Thermal equation of state of Li-rich schorl up to 15.5 GPa and 673 K: Implications for lithium and boron transport in slab subduction
文献类型:期刊论文
| 作者 | Wei Chen; Shanrong Zhang; Mengzeng Wu; Qifa Zhong; Shijie Huang; Kai Wang; Wei Zhao; Jingui Xu; Dawei Fan; Wenge Zhou |
| 刊名 | American Mineralogist
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| 出版日期 | 2024 |
| 卷号 | 109期号:12页码:2095-2104 |
| 关键词 | Schorl, Equation Of State, High Pressure And High Temperature, X-ray Diffraction, Diamond-anvil Cell |
| DOI | 10.2138/am-2023-9150 |
| 英文摘要 | The thermal equation of state (EoS) of a natural schorl has been determined at high temperatures up to 673 K and high pressures up to 15.5 GPa using in situ synchrotron X-ray diffraction combined with a diamond-anvil cell. The pressure-volume (P-V) data were fitted to a third-order Birch-Murnaghan EoS with V0 = 1581.45 ± 0.25 Å3, K0 = 111.6 ± 0.9 GPa, and K0′ = 4.4 ± 0.2; additionally, when K0′ was fixed at a value of 4, V0 = 1581.04 ± 0.20 Å3, and K0 = 113.6 ± 0.3 GPa. The V0 (1581.45 ± 0.25 Å3) obtained by the third-order Birch-Murnaghan EoS agrees well with the V0 (1581.45 ± 0.05 Å3) measured at ambient conditions. Furthermore, the axial compression data of schorl at room temperature were fitted to a “linearized” third-order Birch-Murnaghan EoS, and the obtained axial moduli for the a- and c-axes are Ka = 621 ± 9 GPa and Kc = 174 ± 2 GPa, respectively. Consequently, the axial compressibilities are βa = 1.61 × 10–3 GPa–1 and βc = 5.75 × 10–3 GPa–1 with an anisotropic ratio of βa:βc = 0.28:1.00, indicating axial compression anisotropy. In addition, the compositional effect on the axial compressibilities of tourmalines was discussed. Fitting our pressure-volume-temperature (P-V-T) data to a high-temperature third-order Birch-Murnaghan EoS yielded the following thermal EoS parameters: V0 = 1581.2 ± 0.2 Å3, K0 = 110.5 ± 0.6 GPa, K0′ = 4.6 ± 0.2, (∂KT/∂T)P = –0.012 ± 0.003 GPa K–1 and αV0 = (2.4 ± 0.2) × 10–5 K–1. These parameters were compared with those of previous studies on other tourmalines, and the potential factors influencing the thermal EoS parameters of tourmalines were further discussed. |
| URL标识 | 查看原文 |
| 语种 | 英语 |
| 源URL | ![]() |
| 专题 | 地球化学研究所_地球内部物质高温高压实验室 |
| 作者单位 | 1.Key Laboratory of High-Temperature and High-Pressure Study of the Earth’s Interior, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang, Guizhou 550081, China 2.University of Chinese Academy of Sciences, Beijing 100049, China 3.Guizhou Polytechnic of Construction, Guiyang, Guizhou 551400, China |
| 推荐引用方式 GB/T 7714 | Wei Chen,Shanrong Zhang,Mengzeng Wu,et al. Thermal equation of state of Li-rich schorl up to 15.5 GPa and 673 K: Implications for lithium and boron transport in slab subduction[J]. American Mineralogist,2024,109(12):2095-2104. |
| APA | Wei Chen.,Shanrong Zhang.,Mengzeng Wu.,Qifa Zhong.,Shijie Huang.,...&Wenge Zhou.(2024).Thermal equation of state of Li-rich schorl up to 15.5 GPa and 673 K: Implications for lithium and boron transport in slab subduction.American Mineralogist,109(12),2095-2104. |
| MLA | Wei Chen,et al."Thermal equation of state of Li-rich schorl up to 15.5 GPa and 673 K: Implications for lithium and boron transport in slab subduction".American Mineralogist 109.12(2024):2095-2104. |
入库方式: OAI收割
来源:地球化学研究所
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