胡明军, 张枝华, 殷跃平, 等. 2023. 三峡库区巫峡段消落带碳酸盐岩强度弱化研究[J]. 工程地质学报, 31(5): 1615-1627. doi: 10.13544/j.cnki.jeg.2021-0220.
    引用本文: 胡明军, 张枝华, 殷跃平, 等. 2023. 三峡库区巫峡段消落带碳酸盐岩强度弱化研究[J]. 工程地质学报, 31(5): 1615-1627. doi: 10.13544/j.cnki.jeg.2021-0220.
    Hu Mingjun, Zhang Zhihua, Yin Yueping, et al. 2023. Study on strength weakening of carbonate rocks with water level fluctuating in Wuxia of Three Gorges Reservoir area[J]. Journal of Engineering Geology, 31(5): 1615-1627. doi: 10.13544/j.cnki.jeg.2021-0220.
    Citation: Hu Mingjun, Zhang Zhihua, Yin Yueping, et al. 2023. Study on strength weakening of carbonate rocks with water level fluctuating in Wuxia of Three Gorges Reservoir area[J]. Journal of Engineering Geology, 31(5): 1615-1627. doi: 10.13544/j.cnki.jeg.2021-0220.

    三峡库区巫峡段消落带碳酸盐岩强度弱化研究

    STUDY ON STRENGTH WEAKENING OF CARBONATE ROCKS WITH WATER LEVEL FLUCTUATING IN WUXIA OF THREE GORGES RESERVOIR AREA

    • 摘要: 三峡库区175 m蓄水以来,巫峡段碳酸盐类岩溶岸坡在周期性水位变动下岩体劣化强烈,新生或加速形成了大量地质灾害。为探讨在周期性水位变动下碳酸盐岩类岸坡的强度弱化规律,文章从岩石(体)物理结构、化学性质、力学性质等方面开展研究,通过在巫峡最具代表性的6处库岸段开展原位岩体回弹强度测试、原位点荷载试验以及室内干湿循环试验、岩石矿物成分分析、岩石表观裂隙扫描等试验,获取水位变动条件下碳酸盐类岩石(体)的强度弱化数据。原位岩体回弹强度测试结果表明,原位岩体单一年度的强度弱化率为0.3%~25.9%,岩体强度弱化主要沿结构面产生;室内干湿循环试验结果表明,在50次干湿循环后,岩石强度弱化率为16.4%~23.9%,变形模量弱化率为17.1%~24.9%;岩石矿物成分分析结果表明,在100次循环后,CaO的溶失量为0.5%~5.6%;岩石表观裂隙扫描结果表明,岩块表面裂纹发育位置发生了水蚀痕迹加重、溶孔变大、裂纹延伸等变形现象。基于干湿循环试验数据,建立岩石强度弱化函数,推导出各点位上的指数函数弱化计算模型。该计算模型可用来预测岩石强度、变形模量与水位循环次数间的数值关系。最后以曲子滩危岩“溃屈”式破坏计算为例,探讨了岩体强度弱化后的灾变效应。研究提出的工作方法和通过试验所得到的数据可为三峡库区岸坡劣化带的防治提供数据和技术支撑。

       

      Abstract: Since the impoundment to the elevation 175 m above sea level in the Three Gorges reservoir area, the carbonate karst bank slopes of the Wuxia area have been deteriorating strongly under the periodic water level fluctuations, and a large number of geological disasters have been new-born or developed rapidly. This paper aims to study the law of strength weakening of carbonate bank slopes under cyclical water level fluctuations. It conducted researches from the physical structure, chemical properties, and mechanical properties of the rock(or rockmass). Six most representative reservoir banks in Wuxia area were selected, where in-situ rock rebound strength test, in-situ point loading test and indoor wet-dry cycle test, rock mineral composition analysis, rock apparent fissures scanning test were carried out. Through these tests, the strength weakening data of carbonate rocks(or rockmass) under the condition of fluctuating water were obtained. The results of in-situ rock rebound strength test show that the strength weakening rate of in-situ rockmass is 0.3% to 25.9% per year. The results of indoor dry-wet cycle test show that after 50 dry-wet cycles, the strength weakening rate of rock is 16.4% to 23.9%, and the deformation modulus weakening rate is 17.1% to 24.9%. The results of mineral composition analysis show that the dissolution loss of CaO is 0.5% to 5.6% after 100 cycles. Through the scanning results of rock apparent fissures, new signs of deformation were found on the rock surface, the water erosion marks were aggravated, the solution pores were enlarged and the cracks were extended. Based on the dry-wet cycle test data, the rock strength weakening function is established, and the exponential function weakening calculation model at each point is deduced. Then such functions can be used to predict the numerical relationship between rock strengths, deformation modulus and water level cycle times. Taking the Quzitan dangerous rock as an example, the catastrophic effect of rock strength weakening is discussed. The work methods and the data obtained from the research can provide data and technical supports for the prevention and control of the bank slope deterioration zone in the Three Gorges Reservoir area.

       

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