中国北方裂隙岩溶水资源开发和保护中若干问题的研究  

Study of Some Problems on the Development and Protection of Fracture-karst Water Resources in North China

作　　者：刘建立[1] 朱学愚[1] 钱孝星[2] 

机构地区：[1]南京大学地球科学系,210093 [2]河海大学土木工程学院,南京210098

出　　处：《地质学报》2000年第4期344-352,共9页Acta Geologica Sinica

基　　金：国家自然科学基金(编号49772162);博士点基金(编号1999028421)

摘　　要：我国由于人口多、水资源贫乏,裂隙岩溶水成为北方重要的供水水源。本文从裂隙岩溶水和裂隙岩溶含水层的水力特性出发,研究了裂隙岩溶水井的成井深度,裂隙岩溶水资源的特点,补给量和储存量对水资源开发的影响,裂隙岩溶含水层中污染物的运移特征和治理对策以及城市总体规划或选厂址时如何保护裂隙岩溶水资源等问题。本文以解决实际应用问题为目的,从地下水水力学的角度研究中国北方的裂隙岩溶水的开发和保护。Water resources are in shortage in China, especially in northern China. As surface water often dries in spring and summer, fracture-karst water becomes an important source for supply.Karst in China can be divided into three types: karst in northern China, karst in southern China and karst in western China. Karst in northern China is not a typical karst but a fracture karst. The aquifers are networks of solution fractures, fissures and openings. Some wide solution fractures become strong runoff zones. The aquifer has a large coefficient of transmissibility and small storage capacity. It is strongly heterogeneous and anisotropic. Fracture-karst water flows at a high velocity and so the transport of contaminants is a advection-dominated problem. The amount of fracture-karst water depends on the condition of recharge. As the storage capacity is small, the fluctuation of water level in wells is greater than that in porous aquifer.According to the previous data, some authors suggested that the depths of wells in a fracture-karst aquifer should be less than 100-300 m. In the Zibo area we found that some deep wells (at depths 500-700 m) had also great pumping rates and the yields reached 3000-5000 m3/d. It may be related to the palaeokarst in the geologic history.Fracture-karst water is vulnerable to contamination and the environment is fragile. Therefore, factories, plants, dumps and landfills should not be placed on the recharge areas of fracture-karst water. When making land planning, considerations should be given to protect cultivated land as well as groundwater resources. Compared with porous water both the velocity and the distance of plume movement in fracture-karst water are much larger. The curves of contaminant concentrations versus time in fracture-karst wells often fluctuate greatly, which are different from those in porous water wells. Pumping is one of the best methods for remediation. If the area of the groundwater basin is not large, we can renew contaminated water by pumping. If it is large or the pollu

关 键 词：裂隙岩溶水 地下水 水力学特性 水资源 保护 

分 类 号：P641.8[天文地球—地质矿产勘探] P641.135[天文地球—地质学]