Frustration wave order in iron(II) oxide spinels
Frustrated magnetic materials can show unconventional correlations such as quantum spin liquid states and monopole excitations in spin ices. These phenomena are observed on uniformly frustrated lattices such as triangular, kagome or pyrochlore types, where all nearest neighbour interactions are equi...
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creator | Perversi, Giuditta Arevalo-Lopez, Angel M. Ritter, Clemens Attfield, J. Paul |
description | Frustrated magnetic materials can show unconventional correlations such as quantum spin liquid states and monopole excitations in spin ices. These phenomena are observed on uniformly frustrated lattices such as triangular, kagome or pyrochlore types, where all nearest neighbour interactions are equivalent. Here we report incommensurate long-range spin amplitude waves in the spinels Fe
2
GeO
4
and γ-Fe
2
SiO
4
at low temperatures, which indicate that the degree of frustration may itself be a fluctuating quantity that can spontaneously order without a lattice distortion as a ‘frustration wave’. Fe
2
GeO
4
with propagation vector (
2
/
3
+ δ
2
/
3
+ δ 0) has ordered Fe
2+
moments that vary between fully saturated 4 μB and 0 values, consistent with a frustration wave order. γ-Fe
2
SiO
4
has a more complex (¾ + δ ¾ + δ 0) order that coexists with an ordered spin ice phase. Dynamic orbital fluctuations are proposed to give rise to locally correlated patterns of ferromagnetic and antiferromagnetic interactions consistent with the observed orders.
Frustrated magnetic materials provide a great laboratory to study the interplay between classical order and quantum fluctuations. The authors study the frustrated magnetic ground states of two Fe spinel oxides showing that the frustration is a fluctuating characteristic that manifests itself as a “frustration wave” |
doi_str_mv | 10.1038/s42005-018-0067-7 |
format | Article |
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2
GeO
4
and γ-Fe
2
SiO
4
at low temperatures, which indicate that the degree of frustration may itself be a fluctuating quantity that can spontaneously order without a lattice distortion as a ‘frustration wave’. Fe
2
GeO
4
with propagation vector (
2
/
3
+ δ
2
/
3
+ δ 0) has ordered Fe
2+
moments that vary between fully saturated 4 μB and 0 values, consistent with a frustration wave order. γ-Fe
2
SiO
4
has a more complex (¾ + δ ¾ + δ 0) order that coexists with an ordered spin ice phase. Dynamic orbital fluctuations are proposed to give rise to locally correlated patterns of ferromagnetic and antiferromagnetic interactions consistent with the observed orders.
Frustrated magnetic materials provide a great laboratory to study the interplay between classical order and quantum fluctuations. The authors study the frustrated magnetic ground states of two Fe spinel oxides showing that the frustration is a fluctuating characteristic that manifests itself as a “frustration wave”</description><identifier>ISSN: 2399-3650</identifier><identifier>EISSN: 2399-3650</identifier><identifier>DOI: 10.1038/s42005-018-0067-7</identifier><language>eng</language><publisher>London: Nature Publishing Group UK</publisher><subject>639/766/119/2795 ; 639/766/119/997 ; Antiferromagnetism ; Chemical Sciences ; Condensed Matter ; Ferromagnetic materials ; Frustration ; Iron ; Lattices ; Low temperature ; Magnetic materials ; Material chemistry ; Physics ; Physics and Astronomy ; Spin dynamics ; Spin ice ; Spin liquid ; Spinel ; Strongly Correlated Electrons ; Wave propagation</subject><ispartof>Communications physics, 2018-10, Vol.1 (1), Article 69</ispartof><rights>The Author(s) 2018</rights><rights>The Author(s) 2018. This work is published under http://creativecommons.org/licenses/by/4.0/ (the “License”). Notwithstanding the ProQuest Terms and Conditions, you may use this content in accordance with the terms of the License.</rights><rights>Distributed under a Creative Commons Attribution 4.0 International License</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c393t-9a7cfb6d7b05b3d91df3e5497be263be5a6a603d703271c3f4f34d12703e6d743</citedby><cites>FETCH-LOGICAL-c393t-9a7cfb6d7b05b3d91df3e5497be263be5a6a603d703271c3f4f34d12703e6d743</cites><orcidid>0000-0001-9763-3987</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>230,314,780,784,864,885,27924,27925</link.rule.ids><backlink>$$Uhttps://hal.univ-lille.fr/hal-02297713$$DView record in HAL$$Hfree_for_read</backlink></links><search><creatorcontrib>Perversi, Giuditta</creatorcontrib><creatorcontrib>Arevalo-Lopez, Angel M.</creatorcontrib><creatorcontrib>Ritter, Clemens</creatorcontrib><creatorcontrib>Attfield, J. Paul</creatorcontrib><title>Frustration wave order in iron(II) oxide spinels</title><title>Communications physics</title><addtitle>Commun Phys</addtitle><description>Frustrated magnetic materials can show unconventional correlations such as quantum spin liquid states and monopole excitations in spin ices. These phenomena are observed on uniformly frustrated lattices such as triangular, kagome or pyrochlore types, where all nearest neighbour interactions are equivalent. Here we report incommensurate long-range spin amplitude waves in the spinels Fe
2
GeO
4
and γ-Fe
2
SiO
4
at low temperatures, which indicate that the degree of frustration may itself be a fluctuating quantity that can spontaneously order without a lattice distortion as a ‘frustration wave’. Fe
2
GeO
4
with propagation vector (
2
/
3
+ δ
2
/
3
+ δ 0) has ordered Fe
2+
moments that vary between fully saturated 4 μB and 0 values, consistent with a frustration wave order. γ-Fe
2
SiO
4
has a more complex (¾ + δ ¾ + δ 0) order that coexists with an ordered spin ice phase. Dynamic orbital fluctuations are proposed to give rise to locally correlated patterns of ferromagnetic and antiferromagnetic interactions consistent with the observed orders.
Frustrated magnetic materials provide a great laboratory to study the interplay between classical order and quantum fluctuations. The authors study the frustrated magnetic ground states of two Fe spinel oxides showing that the frustration is a fluctuating characteristic that manifests itself as a “frustration wave”</description><subject>639/766/119/2795</subject><subject>639/766/119/997</subject><subject>Antiferromagnetism</subject><subject>Chemical Sciences</subject><subject>Condensed Matter</subject><subject>Ferromagnetic materials</subject><subject>Frustration</subject><subject>Iron</subject><subject>Lattices</subject><subject>Low temperature</subject><subject>Magnetic materials</subject><subject>Material chemistry</subject><subject>Physics</subject><subject>Physics and Astronomy</subject><subject>Spin dynamics</subject><subject>Spin ice</subject><subject>Spin liquid</subject><subject>Spinel</subject><subject>Strongly Correlated Electrons</subject><subject>Wave propagation</subject><issn>2399-3650</issn><issn>2399-3650</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2018</creationdate><recordtype>article</recordtype><sourceid>C6C</sourceid><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><recordid>eNp1kMFKAzEQhoMoWGofwNuCF3uITjK7yeZYirWFghc9h-wmq1vqpibbqm9vyop68TSZ8P0_w0fIJYMbBljexpwDFBRYSQGEpPKEjDgqRVEUcPrnfU4mMW4AgLMcJIoRgUXYxz6YvvVd9m4OLvPBupC1XdYG312vVtPMf7TWZXHXdm4bL8hZY7bRTb7nmDwt7h7nS7p-uF_NZ2tao8KeKiPrphJWVlBUaBWzDboiV7JyXGDlCiOMALQSkEtWY5M3mFvG0-5SKscxmQ69L2ard6F9NeFTe9Pq5Wytj3_AuZKS4YEl9mpgd8G_7V3s9cbvQ5fO0xxLJUpRFmWi2EDVwccYXPNTy0AfPerBo04e9dGjlinDh0xMbPfswm_z_6EvKcxyQg</recordid><startdate>20181029</startdate><enddate>20181029</enddate><creator>Perversi, Giuditta</creator><creator>Arevalo-Lopez, Angel M.</creator><creator>Ritter, Clemens</creator><creator>Attfield, J. 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Paul</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c393t-9a7cfb6d7b05b3d91df3e5497be263be5a6a603d703271c3f4f34d12703e6d743</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2018</creationdate><topic>639/766/119/2795</topic><topic>639/766/119/997</topic><topic>Antiferromagnetism</topic><topic>Chemical Sciences</topic><topic>Condensed Matter</topic><topic>Ferromagnetic materials</topic><topic>Frustration</topic><topic>Iron</topic><topic>Lattices</topic><topic>Low temperature</topic><topic>Magnetic materials</topic><topic>Material chemistry</topic><topic>Physics</topic><topic>Physics and Astronomy</topic><topic>Spin dynamics</topic><topic>Spin ice</topic><topic>Spin liquid</topic><topic>Spinel</topic><topic>Strongly Correlated Electrons</topic><topic>Wave propagation</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Perversi, Giuditta</creatorcontrib><creatorcontrib>Arevalo-Lopez, Angel M.</creatorcontrib><creatorcontrib>Ritter, Clemens</creatorcontrib><creatorcontrib>Attfield, J. 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Paul</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Frustration wave order in iron(II) oxide spinels</atitle><jtitle>Communications physics</jtitle><stitle>Commun Phys</stitle><date>2018-10-29</date><risdate>2018</risdate><volume>1</volume><issue>1</issue><artnum>69</artnum><issn>2399-3650</issn><eissn>2399-3650</eissn><abstract>Frustrated magnetic materials can show unconventional correlations such as quantum spin liquid states and monopole excitations in spin ices. These phenomena are observed on uniformly frustrated lattices such as triangular, kagome or pyrochlore types, where all nearest neighbour interactions are equivalent. Here we report incommensurate long-range spin amplitude waves in the spinels Fe
2
GeO
4
and γ-Fe
2
SiO
4
at low temperatures, which indicate that the degree of frustration may itself be a fluctuating quantity that can spontaneously order without a lattice distortion as a ‘frustration wave’. Fe
2
GeO
4
with propagation vector (
2
/
3
+ δ
2
/
3
+ δ 0) has ordered Fe
2+
moments that vary between fully saturated 4 μB and 0 values, consistent with a frustration wave order. γ-Fe
2
SiO
4
has a more complex (¾ + δ ¾ + δ 0) order that coexists with an ordered spin ice phase. Dynamic orbital fluctuations are proposed to give rise to locally correlated patterns of ferromagnetic and antiferromagnetic interactions consistent with the observed orders.
Frustrated magnetic materials provide a great laboratory to study the interplay between classical order and quantum fluctuations. The authors study the frustrated magnetic ground states of two Fe spinel oxides showing that the frustration is a fluctuating characteristic that manifests itself as a “frustration wave”</abstract><cop>London</cop><pub>Nature Publishing Group UK</pub><doi>10.1038/s42005-018-0067-7</doi><orcidid>https://orcid.org/0000-0001-9763-3987</orcidid><oa>free_for_read</oa></addata></record> |
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subjects | 639/766/119/2795 639/766/119/997 Antiferromagnetism Chemical Sciences Condensed Matter Ferromagnetic materials Frustration Iron Lattices Low temperature Magnetic materials Material chemistry Physics Physics and Astronomy Spin dynamics Spin ice Spin liquid Spinel Strongly Correlated Electrons Wave propagation |
title | Frustration wave order in iron(II) oxide spinels |
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