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<front>
<journal-meta>
<journal-id journal-id-type="pmc">IJASE</journal-id>
<journal-id journal-id-type="nlm-ta">IJASE</journal-id>
<journal-id journal-id-type="publisher-id">IJASE</journal-id>
<journal-title-group>
<journal-title>International Journal of Applied Science and Engineering</journal-title>
</journal-title-group>
<issn pub-type="ppub">2321-0745</issn>
<issn pub-type="epub">2322-0465</issn>
<publisher>
<publisher-name>IST Foundation</publisher-name>
<publisher-loc>India</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="other">IJASE-8-01-11</article-id>
<article-categories>
<subj-group subj-group-type="heading">
<subject>Research Paper</subject>
</subj-group>
</article-categories>
<title-group>
<article-title>Hydrothermal Synthesis and Spectroscopic Characterization of one-dimentional Rod-like Hematite (&#x03B1;-Fe<sub>2</sub>O<sub>3</sub>) Mineral in Alkaline Medium</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name><surname>Abdus-Salam</surname><given-names>N.</given-names></name>
<xref ref-type="aff" rid="A1">1</xref>
</contrib>
<contrib contrib-type="author">
<name><surname>Godwin</surname><given-names>John</given-names></name>
<xref ref-type="aff" rid="A1">1</xref>
<xref ref-type="aff" rid="A2">2</xref>
<xref ref-type="aff" rid="A3">3</xref>
<xref ref-type="corresp" rid="cor001">*</xref>
</contrib>
<contrib contrib-type="author">
<name><surname>Tripathy</surname><given-names>Bankim Chandra</given-names></name>
<xref ref-type="aff" rid="A2">2</xref>
</contrib>
</contrib-group>
<aff id="A1"><label>1</label>Department of Chemistry, University of Ilorin, P.M.B. 1515, Ilorin, Nigeria</aff>
<aff id="A2"><label>2</label>Hydro &#x0026; Electrometallurgy Department, Institute of Minerals and Materials Technology, Bhubaneswar - 751 013, India</aff>
<aff id="A3"><label>3</label>Department of Chemistry, Kogi State College of Education (Tecchnical), P.O.B 242 Kabba, Nigeria</aff>
<author-notes>
<corresp id="cor001"><label>*</label>Corresponding author: <email>godwinjohn1380@gmail.com</email></corresp>
</author-notes>
<pub-date pub-type="ppub">
<month>06</month>
<year iso-8601-date="2020">2020</year>
</pub-date>
<volume>8</volume>
<issue>1</issue>
<fpage>11</fpage>
<lpage>18</lpage>
<history>
<date date-type="received" iso-8601-date="2020-01-17">
<day>17</day>
<month>01</month>
<year>2020</year>
</date>
<date date-type="revised" iso-8601-date="2020-04-21">
<day>21</day>
<month>04</month>
<year>2020</year>
</date>
<date date-type="accepted" iso-8601-date="2020-05-23">
<day>23</day>
<month>05</month>
<year>2020</year>
</date>
</history>
<permissions>
<copyright-statement>&#x00A9; IST Foundation, India</copyright-statement>
<copyright-year>2020</copyright-year>
<copyright-holder>IST Foundation, India</copyright-holder>
</permissions>
<self-uri content-type="pdf" xlink:href="IJASE-8-01-11.pdf"></self-uri>
<abstract>
<p>Rod-like &#x03B1;-Fe<sub>2</sub>O<sub>3</sub> was synthesized by hydrothermal method and characterized using spectroscopic methods of analysis. X-ray diffraction (XRD), Fourier transform infrared (FTIR), X-field emission scanning electron microscopy (FESEM), elemental diffraction X- ray (EDX), transmission electron microscopy (TEM) and dynamic light scattering (DLS) methods were used to characterize the synthesized mineral. XRD analysis shows that the single-crystalline sample indexed as the pure rhombohedra &#x03B1;<bold>-</bold> Fe<sub>2</sub>O<sub>3</sub> material was formed while the DLS and zeta potential analysis indicated average particles sizes of about 1300.9 nm and 31.2 mV respectively. The morphology and shape of the synthesized mineral was studied with FESEM and TEM while the elemental analysis was done with EDX. FESEM and TEM analysis show that the synthesized <bold>&#x03B1;-</bold> Fe<sub>2</sub>O<sub>3</sub> minerals were rod-like in shape while EDX analysis gave a good composition of the elements of the synthesized material. Therefore, this method may be applied to synthesize other forms of iron minerals or other inorganic materials at industrial scale especially when rod-like materials are needed.</p>
</abstract>
<kwd-group>
<kwd>Synthesis</kwd>
<kwd>Hematite</kwd>
<kwd>characterization</kwd>
<kwd>rod-like</kwd>
</kwd-group>
<counts>
<fig-count count="6"/>
<table-count count="1"/>
<ref-count count="10"/>
<page-count count="8"/>
</counts>
</article-meta>
</front>
<body>
<sec id="S1">
<title/>
<p>Iron based minerals have been used for centuries in many applications such as in science, technology and engineering. The use of iron oxides, hydroxides and oxohydroxides in different scales or sizes has been applied in medicine, as coloring pigment and in environmental remediation. Other areas where iron minerals have been utilized include microbial sciences, imaging systems, pharmaceutical sciences, biological products, civil engineering, immobilization techniques, and chemical industries. Among these iron based minerals, &#x03B1;-Fe<sub>2</sub>O<sub>3</sub> is a major component of various types of sediments, soils and iron ores and has gained prominent use as catalysts, electrodes, gas sensors, magnetic materials, photo catalyst, corrosion protective paints and for red pigment (1). Fe<sub>2</sub>O<sub>3</sub> has shown a special property in the adsorption of metal ion wastewater in different research work (2). As a result of its wide areas of applications, efforts have been made by various researchers to find the easiest and fastest method to synthesize it. Some of the methods that have been applied to synthesize &#x03B1;-Fe<sub>2</sub>O<sub>3</sub> include hydrolysis (2), co-precipitation [<xref ref-type="bibr" rid="R3">3</xref>, <xref ref-type="bibr" rid="R4">4</xref>, <xref ref-type="bibr" rid="R5">5</xref>], electrical explosion of iron [<xref ref-type="bibr" rid="R6">6</xref>], sol-gel method [<xref ref-type="bibr" rid="R7">7</xref>] and others. These synthesis methods have been used as templates by many researchers with many disadvantages including low yield of pure &#x03B1;-Fe<sub>2</sub>O<sub>3</sub> and multi-dimensional synthesized materials.</p>
<p>In this research work, we have designed an easy and simple hydrothermal approach for synthesizing pure rod-like &#x03B1;-Fe<sub>2</sub>O<sub>3</sub> in an alkaline medium using a hydrated salt of iron without any hard template or surfactants.</p>
</sec>
<sec id="S2">
<title>MATERIALS AND METHODS</title>
<p>Rod-like Fe<sub>2</sub>O<sub>3</sub> was synthesized with Fe(NO<sub>3</sub>)2.9H<sub>2</sub>O (98.0%) and NaOH (97.0 %). A 20 ml of ferric nitrate solution (0.2 M) with was prepared in a beaker with constant stirring at 600 rpm to a clear solution. Similarly, a 10 ml solution of 2.5 M NaOH was prepared in a beaker and stirred till the NaOH pellets completely dissolved in solution. The alkaline solution was gradually added to the nitrate solution in the beaker with continuous stirring at the same speed. After complete addition of the NaOH solution, the stirring is allowed to continue for 5 minutes and then transferred to the autoclave and water was added to make up about 80 % of the volume of the autoclave. The autoclave and its contents were transferred to an oven that was earlier put on to attain a temperature of 160&#x00B0;C for hydrothermal reaction for 46 hours including the 1 hour that the autoclave was allowed to attain the temperature of the oven environment. After the reaction time, the autoclave was brought out and allowed to cool naturally to prevent change in the composition and morphology of the content. After cooling to the ambient temperature, the precipitate was filtered and washed for several times with ethanol and doubly distilled water thoroughly till free of nitrate ions and other impurities and then dried in an oven at 100&#x00B0;C for 20 hours and the synthesized material was stored in a reagent bottle while a little quantity was taken for XRD, FTIR, FESEM, EDX, TEM, DLS and Zeta potential analysis.</p>
<sec id="S2_1">
<title>Spectroscopic Characterization of &#x03B1;-Fe<sub>2</sub>O<sub>3</sub></title>
<p>The phase identification of the synthesized mineral was characterized by X-ray diffractometer (XRD) with type empyrean series 2. The XRD pattern were recorded with 2&#x03B8; in the range of 10 &#x2013; 90&#x00B0;C with panalytical X-Pert high score (POM) equipped with Cu-K&#x03B1; (&#x03BB; = 1.54606 &#x00C5;) at a scan rate time of 24.765 seconds with a generating set of 40 mA and 45 Kv at a temperature of 25&#x00B0;C. The morphology of the synthesized material was characterized by field emission scanning electron microscopy (FESEM) with type ZEISS evolution series 2000, 25 kV and transmission electron microscopy (TEM) with type tecnai G2 20 twin, FEI Netherland, 80 kV. The Fe and O elemental analysis of the samples was performed by energy dispersive spectroscopy (EDS) type Anton paar Lenovo litesizier 500. All the measurements were carried out at room temperature.</p>
<table-wrap id="T1">
<label>Table 1</label>
<caption>
<p>List of XRD peaks for the synthesized rod-like &#x03B1;-Fe<sub>2</sub>O<sub>3</sub> by hydrothermal method</p>
</caption>
<graphic xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="IJASE-8-01-11-t001.jpg"/>
</table-wrap>
</sec>
</sec>
<sec id="S3">
<title>RESULTS AND DISCUSSION</title>
<p>X-ray diffraction spectroscopy (XRD) of the synthesized &#x03B1;-Fe<sub>2</sub>O<sub>3</sub> material by hydrothermal method at 45 Kv and 40 Am was used to identify crystalline phases of the sample. <xref ref-type="fig" rid="F1">Fig. 1a</xref> shows the XRD pattern of the powdered material which shows that &#x03B1;-Fe<sub>2</sub>O<sub>3</sub> was the only phase present.</p>
<fig id="F1">
<label>Fig. 1</label>
<caption>
<p><bold>(a)</bold> XRD pattern <bold>(b)</bold> Plot of identified phases of rod-like &#x03B1;-Fe<sub>2</sub>O<sub>3</sub> synthesized by hydrothermal method</p>
</caption>
<graphic xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="IJASE-8-01-11-f001.jpg"/>
</fig>
<p>The XRD peaks at 2&#x04E8; = 17.7153, 24.2008, 33.1810, 35.6822, 40.8855, 49.4759, 54.0560, 62.4567, 64.0193 and 71.9109 represented in <xref ref-type="table" rid="T1">Table 1</xref> correspond to the crystal planes (012), (104), (110), (113), (024), (116), (018), (214), (300) and (101) indexed as pure rhombohedra structure of &#x03B1;-Fe<sub>2</sub>O<sub>3</sub> (<italic>a =</italic> 5<italic>.</italic>0380 A&#x00B0;, <italic>c =</italic> 13<italic>.</italic>7720 A&#x00B0; )which is identified using the standard data file No. 98-016-1283 (JCPDS). The plot of the identified phases of the prepared material is also represented in <xref ref-type="fig" rid="F1">Fig. 1b</xref>. The peaks in the identifier plot correspond to peaks of pure phase of &#x03B1;-Fe<sub>2</sub>O<sub>3</sub> mineral [<xref ref-type="bibr" rid="R8">8</xref>, <xref ref-type="bibr" rid="R9">9</xref>, <xref ref-type="bibr" rid="R10">10</xref>].</p>
<p>The surface morphology of the synthesized material was studied using field emission scanning electron microscopy (FESEM) method of analysis. The images of the &#x03B1;-Fe<sub>2</sub>O<sub>3</sub> material as represented in <xref ref-type="fig" rid="F2">Fig. 2</xref> shows that &#x03B1;-Fe<sub>2</sub>O<sub>3</sub> samples prepared by hydrothermal method are rod-like in nature with little agglomeration.</p>
<fig id="F2">
<label>Fig. 2</label>
<caption>
<p>FESEM pattern for the rod-like &#x03B1;-Fe<sub>2</sub>O<sub>3</sub> synthesized by hydrothermal method</p>
</caption>
<graphic xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="IJASE-8-01-11-f002.jpg"/>
</fig>
<fig id="F3">
<label>Fig. 3</label>
<caption>
<p>EDS analysis for the rod-like &#x03B1;-Fe<sub>2</sub>O<sub>3</sub> synthesized by hydrothermal method</p>
</caption>
<graphic xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="IJASE-8-01-11-f003.jpg"/>
</fig>
<p>The transmission electron microscopic (TEM) method of analysis was carried out after the synthesis of &#x03B1;-Fe<sub>2</sub>O<sub>3</sub> mineral to confirm the growth pattern and the distribution of the crystallites sample. <xref ref-type="fig" rid="F4">Figure 4</xref> shows that the TEM image of the synthesized material by hydrothermal route is rod-like in structure which confirms the result obtained by FESEM analysis above. It can also be seen that the materials were prepared with less aggregation.</p>
<fig id="F4">
<label>Fig. 4</label>
<caption>
<p>TEM images for the rod-like &#x03B1;-Fe<sub>2</sub>O<sub>3</sub> synthesized by hydrothermal method</p>
</caption>
<graphic xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="IJASE-8-01-11-f004.jpg"/>
</fig>
<p>Elemental diffraction spectroscopy (EDS) was used to analyze the chemical composition of the material prepared by hydrothermal method under FESEM analysis. <xref ref-type="fig" rid="F3">Fig. 3</xref> shows the EDS analysis of the synthesized rod-like &#x03B1;-Fe<sub>2</sub>O<sub>3</sub> which confirms the presence of Fe and O with weight percent. The EDS result shows the peaks of iron and oxygen without any other elements present except the peak due to aluminium as a result of aluminium foil used to prepare the samples before analysis. The EDS result shows the degree of purity of the rod-like &#x03B1;-Fe<sub>2</sub>O<sub>3</sub> prepared by hydrothermal method.</p>
<p>The mean size of the ordered rod-like &#x03B1;-Fe<sub>2</sub>O<sub>3</sub> prepared by this method as represented in <xref ref-type="fig" rid="F5">Fig. 5</xref> was determined by using dynamic light scattering (DLS) method and was found to be about 1300.9 nm with a zeta potential of 31.20 mV as represented in <xref ref-type="fig" rid="F5a">Fig. 6</xref>.</p>
<fig id="F5">
<label>Fig. 5</label>
<caption>
<p>DLS analysis for the rod-like &#x03B1;-Fe<sub>2</sub>O<sub>3</sub> synthesized by hydrothermal method</p>
</caption>
<graphic xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="IJASE-8-01-11-f005.jpg"/>
</fig>
<fig id="F5a">
<label>Fig. 5</label>
<caption>
<p>Zeta potential analysis for the rod-like &#x03B1;-Fe<sub>2</sub>O<sub>3</sub> synthesized by hydrothermal method</p>
</caption>
<graphic xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="IJASE-8-01-11-f006.jpg"/>
</fig>
</sec>
<sec id="S4">
<title>CONCLUSIONS</title>
<p>Simple hydrothermal method has been successfully carried out to synthesize &#x03B1;-Fe<sub>2</sub>O<sub>3</sub>. XRD pattern shows rod-like structure of &#x03B1;-Fe<sub>2</sub>O<sub>3</sub>. A SEM image clearly shows that the morphology of the synthesized material is rod-like in shaped with less agglomerate. The TEM image also shows that the synthesized &#x03B1;-Fe<sub>2</sub>O<sub>3</sub> prepared by hydrothermal route has an average diameter of about 1300.9 nm and a zeta potential of 31.20 mV with less aggregation. The EDS result shows only peaks of iron (Fe) and oxygen (O<sub>2</sub>) in the absence of other impurities in the synthesized rod-like &#x03B1;-Fe<sub>2</sub>O<sub>3</sub>.</p>
</sec>
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