摘要
Different karst water features and related water resources are present both in southern and northern China. There are over 3,358 well-developed karst ground river systems with total discharges in the dry season of about 420×10^8 m^3 in the main karst regions in the southern part of China. Exploitation rates are only 8-15%. Over 100 larger karst spring systems in the main karst regions of northern China cover a catchment area from 500 km^2 to over 4,000 km^2, of which the average discharge appears to be from about 1 m^3/s to 13 m^3/s and the exploitation rates are 70-80%. Six aspects of the eco- hydrological features of some typical karst regions in China comprising water environment, ecological features, materials and structures between parent rock and soil, bio-geological processes and palynological studies （spore-pollen） are discussed. Qualitative evaluation of eco-geology and rocky desertification in the karst regions should be based on the main karst ecological conditions as well as artificial, i.e., man-made impacts.
Different karst water features and related water resources are present both in southern and northern China. There are over 3,358 well-developed karst ground river systems with total discharges in the dry season of about 420×10^8 m^3 in the main karst regions in the southern part of China. Exploitation rates are only 8-15%. Over 100 larger karst spring systems in the main karst regions of northern China cover a catchment area from 500 km^2 to over 4,000 km^2, of which the average discharge appears to be from about 1 m^3/s to 13 m^3/s and the exploitation rates are 70-80%. Six aspects of the eco- hydrological features of some typical karst regions in China comprising water environment, ecological features, materials and structures between parent rock and soil, bio-geological processes and palynological studies （spore-pollen） are discussed. Qualitative evaluation of eco-geology and rocky desertification in the karst regions should be based on the main karst ecological conditions as well as artificial, i.e., man-made impacts.
基金
This paper results from a comprehensive research project related to water resources supported in 1999-2002 by the Chinese Academy of Engineering
the project of Sulfate Karst Developmental Mechanism and Its Engineering Impacts supported by the National Natural Science Foundation of China(No.49872095)in 2005
research of the Stone Forest Development and Its Environmental Evolution supported by the Shilin Research Centre.
