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The effect of chemical composition and oxygen fugacity on the electrical conductivity of dry and hydrous garnet at high temperatures and pressures

机译:高温高压下化学成分和氧逸度对干石榴石和含水石榴石电导率的影响

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The in situ electrical conductivity of hydrous garnet samples (Py_(20)Alm_(76)Grs_4-Py_(73)Alm_(14)Grs_(13)) was determined at pressures of 1.0-4.0 GPa and temperatures of 873-1273 K in the YJ-3000t apparatus using a Solartron-1260 impedance/gain-phase analyzer for various chemical compositions and oxygen fugacities. The oxygen fugacity was controlled by five solid-state oxygen buffers (Fe_2O_3 + Fe_3O_4, Ni + NiO, Fe + Fe_3O_4, Fe + FeO, and Mo + MoO_2). Experimental results indicate that within a frequency range from 10~(-2) to 10~6 Hz, electrical conductivity is strongly dependent on signal frequency. Electrical conductivity shows an Arrhenius increase with temperature.
机译:含水石榴石样品(Py_(20)Alm_(76)Grs_4-Py_(73)Alm_(14)Grs_(13))的原位电导率是在1.0-4.0 GPa的压力和873-1273 K的压力下测定的使用Solartron-1260阻抗/增益相位分析仪的YJ-3000t仪器,用于各种化学成分和氧气逸度。氧逸度由五个固态氧缓冲剂(Fe_2O_3 + Fe_3O_4,Ni + NiO,Fe + Fe_3O_4,Fe + FeO和Mo + MoO_2)控制。实验结果表明,在10〜(-2)到10〜6 Hz的频率范围内,电导率在很大程度上取决于信号频率。电导率显示Arrhenius随着温度增加。

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