龚绪龙, 顾春生, 卢毅, 吕菲菲. 2018: 采水型地裂缝发育演化模型试验研究. 工程地质学报, 26(4): 951-958. DOI: 10.13544/j.cnki.jeg.2017-342
    引用本文: 龚绪龙, 顾春生, 卢毅, 吕菲菲. 2018: 采水型地裂缝发育演化模型试验研究. 工程地质学报, 26(4): 951-958. DOI: 10.13544/j.cnki.jeg.2017-342
    GONG Xulong, GU Chunsheng, LU Yi, LÜ Feifei. 2018: MODEL TEST FOR EVOLUTION OF GROUND FISSURES DUE TO EXTRACTION OF GROUNDWATER. JOURNAL OF ENGINEERING GEOLOGY, 26(4): 951-958. DOI: 10.13544/j.cnki.jeg.2017-342
    Citation: GONG Xulong, GU Chunsheng, LU Yi, LÜ Feifei. 2018: MODEL TEST FOR EVOLUTION OF GROUND FISSURES DUE TO EXTRACTION OF GROUNDWATER. JOURNAL OF ENGINEERING GEOLOGY, 26(4): 951-958. DOI: 10.13544/j.cnki.jeg.2017-342

    采水型地裂缝发育演化模型试验研究

    MODEL TEST FOR EVOLUTION OF GROUND FISSURES DUE TO EXTRACTION OF GROUNDWATER

    • 摘要: 为了研究苏南地区采水型地裂缝成因演化机制,设计建成了抽水与潜山条件大型物理模型系统,运用光纤传感监测技术手段,模拟地裂缝演化进程,并对其分布规律、成因机制做出总结归纳。试验结果表明:(1)模型试验中光纤传感技术能够较为准确地对水位、应力-应变分布等参数进行监测;基于光纤传感技术的模型试验系统为地裂缝研究提供新的方法与手段;(2)岩土体张应力集中区与地裂缝发育位置基本对应,岩土体的张应力集中是判断地裂缝发育阶段的重要标志;(3)通过地裂缝走向玫瑰花图显示,模型平坦区地裂缝发育方向沿排水孔呈放射状分布;而潜山区域地裂缝发育具明显的方向一致性,且与潜山等高线平行;(4)地裂缝分布同时受抽水差异性沉降及潜山形态位置控制。

       

      Abstract: In order to study the formation mechanism of ground fissures in southern Jiangsu, a large-scale physical model is established under the buried-hill condition. The settlement process with water-drawing variability can also be simulated. Fiber optic sensing technology is used for revealing the development and evolution of ground fissures. The distribution and the genetic evolution of ground fissures are summarized. The test results are below:(1)The results of model test are basically consistent with the law of ground fissure disaster in the study area, which provides new methods and means for ground fissure research. (2)The tensile stress concentration of the rock mass is basically the same as the development stage of the ground fissure. Therefore, the stress concentration of the rock mass is an important omen to determine the development stage of the ground fissure. (3)According to rose diagrams analysis, in the flat region, ground fissures are radially distributed and its distribution center is near the drain holes. At the buried hill area, it shows that the shape and location of the buried hill, the settlement curve, and the most serious land area are consistent with the distribution area of ground fissures. (4)Excessive groundwater extraction as well as the location of buried-hill formation have a great influence on the distribution of ground fissures.

       

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