姜伏伟, 雷明堂, 管正德, 吴远斌. 2014: 土洞发育水动力判据及应用研究. 工程地质学报, 22(s1): 77-82. DOI: 10.13544/j.cnki.jeg.2014.s1.014
    引用本文: 姜伏伟, 雷明堂, 管正德, 吴远斌. 2014: 土洞发育水动力判据及应用研究. 工程地质学报, 22(s1): 77-82. DOI: 10.13544/j.cnki.jeg.2014.s1.014
    Jiang Fuwei, Lei Mingtang, Guan Zhengde, Wu Yuanbin. 2014: STUDY ON THE CRITICAL HYDRAULIC CONDITION OF FORMING SOIL-CAVES IN KARST AREA. JOURNAL OF ENGINEERING GEOLOGY, 22(s1): 77-82. DOI: 10.13544/j.cnki.jeg.2014.s1.014
    Citation: Jiang Fuwei, Lei Mingtang, Guan Zhengde, Wu Yuanbin. 2014: STUDY ON THE CRITICAL HYDRAULIC CONDITION OF FORMING SOIL-CAVES IN KARST AREA. JOURNAL OF ENGINEERING GEOLOGY, 22(s1): 77-82. DOI: 10.13544/j.cnki.jeg.2014.s1.014

    土洞发育水动力判据及应用研究

    STUDY ON THE CRITICAL HYDRAULIC CONDITION OF FORMING SOIL-CAVES IN KARST AREA

    • 摘要: 岩溶塌陷主要由土洞造成,但目前对土洞发育临界条件研究较少。本文从管道流理论分析土洞发育判据,建立了数学表达式,并设计了管道流试验装置和试验方法。选取广西武宣县钻孔试样为研究对象,测试计算出地下水位波动临界速度,结合2013年地下水位监测资料,评价土洞发育状况。结果表明,目前情况下,地下水位的波动速度未达到临界值,不具备引起黏性土流失形成土洞的条件。

       

      Abstract: Soil-caves collapse in karst area is a common geological hazard, which make some disaster accidents. However, the critical condition of forming soil-cave is seldom researched now. Based on the theories of pipe flow, this paper derives the formulas of the critical hydraulic condition for assessing soil-caves. The cohesive soils from Wuxuan county, Guangxi province, China, are chosen to be tested to obtain the critical value by a designed test method. Combining the critical value and the monitoring hydraulic data, the results show the current hydraulic condition will not form soil-caves.

       

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