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Polymorphic Transitions in Calcite and the Kinetics of the Aragonite-Calcite Transformation: Evidence from Electrical Impedance Measurements at Pressures up to 2.5 GPa

机译:方解石中的多晶型转变和文石-方解石转变的动力学:压力高达2.5 GPa时电阻抗测量的证据

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High-temperature phase transitions in calcite and the calcite-aragonite transformation were investigated on a piston-cylinder apparatus by means of an electrical impedance measurement within temperature and pressure intervals of 600-1200 deg C and 0.5-2.5 GPa. The measurement cell consisted of a coaxial capacitor with a geometric factor of 6 cm. The bulk component of electrical conductivity was obtained from Argand dia-grams in the fequency range 10~(-1)-10~5 Hz. The starting materials were represented by the polycrystalline CaCO_3 reagent and pressed powders of natural calcite crystals. t each pressure, the transition temperature was recorded by a stepwise change in activation energy, which was determined from the curves of electrical con-ductivity versus temperature. The pressure dependency of the temperature of the transition into the disordered calcite-V phase shows a maximum at a pressure of 10 kbar. The curve that has previously been regarded in the literature as a transition to the intermediate calcite-IV phase was interpreted as the pressure dependency of the onset of continuous orientation disorder in the initial calcite-I phase. The kinetics of the aragonite-calcite trans-formation was determined at pressures of 15 and 25 kbar by the continuous monitoring of changes with time in the electrical conductivity of a sample at conrrelated with the degree of phase transformation.
机译:通过在600-1200摄氏度和0.5-2.5 GPa的温度和压力区间内的电阻抗测量,在活塞-气缸装置上研究了方解石中的高温相变和方解石-文石的转变。测量单元由一个几何系数为6 cm的同轴电容器组成。电导率的主体部分是从Argand图获得的,频率范围为10〜(-1)-10〜5 Hz。起始原料为多晶CaCO_3试剂和天然方解石晶体的压粉。在每个压力下,通过活化能的逐步变化记录转变温度,该变化是根据电导率与温度的关系曲线确定的。转变为无序方解石-V相的温度对压力的依赖性在10 kbar的压力下显示出最大值。先前在文献中被视为过渡到方解石-IV相的过渡的曲线被解释为初始方解石-I相中连续取向紊乱发作的压力依赖性。文石-方解石转化的动力学是在15kbar和25kbar的压力下通过连续监测样品电导率随时间的变化而确定的,该变化与相变的程度有关。

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