<?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">MSA</journal-id><journal-title-group><journal-title>Materials Sciences and Applications</journal-title></journal-title-group><issn pub-type="epub">2153-117X</issn><publisher><publisher-name>Scientific Research Publishing</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.4236/msa.2016.73016</article-id><article-id pub-id-type="publisher-id">MSA-64789</article-id><article-categories><subj-group subj-group-type="heading"><subject>Articles</subject></subj-group><subj-group subj-group-type="Discipline-v2"><subject>Chemistry&amp;Materials Science</subject></subj-group></article-categories><title-group><article-title>
 
 
  Experimental Study of the Water Absorption Kinetics of the Coconut Shells (Nucifera) of Cameroun
 
</article-title></title-group><contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>ieunedort</surname><given-names>Ndapeu</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>Ebénezer</surname><given-names>Njeugna</given-names></name><xref ref-type="aff" rid="aff2"><sup>2</sup></xref></contrib><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Nicodème</surname><given-names>Rodrigue Sikame</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>Sophie</surname><given-names>Brogly Bistac</given-names></name><xref ref-type="aff" rid="aff3"><sup>3</sup></xref></contrib><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Jean</surname><given-names>Yves Drean</given-names></name><xref ref-type="aff" rid="aff4"><sup>4</sup></xref></contrib><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Médard</surname><given-names>Fogue</given-names></name><xref ref-type="aff" rid="aff1"><sup>1</sup></xref></contrib></contrib-group><aff id="aff4"><addr-line>ENSISA, University of Haute Alsace, Mulhouse, France</addr-line></aff><aff id="aff3"><addr-line>Chemestry School, University of Haute Alsace, Mulhouse, France</addr-line></aff><aff id="aff2"><addr-line>ENSET, University of Douala, Douala, Cameroon</addr-line></aff><aff id="aff1"><addr-line>IUT FV de Bandjoun, University of Dschang, Dschang, Cameroon</addr-line></aff><pub-date pub-type="epub"><day>09</day><month>03</month><year>2016</year></pub-date><volume>07</volume><issue>03</issue><fpage>159</fpage><lpage>170</lpage><history><date date-type="received"><day>5</day>	<month>January</month>	<year>2016</year></date><date date-type="rev-recd"><day>accepted</day>	<month>18</month>	<year>March</year>	</date><date date-type="accepted"><day>21</day>	<month>March</month>	<year>2016</year></date></history><permissions><copyright-statement>&#169; Copyright  2014 by authors and Scientific Research Publishing Inc. </copyright-statement><copyright-year>2014</copyright-year><license><license-p>This work is licensed under the Creative Commons Attribution International License (CC BY). http://creativecommons.org/licenses/by/4.0/</license-p></license></permissions><abstract><p>
 
 
  The study is focused on the phenomenon of diffusion of water through the shells of two coconut species (coconut nucifera) of Cameroun. The kinetics absorption of water was studied experimentally by the gravimetric method with discontinuous control of the mass of the samples at the temperature of 23℃. The mature coconut shells were cleaned mechanically, cut in a spherical shape and placed in a drying oven with 105
  ℃ for 4 hours before being plunged in distilled water at 23
  ℃. This study made it possible not only to determine the rate of water absorbed, but also to model the water kinetic absorption of the shells. Of the two models tested (Peleg and Page), the Page model predicted very well the experimental data. The Fick law made it possible to evaluate the effective diffusivity coefficients at the initial and final phases of absorption. The effective diffusivity coefficient was given from the Arrhenius equation.
 
</p></abstract><kwd-group><kwd>Coconut Shells (CSs)</kwd><kwd> Drying</kwd><kwd> Absorption</kwd><kwd> Coefficient of Effective Diffusivity</kwd><kwd> Activation Energy</kwd></kwd-group></article-meta></front><body><sec id="s1"><title>1. Introduction</title><p>The by-products of the coconut occupy an important place in the current research. This is justified by the dash of valorization of green energies and the fight against pollution. The shell of coconut (CS) is the subject of the research and several research tasks are devoted to it. Certain works are interested in the production of the activated carbon from CS. Other works deal with the use of the CS like charges in the composites [<xref ref-type="bibr" rid="scirp.64789-ref1">1</xref>] and also in concrete [<xref ref-type="bibr" rid="scirp.64789-ref2">2</xref>] . While certain works consider the use of the CS like stabilizer of the grounds [<xref ref-type="bibr" rid="scirp.64789-ref3">3</xref>] . Recent studies determined certain physicochemical and mechanics characteristics of this shell [<xref ref-type="bibr" rid="scirp.64789-ref4">4</xref>] . Its use in the composites implies the phenomena of diffusion of water. The kinetics of drying of the CS was the subject of a recent scientific study [<xref ref-type="bibr" rid="scirp.64789-ref5">5</xref>] , this work proposes to study the kinetics of absorption of CSs. <xref ref-type="table" rid="table1">Table 1</xref> presents the nomenclature of the physical quantities used in the present work.</p></sec><sec id="s2"><title>2. Materials and Methods</title><sec id="s2_1"><title>2.1. Materials</title><p>Coconut shells used in this study come from the areas of the South, the Littoral and the South-west of Cameroun. Two varieties of Shells are concerned, and are characterized by the form of their nut: a lengthened form (species 1) and a round form (species 2). Coconuts shells were separated from nuts and remained at the laboratory in approximate ambient moisture of 60% and at a temperature varying between 20˚C and 23˚C, for two months. The separation of coconuts shells from nuts was carried out mechanically and CSs was cleaned and cut in the form of the shape of a sphere in the southernmost direction (<xref ref-type="fig" rid="fig1">Figure 1</xref>(a)) to obtain samples (<xref ref-type="fig" rid="fig1">Figure 1</xref>(b)). For each one of these samples, we estimated, the rays interior noted Ri and outside noted Re, and the aperture θ while basing ourselves on geometrical layouts. For each species, 20 samples were produced for this study.</p><table-wrap id="table1" ><label><xref ref-type="table" rid="table1">Table 1</xref></label><caption><title> Nomenclature of quantities</title></caption><table><tbody><thead><tr><th align="center" valign="middle"  colspan="4"  >Nomenclature</th></tr></thead><tr><td align="center" valign="middle" >w (%)</td><td align="center" valign="middle" >Water content</td><td align="center" valign="middle" >MR<sub>pre,i </sub></td><td align="center" valign="middle" >Predicted moisture ratio</td></tr><tr><td align="center" valign="middle" >m<sub>0 </sub></td><td align="center" valign="middle" >Initial dry mass (g)</td><td align="center" valign="middle" >MR<sub>exp,i </sub></td><td align="center" valign="middle" >Experimental moisture ratio</td></tr><tr><td align="center" valign="middle" >m<sub>(t) </sub></td><td align="center" valign="middle" >Massat instant t</td><td align="center" valign="middle" >D<sub>eff</sub></td><td align="center" valign="middle" >effective diffusivity(m&#178;/s)</td></tr><tr><td align="center" valign="middle" >m<sub>eq </sub></td><td align="center" valign="middle" >Mass at equilibrium (g)</td><td align="center" valign="middle" >D<sub>0</sub><sup> </sup></td><td align="center" valign="middle" >Pre-exponential factor of the Arrhenius equation (m&#178;/s)</td></tr><tr><td align="center" valign="middle" >MR</td><td align="center" valign="middle" >Moisture ratio</td><td align="center" valign="middle" >R<sub>i</sub></td><td align="center" valign="middle" >Interior radius (mm)</td></tr><tr><td align="center" valign="middle" >a, b, c, k, h, n</td><td align="center" valign="middle" >Models constants</td><td align="center" valign="middle" >R<sub>e</sub></td><td align="center" valign="middle" >Exterior radius (mm)</td></tr><tr><td align="center" valign="middle" >RMSE</td><td align="center" valign="middle" >Root Mean Square Errors</td><td align="center" valign="middle" >t</td><td align="center" valign="middle" >Absorption time</td></tr><tr><td align="center" valign="middle" >SSE</td><td align="center" valign="middle" >Mean of the squares errors</td><td align="center" valign="middle" >r<sup>2</sup></td><td align="center" valign="middle" >Coefficient of determination</td></tr><tr><td align="center" valign="middle" >N</td><td align="center" valign="middle" >Number of Observations</td><td align="center" valign="middle" >R</td><td align="center" valign="middle" >Constant of perfect gas (kJ/mol∙K).</td></tr><tr><td align="center" valign="middle" >MR</td><td align="center" valign="middle" >Moisture ratio</td><td align="center" valign="middle" >T</td><td align="center" valign="middle" >Drying temperature (˚C)</td></tr><tr><td align="center" valign="middle" >P</td><td align="center" valign="middle" >Number of constants</td><td align="center" valign="middle" >E</td><td align="center" valign="middle" >Standard deviation</td></tr></tbody></table></table-wrap><fig id="fig1"  position="float"><label><xref ref-type="fig" rid="fig1">Figure 1</xref></label><caption><title> Presentation of the two varieties of coconuts and the geometry of the samples</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/3-7701771x7.png"/></fig></sec><sec id="s2_2"><title>2.2. Methods</title><p>The samples intended for the tests were dried in a standard drying oven of mark memmert model UN 160 to 105˚C for 4 hours. Under the above drying conditions after 4 hours, the mass of the samples of CS do not vary any longer. This was proven experimentally by [<xref ref-type="bibr" rid="scirp.64789-ref5">5</xref>] . After stoving the samples, once cooled, they were putting distilled water in order to follow their kinetics absorption. The experiments undertaken made it possible to determine the rate of water absorption and to model the kinetics of absorption of these shells using the gravimetric method. The experiment was carried with the help of numerical balance of 0.01 g precision. The samples are weighed after stoving before being immerged to determine their initial drying mass m<sub>0</sub>. For each sample, one notes the moment to which it was immerged, the sample was weighted aftertime duration in water. Making sure that the hygroscopy water was delicately removed and by minimizing the removing time from water. We note m(t) the wet mass of the sample at the instance t. We repeat this experiment until the mass of the sample does not vary anymore and it was notes the equilibrium mass m<sub>eq</sub>.</p></sec><sec id="s2_3"><title>2.3. Theoretic Considerations</title><sec id="s2_3_1"><title>2.3.1. Mathematical Model of the Phenomenon of Diffusion</title><p>The rate of absorption of water W compared to the dry matter of the samples is calculated starting from the drying mass m<sub>0</sub> and of the equilibrium mass m<sub>eq</sub> according to the formula (2). The instantaneous humidity content noted M(T) compared to the dry matter is calculated according to the formula (1). The ratio of the instantaneous rate of absorption which is the equivalent without dimension of the instantaneous water content is calculated according to the formula (3).</p><disp-formula id="scirp.64789-formula1182"><label>(1)</label><graphic position="anchor" xlink:href="http://html.scirp.org/file/3-7701771x8.png"  xlink:type="simple"/></disp-formula><disp-formula id="scirp.64789-formula1183"><label>(2)</label><graphic position="anchor" xlink:href="http://html.scirp.org/file/3-7701771x9.png"  xlink:type="simple"/></disp-formula><disp-formula id="scirp.64789-formula1184"><label>. (3)</label><graphic position="anchor" xlink:href="http://html.scirp.org/file/3-7701771x10.png"  xlink:type="simple"/></disp-formula><p><xref ref-type="table" rid="table2">Table 2</xref> presents the two mathematical models of the kinetic absorption of the vegetation products which were used to simulate those of CSs.</p><p>The software Matlab 2009 and Excel 2007 was used for the identification of the parameters of the various models. The effectiveness of a model is evaluated starting from the statistical criteria such as: the root mean square errors (RMSE) and the coefficient of correlation r<sup>2</sup>. In fact a model is better if r<sup>2</sup> tends towards 1 for a lower value and with RMSE which tends towards 0 for a higher value. These parameters are expressed by the Equations ((4) and (5)) respectively.</p><disp-formula id="scirp.64789-formula1185"><label>(4)</label><graphic position="anchor" xlink:href="http://html.scirp.org/file/3-7701771x11.png"  xlink:type="simple"/></disp-formula><p>where <inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/3-7701771x12.png" xlink:type="simple"/></inline-formula> and <inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/3-7701771x13.png" xlink:type="simple"/></inline-formula> are the ratios of predicted and experimental rate of absorption respectively. N is the number of observations and P the number of constants.</p></sec><sec id="s2_3_2"><title>2.3.2. Estimation of the Effective Diffusivity</title><p>The Equation (5) is that of Ficks which governs the diffusion of mass through the vegetation products [<xref ref-type="bibr" rid="scirp.64789-ref14">14</xref>] .</p><table-wrap id="table2" ><label><xref ref-type="table" rid="table2">Table 2</xref></label><caption><title> Mathematical models used in the kinetics absorption of CSs</title></caption><table><tbody><thead><tr><th align="center" valign="middle" >N˚</th><th align="center" valign="middle" >Names of Models</th><th align="center" valign="middle" >Models</th><th align="center" valign="middle" >References</th></tr></thead><tr><td align="center" valign="middle" >1</td><td align="center" valign="middle" >Peleg</td><td align="center" valign="middle" ><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/3-7701771x14.png" xlink:type="simple"/></inline-formula></td><td align="center" valign="middle" >[<xref ref-type="bibr" rid="scirp.64789-ref6">6</xref>]</td></tr><tr><td align="center" valign="middle" >2</td><td align="center" valign="middle" >Page</td><td align="center" valign="middle" ><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/3-7701771x15.png" xlink:type="simple"/></inline-formula></td><td align="center" valign="middle" >[<xref ref-type="bibr" rid="scirp.64789-ref7">7</xref>] - [<xref ref-type="bibr" rid="scirp.64789-ref13">13</xref>]</td></tr></tbody></table></table-wrap><disp-formula id="scirp.64789-formula1186"><label>(5)</label><graphic position="anchor" xlink:href="http://html.scirp.org/file/3-7701771x16.png"  xlink:type="simple"/></disp-formula><p>where D<sub>eff</sub> is the effective coefficient of diffusion in m<sup>2</sup>/s and M is the rate of absorption. The analytical solution of the Equation (5), for a radial diffusion in a hollow sphere (<inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/3-7701771x17.png" xlink:type="simple"/></inline-formula>) was developed by Carslaw and Jaeger in 1959 [<xref ref-type="bibr" rid="scirp.64789-ref14">14</xref>] . By admitting that the effective coefficient of diffusion depends neither on the concentration, nor on the position, the ratio of the instantaneous rate of absorption obeys the Equation (6).</p><disp-formula id="scirp.64789-formula1187"><label>(6)</label><graphic position="anchor" xlink:href="http://html.scirp.org/file/3-7701771x18.png"  xlink:type="simple"/></disp-formula><p>where MR is the moisture ratio of the water content of all the sample at the moment t and n is a positive entirety.</p><p>In the case that the interior radius r = R<sub>i</sub> and the exterior radius r = R<sub>e</sub> are maintained with concentrations C<sub>1</sub> and C<sub>2</sub> respectively such as C<sub>1</sub> = C<sub>2</sub>, the solution of Carslaw and Jaeger is given by the expression of the equation while limiting at the first term of this series we obtain Equation (7) given by;</p><disp-formula id="scirp.64789-formula1188"><label>. (7)</label><graphic position="anchor" xlink:href="http://html.scirp.org/file/3-7701771x19.png"  xlink:type="simple"/></disp-formula><p>The Neperien logarithm of the Equation (7) by taking in account the two phases of absorption, gives the Equation (8) which makes it possible to determine the coefficients of diffusion D<sub>eff</sub><sub>1</sub> and D<sub>eff</sub><sub>2</sub> at the initial and final phases respectively. Where <inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/3-7701771x20.png" xlink:type="simple"/></inline-formula> is the Heaviside function and τ is the duration of the initial phase of absorption.</p><disp-formula id="scirp.64789-formula1189"><label>. (8)</label><graphic position="anchor" xlink:href="http://html.scirp.org/file/3-7701771x21.png"  xlink:type="simple"/></disp-formula><p>To determine the effective coefficient of diffusion, it is enough to trace the linear straight regression line of <inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/3-7701771x22.png" xlink:type="simple"/></inline-formula> according to time t at the initial phase and at the final phase. The slope of this line makes it possible to calculate D<sub>eff</sub> according to Equation (9).</p><disp-formula id="scirp.64789-formula1190"><label>. (9)</label><graphic position="anchor" xlink:href="http://html.scirp.org/file/3-7701771x23.png"  xlink:type="simple"/></disp-formula></sec></sec></sec><sec id="s3"><title>3. Results and Discussion</title><sec id="s3_1"><title>3.1. Absorption Ratio</title><p>The instantaneous rates of absorption made it possible to plot the curves of the rate of absorption as a function of time. <xref ref-type="fig" rid="fig2">Figure 2</xref> shows us the evolution of the rate of recovery according to time for the two species. It appears on this figure that the kinetics of absorption is faster at the beginning.</p><p><xref ref-type="table" rid="table3">Table 3</xref> gives the values of the rates of absorption obtained for each of the two species. It arises that species 2 has a little higher rate of absorption. It appears clearly in <xref ref-type="table" rid="table3">Table 3</xref> that species 2 absorbs water a bit than species 1.</p></sec><sec id="s3_2"><title>3.2. Kinetic of Water Absorption</title><p>To evaluate the kinetics of absorption of these Shells, starting from the experimental data, we calculate the moisture ratio of the instantaneous rate of absorption noted MR from Equation (3). The curve of MR for each species, presents two phases: an initial phase having a very great slope as of the first instance that the CS is in contact with water; and a final stage characterized by a very weak slope which is asymptotic with MR = 1. The</p><fig-group id="fig2"><label><xref ref-type="fig" rid="fig2">Figure 2</xref></label><caption><title> Curves of the experimental points of absorption ratio of CSs. (a) Case of species 1; (b) Case of species 2.</title></caption><fig id ="fig2_1"><label>(b)</label><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/3-7701771x24.png"/></fig><fig id ="fig2_2"><label></label><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/3-7701771x25.png"/></fig></fig-group><p>durations of absorption of the two species are almost identical and equilibrium is reached at the end of 35 days of immersion.</p><p>To model this kinetics of absorption, we tested the models of Peleg, and Page.</p></sec><sec id="s3_3"><title>3.3. Peleg Model</title><p>Equation (10) present the expression of the Peleg model:</p><disp-formula id="scirp.64789-formula1191"><label>(10)</label><graphic position="anchor" xlink:href="http://html.scirp.org/file/3-7701771x26.png"  xlink:type="simple"/></disp-formula><p>where k<sub>1</sub> is the parameter which characterizes the kinetics of absorption as it can show in Equations (11) and (12).</p><table-wrap id="table3" ><label><xref ref-type="table" rid="table3">Table 3</xref></label><caption><title> Values of the rate of absorption of the coconut shells</title></caption><table><tbody><thead><tr><th align="center" valign="middle"  rowspan="2"  >N˚</th><th align="center" valign="middle"  colspan="2"  >% of absorption (d.b)</th></tr></thead><tr><td align="center" valign="middle" >Species 1</td><td align="center" valign="middle" >Species 2</td></tr><tr><td align="center" valign="middle" >1</td><td align="center" valign="middle" >15.95</td><td align="center" valign="middle" >18.07</td></tr><tr><td align="center" valign="middle" >2</td><td align="center" valign="middle" >16.39</td><td align="center" valign="middle" >19.64</td></tr><tr><td align="center" valign="middle" >3</td><td align="center" valign="middle" >18.72</td><td align="center" valign="middle" >18.81</td></tr><tr><td align="center" valign="middle" >4</td><td align="center" valign="middle" >18.53</td><td align="center" valign="middle" >21.00</td></tr><tr><td align="center" valign="middle" >5</td><td align="center" valign="middle" >18.89</td><td align="center" valign="middle" >17.79</td></tr><tr><td align="center" valign="middle" >6</td><td align="center" valign="middle" >16.22</td><td align="center" valign="middle" >19.45</td></tr><tr><td align="center" valign="middle" >7</td><td align="center" valign="middle" >16.55</td><td align="center" valign="middle" >18.68</td></tr><tr><td align="center" valign="middle" >8</td><td align="center" valign="middle" >18.31</td><td align="center" valign="middle" >19.36</td></tr><tr><td align="center" valign="middle" >9</td><td align="center" valign="middle" >15.73</td><td align="center" valign="middle" >19.57</td></tr><tr><td align="center" valign="middle" >10</td><td align="center" valign="middle" >16.92</td><td align="center" valign="middle" >22.39</td></tr><tr><td align="center" valign="middle" >11</td><td align="center" valign="middle" >18.98</td><td align="center" valign="middle" >21.73</td></tr><tr><td align="center" valign="middle" >12</td><td align="center" valign="middle" >16.99</td><td align="center" valign="middle" >22.09</td></tr><tr><td align="center" valign="middle" >13</td><td align="center" valign="middle" >18.14</td><td align="center" valign="middle" >17.42</td></tr><tr><td align="center" valign="middle" >14</td><td align="center" valign="middle" >16.17</td><td align="center" valign="middle" >24.08</td></tr><tr><td align="center" valign="middle" >15</td><td align="center" valign="middle" >17.42</td><td align="center" valign="middle" >23.21</td></tr><tr><td align="center" valign="middle" >16</td><td align="center" valign="middle" >17.22</td><td align="center" valign="middle" >23.58</td></tr><tr><td align="center" valign="middle" >17</td><td align="center" valign="middle" >18.32</td><td align="center" valign="middle" >20.53</td></tr><tr><td align="center" valign="middle" >18</td><td align="center" valign="middle" >16.32</td><td align="center" valign="middle" >20.23</td></tr><tr><td align="center" valign="middle" >19</td><td align="center" valign="middle" >17.62</td><td align="center" valign="middle" >21.43</td></tr><tr><td align="center" valign="middle" >20</td><td align="center" valign="middle" >17.02</td><td align="center" valign="middle" >19.43</td></tr><tr><td align="center" valign="middle" >A</td><td align="center" valign="middle" >17.32</td><td align="center" valign="middle" >20.42</td></tr><tr><td align="center" valign="middle" >S</td><td align="center" valign="middle" >1.06</td><td align="center" valign="middle" >1.95</td></tr></tbody></table></table-wrap><disp-formula id="scirp.64789-formula1192"><label>(11)</label><graphic position="anchor" xlink:href="http://html.scirp.org/file/3-7701771x27.png"  xlink:type="simple"/></disp-formula><p>and</p><disp-formula id="scirp.64789-formula1193"><label>(12)</label><graphic position="anchor" xlink:href="http://html.scirp.org/file/3-7701771x28.png"  xlink:type="simple"/></disp-formula><p>k<sub>2</sub> characterizes the rate of absorption indeed at equilibrium, when <inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/3-7701771x29.png" xlink:type="simple"/></inline-formula> we obtain the Equation (13).</p><disp-formula id="scirp.64789-formula1194"><label>. (13)</label><graphic position="anchor" xlink:href="http://html.scirp.org/file/3-7701771x30.png"  xlink:type="simple"/></disp-formula><p>The advantage of this model is that it can be put in the form of Equation (14):</p><disp-formula id="scirp.64789-formula1195"><label>. (14)</label><graphic position="anchor" xlink:href="http://html.scirp.org/file/3-7701771x31.png"  xlink:type="simple"/></disp-formula><p>The exploitation of the Equation (14) makes it possible to obtain the values of the parameters k<sub>1</sub> and k<sub>2</sub> of Peleg, by linear regression. These statistical constants and these parameters are presented in <xref ref-type="table" rid="table4">Table 4</xref>. The mean values of the constants of Peleg enable us quantitatively to compare the kinetics of absorption of the two species. It arises from <xref ref-type="table" rid="table4">Table 4</xref> that the values of the constants k<sub>1</sub> and k<sub>2</sub> are a bite different from one species to another since the confidence intervals overlap.</p><table-wrap id="table4" ><label><xref ref-type="table" rid="table4">Table 4</xref></label><caption><title> Parameters values for Peleg model</title></caption><table><tbody><thead><tr><th align="center" valign="middle"  rowspan="2"  >N˚</th><th align="center" valign="middle"  colspan="4"  >Species 1</th><th align="center" valign="middle"  colspan="4"  >Species 2</th></tr></thead><tr><td align="center" valign="middle" >R&#178;</td><td align="center" valign="middle" >RSME</td><td align="center" valign="middle" >k<sub>1</sub> (min∙%<sup>−1</sup>d.b)</td><td align="center" valign="middle" >k<sub>2</sub> (%<sup>−1</sup>d∙b)</td><td align="center" valign="middle" >R&#178;</td><td align="center" valign="middle" >RMSE</td><td align="center" valign="middle" >k<sub>1</sub> (min∙%<sup>−1</sup>d∙b)</td><td align="center" valign="middle" >k<sub>2</sub> (%<sup>−1</sup>d∙b)</td></tr><tr><td align="center" valign="middle" >1</td><td align="center" valign="middle" >0.9995</td><td align="center" valign="middle" >0.96</td><td align="center" valign="middle" >19.380</td><td align="center" valign="middle" >0.0631</td><td align="center" valign="middle" >0.9995</td><td align="center" valign="middle" >0.76</td><td align="center" valign="middle" >13.06</td><td align="center" valign="middle" >0.056</td></tr><tr><td align="center" valign="middle" >2</td><td align="center" valign="middle" >0.9996</td><td align="center" valign="middle" >0.97</td><td align="center" valign="middle" >13.240</td><td align="center" valign="middle" >0.0542</td><td align="center" valign="middle" >0.9993</td><td align="center" valign="middle" >0.84</td><td align="center" valign="middle" >14.92</td><td align="center" valign="middle" >0.057</td></tr><tr><td align="center" valign="middle" >3</td><td align="center" valign="middle" >0.9997</td><td align="center" valign="middle" >0.96</td><td align="center" valign="middle" >13.000</td><td align="center" valign="middle" >0.0608</td><td align="center" valign="middle" >0.9993</td><td align="center" valign="middle" >0.76</td><td align="center" valign="middle" >13.68</td><td align="center" valign="middle" >0.052</td></tr><tr><td align="center" valign="middle" >4</td><td align="center" valign="middle" >0.9987</td><td align="center" valign="middle" >0.97</td><td align="center" valign="middle" >18.590</td><td align="center" valign="middle" >0.0555</td><td align="center" valign="middle" >0.9992</td><td align="center" valign="middle" >0.98</td><td align="center" valign="middle" >16.04</td><td align="center" valign="middle" >0.064</td></tr><tr><td align="center" valign="middle" >5</td><td align="center" valign="middle" >0.9991</td><td align="center" valign="middle" >0.98</td><td align="center" valign="middle" >17.340</td><td align="center" valign="middle" >0.0540</td><td align="center" valign="middle" >0.9993</td><td align="center" valign="middle" >0.57</td><td align="center" valign="middle" >19.8</td><td align="center" valign="middle" >0.051</td></tr><tr><td align="center" valign="middle" >6</td><td align="center" valign="middle" >0.9998</td><td align="center" valign="middle" >0.99</td><td align="center" valign="middle" >13.100</td><td align="center" valign="middle" >0.0619</td><td align="center" valign="middle" >0.9997</td><td align="center" valign="middle" >0.79</td><td align="center" valign="middle" >18.27</td><td align="center" valign="middle" >0.052</td></tr><tr><td align="center" valign="middle" >7</td><td align="center" valign="middle" >0.9997</td><td align="center" valign="middle" >0.98</td><td align="center" valign="middle" >15.330</td><td align="center" valign="middle" >0.0639</td><td align="center" valign="middle" >0.9977</td><td align="center" valign="middle" >0.84</td><td align="center" valign="middle" >14.85</td><td align="center" valign="middle" >0.046</td></tr><tr><td align="center" valign="middle" >8</td><td align="center" valign="middle" >0.9996</td><td align="center" valign="middle" >0.97</td><td align="center" valign="middle" >16.850</td><td align="center" valign="middle" >0.0716</td><td align="center" valign="middle" >0.9995</td><td align="center" valign="middle" >0.72</td><td align="center" valign="middle" >14.79</td><td align="center" valign="middle" >0.042</td></tr><tr><td align="center" valign="middle" >9</td><td align="center" valign="middle" >0.9996</td><td align="center" valign="middle" >0.98</td><td align="center" valign="middle" >18.590</td><td align="center" valign="middle" >0.0555</td><td align="center" valign="middle" >0.9981</td><td align="center" valign="middle" >0.79</td><td align="center" valign="middle" >18.1</td><td align="center" valign="middle" >0.055</td></tr><tr><td align="center" valign="middle" >10</td><td align="center" valign="middle" >0.9998</td><td align="center" valign="middle" >0.99</td><td align="center" valign="middle" >17.340</td><td align="center" valign="middle" >0.0540</td><td align="center" valign="middle" >0.9975</td><td align="center" valign="middle" >0.81</td><td align="center" valign="middle" >16.73</td><td align="center" valign="middle" >0.047</td></tr><tr><td align="center" valign="middle" >11</td><td align="center" valign="middle" >0.9983</td><td align="center" valign="middle" >0.99</td><td align="center" valign="middle" >15.330</td><td align="center" valign="middle" >0.0639</td><td align="center" valign="middle" >0.9986</td><td align="center" valign="middle" >0.58</td><td align="center" valign="middle" >15.57</td><td align="center" valign="middle" >0.049</td></tr><tr><td align="center" valign="middle" >12</td><td align="center" valign="middle" >0.9987</td><td align="center" valign="middle" >0.99</td><td align="center" valign="middle" >16.850</td><td align="center" valign="middle" >0.0716</td><td align="center" valign="middle" >0.9989</td><td align="center" valign="middle" >0.99</td><td align="center" valign="middle" >16.71</td><td align="center" valign="middle" >0.053</td></tr><tr><td align="center" valign="middle" >13</td><td align="center" valign="middle" >0.9968</td><td align="center" valign="middle" >0.96</td><td align="center" valign="middle" >18.720</td><td align="center" valign="middle" >0.0545</td><td align="center" valign="middle" >0.9983</td><td align="center" valign="middle" >0.76</td><td align="center" valign="middle" >17.47</td><td align="center" valign="middle" >0.046</td></tr><tr><td align="center" valign="middle" >14</td><td align="center" valign="middle" >0.9991</td><td align="center" valign="middle" >0.97</td><td align="center" valign="middle" >18.590</td><td align="center" valign="middle" >0.0555</td><td align="center" valign="middle" >0.9984</td><td align="center" valign="middle" >0.70</td><td align="center" valign="middle" >16.32</td><td align="center" valign="middle" >0.043</td></tr><tr><td align="center" valign="middle" >15</td><td align="center" valign="middle" >0.9991</td><td align="center" valign="middle" >0.98</td><td align="center" valign="middle" >16.589</td><td align="center" valign="middle" >0.0600</td><td align="center" valign="middle" >0.9988</td><td align="center" valign="middle" >0.80</td><td align="center" valign="middle" >16.16</td><td align="center" valign="middle" >0.05</td></tr><tr><td align="center" valign="middle" >16</td><td align="center" valign="middle" >0.9996</td><td align="center" valign="middle" >0.99</td><td align="center" valign="middle" >13.240</td><td align="center" valign="middle" >0.0542</td><td align="center" valign="middle" >0.9993</td><td align="center" valign="middle" >0.83</td><td align="center" valign="middle" >14.92</td><td align="center" valign="middle" >0.057</td></tr><tr><td align="center" valign="middle" >17</td><td align="center" valign="middle" >0.9991</td><td align="center" valign="middle" >0.98</td><td align="center" valign="middle" >17.350</td><td align="center" valign="middle" >0.0540</td><td align="center" valign="middle" >0.9993</td><td align="center" valign="middle" >0.58</td><td align="center" valign="middle" >19.8</td><td align="center" valign="middle" >0.051</td></tr><tr><td align="center" valign="middle" >18</td><td align="center" valign="middle" >0.9996</td><td align="center" valign="middle" >0.98</td><td align="center" valign="middle" >18.590</td><td align="center" valign="middle" >0.0555</td><td align="center" valign="middle" >0.9981</td><td align="center" valign="middle" >0.59</td><td align="center" valign="middle" >18.1</td><td align="center" valign="middle" >0.055</td></tr><tr><td align="center" valign="middle" >19</td><td align="center" valign="middle" >0.9991</td><td align="center" valign="middle" >0.99</td><td align="center" valign="middle" >18.590</td><td align="center" valign="middle" >0.0555</td><td align="center" valign="middle" >0.9984</td><td align="center" valign="middle" >0.63</td><td align="center" valign="middle" >16.32</td><td align="center" valign="middle" >0.044</td></tr><tr><td align="center" valign="middle" >20</td><td align="center" valign="middle" >0.9981</td><td align="center" valign="middle" >0.97</td><td align="center" valign="middle" >19.380</td><td align="center" valign="middle" >0.0631</td><td align="center" valign="middle" >0.9995</td><td align="center" valign="middle" >0.74</td><td align="center" valign="middle" >15.623</td><td align="center" valign="middle" >0.056</td></tr><tr><td align="center" valign="middle" >A</td><td align="center" valign="middle" >0.9991</td><td align="center" valign="middle" >0.98</td><td align="center" valign="middle" >16.799</td><td align="center" valign="middle" >0.0591</td><td align="center" valign="middle" >0.9988</td><td align="center" valign="middle" >0.76</td><td align="center" valign="middle" >16.362</td><td align="center" valign="middle" >0.051</td></tr><tr><td align="center" valign="middle" >S</td><td align="center" valign="middle" >0.000</td><td align="center" valign="middle" >0.01</td><td align="center" valign="middle" >2.198</td><td align="center" valign="middle" >0.005</td><td align="center" valign="middle" >0.000</td><td align="center" valign="middle" >0.12</td><td align="center" valign="middle" >1.823</td><td align="center" valign="middle" >0.006</td></tr></tbody></table></table-wrap></sec><sec id="s3_4"><title>3.4. Page Model</title><p>The Page model is governed by the Equation (15).</p><disp-formula id="scirp.64789-formula1196"><label>(15)</label><graphic position="anchor" xlink:href="http://html.scirp.org/file/3-7701771x32.png"  xlink:type="simple"/></disp-formula><p>where a and n are the parameters which are obtained by a nonlinear regression using the software Matlab (2009). The statistical parameters and the values of the parameters of this model are given in <xref ref-type="table" rid="table5">Table 5</xref>.</p><p>The Page model predicts very well the kinetics absorption of the CS according to the values of the statistical parameters such as: r&#178; and RMSE. <xref ref-type="fig" rid="fig3">Figure 3</xref> shows the adjustment of Page and Peleg models to the experimental data of each species.</p></sec><sec id="s3_5"><title>3.5. Coefficients of Effective Diffusivity</title><p>To determine the effective coefficients of diffusion, one takes into account the two phases of absorption kinetics. The Fick law expressed by Equation (7) was adopted for each phase. Equations ((16) and (17)) translate Fick law for the initial and final phases of the water absorption in this study.</p><disp-formula id="scirp.64789-formula1197"><label>(16)</label><graphic position="anchor" xlink:href="http://html.scirp.org/file/3-7701771x33.png"  xlink:type="simple"/></disp-formula><disp-formula id="scirp.64789-formula1198"><label>. (17)</label><graphic position="anchor" xlink:href="http://html.scirp.org/file/3-7701771x34.png"  xlink:type="simple"/></disp-formula><table-wrap id="table5" ><label><xref ref-type="table" rid="table5">Table 5</xref></label><caption><title> Values of the parameters and the statistical data of page model</title></caption><table><tbody><thead><tr><th align="center" valign="middle"  colspan="5"  >Species 1</th><th align="center" valign="middle"  colspan="5"  >Species 2</th></tr></thead><tr><td align="center" valign="middle" >N˚</td><td align="center" valign="middle" >R&#178;</td><td align="center" valign="middle" >RMSE</td><td align="center" valign="middle" >a</td><td align="center" valign="middle" >n</td><td align="center" valign="middle" >N˚</td><td align="center" valign="middle" >R&#178;</td><td align="center" valign="middle" >RMSE</td><td align="center" valign="middle" >a</td><td align="center" valign="middle" >n</td></tr><tr><td align="center" valign="middle" >1</td><td align="center" valign="middle" >0.9944</td><td align="center" valign="middle" >0.0230</td><td align="center" valign="middle" >0.0692</td><td align="center" valign="middle" >0.3853</td><td align="center" valign="middle" >1</td><td align="center" valign="middle" >0.9695</td><td align="center" valign="middle" >0.0551</td><td align="center" valign="middle" >0.0983</td><td align="center" valign="middle" >0.3950</td></tr><tr><td align="center" valign="middle" >2</td><td align="center" valign="middle" >0.9938</td><td align="center" valign="middle" >0.0225</td><td align="center" valign="middle" >0.1087</td><td align="center" valign="middle" >0.3427</td><td align="center" valign="middle" >2</td><td align="center" valign="middle" >0.9952</td><td align="center" valign="middle" >0.0228</td><td align="center" valign="middle" >0.0724</td><td align="center" valign="middle" >0.4366</td></tr><tr><td align="center" valign="middle" >3</td><td align="center" valign="middle" >0.9962</td><td align="center" valign="middle" >0.0179</td><td align="center" valign="middle" >0.0995</td><td align="center" valign="middle" >0.3311</td><td align="center" valign="middle" >3</td><td align="center" valign="middle" >0.9935</td><td align="center" valign="middle" >0.0247</td><td align="center" valign="middle" >0.0664</td><td align="center" valign="middle" >0.3682</td></tr><tr><td align="center" valign="middle" >4</td><td align="center" valign="middle" >0.9953</td><td align="center" valign="middle" >0.0197</td><td align="center" valign="middle" >0.0996</td><td align="center" valign="middle" >0.3648</td><td align="center" valign="middle" >4</td><td align="center" valign="middle" >0.9830</td><td align="center" valign="middle" >0.0475</td><td align="center" valign="middle" >0.1139</td><td align="center" valign="middle" >0.3409</td></tr><tr><td align="center" valign="middle" >5</td><td align="center" valign="middle" >0.9967</td><td align="center" valign="middle" >0.0174</td><td align="center" valign="middle" >0.0900</td><td align="center" valign="middle" >0.4053</td><td align="center" valign="middle" >5</td><td align="center" valign="middle" >0.9828</td><td align="center" valign="middle" >0.0421</td><td align="center" valign="middle" >0.1684</td><td align="center" valign="middle" >0.2813</td></tr><tr><td align="center" valign="middle" >6</td><td align="center" valign="middle" >0.9979</td><td align="center" valign="middle" >0.0145</td><td align="center" valign="middle" >0.0884</td><td align="center" valign="middle" >0.3996</td><td align="center" valign="middle" >6</td><td align="center" valign="middle" >0.9876</td><td align="center" valign="middle" >0.1252</td><td align="center" valign="middle" >0.2373</td><td align="center" valign="middle" >0.2492</td></tr><tr><td align="center" valign="middle" >7</td><td align="center" valign="middle" >0.9969</td><td align="center" valign="middle" >0.0177</td><td align="center" valign="middle" >0.1158</td><td align="center" valign="middle" >0.3673</td><td align="center" valign="middle" >7</td><td align="center" valign="middle" >0.9871</td><td align="center" valign="middle" >0.1568</td><td align="center" valign="middle" >0.1498</td><td align="center" valign="middle" >0.2630</td></tr><tr><td align="center" valign="middle" >8</td><td align="center" valign="middle" >0.9969</td><td align="center" valign="middle" >0.0165</td><td align="center" valign="middle" >0.0571</td><td align="center" valign="middle" >0.3982</td><td align="center" valign="middle" >8</td><td align="center" valign="middle" >0.9916</td><td align="center" valign="middle" >0.0272</td><td align="center" valign="middle" >0.0982</td><td align="center" valign="middle" >0.3600</td></tr><tr><td align="center" valign="middle" >9</td><td align="center" valign="middle" >0.9851</td><td align="center" valign="middle" >0.0378</td><td align="center" valign="middle" >0.0571</td><td align="center" valign="middle" >0.3982</td><td align="center" valign="middle" >9</td><td align="center" valign="middle" >0.9676</td><td align="center" valign="middle" >0.0593</td><td align="center" valign="middle" >0.0578</td><td align="center" valign="middle" >0.4799</td></tr><tr><td align="center" valign="middle" >10</td><td align="center" valign="middle" >0.9811</td><td align="center" valign="middle" >0.0388</td><td align="center" valign="middle" >0.0689</td><td align="center" valign="middle" >0.3904</td><td align="center" valign="middle" >10</td><td align="center" valign="middle" >0.9917</td><td align="center" valign="middle" >0.0284</td><td align="center" valign="middle" >0.0780</td><td align="center" valign="middle" >0.3798</td></tr><tr><td align="center" valign="middle" >11</td><td align="center" valign="middle" >0.9908</td><td align="center" valign="middle" >0.0295</td><td align="center" valign="middle" >0.0700</td><td align="center" valign="middle" >0.4204</td><td align="center" valign="middle" >11</td><td align="center" valign="middle" >0.9614</td><td align="center" valign="middle" >0.0632</td><td align="center" valign="middle" >0.0912</td><td align="center" valign="middle" >0.4008</td></tr><tr><td align="center" valign="middle" >12</td><td align="center" valign="middle" >0.9766</td><td align="center" valign="middle" >0.0491</td><td align="center" valign="middle" >0.1554</td><td align="center" valign="middle" >0.3363</td><td align="center" valign="middle" >12</td><td align="center" valign="middle" >0.9937</td><td align="center" valign="middle" >0.0251</td><td align="center" valign="middle" >0.0709</td><td align="center" valign="middle" >0.3902</td></tr><tr><td align="center" valign="middle" >13</td><td align="center" valign="middle" >0.9944</td><td align="center" valign="middle" >0.0230</td><td align="center" valign="middle" >0.0692</td><td align="center" valign="middle" >0.3853</td><td align="center" valign="middle" >13</td><td align="center" valign="middle" >0.9796</td><td align="center" valign="middle" >0.0426</td><td align="center" valign="middle" >0.1176</td><td align="center" valign="middle" >0.3546</td></tr><tr><td align="center" valign="middle" >14</td><td align="center" valign="middle" >0.9938</td><td align="center" valign="middle" >0.0225</td><td align="center" valign="middle" >0.1087</td><td align="center" valign="middle" >0.3427</td><td align="center" valign="middle" >14</td><td align="center" valign="middle" >0.9847</td><td align="center" valign="middle" >0.0381</td><td align="center" valign="middle" >0.1012</td><td align="center" valign="middle" >0.3674</td></tr><tr><td align="center" valign="middle" >15</td><td align="center" valign="middle" >0.9962</td><td align="center" valign="middle" >0.0179</td><td align="center" valign="middle" >0.0995</td><td align="center" valign="middle" >0.3311</td><td align="center" valign="middle" >15</td><td align="center" valign="middle" >0.9927</td><td align="center" valign="middle" >0.0622</td><td align="center" valign="middle" >0.1160</td><td align="center" valign="middle" >0.3758</td></tr><tr><td align="center" valign="middle" >16</td><td align="center" valign="middle" >0.9953</td><td align="center" valign="middle" >0.0197</td><td align="center" valign="middle" >0.0996</td><td align="center" valign="middle" >0.3648</td><td align="center" valign="middle" >16</td><td align="center" valign="middle" >0.9839</td><td align="center" valign="middle" >0.0615</td><td align="center" valign="middle" >0.1149</td><td align="center" valign="middle" >0.3500</td></tr><tr><td align="center" valign="middle" >17</td><td align="center" valign="middle" >0.9962</td><td align="center" valign="middle" >0.0179</td><td align="center" valign="middle" >0.0995</td><td align="center" valign="middle" >0.3311</td><td align="center" valign="middle" >17</td><td align="center" valign="middle" >0.9737</td><td align="center" valign="middle" >0.0583</td><td align="center" valign="middle" >0.1468</td><td align="center" valign="middle" >0.3364</td></tr><tr><td align="center" valign="middle" >18</td><td align="center" valign="middle" >0.9969</td><td align="center" valign="middle" >0.0177</td><td align="center" valign="middle" >0.1158</td><td align="center" valign="middle" >0.3673</td><td align="center" valign="middle" >18</td><td align="center" valign="middle" >0.9943</td><td align="center" valign="middle" >0.0504</td><td align="center" valign="middle" >0.1410</td><td align="center" valign="middle" >0.3065</td></tr><tr><td align="center" valign="middle" >19</td><td align="center" valign="middle" >0.9944</td><td align="center" valign="middle" >0.0230</td><td align="center" valign="middle" >0.0692</td><td align="center" valign="middle" >0.3853</td><td align="center" valign="middle" >19</td><td align="center" valign="middle" >0.9957</td><td align="center" valign="middle" >0.0214</td><td align="center" valign="middle" >0.0664</td><td align="center" valign="middle" >0.4092</td></tr><tr><td align="center" valign="middle" >20</td><td align="center" valign="middle" >0.9969</td><td align="center" valign="middle" >0.0165</td><td align="center" valign="middle" >0.0571</td><td align="center" valign="middle" >0.3982</td><td align="center" valign="middle" >20</td><td align="center" valign="middle" >0.9917</td><td align="center" valign="middle" >0.0251</td><td align="center" valign="middle" >0.0770</td><td align="center" valign="middle" >0.3120</td></tr><tr><td align="center" valign="middle" >A</td><td align="center" valign="middle" >0.9926</td><td align="center" valign="middle" >0.0242</td><td align="center" valign="middle" >0.0911</td><td align="center" valign="middle" >0.3727</td><td align="center" valign="middle" >A</td><td align="center" valign="middle" >0.9851</td><td align="center" valign="middle" >0.0518</td><td align="center" valign="middle" >0.1092</td><td align="center" valign="middle" >0.3578</td></tr><tr><td align="center" valign="middle" >S</td><td align="center" valign="middle" >0.0062</td><td align="center" valign="middle" >0.0097</td><td align="center" valign="middle" >0.0256</td><td align="center" valign="middle" >0.0291</td><td align="center" valign="middle" >S</td><td align="center" valign="middle" >0.0101</td><td align="center" valign="middle" >0.0343</td><td align="center" valign="middle" >0.0435</td><td align="center" valign="middle" >0.0568</td></tr></tbody></table></table-wrap><fig-group id="fig3"><label><xref ref-type="fig" rid="fig3">Figure 3</xref></label><caption><title> Adjustment of the Page model on the experimental data. (a) Case of species 1; (b) Case of species 2.</title></caption><fig id ="fig3_1"><label>(b)</label><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/3-7701771x35.png"/></fig><fig id ="fig3_2"><label></label><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/3-7701771x36.png"/></fig></fig-group><fig id="fig4"  position="float"><label><xref ref-type="fig" rid="fig4">Figure 4</xref></label><caption><title> Curves of Ln(1-Mr.) with respect to time for some samples</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/3-7701771x37.png"/></fig><p>where D<sub>eff</sub><sub>1</sub> and D<sub>eff</sub><sub>2</sub> indicate the coefficients of effective diffusivity at initial and final phases respectively.</p><p><xref ref-type="fig" rid="fig4">Figure 4</xref> shows the linear regression of experimental points of the species 1 and 2 at the initial phase. The slopes of those lines make it possible to calculate D<sub>eff</sub><sub>1</sub> at the initial phase. The same reasoning is used to determine the coefficients of diffusion of the final phase of the two species.</p><p><xref ref-type="table" rid="table6">Table 6</xref> gives the values of these coefficients for the two coconuts species. It is deduced from this table that the coefficients of diffusion of the two species for a given phase are a bite different.</p><p><xref ref-type="table" rid="table7">Table 7</xref> presents the comparison of the effective coefficients of diffusion during water absorption of the CS with some crops. The coefficients of diffusion of CSs at the initial phase are higher than those of a majority of the products except that of wood. According to the results of <xref ref-type="table" rid="table7">Table 7</xref>, the value of the coefficient of diffusion at the initial phase is close to that of grain of rice.</p><table-wrap id="table6" ><label><xref ref-type="table" rid="table6">Table 6</xref></label><caption><title> Values of the coefficients of diffusion of the initial phase and the final phase</title></caption><table><tbody><thead><tr><th align="center" valign="middle"  colspan="3"  >Species 1</th><th align="center" valign="middle"  colspan="3"  >Species 2</th></tr></thead><tr><td align="center" valign="middle" >N˚</td><td align="center" valign="middle" >Deff<sub>1</sub> (m&#178;/min)</td><td align="center" valign="middle" >Deff<sub>2</sub> (m&#178;/min)</td><td align="center" valign="middle" >N˚</td><td align="center" valign="middle" >Deff<sub>1</sub> (m&#178;/min)</td><td align="center" valign="middle" >Deff<sub>2</sub> (m&#178;/min)</td></tr><tr><td align="center" valign="middle" >1</td><td align="center" valign="middle" >6.49E−09</td><td align="center" valign="middle" >1.30E−10</td><td align="center" valign="middle" >1</td><td align="center" valign="middle" >6.49E−09</td><td align="center" valign="middle" >1.46E−10</td></tr><tr><td align="center" valign="middle" >2</td><td align="center" valign="middle" >8.11E−09</td><td align="center" valign="middle" >1.46E−10</td><td align="center" valign="middle" >2</td><td align="center" valign="middle" >8.11E−09</td><td align="center" valign="middle" >1.30E−10</td></tr><tr><td align="center" valign="middle" >3</td><td align="center" valign="middle" >8.11E−09</td><td align="center" valign="middle" >9.74E−11</td><td align="center" valign="middle" >3</td><td align="center" valign="middle" >4.87E−09</td><td align="center" valign="middle" >1.46E−10</td></tr><tr><td align="center" valign="middle" >4</td><td align="center" valign="middle" >8.11E−09</td><td align="center" valign="middle" >9.74E−11</td><td align="center" valign="middle" >4</td><td align="center" valign="middle" >6.49E−09</td><td align="center" valign="middle" >1.30E−10</td></tr><tr><td align="center" valign="middle" >5</td><td align="center" valign="middle" >4.87E−09</td><td align="center" valign="middle" >1.62E−10</td><td align="center" valign="middle" >5</td><td align="center" valign="middle" >6.49E−09</td><td align="center" valign="middle" >1.62E−14</td></tr><tr><td align="center" valign="middle" >6</td><td align="center" valign="middle" >4.87E−09</td><td align="center" valign="middle" >9.74E−11</td><td align="center" valign="middle" >6</td><td align="center" valign="middle" >4.87E−09</td><td align="center" valign="middle" >1.30E−10</td></tr><tr><td align="center" valign="middle" >7</td><td align="center" valign="middle" >4.87E−09</td><td align="center" valign="middle" >1.30E−10</td><td align="center" valign="middle" >7</td><td align="center" valign="middle" >6.49E−09</td><td align="center" valign="middle" >1.30E−10</td></tr><tr><td align="center" valign="middle" >8</td><td align="center" valign="middle" >4.87E−09</td><td align="center" valign="middle" >1.14E−10</td><td align="center" valign="middle" >8</td><td align="center" valign="middle" >4.87E−09</td><td align="center" valign="middle" >1.14E−10</td></tr><tr><td align="center" valign="middle" >9</td><td align="center" valign="middle" >4.87E−09</td><td align="center" valign="middle" >1.30E−10</td><td align="center" valign="middle" >9</td><td align="center" valign="middle" >6.49E−09</td><td align="center" valign="middle" >1.46E−10</td></tr><tr><td align="center" valign="middle" >10</td><td align="center" valign="middle" >4.87E−09</td><td align="center" valign="middle" >9.74E−11</td><td align="center" valign="middle" >10</td><td align="center" valign="middle" >6.49E−09</td><td align="center" valign="middle" >1.46E−10</td></tr><tr><td align="center" valign="middle" >11</td><td align="center" valign="middle" >6.49E−09</td><td align="center" valign="middle" >1.46E−10</td><td align="center" valign="middle" >11</td><td align="center" valign="middle" >6.49E−09</td><td align="center" valign="middle" >1.14E−10</td></tr><tr><td align="center" valign="middle" >12</td><td align="center" valign="middle" >6.49E−09</td><td align="center" valign="middle" >9.74E−11</td><td align="center" valign="middle" >12</td><td align="center" valign="middle" >8.11E−09</td><td align="center" valign="middle" >9.74E−11</td></tr><tr><td align="center" valign="middle" >13</td><td align="center" valign="middle" >6.49E−09</td><td align="center" valign="middle" >1.30E−10</td><td align="center" valign="middle" >13</td><td align="center" valign="middle" >8.11E−09</td><td align="center" valign="middle" >1.46E−10</td></tr><tr><td align="center" valign="middle" >14</td><td align="center" valign="middle" >8.11E−09</td><td align="center" valign="middle" >9.74E−11</td><td align="center" valign="middle" >14</td><td align="center" valign="middle" >8.11E−09</td><td align="center" valign="middle" >1.46E−10</td></tr><tr><td align="center" valign="middle" >15</td><td align="center" valign="middle" >8.11E−09</td><td align="center" valign="middle" >9.74E−11</td><td align="center" valign="middle" >15</td><td align="center" valign="middle" >8.11E−09</td><td align="center" valign="middle" >9.74E−11</td></tr><tr><td align="center" valign="middle" >16</td><td align="center" valign="middle" >8.11E−09</td><td align="center" valign="middle" >9.74E−11</td><td align="center" valign="middle" >16</td><td align="center" valign="middle" >4.87E−09</td><td align="center" valign="middle" >1.46E−10</td></tr><tr><td align="center" valign="middle" >17</td><td align="center" valign="middle" >6.49E−09</td><td align="center" valign="middle" >9.74E−11</td><td align="center" valign="middle" >17</td><td align="center" valign="middle" >4.87E−09</td><td align="center" valign="middle" >9.74E−11</td></tr><tr><td align="center" valign="middle" >18</td><td align="center" valign="middle" >6.49E−09</td><td align="center" valign="middle" >1.30E−10</td><td align="center" valign="middle" >18</td><td align="center" valign="middle" >4.87E−09</td><td align="center" valign="middle" >1.14E−10</td></tr><tr><td align="center" valign="middle" >19</td><td align="center" valign="middle" >8.11E−09</td><td align="center" valign="middle" >9.74E−11</td><td align="center" valign="middle" >19</td><td align="center" valign="middle" >4.87E−09</td><td align="center" valign="middle" >1.14E−10</td></tr><tr><td align="center" valign="middle" >20</td><td align="center" valign="middle" >8.11E−09</td><td align="center" valign="middle" >9.74E−11</td><td align="center" valign="middle" >20</td><td align="center" valign="middle" >4.87E−09</td><td align="center" valign="middle" >1.14E−10</td></tr><tr><td align="center" valign="middle" >A</td><td align="center" valign="middle" >6.65E−09</td><td align="center" valign="middle" >1.14E−10</td><td align="center" valign="middle" >A</td><td align="center" valign="middle" >6.25E−09</td><td align="center" valign="middle" >1.25E−10</td></tr><tr><td align="center" valign="middle" >S</td><td align="center" valign="middle" >1.38E−09</td><td align="center" valign="middle" >2.13E−11</td><td align="center" valign="middle" >S</td><td align="center" valign="middle" >1.31E−09</td><td align="center" valign="middle" >1.90E−11</td></tr></tbody></table></table-wrap><table-wrap id="table7" ><label><xref ref-type="table" rid="table7">Table 7</xref></label><caption><title> Comparison of the effective coefficients of diffusion during absorption</title></caption><table><tbody><thead><tr><th align="center" valign="middle"  rowspan="2"  >Products</th><th align="center" valign="middle"  rowspan="2"  >Temp</th><th align="center" valign="middle"  colspan="2"  >D<sub>eff</sub> (m&#178;/s)</th><th align="center" valign="middle"  rowspan="2"  >References</th></tr></thead><tr><td align="center" valign="middle" >Initiale phase</td><td align="center" valign="middle" >Final phase</td></tr><tr><td align="center" valign="middle" >CS esp&#232;ce 1</td><td align="center" valign="middle" >23˚C</td><td align="center" valign="middle" >1.10 &#177; 0.23 &#215; 10<sup>−10 </sup></td><td align="center" valign="middle" >1.90 &#177; 0.35 &#215; 10<sup>−12</sup></td><td align="center" valign="middle"  rowspan="2"  >Study case</td></tr><tr><td align="center" valign="middle" >CS esp&#232;ce 2</td><td align="center" valign="middle" >23˚C</td><td align="center" valign="middle" >1.04 &#177; 0.21 &#215; 10<sup>−10</sup></td><td align="center" valign="middle" >2.08 &#177; 0.31 &#215; 10<sup>−12</sup></td></tr><tr><td align="center" valign="middle" >wood afra</td><td align="center" valign="middle"  rowspan="3"  >23˚C</td><td align="center" valign="middle"  colspan="2"  >1.38 &#215; 10<sup>−3</sup></td><td align="center" valign="middle"  rowspan="3"  >[<xref ref-type="bibr" rid="scirp.64789-ref15">15</xref>]</td></tr><tr><td align="center" valign="middle" >wood ojamlesh</td><td align="center" valign="middle"  colspan="2"  >3.71 &#215; 10<sup>−4</sup></td></tr><tr><td align="center" valign="middle" >wood roosi</td><td align="center" valign="middle"  colspan="2"  >4.88 &#215; 10<sup>−4</sup></td></tr><tr><td align="center" valign="middle" >grain of Amaranth</td><td align="center" valign="middle" >23˚C</td><td align="center" valign="middle"  colspan="2"  >[10<sup>−11</sup> - 10<sup>−12</sup>]</td><td align="center" valign="middle" >[<xref ref-type="bibr" rid="scirp.64789-ref16">16</xref>]</td></tr><tr><td align="center" valign="middle" >Grain of rice</td><td align="center" valign="middle" >23˚C</td><td align="center" valign="middle"  colspan="2"  >7 &#215; 10<sup>−10</sup></td><td align="center" valign="middle" >[<xref ref-type="bibr" rid="scirp.64789-ref17">17</xref>]</td></tr><tr><td align="center" valign="middle" >Chickpeas</td><td align="center" valign="middle" >23˚C</td><td align="center" valign="middle"  colspan="2"  >[1.85 &#215; 10<sup>−10</sup> - 1.98 &#215; 10<sup>−10</sup></td><td align="center" valign="middle"  rowspan="2"  >[<xref ref-type="bibr" rid="scirp.64789-ref18">18</xref>]</td></tr><tr><td align="center" valign="middle" >Beans</td><td align="center" valign="middle" >23˚C</td><td align="center" valign="middle"  colspan="2"  >[2.56 &#215; 10<sup>−9</sup> - 8.18 &#215; 10<sup>−11</sup>]</td></tr><tr><td align="center" valign="middle" >Wheatkernel</td><td align="center" valign="middle" >25˚C</td><td align="center" valign="middle"  colspan="2"  >2.8 &#215; 10<sup>−12</sup></td><td align="center" valign="middle" >[<xref ref-type="bibr" rid="scirp.64789-ref19">19</xref>]</td></tr><tr><td align="center" valign="middle" >chestnuts</td><td align="center" valign="middle" >40˚C</td><td align="center" valign="middle" >0.98 &#177; 0.037 &#215; 10<sup>−8</sup></td><td align="center" valign="middle" >0.96 &#177; 1.85 &#215; 10<sup>−8 </sup></td><td align="center" valign="middle" >[<xref ref-type="bibr" rid="scirp.64789-ref20">20</xref>]</td></tr><tr><td align="center" valign="middle" >Food paste</td><td align="center" valign="middle" >23˚C</td><td align="center" valign="middle" >5.69 &#215; 10<sup>−11</sup></td><td align="center" valign="middle" >4.20 &#215; 10<sup>−11</sup></td><td align="center" valign="middle" >[<xref ref-type="bibr" rid="scirp.64789-ref21">21</xref>]</td></tr><tr><td align="center" valign="middle" >fiber of hemp</td><td align="center" valign="middle" ></td><td align="center" valign="middle" >5.29 &#215; 10<sup>−12</sup></td><td align="center" valign="middle" >5.80 &#215; 10<sup>−13</sup></td><td align="center" valign="middle"  rowspan="4"  >[<xref ref-type="bibr" rid="scirp.64789-ref22">22</xref>]</td></tr><tr><td align="center" valign="middle" >jute fiber</td><td align="center" valign="middle" ></td><td align="center" valign="middle" >2.33 &#215; 10<sup>−12</sup></td><td align="center" valign="middle" >2.30 &#215; 10<sup>−13</sup></td></tr><tr><td align="center" valign="middle" >flax fiber</td><td align="center" valign="middle" >23˚C</td><td align="center" valign="middle" >2.11 &#215; 10<sup>−12</sup></td><td align="center" valign="middle" >2.11 &#215; 10<sup>−13</sup></td></tr><tr><td align="center" valign="middle" >fiber of sisal</td><td align="center" valign="middle" ></td><td align="center" valign="middle" >4.00 &#215; 10<sup>−12</sup></td><td align="center" valign="middle" >4.38 &#215; 10<sup>−13</sup></td></tr><tr><td align="center" valign="middle" >fiber of Okra</td><td align="center" valign="middle"  rowspan="2"  >23˚C</td><td align="center" valign="middle"  colspan="2"  >5.40 &#215; 10<sup>−10</sup></td><td align="center" valign="middle"  rowspan="2"  >[<xref ref-type="bibr" rid="scirp.64789-ref23">23</xref>]</td></tr><tr><td align="center" valign="middle" >nut fiber of b&#233;tel</td><td align="center" valign="middle"  colspan="2"  >80 &#215; 10<sup>−10</sup></td></tr></tbody></table></table-wrap></sec></sec><sec id="s4"><title>4. Conclusion</title><p>The shells of two coconut species were separated from nuts and remained at the laboratory in approximate ambient moisture of 60% and at a temperature varying between 20˚C and 23˚C, for two months. Sample was obtained by cutting shells in portion of hollow sphere. Samples were dried in oven and immersed in the distilled water with an aim of studying their absorption kinetics. It was noted that at a temperature of 23˚C &#177; 1˚C, equilibrium content of balance is reached after a period of approximately 35 days in water. The rate of absorption of species 1 is 17.32% &#177; l.06% and that of species 2 is 20.42% &#177; 1.95%. The absorption kinetics of CSs presents two phases: an initial phase with great absorption kinetics in the first 28 minutes; and a final phase for the rest of time. It appeared clearly that the absorption kinetics of the two species is nearly identical. Of the 2 models tested (Peleg and Page), the Page models model very well the experimental data with a coefficient of correlation r<sup>2</sup> &gt; 0.98. The effective coefficients of diffusion obtained starting from the law of Fick: in the initial phase, they are (1.10 &#177; 0.23) &#215; 10<sup>−10</sup> m&#178;/s and (1.04 &#177; 0.21) &#215; 10<sup>−10</sup> m&#178;/s for species 1 and 2 respectively; in the final phase, they are (1.90 &#177; 0.35) &#215; 10<sup>−12</sup> m&#178;/s and (2.08 &#177; 0.31) &#215; 10<sup>−12</sup> m&#178;/s for species 1 and 2 respectively.</p></sec><sec id="s5"><title>Acknowledgements</title><p>Thanks are due to the Head of the Civil Engineering Department of Fotso Victor University Institute of Technology for his help in various stages of the experimental work.</p></sec><sec id="s6"><title>Cite this paper</title><p>Dieunedort Ndapeu,Eb&#233;nezer Njeugna,Nicod&#232;me Rodrigue Sikame,Sophie Brogly Bistac,Jean Yves Drean,M&#233;dard Fogue, (2016) Experimental Study of the Water Absorption Kinetics of the Coconut Shells (Nucifera) of Cameroun. Materials Sciences and Applications,07,159-170. doi: 10.4236/msa.2016.73016</p></sec><sec id="s7"><title>NOTES</title></sec></body><back><ref-list><title>References</title><ref id="scirp.64789-ref1"><label>1</label><mixed-citation publication-type="other" xlink:type="simple">Saikia, D. (2010) Studies of Water Absorption Behavior of Plant Fibers at Different Temperatures. International Journal of Thermophysics, 31, 1020-1026. http://dx.doi.org/10.1007/s10765-010-0774-0</mixed-citation></ref><ref id="scirp.64789-ref2"><label>2</label><mixed-citation publication-type="other" xlink:type="simple">Célino, A., Fréour, S., Jacquemin, F. and Casari, P. (2013) Characterization and Modeling of the Moisture Diffusion Behavior of Natural Fibers. 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