反铁磁性
塞贝克系数
价(化学)
铁磁性
磁性
热电效应
微晶
凝聚态物理
晶体结构
结晶学
材料科学
充电顺序
钙钛矿(结构)
分析化学(期刊)
化学
电荷(物理)
物理
有机化学
色谱法
热力学
量子力学
作者
Hiroshi Nakatsugawa,Yudai Kamatani,Yoichi Okamoto,Charles H. Hervoches
标识
DOI:10.35848/1347-4065/acc9f3
摘要
Abstract Polycrystalline Nd 1− x Sr x FeO 3− δ (0.1 ≤ x ≤ 0.9) samples exhibit a single-phase perovskite-type crystal structure and G-type antiferromagnetism with small ferromagnetic order. Assuming that the Fe site is in the mixed-valence state, the spin state of Fe changes from a low-spin (LS) or intermediate spin Fe 3+ -dominant state at x ≤ 0.5 to a LS Fe 4+ dominant state at x ≥ 0.6. This strongly suggests that the charge carriers change from holes to electrons. In fact, at temperatures less than 500 K, these samples show a p -type Seebeck coefficient for 0.1 ≤ x ≤ 0.5 and an n -type Seebeck coefficient for 0.6 ≤ x ≤ 0.9. However, for 0.6 ≤ x ≤ 0.9, Fe 4+ is reduced to Fe 3+ because of an oxygen deficiency in the 500–600 K temperature range. In particular, Nd 0.7 Sr 0.3 FeO 2.99(1) shows the largest p -type ZT = 0.025 at 765 K, whereas compositions with high n -type ZT could not be identified.
科研通智能强力驱动
Strongly Powered by AbleSci AI