计算部分熔融岩石电导率方法的综述

部分熔融岩石的电导率是由固体岩石的低电导率和硅酸盐熔体的高电导率组成，因此熔体的几何形态和空间分布对部分熔融岩石的电导率将产生重大影响.本文介绍了熔体在岩石中的分布特征和它们的几何分布形态，同时，评述了各种数学模型在模拟计算部分熔融岩石电导率中的优缺点.

Review of model calculations of electrical conductivity for partially molten rocks

The electrical conductivity of partially molten rocks is mainly controlled by solid grain with low conductivity and silicate melt with high conductivity. Melt geometry and melt distribution have an great influence on electrical conductivity of partially molten rocks. The form of melt distribution is roughly classified into two type, that is connected melt constructing a network of melt along grain boundaries and nearly isolated melt pockets occupying the space like pools almost separately from each other. The types of melt geometry distributed in the rock matrix is classified into spheres, tubes, cubes, ellipsoids and so on. The models and formula correspond to different melt geometries and distributions are introduced and evaluated.