<?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">MSCE</journal-id><journal-title-group><journal-title>Journal of Materials Science and Chemical Engineering</journal-title></journal-title-group><issn pub-type="epub">2327-6045</issn><publisher><publisher-name>Scientific Research Publishing</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.4236/msce.2015.312005</article-id><article-id pub-id-type="publisher-id">MSCE-61955</article-id><article-categories><subj-group subj-group-type="heading"><subject>Articles</subject></subj-group><subj-group subj-group-type="Discipline-v2"><subject>Chemistry&amp;Materials Science</subject></subj-group></article-categories><title-group><article-title>
 
 
  Direct Preparation of the Nanocrystalline MnZn Ferrites by Using Oxalate as Precipitant
 
</article-title></title-group><contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Fei</surname><given-names>Hua</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>Cuicui</surname><given-names>Yin</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>Huanque</surname><given-names>Zhang</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>Qiangqiang</surname><given-names>Suo</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>Xin</surname><given-names>Wang</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>Huifen</surname><given-names>Peng</given-names></name><xref ref-type="aff" rid="aff1"><sup>1</sup></xref></contrib></contrib-group><aff id="aff2"><addr-line>School of Chemical Engineering, Hebei University of Technology, Tianjin, China</addr-line></aff><aff id="aff1"><addr-line>School of Materials Science &amp;amp; Engineering, Hebei University of Technology, Tianjin, China</addr-line></aff><pub-date pub-type="epub"><day>17</day><month>12</month><year>2015</year></pub-date><volume>03</volume><issue>12</issue><fpage>23</fpage><lpage>29</lpage><history><date date-type="received"><day>28</day>	<month>September</month>	<year>2015</year></date><date date-type="rev-recd"><day>accepted</day>	<month>10</month>	<year>December</year>	</date><date date-type="accepted"><day>17</day>	<month>December</month>	<year>2015</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>
 
 
   Oxalate was generally used as a precipitant for synthesis of MnZn ferrites during the co-precipitation process. However, the MnZn ferrite couldn’t be directly obtained and a calcination process was needed. In this research, we reported a direct preparation of the MnZn ferrite nanoparticles by using co-precipitation method, together with refluxing process. XRD measurements proved that crystallite size of the obtained samples increased with an increase in pH value of the co-precipitation solution, and that the crystallite size of about 25 nm was obtained for the sample at a pH of 13. This sample showed the maximum Ms of 58.6 emu/g, which was about one times larger than that of 12 (pH value). Calcination to the obtained samples result in an enlargement in their crystal size and an improvement in their magnetic properties with an increase in temperatures. The samples calcinated in CO<sub>2</sub> + H<sub>2</sub> atmosphere presented good stability, and the maximum Ms value of 188.2 emu/g was obtained for the 1100<sup>。</sup>C-heated sample. Unfortunately, precipitation of some Fe<sub>2</sub>O<sub>3</sub> at 800<sup>。</sup>C suggested poor stability of the nanocrystalline MnZn ferrite in N<sub>2</sub> atmosphere.  
     
 
</p></abstract><kwd-group><kwd>Magnetic Material</kwd><kwd> MnZn Ferrite</kwd><kwd> Co-Precipitation Process</kwd><kwd> Nanocrystalline Material</kwd></kwd-group></article-meta></front><body><sec id="s1"><title>1. Introduction</title><p>MnZn ferrite is one of the most important soft ferrites, which present high magnetic permeability, high saturation magnetization, high resistivity, low coercivity, low power losses and so on [<xref ref-type="bibr" rid="scirp.61955-ref1">1</xref>]. It is widely used in many fields, such as deflection yoke rings, computer memory chips, magnetic recording heads, microwave devices, transducers, transformers and so on [<xref ref-type="bibr" rid="scirp.61955-ref2">2</xref>]. Additionally, nano-sized MnZn ferrite is a good candidate for biomedical purposes, including magnetically guided drug delivery and magnetic resonance image [<xref ref-type="bibr" rid="scirp.61955-ref3">3</xref>], because of its high magnetic moment, good chemical stability and reactive surfaces when attaching to biological molecules [<xref ref-type="bibr" rid="scirp.61955-ref4">4</xref>].</p><p>Ferrite is usually synthesized by the conventional ceramic technique, where high temperature is needed in order for enough solid-state reactions between raw materials, large and inhomogeneous particles, together with some impurities, greatly restrict magnetic properties of the products [<xref ref-type="bibr" rid="scirp.61955-ref5">5</xref>]-[<xref ref-type="bibr" rid="scirp.61955-ref7">7</xref>]. Therefore, wet chemical synthesis like co-precipitation [<xref ref-type="bibr" rid="scirp.61955-ref8">8</xref>]-[<xref ref-type="bibr" rid="scirp.61955-ref10">10</xref>], sol-gel [<xref ref-type="bibr" rid="scirp.61955-ref11">11</xref>] [<xref ref-type="bibr" rid="scirp.61955-ref12">12</xref>], hydrothermal method [<xref ref-type="bibr" rid="scirp.61955-ref13">13</xref>], and micro-emulsion process [<xref ref-type="bibr" rid="scirp.61955-ref14">14</xref>] [<xref ref-type="bibr" rid="scirp.61955-ref15">15</xref>] is expected for the production of ferrites with excellent magnetic properties. Among these methods, co-precipi- tation process is often used to the preparation of the homogeneous ferrite nanoparticles [<xref ref-type="bibr" rid="scirp.61955-ref4">4</xref>]. During this process, oxalate is generally used as a precipitant to prepare the ferrite powder. Angerman et al. [<xref ref-type="bibr" rid="scirp.61955-ref16">16</xref>] reported that β-oxalate with orthorhombic structure was formed when precipitating at room temperature, and that monoclinic α-oxalate was obtained at 90˚C. Those oxalates could be completely transformed to ferrite when decomposition at 650˚C [<xref ref-type="bibr" rid="scirp.61955-ref17">17</xref>]. On the other hand, Fritsch et al. [<xref ref-type="bibr" rid="scirp.61955-ref18">18</xref>] found that Mn-riched ferrite (Fe<sub>3−x</sub>Mn<sub>x□3δ/4</sub>O<sub>4+δ</sub>) with x &gt; 1.5 presented complex structures like cubic, tetragonal or a mixture of them. This phenomenon should be attributed to the lack of miscibility at low temperature in the Fe<sub>3</sub>O<sub>4</sub>-Mn<sub>3</sub>O<sub>4</sub> system. In this paper, nanocrystaline MnZn ferrite was directly synthesized at room temperature by using the co-precipitation method, followed by a refluxing process. We investigated structures of the products and their phase transitions during heating under different atmosphere.</p></sec><sec id="s2"><title>2. Experimental</title><sec id="s2_1"><title>2.1. Sample Preparation</title><p>Reagent-grade FeCl<sub>3</sub>∙6H<sub>2</sub>O (Bodi Chemical, Tianjin, 99%), ZnSO<sub>4</sub>∙7H<sub>2</sub>O (Bodi Chemical, Tianjin, 99.5%), MnSO<sub>4</sub>∙H<sub>2</sub>O (Bodi Chemical, Tianjin, 99%) were used as starting materials. Reagent-grade (NH<sub>4</sub>) <sub>2</sub>C <sub>2</sub>O<sub>4</sub>∙H<sub>2</sub>O (Fengchen Chemical, Tianjin, 99.8%) and NaOH (Bodi Chemical, Tianjin, 99%) were used as co-precipitants, they were dissolved into de-ionized water at a concentration of 0.2mol/L and 6mol/L, respectively. NH<sub>3</sub>∙H<sub>2</sub>O (Fengchen Chemical, Tianjin, 25%) was used during precipitation at a concentration of about 5%.</p><p>The starting materials were weighed according to the formula Mn<sub>0.7</sub>Zn<sub>0.2</sub>Fe<sub>2.1</sub>O<sub>4</sub>. Suitable (NH<sub>4</sub>) <sub>2</sub>C <sub>2</sub>O<sub>4</sub>∙H<sub>2</sub>O and NH<sub>3</sub>∙H<sub>2</sub>O were initially added into 0.1 mol/L FeCl<sub>3</sub>∙6H<sub>2</sub>O solution under constant magnetic stirring to remain pH value of the solution at about 4. Then 0.9 mol/L MnSO<sub>4</sub>∙H<sub>2</sub>O and 0.2 mol/L ZnSO<sub>4</sub>∙7H<sub>2</sub>O were introduced to the above solution. The (NH<sub>4</sub>) <sub>2</sub>C <sub>2</sub>O<sub>4</sub>∙H<sub>2</sub>O and NH<sub>3</sub>・H<sub>2</sub>O were re-added into the solution till its pH value of 8.5. At last, NaOH was added to the solution until its pH value of 13. Then the solution was refluxed for 7 h. The obtained precipitated product was washed with distilled water until a clear solution, and then dried at 80˚C for 7 h. The dried powder was calcinated between 400˚C to 1200˚C under different atmosphere.</p></sec><sec id="s2_2"><title>2.2. Sample Characterization</title><p>X-ray diffraction (XRD) patterns were recorded at room temperature with a Bruker AXS X-ray diffractometer using a Cu-Kα radiation at a continuous scanning rate of 10 min<sup>−1</sup> in the 2θ range of 10˚ to 90˚. Crystallite size of the samples was calculated according to (311) peak in the XRD patterns using the Debye-Scherrer’s equation:</p><disp-formula id="scirp.61955-formula7"><label>(1)</label><graphic position="anchor" xlink:href="http://html.scirp.org/file/61955x4.png"  xlink:type="simple"/></disp-formula><p>where λ is the X-ray wavelength, θ is Bragg’s angle and β is full width at half the maxima (FWHM). The saturation magnetization M<sub>s</sub>, remanence magnetization, M<sub>r</sub>, and coercive force, H<sub>c</sub>, of the samples were calculated in terms of hysteresis loops measured by LakeShore-7400 vibrating sample magnetometer (VSM). In order to identify possible phase transformation in samples, the TG/DTA measurements were conducted in N<sub>2</sub> between 25˚C and 1200˚C at a rate of 10˚C min<sup>−1</sup> using a Thermo Analyzer (TA, SDT-DTA 2960).</p></sec></sec><sec id="s3"><title>3. Results and Discussion</title><p><xref ref-type="fig" rid="fig1">Figure 1</xref> shows XRD patterns of as-synthesized samples, of which XRD peaks match well with those of the spinel MnZn ferrite (JCPDS No.74-2402). Almost no other peaks are found in the XRD patterns. Those results suggest that the samples prepared at different pH values are pure MnZn ferrite with spinel structure. In addition, apparent widening in the XRD peaks indicates a nano-scale crystallit size in those samples, and the narrower XRD peaks suggest that the crystals enlarge with an increase in the pH values (about 17 nm at pH of 12, and 25 nm at pH of 13).</p><p><xref ref-type="fig" rid="fig2">Figure 2</xref> shows the measured room-temperature hysteresis loops of the samples in <xref ref-type="fig" rid="fig1">Figure 1</xref>. Upon increasing pH values in the co-precipitation solutions, the saturation magnetization, M<sub>s</sub>, apparently increase. And the</p><fig id="fig1"  position="float"><label><xref ref-type="fig" rid="fig1">Figure 1</xref></label><caption><title> XRD patterns for the samples synthesized at various pH values</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/61955x5.png"/></fig><fig id="fig2"  position="float"><label><xref ref-type="fig" rid="fig2">Figure 2</xref></label><caption><title> Magnetic hysteresis loops for the samples in <xref ref-type="fig" rid="fig1">Figure 1</xref></title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/61955x6.png"/></fig><p>maximum M<sub>s</sub> of 58.6 emu/g is obtained in the sample at a pH of 13. This M<sub>s</sub> value is almost the highest one reported recently [<xref ref-type="bibr" rid="scirp.61955-ref5">5</xref>] [<xref ref-type="bibr" rid="scirp.61955-ref19">19</xref>]-[<xref ref-type="bibr" rid="scirp.61955-ref22">22</xref>], is about one times larger than that of pH = 12. Similar results were reported by Narasimhan et al. [<xref ref-type="bibr" rid="scirp.61955-ref23">23</xref>].</p><p>It is known that magnetism of the powdered MnZn ferrite is tightly related to its crystal size. Szczygiel et al. [<xref ref-type="bibr" rid="scirp.61955-ref24">24</xref>]<sup> </sup>found that superparamagnetism occurred in the MnZn ferrite powder with its crystal size less than 10 nm. Therefore, decrease in M<sub>s</sub> with decrease in pH value should be attributable to the decrease in the crystallite size of the samples in the present research.</p><p>It is reported that MnZn ferrite cannot be directly obtained by using oxalate as precipitant during the co-pre- cipitation process, and that heat treatment at certain temperature is generally needed to precursor [<xref ref-type="bibr" rid="scirp.61955-ref16">16</xref>] [<xref ref-type="bibr" rid="scirp.61955-ref22">22</xref>]. Results obtained in the present research not only simplify the preparation process of the MnZn ferrite, but also improve its quality because inclusion is easily produced during the heat treatment.</p><p><xref ref-type="fig" rid="fig3">Figure 3</xref> shows thermal analysis curves of the sample prepared at pH of 13. Total mass loss of the sample is about 8% during heating between room temperature and 1000˚C, and the sharp mass loss occurring below 400˚C should be attributable to evaporation of the adsorbed water and the crystallized water contained in the sample. No apparent endothermal or exothermal peaks are found in the DTA curves. Those results further prove that the samples prepared in this research are pure MnZn ferrite.</p><p>The MnZn ferrite is generally used in the bulk state, and then a sintering process is needed for the powdered one. However, the MnZn ferrite is reported to easily decompose according to Equation (2) in a heated state</p><fig id="fig3"  position="float"><label><xref ref-type="fig" rid="fig3">Figure 3</xref></label><caption><title> TG and DTA curves measured in N<sub>2</sub> for the sample at pH of 13</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/61955x7.png"/></fig><p>under the oxidation atmosphere [<xref ref-type="bibr" rid="scirp.61955-ref2">2</xref>], and precipitation of Fe<sub>2</sub>O<sub>3</sub> greatly deteriorates its magnetic properties.</p><disp-formula id="scirp.61955-formula8"><label>(2)</label><graphic position="anchor" xlink:href="http://html.scirp.org/file/61955x8.png"  xlink:type="simple"/></disp-formula><p>Accordingly, we investigate phase transitions and variation in magnetic properties of the prepared samples during calcinations. <xref ref-type="fig" rid="fig4">Figure 4</xref> shows XRD patterns of the calcinated samples under different atmosphere. XRD patterns of the uncalcinated ones are also presented in this figure for comparison. Under certain atmosphere, XRD peaks of the sample become stronger in intensity and narrower in width, followed by a gradual color variation form brown to dark brown, with an increase in the calcination temperature. It is noteworthy that some XRD peaks attributable to Fe<sub>2</sub>O<sub>3</sub>, concomitant with a reddish color in sample, appear in the XRD pattern of the sample calcinated at 800˚C under N<sub>2</sub> atmosphere. Further calcination at high temperature results in disappearance of those XRD peaks. Precipitation of some Fe<sub>2</sub>O<sub>3</sub> from the MnZn ferrite may result from a little oxygen existing in the N<sub>2 </sub>atmosphere. In contrast, the CO<sub>2</sub> + H<sub>2</sub> atmosphere is favorable to remain stability of the MnZn ferrite.</p><p>The measured hysteresis loops of the samples corresponding to those in <xref ref-type="fig" rid="fig4">Figure 4</xref> are shown in <xref ref-type="fig" rid="fig5">Figure 5</xref>. Their magnetization nearly saturates at the maximum field of 20 kOe, the magnetic parameters like M<sub>s</sub>, M<sub>r</sub> and H<sub>c</sub> calculated according to <xref ref-type="fig" rid="fig5">Figure 5</xref> are presented in <xref ref-type="table" rid="table1">Table 1</xref>. Decrease in M<sub>s</sub> with an increase in the calcination temperature below 800˚C under N<sub>2</sub> atmosphere should be related to decomposition of the MnZn ferrite or precipitation of non-magnetic Fe<sub>2</sub>O<sub>3</sub>, shown in <xref ref-type="fig" rid="fig4">Figure 4</xref>(a). Solution of the Fe<sub>2</sub>O<sub>3</sub> into the MnZn ferrites at 1000˚C results in a sharp increase in M<sub>s</sub> from 27.1 to 80.3 emu/g. On the other hand, the M<sub>s</sub> gradually increases with an increase in the calcination temperature below 1100˚C for the samples calainated under CO<sub>2</sub> + H<sub>2</sub> atmosphere, concomitant with a decrease in H<sub>c</sub>. The highest M<sub>s</sub> of 188.2 emu/g is obtained for the sample, with the crystallite size of about 68.1 nm, calcinated at 1000˚C. This is consistent with growth in crystallite size of samples during the calcination. The sharp decrease in M<sub>s</sub> at 1200˚C is perhaps related to evaporation of some elements like Zn at high temperate. The M<sub>s</sub> of the samples under CO<sub>2</sub> + H<sub>2</sub> is larger than that of N<sub>2</sub>at same calcinations temperature.</p></sec><sec id="s4"><title>4. Conclusion</title><p>MnZn ferrite nanoparticles could be directly prepared by using co-precipitation and then refluxing process. Crystallite size of the obtained samples increased with an increase in pH value of the co-precipitation solution, and that the crystallite size of about 25 nm was obtained for the sample at a pH of 13. This sample also showed the maximum M<sub>s</sub> of 58.6 emu/g, which was about one times larger than that of 12 (pH value). Calcination to the obtained samples resulted in an enlargement in their crystal size and an improvement in magnetic properties with an increase in temperatures. The samples calcinated in CO<sub>2</sub> + H<sub>2</sub> atmosphere presented good stability, and the maximum M<sub>s</sub> of 188.2 emu/g was obtained for the sample heated at 1100˚C. Unfortunately, precipitation of some Fe<sub>2</sub>O<sub>3</sub> at 800˚C suggested poor stability of the nanocrystalline MnZn ferrite in N<sub>2</sub> atmosphere.</p><fig id="fig4"  position="float"><label><xref ref-type="fig" rid="fig4">Figure 4</xref></label><caption><title> XRD patterns of the samples under different temperatures, (a) N<sub>2</sub> and (b) CO<sub>2</sub> + H<sub>2</sub></title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/61955x9.png"/></fig><fig id="fig5"  position="float"><label><xref ref-type="fig" rid="fig5">Figure 5</xref></label><caption><title> Hysteresis loops of the samples corresponding to those in <xref ref-type="fig" rid="fig4">Figure 4</xref>, (a) N<sub>2</sub> and (b) CO<sub>2</sub> + H<sub>2</sub></title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/61955x10.png"/></fig><table-wrap id="table1" ><label><xref ref-type="table" rid="table1">Table 1</xref></label><caption><title> Magnetic properties of the samples calculated in terms of <xref ref-type="fig" rid="fig5">Figure 5</xref></title></caption><table><tbody><thead><tr><th align="center" valign="middle" >atmosphere</th><th align="center" valign="middle" >Calcined Temperature T (˚C)</th><th align="center" valign="middle" >M<sub>s</sub> (emu/g)</th><th align="center" valign="middle" >H<sub>c</sub> (Oe)</th><th align="center" valign="middle" >M<sub>r</sub> (emu/g)</th><th align="center" valign="middle" >Crystallite size (nm)</th></tr></thead><tr><td align="center" valign="middle"  rowspan="5"  >N<sub>2</sub></td><td align="center" valign="middle" >400</td><td align="center" valign="middle" >43.9</td><td align="center" valign="middle" >118.4</td><td align="center" valign="middle" >7.3</td><td align="center" valign="middle" >32.9</td></tr><tr><td align="center" valign="middle" >600</td><td align="center" valign="middle" >35.7</td><td align="center" valign="middle" >80.1</td><td align="center" valign="middle" >4.0</td><td align="center" valign="middle" >18.5</td></tr><tr><td align="center" valign="middle" >800</td><td align="center" valign="middle" >27.1</td><td align="center" valign="middle" >58.4</td><td align="center" valign="middle" >2.2</td><td align="center" valign="middle" >26.0</td></tr><tr><td align="center" valign="middle" >1000</td><td align="center" valign="middle" >80.3</td><td align="center" valign="middle" >135.1</td><td align="center" valign="middle" >11.4</td><td align="center" valign="middle" >52.8</td></tr><tr><td align="center" valign="middle" >1200</td><td align="center" valign="middle" >87.2</td><td align="center" valign="middle" >123.6</td><td align="center" valign="middle" >9.8</td><td align="center" valign="middle" >81.6</td></tr><tr><td align="center" valign="middle"  rowspan="5"  >CO<sub>2</sub> + H<sub>2</sub></td><td align="center" valign="middle" >600</td><td align="center" valign="middle" >73.1</td><td align="center" valign="middle" >195.3</td><td align="center" valign="middle" >14.1</td><td align="center" valign="middle" >31.7</td></tr><tr><td align="center" valign="middle" >800</td><td align="center" valign="middle" >90.9</td><td align="center" valign="middle" >175.7</td><td align="center" valign="middle" >17.2</td><td align="center" valign="middle" >33.5</td></tr><tr><td align="center" valign="middle" >1000</td><td align="center" valign="middle" >90.8</td><td align="center" valign="middle" >128.1</td><td align="center" valign="middle" >9.0</td><td align="center" valign="middle" >63.4</td></tr><tr><td align="center" valign="middle" >1100</td><td align="center" valign="middle" >180.2</td><td align="center" valign="middle" >128.6</td><td align="center" valign="middle" >18.9</td><td align="center" valign="middle" >68.1</td></tr><tr><td align="center" valign="middle" >1200</td><td align="center" valign="middle" >92.6</td><td align="center" valign="middle" >126.1</td><td align="center" valign="middle" >9.0</td><td align="center" valign="middle" >69.3</td></tr></tbody></table></table-wrap></sec><sec id="s5"><title>Acknowledgements</title><p>This work was supported by Tianjin Research Program of Application Foundation and Advanced Technology (major project) under a contract No.15JEZDJC31000.</p></sec><sec id="s6"><title>Cite this paper</title><p>Fei Hua,Cuicui Yin,Huanque Zhang,Qiangqiang Suo,Xin Wang,Huifen Peng, (2015) Direct Preparation of the Nanocrystalline MnZn Ferrites by Using Oxalate as Precipitant. 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