Mechanical Behavior and Damage Modeling of Dolomite Under Drying–Wetting Cycles and Variable Lower Bound Cyclic Loading

IF 1.3 4区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS
Geofluids Pub Date : 2026-07-07 DOI:10.1155/gfl/5592198
Xinqi Yang, Qihang Li, Yunmin Wang, Xiaoshuang Li, Jun Lu, Yanhong Xie
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Abstract

To investigate the long-term stability of open-pit mine slopes under the coupled effects of seasonal rainfall-induced drying–wetting (D-W) cycles and mining-related transportation machinery loads, variable lower limit cyclic loading tests were conducted under a confining pressure of 1 MPa on intact dolomite specimens subjected to 0, 1, 5, 10, and 30 D-W cycles. The evolution of physical and mechanical properties, energy dissipation behavior, and failure modes was systematically investigated. Results show that water absorption increased significantly from 0.48% to 1.56% with an increasing number of D-W cycles, whereas the peak strength gradually decreased. Specifically, peak strain increased markedly in the early stage and then tended to stabilize. As the lower stress limit increased, the peak strength exhibited a quadratic trend. Moreover, when the lower stress limit was ≤ 15 MPa, cyclic loading produced a strengthening effect, with the peak strength increasing by up to 10.2%. The dissipated energy density increased significantly with the number of D-W cycles, and a damage constitutive model—derived primarily from theoretical analysis and refined through empirical correction—was established. Moreover, increasing the lower stress limit promoted a transition in the macroscopic failure mode from tensile to shear failure, which was further intensified by D-W cycling.

Abstract Image

干湿循环和变下界循环加载下白云岩力学行为及损伤建模
为了研究季节性降雨干湿循环和采矿相关运输机械载荷耦合作用下露天矿边坡的长期稳定性,在1 MPa围压条件下,对完整白云岩试件进行了0、1、5、10和30个D-W循环的可变下限循环加载试验。系统地研究了其物理力学性能、能量耗散行为和破坏模式的演变。结果表明:随着D-W循环次数的增加,吸水率从0.48%显著增加到1.56%,而峰值强度逐渐降低;其中,峰值应变在早期显著增加,之后趋于稳定。随着下应力极限的增大,峰值强度呈二次曲线趋势。当下应力极限≤15 MPa时,循环加载产生强化效果,峰值强度提高10.2%。随着D-W循环次数的增加,耗散能量密度显著增加,并建立了以理论分析为主、经验修正为基础的损伤本构模型。提高下应力极限,促进宏观破坏模式由拉伸破坏向剪切破坏转变,而D-W循环进一步强化了这一破坏模式。
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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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