Journal of the Korean Society of Groundwater Environment (대한지하수환경학회지)
- Volume 6 Issue 3
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- Pages.152-157
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- 1999
Determination of Hydraulic Parameters in Unconfined Sandy Aquifer in a Laboratory Scale
실내 자유면 사질 대수층의 수리상수 결정
Abstract
Oil leaked from underwound storage tanks and leachate from sanitary landfills have been known as contaminant sources of the high-quality groundwater resources. The mobility of contaminants in the aquifer largely depends on the groundwater flow and the determination of associated hydraulic parameters is essential for a proper remediation of contaminated grnundwater. This study aimed at determining an optimum set of hydraulic parameters for an unconfined sandy aquifer of a laboratory scale through comparison of various methods. Results showed that the specific yield obtained from gravity drainage experiment was an average of 0.20 with minor variations in aquifer depths. and the permeabilities obtained from Dupuit approximation and slug test gave similar values of 5.33 cm/min and 5.85 cm/min but the constant head method gave 0.17 cm/min, which is much ion than the other methods. This experimental evidence reveals that the permeability of the unconfined sandy aquifer could be accurately determined by Dupuit assumption or slug tut rather than by constant head method conducted for a disturbed separate soil column.
지하 저장 유류 탱크로부터의 기름 유출이나 쓰레기 매립장으로부터의 침출수는 양질의 지하수 자원에 대한 오염원으로 널리 인지되고 있다. 지하 대수층에 유입된 오염물질의 이동성은 지하수 흐름에 의존하며 이에 관련된 수리상수의 결정은 중요한 과제가 된다. 본 연구의 목적은 사질토로 구성된 실내 자유면 대수층 모형을 구축하여 대수층의 수리상수를 기존의 방법들을 이용하여 결정, 비교함으로써 최적의 수리상수를 결정하는데 있다. 자유면 대수층의 저장율을 나타내는 비산출량(
Keywords