摘要
盐岩腔体溶蚀过程是发生在边界层内的溶腔固壁表面与溶液之间的物质交换动态平衡过程,根据盐岩的水溶建腔机理建立数学模型,可以为盐穴储气库的水溶建腔设计提供理论依据。根据物质平衡原理及Fick扩散定律,建立了盐岩溶蚀物理模型;根据流体力学基本原理、对流扩散理论及物质平衡原理,建立了溶腔溶质传输-流体流动数学模型,可求解溶蚀过程中腔体内流体的浓度场和流动速度场分布;根据盐岩溶蚀机理研究,推导出盐岩溶解速度方程,可求解溶腔动边界。用该数学模型进行数值模拟得到的溶腔形态与物理模拟结果吻合较好,能够正确描述盐穴储气库水溶建腔的基本规律,可以用于指导水溶建腔的工程实际。
Process of salt cavern dissolution is a dynamic process of material balance between cavern surface and solution. Based on the theory of hydrodynamics, convection-diffusion and material balance, the mathematics model for solute transmission and liquid flowage was established to evaluate the field of consistence and velocity in the salt cavern. According to the solution mining mechanism, a dissolution velocity equation for halite was derived to describe the development of salt cavern. The numerical simulating result and the physical simulating result were in good agreement, suggesting that the mathematics model will be able to describe the pattern of solution mining and direct the engineering.
出处
《石油勘探与开发》
SCIE
EI
CAS
CSCD
北大核心
2003年第5期107-109,共3页
Petroleum Exploration and Development
关键词
地下储气库
水溶采矿
盐穴
数学模型
underground gas storage
solution mining
salt cavern
mathematics model
