Creep Energy Evolution of Red-Bed Soft Rocks in South China under Chemical-Stress-Seepage Coupling

IF 1.2 4区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS Geofluids Pub Date : 2024-04-29 DOI:10.1155/2024/1113144
Shuguang Zhang, Fanyao Peng, Yingbo Li, Zhifeng Liu, Wenbo Liu
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Abstract

The red-bed soft rocks in South China have obvious creep characteristics and are prone to engineering geological disasters such as landslide and foundation settlement under the action of rainfall, groundwater, and load. In order to reveal its creep characteristics and mechanism under complex conditions, a step-loading creep test was carried out under chemical-stress-seepage coupling, and the energy evolution law of the whole creep process was analyzed based on linear energy storage and energy dissipation theory. The results also show that the acid chemical solution has the greatest influence on the triaxial strength and creep strength, and the creep damage and energy evolution of red-bed soft rock are universal. The creep damage and total strain increase with the increase of acidity, the decrease of confining pressure, and the increase of seepage pressure. The evolution law of creep damage shows the characteristics of slow-acceleration-rapid growth, and with the increase of load level, it has obvious transfer and accumulation. After entering the constant velocity creep stage, the damage rate begins to accelerate. The proportion of instantaneous strain and creep strain in the total strain increment is about 50%, and confining pressure has little influence on their respective proportions. The instantaneous strain is more sensitive to the acidity of the chemical solution, and the proportion of creep strain increases gradually with the increase of seepage pressure. The relationship between elastic energy density and total energy density is linear. The elastic energy density and dissipated energy density in the loading stage and creep stage all increase nonlinearly with loading time. The density of dissipated energy in the creep phase is lower than that in the loading phase, but the opposite is true in the higher stress phase, and the law of energy dissipation can explain the hardening damage effect in the creep process of soft rock samples. The research results provide a new perspective for us to reveal the mechanical properties and failure mechanism of red-bed soft rocks and provide an important theoretical basis for predicting and evaluating the creep instability and long-term stability of such rocks.

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化学-应力-渗流耦合作用下华南红床软岩的蠕变能演化
华南地区的红层软岩具有明显的蠕变特征,在降雨、地下水和荷载作用下易发生滑坡、地基沉降等工程地质灾害。为揭示其在复杂条件下的蠕变特性和机理,在化学-应力-渗流耦合作用下进行了阶跃加载蠕变试验,并基于线性储能和耗能理论分析了整个蠕变过程的能量演化规律。结果还表明,酸性化学溶液对三轴强度和蠕变强度的影响最大,红层软岩的蠕变损伤和能量演化具有普遍性。蠕变损伤和总应变随着酸度的增加、约束压力的降低和渗流压力的增加而增加。蠕变损伤的演化规律表现为缓慢-加速-快速增长的特征,且随着荷载水平的增加,具有明显的传递和积累作用。进入恒速蠕变阶段后,破坏速率开始加快。瞬时应变和蠕变应变在总应变增量中的比例约为 50%,约束压力对它们各自的比例影响不大。瞬时应变对化学溶液的酸度更为敏感,蠕变应变的比例随着渗流压力的增加而逐渐增大。弹性能量密度与总能量密度之间呈线性关系。加载阶段和蠕变阶段的弹性能量密度和耗散能量密度均随加载时间非线性增加。蠕变阶段的耗散能量密度低于加载阶段,但在高应力阶段则相反,能量耗散规律可以解释软岩样本蠕变过程中的硬化破坏效应。该研究成果为我们揭示红床软岩的力学性质和破坏机理提供了新的视角,为预测和评价此类岩石的蠕变不稳定性和长期稳定性提供了重要的理论依据。
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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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