多孔介质
水力压裂
压缩性
材料科学
成核
机械
多孔性
岩土工程
相(物质)
混合理论
领域(数学)
地质学
复合材料
热力学
物理
计算机科学
人工智能
量子力学
混合模型
纯数学
数学
作者
Mangesh Pise,Joachim Bluhm,Jörg Schröder
标识
DOI:10.1615/intjmultcompeng.2019027066
摘要
In many fields of engineering, especially in geo sciences and rock mechanics, the theoretical and numerical modeling of hydraulic fracturing of porous materials plays an important role. Hydraulic fracturing is a well-known technology in which porous materials are fractured by a pressurized liquid. The process involves the pressure injection of a fracking fluid (primarily water, often enriched with filling materials and thickening agents) and accompanied by crack nucleation and propagation, as well as mass transport. This article presents a macroscopic model based on the Theory of Porous Media (TPM). For simplification, an incompressible binary model consisting of the solid and liquid phases is used. The development of the damage of the elastic-plastic solid phase is controlled by an evolution equation, which corresponds to known diffusive phase-field models within a continuum mechanical framework. A numerical example shows that the simplified model is indeed capable of simulating hydraulic fracturing of porous media.
科研通智能强力驱动
Strongly Powered by AbleSci AI