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Compressibility and expansivity of anglesite (PbSO 4) using in situ synchrotron X-ray diffraction at high-pressure and high-temperature conditions

机译:在高压和高温条件下,使用原位同步X射线衍射在高压和高温条件下的压缩性和扩张性(PBSO <下标> 4

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摘要

The compressibility and expansivity of anglesite (PbSO~(4)) have been measured at high pressure up to 21.6?GPa and high temperature up to 700?K using in situ angle-dispersive X-ray diffraction and diamond anvil cell. The third-order Birch–Murnaghan equation of state (III-BM-EoS) was used to analyze the pressure–volume ( P–V ) data of PbSO~(4). We obtained the bulk modulus K ~( 0 )?=?59(1)?GPa, and its pressure derivative $$K_{0}^{'}$$ K 0 ′ ?=?5.3(4), respectively. Using Holland–Powell thermal EoS to fit the temperature–volume ( T–V ) data, the thermal expansion coefficient α ~(0)?=?4.59(2)?×?10_(??5)?K_(??1)for PbSO~(4)was also derived. Simultaneously, the ambient-pressure axial compressibilities ( β ~( a 0)?=?1.79(4)?×?10_(??3)?GPa_(??1), β ~( b 0)?=?1.75(5)?×?10_(??3)?GPa_(??1), β ~( c 0)?=?2.12(4)?×?10_(??3)?GPa_(??1)) and axial thermal expansivities ( α ~( a 0)?=?1.23(4)?×?10_(??5)?K_(??1), α ~( b 0)?=?1.93(2)?×?10_(??5)?K_(??1), and α ~( c 0)?=?1.43(1)?×?10_(??5)?K_(??1)) along a -axis, b -axis and c -axis were derived at 300?K, respectively. Furthermore, the potential influencing factors (e.g., the effective size of M_(2+)cation, polarizability and electronegativity) on the bulk moduli of barite-type (belonging to Pbnm space group) sulfates (anglesite, barite, and celestine) were discussed. We found that the polarizability might be the most important factor. Finally, the anisotropic linear compressibility and thermal expansivity in barite-type sulfates were also discussed, respectively.
机译:在原位角度分散X射线衍射和金刚石砧座和金刚石砧座和金刚石砧座和金刚石砧座和金刚石砧座中,在高压高达21.6℃和高温高达700〜K的高压下测量的可压缩性和扩张性。状态(III-BM-EOS)的三阶Birch-Murnaghan方程用于分析PBO〜(4)的压力体积(P-V)数据。我们获得了批量模量k〜(0)?=?59(1)?GPA,其压力导数$$ k_ {0} ^ {'} $$ k 0'分别?=?5.3(4)。使用Holland-Powell热EOS适合温度(T-V)数据,热膨胀系数α〜(0)?=?4.59(2)?×10 _(?? 5)?k _(?? 1 )对于PBO〜(4)也是衍生的。同时,环境压力轴向压缩性(β〜(a 0)?=?1.79(4)?×10 _(?? 3)?GPA _(?? 1),β〜(B 0)?=?1.75( 5)?×10 _(?? 3)?GPA _(?? 1),β〜(0)?=?2.12(4)?×10 _(?? 3)?GPA _(?? 1))和轴向热膨胀率(α〜(a 0)?=?1.23(4)?×10 _(?? 5)?k _(?? 1),α〜(b 0)?=?1.93(2)?×? 10 _(?? 5)?k _(?? 1),α〜(0)?=?1.43(1)?×10 _(?? 5)?x _(?? 1))沿着-axis, B-XXIS和C -axis分别以300μk衍生出300μk。此外,讨论了在讨论了硫酸盐型(属于PBNM空间组)硫酸盐(Anglesite,Barite和Celestine)的体积模量的潜在影响因素(例如,M_(2+)阳离子,极化性和电负性的有效尺寸) 。我们发现极化性可能是最重要的因素。最后,还分别讨论了重晶石型硫酸盐的各向异性线性可压缩性和热膨胀性。

著录项

  • 来源
    《Physics and chemistry of minerals》 |2018年第9期|共11页
  • 作者单位

    Key Laboratory of High Temperature and High Pressure Study of the Earth’s Interior Institute of Geochemistry Chinese Academy of Sciences;

    Key Laboratory of High Temperature and High Pressure Study of the Earth’s Interior Institute of Geochemistry Chinese Academy of Sciences;

    Guizhou Polytechnic of Construction;

    Key Laboratory of High Temperature and High Pressure Study of the Earth’s Interior Institute of Geochemistry Chinese Academy of Sciences;

    Key Laboratory of High Temperature and High Pressure Study of the Earth’s Interior Institute of Geochemistry Chinese Academy of Sciences;

    Key Laboratory of High Temperature and High Pressure Study of the Earth’s Interior Institute of Geochemistry Chinese Academy of Sciences;

    Key Laboratory of High Temperature and High Pressure Study of the Earth’s Interior Institute of Geochemistry Chinese Academy of Sciences;

    Key Laboratory of High Temperature and High Pressure Study of the Earth’s Interior Institute of Geochemistry Chinese Academy of Sciences;

  • 收录信息
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 矿物学;
  • 关键词

    Anglesite (PbSO4); Compressibility and expansivity; High pressure and high temperature; Synchrotron X-ray diffraction; Diamond anvil cell;

    机译:角钻(PBSO4);可压缩性和扩张性;高压和高温;同步X射线衍射;金刚石砧座细胞;

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