南方岩溶地区1∶5万水文地质环境地质调查技术要点分析

夏日元; 邹胜章; 唐建生; 梁彬; 曹建文; 卢海平

doi:10.11932/karst20170501

南方岩溶地区1∶5万水文地质环境地质调查技术要点分析

doi: 10.11932/karst20170501

中国地质科学院岩溶地质研究所/国土资源部、广西岩溶动力学重点实验室

基金项目: “岩溶地区水文地质环境地质综合调查工程”、中国地质调查局地质调查项目(1212011121157，1212011121164,1212011121166, 1212011220959，DD20160300，DD20160302)

计量
- 文章访问数: 2229
- HTML浏览量: 739
- PDF下载量: 2407
- 被引次数: 0
出版历程
- 发布日期: 2017-10-25

Technical key points of 1∶50，000 hydrogeological and environmental geology surveys in karst areas of South China

Institute of Karst Geology, CAGS/Key Laboratory of Karst Dynamics, MLR & GZAR

摘要

摘要: 通过总结南方岩溶地区水文地质环境地质综合调查和地下水开发利用示范6个方面成果，得出南方岩溶地区水文地质环境地质条件具有10个特性：岩溶发育受层组结构类型、地质构造格局和水动力条件等因素控制的综合性，岩溶地下水分布的非均一性，岩溶含水介质由孔、隙、缝、管、洞构成的多重性，岩溶地下水流运动的多相性，岩溶地下水动态变化的剧变性，岩溶水资源时间分布的季节性，干旱与洪涝的交替性，岩溶地下水污染的隐蔽性，岩溶地下水的深埋性，岩溶地下水与生态经济的相关性；论述了对碳酸盐岩层组结构类型、构造演化与岩溶发育期次、岩溶形态组合关系、表层岩溶带、岩溶地下水系统、岩溶地下河、主要环境地质问题和岩溶水资源开发利用条件8个关键科学问题调查研究的技术要点。
- 南方岩溶地区 /
- 水文地质调查 /
- 环境地质问题 /
- 地下河 /
- 水资源
Abstract: The karst area in South China is about 520,000 square kilometers, which is controlled by the rock properties, group structure types, geological structural framework, topography and hydrodynamic conditions. The development and distribution of karst in the area is quite uneven. The special subsurface-underground double-deck structure leads to the lack of surface water and deep buried underground water. With the influence of global climate change and irrational human activities, rocky desertification, drought and flood disasters, groundwater pollution and other major environmental geological problems have occurred in karst areas of South China. These natural and man-made factors have seriously restricted the sustainable development of regional social economy, making many karst areas become one of the poorest areas in the country. In order to promote the economic development, ecological civilization construction and poverty alleviation of the karst areas in South China, it is necessary to further clarify the karst hydrogeology and environmental geology conditions, providing a basis for the development and utilization of resources, offering water resources guarantee for the residents and economic development of areas with serious water shortage, and technical support for the protection and control of ecological environments.By summarizing the six research results on the comprehensive investigations of hydrogeology and environmental geology and groundwater development and utilization in the karst areas of South China, this study suggests 10 characteristics of hydrogeological and environmental geology conditions in karst areas of South China, which are stated below, the comprehensiveness of karst development controlled by the strata structure, geologic structure frames and hydrodynamic conditions; heterogeneity of karst groundwater distribution; multiplicity of karst water-bearing media by pores, gaps, joints, pipes and holes; multiphase characteristics of karst groundwater flow; variability of karst groundwater dynamics; seasonal distribution of karst groundwater resources; alternation of drought and flood; concealment of karst groundwater pollution; big buried depth of karst groundwater; and correlation between karst groundwater and ecological economy. At the same time, this study discusses the technical points of investigations and research on the 8 key scientific problems, including carbonate rock group structure, tectonic evolution and development period of karst, karst-form combination relationship, surface karst zones, karst groundwater systems, karst underground river, the main problems of environmental geology, and development and utilization of karst water resources.
- karst areas in South China /
- hydrogeology survey /
- environmental geological problems /
- underground water /
- water resources

HTML

参考文献(25)

[1]	袁道先.西南岩溶石山地区重大环境地质问题及对策研究［M］.北京：科学出版社，2014：3-8.
[2]	陈梦熊.西南岩溶石山地区岩溶水资源与石漠化治理.中国岩溶地下水与石漠化研［M］.南宁：广西科学技术出版社，2003：1-12.
[3]	张之淦.岩溶发生学［M］.桂林：广西师范大学出版社，2006：198-232.
[4]	袁道先，曹建华.岩溶动力学的理论与实践［M］.北京：科学出版社，2008：23-35.
[5]	王明章，张林，王伟.贵州省岩溶区地下水与地质环境［M］.北京：地质出版社，2015：163-257.
[6]	曹建华，袁道先，裴建国.受地质条件制约的中国西南岩溶生态系统［M］.北京：地质出版社，2005：36-45.
[7]	夏日元，蒋忠诚，邹胜章，等.岩溶地区水文地质环境地质综合调查工程进展［J］.中国地质调查，2017，4（1）：1-10.
[8]	王宇，李燕，谭继中.断陷盆地岩溶水赋存规律［M］.昆明：云南科技出版社，2003：4-22.
[9]	王喆，卢丽，夏日元.岩溶地下河系统演化的数值模拟［J］.长江科学院院报，2013，30（7）：22-28.
[10]	王宇，张华，张贵，等．云南省石漠化调查及治理综述［J］．中国岩溶，2016，35(5)：486-496．
[11]	张华，王宇，柴金龙．滇池流域石漠化特征分析［J］．中国岩溶，2011，30(2)：181-186.
[12]	蒋忠诚,夏日元，时坚，等. 西南岩溶地下水资源开发利用效应与潜力分析［J］. 地球学报, 2006, 27(5):495-502.
[13]	唐建生，何成新，庞冬辉.桂中岩溶干旱区综合治理技术开发与示范［M］.北京：地质出版社，2007：57-82.
[14]	张之淦，苏宗明，吴其祥，等.岩溶干旱治理［M］.武汉：中国地质大学出版社，2005：3-67.
[15]	蒋忠诚，李先琨，曾馥平.岩溶峰丛洼地生态重建［M］.北京：地质出版社，2007：1-20.
[16]	Lianxing Yi， Riyuan Xia， Jiansheng Tang，et al. Karst conduit hydro-gradient nonlinear variation feature study:case study of Zhaidi karst underground river［J］. Environment Earth Science,2015,74(2):1071-1078.
[17]	覃小群，蒋忠诚，李庆松.广西岩溶区地下河分布特征与开发利用［J］.水文地质工程地质，2007，34（6）：10-13.
[18]	王明章,王伟, 周忠赋. 峰丛洼地区地下地表联合成库地下水开发模式：贵州普定马官水洞地下河开发利用［J］. 贵州地质, 2005,22(4)：279-283.
[19]	陈伟海. 峰林平原区含水层特征与地下水开发：以广西来宾峰林平原区为例［J］. 广西科学，2000, 7(4)：289-292.
[20]	袁道先，蔡桂鸿．岩溶环境学［M］．重庆：重庆出版社，1988：124．
[21]	易连兴，夏日元，卢东华.水化学分析在勘探确认地下河管道中的应用［J］.工程勘察，2012（2）：43-46.
[22]	朱学稳.喀斯特与洞穴研究［M］.北京：地质出版社，2010：299-307.
[23]	陈宏峰，何愿，夏日元.岩溶水文地质学方法（译）［M］.北京：科学出版社，2015：191-205.
[24]	杨立铮.中国南方地下河分布特征［J］.中国岩溶，1985，4（1-2）：92-99.
[25]	XIA Riyuan.The Groundwater Resources in the Karst Area in Southern China and the Sustainable Utilization Pattern［J］.Journal of Groundwater Science and Engineering,2016,4(4)：301-309.