天然富铁氧硼酸钙钒辉石和壳体的低温研究:晶体结构的热变形、强负热膨胀和磁跃迁级联

Y. Biryukov, A. Zinnatullin, M. Cherosov, A. Shablinskii, R. Yusupov, R. Bubnova, F. Vagizov, S. Filatov, M. Avdontceva, I. Pekov
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引用次数: 1

摘要

本文研究了天然氧硼酸钙钒辉石和壳体在5-500 K温度范围内的磁性和热行为。利用Mössbauer光谱测定了局部环境、Fe和Sn原子的氧化态和电荷分布,并首次在各向异性近似下通过单晶x射线衍射数据(SCXRD)对壳体的晶体结构进行了改进。用振动样品磁强计(VSM)(5≤T≤400 K)研究了富铁体的磁性能,首次报道了富铁体的磁性能。两种氧硼酸盐都表现出非常复杂的磁性行为。揭示了磁跃迁的级联,并确定了临界温度。随着温度的升高,菱铁矿和船体石的磁性转变顺序为:磁性有序态→部分磁性有序态→顺磁性态。根据x射线衍射数据(93≤T≤500 K),这些过程伴随着单位胞参数的异常和氧硼酸盐在临界温度下的热膨胀。在低于~ 120k的温度下,两种氧硼酸盐都观察到强烈的负体积热膨胀。
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Low-temperature investigation of natural iron-rich oxoborates vonsenite and hulsite: thermal deformations of crystal structure, strong negative thermal expansion and cascades of magnetic transitions
This work is devoted to an investigation of the magnetic properties and thermal behaviour of the natural oxoborates vonsenite and hulsite in the temperature range 5–500 K. The local environment, the oxidation states of the Fe and Sn atoms, and the charge distribution were determined using Mössbauer spectroscopy and are in accordance with a refinement of the crystal structure of hulsite from single-crystal X-ray diffraction data (SCXRD) in anisotropic approximation for the first time. The magnetic properties were studied by vibrating sample magnetometry (VSM) (5 ≤ T ≤ 400 K) and are reported for the first time for iron-rich hulsite. Both oxoborates show a very complex magnetic behaviour. Cascades of magnetic transitions are revealed and the critical temperatures were determined. The sequences of magnetic transitions in both vonsenite and hulsite with increasing temperature were found to be as follows: magnetically ordered state → partial magnetic ordering → paramagnetic state. According to X-ray diffraction data (93 ≤ T ≤ 500 K), these processes are accompanied by anomalies in the unit-cell parameters and thermal expansion of the oxoborates at critical temperatures. A strong negative volume thermal expansion is observed for both oxoborates at temperatures below ∼120 K.
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