Effect of Water Content on the Impact Propensity of White Sandstone

IF 1.2 4区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS
Geofluids Pub Date : 2023-10-17 DOI:10.1155/2023/8839852
Jiankui Bai, Chuanming Li, Ruimin Feng, Nan Liu, Xiang Gao, Zhengrong Zhang, Bochao Nie
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引用次数: 0

Abstract

Impact ground pressure is one of the most common dynamic disasters induced by mining activities, and water content is an important factor affecting such dynamic disasters. In this paper, uniaxial compression test, cyclic loading and unloading test, and acoustic emission test were conducted on white sandstone using RMT-150B rock mechanics test system and DS5 acoustic emission test system. The influence law of water content was analyzed on the strength characteristics, energy change characteristics, and impact propensity of white sandstone. The results showed that (1) the internal structure of the sandstone gets softened with the increase of the water content. The cohesive effect within the rock also begins to weaken, which in turn reduces the stiffness of the material and enhances its plasticity. The ability of the rock to resist elastic deformation becomes weaker, resulting in lower compressive strength and elastic modulus when the rock is subjected to external forces, making it more prone to deform and fail. The decrease in compressive strength of the water-saturated rock is 33.3%, and the decrease in its elastic modulus is 28.1% compared to the dry rock. (2) As the water content increases, the cohesion of the rock decreases and the internal structure of the rock fails more easily, which ultimately makes the energy needed for rock destruction lower. As a result, the total energy, elastic energy, and dissipative energy of the rock are reduced. The accumulated AE energy also decreases with the increase of the water content, indicating that rocks with higher water content gather less elastic energy before damage and accumulate less energy when deformation damage occurs. (3) The impact energy index and elastic energy index are negatively correlated with the water content. The impact energy index is reduced by 28.6%, and the elastic energy index is reduced by 20.9% for the saturated rock compared to the dry rock. The elastic energy index and impact energy index both decrease with the increase of rock water content, indicating that the less elastic energy is stored before the destruction of the rock and no excess energy is transformed into energy in rock crushing when the rock breaks, and therefore, the impact propensity of the rock is smaller. The results of the study can provide a theoretical basis for underground construction as well as rock fracture destabilization.
含水量对白色砂岩冲击倾向性的影响
冲击地压是采矿活动引起的最常见的动力灾害之一,而含水率是影响冲击地压动力灾害的重要因素。本文采用RMT-150B岩石力学试验系统和DS5声发射试验系统对白色砂岩进行单轴压缩试验、循环加卸载试验和声发射试验。分析了含水量对白砂岩强度特性、能量变化特性和冲击倾向的影响规律。结果表明:(1)砂岩内部结构随着含水率的增加而软化;岩石内部的黏结作用也开始减弱,从而降低了材料的刚度,增强了材料的塑性。岩石抵抗弹性变形的能力变弱,导致岩石在外力作用下抗压强度和弹性模量降低,更容易变形破坏。与干岩相比,饱和水岩石抗压强度降低33.3%,弹性模量降低28.1%。(2)随着含水率的增加,岩石的凝聚力降低,岩石内部结构更容易破坏,最终使岩石破坏所需的能量降低。从而降低了岩石的总能量、弹性能量和耗散能量。累积声发射能量也随着含水率的增加而减小,说明含水率高的岩石在损伤前聚集的弹性能较少,发生变形损伤时积累的能量较少。(3)冲击能指数和弹性能指数与含水率呈负相关。与干燥岩石相比,饱和岩石的冲击能指数降低了28.6%,弹性能指数降低了20.9%。弹性能指数和冲击能指数均随着岩石含水量的增加而减小,说明岩石破坏前储存的弹性能较少,岩石破碎时没有多余的能量转化为破碎时的能量,因此岩石的冲击倾向较小。研究结果可为地下施工及岩体裂隙失稳提供理论依据。
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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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