中国北方喀斯特水的某些特征
SOME CHARACTERISTICS OF KARST WATER IN NORTH CHINA
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摘要: <正> 我国北方喀斯特主要分布在华北、东北南部、华东和中南北部以及西北东部,位于秦岭——淮河一线以北的广阔区域内。区内除松辽平原、华北平原和淮河平原外,多为丘陵、山地和高原地形。有辽河、海河、黄河、淮河等水系。主要属亚干旱——亚湿润温带大陆性气候,年降水量为400~800毫米,局部地区小于400毫米;蒸发量为1500~1800毫米(大部地区);年平均相对湿度为55~70%。溶蚀量为10(晋北)及30(鲁中)毫米/千年。Abstract: In North China, karst features occur mainly in Hebei, Shanxi, South Liaoning, northern parts of Shandong and Henan, and Shanxi Provinces, extending to the north of the line from the Qingling mountain range to the Huaihe River. The terrain belongs to a semi-arid and semi-humid warm temperate zone. Karst is not well developed on the land surface, whereas underground is mostly developed in the forms of fissures and pores. The main water-bearing formations are Mid-Ordovician limestones, with copious groundwater...
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