Study on Characteristics of the Water-Sediment Two-Phase Flow in Fractures Based on Numerical Simulation

Author:

Cao Lili1,Wu Chuan1ORCID,Xu Hanhua23,Yu Hao4,Li Ming4ORCID,Han Yu4ORCID,Chen Zhanqing4

Affiliation:

1. School of Medical Information and Engineering, Xuzhou Medical University, Xuzhou, Jiangsu 221004, China

2. Kunming Prospecting Design Institute of China Nonferrous Metals Industry Co., Ltd., Kunming, Yunnan 650051, China

3. State Key Laboratory for Geomechanics and Deep Underground Engineering, China University of Mining and Technology, Xuzhou, Jiangsu 221116, China

4. School of Earth Science, China University of Geosciences, Wuhan, Hubei 430074, China

Abstract

The instability of water-sediment flow in fractures can easily induce water-sediment disasters. Therefore, it is of great significance for the prevention and control of water-sediment inrush to study the water-sediment two-phase flow in fractures. Based on the water-sediment two-phase flow theory, a model of the water-sediment two-phase flow system was established. The Ansys Fluent software was used to study the characteristics of the water-sediment two-phase flow in smooth and rough fractures. The spatial-temporal evolution laws of the water-sediment two-phase flow were studied; the results indicated that they did not change with time in the smooth fractured flow fields, while changing continuously with time in the rough fractured flow fields and in a dynamic steady state. The research results can provide references for the water-sediment two-phase flow in fractures and rock mass.

Publisher

Hindawi Limited

Subject

General Earth and Planetary Sciences

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