Research on influential factors of the karst collapse in the Tailai Basin of Shandong Province
-
摘要: 岩溶塌陷地质灾害的发生是一个复杂的、多因素共同作用的过程。塌陷虽然受多种因素的影响,但不外乎可溶岩类岩溶发育程度、覆盖层特征和动力条件(主要是地下水动力条件)3个基本因素。文章在总结和分析前人研究的基础上,结合最新调查成果,对影响岩溶塌陷的3个基本因素逐一分解,揭示了各因素对岩溶塌陷的影响和作用规律,探讨了岩溶塌陷地质灾害与其主要影响因素的相关关系:质纯厚层的石灰岩分布区岩溶塌陷最为发育,地质构造对岩溶塌陷具有明显的控制作用;研究区内主要岩溶塌陷区的覆盖层以多元结构为主,其次为一元结构和二元结构,区内岩溶塌陷发生于覆盖层厚度小于30 m的区域;岩溶地下水位在基岩面上下波动时最易引发岩溶塌陷,岩溶塌陷点数量的自然对数与岩溶地下水位变幅近似呈线型正相关,塌陷点数量与岩溶地下水开采模数的自然对数值近似呈指数型正相关。Abstract: The geologic disaster of karst collapse is a complicated process controlled by multiple factors. Though the karst collapse is influenced by many factors, it is largely controlled by the degree of karstification,the characteristics of overburden layers and the dynamic conditions (mainly groundwater dynamic condition). On the basis of previous studies and the latest investigation,this paper has analyzed the 3 influential factors and reveals the impact conditions and function on karst collapses. Results show that,(1) the karst collapses mostly develop in the locality with thick-layered limestone of high purity, while geological structure has an obvious control on the karst collapse; (2) the karst collapses in the study area mainly occur in Quaternary strata with multiple structures, followed by quaternary strata with unitary structure and dualistic structures. Moreover, karst the collapse occurred in the area of quaternary strata are less than 30 meters in thickness; (3) the karst collapse most frequently happen at where the cavern water level fluctuates around the bedrock surface. There is an approximately linear positive correlation between the natural logarithm of the karst collapse number and changes in cavern water level; there is also an approximately exponential positive correlation between the karst collapse number and natural logarithm of the exploitation modulus of cavern water. This paper can provide scientific basis for the integrated control of karst collapse in the study area.
-
Key words:
- karst collapse /
- influencing factors /
- correlations /
- geological hazard /
- Tailai Basin
-
[1] 于青春,沈继芳.岩溶地面塌陷机理分析[J].地质灾害与防治,1991,2(1):97-102. [2] 朱大力. 泰安地面塌陷若干数理统计[J]. 铁道工程学报,1996,(4):66-70. [3] 袁杰,高宗军,马海会.论岩溶地下水位对岩溶塌陷形成的控制作用:以山东枣庄市岩溶地面塌陷区为例[J].中国地质灾害与防治学报,2010,21(4):95-98. [4] 王国强.隐伏岩溶地面塌陷的探讨[J].水文地质工程地质,1993,1993,(3):50-51. [5] 何宗彬.喀斯特机理研究[J].上海地质,1993,(2):63. [6] 王延岭,陈伟清,蒋小珍,等.山东省泰莱盆地岩溶塌陷发育特征及形成机理[J].中国岩溶,2015,34(5):495-506. [7] 赵博超,朱蓓,王弘元,等.浅谈岩溶塌陷的影响因素与模型研究[J].中国岩溶,2015,34(5):515-521. [8] 王滨,贺可强.山东省枣庄市市中区岩溶塌陷调查与成因分析[J].地质灾害与环境保护,2004,15(4):26-34. [9] 蒙彦,殷坤龙,雷明堂.水位波动诱发岩溶塌陷的概率分析[J].中国岩溶,2006,25(3):239-245. [10] 刘建茂,郑文忠.新构造断裂对莱芜铁矿田中岩溶地面塌陷的控制作用[J].地质找矿论丛,2002,17(4):282-286. [11] 贺可强,王滨,杜汝霖.中国北方岩溶塌陷[M].北京:地质出版社,2005:45-65. [12] 高宗军.岩溶地面塌陷形成机理与成因模式研究:以山东泰安-莱芜为例[J].中国工程科学,2008,(4):38-43. [13] 成世才,郭加朋,马海会,等.泰安市岩溶地面塌陷动力诱导因素分析[J].山东国土资源,2009,25(12):42-45. [14] 高宗军.泰安市岩溶地面形成机理与防治对策[J].中国地质灾害与防治学报,2001,12(4):73-76. [15] 高宗军,孙文广,唐蒙生,等.泰安-旧县水源区岩溶水开采与地质环境的关系[J].山东地质,2001,17(3-4):86-91. [16] 高宗军,张富中,鲁峰.山东泰安岩溶地面塌陷前兆及其预测预报[J].中国地质灾害与防治学报,2004,15(3):149-150. [17] 山东省地质调查院.山东省泰安地区岩溶塌陷调查与风险评估报告[R].2006. [18] 山东省第五地质矿产勘查院.山东省泰莱盆地岩溶塌陷机理研究及风险区预测报告[R].2014. [19] 山东省地质环境研究院.山东省莱芜市孟公清-西泉河地区矿山地质灾害勘查报告[R].1997. [20] 泰安地质环境监测站.山东省泰安市地下水动态监测报告[R].1981-2014. [21] 莱芜地质环境监测站.山东省莱芜市地下水动态监测报告[R].1994-2014.
点击查看大图
计量
- 文章访问数: 2646
- HTML浏览量: 507
- PDF下载量: 1240
- 被引次数: 0