Spin reorientation and magnetic frustration in Fe<sub>32+<i>δ</i></sub>Ge<sub>35−<i>x</i></sub>Si<sub><i>x</i></sub> with a kagome lattice broken by crystallographic intergrowth

Fe<sub>32+<i>δ</i></sub>Ge<sub>35-<i>x</i></sub>Si<sub><i>x</i></sub> was synthesized using solid-state and chemical vapor transport reactions in both powder and single crystalline forms. Single crystal and high-resolution powder X-ray diffraction experiments revealed Fe<sub>32+<i>δ</i></sub>Ge<sub>35-<i>x</i></sub>Si<sub><i>x</i></sub> to be the third member of the Fe<sub>32+<i>δ</i></sub>Ge<sub>35-<i>x</i></sub>E<sub><i>x</i></sub> (E = p-element) family of ternary compounds alongside Fe<sub>32+<i>δ</i></sub>Ge<sub>33</sub>As<sub>2</sub> and Fe<sub>32+<i>δ</i></sub>Ge<sub>35-<i>x</i></sub>P<sub><i>x</i></sub>. Fe<sub>32+<i>δ</i></sub>Ge<sub>35-<i>x</i></sub>Si<sub><i>x</i></sub> features a two-dimensional intergrowth structure of two parent structure types: MgFe<sub>6</sub>Ge<sub>6</sub> and Co<sub>2</sub>Al<sub>5</sub>. Similar to the other members, the stabilisation of the intergrowth structure in Fe<sub>32+<i>δ</i></sub>Ge<sub>35-<i>x</i></sub>Si<sub><i>x</i></sub> occurs as a result of p-element substitution in the MgFe<sub>6</sub>Ge<sub>6</sub>-type block. The intergrowth breaks the kagome net of MgFe<sub>6</sub>Ge<sub>6</sub> into individual hexagrams while providing additional layers of geometrically frustrated atomic arrangements. Magnetic measurements showed antiferromagnetic ordering at <i>T</i><sub>N</sub> ∼ 150-160 K and spin reorientation below 80-90 K owing to the competition between magnetic interactions in the frustrated magnetic lattice of Fe<sub>32+<i>δ</i></sub>Ge<sub>35-<i>x</i></sub>Si<sub><i>x</i></sub>.

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Publication Details

Journal
Dalton Transactions
Published
2025-01-01
DOI
https://doi.org/10.1039/d5dt00654f
Citations
3
Primary Topic
Mineralogy and Gemology Studies
Type
article
Field-Weighted Citation Impact
4.01
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Spin reorientation and magnetic frustration in Fe32+δGe35−xSix with a kagome lattice broken by crystallographic intergrowth

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Dalton Transactions
Mineralogy and Gemology Studies
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Spin reorientation and magnetic frustration in Fe32+δGe35−xSix with a kagome lattice broken by crystallographic intergrowth

А. В. Миронов, Valeriy Yu. Verchenko, Roman A. Khalaniya, Evgeny V. Dikarev, A. N. Samarin, Raivo Stern, Аndrei V. Shevelkov, Alexey O. Polevik, Aleksandr Kulchu, Zheng Wei, Alexey V. Bogach
article en
3 citations

Abstract

Fe<sub>32+<i>δ</i></sub>Ge<sub>35-<i>x</i></sub>Si<sub><i>x</i></sub> was synthesized using solid-state and chemical vapor transport reactions in both powder and single crystalline forms. Single crystal and high-resolution powder X-ray diffraction experiments revealed Fe<sub>32+<i>δ</i></sub>Ge<sub>35-<i>x</i></sub>Si<sub><i>x</i></sub> to be the third member of the Fe<sub>32+<i>δ</i></sub>Ge<sub>35-<i>x</i></sub>E<sub><i>x</i></sub> (E = p-element) family of ternary compounds alongside Fe<sub>32+<i>δ</i></sub>Ge<sub>33</sub>As<sub>2</sub> and Fe<sub>32+<i>δ</i></sub>Ge<sub>35-<i>x</i></sub>P<sub><i>x</i></sub>. Fe<sub>32+<i>δ</i></sub>Ge<sub>35-<i>x</i></sub>Si<sub><i>x</i></sub> features a two-dimensional intergrowth structure of two parent structure types: MgFe<sub>6</sub>Ge<sub>6</sub> and Co<sub>2</sub>Al<sub>5</sub>. Similar to the other members, the stabilisation of the intergrowth structure in Fe<sub>32+<i>δ</i></sub>Ge<sub>35-<i>x</i></sub>Si<sub><i>x</i></sub> occurs as a result of p-element substitution in the MgFe<sub>6</sub>Ge<sub>6</sub>-type block. The intergrowth breaks the kagome net of MgFe<sub>6</sub>Ge<sub>6</sub> into individual hexagrams while providing additional layers of geometrically frustrated atomic arrangements. Magnetic measurements showed antiferromagnetic ordering at <i>T</i><sub>N</sub> ∼ 150-160 K and spin reorientation below 80-90 K owing to the competition between magnetic interactions in the frustrated magnetic lattice of Fe<sub>32+<i>δ</i></sub>Ge<sub>35-<i>x</i></sub>Si<sub><i>x</i></sub>.

Dalton TransactionsVol. 54(20)
Lomonosov Moscow State University (RU), National Institute of Chemical Physics and Biophysics (EE), University at Albany, State University of New York (US), Moscow State University (TJ), Prokhorov General Physics Institute (RU)
Openalex Percentile: Top 8%
Mineralogy and Gemology Studies
4.01
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