含水层脆弱性量化的动态因子分析

J. Kovács, L. Márkus, Gábor Halupka
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引用次数: 20

摘要

地下岩溶水位的波动是一种具有内在随机性的、非常复杂的时变现象,在人为干扰的情况下,其变化过程更加复杂。然而,它的结构可以通过识别几个潜在的影响或因素(通常是简单得多的动态结构)来探索,这些因素是其背后的驱动力。从时间上相互依赖的观测中确定潜在影响的正确统计工具是动态因子分析(DFA)。与普通因子分析类似,DFA还确定了代表与该因子对应的潜在效应强度度量的负荷。所获得的因子强度提供了关于地质环境的基本信息,当环境问题被提上议程时,提高了作出正确决定的机会。在给定的情况下,这些因素对应于渗透和水提取;因此,强度似乎与含水层的脆弱性有关。密集的w……
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Dynamic factor analysis for quantifying aquifer vulnerability
The fluctuation of underground karstwater levels constitutes an inherently random, very complex time-dependent phenomenon further complicated when human interference disturbs the natural course. However, its structure can be explored by identifying only a few latent effects or factors (usually of significantly simpler dynamic structure), that are the driving forces behind it. The correct statistical tool to determine latent effects from the temporally interdependent observations is dynamic factor analysis (DFA). Analogously to ordinary factor analysis, DFA also determines loadings representing the measure of intensity of the latent effect corresponding to the factor. The obtained factor-intensities provide essential information on the geologic environment, improving the chance of correct decisions when environmental issues are on the agenda. In the given case the factors correspond to the infiltration and water extraction; hence, the intensities appear to be connected to aquifer vulnerability. Intensive w...
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