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Pressure Induced Polymorphic Phase Transition of Natural Metamorphic Kalsilite; Electrical Resistivity and Infrared Spectroscopic Investigations

机译:天然变质硅钙石的压力诱导多态相变;电阻率和红外光谱研究

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We report here pressure dependence of the electrical resistivity of natural kalsilite (K0.998Na0.002Al0.998Fe0.002SiO4) from a granulite facies terrain in southern India. The electrical resistivity of kalsilite was measured with four probe technique up to 7.5 GPa at room temperature. The electrical resistivity decreases continuously with the increase of pressure up to 3.7 GPa, where there is a discontinuous drop in the electrical resistivity by 14%–16% indicating a first order transition. Further increase of pressure does not induce any phase transition up to 7.5 GPa at room temperature. Fourier transform infrared (FTIR) spectroscopy of the kalsilite sample at various pressures indicates that the observed transition is reversible in nature.
机译:我们在这里报告天然钾盐(K 0.998 Na 0.002 Al 0.998 Fe 0.002 SiO 4 )来自印度南部的花岗石相地貌。在室温下,通过四探针技术测量了钾盐岩的电阻率,最高可达7.5 GPa。电阻率随着压力的增加而不断降低,直到3.7 GPa,电阻率不连续下降14%–16%,表明发生了一次过渡。在室温下,压力的进一步增加不会引起高达7.5 GPa的任何相变。在不同压力下对钾铝石样品的傅里叶变换红外(FTIR)光谱表明,观察到的转变本质上是可逆的。

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