<?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.2024.141002</article-id><article-id pub-id-type="publisher-id">IJAA-131976</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>
 
 
  Does the Redshift Distribution of &lt;i&gt;Swift&lt;/i&gt; Long GRBs Trace the Star-Formation Rate?
 
</article-title></title-group><contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Ali</surname><given-names>M. Hasan</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>Walid</surname><given-names>J. Azzam</given-names></name><xref ref-type="aff" rid="aff1"><sup>1</sup></xref><xref ref-type="corresp" rid="cor1"><sup>*</sup></xref></contrib></contrib-group><aff id="aff1"><addr-line>Department of Physics, College of Science, University of Bahrain, Sakhir, Bahrain</addr-line></aff><pub-date pub-type="epub"><day>18</day><month>03</month><year>2024</year></pub-date><volume>14</volume><issue>01</issue><fpage>20</fpage><lpage>44</lpage><history><date date-type="received"><day>3,</day>	<month>February</month>	<year>2024</year></date><date date-type="rev-recd"><day>22,</day>	<month>March</month>	<year>2024</year>	</date><date date-type="accepted"><day>25,</day>	<month>March</month>	<year>2024</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>
 
 
  Gamma-ray bursts (GRBs) are extremely powerful explosions that have been traditionally classified into two categories: long bursts (LGRBs) with an observed duration 
  <em>T</em>
  <sub>90 </sub>&gt; 2 s, and short bursts (SGRBs) with an observed duration 
  <em>T</em>
  <sub>90</sub> &lt; 2 s, where 
  <em>T</em>
  <sub>90</sub> is the time interval during which 90% of the fluence is detected. LGRBs are believed to emanate from the core-collapse of massive stars, while SGRBs are believed to result from the merging of two compact objects, like two neutron stars. Because LGRBs are produced by the violent death of massive stars, we expect that their redshift distribution should trace the star-formation rate (SFR). The purpose of our study is to investigate the extent to which the redshift distribution of LGRBs follows and reflects the SFR. We use a sample of 370 LGRBs taken from the 
  <em>Swift</em> catalog, and we investigate different models for the LGRB redshift distribution. We also carry out Monte Carlo simulations to check the consistency of our results. Our results indicate that the SFR can describe the LGRB redshift distribution well for high redshift bursts, but it needs an evolution term to fit the distribution well at low redshift.
 
</p></abstract><kwd-group><kwd>Gamma-Ray Bursts</kwd><kwd> Redshift Distribution</kwd><kwd> Star-Formation Rate</kwd></kwd-group></article-meta></front><body><sec id="s1"><title>1. Introduction</title><p>Although more than 50 years have passed since the first paper on gamma-ray bursts (GRBs) was published [<xref ref-type="bibr" rid="scirp.131976-ref1">1</xref>] , we still have many questions regarding their nature and characteristics. They are the focus of many research studies due to their potential as cosmological probes [<xref ref-type="bibr" rid="scirp.131976-ref2">2</xref>] - [<xref ref-type="bibr" rid="scirp.131976-ref8">8</xref>] . GRBs are traditionally classified into two main types: long GRBs (LGRBs) with T<sub>90</sub> &gt; 2 s and short GRBs (SGRBs) with T<sub>90</sub> &lt; 2 s [<xref ref-type="bibr" rid="scirp.131976-ref9">9</xref>] , where T<sub>90</sub> is the observed duration during which 90% of the fluence is detected. It is theorized that the origin of LGRBs is the core-collapse of massive stars, while SGRBs are thought to originate from compact object mergers [<xref ref-type="bibr" rid="scirp.131976-ref10">10</xref>] [<xref ref-type="bibr" rid="scirp.131976-ref11">11</xref>] [<xref ref-type="bibr" rid="scirp.131976-ref12">12</xref>] . Hence, it is expected that there will be a correlation between the star formation rate (SFR) and the LGRB formation rate, which encouraged researchers to investigate the redshift distribution of GRBs, and especially that of LGRBs.</p><p>However, it is important to note that the connection between the SFR and the LGRB redshift distribution is a controversial one, with many conflicting results in the literature. The controversy lies in whether there is an observed excess of GRBs at low or high redshift compared to what is implied by the SFR. The study by [<xref ref-type="bibr" rid="scirp.131976-ref13">13</xref>] is one of the first major contributions to this problem. Although the connection between the SFR and LGRB redshift distribution had been studied before, see for example [<xref ref-type="bibr" rid="scirp.131976-ref14">14</xref>] , the study by [<xref ref-type="bibr" rid="scirp.131976-ref13">13</xref>] is one of the first to account for completeness and to place constraints on the GRB luminosity function and its evolution. Their study found evidence for a possible luminosity or density evolution of LGRBs compared to what is expected from the SFR [<xref ref-type="bibr" rid="scirp.131976-ref13">13</xref>] . A recent study, but with a larger data sample, by [<xref ref-type="bibr" rid="scirp.131976-ref15">15</xref>] found similar results. An earlier study by [<xref ref-type="bibr" rid="scirp.131976-ref16">16</xref>] , which utilized 127 LGRBs observed by the Swift satellite, found an excess in GRBs at low redshift compared to the SFR. Although some studies backed the low-redshift excess claims [<xref ref-type="bibr" rid="scirp.131976-ref17">17</xref>] [<xref ref-type="bibr" rid="scirp.131976-ref18">18</xref>] [<xref ref-type="bibr" rid="scirp.131976-ref19">19</xref>] [<xref ref-type="bibr" rid="scirp.131976-ref20">20</xref>] , other studies found an excess in GRBs, not at low redshift, but at high redshift [<xref ref-type="bibr" rid="scirp.131976-ref21">21</xref>] [<xref ref-type="bibr" rid="scirp.131976-ref22">22</xref>] .</p><p>Moreover, many studies have opposed the excess GRB accounts, especially at low redshifts. The study by [<xref ref-type="bibr" rid="scirp.131976-ref23">23</xref>] was one of the earliest to do so, where they carried out Monte Carlo simulations and compared their results with previously published claims of low redshift excess – the aforementioned [<xref ref-type="bibr" rid="scirp.131976-ref16">16</xref>] [<xref ref-type="bibr" rid="scirp.131976-ref19">19</xref>] studies. They showed that the excess GRBs result from the incompleteness of the dataset, and that a complete dataset shows no excess in GRBs. The study by [<xref ref-type="bibr" rid="scirp.131976-ref23">23</xref>] also conducted a non-parametric C<sup>−</sup> investigation. However, their non-parametric study seems misleading as discussed by [<xref ref-type="bibr" rid="scirp.131976-ref24">24</xref>] who made an in-depth study about the non-parametric methods and how their misuse can lead to incorrect results. They analyzed datasets of previous GRB luminosity/redshift evolution studies, like the previously mentioned [<xref ref-type="bibr" rid="scirp.131976-ref16">16</xref>] [<xref ref-type="bibr" rid="scirp.131976-ref18">18</xref>] [<xref ref-type="bibr" rid="scirp.131976-ref20">20</xref>] [<xref ref-type="bibr" rid="scirp.131976-ref23">23</xref>] . They found that many studies underestimated the detection threshold of GRB satellites which resulted in incomplete datasets, and hence showed an excess in GRBs. They also created a Monte Carlo simulation, which they found to agree with the Monte Carlo simulations conducted by [<xref ref-type="bibr" rid="scirp.131976-ref23">23</xref>] ; in other words, excess GRBs resulted from incomplete datasets. The investigation by [<xref ref-type="bibr" rid="scirp.131976-ref25">25</xref>] also found no excess GRBs at any redshift.</p><p>More recently, the excess GRBs at low redshift claims have started to reemerge. They are mainly driven by studies conducted by [<xref ref-type="bibr" rid="scirp.131976-ref26">26</xref>] [<xref ref-type="bibr" rid="scirp.131976-ref27">27</xref>] . In the first study, [<xref ref-type="bibr" rid="scirp.131976-ref26">26</xref>] formed two sets of GRBs composed of 54 and 79 LGRBs, with 61% and 67% completeness, respectively. They found an excess of LGRBs at low redshift, even with the completeness of the dataset taken into consideration. The second study [<xref ref-type="bibr" rid="scirp.131976-ref27">27</xref>] focused on potential reasons for this excess of LGRBs. They split their datasets into low and high luminosity LGRBs. They found that the high luminosity LGRB dataset follows the SFR without any excess, while the low luminosity LGRB dataset did show an excess of LGRBs at low redshifts. They argue that their results may hint at new origins for low luminosity LGRBs, thus disconnecting the LGRB formation rate from the SFR. Interestingly, there were some recent reports that suggest that LGRBs can be produced by compact object mergers, instead of massive star collapse [<xref ref-type="bibr" rid="scirp.131976-ref28">28</xref>] [<xref ref-type="bibr" rid="scirp.131976-ref29">29</xref>] . Moreover, there have been studies that investigated the effect of metallicity on the LGRB distribution and have found it to be influential [<xref ref-type="bibr" rid="scirp.131976-ref30">30</xref>] [<xref ref-type="bibr" rid="scirp.131976-ref31">31</xref>] . Perhaps these can be potential reasons for the excess GRB dilemma. Although as it stands, there is no clear answer to this problem.</p><p>The aim of our current study is to investigate the distribution of LGRBs with redshift and to fit it with several proposed models. A full LGRB data set is used without constraints, including biases in detection, to study how it is linked to the star formation rate. We aim to examine the nature of the evolution term and see how it impacts the redshift distribution of LGRBs. Section 2 provides a detailed description of our method, while Section 3 presents our results and analysis. We provide a brief conclusion in the last section.</p></sec><sec id="s2"><title>2. Method</title><p>The data sample that we use is collected from the Swift catalog<sup>1</sup>. The data sample is composed of 370 LGRBs with T<sub>90</sub> &gt; 2 s. The dataset is found in <xref ref-type="table" rid="table">Table </xref>A1 in Appendix A. We divided the sample into 30 bins for 0 ≤ z ≤ 10 with equal bin</p><p>sizes d z = 1 3 , and we then normalized the distribution. Mathematically, the distribution of GRBs can be written as:</p><p>Φ ( z ) = d N d z = d N d V d V d z = A ψ * ( z ) 1 + z ϕ ( z ) d V ( z ) d z (1)</p><p>where ψ * ( z ) is the star-formation rate density (SFRD), ϕ ( z ) is a term that contains all contributions to the distribution other than the SFRD, d V d z is the</p><p>co-moving volume element and A is a normalization constant. In this paper, we do not assign any specific “meaning” to ϕ ( z ) and A. All possible contributions such as the luminosity function, density evolution, sensitivity of the detectors and others are included in ϕ ( z ) . Our aim is to gain insight on the nature of ϕ ( z ) without presuming any prior connections or contributions from other sources. This is done to focus our work on the link to the SFRD, and to evaluate how significant the other contributions are to the redshift distribution of LGRBs. We caution here that since detection bias is also considered in Equation (1), then the equation represents the GRB detection distribution, rather than the formation distribution.</p><p>The SFRD that is typically used in the literature in units of M ⊙ ⋅ yr − 1 ⋅ Mpc − 3 is [<xref ref-type="bibr" rid="scirp.131976-ref32">32</xref>] [<xref ref-type="bibr" rid="scirp.131976-ref33">33</xref>] :</p><p>ψ * ( z ) = 0.0157 + 0.118 z 1 + ( z 3.23 ) 4.66 (2)</p><p>We adopt the ΛCMD model in this study, which gives:</p><p>d V d z = 4 π c D L 2 H 0 ( 1 + z ) 2 Ω M ( 1 + z ) 3 + Ω Λ (3)</p><p>where D L is the luminosity distance, which is given by:</p><p>D L ( z ) = ( 1 + z ) c H 0 ∫ 0 z d z Ω M ( 1 + z ) 3 + Ω Λ (4)</p><p>and H 0 = 70.8   km / s / MPc , Ω M = 0.27 , and Ω Λ = 1 − Ω M = 0.73 are the adopted cosmological parameters.</p><p>We investigated and fitted our data sample with multiple models and the goodness of the fit for each model was determined using the least χ 2 test:</p><p>χ 2 = ∑ i ( N i swift − N i cal ) 2 σ i 2 (5)</p><p>where σ i = N i swift is the Poisson error (68% confidence). The best fitting model is the one that gave the least χ 2 value.</p><p>The first model that we tried was a “no contributions” model, ϕ ( z ) = constant , with the SFRD and the cosmological model being the only contributors. Then, we tested five different contribution terms ϕ ( z ) : a power law, a broken power law, a triple power law, an exponential term, and an exponential-power law, as follows:</p><p>ϕ pow ( z ) = ( 1 + z ) α (6)</p><p>ϕ broken ( z ) = { ( 1 + z ) α ( 1 + r 1 ) α         for   z ≤ r 1 ( 1 + z ) β ( 1 + r 1 ) β         for   z &gt; r 1 (7)</p><p>ϕ triple ( z ) = { ( 1 + z ) α ( 1 + r 1 ) α for   z ≤ r 1 ( 1 + z ) β ( 1 + r 1 ) β for   r 1 &lt; z ≤ r 2 ( 1 + r 2 ) β ( 1 + r 1 ) δ 2 ( 1 + z ) γ ( 1 + r 2 ) γ for   r 2 ≤ z (8)</p><p>ϕ exp ( z ) = e μ z (9)</p><p>ϕ exp -pow ( z ) = ( 1 + z ) α e μ z (10)</p><p>where α , β , γ , μ , r 1 , and r 2 are the optimization parameters<sup>2</sup>. Although we do not force any specific form on ϕ ( z ) , the expressions that we selected and chose to investigate are based on our intuitive expectations of the insight that they might provide. The broken and triple power laws were selected to give insight on how the distribution behaves at different redshift ranges. The power and exponential laws were selected to be compared with the broken/triple power law to see if the evolution is region specific, or generic to the whole distribution.</p><p>In this work, we chose two optimization methods. The first was a fitting method. The fitting was done for α , β , γ , μ , while r 1 and r 2 were found by looping over them and finding the optimal values that minimize χ 2 . The second method involved using the Metropolis-Hastings Markov Chain Monte Carlo (MCMC) algorithm [<xref ref-type="bibr" rid="scirp.131976-ref34">34</xref>] . The method used is described by Foreman-Mackey and Hogg and utilizes their Python libraries emcee<sup>3</sup> and corner.py<sup>4</sup> [<xref ref-type="bibr" rid="scirp.131976-ref35">35</xref>] [<xref ref-type="bibr" rid="scirp.131976-ref36">36</xref>] . The log of the likelihood function that we wish to maximize is of the form:</p><p>ln L = − 1 2 ∑ i [ ( N i swift − N i cal ) 2 σ i 2 ] = − 1 2 χ 2 . (11)</p><p>Then χ 2 can be calculated as follows:</p><p>χ 2 = − 2 ln L (12)</p><p>Here maximizing the likelihood function is equivalent to minimizing the χ 2 value. However, since the models used include different numbers of parameters, the Akaike information criterion (AIC) was used to assess the goodness of the fits and to compare the different models [<xref ref-type="bibr" rid="scirp.131976-ref37">37</xref>] [<xref ref-type="bibr" rid="scirp.131976-ref38">38</xref>] :</p><p>AIC = 2 k + χ 2 = 2 k − 2 ln ( L ) (13)</p><p>where k is the number of parameters. The better fitting model is the one that minimizes the AIC value.</p><p>We then used the MCMC simulations to fit the data to the following:</p><p>1) A new SFRD-like function—call it the GRB detection density function (GRB-DD):</p><p>ψ GRB ( z ) = α + β z 1 + ( z γ ) δ (14)</p><p>2) A broken power law (see Equation (7)).</p><p>3) A triple power law (see Equation (8)).</p><p>4) An exponential-power law (see Equation (10)).</p><p>For each case, we report the mean of the probability distribution and its deviation, the best fitting value, the χ 2 value, and the AIC.</p></sec><sec id="s3"><title>3. Results</title><p>The normalized redshift distribution of the data sample used is shown in <xref ref-type="fig" rid="fig1">Figure 1</xref>(a).</p><p>The main highlight of the results is the immediate spike of the number density, peaking at z ~ 1.25 . Comparing that with the density calculated with no evolution (<xref ref-type="fig" rid="fig1">Figure 1</xref>(b)), we can see that the “no evolution” density peaks at z = 2 with a subtle increase compared to the Swift data. Focusing on the low and high redshift regions, we notice the calculated density matches the Swift distribution at high redshifts. However, at low redshifts it is a shifted version of the Swift data, shifted to the right by about Δ z ~ 0.5 . To solve this issue, one might shift the density left but that would not solve the problem, as then it would underestimate the number density at z ≳ 4 , which presents the main issue with this model. We need a term ϕ ( z ) to be included in the density that scales it at low redshift while maintaining a good fit at high redshifts, like the SFRD (<xref ref-type="fig" rid="fig1">Figure 1</xref>(b)).</p><sec id="s3_1"><title>3.1. Fitting Results</title><p>We fitted the data sample with the proposed functions (Equations (6) to (10)), and we extracted the relevant parameters. The results are shown in <xref ref-type="table" rid="table">Table </xref>1. Based on the AIC test, the best fit occurred when we used the triple power law, the second best fit when we used the broken power law, and the third best fit when we used the exponential-power law. The power law and the exponential cases show very poor fitting. These results highlight the need for an additional ϕ ( z ) factor and suggest that it is redshift “region” specific.</p></sec><sec id="s3_2"><title>3.2. MCMC Results</title><p>The MCMC results are shown in <xref ref-type="table" rid="table">Table </xref>2. It is notable that the results agree mostly with the fitting results found (within 1σ) and lead to the same conclusion. Thus, we can conclude that the results are consistent with each other. All proposed models show good fitting, with the triple power law showing the best fit. <xref ref-type="fig" rid="fig2">Figure 2</xref> plots all the models for comparison.</p><p>Now focusing on the variation between the fitting of the contributions at low and high redshifts, we notice that the results show a significant difference between the two redshift regions. This is clearly exhibited by the fitting and MCMC results, particularly in the broken power law and the triple power law cases. These cases mainly split the distribution into two regions, separated at around z ~ 1.75 . Below z ≲ 1.75 , there is a high contribution from ϕ ( z ) with powers α = − 2.56 − 0.54 + 0.41 (broken power law), and α = − 5.36 − 2.12 + 2.60 and β = − 2.01 − 0.50 + 0.91 (triple power law). Meanwhile, for z ≳ 1.75 , the contribution from ϕ ( z ) becomes much less impactful with values β = 0.00 − 0.31 + 0.30 (broken power law) and γ = 0.06 − 0.29 + 0.30 (triple power law).</p><p>We see the same behavior with the GRB-DD fit. The values for β , γ , and δ that we found coincide with the literature reported values (see Equation (2)) within 1σ (2σ in the case of β ). The major difference is in α , with the value found by MCMC being α = 2.88 − 1.37 + 1.28 compared to the literature reported value</p><table-wrap id="table1" ><label><xref ref-type="table" rid="table">Table </xref>1</label><caption><title> The parameters calculated by fitting for the different cases studied with their standard deviations (if applicable)</title></caption><table><tbody><thead><tr><th align="center" valign="middle" ></th><th align="center" valign="middle" >α</th><th align="center" valign="middle" >β</th><th align="center" valign="middle" >γ</th><th align="center" valign="middle" >μ</th><th align="center" valign="middle" >r 1</th><th align="center" valign="middle" >r 2</th><th align="center" valign="middle" >χ 2</th><th align="center" valign="middle" >AIC</th></tr></thead><tr><td align="center" valign="middle" >Only SFRD Contribution</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><td align="center" valign="middle" >83.948</td><td align="center" valign="middle" >---</td></tr><tr><td align="center" valign="middle" >Power Law</td><td align="center" valign="middle" >−1.242 &#177; 0.166</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" >50.964</td><td align="center" valign="middle" >52.964</td></tr><tr><td align="center" valign="middle" >Broken Power Law</td><td align="center" valign="middle" >−2.845 &#177; 0.276</td><td align="center" valign="middle" >0.043 &#177; 0.244</td><td align="center" valign="middle" >-</td><td align="center" valign="middle" >-</td><td align="center" valign="middle" >1.780</td><td align="center" valign="middle" >-</td><td align="center" valign="middle" >15.748</td><td align="center" valign="middle" >21.748</td></tr><tr><td align="center" valign="middle" >Triple Power Law</td><td align="center" valign="middle" >−7.117 &#177; 1.078</td><td align="center" valign="middle" >−2.595 &#177; 0.297</td><td align="center" valign="middle" >−0.016 &#177; 0.249</td><td align="center" valign="middle" >-</td><td align="center" valign="middle" >0.500</td><td align="center" valign="middle" >1.800</td><td align="center" valign="middle" >8.184</td><td align="center" valign="middle" >18.184</td></tr><tr><td align="center" valign="middle" >Exponential</td><td align="center" valign="middle" >-</td><td align="center" valign="middle" >-</td><td align="center" valign="middle" >-</td><td align="center" valign="middle" >−0.271 &#177; 0.054</td><td align="center" valign="middle" >-</td><td align="center" valign="middle" >-</td><td align="center" valign="middle" >66.960</td><td align="center" valign="middle" >68.960</td></tr><tr><td align="center" valign="middle" >Exponential-Power</td><td align="center" valign="middle" >−3.742 &#177; 0.466</td><td align="center" valign="middle" >-</td><td align="center" valign="middle" >-</td><td align="center" valign="middle" >0.767 &#177; 0.134</td><td align="center" valign="middle" >-</td><td align="center" valign="middle" >-</td><td align="center" valign="middle" >23.684</td><td align="center" valign="middle" >27.684</td></tr></tbody></table></table-wrap><table-wrap id="table2" ><label><xref ref-type="table" rid="table">Table </xref>2</label><caption><title> The MCMC optimization results. The table includes the mean of the probability distribution and its deviation, the best fitting value, the χ 2 value, and the AIC value for each case. The corresponding contour plots of each case can be found in Appendix B</title></caption><table><tbody><thead><tr><th align="center" valign="middle"  colspan="2"  ></th><th align="center" valign="middle" >α</th><th align="center" valign="middle" >β</th><th align="center" valign="middle" >γ</th><th align="center" valign="middle" >δ</th><th align="center" valign="middle" >μ</th><th align="center" valign="middle" >r 1</th><th align="center" valign="middle" >r 2</th><th align="center" valign="middle" >χ 2</th><th align="center" valign="middle" >AIC</th></tr></thead><tr><td align="center" valign="middle"  rowspan="2"  >GRB-DD Contribution</td><td align="center" valign="middle" >Most Probable</td><td align="center" valign="middle" >2.88 − 1.37 + 1.28</td><td align="center" valign="middle" >− 0.20 − 0.13 + 0.16</td><td align="center" valign="middle" >4.74 − 0.60 + 0.69</td><td align="center" valign="middle" >4.94 − 1.23 + 1.26</td><td align="center" valign="middle" >-</td><td align="center" valign="middle" >-</td><td align="center" valign="middle" >-</td><td align="center" valign="middle"  rowspan="2"  >17.499</td><td align="center" valign="middle"  rowspan="2"  >25.499</td></tr><tr><td align="center" valign="middle" >Best Fit</td><td align="center" valign="middle" >3.190</td><td align="center" valign="middle" >−0.365</td><td align="center" valign="middle" >5.434</td><td align="center" valign="middle" >5.463</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"  rowspan="2"  >Broken Power Law</td><td align="center" valign="middle" >Most Probable</td><td align="center" valign="middle" >− 2.56 − 0.54 + 0.41</td><td align="center" valign="middle" >0.00 − 0.31 + 0.30</td><td align="center" valign="middle" >-</td><td align="center" valign="middle" >-</td><td align="center" valign="middle" >-</td><td align="center" valign="middle" >1.71 − 0.30 + 0.23</td><td align="center" valign="middle" >-</td><td align="center" valign="middle"  rowspan="2"  >17.145</td><td align="center" valign="middle"  rowspan="2"  >23.145</td></tr><tr><td align="center" valign="middle" >Best Fit</td><td align="center" valign="middle" >−2.485</td><td align="center" valign="middle" >0.082</td><td align="center" valign="middle" >-</td><td align="center" valign="middle" >-</td><td align="center" valign="middle" >-</td><td align="center" valign="middle" >1.767</td><td align="center" valign="middle" >-</td></tr><tr><td align="center" valign="middle"  rowspan="2"  >Triple Power Law</td><td align="center" valign="middle" >Most Probable</td><td align="center" valign="middle" >− 5.36 − 2.12 + 2.60</td><td align="center" valign="middle" >− 2.01 − 0.50 + 0.91</td><td align="center" valign="middle" >0.06 − 0.29 + 0.30</td><td align="center" valign="middle" >-</td><td align="center" valign="middle" >-</td><td align="center" valign="middle" >0.55 − 0.19 + 0.73</td><td align="center" valign="middle" >1.89 − 0.22 + 0.43</td><td align="center" valign="middle"  rowspan="2"  >10.657</td><td align="center" valign="middle"  rowspan="2"  >20.657</td></tr><tr><td align="center" valign="middle" >Best Fit</td><td align="center" valign="middle" >−6.280</td><td align="center" valign="middle" >−2.111</td><td align="center" valign="middle" >0.052</td><td align="center" valign="middle" >-</td><td align="center" valign="middle" >-</td><td align="center" valign="middle" >0.520</td><td align="center" valign="middle" >1.855</td></tr><tr><td align="center" valign="middle"  rowspan="2"  >Exponential-Power</td><td align="center" valign="middle" >Most Probable</td><td align="center" valign="middle" >− 3.23 − 0.44 + 0.48</td><td align="center" valign="middle" >-</td><td align="center" valign="middle" >-</td><td align="center" valign="middle" >-</td><td align="center" valign="middle" >0.67 − 0.13 + 0.12</td><td align="center" valign="middle" >-</td><td align="center" valign="middle" >-</td><td align="center" valign="middle"  rowspan="2"  >26.523</td><td align="center" valign="middle"  rowspan="2"  >30.523</td></tr><tr><td align="center" valign="middle" >Best Fit</td><td align="center" valign="middle" >−3.291</td><td align="center" valign="middle" >-</td><td align="center" valign="middle" >-</td><td align="center" valign="middle" >-</td><td align="center" valign="middle" >0.686</td><td align="center" valign="middle" >-</td><td align="center" valign="middle" >-</td></tr></tbody></table></table-wrap><p>of α = 0.0157 (see Equation (2)). <xref ref-type="fig" rid="fig3">Figure 3</xref> shows a plot of the GRB-DD and SFRD for reference. We see that the difference between the two functions is very large at low redshifts but becomes smaller as the redshift increases to z &gt; 4 .</p><p>To summarize, our results show that the Swift data are consistent with the SFRD at high redshifts, and only requires an evolution term that enhances it at low redshifts. This means that if the LGRBs are to follow the SFR, then whatever factors that might affect their detection must have a stronger influence at low redshift than at high redshift. Also, it is notable that high redshift LGRBs detected by Swift are predominantly high luminosity ones. Hence, since our results follow the SFR at high redshifts, they support the findings of [<xref ref-type="bibr" rid="scirp.131976-ref27">27</xref>] .</p><p>One important factor to mention that may affect the results is the classification of GRBs. In our analysis, we followed the traditional definition of LGRBs (T<sub>90</sub> &gt; 2 s). This definition is widely debated among researchers with many of the newer studies pushing for updated classifications [<xref ref-type="bibr" rid="scirp.131976-ref39">39</xref>] - [<xref ref-type="bibr" rid="scirp.131976-ref45">45</xref>] . Thus, in the future one might investigate this issue further when studying the connection between LGRBs and SFR, by considering a different classification and seeing if it would change the results found in the literature.</p></sec></sec><sec id="s4"><title>4. Conclusion</title><p>In this paper, different models for the LGRB redshift distribution were studied. A complete data sample of Swift long GRBs with known redshifts was used without imposing any constraints. Our study shows that the SFRD can describe the LGRB redshift distribution for high redshift but needs an evolution term, to fit the distribution well, at low redshift. Although the data selected may have detection biases, primarily at low redshift, our results support the connection between long GRBs and stellar core-collapse. Our results indicate that the redshift distribution of the data sample fits the SFRD well at high redshifts. However, the issue of excess GRBs at low redshifts persists, because as far as our results go, they do not give us any indication about the nature of the extra contribution term ϕ ( z ) . To verify our results, future studies should consider data sets from other satellites or a combined data sample from more than one satellite with a focus on high redshift GRBs.</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>Hasan, A.M. and Azzam, W.J. (2024) Does the Redshift Distribution of Swift Long GRBs Trace the Star-Formation Rate? International Journal of Astronomy and Astrophysics, 14, 20-44. https://doi.org/10.4236/ijaa.2024.141002</p></sec><sec id="s7"><title>Appendix A. GRB Dataset</title><table-wrap id="table3" ><label><xref ref-type="table" rid="table">Table </xref>A1</label><caption><title> Shows the GRB dataset used</title></caption><table><tbody><thead><tr><th align="center" valign="middle" >GRB</th><th align="center" valign="middle" >T<sub>90</sub></th><th align="center" valign="middle" >Redshift</th></tr></thead><tr><td align="center" valign="middle" >230506C</td><td align="center" valign="middle" >31.00</td><td align="center" valign="middle" >3.7</td></tr><tr><td align="center" valign="middle" >230414B</td><td align="center" valign="middle" >25.98</td><td align="center" valign="middle" >3.568</td></tr><tr><td align="center" valign="middle" >230116D</td><td align="center" valign="middle" >41.00</td><td align="center" valign="middle" >3.81</td></tr><tr><td align="center" valign="middle" >221226B</td><td align="center" valign="middle" >3.44</td><td align="center" valign="middle" >2.694</td></tr><tr><td align="center" valign="middle" >221110A</td><td align="center" valign="middle" >8.98</td><td align="center" valign="middle" >4.06</td></tr><tr><td align="center" valign="middle" >221009A</td><td align="center" valign="middle" >1068.40</td><td align="center" valign="middle" >0.1505</td></tr><tr><td align="center" valign="middle" >220611A</td><td align="center" valign="middle" >57.00</td><td align="center" valign="middle" >2.3608</td></tr><tr><td align="center" valign="middle" >220521A</td><td align="center" valign="middle" >13.55</td><td align="center" valign="middle" >5.6</td></tr><tr><td align="center" valign="middle" >220117A</td><td align="center" valign="middle" >49.81</td><td align="center" valign="middle" >4.961</td></tr><tr><td align="center" valign="middle" >220101A</td><td align="center" valign="middle" >173.36</td><td align="center" valign="middle" >4.61</td></tr><tr><td align="center" valign="middle" >211207A</td><td align="center" valign="middle" >3.73</td><td align="center" valign="middle" >2.272</td></tr><tr><td align="center" valign="middle" >211024B</td><td align="center" valign="middle" >603.5</td><td align="center" valign="middle" >1.1137</td></tr><tr><td align="center" valign="middle" >10822A</td><td align="center" valign="middle" >180.8</td><td align="center" valign="middle" >1.736</td></tr><tr><td align="center" valign="middle" >210731A</td><td align="center" valign="middle" >22.51</td><td align="center" valign="middle" >1.2525</td></tr><tr><td align="center" valign="middle" >210722A</td><td align="center" valign="middle" >50.20</td><td align="center" valign="middle" >1.145</td></tr><tr><td align="center" valign="middle" >210702A</td><td align="center" valign="middle" >138.2</td><td align="center" valign="middle" >1.1757</td></tr><tr><td align="center" valign="middle" >210619B</td><td align="center" valign="middle" >60.90</td><td align="center" valign="middle" >1.937</td></tr><tr><td align="center" valign="middle" >210610B</td><td align="center" valign="middle" >69.38</td><td align="center" valign="middle" >1.13</td></tr><tr><td align="center" valign="middle" >210610A</td><td align="center" valign="middle" >13.62</td><td align="center" valign="middle" >3.54</td></tr><tr><td align="center" valign="middle" >210517A</td><td align="center" valign="middle" >3.06</td><td align="center" valign="middle" >2.486</td></tr><tr><td align="center" valign="middle" >210504A</td><td align="center" valign="middle" >135.06</td><td align="center" valign="middle" >2.077</td></tr><tr><td align="center" valign="middle" >210420B</td><td align="center" valign="middle" >158.8</td><td align="center" valign="middle" >1.400</td></tr><tr><td align="center" valign="middle" >210411C</td><td align="center" valign="middle" >12.80</td><td align="center" valign="middle" >2.826</td></tr><tr><td align="center" valign="middle" >210321A</td><td align="center" valign="middle" >8.21</td><td align="center" valign="middle" >1.487</td></tr><tr><td align="center" valign="middle" >210222B</td><td align="center" valign="middle" >12.82</td><td align="center" valign="middle" >2.198</td></tr><tr><td align="center" valign="middle" >210210A</td><td align="center" valign="middle" >6.60</td><td align="center" valign="middle" >0.715</td></tr><tr><td align="center" valign="middle" >201221A</td><td align="center" valign="middle" >44.5</td><td align="center" valign="middle" >5.70</td></tr><tr><td align="center" valign="middle" >201216C</td><td align="center" valign="middle" >48.0</td><td align="center" valign="middle" >1.10</td></tr><tr><td align="center" valign="middle" >201104B</td><td align="center" valign="middle" >8.66</td><td align="center" valign="middle" >1.954</td></tr><tr><td align="center" valign="middle" >201024A</td><td align="center" valign="middle" >5.00</td><td align="center" valign="middle" >0.999</td></tr><tr><td align="center" valign="middle" >201021C</td><td align="center" valign="middle" >24.38</td><td align="center" valign="middle" >1.070</td></tr><tr><td align="center" valign="middle" >201020A</td><td align="center" valign="middle" >14.17</td><td align="center" valign="middle" >2.903</td></tr><tr><td align="center" valign="middle" >201015A</td><td align="center" valign="middle" >9.78</td><td align="center" valign="middle" >0.423</td></tr><tr><td align="center" valign="middle" >201014A</td><td align="center" valign="middle" >36.2</td><td align="center" valign="middle" >4.56</td></tr><tr><td align="center" valign="middle" >200829A</td><td align="center" valign="middle" >13.04</td><td align="center" valign="middle" >1.25</td></tr><tr><td align="center" valign="middle" >200205B</td><td align="center" valign="middle" >458.0</td><td align="center" valign="middle" >1.465</td></tr><tr><td align="center" valign="middle" >191221B</td><td align="center" valign="middle" >48.00</td><td align="center" valign="middle" >1.148</td></tr><tr><td align="center" valign="middle" >191019A</td><td align="center" valign="middle" >64.35</td><td align="center" valign="middle" >0.248</td></tr><tr><td align="center" valign="middle" >191011A</td><td align="center" valign="middle" >7.37</td><td align="center" valign="middle" >1.722</td></tr><tr><td align="center" valign="middle" >191004B</td><td align="center" valign="middle" >37.7</td><td align="center" valign="middle" >3.503</td></tr><tr><td align="center" valign="middle" >190829A</td><td align="center" valign="middle" >58.2</td><td align="center" valign="middle" >0.0785</td></tr><tr><td align="center" valign="middle" >190719C</td><td align="center" valign="middle" >185.7</td><td align="center" valign="middle" >2.469</td></tr><tr><td align="center" valign="middle" >190324A</td><td align="center" valign="middle" >28.4</td><td align="center" valign="middle" >1.1715</td></tr><tr><td align="center" valign="middle" >190114C</td><td align="center" valign="middle" >361.5</td><td align="center" valign="middle" >0.42</td></tr><tr><td align="center" valign="middle" >190114A</td><td align="center" valign="middle" >66.6</td><td align="center" valign="middle" >3.3765</td></tr><tr><td align="center" valign="middle" >190106A</td><td align="center" valign="middle" >76.8</td><td align="center" valign="middle" >1.86</td></tr><tr><td align="center" valign="middle" >181110A</td><td align="center" valign="middle" >138.4</td><td align="center" valign="middle" >1.505</td></tr><tr><td align="center" valign="middle" >181020A</td><td align="center" valign="middle" >238.0</td><td align="center" valign="middle" >2.938</td></tr><tr><td align="center" valign="middle" >181010A</td><td align="center" valign="middle" >16.4</td><td align="center" valign="middle" >1.39</td></tr><tr><td align="center" valign="middle" >180728A</td><td align="center" valign="middle" >8.68</td><td align="center" valign="middle" >0.117</td></tr><tr><td align="center" valign="middle" >180624A</td><td align="center" valign="middle" >486.4</td><td align="center" valign="middle" >2.855</td></tr><tr><td align="center" valign="middle" >180620B</td><td align="center" valign="middle" >198.8</td><td align="center" valign="middle" >1.1175</td></tr><tr><td align="center" valign="middle" >180510B</td><td align="center" valign="middle" >134.3</td><td align="center" valign="middle" >1.305</td></tr><tr><td align="center" valign="middle" >180404A</td><td align="center" valign="middle" >35.2</td><td align="center" valign="middle" >1.000</td></tr><tr><td align="center" valign="middle" >180329B</td><td align="center" valign="middle" >210.0</td><td align="center" valign="middle" >1.998</td></tr><tr><td align="center" valign="middle" >180325A</td><td align="center" valign="middle" >94.1</td><td align="center" valign="middle" >2.25</td></tr><tr><td align="center" valign="middle" >180314A</td><td align="center" valign="middle" >51.2</td><td align="center" valign="middle" >1.445</td></tr><tr><td align="center" valign="middle" >180205A</td><td align="center" valign="middle" >15.5</td><td align="center" valign="middle" >1.409</td></tr><tr><td align="center" valign="middle" >180115A</td><td align="center" valign="middle" >40.9</td><td align="center" valign="middle" >2.487</td></tr><tr><td align="center" valign="middle" >171222A</td><td align="center" valign="middle" >174.8</td><td align="center" valign="middle" >2.409</td></tr><tr><td align="center" valign="middle" >171205A</td><td align="center" valign="middle" >189.4</td><td align="center" valign="middle" >0.0368</td></tr><tr><td align="center" valign="middle" >171020A</td><td align="center" valign="middle" >41.9</td><td align="center" valign="middle" >1.87</td></tr><tr><td align="center" valign="middle" >170903A</td><td align="center" valign="middle" >29.2</td><td align="center" valign="middle" >0.886</td></tr><tr><td align="center" valign="middle" >170705A</td><td align="center" valign="middle" >217.3</td><td align="center" valign="middle" >2.010</td></tr><tr><td align="center" valign="middle" >170604A</td><td align="center" valign="middle" >26.70</td><td align="center" valign="middle" >1.329</td></tr><tr><td align="center" valign="middle" >170531B</td><td align="center" valign="middle" >164.13</td><td align="center" valign="middle" >2.366</td></tr><tr><td align="center" valign="middle" >170519A</td><td align="center" valign="middle" >216.4</td><td align="center" valign="middle" >0.818</td></tr><tr><td align="center" valign="middle" >170405A</td><td align="center" valign="middle" >164.7</td><td align="center" valign="middle" >3.510</td></tr><tr><td align="center" valign="middle" >170202A</td><td align="center" valign="middle" >46.2</td><td align="center" valign="middle" >3.645</td></tr><tr><td align="center" valign="middle" >170113A</td><td align="center" valign="middle" >20.66</td><td align="center" valign="middle" >1.968</td></tr><tr><td align="center" valign="middle" >161219B</td><td align="center" valign="middle" >6.94</td><td align="center" valign="middle" >0.1475</td></tr><tr><td align="center" valign="middle" >161129A</td><td align="center" valign="middle" >35.53</td><td align="center" valign="middle" >0.645</td></tr><tr><td align="center" valign="middle" >161117A</td><td align="center" valign="middle" >125.7</td><td align="center" valign="middle" >1.549</td></tr><tr><td align="center" valign="middle" >161108A</td><td align="center" valign="middle" >105.1</td><td align="center" valign="middle" >1.159</td></tr><tr><td align="center" valign="middle" >161017A</td><td align="center" valign="middle" >216.3</td><td align="center" valign="middle" >2.0127</td></tr><tr><td align="center" valign="middle" >161014A</td><td align="center" valign="middle" >18.3</td><td align="center" valign="middle" >2.823</td></tr><tr><td align="center" valign="middle" >160804A</td><td align="center" valign="middle" >144.2</td><td align="center" valign="middle" >0.736</td></tr><tr><td align="center" valign="middle" >160425A</td><td align="center" valign="middle" >304.58</td><td align="center" valign="middle" >0.555</td></tr><tr><td align="center" valign="middle" >160410A</td><td align="center" valign="middle" >8.2</td><td align="center" valign="middle" >1.717</td></tr><tr><td align="center" valign="middle" >160327A</td><td align="center" valign="middle" >28</td><td align="center" valign="middle" >4.99</td></tr><tr><td align="center" valign="middle" >160314A</td><td align="center" valign="middle" >8.73</td><td align="center" valign="middle" >0.726</td></tr><tr><td align="center" valign="middle" >160227A</td><td align="center" valign="middle" >316.5</td><td align="center" valign="middle" >2.38</td></tr><tr><td align="center" valign="middle" >160203A</td><td align="center" valign="middle" >20.2</td><td align="center" valign="middle" >3.52</td></tr><tr><td align="center" valign="middle" >160131A</td><td align="center" valign="middle" >325</td><td align="center" valign="middle" >0.97</td></tr><tr><td align="center" valign="middle" >160121A</td><td align="center" valign="middle" >12.0</td><td align="center" valign="middle" >1.960</td></tr><tr><td align="center" valign="middle" >151215A</td><td align="center" valign="middle" >17.8</td><td align="center" valign="middle" >2.59</td></tr><tr><td align="center" valign="middle" >151112A</td><td align="center" valign="middle" >19.32</td><td align="center" valign="middle" >4.1</td></tr><tr><td align="center" valign="middle" >151111A</td><td align="center" valign="middle" >76.93</td><td align="center" valign="middle" >3.5</td></tr><tr><td align="center" valign="middle" >151031A</td><td align="center" valign="middle" >5.00</td><td align="center" valign="middle" >1.167</td></tr><tr><td align="center" valign="middle" >151029A</td><td align="center" valign="middle" >8.95</td><td align="center" valign="middle" >1.423</td></tr><tr><td align="center" valign="middle" >151027B</td><td align="center" valign="middle" >80.00</td><td align="center" valign="middle" >4.063</td></tr><tr><td align="center" valign="middle" >151027A</td><td align="center" valign="middle" >129.69</td><td align="center" valign="middle" >0.81</td></tr><tr><td align="center" valign="middle" >151021A</td><td align="center" valign="middle" >110.2</td><td align="center" valign="middle" >2.330</td></tr><tr><td align="center" valign="middle" >150915A</td><td align="center" valign="middle" >164.7</td><td align="center" valign="middle" >1.968</td></tr><tr><td align="center" valign="middle" >150910A</td><td align="center" valign="middle" >112.2</td><td align="center" valign="middle" >1.359</td></tr><tr><td align="center" valign="middle" >150821A</td><td align="center" valign="middle" >172.1</td><td align="center" valign="middle" >0.755</td></tr><tr><td align="center" valign="middle" >150818A</td><td align="center" valign="middle" >123.3</td><td align="center" valign="middle" >0.282</td></tr><tr><td align="center" valign="middle" >150727A</td><td align="center" valign="middle" >88</td><td align="center" valign="middle" >0.313</td></tr><tr><td align="center" valign="middle" >150413A</td><td align="center" valign="middle" >263.6</td><td align="center" valign="middle" >3.2</td></tr><tr><td align="center" valign="middle" >150403A</td><td align="center" valign="middle" >40.90</td><td align="center" valign="middle" >2.06</td></tr><tr><td align="center" valign="middle" >150323A</td><td align="center" valign="middle" >149.6</td><td align="center" valign="middle" >0.593</td></tr><tr><td align="center" valign="middle" >150314A</td><td align="center" valign="middle" >14.79</td><td align="center" valign="middle" >1.758</td></tr><tr><td align="center" valign="middle" >150301B</td><td align="center" valign="middle" >12.44</td><td align="center" valign="middle" >1.5169</td></tr><tr><td align="center" valign="middle" >150206A</td><td align="center" valign="middle" >83.2</td><td align="center" valign="middle" >2.087</td></tr><tr><td align="center" valign="middle" >141225A</td><td align="center" valign="middle" >40.24</td><td align="center" valign="middle" >0.915</td></tr><tr><td align="center" valign="middle" >141221A</td><td align="center" valign="middle" >36.9</td><td align="center" valign="middle" >1.452</td></tr><tr><td align="center" valign="middle" >141220A</td><td align="center" valign="middle" >7.21</td><td align="center" valign="middle" >1.3195</td></tr><tr><td align="center" valign="middle" >141121A</td><td align="center" valign="middle" >549.9</td><td align="center" valign="middle" >1.47</td></tr><tr><td align="center" valign="middle" >141109A</td><td align="center" valign="middle" >200</td><td align="center" valign="middle" >2.993</td></tr><tr><td align="center" valign="middle" >141026A</td><td align="center" valign="middle" >146</td><td align="center" valign="middle" >3.35</td></tr><tr><td align="center" valign="middle" >141004A</td><td align="center" valign="middle" >3.92</td><td align="center" valign="middle" >0.573</td></tr><tr><td align="center" valign="middle" >140907A</td><td align="center" valign="middle" >79.2</td><td align="center" valign="middle" >1.21</td></tr><tr><td align="center" valign="middle" >140710A</td><td align="center" valign="middle" >3.52</td><td align="center" valign="middle" >0.558</td></tr><tr><td align="center" valign="middle" >140703A</td><td align="center" valign="middle" >67.1</td><td align="center" valign="middle" >3.14</td></tr><tr><td align="center" valign="middle" >140629A</td><td align="center" valign="middle" >42.0</td><td align="center" valign="middle" >2.275</td></tr><tr><td align="center" valign="middle" >140614A</td><td align="center" valign="middle" >720</td><td align="center" valign="middle" >4.233</td></tr><tr><td align="center" valign="middle" >140518A</td><td align="center" valign="middle" >60.5</td><td align="center" valign="middle" >4.707</td></tr><tr><td align="center" valign="middle" >140515A</td><td align="center" valign="middle" >23.4</td><td align="center" valign="middle" >6.32</td></tr><tr><td align="center" valign="middle" >140512A</td><td align="center" valign="middle" >154.8</td><td align="center" valign="middle" >0.725</td></tr><tr><td align="center" valign="middle" >140506A</td><td align="center" valign="middle" >111.1</td><td align="center" valign="middle" >0.889</td></tr><tr><td align="center" valign="middle" >140430A</td><td align="center" valign="middle" >173.6</td><td align="center" valign="middle" >1.60</td></tr><tr><td align="center" valign="middle" >140428A</td><td align="center" valign="middle" >17.42</td><td align="center" valign="middle" >4.7</td></tr><tr><td align="center" valign="middle" >140423A</td><td align="center" valign="middle" >134</td><td align="center" valign="middle" >3.26</td></tr><tr><td align="center" valign="middle" >140419A</td><td align="center" valign="middle" >94.7</td><td align="center" valign="middle" >3.956</td></tr><tr><td align="center" valign="middle" >140318A</td><td align="center" valign="middle" >8.43</td><td align="center" valign="middle" >1.02</td></tr><tr><td align="center" valign="middle" >140311A</td><td align="center" valign="middle" >71.4</td><td align="center" valign="middle" >4.95</td></tr><tr><td align="center" valign="middle" >140304A</td><td align="center" valign="middle" >15.6</td><td align="center" valign="middle" >5.283</td></tr><tr><td align="center" valign="middle" >140301A</td><td align="center" valign="middle" >31.0</td><td align="center" valign="middle" >1.416</td></tr><tr><td align="center" valign="middle" >140213A</td><td align="center" valign="middle" >60.0</td><td align="center" valign="middle" >1.2076</td></tr><tr><td align="center" valign="middle" >140206A</td><td align="center" valign="middle" >93.6</td><td align="center" valign="middle" >2.73</td></tr><tr><td align="center" valign="middle" >140114A</td><td align="center" valign="middle" >139.7</td><td align="center" valign="middle" >3.0</td></tr><tr><td align="center" valign="middle" >131227A</td><td align="center" valign="middle" >18.0</td><td align="center" valign="middle" >5.3</td></tr><tr><td align="center" valign="middle" >131117A</td><td align="center" valign="middle" >11.00</td><td align="center" valign="middle" >4.042</td></tr><tr><td align="center" valign="middle" >131105A</td><td align="center" valign="middle" >112.3</td><td align="center" valign="middle" >1.686</td></tr><tr><td align="center" valign="middle" >131103A</td><td align="center" valign="middle" >17.3</td><td align="center" valign="middle" >0.599</td></tr><tr><td align="center" valign="middle" >131030A</td><td align="center" valign="middle" >41.1</td><td align="center" valign="middle" >1.293</td></tr><tr><td align="center" valign="middle" >130907A</td><td align="center" valign="middle" >&gt;360</td><td align="center" valign="middle" >1.238</td></tr><tr><td align="center" valign="middle" >130831A</td><td align="center" valign="middle" >32.5</td><td align="center" valign="middle" >0.4791</td></tr><tr><td align="center" valign="middle" >130701A</td><td align="center" valign="middle" >4.38</td><td align="center" valign="middle" >1.155</td></tr><tr><td align="center" valign="middle" >130612A</td><td align="center" valign="middle" >4.0</td><td align="center" valign="middle" >2.006</td></tr><tr><td align="center" valign="middle" >130610A</td><td align="center" valign="middle" >46.4</td><td align="center" valign="middle" >2.092</td></tr><tr><td align="center" valign="middle" >130606A</td><td align="center" valign="middle" >276.58</td><td align="center" valign="middle" >5.913</td></tr><tr><td align="center" valign="middle" >130604A</td><td align="center" valign="middle" >37.7</td><td align="center" valign="middle" >1.06</td></tr><tr><td align="center" valign="middle" >130514A</td><td align="center" valign="middle" >204</td><td align="center" valign="middle" >3.6</td></tr><tr><td align="center" valign="middle" >130511A</td><td align="center" valign="middle" >5.43</td><td align="center" valign="middle" >1.3033</td></tr><tr><td align="center" valign="middle" >130505A</td><td align="center" valign="middle" >88</td><td align="center" valign="middle" >2.27</td></tr><tr><td align="center" valign="middle" >130427B</td><td align="center" valign="middle" >27.0</td><td align="center" valign="middle" >2.78</td></tr><tr><td align="center" valign="middle" >130427A</td><td align="center" valign="middle" >162.83</td><td align="center" valign="middle" >0.34</td></tr><tr><td align="center" valign="middle" >130420A</td><td align="center" valign="middle" >123.5</td><td align="center" valign="middle" >1.297</td></tr><tr><td align="center" valign="middle" >130418A</td><td align="center" valign="middle" >&gt;300</td><td align="center" valign="middle" >1.218</td></tr><tr><td align="center" valign="middle" >130408A</td><td align="center" valign="middle" >28</td><td align="center" valign="middle" >3.758</td></tr><tr><td align="center" valign="middle" >130215A</td><td align="center" valign="middle" >65.7</td><td align="center" valign="middle" >0.597</td></tr><tr><td align="center" valign="middle" >130131B</td><td align="center" valign="middle" >4.30</td><td align="center" valign="middle" >2.539</td></tr><tr><td align="center" valign="middle" >121211A</td><td align="center" valign="middle" >182</td><td align="center" valign="middle" >1.023</td></tr><tr><td align="center" valign="middle" >121201A</td><td align="center" valign="middle" >85</td><td align="center" valign="middle" >3.385</td></tr><tr><td align="center" valign="middle" >121128A</td><td align="center" valign="middle" >23.3</td><td align="center" valign="middle" >2.20</td></tr><tr><td align="center" valign="middle" >121027A</td><td align="center" valign="middle" >62.6</td><td align="center" valign="middle" >1.773</td></tr><tr><td align="center" valign="middle" >121024A</td><td align="center" valign="middle" >69</td><td align="center" valign="middle" >2.298</td></tr><tr><td align="center" valign="middle" >120922A</td><td align="center" valign="middle" >173</td><td align="center" valign="middle" >3.1</td></tr><tr><td align="center" valign="middle" >120907A</td><td align="center" valign="middle" >16.9</td><td align="center" valign="middle" >0.970</td></tr><tr><td align="center" valign="middle" >120815A</td><td align="center" valign="middle" >9.7</td><td align="center" valign="middle" >2.358</td></tr><tr><td align="center" valign="middle" >120811C</td><td align="center" valign="middle" >26.8</td><td align="center" valign="middle" >2.671</td></tr><tr><td align="center" valign="middle" >120805A</td><td align="center" valign="middle" >48.00</td><td align="center" valign="middle" >3.1</td></tr><tr><td align="center" valign="middle" >120802A</td><td align="center" valign="middle" >50</td><td align="center" valign="middle" >3.796</td></tr><tr><td align="center" valign="middle" >120729A</td><td align="center" valign="middle" >71.5</td><td align="center" valign="middle" >0.80</td></tr><tr><td align="center" valign="middle" >120724A</td><td align="center" valign="middle" >72.8</td><td align="center" valign="middle" >1.48</td></tr><tr><td align="center" valign="middle" >120722A</td><td align="center" valign="middle" >42.4</td><td align="center" valign="middle" >0.9586</td></tr><tr><td align="center" valign="middle" >120714B</td><td align="center" valign="middle" >159</td><td align="center" valign="middle" >0.3984</td></tr><tr><td align="center" valign="middle" >120712A</td><td align="center" valign="middle" >14.7</td><td align="center" valign="middle" >4.1745</td></tr><tr><td align="center" valign="middle" >120521C</td><td align="center" valign="middle" >26.7</td><td align="center" valign="middle" >6.0</td></tr><tr><td align="center" valign="middle" >120422A</td><td align="center" valign="middle" >5.35</td><td align="center" valign="middle" >0.28</td></tr><tr><td align="center" valign="middle" >120404A</td><td align="center" valign="middle" >38.7</td><td align="center" valign="middle" >2.876</td></tr><tr><td align="center" valign="middle" >120327A</td><td align="center" valign="middle" >62.9</td><td align="center" valign="middle" >2.81</td></tr><tr><td align="center" valign="middle" >120326A</td><td align="center" valign="middle" >69.6</td><td align="center" valign="middle" >1.798</td></tr><tr><td align="center" valign="middle" >120119A</td><td align="center" valign="middle" >253.8</td><td align="center" valign="middle" >1.728</td></tr><tr><td align="center" valign="middle" >120118B</td><td align="center" valign="middle" >23.26</td><td align="center" valign="middle" >2.943</td></tr><tr><td align="center" valign="middle" >111229A</td><td align="center" valign="middle" >25.4</td><td align="center" valign="middle" >1.3805</td></tr><tr><td align="center" valign="middle" >111228A</td><td align="center" valign="middle" >101.20</td><td align="center" valign="middle" >0.714</td></tr><tr><td align="center" valign="middle" >111225A</td><td align="center" valign="middle" >106.8</td><td align="center" valign="middle" >0.297</td></tr><tr><td align="center" valign="middle" >111123A</td><td align="center" valign="middle" >290.0</td><td align="center" valign="middle" >3.1516</td></tr><tr><td align="center" valign="middle" >111107A</td><td align="center" valign="middle" >26.6</td><td align="center" valign="middle" >2.893</td></tr><tr><td align="center" valign="middle" >111008A</td><td align="center" valign="middle" >63.46</td><td align="center" valign="middle" >4.9898</td></tr><tr><td align="center" valign="middle" >110818A</td><td align="center" valign="middle" >103</td><td align="center" valign="middle" >3.36</td></tr><tr><td align="center" valign="middle" >110808A</td><td align="center" valign="middle" >48</td><td align="center" valign="middle" >1.348</td></tr><tr><td align="center" valign="middle" >110801A</td><td align="center" valign="middle" >385</td><td align="center" valign="middle" >1.858</td></tr><tr><td align="center" valign="middle" >110731A</td><td align="center" valign="middle" >38.8</td><td align="center" valign="middle" >2.83</td></tr><tr><td align="center" valign="middle" >110715A</td><td align="center" valign="middle" >13.0</td><td align="center" valign="middle" >0.82</td></tr><tr><td align="center" valign="middle" >110503A</td><td align="center" valign="middle" >10.0</td><td align="center" valign="middle" >1.613</td></tr><tr><td align="center" valign="middle" >110422A</td><td align="center" valign="middle" >25.9</td><td align="center" valign="middle" >1.77</td></tr><tr><td align="center" valign="middle" >110213A</td><td align="center" valign="middle" >48.0</td><td align="center" valign="middle" >1.46</td></tr><tr><td align="center" valign="middle" >110205A</td><td align="center" valign="middle" >257</td><td align="center" valign="middle" >2.22</td></tr><tr><td align="center" valign="middle" >110128A</td><td align="center" valign="middle" >30.7</td><td align="center" valign="middle" >2.339</td></tr><tr><td align="center" valign="middle" >101225A</td><td align="center" valign="middle" >1088.0</td><td align="center" valign="middle" >0.847</td></tr><tr><td align="center" valign="middle" >101219B</td><td align="center" valign="middle" >34</td><td align="center" valign="middle" >0.5519</td></tr><tr><td align="center" valign="middle" >100906A</td><td align="center" valign="middle" >114.4</td><td align="center" valign="middle" >1.727</td></tr><tr><td align="center" valign="middle" >100902A</td><td align="center" valign="middle" >428.8</td><td align="center" valign="middle" >4.5</td></tr><tr><td align="center" valign="middle" >100901A</td><td align="center" valign="middle" >439</td><td align="center" valign="middle" >1.408</td></tr><tr><td align="center" valign="middle" >100816A</td><td align="center" valign="middle" >2.9</td><td align="center" valign="middle" >0.8034</td></tr><tr><td align="center" valign="middle" >100814A</td><td align="center" valign="middle" >174.5</td><td align="center" valign="middle" >1.44</td></tr><tr><td align="center" valign="middle" >100728B</td><td align="center" valign="middle" >12.1</td><td align="center" valign="middle" >2.106</td></tr><tr><td align="center" valign="middle" >100728A</td><td align="center" valign="middle" >198.5</td><td align="center" valign="middle" >1.567</td></tr><tr><td align="center" valign="middle" >100704A</td><td align="center" valign="middle" >197.5</td><td align="center" valign="middle" >3.6</td></tr><tr><td align="center" valign="middle" >100621A</td><td align="center" valign="middle" >63.6</td><td align="center" valign="middle" >0.542</td></tr><tr><td align="center" valign="middle" >100615A</td><td align="center" valign="middle" >39</td><td align="center" valign="middle" >1.398</td></tr><tr><td align="center" valign="middle" >100513A</td><td align="center" valign="middle" >84</td><td align="center" valign="middle" >4.772</td></tr><tr><td align="center" valign="middle" >100425A</td><td align="center" valign="middle" >37.0</td><td align="center" valign="middle" >1.755</td></tr><tr><td align="center" valign="middle" >100424A</td><td align="center" valign="middle" >104</td><td align="center" valign="middle" >2.465</td></tr><tr><td align="center" valign="middle" >100418A</td><td align="center" valign="middle" >7.0</td><td align="center" valign="middle" >0.6235</td></tr><tr><td align="center" valign="middle" >100413A</td><td align="center" valign="middle" >191</td><td align="center" valign="middle" >3.9</td></tr><tr><td align="center" valign="middle" >100316B</td><td align="center" valign="middle" >3.8</td><td align="center" valign="middle" >1.180</td></tr><tr><td align="center" valign="middle" >100302A</td><td align="center" valign="middle" >17.9</td><td align="center" valign="middle" >4.813</td></tr><tr><td align="center" valign="middle" >100219A</td><td align="center" valign="middle" >18.8</td><td align="center" valign="middle" >4.5</td></tr><tr><td align="center" valign="middle" >091208B</td><td align="center" valign="middle" >14.9</td><td align="center" valign="middle" >1.063</td></tr><tr><td align="center" valign="middle" >091127</td><td align="center" valign="middle" >7.1</td><td align="center" valign="middle" >0.490</td></tr><tr><td align="center" valign="middle" >091109A</td><td align="center" valign="middle" >48</td><td align="center" valign="middle" >3.076</td></tr><tr><td align="center" valign="middle" >091029</td><td align="center" valign="middle" >39.2</td><td align="center" valign="middle" >2.752</td></tr><tr><td align="center" valign="middle" >091024</td><td align="center" valign="middle" >109.8</td><td align="center" valign="middle" >1.092</td></tr><tr><td align="center" valign="middle" >091020</td><td align="center" valign="middle" >34.6</td><td align="center" valign="middle" >1.71</td></tr><tr><td align="center" valign="middle" >091018</td><td align="center" valign="middle" >4.4</td><td align="center" valign="middle" >0.971</td></tr><tr><td align="center" valign="middle" >090927</td><td align="center" valign="middle" >2.2</td><td align="center" valign="middle" >1.37</td></tr><tr><td align="center" valign="middle" >090926B</td><td align="center" valign="middle" >109.7</td><td align="center" valign="middle" >1.24</td></tr><tr><td align="center" valign="middle" >090812</td><td align="center" valign="middle" >66.7</td><td align="center" valign="middle" >2.452</td></tr><tr><td align="center" valign="middle" >090809</td><td align="center" valign="middle" >5.4</td><td align="center" valign="middle" >2.737</td></tr><tr><td align="center" valign="middle" >090726</td><td align="center" valign="middle" >67.0</td><td align="center" valign="middle" >2.71</td></tr><tr><td align="center" valign="middle" >090715B</td><td align="center" valign="middle" >266</td><td align="center" valign="middle" >3.00</td></tr><tr><td align="center" valign="middle" >090618</td><td align="center" valign="middle" >113.2</td><td align="center" valign="middle" >0.54</td></tr><tr><td align="center" valign="middle" >090530</td><td align="center" valign="middle" >48</td><td align="center" valign="middle" >1.266</td></tr><tr><td align="center" valign="middle" >090529</td><td align="center" valign="middle" >&gt;100</td><td align="center" valign="middle" >2.625</td></tr><tr><td align="center" valign="middle" >090519</td><td align="center" valign="middle" >64</td><td align="center" valign="middle" >3.9</td></tr><tr><td align="center" valign="middle" >090516A</td><td align="center" valign="middle" >210</td><td align="center" valign="middle" >4.109</td></tr><tr><td align="center" valign="middle" >090424</td><td align="center" valign="middle" >48</td><td align="center" valign="middle" >0.544</td></tr><tr><td align="center" valign="middle" >090423</td><td align="center" valign="middle" >10.3</td><td align="center" valign="middle" >8.0</td></tr><tr><td align="center" valign="middle" >090418A</td><td align="center" valign="middle" >56</td><td align="center" valign="middle" >1.608</td></tr><tr><td align="center" valign="middle" >090407</td><td align="center" valign="middle" >310</td><td align="center" valign="middle" >1.4485</td></tr><tr><td align="center" valign="middle" >090313</td><td align="center" valign="middle" >79</td><td align="center" valign="middle" >3.375</td></tr><tr><td align="center" valign="middle" >090205</td><td align="center" valign="middle" >8.8</td><td align="center" valign="middle" >4.7</td></tr><tr><td align="center" valign="middle" >090113</td><td align="center" valign="middle" >9.1</td><td align="center" valign="middle" >1.7493</td></tr><tr><td align="center" valign="middle" >090102</td><td align="center" valign="middle" >27.0</td><td align="center" valign="middle" >1.547</td></tr><tr><td align="center" valign="middle" >081222</td><td align="center" valign="middle" >24</td><td align="center" valign="middle" >2.77</td></tr><tr><td align="center" valign="middle" >081221</td><td align="center" valign="middle" >34</td><td align="center" valign="middle" >2.26</td></tr><tr><td align="center" valign="middle" >081203A</td><td align="center" valign="middle" >294</td><td align="center" valign="middle" >2.1</td></tr><tr><td align="center" valign="middle" >081121</td><td align="center" valign="middle" >14</td><td align="center" valign="middle" >2.512</td></tr><tr><td align="center" valign="middle" >081118</td><td align="center" valign="middle" >67</td><td align="center" valign="middle" >2.58</td></tr><tr><td align="center" valign="middle" >081029</td><td align="center" valign="middle" >270</td><td align="center" valign="middle" >3.8479</td></tr><tr><td align="center" valign="middle" >081028A</td><td align="center" valign="middle" >260</td><td align="center" valign="middle" >3.038</td></tr><tr><td align="center" valign="middle" >081008</td><td align="center" valign="middle" >185.5</td><td align="center" valign="middle" >1.9685</td></tr><tr><td align="center" valign="middle" >081007</td><td align="center" valign="middle" >10.0</td><td align="center" valign="middle" >0.5295</td></tr><tr><td align="center" valign="middle" >080928</td><td align="center" valign="middle" >280</td><td align="center" valign="middle" >1.692</td></tr><tr><td align="center" valign="middle" >080916A</td><td align="center" valign="middle" >60</td><td align="center" valign="middle" >0.689</td></tr><tr><td align="center" valign="middle" >080913</td><td align="center" valign="middle" >8</td><td align="center" valign="middle" >6.44</td></tr><tr><td align="center" valign="middle" >080906</td><td align="center" valign="middle" >147</td><td align="center" valign="middle" >2.0</td></tr><tr><td align="center" valign="middle" >080905B</td><td align="center" valign="middle" >128</td><td align="center" valign="middle" >2.374</td></tr><tr><td align="center" valign="middle" >080810</td><td align="center" valign="middle" >106</td><td align="center" valign="middle" >3.35</td></tr><tr><td align="center" valign="middle" >080805</td><td align="center" valign="middle" >78</td><td align="center" valign="middle" >1.505</td></tr><tr><td align="center" valign="middle" >080804</td><td align="center" valign="middle" >34</td><td align="center" valign="middle" >2.2045</td></tr><tr><td align="center" valign="middle" >080721</td><td align="center" valign="middle" >16.2</td><td align="center" valign="middle" >2.602</td></tr><tr><td align="center" valign="middle" >080710</td><td align="center" valign="middle" >120</td><td align="center" valign="middle" >0.845</td></tr><tr><td align="center" valign="middle" >080707</td><td align="center" valign="middle" >27.1</td><td align="center" valign="middle" >1.23</td></tr><tr><td align="center" valign="middle" >080607</td><td align="center" valign="middle" >79</td><td align="center" valign="middle" >3.036</td></tr><tr><td align="center" valign="middle" >080605</td><td align="center" valign="middle" >20</td><td align="center" valign="middle" >1.6398</td></tr><tr><td align="center" valign="middle" >080604</td><td align="center" valign="middle" >82</td><td align="center" valign="middle" >1.416</td></tr><tr><td align="center" valign="middle" >080603B</td><td align="center" valign="middle" >60</td><td align="center" valign="middle" >2.69</td></tr><tr><td align="center" valign="middle" >080520</td><td align="center" valign="middle" >2.8</td><td align="center" valign="middle" >1.545</td></tr><tr><td align="center" valign="middle" >080516</td><td align="center" valign="middle" >5.8</td><td align="center" valign="middle" >3.2</td></tr><tr><td align="center" valign="middle" >080430</td><td align="center" valign="middle" >16.2</td><td align="center" valign="middle" >0.767</td></tr><tr><td align="center" valign="middle" >080413B</td><td align="center" valign="middle" >8.0</td><td align="center" valign="middle" >1.10</td></tr><tr><td align="center" valign="middle" >080413A</td><td align="center" valign="middle" >46</td><td align="center" valign="middle" >2.433</td></tr><tr><td align="center" valign="middle" >080411</td><td align="center" valign="middle" >56</td><td align="center" valign="middle" >1.03</td></tr><tr><td align="center" valign="middle" >080330</td><td align="center" valign="middle" >61</td><td align="center" valign="middle" >1.51</td></tr><tr><td align="center" valign="middle" >080319C</td><td align="center" valign="middle" >34</td><td align="center" valign="middle" >1.95</td></tr><tr><td align="center" valign="middle" >080319B</td><td align="center" valign="middle" >&gt;50</td><td align="center" valign="middle" >0.937</td></tr><tr><td align="center" valign="middle" >080310</td><td align="center" valign="middle" >365</td><td align="center" valign="middle" >2.4266</td></tr><tr><td align="center" valign="middle" >080210</td><td align="center" valign="middle" >45</td><td align="center" valign="middle" >2.641</td></tr><tr><td align="center" valign="middle" >080207</td><td align="center" valign="middle" >340</td><td align="center" valign="middle" >2.0858</td></tr><tr><td align="center" valign="middle" >071122</td><td align="center" valign="middle" >68.7</td><td align="center" valign="middle" >1.14</td></tr><tr><td align="center" valign="middle" >071117</td><td align="center" valign="middle" >6.6</td><td align="center" valign="middle" >1.331</td></tr><tr><td align="center" valign="middle" >071112C</td><td align="center" valign="middle" >15</td><td align="center" valign="middle" >0.8230</td></tr><tr><td align="center" valign="middle" >071031</td><td align="center" valign="middle" >180</td><td align="center" valign="middle" >2.692</td></tr><tr><td align="center" valign="middle" >071028B</td><td align="center" valign="middle" >55</td><td align="center" valign="middle" >0.94</td></tr><tr><td align="center" valign="middle" >071021</td><td align="center" valign="middle" >225</td><td align="center" valign="middle" >2.4520</td></tr><tr><td align="center" valign="middle" >071020</td><td align="center" valign="middle" >4.2</td><td align="center" valign="middle" >2.142</td></tr><tr><td align="center" valign="middle" >071010B</td><td align="center" valign="middle" >&gt;35.7</td><td align="center" valign="middle" >0.947</td></tr><tr><td align="center" valign="middle" >071010A</td><td align="center" valign="middle" >6</td><td align="center" valign="middle" >0.98</td></tr><tr><td align="center" valign="middle" >071003</td><td align="center" valign="middle" >150</td><td align="center" valign="middle" >1.100</td></tr><tr><td align="center" valign="middle" >070810A</td><td align="center" valign="middle" >11.0</td><td align="center" valign="middle" >2.17</td></tr><tr><td align="center" valign="middle" >070802</td><td align="center" valign="middle" >16.4</td><td align="center" valign="middle" >2.45</td></tr><tr><td align="center" valign="middle" >070714B</td><td align="center" valign="middle" >64</td><td align="center" valign="middle" >0.92</td></tr><tr><td align="center" valign="middle" >070612A</td><td align="center" valign="middle" >368.800</td><td align="center" valign="middle" >0.617</td></tr><tr><td align="center" valign="middle" >070611</td><td align="center" valign="middle" >12.200</td><td align="center" valign="middle" >2.04</td></tr><tr><td align="center" valign="middle" >070529</td><td align="center" valign="middle" >109.200</td><td align="center" valign="middle" >2.4996</td></tr><tr><td align="center" valign="middle" >070521</td><td align="center" valign="middle" >37.900</td><td align="center" valign="middle" >0.553</td></tr><tr><td align="center" valign="middle" >070508</td><td align="center" valign="middle" >20.900</td><td align="center" valign="middle" >0.82</td></tr><tr><td align="center" valign="middle" >070506</td><td align="center" valign="middle" >4.300</td><td align="center" valign="middle" >2.31</td></tr><tr><td align="center" valign="middle" >070419A</td><td align="center" valign="middle" >115.600</td><td align="center" valign="middle" >0.97</td></tr><tr><td align="center" valign="middle" >070411</td><td align="center" valign="middle" >121.500</td><td align="center" valign="middle" >2.954</td></tr><tr><td align="center" valign="middle" >070318</td><td align="center" valign="middle" >74.600</td><td align="center" valign="middle" >0.836</td></tr><tr><td align="center" valign="middle" >070306</td><td align="center" valign="middle" >209.500</td><td align="center" valign="middle" >1.497</td></tr><tr><td align="center" valign="middle" >070208</td><td align="center" valign="middle" >47.700</td><td align="center" valign="middle" >1.165</td></tr><tr><td align="center" valign="middle" >070129</td><td align="center" valign="middle" >460.600</td><td align="center" valign="middle" >2.3384</td></tr><tr><td align="center" valign="middle" >070110</td><td align="center" valign="middle" >88.400</td><td align="center" valign="middle" >2.352</td></tr><tr><td align="center" valign="middle" >070103</td><td align="center" valign="middle" >18.600</td><td align="center" valign="middle" >2.6208</td></tr><tr><td align="center" valign="middle" >061222B</td><td align="center" valign="middle" >40.000</td><td align="center" valign="middle" >3.355</td></tr><tr><td align="center" valign="middle" >061222A</td><td align="center" valign="middle" >71.400</td><td align="center" valign="middle" >2.088</td></tr><tr><td align="center" valign="middle" >061210</td><td align="center" valign="middle" >85.300</td><td align="center" valign="middle" >0.41</td></tr><tr><td align="center" valign="middle" >061121</td><td align="center" valign="middle" >81.300</td><td align="center" valign="middle" >1.314</td></tr><tr><td align="center" valign="middle" >061110B</td><td align="center" valign="middle" >134.000</td><td align="center" valign="middle" >3.44</td></tr><tr><td align="center" valign="middle" >061110A</td><td align="center" valign="middle" >40.700</td><td align="center" valign="middle" >0.758</td></tr><tr><td align="center" valign="middle" >061021</td><td align="center" valign="middle" >46.200</td><td align="center" valign="middle" >0.3463</td></tr><tr><td align="center" valign="middle" >061007</td><td align="center" valign="middle" >75.300</td><td align="center" valign="middle" >1.261</td></tr><tr><td align="center" valign="middle" >060927</td><td align="center" valign="middle" >22.500</td><td align="center" valign="middle" >5.6</td></tr><tr><td align="center" valign="middle" >060926</td><td align="center" valign="middle" >8.000</td><td align="center" valign="middle" >3.208</td></tr><tr><td align="center" valign="middle" >060912A</td><td align="center" valign="middle" >5.000</td><td align="center" valign="middle" >0.937</td></tr><tr><td align="center" valign="middle" >060908</td><td align="center" valign="middle" >19.300</td><td align="center" valign="middle" >1.8836</td></tr><tr><td align="center" valign="middle" >060906</td><td align="center" valign="middle" >43.500</td><td align="center" valign="middle" >3.685</td></tr><tr><td align="center" valign="middle" >060904B</td><td align="center" valign="middle" >171.500</td><td align="center" valign="middle" >0.703</td></tr><tr><td align="center" valign="middle" >060814</td><td align="center" valign="middle" >145.300</td><td align="center" valign="middle" >0.84</td></tr><tr><td align="center" valign="middle" >060729</td><td align="center" valign="middle" >115.300</td><td align="center" valign="middle" >0.54</td></tr><tr><td align="center" valign="middle" >060719</td><td align="center" valign="middle" >66.900</td><td align="center" valign="middle" >1.5320</td></tr><tr><td align="center" valign="middle" >060714</td><td align="center" valign="middle" >115.000</td><td align="center" valign="middle" >2.71</td></tr><tr><td align="center" valign="middle" >060707</td><td align="center" valign="middle" >66.200</td><td align="center" valign="middle" >3.43</td></tr><tr><td align="center" valign="middle" >060614</td><td align="center" valign="middle" >108.700</td><td align="center" valign="middle" >0.125</td></tr><tr><td align="center" valign="middle" >060607A</td><td align="center" valign="middle" >102.200</td><td align="center" valign="middle" >3.082</td></tr><tr><td align="center" valign="middle" >060605</td><td align="center" valign="middle" >79.100</td><td align="center" valign="middle" >3.78</td></tr><tr><td align="center" valign="middle" >060604</td><td align="center" valign="middle" >95.000</td><td align="center" valign="middle" >2.1357</td></tr><tr><td align="center" valign="middle" >060602A</td><td align="center" valign="middle" >75.000</td><td align="center" valign="middle" >0.787</td></tr><tr><td align="center" valign="middle" >060526</td><td align="center" valign="middle" >298.200</td><td align="center" valign="middle" >3.21</td></tr><tr><td align="center" valign="middle" >060522</td><td align="center" valign="middle" >71.100</td><td align="center" valign="middle" >5.11</td></tr><tr><td align="center" valign="middle" >060512</td><td align="center" valign="middle" >8.500</td><td align="center" valign="middle" >0.4428</td></tr><tr><td align="center" valign="middle" >060510B</td><td align="center" valign="middle" >275.200</td><td align="center" valign="middle" >4.9</td></tr><tr><td align="center" valign="middle" >060505</td><td align="center" valign="middle" >~4</td><td align="center" valign="middle" >0.089</td></tr><tr><td align="center" valign="middle" >060502A</td><td align="center" valign="middle" >28.400</td><td align="center" valign="middle" >1.51</td></tr><tr><td align="center" valign="middle" >060418</td><td align="center" valign="middle" >103.100</td><td align="center" valign="middle" >1.490</td></tr><tr><td align="center" valign="middle" >060223A</td><td align="center" valign="middle" >11.300</td><td align="center" valign="middle" >4.41</td></tr><tr><td align="center" valign="middle" >060218</td><td align="center" valign="middle" >~2100</td><td align="center" valign="middle" >0.0331</td></tr><tr><td align="center" valign="middle" >060210</td><td align="center" valign="middle" >255.000</td><td align="center" valign="middle" >3.91</td></tr><tr><td align="center" valign="middle" >060206</td><td align="center" valign="middle" >7.600</td><td align="center" valign="middle" >4.045</td></tr><tr><td align="center" valign="middle" >060124</td><td align="center" valign="middle" >~750</td><td align="center" valign="middle" >2.30</td></tr><tr><td align="center" valign="middle" >060123</td><td align="center" valign="middle" >900</td><td align="center" valign="middle" >1.099</td></tr><tr><td align="center" valign="middle" >060115</td><td align="center" valign="middle" >139.600</td><td align="center" valign="middle" >3.53</td></tr><tr><td align="center" valign="middle" >060108</td><td align="center" valign="middle" >14.300</td><td align="center" valign="middle" >2.03</td></tr><tr><td align="center" valign="middle" >051117B</td><td align="center" valign="middle" >9.000</td><td align="center" valign="middle" >0.481</td></tr><tr><td align="center" valign="middle" >051111</td><td align="center" valign="middle" >46.100</td><td align="center" valign="middle" >1.549</td></tr><tr><td align="center" valign="middle" >051109B</td><td align="center" valign="middle" >14.300</td><td align="center" valign="middle" >0.080</td></tr><tr><td align="center" valign="middle" >051109A</td><td align="center" valign="middle" >37.200</td><td align="center" valign="middle" >2.346</td></tr><tr><td align="center" valign="middle" >051016B</td><td align="center" valign="middle" >4.000</td><td align="center" valign="middle" >0.9364</td></tr><tr><td align="center" valign="middle" >051006</td><td align="center" valign="middle" >34.800</td><td align="center" valign="middle" >1.059</td></tr><tr><td align="center" valign="middle" >051001</td><td align="center" valign="middle" >189.100</td><td align="center" valign="middle" >2.4296</td></tr><tr><td align="center" valign="middle" >050922C</td><td align="center" valign="middle" >4.500</td><td align="center" valign="middle" >2.198</td></tr><tr><td align="center" valign="middle" >050915A</td><td align="center" valign="middle" >52.000</td><td align="center" valign="middle" >2.5273</td></tr><tr><td align="center" valign="middle" >050908</td><td align="center" valign="middle" >19.400</td><td align="center" valign="middle" >3.350</td></tr><tr><td align="center" valign="middle" >050904</td><td align="center" valign="middle" >174.200</td><td align="center" valign="middle" >6.10</td></tr><tr><td align="center" valign="middle" >050826</td><td align="center" valign="middle" >35.500</td><td align="center" valign="middle" >0.297</td></tr><tr><td align="center" valign="middle" >050824</td><td align="center" valign="middle" >22.600</td><td align="center" valign="middle" >0.83</td></tr><tr><td align="center" valign="middle" >050820A</td><td align="center" valign="middle" >26</td><td align="center" valign="middle" >2.612</td></tr><tr><td align="center" valign="middle" >050819</td><td align="center" valign="middle" >37.700</td><td align="center" valign="middle" >2.5043</td></tr><tr><td align="center" valign="middle" >050814</td><td align="center" valign="middle" >150.900</td><td align="center" valign="middle" >5.3</td></tr><tr><td align="center" valign="middle" >050803</td><td align="center" valign="middle" >87.900</td><td align="center" valign="middle" >0.422</td></tr><tr><td align="center" valign="middle" >050802</td><td align="center" valign="middle" >19.000</td><td align="center" valign="middle" >1.71</td></tr><tr><td align="center" valign="middle" >050730</td><td align="center" valign="middle" >156.500</td><td align="center" valign="middle" >3.96855</td></tr><tr><td align="center" valign="middle" >050724</td><td align="center" valign="middle" >96.000</td><td align="center" valign="middle" >0.257</td></tr><tr><td align="center" valign="middle" >050525A</td><td align="center" valign="middle" >8.800</td><td align="center" valign="middle" >0.606</td></tr><tr><td align="center" valign="middle" >050505</td><td align="center" valign="middle" >58.900</td><td align="center" valign="middle" >4.27</td></tr><tr><td align="center" valign="middle" >050416A</td><td align="center" valign="middle" >2.500</td><td align="center" valign="middle" >0.6535</td></tr><tr><td align="center" valign="middle" >050406</td><td align="center" valign="middle" >5.400</td><td align="center" valign="middle" >2.44</td></tr><tr><td align="center" valign="middle" >050401</td><td align="center" valign="middle" >33.300</td><td align="center" valign="middle" >2.9</td></tr><tr><td align="center" valign="middle" >050319</td><td align="center" valign="middle" >152.500</td><td align="center" valign="middle" >3.24</td></tr><tr><td align="center" valign="middle" >050318</td><td align="center" valign="middle" >32</td><td align="center" valign="middle" >1.44</td></tr><tr><td align="center" valign="middle" >050315</td><td align="center" valign="middle" >95.600</td><td align="center" valign="middle" >1.949</td></tr><tr><td align="center" valign="middle" >050223</td><td align="center" valign="middle" >22.500</td><td align="center" valign="middle" >0.5915</td></tr><tr><td align="center" valign="middle" >050126</td><td align="center" valign="middle" >24.800</td><td align="center" valign="middle" >1.29</td></tr></tbody></table></table-wrap></sec><sec id="s8"><title>Appendix B. MCMC Contour Plots</title></sec><sec id="s9"><title>NOTES</title></sec></body><back><ref-list><title>References</title><ref id="scirp.131976-ref1"><label>1</label><mixed-citation publication-type="other" xlink:type="simple">Klebesadel, R.W., Strong, I.B. and Olson, R.A. (1973) Observations of Gamma-Ray Bursts of Cosmic Origin. The Astrophysical Journal, 182, L85-L88.</mixed-citation></ref><ref id="scirp.131976-ref2"><label>2</label><mixed-citation publication-type="other" xlink:type="simple">Dainotti, M.G., Lenart, A.&amp;#321;., Chraya, A., Sarracino, G., Nagataki, S., Fraija, N., Capozziello, S. and Bogdan, M. (2023) The Gamma-Ray Bursts Fundamental Plane Correlation as a Cosmological Tool. Monthly Notices of the Royal Astronomical Society, 518, 2201-2240. https://doi.org/10.1093/mnras/stac2752</mixed-citation></ref><ref id="scirp.131976-ref3"><label>3</label><mixed-citation publication-type="other" xlink:type="simple">De Simone, B., Nielson, V., Rinaldi, E. and Dainotti, M.G. (2022) A New Perspective on Cosmology Through Supernovae Ia and Gamma-Ray Bursts. Proceedings of the 16th Marcel Grossmann Meeting, 5-10 July 2021, 3130-3140. https://doi.org/doi:10.1142/9789811269776_0256</mixed-citation></ref><ref id="scirp.131976-ref4"><label>4</label><mixed-citation publication-type="other" xlink:type="simple">Horvath, I., Bagoly, Z., Balazs, L.G., Hakkila, J., Horvath, Z., Joo, A.P., Pinter, S., Tóth, L.V., Veres, P. and Racz, I.I. (2024) Mapping the Universe with Gamma-Ray Bursts. Monthly Notices of the Royal Astronomical Society, 527, 7191-7202. https://doi.org/10.1093/mnras/stad3669</mixed-citation></ref><ref id="scirp.131976-ref5"><label>5</label><mixed-citation publication-type="other" xlink:type="simple">Kumar, D., Rani, N., Jain, D., Mahajan, S. and Mukherjee, A. (2023). Gamma-Ray Bursts: A Viable Cosmological Probe? Journal of Cosmology and Astroparticle Physics, 2023, Article No. 021. https://doi.org/10.1088/1475-7516/2023/07/021</mixed-citation></ref><ref id="scirp.131976-ref6"><label>6</label><mixed-citation publication-type="other" xlink:type="simple">Luongo, O. and Muccino, M. (2021) A Roadmap to Gamma-Ray Bursts: New Developments and Applications to Cosmology. Galaxies, 9, Article No. 77. https://doi.org/10.3390/galaxies9040077</mixed-citation></ref><ref id="scirp.131976-ref7"><label>7</label><mixed-citation publication-type="other" xlink:type="simple">Schady, P. (2017) Gamma-Ray Bursts and Their Use as Cosmic Probes. Royal Society Open Science, 4, Article ID: 170304. https://doi.org/10.1098/rsos.170304</mixed-citation></ref><ref id="scirp.131976-ref8"><label>8</label><mixed-citation publication-type="other" xlink:type="simple">Xu, F. and Huang, Y.-F. (2022) Probe the Universe by Using Gamma-Ray Bursts with X-Ray Plateaus. Proceedings of the Sixteenth Marcel Grossmann Meeting, 5-10 July 2021, 3124-3129. https://doi.org/doi:10.1142/9789811269776_0255</mixed-citation></ref><ref id="scirp.131976-ref9"><label>9</label><mixed-citation publication-type="other" xlink:type="simple">Kouveliotou, C., Meegan, C.A., Fishman, G.J., Bhat, N.P., Briggs, M.S., Koshut, T.M., Paciesas, W.S., Pendleton, G.N., Kouveliotou, C., Meegan, C.A., Fishman, G.J., Bhat, N.P., Briggs, M.S., Koshut, T.M., Paciesas, W.S. and Pendleton, G.N. (1993) Identification of Two Classes of Gamma-Ray Bursts. The Astrophysical Journal Letters, 413, L101. https://doi.org/10.1086/186969</mixed-citation></ref><ref id="scirp.131976-ref10"><label>10</label><mixed-citation publication-type="other" xlink:type="simple">Azzam, W.J. and Al Dallal, S. (2015) Gamma-Ray Bursts: Origin, Types, and Prospects. Journal of Magnetohydrodynamics and Plasma Research, 20, 367.</mixed-citation></ref><ref id="scirp.131976-ref11"><label>11</label><mixed-citation publication-type="other" xlink:type="simple">Dai, Z., Daigne, F. and Mészáros, P. (2017) The Theory of Gamma-Ray Bursts. Space Science Reviews, 212, 409-427. https://doi.org/10.1007/s11214-017-0423-z</mixed-citation></ref><ref id="scirp.131976-ref12"><label>12</label><mixed-citation publication-type="other" xlink:type="simple">D’Avanzo, P. (2015) Short Gamma-Ray Bursts: A Review. Journal of High Energy Astrophysics, 7, 73-80. https://doi.org/10.1016/j.jheap.2015.07.002</mixed-citation></ref><ref id="scirp.131976-ref13"><label>13</label><mixed-citation publication-type="other" xlink:type="simple">Salvaterra, R., Campana, S., Vergani, S.D., Covino, S., D’Avanzo, P., Fugazza, D., Ghirlanda, G., Ghisellini, G., Melandri, A., Nava, L., Sbarufatti, B., Flores, H., Piranomonte, S. and Tagliaferri, G. (2012) A Complete Sample of Bright Swift Long Gamma-Ray Bursts. I. Sample Presentation, Luminosity Function and Evolution. The Astrophysical Journal, 749, Article No. 68. https://doi.org/10.1088/0004-637X/749/1/68</mixed-citation></ref><ref id="scirp.131976-ref14"><label>14</label><mixed-citation publication-type="other" xlink:type="simple">Natarajan, P., Albanna, B., Hjorth, J., Ramirez-Ruiz, E., Tanvir, N. and Wijers, R. (2005) The Redshift Distribution of Gamma-Ray Bursts Revisited. Monthly Notices of the Royal Astronomical Society: Letters, 364, L8-L12. https://doi.org/10.1111/j.1745-3933.2005.00094.x</mixed-citation></ref><ref id="scirp.131976-ref15"><label>15</label><mixed-citation publication-type="other" xlink:type="simple">Lan, G.-X., Wei, J.-J., Zeng, H.-D., Li, Y. and Wu, X.-F. (2021) Revisiting the Luminosity and Redshift Distributions of Long Gamma-Ray Bursts. Monthly Notices of the Royal Astronomical Society, 508, 52-68. https://doi.org/10.1093/mnras/stab2508</mixed-citation></ref><ref id="scirp.131976-ref16"><label>16</label><mixed-citation publication-type="other" xlink:type="simple">Yu, H., Wang, F.Y., Dai, Z.G. and Cheng, K.S. (2015) An Unexpectedly Low-Redshift Excess of Swift Gamma-Ray Burst Rate. The Astrophysical Journal Supplement Series, 218, Article No. 13. https://doi.org/10.1088/0067-0049/218/1/13</mixed-citation></ref><ref id="scirp.131976-ref17"><label>17</label><mixed-citation publication-type="other" xlink:type="simple">Le, T. and Mehta, V. (2017) Revisiting the Redshift Distribution of Gamma-Ray Bursts in the Swift Era. The Astrophysical Journal, 837, Article No. 17. https://doi.org/10.3847/1538-4357/aa5fa7</mixed-citation></ref><ref id="scirp.131976-ref18"><label>18</label><mixed-citation publication-type="other" xlink:type="simple">Lloyd-Ronning, N.M., Aykutalp, A. and Johnson, J.L. (2019) On the Cosmological Evolution of Long Gamma-Ray Burst Properties. Monthly Notices of the Royal Astronomical Society, 488, 5823-5832. https://doi.org/10.1093/mnras/stz2155</mixed-citation></ref><ref id="scirp.131976-ref19"><label>19</label><mixed-citation publication-type="other" xlink:type="simple">Petrosian, V., Kitanidis, E. and Kocevski, D. (2015) Cosmological Evolution of Long Gamma-Ray Bursts and the Star Formation Rate. The Astrophysical Journal, 806, Article No. 44. https://doi.org/10.1088/0004-637X/806/1/44</mixed-citation></ref><ref id="scirp.131976-ref20"><label>20</label><mixed-citation publication-type="other" xlink:type="simple">Tsvetkova, A., Frederiks, D., Golenetskii, S., Lysenko, A., Oleynik, P., Pal’shin, V., Svinkin, D., Ulanov, M., Cline, T., Hurley, K. and Aptekar, R. (2017) The Konus-Wind Catalog of Gamma-Ray Bursts with Known Redshifts. I. Bursts Detected in the Triggered Mode. The Astrophysical Journal, 850, Article No. 161. https://doi.org/10.3847/1538-4357/aa96af</mixed-citation></ref><ref id="scirp.131976-ref21"><label>21</label><mixed-citation publication-type="other" xlink:type="simple">Lan, G.-X., Zeng, H.-D., Wei, J.-J. and Wu, X.-F. (2019) The Luminosity Function and Formation Rate of a Complete Sample of Long Gamma-Ray Bursts. Monthly Notices of the Royal Astronomical Society, 488, 4607-4613. https://doi.org/10.1093/mnras/stz2011</mixed-citation></ref><ref id="scirp.131976-ref22"><label>22</label><mixed-citation publication-type="other" xlink:type="simple">Perley, D.A., et al. (2016) The Swift Gamma-Ray Burst Host Galaxy Legacy Survey. I. Sample Selection and Redshift Distribution. The Astrophysical Journal, 817, Article No. 7. https://doi.org/10.3847/0004-637x/817/1/7</mixed-citation></ref><ref id="scirp.131976-ref23"><label>23</label><mixed-citation publication-type="other" xlink:type="simple">Pescalli, A., Ghirlanda, G., Salvaterra, R., Ghisellini, G., Vergani, S.D., Nappo, F., Salafia, O.S., Melandri, A., Covino, S. and G&amp;#246;tz, D. (2016) The Rate and Luminosity Function of Long Gamma-Ray Bursts. Astronomy and Astrophysics, 587, A40. https://doi.org/10.1051/0004-6361/201526760</mixed-citation></ref><ref id="scirp.131976-ref24"><label>24</label><mixed-citation publication-type="other" xlink:type="simple">Bryant, C.M., Osborne, J.A. and Shahmoradi, A. (2021) How Unbiased Statistical Methods Lead to Biased Scientific Discoveries: A Case Study of the Efron-Petrosian Statistic Applied to the Luminosity-Redshift Evolution of Gamma-Ray Bursts. Monthly Notices of the Royal Astronomical Society, 504, 4192-4203. https://doi.org/10.1093/mnras/stab1098</mixed-citation></ref><ref id="scirp.131976-ref25"><label>25</label><mixed-citation publication-type="other" xlink:type="simple">Le, T., Ratke, C. and Mehta, V. (2020) Resolving the Excess of Long GRBs at Low Redshift in the Swift Era. Monthly Notices of the Royal Astronomical Society, 493, 1479-1491. https://doi.org/10.1093/mnras/staa366</mixed-citation></ref><ref id="scirp.131976-ref26"><label>26</label><mixed-citation publication-type="other" xlink:type="simple">Dong, X.F., Li, X.J., Zhang, Z.B. and Zhang, X.L. (2022) A Comparative Study of Luminosity Functions and Event Rate Densities of Long GRBs with Non-Parametric Method. Monthly Notices of the Royal Astronomical Society, 513, 1078-1087. https://doi.org/10.1093/mnras/stac949</mixed-citation></ref><ref id="scirp.131976-ref27"><label>27</label><mixed-citation publication-type="other" xlink:type="simple">Dong, X.F., Zhang, Z.B., Li, Q.M., Huang, Y.F. and Bian, K. (2023) The Origin of Low-Redshift Event Rate Excess as Revealed by the Low-luminosity Gamma-Ray Bursts. The Astrophysical Journal, 958, Article No. 37. https://doi.org/10.3847/1538-4357/acf852</mixed-citation></ref><ref id="scirp.131976-ref28"><label>28</label><mixed-citation publication-type="other" xlink:type="simple">Troja, E., et al. (2022) A Nearby Long Gamma-Ray Burst from a Merger of Compact Objects. Nature, 612, 228-231. https://doi.org/10.1038/s41586-022-05327-3</mixed-citation></ref><ref id="scirp.131976-ref29"><label>29</label><mixed-citation publication-type="other" xlink:type="simple">Petrosian, V. and Dainotti, M.G. (2023) Progenitors of Low Redshift Gamma-Ray Bursts. https://arxiv.org/abs/2305.15081</mixed-citation></ref><ref id="scirp.131976-ref30"><label>30</label><mixed-citation publication-type="other" xlink:type="simple">Ghirlanda, G. and Salvaterra, R. (2022) The Cosmic History of Long Gamma-Ray Bursts. The Astrophysical Journal, 932, Article No. 10. https://doi.org/10.3847/1538-4357/ac6e43</mixed-citation></ref><ref id="scirp.131976-ref31"><label>31</label><mixed-citation publication-type="other" xlink:type="simple">Wang, F.Y. and Dai, Z.G. (2014) Long GRBs Are Metallicity-Biased Tracers of Star Formation: Evidence from Host Galaxies and Redshift Distribution. The Astrophysical Journal Supplement Series, 213, Article No. 15. https://doi.org/10.1088/0067-0049/213/1/15</mixed-citation></ref><ref id="scirp.131976-ref32"><label>32</label><mixed-citation publication-type="other" xlink:type="simple">Hopkins, A.M. and Beacom, J.F. (2006) On the Normalization of the Cosmic Star Formation History. The Astrophysical Journal, 651, 142-154. https://doi.org/10.1086/506610</mixed-citation></ref><ref id="scirp.131976-ref33"><label>33</label><mixed-citation publication-type="other" xlink:type="simple">Li, L.X. (2008) Star Formation History up to z = 7.4: Implications for Gamma-Ray Bursts and Cosmic Metallicity Evolution. Monthly Notices of the Royal Astronomical Society, 388, 1487-1500. https://doi.org/10.1111/j.1365-2966.2008.13488.x</mixed-citation></ref><ref id="scirp.131976-ref34"><label>34</label><mixed-citation publication-type="other" xlink:type="simple">Goodman, J. and Weare, J. (2010) Ensemble Samplers with Affine Invariance. Communications in Applied Mathematics and Computational Science, 5, 65-80. https://doi.org/10.2140/camcos.2010.5.65</mixed-citation></ref><ref id="scirp.131976-ref35"><label>35</label><mixed-citation publication-type="other" xlink:type="simple">Foreman-Mackey, D., Hogg, D.W., Lang, D. and Goodman, J. (2013) Emcee: The MCMC Hammer. http://dan.iel.fm/emcee</mixed-citation></ref><ref id="scirp.131976-ref36"><label>36</label><mixed-citation publication-type="other" xlink:type="simple">Hogg, D.W. and Foreman-Mackey, D. (2018) Data Analysis Recipes: Using Markov Chain Monte Carlo. The Astrophysical Journal Supplement Series, 236, Article No. 11. https://doi.org/10.3847/1538-4365/aab76e</mixed-citation></ref><ref id="scirp.131976-ref37"><label>37</label><mixed-citation publication-type="other" xlink:type="simple">Akaike, H. (1974) A New Look at the Statistical Model Identification. IEEE Transactions on Automatic Control, 19, 716-723. https://doi.org/10.1109/TAC.1974.1100705</mixed-citation></ref><ref id="scirp.131976-ref38"><label>38</label><mixed-citation publication-type="other" xlink:type="simple">Liddle, A.R. (2007) Information Criteria for Astrophysical Model Selection. Monthly Notices of the Royal Astronomical Society, 377, L74-L78. https://doi.org/10.1111/j.1745-3933.2007.00306.x</mixed-citation></ref><ref id="scirp.131976-ref39"><label>39</label><mixed-citation publication-type="other" xlink:type="simple">Deng, Q., Zhang, Z.-B., Li, X.-J., Chang, H.-Y., Zhang, X.-L., Zhen, H.-Y., Sun, H., Pan, Q. and Dong, X.-F. (2022) Reclassifying Swift Gamma-Ray Bursts with Diverse Duration Distributions. The Astrophysical Journal, 940, Article No. 5. https://doi.org/10.3847/1538-4357/ac9590</mixed-citation></ref><ref id="scirp.131976-ref40"><label>40</label><mixed-citation publication-type="other" xlink:type="simple">Kulkarni, S. and Desai, S. (2016) Classification of Gamma-Ray Burst Durations Using Robust Model-Comparison Techniques.</mixed-citation></ref><ref id="scirp.131976-ref41"><label>41</label><mixed-citation publication-type="other" xlink:type="simple">Ruffini, R., Rueda, J.A., Muccino, M., Aimuratov, Y., Becerra, L.M., Bianco, C.L., Kovacevic, M., Moradi, R., Oliveira, F.G., Pisani, G.B. and Wang, Y. (2016) On the Classification of GRBs and Their Occurrence Rates. The Astrophysical Journal, 832, Article No. 136. https://doi.org/10.3847/0004-637x/832/2/136</mixed-citation></ref><ref id="scirp.131976-ref42"><label>42</label><mixed-citation publication-type="other" xlink:type="simple">Salmon, L., Hanlon, L. and Martin-Carrillo, A. (2022) Two Classes of Gamma-Ray Bursts Distinguished within the First Second of Their Prompt Emission. Galaxies, 10, Article No. 78. https://doi.org/10.3390/galaxies10040078</mixed-citation></ref><ref id="scirp.131976-ref43"><label>43</label><mixed-citation publication-type="other" xlink:type="simple">Steinhardt, C.L., Mann, W.J., Rusakov, V. and Jespersen, C.K. (2023) Classification of BATSE, Swift, and Fermi Gamma-Ray Bursts from Prompt Emission Alone. The Astrophysical Journal, 945, Article No. 67. https://doi.org/10.3847/1538-4357/acb999</mixed-citation></ref><ref id="scirp.131976-ref44"><label>44</label><mixed-citation publication-type="other" xlink:type="simple">Tarnopolski, M. (2016) Analysis of the Observed and Intrinsic Durations of Gamma-Ray Bursts with Known Redshift. Astrophysics and Space Science, 361, Article No. 125. https://doi.org/10.1007/s10509-016-2687-2</mixed-citation></ref><ref id="scirp.131976-ref45"><label>45</label><mixed-citation publication-type="other" xlink:type="simple">Zitouni, H., Guessoum, N., Azzam, W.J. and Mochkovitch, R. (2015) Statistical Study of Observed and Intrinsic Durations among BATSE and Swift/BAT GRBs. Astrophysics and Space Science, 357, Article No. 7. https://doi.org/10.1007/s10509-015-2311-x</mixed-citation></ref></ref-list></back></article>