Synthesis and magnetic properties of Fe substituted hibonite
We have investigated the synthesis conditions and magnetic properties of Fe substituted hibonite with initial compositions of CaAl12-xFexO19 (0≤x≤12) and CaAl10-xFexO19-δ (0≤x≤10). The Fe doped hibonite can be synthesized at a sintering temperature of 1300˚C. The X-ray diffraction patterns of Fe s...
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| Veröffentlicht in: | Journal of the Magnetics Society of Japan 2017, Vol.41(2), pp.20-24 |
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| container_title | Journal of the Magnetics Society of Japan |
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| creator | Nagumo, H. Watanabe, K. Kakizaki, K. Kamishima, K. |
| description | We have investigated the synthesis conditions and magnetic properties of Fe substituted hibonite with initial compositions of CaAl12-xFexO19 (0≤x≤12) and CaAl10-xFexO19-δ (0≤x≤10). The Fe doped hibonite can be synthesized at a sintering temperature of 1300˚C. The X-ray diffraction patterns of Fe substituted hibonite samples are in good agreement with the pattern of hibonite. The lattice parameter increased due to the difference between the radius of Al3+ and that of Fe3+. The magnetization and Curie temperature of the best sample (CaAl2Fe8O19-δ) are 31 emu/g and 290˚C, respectively. |
| doi_str_mv | 10.3379/msjmag.1701R001 |
| format | Article |
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The Fe doped hibonite can be synthesized at a sintering temperature of 1300˚C. The X-ray diffraction patterns of Fe substituted hibonite samples are in good agreement with the pattern of hibonite. The lattice parameter increased due to the difference between the radius of Al3+ and that of Fe3+. The magnetization and Curie temperature of the best sample (CaAl2Fe8O19-δ) are 31 emu/g and 290˚C, respectively.</description><identifier>ISSN: 1882-2924</identifier><identifier>EISSN: 1882-2932</identifier><identifier>DOI: 10.3379/msjmag.1701R001</identifier><language>eng</language><publisher>Tokyo: The Magnetics Society of Japan</publisher><subject>Curie temperature ; Diffraction patterns ; hexaferrite ; M-type ; Magnetic properties ; Materials substitution ; Synthesis</subject><ispartof>Journal of the Magnetics Society of Japan, 2017, Vol.41(2), pp.20-24</ispartof><rights>2017 The Magnetics Society of Japan</rights><rights>Copyright Japan Science and Technology Agency 2017</rights><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c3401-fc0e4144c5543aa2054566584f82fd6152846d8f94122313e3fbc49a2766b4c23</citedby><cites>FETCH-LOGICAL-c3401-fc0e4144c5543aa2054566584f82fd6152846d8f94122313e3fbc49a2766b4c23</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,776,780,1877,4010,27900,27901,27902</link.rule.ids></links><search><creatorcontrib>Nagumo, H.</creatorcontrib><creatorcontrib>Watanabe, K.</creatorcontrib><creatorcontrib>Kakizaki, K.</creatorcontrib><creatorcontrib>Kamishima, K.</creatorcontrib><title>Synthesis and magnetic properties of Fe substituted hibonite</title><title>Journal of the Magnetics Society of Japan</title><addtitle>J. Magn. Soc. Jpn.</addtitle><description> We have investigated the synthesis conditions and magnetic properties of Fe substituted hibonite with initial compositions of CaAl12-xFexO19 (0≤x≤12) and CaAl10-xFexO19-δ (0≤x≤10). The Fe doped hibonite can be synthesized at a sintering temperature of 1300˚C. The X-ray diffraction patterns of Fe substituted hibonite samples are in good agreement with the pattern of hibonite. The lattice parameter increased due to the difference between the radius of Al3+ and that of Fe3+. The magnetization and Curie temperature of the best sample (CaAl2Fe8O19-δ) are 31 emu/g and 290˚C, respectively.</description><subject>Curie temperature</subject><subject>Diffraction patterns</subject><subject>hexaferrite</subject><subject>M-type</subject><subject>Magnetic properties</subject><subject>Materials substitution</subject><subject>Synthesis</subject><issn>1882-2924</issn><issn>1882-2932</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2017</creationdate><recordtype>article</recordtype><recordid>eNo9kMtLw0AQxhdRsFbPXgOe0-5jstmAFymtCgXBx3nZbGbbhDapu5tD_3tTYnuZGZjfN4-PkEdGZ0LkxXwfmr3ZzFhO2Sel7IpMmFI85YXg15eawy25C6GhVOZCyQl5_jq2cYuhDolpq2SY0GKsbXLw3QF9rDEknUtWmIS-DLGOfcQq2dZl19YR78mNM7uAD_95Sn5Wy-_FW7r-eH1fvKxTK4Cy1FmKwABsloEwhtMMMikzBU5xV0mWcQWyUq4AxrlgAoUrLRSG51KWYLmYkqdx7nDVb48h6qbrfTus1EzlADmIQg7UfKSs70Lw6PTB13vjj5pRfbJIjxbps0WDYjkqmhDNBi-8GR63OzzzwDQ_hbPu0rdb4zW24g8rFHI4</recordid><startdate>2017</startdate><enddate>2017</enddate><creator>Nagumo, H.</creator><creator>Watanabe, K.</creator><creator>Kakizaki, K.</creator><creator>Kamishima, K.</creator><general>The Magnetics Society of Japan</general><general>Japan Science and Technology Agency</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7SP</scope><scope>7U5</scope><scope>8BQ</scope><scope>8FD</scope><scope>JG9</scope><scope>L7M</scope></search><sort><creationdate>2017</creationdate><title>Synthesis and magnetic properties of Fe substituted hibonite</title><author>Nagumo, H. ; Watanabe, K. ; Kakizaki, K. ; Kamishima, K.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c3401-fc0e4144c5543aa2054566584f82fd6152846d8f94122313e3fbc49a2766b4c23</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2017</creationdate><topic>Curie temperature</topic><topic>Diffraction patterns</topic><topic>hexaferrite</topic><topic>M-type</topic><topic>Magnetic properties</topic><topic>Materials substitution</topic><topic>Synthesis</topic><toplevel>online_resources</toplevel><creatorcontrib>Nagumo, H.</creatorcontrib><creatorcontrib>Watanabe, K.</creatorcontrib><creatorcontrib>Kakizaki, K.</creatorcontrib><creatorcontrib>Kamishima, K.</creatorcontrib><collection>CrossRef</collection><collection>Electronics & Communications Abstracts</collection><collection>Solid State and Superconductivity Abstracts</collection><collection>METADEX</collection><collection>Technology Research Database</collection><collection>Materials Research Database</collection><collection>Advanced Technologies Database with Aerospace</collection><jtitle>Journal of the Magnetics Society of Japan</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Nagumo, H.</au><au>Watanabe, K.</au><au>Kakizaki, K.</au><au>Kamishima, K.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Synthesis and magnetic properties of Fe substituted hibonite</atitle><jtitle>Journal of the Magnetics Society of Japan</jtitle><addtitle>J. Magn. Soc. Jpn.</addtitle><date>2017</date><risdate>2017</risdate><volume>41</volume><issue>2</issue><spage>20</spage><epage>24</epage><pages>20-24</pages><issn>1882-2924</issn><eissn>1882-2932</eissn><abstract> We have investigated the synthesis conditions and magnetic properties of Fe substituted hibonite with initial compositions of CaAl12-xFexO19 (0≤x≤12) and CaAl10-xFexO19-δ (0≤x≤10). The Fe doped hibonite can be synthesized at a sintering temperature of 1300˚C. The X-ray diffraction patterns of Fe substituted hibonite samples are in good agreement with the pattern of hibonite. The lattice parameter increased due to the difference between the radius of Al3+ and that of Fe3+. The magnetization and Curie temperature of the best sample (CaAl2Fe8O19-δ) are 31 emu/g and 290˚C, respectively.</abstract><cop>Tokyo</cop><pub>The Magnetics Society of Japan</pub><doi>10.3379/msjmag.1701R001</doi><tpages>5</tpages><oa>free_for_read</oa></addata></record> |
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| language | eng |
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| subjects | Curie temperature Diffraction patterns hexaferrite M-type Magnetic properties Materials substitution Synthesis |
| title | Synthesis and magnetic properties of Fe substituted hibonite |
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