<?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">WJNST</journal-id><journal-title-group><journal-title>World Journal of Nuclear Science and Technology</journal-title></journal-title-group><issn pub-type="epub">2161-6795</issn><publisher><publisher-name>Scientific Research Publishing</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.4236/wjnst.2016.63017</article-id><article-id pub-id-type="publisher-id">WJNST-68137</article-id><article-categories><subj-group subj-group-type="heading"><subject>Articles</subject></subj-group><subj-group subj-group-type="Discipline-v2"><subject>Engineering</subject><subject> Physics&amp;Mathematics</subject></subj-group></article-categories><title-group><article-title>
 
 
  Measurement of Natural Radioactivity and Radon Exhalation Rate in Coal Ash Samples from a Thermal Power Plant
 
</article-title></title-group><contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Aziz</surname><given-names>Boukhair</given-names></name><xref ref-type="aff" rid="aff1"><sup>1</sup></xref><xref ref-type="corresp" rid="cor1"><sup>*</sup></xref></contrib><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Laila</surname><given-names>Belahbib</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>Khadija</surname><given-names>Azkour</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>Hamid</surname><given-names>Nebdi</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>Mohammed</surname><given-names>Benjelloun</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>Abdelmjid</surname><given-names>Nourreddine</given-names></name><xref ref-type="aff" rid="aff4"><sup>4</sup></xref></contrib></contrib-group><aff id="aff2"><addr-line>Centre Régional des Métiers de l’Education et de la Formation, El Jadida, Morocco</addr-line></aff><aff id="aff3"><addr-line>Ministère de l’Intérieur, Secrétariat général, Province d’El Jadida, Morocco</addr-line></aff><aff id="aff4"><addr-line>Groupe RaMsEs, Institut Pluridisciplinaire Hubert Curien (IPHC), Université de Strasbourg, Strasbourg, France</addr-line></aff><aff id="aff1"><addr-line>Laboratoire de Physique Nucléaire, Atomique et Moléculaire, Département de Physique, Faculté des Sciences Université Chouaib Doukkali, El Jadida, Morocco</addr-line></aff><author-notes><corresp id="cor1">* E-mail:<email>mouad.boukhair@gmail.com(AB)</email>;</corresp></author-notes><pub-date pub-type="epub"><day>09</day><month>07</month><year>2016</year></pub-date><volume>06</volume><issue>03</issue><fpage>153</fpage><lpage>160</lpage><history><date date-type="received"><day>3</day>	<month>June</month>	<year>2016</year></date><date date-type="rev-recd"><day>accepted</day>	<month>8</month>	<year>July</year>	</date><date date-type="accepted"><day>11</day>	<month>July</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>
 
 
  Coal is the main energy source for electricity generation in the world. In Morocco, 37% of electricity generation comes from combustion coal in thermal power plants. This combustion process generates large amounts of fly and bottom ashes. In recent years, these ashes became a great topic of interest be
  cause of their different uses and especially in construction materials. In this work, we a
  ssess radiation risks due to natural radioactivity in samples of fly and bottom ashes collected f
  rom JLEC (Jorf Lasfar Energy Company) thermal power plant, and different analyses are performed through two nuclear techniques such as gamma spectrometry and alpha dosimetry based on the use of LR115 films detectors. Our analysis shows that 
  <sup>226</sup>Ra activities and 
  <sup>232</sup>Th in both ash samples are well above the permissible activity. The values of the external risk index (H
  <sub>ex</sub>) and internal o
  ne (H<sub>in</sub>) for these ashes are below unity, with the exception of 1.28 in fly ash for H
  <sub>in</sub>. The 
  obtained values for the equivalent radium Ra<sub>eq</sub> and annual effective doses &amp;#278; in fly and bottom 
  ashes are 324 Bq/kg and 210 Bq/kg, and 0.18 mSv/y and 0.11 mSv/y, respectively. The surface 
  radon exhalation rates for the samples of fly and bottom ashes are 276 mBq&amp;sdot;m<sup>-2</sup>&amp;sdot;h<sup>-1</sup> and 381 
  mBq&amp;sdot;m<sup>-2</sup>&amp;sdot;h<sup>-1</sup>, respectively. Based on these results, we have shown that fly ash and bottom one from thermal power plant JLEC didn’t have, in any case, a health risk to the public so it can be effectively used in various construction activities.
 
</p></abstract><kwd-group><kwd>Natural Radioactivity</kwd><kwd> Gamma Spectrometry</kwd><kwd> LR115</kwd><kwd> Fly Ash</kwd><kwd> Bottom Ash</kwd><kwd> Equivalent Radium</kwd><kwd>  Annual Effective Doses</kwd><kwd> Exhalation of Radon</kwd></kwd-group></article-meta></front><body><sec id="s1"><title>1. Introduction</title><p>The socio-economic development of Morocco and the major projects being initiated in all sectors, particularly the global rural electrification program, contributed strongly to increase the national request of energy. The main source of energy for the electricity production comes from the coal combustion in thermal power plants [<xref ref-type="bibr" rid="scirp.68137-ref1">1</xref>] . This combustion generates large amounts of solid residues such as fly and bottom ashes. The radioactivity content of different mineral coal is very heterogeneous and varies depending on their origin. Generally, coal contains radionuclides with activity ranging from 30 to 100 Bq/kg, 10 to 600 Bq/kg and 10 to 200 kg/Bq, for <sup>40</sup>K, <sup>238</sup>U and <sup>232</sup>Th, respectively [<xref ref-type="bibr" rid="scirp.68137-ref2">2</xref>] . The specific activity of the coal ash can reach three to five times higher than the original one. This is called Technologically Enhanced Naturally Occurring Radioactive Materials (TENORM). While the levels of radioactivity of these ashes remain moderate, a prolonged exposure may become significant when large quantities of these ashes are landfilled or recycled in building materials. The use of coal ashes has economic advantages but can affect the doses received by the human being indoors. Indeed, this use increases the external and internal radiations due to inhalation or ingestion of radon and its descendants [<xref ref-type="bibr" rid="scirp.68137-ref3">3</xref>] .</p><p>Radon-222 is the most commonly measured because of its relatively long period (3.824 d). It is an odorless natural radioactive gas, and is the main source of radiation exposure for humans. Its contribution is estimated at more than half of the average annual dose after natural radioactivity received by the population [<xref ref-type="bibr" rid="scirp.68137-ref4">4</xref>] . In 1987, the International Agency for Research on Cancer (IARC) of the World Health Organization (WHO) recognized radon as lung human carcinogen [<xref ref-type="bibr" rid="scirp.68137-ref5">5</xref>] .</p><p>In the present work, we assess the radiation hazards due to natural radioactivity in coal ash from radionuclides of three chains of radioactive decay (<sup>238</sup>U, <sup>235</sup>U and <sup>232</sup>Th) and <sup>40</sup>K, calculations of external hazard index (H<sub>ex</sub>) and internal one (H<sub>in</sub>), the equivalent radium (Ra<sub>eq</sub>), the absorbed dose rate (Ḋ), the annual effective dose (Ė) and the radon exhalation rate (E<sub>x</sub>) are performed on samples of fly and bottom ashes delivered by the thermal power plant of Jorf Lasfar Energy Company (JLEC), the first private electricity producer in Morocco.</p></sec><sec id="s2"><title>2. Overview of the Thermal Power Plant of JLEC</title><p>The power plant of JLEC is the largest thermal coal one, independent of Middle East and North Africa. It is the main provider of the National Office of Electricity and Water Supply in Morocco with a total annual production capacity about 2056 MW of electricity [<xref ref-type="bibr" rid="scirp.68137-ref6">6</xref>] . It is located in the port Jorf Lasfar, which is 127 km far from the southwest of Casablanca, on the Atlantic Ocean coast. It occupies an area of 60 hectares and is located on a narrow strip of land between a 60 m cliff height on the East and West Atlantic Ocean as shown in <xref ref-type="fig" rid="fig1">Figure 1</xref>.</p><p>In JLEC thermal power plant, coal combustion generates large masses of solid wastes that exceed 640,000 tons per year. Fly ashes are a majority and are around 500,000 tons per year. And for the bottom ones, the production rate exceeds 50,000 tons per year [<xref ref-type="bibr" rid="scirp.68137-ref7">7</xref>] .</p><disp-formula id="scirp.68137-formula405"><graphic  xlink:href="http://html.scirp.org/file/5-1090301x7.png"  xlink:type="simple"/></disp-formula><p>Today, 80% - 95% of fly ash is valued by some national cement, while the bottom ash continues to be stored in large quarries.</p></sec><sec id="s3"><title>3. Materials and Methods</title><p>In the present work, we evaluate radiation hazards due to natural radioactivity in coal ash from radionuclides of three chains of radioactive decay (<sup>238</sup>U, <sup>235</sup>U and <sup>232</sup>Th) and <sup>40</sup>K. Our analyzes were carried out on samples of fly</p><fig id="fig1"  position="float"><label><xref ref-type="fig" rid="fig1">Figure 1</xref></label><caption><title> The power plant Jorf Lasfar Energy Company (JLEC)</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/5-1090301x8.png"/></fig><p>and bottom ashes delivered by the thermal power plant JLEC using two nuclear techniques: gamma spectrometry for identifying the gamma radio transmitters and quantify their activities, and alpha dosimetry based on quantitative exploitation of Solid-State Nuclear Track Detectors (SSNTD, LR115).</p><p>Before any measures and for homogeneous samples, fly and bottom ashes were dried in stove at 40˚C during 24 hours, then crushed and sieved through a sieve of 100 μm. The sieved samples were packaged in sealed radon containers for at least 4 weeks to establish secular equilibrium corresponding to seven half-lives of <sup>222</sup>Rn.</p><sec id="s3_1"><title>3.1. Samples Activities of Coal Ash</title><p>To measure the natural radioactivity in coal ash, samples of fly and bottom ashes were studied and analyzed by gamma ray spectrometer with Broad Energy Germanium detector (BEGe) at the Multidisciplinary Institute Hubert Curien in Strasbourg, France. This is a Hyper-Pure Germanium planar type HPGe detector associated with a set of electronic modules for the pulse shaping, amplification and storing of pulses delivered during the passage of gamma radiation through the detector. Its area of energy measurement is 30 to 3000 keV with a resolution of 0.633 keV to 122 keV, and 1.934 keV to 1332 keV [<xref ref-type="bibr" rid="scirp.68137-ref8">8</xref>] .</p><p>With regard to energy efficiency and calibration of the BEGe detector, a multi-energy certified standard was analyzed under the same conditions and geometry of the studied samples. This standard contains several emitting radionuclides γ such as <sup>241</sup>Am (60 keV), <sup>109</sup>Cd (88 keV), <sup>57</sup>Co (122, 136 keV) <sup>139</sup>Ce (165 keV), <sup>51</sup>Cr (320 keV) <sup>113</sup>Sn (391 keV), <sup>85</sup>Sr (514 keV), <sup>137</sup>Cs (661 keV), <sup>88</sup>Y (898, 1836 keV) and <sup>60</sup>Co (1173, 1332 keV). The samples of coal ash have been conditioned by SG50 and geometry set during 263000 seconds counting; a little less than 74 hours. Treatment of amplitude spectra was carried out with automatic counting software (Genie 2000) [<xref ref-type="bibr" rid="scirp.68137-ref8">8</xref>] to give directly the activity concentration of each radioactive element present in the sample.</p><p>The radionuclides, in which we are interested, are the radium 226, the thorium 232 and the potassium 40. <sup>226</sup>Ra is difficult to differentiate from <sup>235</sup>U; as they emit photons with very close energies; 186.1 keV and 185.72 keV, respectively, and the interference can be created. The activity of <sup>226</sup>Ra can be performed from the <sup>214</sup>Pb (295 keV and 352 keV rays) and <sup>214</sup>Bi (609 keV, 1120 keV and 1764 keV rays) after establishment of the secular equilibrium between <sup>226</sup>Ra, <sup>222</sup>Rn, <sup>214</sup>Pb and the <sup>214</sup>Bi. <sup>232</sup>Th has a ray at 63.81 keV which has a very low emission probability of 0.263%. This ray interferes with that of <sup>234</sup>Th at 63.28 keV which has a higher transmission probability equal to 4.1%. The determination of <sup>232</sup>Th activity is from the <sup>228</sup>Ac (911 keV and 969 keV rays) and <sup>212</sup>Pb (239 keV ray). Given the short period (56 s) of <sup>220</sup>Rn decay that secular equilibrium is reached quickly for the thorium family. The <sup>40</sup>K is determined from the 1461 keV ray with 10.55% emission intensity.</p></sec><sec id="s3_2"><title>3.2. Surface Radon Exhalation Rate</title><p>In this paragraph, we describe the process and experimental set up used to estimate the radon exhalation rate of ashes samples analyzed by gamma spectrometry. Exhalation is the mechanism which a radon atom produces a gas inside the sample reaching its surface. It groups precisely two steps: the emanation and transport. It is commonly expressed as surface flow exhalation radon (Bq∙m<sup>−2</sup>∙s<sup>−1</sup>). In the laboratory, for samples measurements we use the term of surface radon exhalation rate (Bq∙m<sup>−2</sup>∙h<sup>−1</sup>) [<xref ref-type="bibr" rid="scirp.68137-ref9">9</xref>] - [<xref ref-type="bibr" rid="scirp.68137-ref11">11</xref>] .</p><p>Each amount of sample fly and bottom ashes (50 g) were placed in the cylindrical “cans” as shown in <xref ref-type="fig" rid="fig2">Figure 2</xref>. The Solid-State Nuclear Track Detectors (SSNTD) LR115 type II non strippable (2 &#215; 2 cm<sup>2</sup>) was fixed on the top inside of the “can”.</p><p>These films badges are LR115 type nuclear track ones produced by KODAK and they consist of a 100 &#181;m thick polyester substrate coated with a 12 &#181;m thick layer of red colored cellulose nitrate (C<sub>6</sub>H<sub>8</sub>N<sub>2</sub>O<sub>9</sub>). It can record energy particles between 1.4 and 4.7 MeV with an incidence angle up to 50˚. Alpha particles traverse the detector leaving various holes with diameters depending to the incident energy. After two months of irradiation, the LR115 was chemically treated in 2.5 N sodium hydroxide solution (NaOH) at 60˚C for time periods of 100 min. An optical microscope was used to read the developed films.</p><p>The density of traces per unit area and per unit time D<sub>LR</sub> in the LR115 and the volumetric activity of radon <inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/5-1090301x9.png" xlink:type="simple"/></inline-formula> are related by the following relationship:</p><disp-formula id="scirp.68137-formula406"><label>(1)</label><graphic position="anchor" xlink:href="http://html.scirp.org/file/5-1090301x10.png"  xlink:type="simple"/></disp-formula><p>where <inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/5-1090301x11.png" xlink:type="simple"/></inline-formula> is the efficiency of detection based on the critical recording angle<inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/5-1090301x12.png" xlink:type="simple"/></inline-formula>, and the energy of the alpha particle <inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/5-1090301x13.png" xlink:type="simple"/></inline-formula> calculated numerically [<xref ref-type="bibr" rid="scirp.68137-ref12">12</xref>] . This efficiency is equal to 0.0258 (traces∙cm<sup>−2</sup>∙d<sup>−1</sup>/Bq∙m<sup>−3</sup>).</p><p>Exhalation rate <sup>222</sup>Rn is obtained from the following expression [<xref ref-type="bibr" rid="scirp.68137-ref13">13</xref>] [<xref ref-type="bibr" rid="scirp.68137-ref14">14</xref>] :</p><disp-formula id="scirp.68137-formula407"><label>(2)</label><graphic position="anchor" xlink:href="http://html.scirp.org/file/5-1090301x14.png"  xlink:type="simple"/></disp-formula><p>where E<sub>X</sub> is measured in (Bq∙m<sup>−2</sup>∙h<sup>−1</sup>); <inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/5-1090301x15.png" xlink:type="simple"/></inline-formula>is the volumetric activity of radon (Bq∙m<sup>−3</sup>∙h); <inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/5-1090301x16.png" xlink:type="simple"/></inline-formula>is the decay constant for radon (h<sup>−1</sup>); S<sub>e</sub> is the sample surface (m<sup>2</sup>); V is the effective volume of can (m<sup>3</sup>) and t is the exposure time (h).</p><fig id="fig2"  position="float"><label><xref ref-type="fig" rid="fig2">Figure 2</xref></label><caption><title> Diagram dosimeter to measure the exhalation of radon in samples of coal ash at thermal power plant JLEC</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/5-1090301x17.png"/></fig></sec><sec id="s3_3"><title>3.3. Evaluation of the Radiological Effects and Dose Estimation</title><p>In recent years, fly and bottom ashes have become a topic of great interest in the world because of the diversity of their uses in building materials. For this purpose, to evaluate the radiological hazards of fly and bottom ashes from the thermal power plant JLEC due to non-uniform distribution of radionuclides in the samples of coal ash, the UNSCEAR 2000 report [<xref ref-type="bibr" rid="scirp.68137-ref15">15</xref>] offers templates to define some dosimetric quantities such as radium equivalent, the index of internal/external hazard, the flow of the absorbed dose and the annual effective dose. Certain limits not to be exceeded are recommended.</p><sec id="s3_3_1"><title>3.3.1. Radium Equivalent Ra<sub>eq</sub></title><p>To represent the level of activity of <sup>226</sup>Ra, <sup>232</sup>Th and <sup>40</sup>K by a single quantity, a common radiological index was introduced. This index is known as the equivalent radium activity symbolized by Ra<sub>eq</sub> and calculated using the following expression:</p><disp-formula id="scirp.68137-formula408"><label>(3)</label><graphic position="anchor" xlink:href="http://html.scirp.org/file/5-1090301x18.png"  xlink:type="simple"/></disp-formula><p>This relationship is obtained by considering that the activities 1 Bq/kg of <sup>226</sup>Ra, 0.7 Bq/kg of <sup>232</sup>Th and 13 Bq/kg of <sup>40</sup>K produce the same dose of gamma rays [<xref ref-type="bibr" rid="scirp.68137-ref16">16</xref>] [<xref ref-type="bibr" rid="scirp.68137-ref17">17</xref>] .</p><p>It should be noted that the maximum value of the activity of radium equivalent in construction materials must be less than 370 Bq/kg.</p></sec><sec id="s3_3_2"><title>3.3.2. Internal and External Hazard Indices</title><p>The hazard indices are defined by a model taking into account the maximum activity of Ra<sub>eq</sub> (370 Bq/kg). The H<sub>ex</sub> external hazard index is given by:</p><disp-formula id="scirp.68137-formula409"><label>. (4)</label><graphic position="anchor" xlink:href="http://html.scirp.org/file/5-1090301x19.png"  xlink:type="simple"/></disp-formula><p>In addition to the external hazard, the respiratory organs are threatened because of the disintegration of <sup>226</sup>Ra and <sup>222</sup>Rn and their descendants. The maximum permissible activity for <sup>226</sup>Ra has been reduced in half the value of 185 Bq/kg. The internal hazard H<sub>in</sub> must be quantified:</p><disp-formula id="scirp.68137-formula410"><label>. (5)</label><graphic position="anchor" xlink:href="http://html.scirp.org/file/5-1090301x20.png"  xlink:type="simple"/></disp-formula><p>The maximum value of each index is tolerable with the unit value for the upper limit of Ra<sub>eq</sub>.</p></sec><sec id="s3_3_3"><title>3.3.3. Absorbed Dose Rate and Annual Effective Dose</title><p>The absorbed dose rate Ḋ (nGy/h) from natural radionuclides in the air at 1m height is defined by expression (6):</p><disp-formula id="scirp.68137-formula411"><label>. (6)</label><graphic position="anchor" xlink:href="http://html.scirp.org/file/5-1090301x21.png"  xlink:type="simple"/></disp-formula><p>The received dose by the population is called annual effective dose, it calculated by the following equation:</p><disp-formula id="scirp.68137-formula412"><label>. (7)</label><graphic position="anchor" xlink:href="http://html.scirp.org/file/5-1090301x22.png"  xlink:type="simple"/></disp-formula><p>The annual effective dose rates should be obtained to test the health effect of those absorbed dose rates. In order to estimate the annual effective doses, one has to take into account to conversion coefficient from absorbed dose in air to effective and the outdoor occupancy factor. In the UNSCEAR reports [<xref ref-type="bibr" rid="scirp.68137-ref15">15</xref>] , a value of 0.7 Sv/Gy was used for the conversion coefficient from absorbed dose in air to effective dose received by adults and 0.2 for the outdoor occupancy factor.</p></sec></sec></sec><sec id="s4"><title>4. Results and Discussion</title><p>The specific activities of radionuclides <sup>226</sup>Ra, <sup>232</sup>Th and <sup>40</sup>K were determined by gamma spectrometry in samples of fly and bottom ashes from thermal power plant JLEC and other thermal plants of some European countries are regrouped in <xref ref-type="table" rid="table1">Table 1</xref>.</p><p>According to the qualitative analysis of spectra obtained for both samples of fly and bottom ashes, we find practically all radionuclides of natural radioactive families (<sup>238</sup>U, <sup>232</sup>Th, <sup>235</sup>U and <sup>40</sup>K).</p><p>By examining the results in <xref ref-type="table" rid="table1">Table 1</xref>, the first observation is that the specific activities of elements <sup>226</sup>Ra, <sup>232</sup>Th and <sup>40</sup>K in the sample of fly ash are higher compared to those found in the bottom ash with factors of 2.07, 1.77 and 1.32 for <sup>40</sup>K, <sup>226</sup>Ra and <sup>232</sup>Th, respectively.</p><p>The activities of <sup>226</sup>Ra and <sup>232</sup>Th in both ash samples are well above the permissible activity which is in the order of 40 Bq/kg, while the activity of <sup>40</sup>K is less than 370 Bq/kg [<xref ref-type="bibr" rid="scirp.68137-ref15">15</xref>] even if the activity of <sup>40</sup>K (348 Bq/kg) in the sample of fly ash is very close to the eligible activity.</p><p>The levels of <sup>226</sup>Ra, <sup>232</sup>Th and <sup>40</sup>K measured in our samples of coal ash from thermal power plant JLEC are comparable to those found in other thermal power plants in Europe.</p><p><xref ref-type="table" rid="table2">Table 2</xref> shows that the values of Ra<sub>eq</sub>, H<sub>ex</sub> and H<sub>in</sub> in fly ash and bottom ash are below the maximum values defined by the UNSCEAR 2000 report [<xref ref-type="bibr" rid="scirp.68137-ref15">15</xref>] , except for the value of the H<sub>in</sub> (1.28) in fly ash that remains a little higher than the unit.</p><p>The absorbed gamma dose rates measured in the samples of fly and bottom ashes are of the order of 146 nGy/h and 93 nGy/h, respectively. After conversion of these values, the annual effective dose of these samples of fly and bottom ashes are on the order of 0.18 mSv/y and 0.11 mSv/y, respectively. Those values not exceeding the annual effective dose limit set of 1 mSv/y.</p><p>The results presented in <xref ref-type="table" rid="table3">Table 3</xref> show that the values of activity concentrations of radon and the rate of surface exhalation in the bottom ash samples are higher than those of the samples of fly ash. The exhalation of radon levels in coal ash samples are below the world average (57.6 Bq∙m<sup>−2</sup>∙h<sup>−1</sup>) [<xref ref-type="bibr" rid="scirp.68137-ref15">15</xref>] . These results agree with those found by other authors (<xref ref-type="table" rid="table3">Table 3</xref>).</p><table-wrap id="table1" ><label><xref ref-type="table" rid="table1">Table 1</xref></label><caption><title> The specific activities of <sup>226</sup>Ra, <sup>232</sup>Th and <sup>40</sup>K obtained for fly ash (FA) and bottom ash (BA) compared to other works</title></caption><table><tbody><thead><tr><th align="center" valign="middle"  rowspan="2"  >Thermal Power Plants</th><th align="center" valign="middle"  rowspan="2"  >Sample</th><th align="center" valign="middle"  colspan="3"  >Activity in Bg/kg</th></tr></thead><tr><td align="center" valign="middle" ><sup>226</sup>Ra</td><td align="center" valign="middle" ><sup>232</sup>Th</td><td align="center" valign="middle" ><sup>40</sup>K</td></tr><tr><td align="center" valign="middle"  rowspan="2"  >JLEC-Morocco (Present Study)</td><td align="center" valign="middle" >FA</td><td align="center" valign="middle" >149 &#177; 26</td><td align="center" valign="middle" >104 &#177; 18</td><td align="center" valign="middle" >348 &#177; 47</td></tr><tr><td align="center" valign="middle" >BA</td><td align="center" valign="middle" >84 &#177; 16</td><td align="center" valign="middle" >79 &#177; 15</td><td align="center" valign="middle" >168 &#177; 30</td></tr><tr><td align="center" valign="middle"  rowspan="2"  >Serbia (2011) [<xref ref-type="bibr" rid="scirp.68137-ref18">18</xref>]</td><td align="center" valign="middle" >FA</td><td align="center" valign="middle" >120</td><td align="center" valign="middle" >72</td><td align="center" valign="middle" >360</td></tr><tr><td align="center" valign="middle" >BA</td><td align="center" valign="middle" >65</td><td align="center" valign="middle" >39</td><td align="center" valign="middle" >241</td></tr><tr><td align="center" valign="middle"  rowspan="2"  >Spain (2009) [<xref ref-type="bibr" rid="scirp.68137-ref19">19</xref>]</td><td align="center" valign="middle" >FA</td><td align="center" valign="middle" >191 &#177; 9</td><td align="center" valign="middle" >74 &#177; 3</td><td align="center" valign="middle" >306 &#177; 13</td></tr><tr><td align="center" valign="middle" >BA</td><td align="center" valign="middle" >149 &#177; 6</td><td align="center" valign="middle" >66 &#177; 3</td><td align="center" valign="middle" >235 &#177; 11</td></tr><tr><td align="center" valign="middle"  rowspan="2"  >Turkey (2008) [<xref ref-type="bibr" rid="scirp.68137-ref20">20</xref>]</td><td align="center" valign="middle" >FA</td><td align="center" valign="middle" >149 &#177; 2</td><td align="center" valign="middle" >58 &#177; 4</td><td align="center" valign="middle" >94 &#177; 28</td></tr><tr><td align="center" valign="middle" >BA</td><td align="center" valign="middle" >50 &#177; 1</td><td align="center" valign="middle" >25 &#177; 2</td><td align="center" valign="middle" >376 &#177; 9</td></tr><tr><td align="center" valign="middle"  rowspan="2"  >Greece (2004) [<xref ref-type="bibr" rid="scirp.68137-ref21">21</xref>]</td><td align="center" valign="middle" >FA</td><td align="center" valign="middle" >904 &#177; 9</td><td align="center" valign="middle" >53 &#177; 5</td><td align="center" valign="middle" >454 &#177; 11</td></tr><tr><td align="center" valign="middle" >BA</td><td align="center" valign="middle" >662 &#177; 9</td><td align="center" valign="middle" >44 &#177; 5</td><td align="center" valign="middle" >405 &#177; 11</td></tr></tbody></table></table-wrap><table-wrap id="table2" ><label><xref ref-type="table" rid="table2">Table 2</xref></label><caption><title> Radium equivalent Ra<sub>eq</sub>, internal hazard index H<sub>in</sub>, external hazard index H<sub>ex</sub>, absorbed dose rate Ḋ and annual effective dose Ė in ash coal</title></caption><table><tbody><thead><tr><th align="center" valign="middle" >Sample</th><th align="center" valign="middle" >Ra<sub>eq</sub> (Bq/kg)</th><th align="center" valign="middle" >H<sub>ex</sub></th><th align="center" valign="middle" >H<sub>in</sub></th><th align="center" valign="middle" >Ḋ (nGy/h)</th><th align="center" valign="middle" >Ė (mSv/y)</th></tr></thead><tr><td align="center" valign="middle" >Fly Ash</td><td align="center" valign="middle" >324 &#177; 30</td><td align="center" valign="middle" >0.88</td><td align="center" valign="middle" >1.28</td><td align="center" valign="middle" >146 &#177; 9</td><td align="center" valign="middle" >0.18 &#177; 0.01</td></tr><tr><td align="center" valign="middle" >Bottom Ash</td><td align="center" valign="middle" >210 &#177; 28</td><td align="center" valign="middle" >0.57</td><td align="center" valign="middle" >0.79</td><td align="center" valign="middle" >93 &#177; 6</td><td align="center" valign="middle" >0.11 &#177; 0.01</td></tr></tbody></table></table-wrap><table-wrap id="table3" ><label><xref ref-type="table" rid="table3">Table 3</xref></label><caption><title> Experimental results of the volume activity of radon <inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/5-1090301x23.png" xlink:type="simple"/></inline-formula> and the surface exhalation rate E<sub>X</sub> in samples of ash coal JLEC</title></caption><table><tbody><thead><tr><th align="center" valign="middle" >Thermal Plants</th><th align="center" valign="middle" >Sample</th><th align="center" valign="middle" ><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/5-1090301x24.png" xlink:type="simple"/></inline-formula>(Bq/m<sup>3</sup>)</th><th align="center" valign="middle" >E<sub>X</sub> (mBq∙m<sup>−</sup><sup>2</sup>∙h<sup>−</sup><sup>1</sup>)</th></tr></thead><tr><td align="center" valign="middle"  rowspan="2"  >JLEC-Morocco (Our Study)</td><td align="center" valign="middle" >FA</td><td align="center" valign="middle" >337 &#177; 27</td><td align="center" valign="middle" >276 &#177; 22</td></tr><tr><td align="center" valign="middle" >BA</td><td align="center" valign="middle" >465 &#177; 38</td><td align="center" valign="middle" >381 &#177; 31</td></tr><tr><td align="center" valign="middle" >India (2013) [<xref ref-type="bibr" rid="scirp.68137-ref22">22</xref>]</td><td align="center" valign="middle" >FA</td><td align="center" valign="middle" >431.70 &#177; 35.50</td><td align="center" valign="middle" >155.00 &#177; 12.8</td></tr><tr><td align="center" valign="middle" >India (2010) [<xref ref-type="bibr" rid="scirp.68137-ref23">23</xref>]</td><td align="center" valign="middle" >FA</td><td align="center" valign="middle" >214 to 590</td><td align="center" valign="middle" >138 to 381</td></tr></tbody></table></table-wrap></sec><sec id="s5"><title>5. Conclusions</title><p>In this study, we assess radiation risks due to natural radioactivity in fly and bottom ashes from thermal power plant of JLEC. For this ending, we measured the natural radioactivity in these samples using gamma spectrometry technique. The activities of <sup>226</sup>Ra and <sup>232</sup>Th in both ashes samples are well above the permissible activity, which is on the order of 40 Bq/kg, while the <sup>40</sup>K activity is less than 370 Bq/kg. Based on the models proposed by the UNSCEAR, our analyses reveal that H<sub>ex</sub> and H<sub>in</sub> values for fly and bottom ashes are below the standard value, except for the one of H<sub>in</sub> (1.28) in the fly ash, which is a little more than unity. The values obtained for the equivalent radium and annual effective doses of the fly and bottom ashes are (324 Bq/kg and 210 Bq/kg) and (0.18 mSv/y and 0.11 mSv/y), respectively. These values do not exceed the recommended limits which are 370 Bq/kg and 1 mSv/y, respectively.</p><p>To estimate the Exhalation of radon levels in coal ash, we used the alpha dosimetry based on quantitative exploitation of LR115 detector. Exhalation rates found for samples of fly and bottom ashes are 276 mBq∙m<sup>−2</sup>∙h<sup>−1</sup> and 381 mBq∙m<sup>−2</sup>∙h<sup>−1</sup>, respectively; these values remain below the eligible limit (57.6 Bq∙m<sup>−2</sup>∙h<sup>−1</sup>).</p><p>During our work, we find that the results for our samples of coal ash from thermal power plant JLEC are comparable to those obtained in other countries.</p><p>Based on the above results, we can conclude that the fly and bottom ashes from thermal power plant of JLEC can be classified in the category of products exempt from any usage restrictions. Therefore, these coal ashes did not present, in any case, a health risk to the public and can be effectively used in various construction activities.</p></sec><sec id="s6"><title>Cite this paper</title><p>Aziz Boukhair,Laila Belahbib,Khadija Azkour,Hamid Nebdi,Mohammed Benjelloun,Abdelmjid Nourreddine, (2016) Measurement of Natural Radioactivity and Radon Exhalation Rate in Coal Ash Samples from a Thermal Power Plant. 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