Economic and Environmental Geology (자원환경지질)
- Volume 9 Issue 4
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- Pages.225-240
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- 1976
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- 1225-7281(pISSN)
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- 2288-7962(eISSN)
A Studyon the Movment of Ground Water of Banayweol Formation
반야월층(半夜月層)의 지하수운동(地下水運動)에 관(關)한 연구(硏究)
Abstract
This study deals with the flow of bed rock ground water of Banyaweol Formation, which is presently cleared up as a laminar flow. The result obtained may be summarized as the following. 1) The Banyaweol Formation consists mainly of thin-bedded, green to blackish green shale, mudstone, and marl. The marl and mudstone alternatively occur with shale. The marl and mudstone form a aquifer of Banyaweol Formation. In this study, a group of aquifer is in convenience named as a aquifer zone. The aquifer occurs in lenticular form. The aquifer seems to be a type of artesian aquifer because it is covered with aquicludes, but it actually forms a unconfined aquifer because its piezometric surface stays under the lower aquiclude. The lowering of piezometric level is formed because of leakage of the ground water to the lower aquifer undersaturated. 2) The coefficient of permeability of Banyaweol Formation's ground water body (K) is derived by using Dupuit's equation as the following
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