Numerical Simulation on the Seepage Properties of Soil-Rock Mixture
To reveal the mechanism of water inrush in a fault tunnel and study the influence of different structures on the seepage process, a filling structure composed of a soil skeleton (fixed particles), a movable particles phase, and a water phase is constructed to simulate the rock mass broken by the fau...
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Wiley
2018-01-01
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Series: | Advances in Materials Science and Engineering |
Online Access: | http://dx.doi.org/10.1155/2018/1859319 |
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author | Ning Zhao Yingchao Wang Bo Meng Ning Luo |
author_facet | Ning Zhao Yingchao Wang Bo Meng Ning Luo |
author_sort | Ning Zhao |
collection | DOAJ |
description | To reveal the mechanism of water inrush in a fault tunnel and study the influence of different structures on the seepage process, a filling structure composed of a soil skeleton (fixed particles), a movable particles phase, and a water phase is constructed to simulate the rock mass broken by the fault. Fluent software is used to simulate the migration of the water phase in three different filling structures under different initial water velocities and dynamic viscosities. The variation law of the seepage time with the initial water velocity and dynamic viscosity in the three types of filling structures is obtained. The research shows the following: (1) the looser the filling structure, the greater the influence of gravity on the water phase seepage; the more compact the filling structure, the greater the spread range of the water phase and the more uniform the spread of the water phase. (2) The seepage time decreases with the increase in the initial water velocity. The seepage time and initial water velocity can be fitted by an exponential function. The effect of initial water velocity on seepage time is much greater than that of the structure. (3) The seepage time is related to both the dynamic viscosity and the structure. The seepage time increases with the increase in dynamic viscosity. |
format | Article |
id | doaj-art-3eafe7f57b714548b144ea88c700f791 |
institution | Kabale University |
issn | 1687-8434 1687-8442 |
language | English |
publishDate | 2018-01-01 |
publisher | Wiley |
record_format | Article |
series | Advances in Materials Science and Engineering |
spelling | doaj-art-3eafe7f57b714548b144ea88c700f7912025-02-03T01:30:13ZengWileyAdvances in Materials Science and Engineering1687-84341687-84422018-01-01201810.1155/2018/18593191859319Numerical Simulation on the Seepage Properties of Soil-Rock MixtureNing Zhao0Yingchao Wang1Bo Meng2Ning Luo3State Key Laboratory for Geomechanics and Deep Underground Engineering, China University of Mining and Technology, Xuzhou, Jiangsu 221116, ChinaState Key Laboratory for Geomechanics and Deep Underground Engineering, China University of Mining and Technology, Xuzhou, Jiangsu 221116, ChinaSchool of Mechanics & Civil Engineering, China University of Mining and Technology, Xuzhou, Jiangsu 221116, ChinaSchool of Mechanics & Civil Engineering, China University of Mining and Technology, Xuzhou, Jiangsu 221116, ChinaTo reveal the mechanism of water inrush in a fault tunnel and study the influence of different structures on the seepage process, a filling structure composed of a soil skeleton (fixed particles), a movable particles phase, and a water phase is constructed to simulate the rock mass broken by the fault. Fluent software is used to simulate the migration of the water phase in three different filling structures under different initial water velocities and dynamic viscosities. The variation law of the seepage time with the initial water velocity and dynamic viscosity in the three types of filling structures is obtained. The research shows the following: (1) the looser the filling structure, the greater the influence of gravity on the water phase seepage; the more compact the filling structure, the greater the spread range of the water phase and the more uniform the spread of the water phase. (2) The seepage time decreases with the increase in the initial water velocity. The seepage time and initial water velocity can be fitted by an exponential function. The effect of initial water velocity on seepage time is much greater than that of the structure. (3) The seepage time is related to both the dynamic viscosity and the structure. The seepage time increases with the increase in dynamic viscosity.http://dx.doi.org/10.1155/2018/1859319 |
spellingShingle | Ning Zhao Yingchao Wang Bo Meng Ning Luo Numerical Simulation on the Seepage Properties of Soil-Rock Mixture Advances in Materials Science and Engineering |
title | Numerical Simulation on the Seepage Properties of Soil-Rock Mixture |
title_full | Numerical Simulation on the Seepage Properties of Soil-Rock Mixture |
title_fullStr | Numerical Simulation on the Seepage Properties of Soil-Rock Mixture |
title_full_unstemmed | Numerical Simulation on the Seepage Properties of Soil-Rock Mixture |
title_short | Numerical Simulation on the Seepage Properties of Soil-Rock Mixture |
title_sort | numerical simulation on the seepage properties of soil rock mixture |
url | http://dx.doi.org/10.1155/2018/1859319 |
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