裂隙岩溶水水源地水位动态模拟和预报中耦合法的运用  

Simulation and Prediction on Karstic Water Level Regime in Groundwater Field

作　　者：陶月赞[1] 席道瑛[1] 

机构地区：[1]中国科学技术大学地球与空间科学学院,合肥市230026

出　　处：《勘察科学技术》2005年第2期12-14,30,共4页Site Investigation Science and Technology

摘　　要：在裂隙岩溶水水源地,由于地下水系统的存储与调蓄作用,地下水水位时间上的自相关性显著。该文结合实例介绍了用水位自回归与多元回归相结合进行水位动态模拟的方法原理,阐述该方法的应用步骤,并与多元回归方法进行了对比分析。Due to the larger volume of storage and regulation in karstic water fi eld, the time-autocorrelation of groundwater level is outstanding.Simulati on and Prediction on the groundwater regime should be interdependent on w ater level autore gression and multivariate regression. The principle and applied process of this method is introduced by this paper.Compared with multivariate regressio n, comprehensive analysis about a real karstic water field is executed.

关 键 词：裂隙岩溶水 水位动态 自回归 动态模拟 耦合法 多元回归 

分 类 号：P641.134[天文地球—地质矿产勘探]