Mössbauer study of copper ferrite diluted by Ga3+ and Al3+ ions
Mössbauer spectra of the CuGa x Al 2 x Fe 2 − 3 x O 4 system ( x = 0.1, 0.2, 0.3, 0.4, 0.5) have been studied at a temperature of 295 K. The results obtained are compared with Mössbauer data for the CuGa x Al x Fe 2−2 x O 4 system. It is established that the hyperfine magnetic fields H B (for octahe...
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| Veröffentlicht in: | Physics of the solid state 2009-04, Vol.51 (4), p.781-784 |
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| container_title | Physics of the solid state |
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| creator | Antoshina, L. G. Evstaf’eva, E. N. Opalenko, A. A. |
| description | Mössbauer spectra of the CuGa
x
Al
2
x
Fe
2 − 3
x
O
4
system (
x
= 0.1, 0.2, 0.3, 0.4, 0.5) have been studied at a temperature of 295 K. The results obtained are compared with Mössbauer data for the CuGa
x
Al
x
Fe
2−2
x
O
4
system. It is established that the hyperfine magnetic fields
H
B
(for octahedral sites) and
H
A
(for tetrahedral sites) for ferrites in both systems with ferrimagnetic ordering decrease linearly depending on the total number of nonmagnetic ions in octahedral and tetrahedral sites of the two systems. |
| doi_str_mv | 10.1134/S1063783409040246 |
| format | Article |
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x
Al
2
x
Fe
2 − 3
x
O
4
system (
x
= 0.1, 0.2, 0.3, 0.4, 0.5) have been studied at a temperature of 295 K. The results obtained are compared with Mössbauer data for the CuGa
x
Al
x
Fe
2−2
x
O
4
system. It is established that the hyperfine magnetic fields
H
B
(for octahedral sites) and
H
A
(for tetrahedral sites) for ferrites in both systems with ferrimagnetic ordering decrease linearly depending on the total number of nonmagnetic ions in octahedral and tetrahedral sites of the two systems.</description><identifier>ISSN: 1063-7834</identifier><identifier>EISSN: 1090-6460</identifier><identifier>DOI: 10.1134/S1063783409040246</identifier><language>eng</language><publisher>Dordrecht: SP MAIK Nauka/Interperiodica</publisher><subject>Magnetism and Ferroelectricity ; Physics ; Physics and Astronomy ; Solid State Physics</subject><ispartof>Physics of the solid state, 2009-04, Vol.51 (4), p.781-784</ispartof><rights>Pleiades Publishing, Ltd. 2009</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><cites>FETCH-LOGICAL-c170t-3946b13f14330af9da0cd7d2ec743d7f6c9398e36cb17273b0870c6ce7a0a4713</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1134/S1063783409040246$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1134/S1063783409040246$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,776,780,27901,27902,41464,42533,51294</link.rule.ids></links><search><creatorcontrib>Antoshina, L. G.</creatorcontrib><creatorcontrib>Evstaf’eva, E. N.</creatorcontrib><creatorcontrib>Opalenko, A. A.</creatorcontrib><title>Mössbauer study of copper ferrite diluted by Ga3+ and Al3+ ions</title><title>Physics of the solid state</title><addtitle>Phys. Solid State</addtitle><description>Mössbauer spectra of the CuGa
x
Al
2
x
Fe
2 − 3
x
O
4
system (
x
= 0.1, 0.2, 0.3, 0.4, 0.5) have been studied at a temperature of 295 K. The results obtained are compared with Mössbauer data for the CuGa
x
Al
x
Fe
2−2
x
O
4
system. It is established that the hyperfine magnetic fields
H
B
(for octahedral sites) and
H
A
(for tetrahedral sites) for ferrites in both systems with ferrimagnetic ordering decrease linearly depending on the total number of nonmagnetic ions in octahedral and tetrahedral sites of the two systems.</description><subject>Magnetism and Ferroelectricity</subject><subject>Physics</subject><subject>Physics and Astronomy</subject><subject>Solid State Physics</subject><issn>1063-7834</issn><issn>1090-6460</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2009</creationdate><recordtype>article</recordtype><recordid>eNp9kM9KxDAQh4MouK4-gLfcpTrTicn25rLoKqx4UM8lzR_pUtuStIe-mC_gi5my3gRP8w0z3zD8GLtEuEYkcfOKIEmtSEABAnIhj9gCE2dSSDieWVI2z0_ZWYx7AES8LRbs7vn7K8ZKjy7wOIx24p3npuv71HsXQj04butmHJzl1cS3mq64bi1fNwnqro3n7MTrJrqL37pk7w_3b5vHbPeyfdqsd5lBBUNGhZAVkkdBBNoXVoOxyubOKEFWeWkKKlaOpKlQ5YoqWCkw0jilQQuFtGR4uGtCF2NwvuxD_anDVCKUcwTlnwiSkx-cmHbbDxfKfTeGNr35j_QDnXFcVw</recordid><startdate>20090401</startdate><enddate>20090401</enddate><creator>Antoshina, L. G.</creator><creator>Evstaf’eva, E. N.</creator><creator>Opalenko, A. A.</creator><general>SP MAIK Nauka/Interperiodica</general><scope>AAYXX</scope><scope>CITATION</scope></search><sort><creationdate>20090401</creationdate><title>Mössbauer study of copper ferrite diluted by Ga3+ and Al3+ ions</title><author>Antoshina, L. G. ; Evstaf’eva, E. N. ; Opalenko, A. A.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c170t-3946b13f14330af9da0cd7d2ec743d7f6c9398e36cb17273b0870c6ce7a0a4713</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2009</creationdate><topic>Magnetism and Ferroelectricity</topic><topic>Physics</topic><topic>Physics and Astronomy</topic><topic>Solid State Physics</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Antoshina, L. G.</creatorcontrib><creatorcontrib>Evstaf’eva, E. N.</creatorcontrib><creatorcontrib>Opalenko, A. A.</creatorcontrib><collection>CrossRef</collection><jtitle>Physics of the solid state</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Antoshina, L. G.</au><au>Evstaf’eva, E. N.</au><au>Opalenko, A. A.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Mössbauer study of copper ferrite diluted by Ga3+ and Al3+ ions</atitle><jtitle>Physics of the solid state</jtitle><stitle>Phys. Solid State</stitle><date>2009-04-01</date><risdate>2009</risdate><volume>51</volume><issue>4</issue><spage>781</spage><epage>784</epage><pages>781-784</pages><issn>1063-7834</issn><eissn>1090-6460</eissn><abstract>Mössbauer spectra of the CuGa
x
Al
2
x
Fe
2 − 3
x
O
4
system (
x
= 0.1, 0.2, 0.3, 0.4, 0.5) have been studied at a temperature of 295 K. The results obtained are compared with Mössbauer data for the CuGa
x
Al
x
Fe
2−2
x
O
4
system. It is established that the hyperfine magnetic fields
H
B
(for octahedral sites) and
H
A
(for tetrahedral sites) for ferrites in both systems with ferrimagnetic ordering decrease linearly depending on the total number of nonmagnetic ions in octahedral and tetrahedral sites of the two systems.</abstract><cop>Dordrecht</cop><pub>SP MAIK Nauka/Interperiodica</pub><doi>10.1134/S1063783409040246</doi><tpages>4</tpages></addata></record> |
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| ispartof | Physics of the solid state, 2009-04, Vol.51 (4), p.781-784 |
| issn | 1063-7834 1090-6460 |
| language | eng |
| recordid | cdi_crossref_primary_10_1134_S1063783409040246 |
| source | SpringerLink Journals |
| subjects | Magnetism and Ferroelectricity Physics Physics and Astronomy Solid State Physics |
| title | Mössbauer study of copper ferrite diluted by Ga3+ and Al3+ ions |
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