<?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">JMMCE</journal-id><journal-title-group><journal-title>Journal of Minerals and Materials Characterization and Engineering</journal-title></journal-title-group><issn pub-type="epub">2327-4077</issn><publisher><publisher-name>Scientific Research Publishing</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.4236/jmmce.2017.51004</article-id><article-id pub-id-type="publisher-id">JMMCE-73412</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><subject> Engineering</subject></subj-group></article-categories><title-group><article-title>
 
 
  Metal Extraction Process for High Grade Stibnite of Kharan (Balochistan Pakistan)
 
</article-title></title-group><contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Irfan</surname><given-names>Hafeez</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>Saqib</surname><given-names>Nasir</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>Samreen</surname><given-names>Zahra</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>Muhammad</surname><given-names>Aamir</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>Zahid</surname><given-names>Mahmood</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>Adnan</surname><given-names>Akram</given-names></name><xref ref-type="aff" rid="aff1"><sup>1</sup></xref></contrib></contrib-group><aff id="aff1"><addr-line>Mineral Processing Research Centre, Pakistan Council of Scientific &amp;amp; Industrial Research Laboratories Complex, 
Lahore, Pakistan</addr-line></aff><pub-date pub-type="epub"><day>16</day><month>12</month><year>2016</year></pub-date><volume>05</volume><issue>01</issue><fpage>39</fpage><lpage>48</lpage><history><date date-type="received"><day>January</day>	<month>14,</month>	<year>2016</year></date><date date-type="rev-recd"><day>Accepted:</day>	<month>January</month>	<year>9,</year>	</date><date date-type="accepted"><day>January</day>	<month>12,</month>	<year>2017</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>
 
 
  A rapid and simple process has been developed for the recovery of antimony metal from stibnite ore of Kharan area (Balochistan) of Pakistan. The ore was characterized by X-ray diffraction (XRD) technique and found to contain 66% stibnite i.e. antimony sulfide (Sb
  <sub>2</sub>S
  <sub>3</sub>). The process parameters for the extraction of antimony were optimized on laboratory scale by varying reaction temperature from 900
  ℃ - 1000
  ℃, reaction time from 20 - 80 minutes and flux concentration was varied from 5 - 25 weight percent of the reaction mixture. The metal thus recovered with optimum conditions was evaluated by X-ray fluorescence (XRF) technique and was found to be more than 94% pure. The recovery yield calculated on the basis of stibnite present in the ore was 98.52%.
 
</p></abstract><kwd-group><kwd>Antimony</kwd><kwd> Stibnite</kwd><kwd> Extraction</kwd><kwd> Recovery Yield</kwd></kwd-group></article-meta></front><body><sec id="s1"><title>1. Introduction</title><p>Stibnite, also called as antimonite, is a major source of antimony which is in fact its sulphide mineral (Sb<sub>2</sub>S<sub>3</sub>). It occurs enormously as veins mainly associated with quartz and other antimony minerals like antimony oxide, formed by the decomposition of stibnite. The abundant deposits of stibnite are found in Kharan, Qilla Abdullah, Kalat, Pishin, Kurram valley, Karangli hill, Krinj and Chitral areas of Pakistan [<xref ref-type="bibr" rid="scirp.73412-ref1">1</xref>] . In addition to these reserves, the deposits of stibnite are being discovered in Kharan [<xref ref-type="bibr" rid="scirp.73412-ref2">2</xref>] , are economically feasible and should explore for country demand. These significant mineral deposits can be utilized effectively for the extraction of antimony metal as it contains 60% - 66% stibnite mineral.</p><p>The extraction of metal from an ore mainly depends on its grade; low grade ores required up-gradation prior to extraction for the removal of associated gangue minerals which are often pyrite, sphalerite, calcite, barite and other clay mineral [<xref ref-type="bibr" rid="scirp.73412-ref1">1</xref>] . Such ores are usually up-graded by froth-flotation process [<xref ref-type="bibr" rid="scirp.73412-ref3">3</xref>] while high grade ores can be utilized directly for metal recovery due to substantial decrease in gangue content.</p><p>Antimony is usually extracted from its ores by either hydro-metallurgical or pyro-metallurgical processes. In addition to these, a variety of solvents have also been used in the past, for the extraction of antimony from aqueous solutions [<xref ref-type="bibr" rid="scirp.73412-ref4">4</xref>] [<xref ref-type="bibr" rid="scirp.73412-ref5">5</xref>] . Hydrometallurgical processes usually involve acid or alkaline leaching of ores. The acid leaching is often carried out by mineral acids i.e. hydrochloric acid, nitric acid and sulphuric acid. Since stibnite ore reacts slowly and incompletely with mineral acids alone, they have been used in combination with other reagents e.g. tartaric acid [<xref ref-type="bibr" rid="scirp.73412-ref6">6</xref>] . The reductive leaching using iron powder in mineral acid has also been reported for the efficient recovery of antimony from stibnite [<xref ref-type="bibr" rid="scirp.73412-ref7">7</xref>] . The other hydrometallurgical method commonly investigated by the researchers i.e. alkaline leaching, has been performed using solutions of either sodium hydroxide or sodium hydroxide along with sodium sulfide and 70% to 90% recovery of antimony has been achieved [<xref ref-type="bibr" rid="scirp.73412-ref8">8</xref>] [<xref ref-type="bibr" rid="scirp.73412-ref9">9</xref>] [<xref ref-type="bibr" rid="scirp.73412-ref10">10</xref>] . Veglio and co-worker have optimized parameters for alkaline leaching with sodium hydroxide and sodium sulfide using pure antimony sulfide instead of antimony ore and have obtained 98% - 100% extraction yield of antimony during study [<xref ref-type="bibr" rid="scirp.73412-ref11">11</xref>] ; however its yield decreases subsequently if the same procedure may be followed for the original ore. All these hydrometallurgical processes involve use of finer fractions of up-graded ores and leaching pre-treatment followed by separation of metal from the leach solution which is usually carried out by electro winning technology [<xref ref-type="bibr" rid="scirp.73412-ref12">12</xref>] . Moreover, these methods require several hours for their completion and involvement of numerous steps makes them relatively expensive and tedious. Furthermore acid leaching is accompanied by the evolution of hydrogen sulfide gas which is toxic and causes environmental hazards [<xref ref-type="bibr" rid="scirp.73412-ref7">7</xref>] .</p><p>Pyro-metallurgical technique has also been used successfully by the previous researchers and found to be extremely beneficial for the recovery of antimony from its ores since reactants undergo spontaneous chemical changes due to application of high temperature and metal is readily separated from the molten mixture [<xref ref-type="bibr" rid="scirp.73412-ref13">13</xref>] [<xref ref-type="bibr" rid="scirp.73412-ref14">14</xref>] . In contrast to hydro-metallurgy, pyro-metallurgical routes are extensively used on commercial scale as it is economically viable although required high temperatures i.e. 1150˚C to 1350˚C and as a consequence produce toxic antimony vapours and sulphur dioxide gas. However, the sulphur dioxide gas produced can be converted to sulphuric acid by the well-known contact process which can subsequently reduce the environmental hazards of this technology. Analogous to hydrometallurgical procedures most of the previously developed pyro-metallurgical methods are multi-step processes which often begin with the smelting of concentrates [<xref ref-type="bibr" rid="scirp.73412-ref14">14</xref>] [<xref ref-type="bibr" rid="scirp.73412-ref15">15</xref>] .</p><p>In view of the fact that antimony and its compounds are widely used in flame-retardants textile finishing compounds, lead alloys, semiconductors, ceramic enamels and pigments etc. [<xref ref-type="bibr" rid="scirp.73412-ref16">16</xref>] , the present studies was undertaken to develop a one-step pathway for the recovery of antimony metal directly from stibnite high grade ore of Distt. Kharan (Balochistan) and can be employed for economic recovery of antimony metal without up-gradation. This can be achieved with iron reduction method [<xref ref-type="bibr" rid="scirp.73412-ref16">16</xref>] and the process parameters were optimized on laboratory scale to obtained maximum recovery of antimony metal.</p></sec><sec id="s2"><title>2. Experimental Methodology</title><sec id="s2_1"><title>2.1. Ore Samples</title><p>Stibnite ore of Kharan area of Pakistan was employed for the extraction of metal which contains 66% antimony sulfide content. Iron scrape was used as a source of iron whereas analytical grade sodium chloride was used as a flux.</p></sec><sec id="s2_2"><title>2.2. Characterization of Stibnite Ore of Kharan</title><p>Stibnite ore of Kharan was characterized by Xpert High Score Plus Diffractometer using monochromatised CuK<sub>α</sub> radiation having wavelength of 1.5404 &#197;.</p></sec><sec id="s2_3"><title>2.3. Extraction Procedure</title><p>Stibnite ore of −30 mesh size was mixed with iron scrape in stoichiometric ratio according to the following equation [<xref ref-type="bibr" rid="scirp.73412-ref16">16</xref>] :</p><disp-formula id="scirp.73412-formula90"><graphic  xlink:href="http://html.scirp.org/file/4-2710404x2.png"  xlink:type="simple"/></disp-formula><p>The flux was then added and the mixture was heated at ambient temperature in graphite crucible on a gas fired furnace for constant time. The melting product contains molten antimony metal and slag; the slag obtained was a mixture of flux and iron sulfide formed as a by-product. The molten material was then poured into a mould and the metal was separated from iron sulfide.</p><p>The process parameters were optimized and the effect of temperature was studied in a range of 900˚C to 1000˚C and time was varied from 20 to 80 minutes whereas effect of flux i.e. sodium chloride was studied by varying its concentration from 5% to 25% by weight of reaction mixture.</p></sec><sec id="s2_4"><title>2.4. Characterization of Antimony Metal</title><p>The final product obtained i.e. antimony metal was characterized by X-ray fluorescence technique (XRF) using Spectro Midex MID 01.</p></sec></sec><sec id="s3"><title>3. Results and Discussion</title><p>Stibnite ore of Kharan is a high grade ore and it contains 66% antimony sulfide as confirmed by X-ray diffraction (XRD) analysis. Therefore, up-gradation through froth-flotation is not required and instead of using concentrate the ore is employed directly for extraction of antimony metal as its recovery is better by iron precipitation since stibnite is a sulfide ore. The process is based on a displacement reaction in which iron displaces antimony in the sulfide mineral, as a result of which antimony sulfide is converted to antimony metal and iron sulfide is formed as a by-product which can be utilized for production of hydrogen sulfide gas in Kipp’s apparatus. In present study, the ore after crushing was ground to pass 30 mesh sieve and subjected to reduction using iron scrape in the presence of flux and the process parameters were optimized on laboratory scale by varying flux concentration at variable temperature and reaction time.</p><sec id="s3_1"><title>3.1. X-Ray Diffraction Analysis</title><p>Mineralogical composition of the stibnite ore was confirmed by X-ray diffraction analysis and diffraction pattern is illustrated in <xref ref-type="fig" rid="fig1">Figure 1</xref>. All the peaks were matched by the search-match program using Xpert High Score Plus Software which reveals that the ore predominantly consists of stibnite (Sb<sub>2</sub>S<sub>3</sub>) i.e. 66%, whereas 6% senarmontite (Sb<sub>2</sub>O<sub>3</sub>) was also detected as shown in <xref ref-type="table" rid="table1">Table 1</xref>. These results suggest that it is a mixed ore but contains oxide mineral in a minor quantity as compared to sulfide. The host mineral was entirely composed of quartz (SiO<sub>2</sub>) which was found to be 28%. The remaining associated gangue minerals i.e. pyrite, sphalarite, calcite, barite and clay minerals might be present in traces, so these were not detected due to limitation of X-ray diffraction technique.</p></sec><sec id="s3_2"><title>3.2. Process Parameters Optimization</title><sec id="s3_2_1"><title>3.2.1. Effect of Reaction Temperature</title><p>The temperature was varied from 900˚C to 1000˚C and its effect on the recovery of antimony metal was studied. The process was carried out at five different temperatures ranging from 900˚C to 1000˚C keeping time and flux concentration constant and results as shown in <xref ref-type="table" rid="table3">Table 3</xref>. Sodium chloride (NaCl) was used as flux in all the five experiments which was taken as 15% of the weight of the reaction mixture and the reaction was continued for 40 minutes. The results of experiments show a gradual increase in the recovery of antimony as the temperature changes from 900˚C to 950˚C whereas a sudden increase can be observed in the recovery of metal at 975˚C which remained constant as the temperature was increased up to 1000˚C. It can be noted that the recovery was quite low at temperatures 900˚C, 925˚C and 950˚C i.e. 32.55%, 42.46% and 53.78% respectively but as the temperature was increased to 975˚C a substantial quantity of metal i.e. 98.52% was recovered which was observed to be almost the same at 1000˚C. It is therefore inferred that the optimum temperature for the extraction of antimony metal through this process is 975˚C, as further increase in the temperature was found to be ineffective (<xref ref-type="fig" rid="fig2">Figure 2</xref>).</p></sec><sec id="s3_2_2"><title>3.2.2. Effect of Reaction Time</title><p>The effect of time on extraction of antimony from stibnite ore was studied and results are given in <xref ref-type="table" rid="table4">Table 4</xref>. A series of experiments were conducted by varying time for 20, 40, 60 and 80 minutes using sodium chloride, 15% of the weight of the reaction mixture, as flux, keeping temperature at 975˚C. It is evident from the results that only 52.37% metal is recovered when the mixture was heated for 20 minutes. The results indicate that the rate of recovery was increased with increase in time duration. However, as the time was increased for 40, 60 and 80 minutes almost similar results were obtained i.e. 98.52% - 98.76%. Therefore,</p><table-wrap id="table1" ><label><xref ref-type="table" rid="table1">Table 1</xref></label><caption><title> X-ray diffraction (XRD) data</title></caption><table><tbody><thead><tr><th align="center" valign="middle" >Pos. [˚2Th.]</th><th align="center" valign="middle" >Height [cts]</th><th align="center" valign="middle" >FWHM [˚2Th.]</th><th align="center" valign="middle" >d-spacing [&#197;]</th><th align="center" valign="middle" >Rel. Int. [%]</th></tr></thead><tr><td align="center" valign="middle" >15.8220</td><td align="center" valign="middle" >71.99</td><td align="center" valign="middle" >0.3149</td><td align="center" valign="middle" >5.60134</td><td align="center" valign="middle" >7.90</td></tr><tr><td align="center" valign="middle" >17.8330</td><td align="center" valign="middle" >135.33</td><td align="center" valign="middle" >0.1968</td><td align="center" valign="middle" >4.97396</td><td align="center" valign="middle" >14.84</td></tr><tr><td align="center" valign="middle" >21.1832</td><td align="center" valign="middle" >377.40</td><td align="center" valign="middle" >0.1968</td><td align="center" valign="middle" >4.19427</td><td align="center" valign="middle" >41.39</td></tr><tr><td align="center" valign="middle" >22.5423</td><td align="center" valign="middle" >46.12</td><td align="center" valign="middle" >0.2362</td><td align="center" valign="middle" >3.94437</td><td align="center" valign="middle" >5.06</td></tr><tr><td align="center" valign="middle" >25.1727</td><td align="center" valign="middle" >295.47</td><td align="center" valign="middle" >0.2362</td><td align="center" valign="middle" >3.53786</td><td align="center" valign="middle" >32.41</td></tr><tr><td align="center" valign="middle" >26.9494</td><td align="center" valign="middle" >911.80</td><td align="center" valign="middle" >0.1574</td><td align="center" valign="middle" >3.30852</td><td align="center" valign="middle" >100.00</td></tr><tr><td align="center" valign="middle" >27.8890</td><td align="center" valign="middle" >82.46</td><td align="center" valign="middle" >0.2362</td><td align="center" valign="middle" >3.19915</td><td align="center" valign="middle" >9.04</td></tr><tr><td align="center" valign="middle" >28.7984</td><td align="center" valign="middle" >127.64</td><td align="center" valign="middle" >0.1574</td><td align="center" valign="middle" >3.10016</td><td align="center" valign="middle" >14.00</td></tr><tr><td align="center" valign="middle" >29.4844</td><td align="center" valign="middle" >91.50</td><td align="center" valign="middle" >0.2362</td><td align="center" valign="middle" >3.02957</td><td align="center" valign="middle" >10.03</td></tr><tr><td align="center" valign="middle" >30.3255</td><td align="center" valign="middle" >25.61</td><td align="center" valign="middle" >0.3149</td><td align="center" valign="middle" >2.94744</td><td align="center" valign="middle" >2.81</td></tr><tr><td align="center" valign="middle" >32.6441</td><td align="center" valign="middle" >102.32</td><td align="center" valign="middle" >0.4723</td><td align="center" valign="middle" >2.74320</td><td align="center" valign="middle" >11.22</td></tr><tr><td align="center" valign="middle" >33.7017</td><td align="center" valign="middle" >38.36</td><td align="center" valign="middle" >0.3149</td><td align="center" valign="middle" >2.65950</td><td align="center" valign="middle" >4.21</td></tr><tr><td align="center" valign="middle" >35.7829</td><td align="center" valign="middle" >203.17</td><td align="center" valign="middle" >0.1968</td><td align="center" valign="middle" >2.50944</td><td align="center" valign="middle" >22.28</td></tr><tr><td align="center" valign="middle" >36.8882</td><td align="center" valign="middle" >228.08</td><td align="center" valign="middle" >0.1968</td><td align="center" valign="middle" >2.43675</td><td align="center" valign="middle" >25.01</td></tr><tr><td align="center" valign="middle" >39.8027</td><td align="center" valign="middle" >59.73</td><td align="center" valign="middle" >0.4723</td><td align="center" valign="middle" >2.26479</td><td align="center" valign="middle" >6.55</td></tr><tr><td align="center" valign="middle" >40.6809</td><td align="center" valign="middle" >75.82</td><td align="center" valign="middle" >0.3149</td><td align="center" valign="middle" >2.21790</td><td align="center" valign="middle" >8.32</td></tr><tr><td align="center" valign="middle" >42.7179</td><td align="center" valign="middle" >166.66</td><td align="center" valign="middle" >0.2362</td><td align="center" valign="middle" >2.11674</td><td align="center" valign="middle" >18.28</td></tr><tr><td align="center" valign="middle" >46.0837</td><td align="center" valign="middle" >33.31</td><td align="center" valign="middle" >0.4723</td><td align="center" valign="middle" >1.96967</td><td align="center" valign="middle" >3.65</td></tr><tr><td align="center" valign="middle" >47.0066</td><td align="center" valign="middle" >109.00</td><td align="center" valign="middle" >0.3149</td><td align="center" valign="middle" >1.93313</td><td align="center" valign="middle" >11.95</td></tr><tr><td align="center" valign="middle" >48.4745</td><td align="center" valign="middle" >44.65</td><td align="center" valign="middle" >0.2362</td><td align="center" valign="middle" >1.87797</td><td align="center" valign="middle" >4.90</td></tr><tr><td align="center" valign="middle" >50.3546</td><td align="center" valign="middle" >121.42</td><td align="center" valign="middle" >0.2755</td><td align="center" valign="middle" >1.81218</td><td align="center" valign="middle" >13.32</td></tr><tr><td align="center" valign="middle" >53.2251</td><td align="center" valign="middle" >51.07</td><td align="center" valign="middle" >0.3149</td><td align="center" valign="middle" >1.72101</td><td align="center" valign="middle" >5.60</td></tr><tr><td align="center" valign="middle" >54.4307</td><td align="center" valign="middle" >117.42</td><td align="center" valign="middle" >0.3149</td><td align="center" valign="middle" >1.68571</td><td align="center" valign="middle" >12.88</td></tr><tr><td align="center" valign="middle" >60.2287</td><td align="center" valign="middle" >70.25</td><td align="center" valign="middle" >0.2362</td><td align="center" valign="middle" >1.53657</td><td align="center" valign="middle" >7.70</td></tr><tr><td align="center" valign="middle" >62.9998</td><td align="center" valign="middle" >18.13</td><td align="center" valign="middle" >0.4723</td><td align="center" valign="middle" >1.47549</td><td align="center" valign="middle" >1.99</td></tr><tr><td align="center" valign="middle" >64.7473</td><td align="center" valign="middle" >10.67</td><td align="center" valign="middle" >0.9446</td><td align="center" valign="middle" >1.43982</td><td align="center" valign="middle" >1.17</td></tr><tr><td align="center" valign="middle" >67.9022</td><td align="center" valign="middle" >468.26</td><td align="center" valign="middle" >0.1181</td><td align="center" valign="middle" >1.38041</td><td align="center" valign="middle" >51.36</td></tr><tr><td align="center" valign="middle" >72.2709</td><td align="center" valign="middle" >22.15</td><td align="center" valign="middle" >0.3149</td><td align="center" valign="middle" >1.30735</td><td align="center" valign="middle" >2.43</td></tr><tr><td align="center" valign="middle" >81.6899</td><td align="center" valign="middle" >41.37</td><td align="center" valign="middle" >0.7680</td><td align="center" valign="middle" >1.17780</td><td align="center" valign="middle" >4.54</td></tr></tbody></table></table-wrap><table-wrap id="table2" ><label><xref ref-type="table" rid="table2">Table 2</xref></label><caption><title> Mineralogical data of stibinite ore</title></caption><table><tbody><thead><tr><th align="center" valign="middle" >Constituents</th><th align="center" valign="middle" >Results (%)</th></tr></thead><tr><td align="center" valign="middle" >Sb<sub>2</sub>S<sub>3</sub></td><td align="center" valign="middle" >66.01</td></tr><tr><td align="center" valign="middle" >Sb<sub>2</sub>O<sub>3</sub></td><td align="center" valign="middle" >5.22</td></tr><tr><td align="center" valign="middle" >Fe<sub>2</sub>O<sub>3</sub></td><td align="center" valign="middle" >0.53</td></tr><tr><td align="center" valign="middle" >Al<sub>2</sub>O<sub>3</sub></td><td align="center" valign="middle" >0.21</td></tr><tr><td align="center" valign="middle" >CaO</td><td align="center" valign="middle" >0.33</td></tr><tr><td align="center" valign="middle" >SiO<sub>2</sub></td><td align="center" valign="middle" >27.32</td></tr><tr><td align="center" valign="middle" >MgO</td><td align="center" valign="middle" >0.07</td></tr></tbody></table></table-wrap><fig id="fig1"  position="float"><label><xref ref-type="fig" rid="fig1">Figure 1</xref></label><caption><title> X-ray diffraction (XRD) of Kharan (Balochistan, Pakistan) stibnite</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/4-2710404x3.png"/></fig><fig id="fig2"  position="float"><label><xref ref-type="fig" rid="fig2">Figure 2</xref></label><caption><title> Effect of reaction temperature for recovery yield</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/4-2710404x4.png"/></fig><table-wrap id="table3" ><label><xref ref-type="table" rid="table3">Table 3</xref></label><caption><title> Effect of reaction temperature on recovery of antimony</title></caption><table><tbody><thead><tr><th align="center" valign="middle" >Temperature (˚C)</th><th align="center" valign="middle" >Recovery Yield (%)</th></tr></thead><tr><td align="center" valign="middle" >900</td><td align="center" valign="middle" >32.55</td></tr><tr><td align="center" valign="middle" >925</td><td align="center" valign="middle" >42.46</td></tr><tr><td align="center" valign="middle" >950</td><td align="center" valign="middle" >53.78</td></tr><tr><td align="center" valign="middle" >975</td><td align="center" valign="middle" >98.52</td></tr><tr><td align="center" valign="middle" >1000</td><td align="center" valign="middle" >98.80</td></tr></tbody></table></table-wrap><p>heating for 40 minutes was found to be the most significant and further increase in reaction time showed no appreciable change in recovery of antimony which also consumes more energy in addition to increased antimony volatilization [<xref ref-type="bibr" rid="scirp.73412-ref14">14</xref>] (<xref ref-type="fig" rid="fig3">Figure 3</xref>).</p></sec><sec id="s3_2_3"><title>3.2.3. Effect of Flux Concentration</title><p>Sodium chloride was used as flux in the present study to reduce volatilization of antimony metal and enhance the dissolution of gangue minerals [<xref ref-type="bibr" rid="scirp.73412-ref16">16</xref>] . A number of experiments were carried out at different concentrations of sodium chloride i.e. 5%, 10%, 15%, 20% and 25% of the weight of the reaction mixture, keeping all other parameters constant and results are illustrated in <xref ref-type="fig" rid="fig4">Figure 4</xref>. The figure shows a regular increase in the recovery of antimony up to 15% and as the concentration of flux is increased to 20% - 25%, no considerable change in the recovery is observed. It is therefore noted that 15 weight percent of flux was found to be appropriate at which 98.52% of the metal was recovered as further addition of flux only affects the consistency of reaction mixture and shows no prominent increase in the recovery yield of metal (<xref ref-type="table" rid="table5">Table 5</xref>).</p><fig id="fig3"  position="float"><label><xref ref-type="fig" rid="fig3">Figure 3</xref></label><caption><title> Effect of reaction time vs recovery yield</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/4-2710404x5.png"/></fig><fig id="fig4"  position="float"><label><xref ref-type="fig" rid="fig4">Figure 4</xref></label><caption><title> Effect of flux concentration vs recovery yield</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/4-2710404x6.png"/></fig></sec></sec><sec id="s3_3"><title>3.3. Confirmation Experiment</title><p>A confirmation experiment was carried out for the extraction of antimony metal from stibnite ore at optimum conditions to substantiate the entire procedure. For this purpose 500 gm of the ore and iron scrape were mixed in stoichiometric ratio and the mixture was heated at 975˚C for 40 minutes in the presence of 15 weight percent of sodium chloride as flux. The metal thus obtained was 99.95% pure, as confirmed through X-ray fluorescence technique and results are reported in <xref ref-type="table" rid="table5">Table 5</xref>. The yield calculated on the basis of stibnite present in the ore was 98.52% which is an evidence of the fact that the remaining 1.48% of the metal present as sulfide mineral was captured as slag. The study reveals that antimony present as an oxide mineral in the ore is not taking part in the recovery of metal; the reason being the procedure followed for the extraction exclusively exploits the sulphide mineral. However, the metal left in the slag can be recovered by performing a second step but it will certainly involve pretreatment of slag and consumption of extensive energy that will reduce the economics of the process (<xref ref-type="fig" rid="fig5">Figure 5</xref>).</p></sec></sec><sec id="s4"><title>4. Conclusion</title><p>The present study provides a one step process for recovery of antimony metal (<xref ref-type="table" rid="table6">Table 6</xref>) from its ore containing 66% sulfide mineral. The process parameters</p><fig-group id="fig5"><label><xref ref-type="fig" rid="fig5">Figure 5</xref></label><caption><title> Photograph of extracted antimony metal.</title></caption><fig id ="fig5_1"><label></label><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/4-2710404x7.png"/></fig><fig id ="fig5_2"><label></label><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/4-2710404x8.png"/></fig></fig-group><table-wrap id="table4" ><label><xref ref-type="table" rid="table4">Table 4</xref></label><caption><title> Effect of reaction time on recovery of antimony</title></caption><table><tbody><thead><tr><th align="center" valign="middle" >Flux Concentration (%)</th><th align="center" valign="middle" >Recovery Yield (%)</th></tr></thead><tr><td align="center" valign="middle" >5</td><td align="center" valign="middle" >31.14</td></tr><tr><td align="center" valign="middle" >10</td><td align="center" valign="middle" >72.18</td></tr><tr><td align="center" valign="middle" >15</td><td align="center" valign="middle" >98.52</td></tr><tr><td align="center" valign="middle" >20</td><td align="center" valign="middle" >98.64</td></tr><tr><td align="center" valign="middle" >25</td><td align="center" valign="middle" >98.68</td></tr></tbody></table></table-wrap><table-wrap id="table5" ><label><xref ref-type="table" rid="table5">Table 5</xref></label><caption><title> Effect of flux concentration on recovery of antimony</title></caption><table><tbody><thead><tr><th align="center" valign="middle" >Time (minutes)</th><th align="center" valign="middle" >Recovery Yield (%)</th></tr></thead><tr><td align="center" valign="middle" >20</td><td align="center" valign="middle" >52.37</td></tr><tr><td align="center" valign="middle" >40</td><td align="center" valign="middle" >98.52</td></tr><tr><td align="center" valign="middle" >60</td><td align="center" valign="middle" >98.68</td></tr><tr><td align="center" valign="middle" >80</td><td align="center" valign="middle" >98.76</td></tr></tbody></table></table-wrap><table-wrap id="table6" ><label><xref ref-type="table" rid="table6">Table 6</xref></label><caption><title> Analysis of recovered antimony metal</title></caption><table><tbody><thead><tr><th align="center" valign="middle" >Sr. No.</th><th align="center" valign="middle" >Symbol</th><th align="center" valign="middle" >No. of Impulses</th><th align="center" valign="middle" >Concentration</th><th align="center" valign="middle" >Unit</th></tr></thead><tr><td align="center" valign="middle" >47</td><td align="center" valign="middle" >Ag</td><td align="center" valign="middle" >477 F</td><td align="center" valign="middle" >0.1144</td><td align="center" valign="middle" >%</td></tr><tr><td align="center" valign="middle" >48</td><td align="center" valign="middle" >Cd</td><td align="center" valign="middle" >506 F</td><td align="center" valign="middle" >0.1527</td><td align="center" valign="middle" >%</td></tr><tr><td align="center" valign="middle" >49</td><td align="center" valign="middle" >In</td><td align="center" valign="middle" >622 F</td><td align="center" valign="middle" >0.249</td><td align="center" valign="middle" >%</td></tr><tr><td align="center" valign="middle" >50</td><td align="center" valign="middle" >Sn</td><td align="center" valign="middle" >444 F</td><td align="center" valign="middle" >0.143</td><td align="center" valign="middle" >%</td></tr><tr><td align="center" valign="middle" >51</td><td align="center" valign="middle" >Sb</td><td align="center" valign="middle" >112997 F</td><td align="center" valign="middle" >~94.08</td><td align="center" valign="middle" >%</td></tr><tr><td align="center" valign="middle" >73</td><td align="center" valign="middle" >Ta</td><td align="center" valign="middle" >459 F</td><td align="center" valign="middle" >0.0546</td><td align="center" valign="middle" >%</td></tr><tr><td align="center" valign="middle" >74</td><td align="center" valign="middle" >W</td><td align="center" valign="middle" >1512 F</td><td align="center" valign="middle" >0.2501</td><td align="center" valign="middle" >%</td></tr><tr><td align="center" valign="middle" >77</td><td align="center" valign="middle" >Ir</td><td align="center" valign="middle" >0</td><td align="center" valign="middle" >&lt;0.0010</td><td align="center" valign="middle" >%</td></tr><tr><td align="center" valign="middle" >78</td><td align="center" valign="middle" >Pt</td><td align="center" valign="middle" >0</td><td align="center" valign="middle" >&lt;0.020</td><td align="center" valign="middle" >%</td></tr><tr><td align="center" valign="middle" >79</td><td align="center" valign="middle" >Au</td><td align="center" valign="middle" >0</td><td align="center" valign="middle" >&lt;0.020</td><td align="center" valign="middle" >%</td></tr><tr><td align="center" valign="middle" >82</td><td align="center" valign="middle" >Pb</td><td align="center" valign="middle" >4599 F</td><td align="center" valign="middle" >&lt;0.4138</td><td align="center" valign="middle" >%</td></tr></tbody></table></table-wrap><p>for the extraction of metal were optimized on laboratory scale and 975˚C reaction temperature, 40 minutes reaction time and 15 weight percent of sodium chloride as flux were found to be the optimal conditions. The purity of metal thus obtained was 99.95% and its recovery calculated on the basis of stibnite present in ore was found to be 98.52%. Since the process involves no up-grada- tion through froth-flotation and the ore is employed directly for extraction; therefore single step and application of lower temperature results in consumption of less energy and low volatility of antimony metal that makes the process economically feasible and reduces environmental hazards during metal extraction.</p></sec><sec id="s5"><title>Cite this paper</title><p>Hafeez, I., Nasir, S., Zahra, S., Aamir, M., Mahmood, Z. and Akram, A. (2017) Metal Extraction Process for High Grade Stibnite of Kharan (Balochistan Pakistan). Journal of Minerals and Materials Characterization and Engineering, 5, 39-48. http://dx.doi.org/10.4236/jmmce.2017.51004</p></sec></body><back><ref-list><title>References</title><ref id="scirp.73412-ref1"><label>1</label><mixed-citation publication-type="other" xlink:type="simple">Bhatti, M.A., Kazmi, K.R., Nizami, M.S., Anwar, M.A., Saleemi, A.A. and Butt, K. (2009) Mineralogical and Liberation Characteristics of Antimony Ore of Chitral, NWFP, Pakistan. Journal of the Chemical Society of Pakistan, 31, 39-45.</mixed-citation></ref><ref id="scirp.73412-ref2"><label>2</label><mixed-citation publication-type="other" xlink:type="simple">Mineral Profile of Balochistan (2009) Geological Survey of Pakistan. Ministry of Petroleum and Natural Resources. http://www.scribd.com</mixed-citation></ref><ref id="scirp.73412-ref3"><label>3</label><mixed-citation publication-type="other" xlink:type="simple">Riaz, M., Jan, N., Hussain, M.T., Khan, F. and Yamin, A. 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