Spin dynamics in natural multiferroic pyroxene NaFeSi
O
天然マルチフェロイイック輝石NaFeSi
O
のスピンダイナミクス
Prokhnenko, O.*; Nikitin, S. E.*; 金子 耕士
; 田端 千紘; 廣瀬 雄介; 常盤 欣文
; 芳賀 芳範
; 藤田 全基; 野尻 浩之*; Anovitz, L. M.*; Podlesnyak, A.*
Prokhnenko, O.*; Nikitin, S. E.*; Kaneko, Koji; Tabata, Chihiro; Hirose, Yusuke; Tokiwa, Yoshifumi; Haga, Yoshinori; Fujita, Masaki; Nojiri, Hiroyuki*; Anovitz, L. M.*; Podlesnyak, A.*
The spin dynamics in the natural mineral aegirine, NaFeSi
O
, which exhibits multiferroic properties, was studied using elastic and inelastic neutron scattering. Magnetism in pyroxenes arises from competing intra- and interchain exchanges that stabilize a variety of commensurate and incommensurate states. The incommensurate helical ground state remains robust, with no metamagnetic transitions observed and only gradual spectral changes under field. A phase diagram constructed in terms of the exchange ratios
and
captures the transition between commensurate and incommensurate regimes and unifies magnetic behavior across different pyroxenes. Despite structural variations (
vs
), the exchange topology and resulting magnetic frustration are closely related. These results establish NaFeSi
O
as a benchmark for understanding exchange-driven magnetism and field-stable spin dynamics in pyroxenes with three-dimensional magnetic coupling.