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贵州普定后寨河流域喀斯特水文地貌空间耦合分析
Karst hydor-geomorphological spatial coupling analysis of the houzhaihe drainage area in puding cocmty cuizhou province
【摘要】 通过趋势面分析等数学手段 ,揭示后寨河流域内地貌演化和水系变迁的规律性 ,并指出波玉 -木拱河的不断下切导致了侵蚀基准面的降低 ,进而对流域内地貌和水系的演化产生了重要影响。
【Abstract】 Hydrology and geomorphology in karst drainage area interact with each other and form an organic system, as is the special case in small karst drainage. This paper, by using a mathematical method of tendency surface analysis, is to reveal the evolutional rgeularity of geomorphology and the alteration of river system in this area, and points out that the constant down cutting of Boyu Mugong river, which results in a lowering of baselevel, has a sighificant effect on the evolution of geomorphology and river system.
【关键词】 喀斯特流域;
趋势面分析;
侵蚀基准面;
裂点;
【Key words】 Karst drainage area; thendency surface analysis; base-level; knick point;
【Key words】 Karst drainage area; thendency surface analysis; base-level; knick point;
【基金】 国家自然科学基金资助项目!(5 95 6 90 0 1)
- 【文献出处】 贵州师范大学学报(自然科学版) ,JOURNAL OF GUIZHOU NORMAL UNIVERSITY(NATURAL SCIENCE) , 编辑部邮箱 ,2000年02期
- 【分类号】P931
- 【被引频次】22
- 【下载频次】331