摘要
本文运用系统科学理论的某些基本原理和洞穴发育模拟实验研究成果，在我国南方喀斯特区多年研究实践的基础上，把一个地下流域看作一个物质与能量的输入─输出系统。将这一系统的洞穴发育分为流入（输入）洞穴，流出（输出）洞穴和含水层洞穴三大部分。分析和讨论了它们的发育机制、基本特征、相互关系及整体系统有序化的演化过程。
In this paper,an underground drainage is considered as a input-output system ofmaterial and energy,through which the caves are divided into three types inflow(input),outflow(output)and aquifer ones,by applying some basic principles of sys-tem science and research data from simulation experiment of cave development,and onthe basis of author's several years'study practice in karst area of southern China.While itsdeveloped mechanism,basic charateristics,interralation and ordered evolution processof the whole system are also analysed and discussed in this paper.
出处
《云南地理环境研究》
1994年第2期7-16,共10页
Yunnan Geographic Environment Research
关键词
地下河洞穴
输入-输出系统
系统演化
洞穴发育
Underground River Cavern,Input-Output System, Input Type
Systematic Evolution.
