode. The approximation formula is</p><p>v ( a ) = − 1 4 a ( − 6 + e ( erf ( 1 ) − 1 2 ) π ) 2 , (22)</p><p>v ( m , k , T ) p = − 1 4 k T m ( − 6 + e ( erf ( 1 ) − 1 2 ) π ) 2 , (23)</p><p>which has a percent error, δ , of δ ≈ 0.04 % in respect to the numerical value. The entropy is</p><p>l n ( 2 π a ) − 1 2 + γ , (24)</p><p>l n ( 2 π k T m ) − 1 2 + γ , (25)</p><p>where γ is the Euler-Mascheroni constant, which is defined as</p><p>γ = l i m n → ∞ ( 1 + 1 2 + 1 3 + ⋯ + 1 n − l n n ) = 0.57721 ⋯ , (26)</p><p>see [<xref ref-type="bibr" rid="scirp.102258-ref10">10</xref>] for more details. The coefficient of skewness is</p><p>( − 10 π + 32 ) 2 ( − 8 + 3 π ) 3 2 ≈ 0.48569, (27)</p><p>and the coefficient of kurtosis is</p><p>15 π 2 + 16 π − 192 ( − 8 + 3 π ) 2 ≈ 3.10816. (28)</p><p>According to [<xref ref-type="bibr" rid="scirp.102258-ref12">12</xref>], a random number generation can be obtained via inverse transform sampling when the distribution function or cumulative distribution function, F ( x ) , is known: 1) a pseudo number generator gives a random number R between zero and one; 2) the inverse function x = F − 1 ( R ) is evaluated; and 3) the procedure is repeated for different values of R. In our case, the inverse function should be evaluated in a numerical way by solving for v the following nonlinear equation</p><p>F ( v ; a ) − R = 0, (29)</p><p>F ( v ; m , k , T ) p − R = 0, (30)</p><p>where F ( v ) and F p ( v ) are the two DF represented by Equations (4) and (5). As a practical example, by inserting in Equation (29) a = 1 and R = 0.5 , we obtain in a numerical way v = 1.538 .</p></sec><sec id="s3"><title>3. The Double Truncated Maxwell-Boltzmann Distribution</title><p>Let V be a random variable that is defined in [ v l , v u ] ; the double truncated version of the Maxwell-Boltzmann PDF, f t ( v ; a , v l , v u ) , is</p><p>f t ( v ; a , v l , v u ) = v 2 e − 1 2 v 2 a 2 , (31)</p><p>where</p><p>C = − 2 C D , (32)</p><p>where</p><p>C D = a 2 ( − a π 2   erf ( 1 2 2 v u a ) + a π 2   erf ( 1 2 2 v l a )     + 2 v u e − 1 2 v u 2 a 2 − 2 v l e − 1 2 v l 2 a 2 ) , (33)</p><p>and erf ( x ) is the error function, which is defined as</p><p>erf ( x ) = 2 π ∫ 0 x   e − t 2 d t , (34)</p><p>see [<xref ref-type="bibr" rid="scirp.102258-ref10">10</xref>]. The physical meaning of a is still represented by Equation (2); however, due to the tendency to obtain complicated expressions, we will omit the double notation. The DF, F t ( v ; a , v l , v u ) , is</p><p>F t ( v ; a , v l , v u ) = C a 2 ( π 2 a   erf ( 1 2 2 v a ) − 2 v e − 1 2 v 2 a 2 ) 2 . (35)</p><p>The average value μ t ( a , v l , v u ) , is</p><p>μ t ( a , v l , v u ) = C a 2 ( 2 e − 1 2 v l 2 a 2 a 2 − 2 e − 1 2   v u 2 a 2 a 2 + e − 1 2 v l 2 a 2 v l 2 − e − 1 2 v u 2 a 2 v u 2 ) . (36)</p><p>The rth moment about the origin for the double truncated MB distribution is, μ ′ r , t ( a , v l , v u ) ,</p><p>μ ′ r , t ( a , v l , v u ) = M N r + 3 (37)</p><p>where</p><p>M N = C 2 r 4 + 5 4 a 2 &#215; ( ( v u 2 a 2 ) − r 4 − 1 4 v u r + 1 e − 1 4 v u 2 a 2 M r 4 + 1 4 , r 4 + 3 4 ( 1 2 v u 2 a 2 )     − v l r + 1 e − 1 4 v l 2 a 2 M r 4 + 1 4 , r 4 + 3 4 ( 1 2 v l 2 a 2 ) ( v l 2 a 2 ) − r 4 − 1 4 ) (38)</p><p>where M μ ,   ν ( z ) is the Whittaker M function, see [<xref ref-type="bibr" rid="scirp.102258-ref10">10</xref>]. The root-mean-square speed, v r m s , t ( a , v l , v u ) , can be obtained from this formula by inserting r = 2 , and is</p><p>v r m s , t ( a , v l , v u ) = N V 5   ( v u 2 a 2 ) 3 / 4 ( v l 2 a 2 ) 3 / 4 , (39)</p><p>where</p><p>N V = 2   C 2 3 / 4 a 2 ( v u 3 e − 1 / 4 v u 2 a 2 M 3 / 4 , 5 / 4 ( 1 / 2 v u 2 a 2 ) ( v l 2 a 2 ) 3 / 4     − v l 3 e − 1 / 4 v l 2 a 2 M 3 / 4 , 5 / 4 ( 1 / 2 v l 2 a 2 ) ( v u 2 a 2 ) 3 / 4 ) . (40)</p><p>The variance σ t 2 ( a , v l , v u ) is defined as</p><p>σ t 2 ( a , v l , v u ) = μ ′ 2, t ( a , v l , v u ) − ( μ ′ 1, t ( a , v l , v u ) ) 2 (41)</p><p>and has the following explicit form</p><p>σ t 2 ( a , v l , v u ) = 4 ( ( ( v l + 2 v u ) a 2 + v l v u ( v l + 1 2 v u ) ) ( a 2 + 1 / 2 v u 2 ) C 2 a 4 e − 1 2 v l 2 + 2 v u 2 a 2     − 2 ( ( v l + 1 2 v u ) a 2 + 1 4 v l v u ( v l + 2 v u ) ) C 2 a 4 ( a 2 + 1 2 v l 2 ) e − 1 2 2 v l 2 + v u 2 a 2     + ( a 2 + 1 2 v u 2 ) ( C   erf ( 1 2 2 v l a ) a 3 2 π     − C   erf ( 1 2 2 v u a ) a 3 2 π + 4 ) C a 2 ( a 2 + 1 2 v l 2 ) e − 1 2 v l 2 + v u 2 a 2</p><p>  + C 2 a 4 ( a 2 + 1 2 v l 2 ) 2 v l e − 3 2 v l 2 a 2 − ( a 2 + 1 2 v u 2 ) 2 C 2 a 4 v u e − 3 2 v u 2 a 2   + ( 3 4 a 2 v l + 1 4   v l 3 ) e − 1 2 v l 2 a 2 + ( − 3 4 a 2 v u − 1 4 v u 3 ) e − 1 2 v u 2 a 2   − 1 2 ( ( C   erf ( 1 2 2 v l a ) a 3 2 π   − C   erf ( 1 2 2 v u a ) a 3 2 π + 4 ) C ( a 2 + 1 2 v l 2 ) 2 e − v l 2 a 2</p><p>  + ( a 2 + 1 2 v u 2 ) 2 ( C   erf ( 1 2 2 v l a ) a 3 2 π   − C   erf ( 1 2 2 v u a ) a 3 2 π + 4 ) C e − v u 2 a 2   + 3 4 π 2 ( − erf ( 1 2 2 v u a ) + erf ( 1 2 2 v l a ) ) a ) a 2 ) C a 2 . (42)</p><p>Although the coefficients of skewness and kurtosis for the truncated MB exist, they have a complicated expression.</p></sec><sec id="s4"><title>4. A Laboratory Application</title><p>The temperature as a function of root-mean-square speed for the MB is given by Equation (15). In the truncated MB distribution, the temperature can be found by solving the following nonlinear equation</p><p>v r m s , t ( k , m , T , v l , v u ) = v r m s , m , (43)</p><p>where v r m s , m is not a theoretical variable but is the root-mean-square speed measured in the laboratory and v r m s , t is given by Equation (39). The laboratory measures of v r m s , m started with [<xref ref-type="bibr" rid="scirp.102258-ref13">13</xref>], where a v r m s , m = 388   m / s at 400˚C was found for a metallic vapor. In the truncated MB distribution, there are three parameters that can be measured in the laboratory from a kinematical point of view, as follows: the lowest velocity, v l ; the highest velocity, v u ; and the root-mean-square speed, v r m s , m . Setting for simplicity v l = 0 , we will now explore the effect of the variation of v u on the root-mean-square speed; see <xref ref-type="fig" rid="fig1">Figure 1</xref>. The first example of the influence of the upper limit in velocity on the temperature is given by potassium gas [<xref ref-type="bibr" rid="scirp.102258-ref14">14</xref>] [<xref ref-type="bibr" rid="scirp.102258-ref15">15</xref>], in which molecular mass is 6.492429890 &#215; 10<sup>−26</sup> kg. In <xref ref-type="fig" rid="fig2">Figure 2</xref>, we evaluate in a numerical way the temperature when v l = 0 and v u is variable in the case of a measured value of v r m s , m .</p><p>The second example is given by diatomic nitrogen, N<sub>2</sub>, in which molecular mass is 4.651737684 &#215; 10<sup>−26</sup> kg. In <xref ref-type="fig" rid="fig3">Figure 3</xref>, we evaluate the temperature when v l = 0 and v u is a variable in the case of a measured value of v r m s , m .</p></sec><sec id="s5"><title>5. The Jeans Escape</title><p>The standard formula for the escape of molecules from the exosphere is reviewed in the framework of the MB distribution. A new formula for the Jeans escape is derived in the framework of the truncated MB.</p><sec id="s5_1"><title>5.1. The Standard Case</title><p>In the exosphere, a molecule of mass m and velocity v e is free to escape when</p><p>1 2 m v e 2 − G M m R e x = 0, (44)</p><p>where G is the Newtonian gravitational constant, M is the mass of the Earth, R e x = R + H is the radius of the exosphere, R is the radius of the Earth and H is the altitude of the exosphere. The flux of the molecules that are living in the exosphere Φ j is</p><p>Φ j = 1 4 N e x μ e , (45)</p><p>where N e x is the number of molecules per unit volume and μ e is the average velocity of escape. In the presence of a given number of molecules per unit volume, the standard MB distribution in velocities in a unit volume, f m , is</p><p>f m ( v ; m , k , T , N e x ) = N e x 2 v 2 e − 1 2 v 2 m k T π ( k T m ) 3 2 . (46)</p><p>The average value of escape is defined as</p><p>μ e = ∫ v e ∞     v f m ( v ; m , k , T , N e x ) d v ∫ 0 ∞     f m ( v ; m , k , T , N e x ) d v . (47)</p><p>In this integral, the following changes are made to the variables</p><p>λ = 1 2 m v 2 k T . (48)</p><p>Therefore,</p><p>μ e = 2   ( λ e + 1 ) e − λ e 2 k T π   m , (49)</p><p>with</p><p>λ e = 2   G M R e x v 0 2 , (50)</p><p>where v 0 is the mode as represented by Equation (21). The flux is now</p><p>Φ j = N e x ( λ e + 1 ) e − λ e v 0 2 π . (51)</p><p>For more details see [<xref ref-type="bibr" rid="scirp.102258-ref16">16</xref>] [<xref ref-type="bibr" rid="scirp.102258-ref17">17</xref>] [<xref ref-type="bibr" rid="scirp.102258-ref18">18</xref>] [<xref ref-type="bibr" rid="scirp.102258-ref19">19</xref>]. On adopting the parameters of <xref ref-type="table" rid="table1">Table 1</xref> the Jeans escape flux for hydrogen is</p><p>Φ j = 3.98 &#215; 10 11   molecules ⋅ m − 2 ⋅ s − 1 , (52)</p><p>and</p><p>λ e = 7.78. (53)</p><p>The Jeans escape flux for Earth at T = 900   K varies between Φ j ≈ 2.7 &#215; 10 11 molecules ⋅ m − 2 ⋅ s − 1 ; see [<xref ref-type="bibr" rid="scirp.102258-ref20">20</xref>] or <xref ref-type="fig" rid="fig1">Figure 1</xref> in [<xref ref-type="bibr" rid="scirp.102258-ref21">21</xref>]. and Φ j ≈ 4 &#215; 10 11 molecules ⋅ m − 2 ⋅ s − 1 , see [<xref ref-type="bibr" rid="scirp.102258-ref22">22</xref>]. Therefore, our choice of parameters is compatible with the suggested interval in flux.</p></sec><sec id="s5_2"><title>5.2. The Truncated Case</title><p>The average value of escape for a truncated MB distribution, μ e , t , is</p><p>μ e , t = ∫ v e ∞     v f t ( v ; m , k , T , N e x , v l , v u ) d v ∫ 0 ∞     f m ( v ; m , k , T , N e x , v l , v u ) d v . (54)</p><p>This integral can be solved by introducing the change of variable as given by Equation (48)</p><p>μ e , t = − 2   ( ( λ u + 1 ) e − λ u − e − λ e ( λ e + 1 ) ) 2 2 λ l e − λ l − 2 λ u e − λ u − π   erf ( λ l ) + π   erf ( λ u ) k T m , (55)</p><p>where λ l is the lower value of λ and λ u is the upper value of λ . The flux of the molecules that are living the exosphere in the truncated MB, Φ j , t , is</p><p>Φ j , t = N e x ( ( λ u + 1 ) e − λ u − e − λ e ( λ e + 1 ) ) 2 4 λ u e − λ u + 2 π   erf ( λ l ) − 2 π   erf ( λ u ) − 4 λ l e − λ l k T m . (56)</p><p>The increasing flux of molecules is outlined when one parameter, λ l , is variable; see <xref ref-type="fig" rid="fig4">Figure 4</xref>. In other words, an increase in λ l produces an increase in the flux of the molecules. The dependence of the flux when two parameters are variable, λ l and λ u , is reported in <xref ref-type="fig" rid="fig5">Figure 5</xref>.</p><table-wrap id="table1" ><label><xref ref-type="table" rid="table1">Table 1</xref></label><caption><title> Adopted physical parameters for the exosphere</title></caption><table><tbody><thead><tr><th align="center" valign="middle" >Parameter</th><th align="center" valign="middle" >Value</th></tr></thead><tr><td align="center" valign="middle" >R<sub>ex</sub></td><td align="center" valign="middle" >6900 km</td></tr><tr><td align="center" valign="middle" >T</td><td align="center" valign="middle" >900 K</td></tr><tr><td align="center" valign="middle" >N<sub>ex</sub></td><td align="center" valign="middle" >10<sup>11</sup> m<sup>−3</sup></td></tr></tbody></table></table-wrap><p>These Jeans escape fluxes for Earth are compatible with the observed values that were reported in Section 5.1.</p></sec></sec><sec id="s6"><title>6. Conclusion</title><p>This paper derived analytical formulae for the following quantities for a double truncated MB distribution: the PDF, the DF, the average value, the rth moment about the origin, the root-mean-square speed and the variance. The traditional correspondence between root-mean-square speed and temperature is replaced by the nonlinear Equation (43). The new formula (56) for the Jeans escape flux of molecules from an atmosphere is now a function of the lower and upper boundary in velocity.</p></sec><sec id="s7"><title>Conflicts of Interest</title><p>The author declares no conflicts of interest regarding the publication of this paper.</p></sec><sec id="s8"><title>Cite this paper</title><p>Zaninetti, L. (2020) New Probability Distributions in Astrophysics: III. The Truncated Maxwell-Boltzmann Distribution. 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