Cubic perovskite polymorph of strontium metasilicate at high pressures

Cubic perovskite polymorph of strontium metasilicate at high pressures
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高压偏硅酸锶的立方钙钛矿多晶型物

DOI:
10.2138/am.2013.4470
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发表时间:
2013-11
影响因子:
3.1
通讯作者:
Jian Xu
Jian Xu
中科院分区:
地球科学3区
文献类型:
--
作者:
Dayong Tan;Wei Zhou;Jing Liu;Jian Xu

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摘要利用金刚石对顶砧(DAC)和激光加热技术,在-38 GPa和1500-2000 K的压力下,首次合成了立方钙钛矿结构的SrSiO 3。当用Birch-Murnaghan状态方程(K 0 ′固定为4)拟合时,新相的P-V数据给出的室温弹性常数分别为V0 = 49.18(5)GPa,K 0 = 211(3)GPa.在减压下,SrSiO 3立方钙钛矿相在-6.2 GPa下变得不稳定,并在-4.7 GPa下完全消失。转化产物可以被认为是无定形相,在无定形基质中具有少量的小尺寸晶体。第一性原理计算预测的立方和六层重复的六方钙钛矿型的SrSiO 3的多晶型物的结构特性与实验结果吻合良好。实验和理论结果表明,在下地幔条件下,较大的Sr ~(2+)离子可以取代Ca ~(2+)离子进入钙钛矿相CaSiO_3的晶格中,而晶格应变很小。这些结果表明,Sr可以托管在立方钙钛矿CaSiO 3中,这些钙钛矿CaSiO 3作为包裹体存在于起源于下地幔的钻石中
Abstract By using a diamond-anvil cell (DAC) with laser heating technology, a cubic perovskite polymorph of SrSiO3 has been synthesized at - 38 GPa and 1500-2000 K for the first time. The P-V data of this new phase give ambient temperate elastic constants of V0 = 49.18(5) Å3, K0 = 211(3) GPa, respectively, when they are fitted against the Birch-Murnaghan equation of state with a fixed K0′ at 4. On decompression, the SrSiO3 cubic perovskite phase becomes unstable at - 6.2 GPa and disappears completely at - 4.7 GPa. The transformed product can be considered as an amorphous phase with a minor amount of small sized crystals in the amorphous matrix. First principle calculations predicted structural properties of both the cubic and the six-layer-repeated hexagonal perovskite polymorphs of SrSiO3 in good agreement with experimental results. The experimental and theoretical results indicate that the larger Sr2+ cation can substitute the Ca2+ cation and enter into the lattice of the cubic perovskite phase of CaSiO3 at lower mantle conditions with only a small lattice strain. These results indicate that Sr can be hosted in cubic perovskite CaSiO3 found as inclusions in diamonds originating from the lower mantle
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