karst basin

基本解释

This paper focuses on application of ANNS in the study of the karst basin and its low flow.
本文主要討論人工神經網絡在喀斯特流域及其枯水逕流研究中的應用。
In Early Carboniferous karst peneplain of Central Guizhou there were a lot of karst negative forms, for example karst basin, karst depression.
黔中一帶早石炭世準溶原麪上，發育大量巖溶負地形，諸如溶盆、溶窪等。
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.
喀斯特流域枯水逕流特征值的影響因素很多，如氣候、流域麪積、巖性、土壤、地貌等等，而能夠確知的信息不多。