北霞浦冈高地Dejima地区地下水流动系统研究(1)

H. Okazaki, T. Ishikawa, S. Shindo
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引用次数: 4

摘要

近年来,人类活动引起的地下水污染问题已引起人们的重视。为了解决这一问题,我们必须跨越传统的思维方式,获得更详细的地下含水条件及其流动系统的信息。本研究的显著标志是应用沉积相分析来明确研究区地下水系统。分析表明,地下水有三相划分,地下水流动特征受沉积相和构造的限制。在相分析的基础上,利用电导率法对几个地块进行了地下水示踪。结果表明,地下水的流速和方向随季节、地形位置和沉积层位的不同而变化。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Study on Groundwater Flow System in the Dejima Area, the North Kasumigaura Upland (1)
Recently, attention has come to be paid to groundwater contamination caused by human activity. To cope with the problem, we must obtain the more detailed informations about groundwater-bearing condition and its flow system taking long strides from the conventional way of thinking.
The distinguished mark of this study is the application of the sedimentary facies analysis to specify the groundwater system of the study area.
Analysis shows that there are three facies to devide the groundwater and the characteristics of the groundwater flow is limited by the sedimentary facies and structure . On the basis of the facies analysis, the tracing of groundwater is carried out at the several plots using electric conductivity method. As a result, it is clarified that the velocity and direction of groundwater vary with the season, topographic locality and sedimentary horizon of groundwater.
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