선택한 단어 수는 입니다.
최소 단어 이상 선택하여야 합니다.
최소 단어 이상 선택하여야 합니다.
선택한 단어 수는 30입니다.
최대 10 단어까지만 선택 가능합니다.
최대 10 단어까지만 선택 가능합니다.
제안 방법
- two different aquifer systems, ie, fractured and porous media. Main goal of the tracer tests was to estimate transport parameter such as dispersivity. The hydrogeologic conditions of the Wonju and Uiwang test sites were well characterized by previous studies (Lee, 1998; Lee and Lee, 1999; Lee and Lee, 2000; Lee et al.
대상 데이터
- The Wonju test site was located at Buron—myun, southwest of Wonju city, Korea. The test site consists mainly of topographically low relief mountains and hills.
- The test site consists mainly of topographically low relief mountains and hills. The top level around the test site is Kinkyungsan (352 m).
- The test site consists mainly of topographically low relief mountains and hills. The top level around the test site is Kinkyungsan (352 m). The stratigraphic units underlying the test site include a Precambrian gneiss bedrock sequence intruded by Jurassic plutonic intmsive and Cretaceous dike, which were covered by reclamation soil (Lee, 1998; Fig.
- The top level around the test site is Kinkyungsan (352 m). The stratigraphic units underlying the test site include a Precambrian gneiss bedrock sequence intruded by Jurassic plutonic intmsive and Cretaceous dike, which were covered by reclamation soil (Lee, 1998; Fig. 1). Natural gradient tracer tests were conducted in both the fractured zone and reclamation zone using bromide (Br ).
- The Uiwang site is located about 45 km southeast of Seoul, Korea. Stratigraphic units underlying the site include Precambnan gneiss, overlying alluvial deposits, and local reclamation soil (Fig. 1). The upper part of the Precambrian gneiss is slightly weathered and lies 5~6 m below the ground surface.
- 5 to 2 m, and 2 to 6 m, respectively, with varying thickness. Surface material is an artificial reclamation soil (clayey-organic soil) or pavement. The main flow of ground water occurs in the gravelly coarse sand layer.
- The Uiwang site is located about 45 km southeast of Seoul, Korea. Stratigraphic units underlying the site include Precambnan gneiss, overlying alluvial deposits, and local reclamation soil (Fig.
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