首页> 外文期刊>International Journal of Rock Mechanics and Mining Sciences >Study on crack formation and propagation in the galleries of the Dagangshan high arch dam in Southwest China based on microseismic monitoring and numerical simulation
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Study on crack formation and propagation in the galleries of the Dagangshan high arch dam in Southwest China based on microseismic monitoring and numerical simulation

机译:基于微震监测和数值模拟的基于微震监测和数值模拟,在中国西南地区大山高拱坝画廊裂缝形成与繁殖研究

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摘要

The Dagangshan high arch dam, located in the area with complicated geological conditions and extremely high seismic intensity in Southwest China, has received substantial attention worldwide. Before the impoundment of the reservoir, continuous deep transverse cracks were observed in the low-elevation galleries of the arch dam. To investigate crack formation and propagation in the galleries of the high arch dam, microseismic monitoring and 3D finite element analysis of the galleries were performed during the filling process. The microseismic monitoring system was installed in the foundation gallery and the drainage gallery to detect microcracks around the galleries of the arch dam. The background stress field for crack formation and propagation in the galleries was studied based on 3D finite element modelling. The results indicate that the self-weight of high arch dam produces excessive circumferential tensile stresses at the arch crown of the galleries near the dam heel before impoundment, which is the cause of crack formation in the galleries of the Dagangshan high arch dam. As the impounded water level rises, the tensile stresses and the microseismicity in the galleries near the arch dam heel transfer to the galleries close to the arch dam toe, and the cracks in the galleries near the dam heel would not propagate further but be closed. However, cracking may occur in the gallery close to the dam toe if its micro-seismicity continues increasing. The conclusions have significant implications for reinforcement and operation of the galleries in similar high concrete arch dams.
机译:DAGANGSHAN高拱坝,位于中国西南地质条件复杂和极高的地震强度的地区,在全球上受到了重大关注。在储存器的蓄水前,在拱门大坝的低升高画廊中观察到连续深横裂。为了研究高拱坝的画廊中的裂缝形成和传播,在填充过程中进行了杂志的微震监测和3D有限元分析。微震监测系统安装在基础库和排水库中,以检测拱门大坝的画廊周围的微裂纹。基于3D有限元建模研究了术的裂缝形成和繁殖中的背景应力场。结果表明,高拱坝的自重在蓄水前在坝鞋跟附近的拱门附近产生过度的圆周拉伸应力,这是大岗山高拱坝的画廊裂缝形成的原因。随着被扣押的水位升高,拱坝脚跟附近的画廊中的拉伸应力和微震性转移到靠近拱门脚趾的画廊,坝跟鞋附近的画廊中的裂缝不会进一步传播,但是被关闭。然而,如果其微观地震性继续增加,则在靠近大坝脚趾的画廊中可能发生破裂。结论对加固和运作具有重大影响,在类似的高混凝土拱坝中的画廊。

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