지원사업
학술연구/단체지원/교육 등 연구자 활동을 지속하도록 DBpia가 지원하고 있어요.
커뮤니티
연구자들이 자신의 연구와 전문성을 널리 알리고, 새로운 협력의 기회를 만들 수 있는 네트워킹 공간이에요.
논문 기본 정보
- 자료유형
- 학술대회자료
- 저자정보
- 발행연도
- 2013.9
- 수록면
- 275 - 278 (4page)
이용수
초록· 키워드
오류제보하기
In the areas for this study, there is a slope on the surface as a result of analyzing the forecast of movement for TPH of mountain areas. While the underground water level is irregular due to effects of difference in water level and rainfalls. It is formed in the silt sand layer and drift by hydraulic gradient prevails due to the permeable layer formed inside the geological stratum, resulting in movement of pollutants to the direction where farmland is located. As a result of analyzing the migration of pollutants for TPH in the detention reservoir, the geological stratum is formed with silt sand and clay. So that in 5 years later, the concentration of TPH pollution source shows the pollution index in the maximum concentration by diffusion-movement. Since TPH has relatively low volatility and solubility, the diffusion of pollutant is slow and moves vertically through soil permeable layer to be accumulated at the upper part of impermeable layer, serving as the long-term pollution source of underground water or infiltration water such as rain water.
목차
SYNOPSIS
1. 서론
2. 오염물질 이동이론
3. 오염물질 장래 이동 및 토양오염분포도
4. 결론
References
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UCI(KEPA) : I410-ECN-0101-2014-530-002858899