Numerical Modeling of Shear Behavior in Rough Joints of Unsaturated Sandstone

IF 1.2 4区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS
Geofluids Pub Date : 2025-07-30 DOI:10.1155/gfl/6667581
Hanwen Jia, Tengfei Fu, Hongtao Bi, Songtao Hu
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引用次数: 0

Abstract

Using a tessellation method in Neper, the simplified 3DEC-GBM (three-dimensional discrete element grain–based model) is proposed for generating joint models with different roughnesses. The model is extended by implementing the generalized effective stress law to mimic the shear behavior of unsaturated sandstone. The grain-scale mechanical parameters of the model were calibrated to correspond to the mechanical behavior of sandstone samples measured in the laboratories. The simulations accurately explain complex macroscopic shear behavior in terms of the mesoscale interaction of grains. The modeling results show that water has a deteriorating effect that weakens the strength of the joint, and the degree of reduction in joint strength rises with increasing saturation. Increasing normal stress and roughness can all improve the shear strength of the joint. We conclude that the proposed model is a convenient approach to analyze the shear response of unsaturated sandstone at varying roughness and normal stress.

Abstract Image

非饱和砂岩粗糙节理剪切特性数值模拟
利用Neper中的镶嵌法,提出了简化的三维离散单元基于晶粒模型(3DEC-GBM),用于生成不同粗糙度的节理模型。通过引入广义有效应力定律对模型进行扩展,模拟非饱和砂岩的剪切特性。模型的粒度力学参数经过校准,以对应于实验室测量的砂岩样品的力学行为。模拟结果准确地解释了颗粒中尺度相互作用下复杂的宏观剪切行为。模拟结果表明,水具有弱化节理强度的变质作用,且随着饱和度的增加,节理强度的减弱程度增大。增大法向应力和粗糙度均能提高接头的抗剪强度。结果表明,该模型是分析非饱和砂岩在不同粗糙度和正应力条件下剪切响应的一种简便方法。
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来源期刊
Geofluids
Geofluids 地学-地球化学与地球物理
CiteScore
2.80
自引率
17.60%
发文量
835
期刊介绍: Geofluids is a peer-reviewed, Open Access journal that provides a forum for original research and reviews relating to the role of fluids in mineralogical, chemical, and structural evolution of the Earth’s crust. Its explicit aim is to disseminate ideas across the range of sub-disciplines in which Geofluids research is carried out. To this end, authors are encouraged to stress the transdisciplinary relevance and international ramifications of their research. Authors are also encouraged to make their work as accessible as possible to readers from other sub-disciplines. Geofluids emphasizes chemical, microbial, and physical aspects of subsurface fluids throughout the Earth’s crust. Geofluids spans studies of groundwater, terrestrial or submarine geothermal fluids, basinal brines, petroleum, metamorphic waters or magmatic fluids.
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