基于FDM-DEM耦合的动态冲击下泥岩宏细观力学特性响应

IF 1.2 4区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS
Geofluids Pub Date : 2025-04-22 DOI:10.1155/gfl/4731135
Jiangkun Yang, Hongfa Ma, Feng Wang, Yuzhong Shen, Linfeng Shi
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引用次数: 0

摘要

现场爆破会对露天矿边坡产生冲击扰动。为了进一步研究露天矿边坡岩体的动态力学特性,本文以内蒙古某露天矿边坡泥岩为研究对象。通过室内劈裂-霍普金森冲击试验和有限差分法与离散元法耦合模拟(FDM-DEM),研究了不同冲击速度下泥岩的宏观和微观冲击力学响应。结果表明,在动荷载作用下,泥岩表现出明显的应变率效应。峰后塑性呈指数递增变化。泥岩裂纹扩展过程可分为未损伤阶段、起裂阶段、扩展阶段和破裂阶段。随着冲击速度的增加,萌生阶段微裂纹增多,破裂阶段裂纹开度增大。三维耦合数值模型能够满足动态冲击过程中的应力有效性。在冲击过程中,微裂纹在应力峰值前急剧增大,且裂纹增量最大值与应力峰值之间存在应变滞后。峰后阶段出现了大量的内部微裂纹,累积裂纹增量呈倒“Z”形。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Response of Macro- and Micromechanical Characteristics of Mudstone Under Dynamic Impact Based on FDM-DEM Coupling

Response of Macro- and Micromechanical Characteristics of Mudstone Under Dynamic Impact Based on FDM-DEM Coupling

The blasting at a site can cause impact disturbances to an open-pit mine slope. For further study the dynamic mechanical properties of rock masses in open-pit mine slope, in this paper, the mudstone of an open-pit slope in Inner Mongolia Autonomous Region of China was taken as research object. Through an indoor split-Hopkinson impact test and a finite difference method and discrete element method coupling simulation (FDM-DEM), the macro and micro impact mechanical response of mudstone under different impact velocities was studied. The results showed that under dynamic load, mudstone exhibited significant strain rate effects. The postpeak plasticity varied in exponentially increasing changes. The crack propagation process in mudstone can be divided into undamaged, initiation, propagation, and rupture stages. As the impact velocity increased, the initiation stage exhibited more microcracks, and the cracks opening in the rupture stage became larger. The 3D coupling numerical model can satisfy stress effectiveness during the dynamic impact process. During the impact process, microcracks increased sharply before the peak stress, and there was a strain lag between the maximum point of crack increment and the peak point of stress. A large number of internal microcracks developed during the postpeak stage, and the cumulative crack increment exhibited a reverse “Z” shape.

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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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