不可溶盖层下石林的岩溶动力学特征对比研究
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引用本文:谢运球,袁道先.2004.不可溶盖层下石林的岩溶动力学特征对比研究[J].地球学报,25(1):59-62.
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作者单位E-mail
谢运球 中国地质大学湖北武汉430074
中国地质科学院岩溶地质研究所广西桂林541004 
yqx@krast.edu.cn;xieyunqiu@21cn.com 
袁道先 中国地质科学院岩溶地质研究所广西桂林541004  
基金项目:石林研究基金“路南石林非可溶岩盖层下的岩溶动力学研究”,国土资源部岩溶动力学开放研究实验室
中文摘要:本文运用岩溶动力学理论和方法对玄武岩和第三系盖层下石林的岩溶动力学特征进行了对比研究。结果表明,玄武岩盖层下空气的CO2浓度具有双向变化梯度与明显的季节变化,而第三系盖层下随深度递减且季节变化不显著;玄武岩水在雨季和旱季对碳酸盐岩都具有侵蚀性,而第三系水在旱季已饱和;玄武岩裂隙最大渗透张量比第三系大,而最大主轴倾角则比第三系小;玄武岩盖层下石灰岩的百日溶蚀量是第三系的14~22倍。上述特征说明玄武岩盖层下的石林发育好,从而较好地解释了为什么发育好的石林常常与玄武岩相伴出现的现象。
中文关键词:玄武岩盖层  第三系盖层  岩溶动力学
 
A Comparison of Karst Dynamics Features between Stone Forests under Insoluble Covers
Abstract:Using karst dynamics theory and methods, the authors made a comparative investigation on karst dynamics features of Stone Forests under basaltic and Tertiary covers in Shilin area, Yunnan Province. The results demonstrate that CO 2 concentration in air under the basaltic cover shows obvious seasonal variation and a two way variation gradient, while in air under the Tertiary cover, the concentration decreases with depth without obvious seasonal variations. The water in the basalt is erosive to carbonate in rainy and dry seasons, whereas the water in the Tertiary cover is saturated in dry season. The biggest fissure permeability tensor of the basalt is larger than that of the Tertiary, while the largest dip angle of the main axis of the basaltic fracture is smaller. The solution amount of limestone per one hundred days in the basaltic cover is 14~22 times that in the Tertiary cover. All these characteristics suggest the frequent development of Stone Forests under the basaltic cover and account for the frequent spatial association of Stone Forests with basalts.
keywords:basaltic cover  Tertiary cover  karst dynamics
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