karst basin

基本解释

This paper focuses on application of ANNS in the study of the karst basin and its low flow.
本文主要讨论人工神经网络在喀斯特流域及其枯水径流研究中的应用。
In Early Carboniferous karst peneplain of Central Guizhou there were a lot of karst negative forms, for example karst basin, karst depression.
黔中一带早石炭世准溶原面上，发育大量岩溶负地形，诸如溶盆、溶洼等。
There are many factors that affect the low flow in a karst basin, such as climate, catchment area, lithology, soil, landform and so on, most of which are uncertain.
喀斯特流域枯水径流特征值的影响因素很多，如气候、流域面积、岩性、土壤、地貌等等，而能够确知的信息不多。