| 峰丛洼地形成动力过程与水资源开发利用 |
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| 引用本文： | 杨明德,梁 虹. 峰丛洼地形成动力过程与水资源开发利用[J]. 中国岩溶, 2000, 19(1): 44-51. DOI: 10.3969/j.issn.1001-4810.2000.01.007 |
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| 作者姓名： | 杨明德 梁 虹 |
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| 作者单位： | 贵州师范大学资源与环境科学系,贵阳 |
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| 摘 要： | 对喀斯特的重要地貌景观—— 峰丛洼地(锥状喀斯特) ,从水文地貌学观点分析论述了其气候形态学特征、地貌结构、地貌发育演化动力过程以及与内源水作用过程相关的多元水赋存特点及其水资源开发利用形式。
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| 关 键 词： | 峰丛洼地 形成动力过程 水资源 开发利用 |
THE PROCESSES OF EVOLUTION DYNAMIC OF CONE KARSTAND THE EXPLOITATION OF THE WATER RESOURCE |
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| Yang Mingde and Liang Hong. THE PROCESSES OF EVOLUTION DYNAMIC OF CONE KARSTAND THE EXPLOITATION OF THE WATER RESOURCE[J]. Carsologica Sinica, 2000, 19(1): 44-51. DOI: 10.3969/j.issn.1001-4810.2000.01.007 |
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| Authors: | Yang Mingde and Liang Hong |
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| Affiliation: | Guizhou Normal University , Guiyang 550001, China |
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| Abstract: | Fromthe viewpoint of hydrogeomorphology, this paper analyses the cone karstclimate-morphologic features in humid-tropic zone,the cone karst dual-structure whichconsists of cone hill equilibrium layer and depression dynamic evolution layer, and thegeomorphologic evolution processes, and then discusses the pluralistic hydrologicoccurrence characteristics relevant to autogenic water, and the exploitation methods ofthe water resources. |
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