<?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.2013.32009</article-id><article-id pub-id-type="publisher-id">WJNST-30782</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>
 
 
  Neutron Induced Fission Track Estimation of Uranium Concentration and Its Associated Health Hazards in Drinking Water of the Faisalabad Industrial City
 
</article-title></title-group><contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>.</surname><given-names>Akram</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>Muddasir</surname><given-names>Nazar</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>A.</surname><given-names>Ghaffar</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>F.</surname><given-names>Malik</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>N.</surname><given-names>Ali</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>S.</surname><given-names>A. Mujahid</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>M.</surname><given-names>U. Rajput</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>Matiullah</surname><given-names>&amp;nbsp</given-names></name><xref ref-type="aff" rid="aff1"><sup>1</sup></xref></contrib></contrib-group><aff id="aff1"><addr-line>Physics Division, PINSTECH, Islamabad, Pakistan</addr-line></aff><aff id="aff2"><addr-line>Department of Physics, University of Agriculture, Faisalabad, Pakistan</addr-line></aff><author-notes><corresp id="cor1">* E-mail:<email>akram1662@gmail.com(.A)</email>;</corresp></author-notes><pub-date pub-type="epub"><day>30</day><month>04</month><year>2013</year></pub-date><volume>03</volume><issue>02</issue><fpage>51</fpage><lpage>58</lpage><history><date date-type="received"><day>August</day>	<month>9,</month>	<year>2012</year></date><date date-type="rev-recd"><day>January</day>	<month>16,</month>	<year>2013</year>	</date><date date-type="accepted"><day>February</day>	<month>3,</month>	<year>2013</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>
 
 
   Drinking water plays a major role regarding quality of human life because polluted water is the main cause of many types of diseases. Besides other pollutants, high concentration of uranium above a certain level in drinking water is also hazardous. As water and food are the main sources of uranium intake, it is absolutely imperative that their level of concentrations is monitored regularly for safety of the general public. In this regard, trace amount of uranium in drinking water samples collected from different locations of Faisalabadcity has been carried out using Neutron Induced Fission Track Technique. The water samples along with the standard of known uranium concentration were poured and dried over Lexan track detectors and then irradiated with thermal neutrons in Reactor. After etching, the tracks produced in the detectors as a result of <sup>235</sup>U (n, f) reaction were counted under an optical microscope. The uranium concentration was determined by counting and comparing the observed fission track density in the samples and the standard. The observed uranium concentration in the studied water samples varied from (1.04 &#177; 0.30) μg&#183;L<sup>-1</sup> to (21.08 &#177; 2. 95) μg&#183;L<sup>-1</sup> with an average value of (7.39 &#177; 1.30) μg&#183;L<sup>-1</sup> and is found to be within safe limits as far as uranium related health hazards are concerned.  
    
 
</p></abstract><kwd-group><kwd>Drinking Water; Uranium; Fission Tracks; Etching; Health Hazard</kwd></kwd-group></article-meta></front><body><sec id="s1"><title>1. Introduction</title><p>Uranium is a radioactive element found in nature discovered by Martin Heinrich Klaprothe in 1789. It has three isotopes namely, <sup>234</sup>U (0.0055%), <sup>235</sup>U (0.720%) and <sup>238</sup>U (99.2745%), all of which are long-lived alpha emitters. It can be present in almost all soil, minerals, rocks, sand, plants food and water in the varying proportions due to their natural occurrences or introduced by the activities of human [<xref ref-type="bibr" rid="scirp.30782-ref1">1</xref>]. The average uranium concentration in the earth’s crust has been reported to be 4 ppm by weight while in the phosphate rocks its value may be as high as 120 ppm by weight [<xref ref-type="bibr" rid="scirp.30782-ref2">2</xref>].</p><p>Uranium and its salts are highly toxic and may exist in the +2, +3, +4, +5 or +6 valence states. The most prevalent are the hexavalent and tetravalent states states [<xref ref-type="bibr" rid="scirp.30782-ref1">1</xref>]. The hexavalent state is particularly important in water and other food items because almost all tetravalent compounds are insoluble. Besides other pollutants, water also contains trace amount of uranium which may find its way right to the human food [<xref ref-type="bibr" rid="scirp.30782-ref3">3</xref>]. Besides being radioactive, uranium is highly chemically toxic thereby resulting in health hazards if exceeds certain limits.</p><p>Uranium may enter into drinking water or food chain from naturally-occurring deposits by leaching processes or as a result of human activity, such as mining and milling [<xref ref-type="bibr" rid="scirp.30782-ref4">4</xref>]. After it enters into the human body through ingestion, most of the ingested uranium is eliminated from the body. However, a small amount is absorbed and carried through the bloodstream into the kidneys. The ingestion of high values of uranium in drinking water and foodstuffs therefore damages kidneys, preventing normal elimination of urea and other waste products, resulting in renal dysfunction [<xref ref-type="bibr" rid="scirp.30782-ref1">1</xref>]. Therefore, it may be hazardous if inhaled or ingested in excessive quantities [1,5-9]. Water having uranium concentration above the proposed Maximum Acceptable Concentration ranges of 9 - 30 mg∙L<sup>−1</sup> is not safe for drinking purposes as it leads to harmful health effects in humans [10-13]. Studies show that elevated levels of uranium in drinking water can increase a person’s risk of kidney damage. The increased kidney damage/cancer risk depends on the concentration of radioactivity found in the drinking water, the amount of water consumed on a daily basis, and the duration one has consumed the water.</p><p>Uranium has been extensively studied in soil, minerals, rocks, sand, plants, food and water [1,3,9,14-20]. Due to industrialization, most of the drinking water sources have been polluted in industrial cities of Pakistan [21-24]. Hence, the assessment of health risk due to the high concentration of uranium in water is most important. In this context, an industrial city of the Faisalabad city was chosen. Drinking water samples were collected from different locations of the city (see, <xref ref-type="fig" rid="fig1">Figure 1</xref>) and ura-</p><p>nium concentration in these samples were estimated using Neutron Induced Fission Track Technique [2,3,14,15, 18,25,26]. Main objective of this investigation was to save the people from harmful effect of uranium if any because the people of city use this water for drinking and other domestic purposes.</p><p>The Neutron Induced Fission Track Technique has been applied for determination of uranium in solid and liquid samples by many workers [3,14,15,18,27,28]. This technique is based on using <sup>235</sup>U (n, f) reaction whose fission cross-section is 4.2 barns for thermal neutron. The basic principle of the technique is that in natural uranium, only <sup>235</sup>U is fissionable by thermal neutrons. Hence, if a drop of unknown liquid sample and standard of known uranium, dried on nuclear track detectors, irradiate simultaneously by the same integrated flux of thermal neutrons in the reactor, the uranium content in the unknown sample is calculated after chemical etching by counting and comparing the total number of observed fission tracks produced in the detectors due to uranium in the samples and standard as a result of (n, f) nuclear reaction in the reactor (<xref ref-type="fig" rid="fig2">Figure 2</xref>).</p></sec><sec id="s2"><title>2. Materials and Methods</title><p>In this study, twenty eight water samples of different sources were collected from different locations of the Faisalabad city in 500 ml plastic bottles as shown in <xref ref-type="table" rid="table1">Table 1</xref>. From each bottle 250 ml water was taken into a conical flask and was heated on a hot plate until 5 ml concentrated solution was left behind. All the water samples were concentrated one by one and kept separately in glass bottles. Standard solution of uranium was also prepared from uranium oxide (having certified composition of 99.94% U<sub>3</sub>O<sub>8</sub>). After concentration, most widely used plastic detector material for recording fission particles namely Lexan (C<sub>16</sub>H<sub>18</sub>O<sub>3</sub>) with trade name of Lexan<sup>&#210;</sup></p><p><xref ref-type="table" rid="table1">Table 1</xref>. Results of uranium contents in water samples from different localities of Faisalabad city, Pakistan (&#181;g∙L<sup>−1</sup>).</p><disp-formula id="scirp.30782-formula72989"><graphic  xlink:href="3-1090078\091f4750-5f7e-43ed-923c-0023dddf55a2.jpg"  xlink:type="simple"/></disp-formula><p><sup>*</sup>Statistical counting error = 1 SD.</p><p>(supplied by General Electric Company, USA) having 125 mm thickness was cut into small pieces each of size 1 cm &#215; 1 cm. A drop of 0.05 ml of concentrated solution of each water sample and standard were taken separately with the help of an accurately calibrated micropipette and poured over the surfaces of the sensitive face of the Lexan detectors. After drying the drop over the surfaces of the Lexan<sup>&#210;</sup> detectors, the solid residue left behind on each detector was then covered with another Lexan detector of the same size so as to sandwich the residues. The procedure was repeated for every sample.</p><p>The Lexan<sup>&#210;</sup> detector assemblies (<xref ref-type="fig" rid="fig3">Figure 3</xref>) along with one blank Lexan<sup>&#210;</sup> detector (for background) were irradiated simultaneously with thermal neutrons in the Pakistan Research Reactor-I (PARR-1), PINSTECH, Islamabad, with thermal neutrons for 100 seconds under a thermal neutron flux of the order of 10<sup>15</sup> neutrons cm<sup>−2</sup>∙s<sup>−</sup><sup>1</sup>. After irradiation, the detectors were etched in 6.5 M NaOH solution for 45 minutes at 50˚C &#177; 1˚C in etching bath. After etching, the fission tracks produced in the water drop area of all the etched detectors due to uranium were counted using Zeiss optical microscope at a magnification of 400&#215;.</p><p>In order to determine uranium concentration in water, the observed track densities in water samples were related to the track density obtained in the standard of known uranium concentration. Because both the sample and the standard were irradiated and etched under similar conditions, the uranium concentration relative to a 10<sup>4</sup> mg∙L<sup>−1</sup> standard uranium solution was calculated by the relation [3,14,15,18,28]:</p><p><img src="3-1090078\8e02646a-fc61-4bc4-87e6-da3ea329b2eb.jpg" /></p><p>where the subscripts x and s stand for unknown and standard sample respectively. In the above relation, C is the uranium concentration, ρ is the track density, I is the isotopic abundance ratio of <sup>235</sup>U and <sup>238</sup>U and R is the range of fission fragments in the detector. The quantities R<sub>S</sub>/R<sub>X</sub> and I<sub>S</sub>/I<sub>X</sub> are correction factors applied when the composition of the sample and the standard are different.</p><p>The values of R<sub>S</sub>/R<sub>X</sub> and I<sub>S</sub>/I<sub>X</sub> were assumed to be unity in the present study because the same isotopic abundance ratio and range of fission fragments in the standard and unknown sample having almost same composition.</p></sec><sec id="s3"><title>3. Results and Discussion</title><p>As mentioned earlier, the present study deals with determination of the uranium concentration in drinking water samples using Lexan based neutron Induced Fission Track Technique. The results of measured uranium concentration in each sample along with their sampling sites and sources of water samples collected from different locations of Faisalabad city area are shown in <xref ref-type="table" rid="table1">Table 1</xref>. As the water samples were 50 times concentrated, therefore, the uranium concentrations in the last column of the <xref ref-type="table" rid="table1">Table 1</xref> are divided by 50.</p><p>As may be seen in <xref ref-type="table" rid="table1">Table 1</xref>, the measured uranium concentration in the studied samples ranges from 1.04 &#177; 0.30 &#181;g∙L<sup>−1</sup> to 21.08 &#177; 2.95 &#181;g∙L<sup>−1</sup> with an average value of 7.39 &#177; 1.30 &#181;g∙L<sup>−1</sup>. Uranium concentration in the samples is seen to vary from tube well to tube well, hand pump to hand pump and place to place showing slight variation in the water of the studied area.</p><p>Higher uranium concentration were observed in the water sample collected from Peoples colony −1 (21.08 &#181;gL<sup>−1</sup>), Shadab Colony (19.53 &#181;g∙L<sup>−1</sup>) and Partab Nagar (16.13 &#181;g∙L<sup>−1</sup>), respectively. Although these concentrations were towards higher side but were within the safe limits of 9 - 30 &#181;g∙L<sup>−1 </sup>set by different health agencies of the world [10-13,29,30]. Uranium concentrations in groundwater depend on the mineralogical, geochemical and chemical composition of the soil rock and water. A recent survey found that drinking waters depends on the local geology of the rock and soil, having uranium contents dangerous for consumer health [<xref ref-type="bibr" rid="scirp.30782-ref31">31</xref>]. Although this area of the city was well established having good facilities and infrastructure, the high uranium concentration in these hand pump water samples might be due to the presence of naturally occurring underground uraniumbearing local geological rocks/soil of the area.</p><p>Minimum uranium concentration of 1.04 &#181;g∙L<sup>−1</sup> and 1.44 &#181;g∙L<sup>−1</sup> were found in the water sample collected from the filtration plant of Civil Lines and tube well of the Millat Town, respectively. The people of the area had facility of filtration plant which might be the reason of low value of uranium concentration in the water sample taken from civil lines area. This water was taken from filtration plant (tube well having more depth) which was naturally filtered as well as filtered in the filtration plant to minimize the contaminations. On the other hand, water from tube well of the Millat Town contained lower concentration. This may be due to the fact this water was taken from more depth of tube well. Therefore, it was more safe as for as contaminations are concerned. So water of both these areas was found to be more clean and safe for public use as for as uranium related hazards are concerned.</p><p>During the current study, it was found that about 71% water samples have uranium concentration levels below 10 &#181;g∙L<sup>−1</sup>, while the percentage of the samples containing uranium concentration in the range 10 - 21 &#181;g∙L<sup>−1</sup> was only about 29%.</p><p>The main rocks exposed in the geological formation of the area are sandstone, siltstone shale, conglomerate etc. These rocks generally do not contain high uranium content to pose any health threat but some contribution from these local rocks and soils is expected due to the leaching and weathering processes of the rocks which contain uranium. Contribution from industrial wastes and anthropogenic discharges from sources such as oil and coal power generation plants, wood burning, glass product manufacturing, bleaching agent in detergents, bleaching of clothes, leaching of treated wood/paper, consumer products (e.g., cosmetics, medicines, insecticides), pesticides, copper smelters, fertilizer etc. into the nearby flowing streams might be the other cause of uranium concentration in the underground water aquifer.</p><p><xref ref-type="table" rid="table2">Table 2</xref> shows observed concentration of uranium in water samples from the hand pumps of the Faisalabad city which ranges from 2.54 - 21.08 mg∙L<sup>−1</sup> with an average of 10.09 mg∙L<sup>−1</sup>. Refering back to <xref ref-type="table" rid="table2">Table 2</xref>, the uranium concentration in tube well water ranged from 1.44 mg∙L<sup>−1</sup> to 12.66 mg∙L<sup>−1</sup> with an average value of 4.03 mg∙L<sup>−1</sup>. Inter comparing hand pumps, tube wells and filtration plants data, it was found that average concentration of uranium in hand pump was 9.7 and 3.9 times greater than filtration plants and tube well water samples respectively.</p><p>The present data have also been compared with uranium concentration in water samples reported for other countries of the world. The reported uranium concentrations ranged from 1.4 - 7.4 in hot springs water in India [<xref ref-type="bibr" rid="scirp.30782-ref25">25</xref>]. The uranium concentration in the range of 0.015 - 973.0 mg∙L<sup>−1</sup> were reported in the domestic water supplies of USA [<xref ref-type="bibr" rid="scirp.30782-ref32">32</xref>]. The uranium concentration in the range of 0.015 - 973.0 mg∙L<sup>−1</sup> were reported in the domestic water supplies of USA [<xref ref-type="bibr" rid="scirp.30782-ref33">33</xref>]. In a 1980-1981 sur-</p><p><xref ref-type="table" rid="table2">Table 2</xref>. The range of uranium contents and their average value in water samples from different sources of water.</p><disp-formula id="scirp.30782-formula72990"><graphic  xlink:href="3-1090078\6d4db9ae-0300-41c3-8133-8da692d02933.jpg"  xlink:type="simple"/></disp-formula><p><sup>*</sup>The figures within parentheses indicate the number of samples.</p><p>vey of 13 selected sites in south-central British Columbia, the mean uranium concentration in 519 water samples of surface and ground water (some treated) has been reported to be 4.06 &#181;g∙L<sup>−1</sup>. The reported values of uranium concentration in various community water supplies of USA are greater than permissible limit of 30 mg∙L<sup>−1</sup>. In another study reported for USA, an average concentration of 3 mg∙L<sup>−1</sup> uranium in drinking groundwater has been reported [<xref ref-type="bibr" rid="scirp.30782-ref1">1</xref>]. Uranium concentrations up to 700&#181;g∙L<sup>−1</sup> have been found in private groundwater supplies of Canada [<xref ref-type="bibr" rid="scirp.30782-ref34">34</xref>]. The mean and median levels of naturally derived uranium in groundwater of 287 wells sampled in the southeastern Manitoba (1982-1984) were 58.3 &#181;g∙L<sup>−1 </sup>and 10 &#181;g∙L<sup>−1</sup>, respectively, with a maximum value of 2020 &#181;g∙L<sup>−1</sup> [<xref ref-type="bibr" rid="scirp.30782-ref35">35</xref>]. The uranium concentrations varied from 0.67 - 20.26 mg∙L<sup>−1</sup> in domestic and surface water samples from India [<xref ref-type="bibr" rid="scirp.30782-ref36">36</xref>]. Uranium concentration in water samples using fission-track technique from the Muzaffarabad area, Azad Kashmir varied from 0.03 &#177; 0.01 mg∙L<sup>−1</sup> to 6.67 &#177; 0.14 mg∙L<sup>−1</sup> with an average of 1.36 &#177; 0.05 mg∙L<sup>−1</sup> [<xref ref-type="bibr" rid="scirp.30782-ref3">3</xref>]. The concentration of uranium in drinking water samples from different states of India was found 0.1 &#177; −19.6 &#181;g∙L<sup>−1</sup> by laser-induced fluorimetry [<xref ref-type="bibr" rid="scirp.30782-ref36">36</xref>]. An association between uranium in drinking water from drilled wells and of kidney function was studied The uranium content of well water samples was measured in the range of &lt;0.20 - 470 &#181;g∙L<sup>−1</sup> having a median value of 6.7 &#181;g∙L<sup>−1</sup>,while uranium levels in all samples of municipal water were below 0.2 &#181;g∙L<sup>−1</sup> [<xref ref-type="bibr" rid="scirp.30782-ref19">19</xref>]. Typical concentration of U in uncontaminated groundwater in many parts of the world is below 1.0 mg∙L<sup>−1</sup> although values in excess of 1000 mg∙L<sup>−1</sup> water have been reported [31,37]. Average uranium concentration in tap water samples from various European countries was found to be 2.2 &#181;g∙L<sup>−1</sup> and values above the WHO guideline (15 &#181;g∙L<sup>−1</sup>) were reported from Germany, France, Sweden, and Switzerland [<xref ref-type="bibr" rid="scirp.30782-ref31">31</xref>]. An average uranium content of 2.5&#181;g∙L<sup>−1</sup> was found in domestic water samples in US in a study performed by the National Uranium Resource Evaluation (NURE) program [31,38]. This comparison shows that, the range of uranium concentration in drinking water found in this study lies towards the lower side of the ranges, reported for other locations. The results of the study can also be compared with the worldwide guidelines for the uranium concentration in drinking water. The average observed uranium concentrations in the drinking water samples are found lower than the maximum acceptable concentration levels of Australia (20 mg∙L<sup>−1</sup>; [<xref ref-type="bibr" rid="scirp.30782-ref10">10</xref>]), Canada (20 mg∙L<sup>−1</sup>; [<xref ref-type="bibr" rid="scirp.30782-ref12">12</xref>]), USA (30 mg∙L<sup>−1</sup>; [<xref ref-type="bibr" rid="scirp.30782-ref11">11</xref>]), WHO (9 mg∙L<sup>−1</sup>; [<xref ref-type="bibr" rid="scirp.30782-ref13">13</xref>]). Consequently, the health hazards related to uranium in drinking water were expected to be negligible.</p><p>It may be noted here that the average value of 7.39 &#177; 1.30 mg∙L<sup>−1</sup> in the text as well as in <xref ref-type="table" rid="table1">Table 1</xref> means the average value of the measured data in this work. It does not mean the real average concentration of uranium in the water in the whole area. It is an easily obtainable figure from a limited number of water samples without taking into account of the water reserve represented by each sample. However, considering health hazard related with ingestion of drinking water having concentration of uranium above recommended level. It is, therefore, desirable that uranium in drinking water samples survey on regional scale should also be monitored to address this issue of public health concern.</p><p>By making a measurement relative to the concentration of uranium in standard, many sources of uncertainty are cancelled out and the remaining dominant uncertainty is the statistics of the track counting. The errors (&#177;represents 1 standard deviation) in the track densities were calculated by multiplying track density by (1/N)<sup>1/2</sup>, where N is the total number of tracks counted in that sample. The tracks of every detector were counted by taking more fields of view to reduce any statistical counting error in the total track density, and uranium concentrations were determined with 1 standard deviation. The systematic error due to the clustering of tracks was small as the numbers of clusters found in this study were negligible. The reliability of the results obtained by this method primarily depends upon the accurate measurements of neutron flux and the number of counted fission tracks. However, the uncertainty due to the first factor is eliminated by comparing track counts for the same flux.</p><p>The total uncertainties in the uranium concentration for each unknown were calculated by combining the statistical uncertainties of track number of unknown sample and that of standard sample as well as the uncertainty of uranium concentration of standard sample. The uranium concentrations were determined up to one standard deviation.</p><p>In order to obtained a reasonably good statistics of track counts, 30 - 60 fields-of-view were selected randomly on each of the detector surfaces, which was in contact with sample residue at the time of irradiation. In order to obtain accurate results, a blank detector was exposed along with the sample to subtract background track density (track density resulting from fission of uranium present as a constituent of the detector) from the total track densities. However, background tracks contribution due to uranium in the Lexan<sup>&#210;</sup> detector was found negligible.</p><p>The uniformly distributed fission tracks formed due to the dissolved uranium were easily differentiated from the cluster-type fission tracks due to the suspended particles in water. From the results of the samples, it was obvious that the distribution of uranium is uniform except in few cases, where clustering of tracks (fission track stars) appeared within the area containing droplet residue. In addition to the uranium, tracks produced due to thorium may interfere in the uranium determination. However, because of its low concentration in the water and relatively smaller thermal neutron cross section, the contribution of thorium was negligible.</p></sec><sec id="s4"><title>4. Conclusion</title><p>To conclude, uranium concentration in drinking water of the Faisalabad city vary from 1.04 &#177; 0.30 to 21.08 &#177; 2.95 &#181;g∙L<sup>−1</sup> with an average value of 7.39 &#177; 1.30 &#181;g∙L<sup>−1</sup>. The observed uranium concentration in hand pump is ~10 and 4 times greater than those of filtration plants and tube wells water samples respectively. The deep underground water obtained from tube well is safer for drinking purposes as compared to shallow surface underground water from hand pump while the water from filtration plant was safest as far as uranium related health hazards are concerned. The average observed levels of uranium concentrations in the studied water samples is within the safe limits (9 - 30 &#181;g∙L<sup>−1</sup>) set by different heath agencies of the world. Consequently, the health hazards related to uranium in drinking water in this area are negligible and use of this water for drinking and other purposes may not pose any health risk. However, health hazards related to other toxic and trace elements present in drinking water samples from this area should also be monitored with great care before declaring it free of any health related hazard.</p></sec><sec id="s5"><title>REFERENCES</title></sec><sec id="s6"><title>NOTES</title></sec></body><back><ref-list><title>References</title><ref id="scirp.30782-ref1"><label>1</label><mixed-citation publication-type="other" xlink:type="simple">C. R. Cothern and W. L. Lappenbusch “Occurrence of Uranium in Drinking in the US,” Health Physic, Vol. 45, No. 1, 1983, pp. 89-99.  
doi:10.1097/00004032-198307000-00009</mixed-citation></ref><ref id="scirp.30782-ref2"><label>2</label><mixed-citation publication-type="other" xlink:type="simple">P. Singh, N. P. S. Rana, A. Azam, A. H. Naqvi and D. S. Srivastava, “Levels of Uranium in Waters from Some Indian Cities Determined by Fission Track Analysis,” Radiation Measurements, Vol. 26, No. 5, 1996, pp. 683-687. 
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