karst basin

基本解釋

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(jīng)網(wǎng)絡(luò)在喀斯特流域及其枯水徑流研究中的應(yīng)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(zhǔn)溶原面上，發(fā)育大量巖溶負(fù)地形，諸如溶盆、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.
喀斯特流域枯水徑流特征值的影響因素很多，如氣候、流域面積、巖性、土壤、地貌等等，而能夠確知的信息不多。