Gravity, Magnetic and VLF Explorations in the Seokdae Landfill, Pusan

부산시 석대 매립지에서의 중력, 자력, VLF탐사

  • Kwon, Byung-Doo (Department of Earth Sciences, Seoul National University) ;
  • Seo, Jung-Hee (Department of Mineral and Petroleum Engineering, Seoul National University) ;
  • Oh, Seok-Hoon (Department of Earth Sciences, Seoul National University)
  • 권병두 (서울대학교 지구과학교육과) ;
  • 서정희 (서울대학교 자원공학과) ;
  • 오석훈 (서울대학교 지구과학교육과)
  • Received : 1997.12.16
  • Published : 1998.02.28

Abstract

Gravity, magnetic and VLF surveys were carried out to investigate the dimension, nature and stability of the waste materials filled in the Seokdae landfill, Pusan. The Seokdae landfill, which is located in a former valley, was used as a dump for mainly domestic-type waste materials for 6 years from 1987. The landfill site is classfied into A, B, C and D areas according to the sequence of dumping period. The Bouguer gravity anomaly map shows maximum variation of 3.1 mgals on the landfill and its general appearance has close relation with the thickness of waste filled. The local variation of anomaly, however, reflect the degree of compactness of waste materials which may be affected by the nature of waste and dumping time. In the case of area A, where dumping process was terminated at the very last stage, most part show negative anomaly compared to other areas. We think that the composition of the waste materials in the area A is high in leftover food and paper trash and they are still in uncompacted condition. In area B, the general trend of variation of gravity anomaly is appeared to be high anomaly in northern part and decrease to the southern part. This is well matched with the prelandfill topography of the landfill site. The southern part of area B is located in the center of valley and its present surface is comparatively rugged, which may be due to the differential settlement of deep burried waste. The thickness of waste in area C is relatively thin, but the gravity anomaly appears to be low. Considering the present condition of surface, it can be inferred that low density wastes such as leftover food were mainly filled in this area. Area D, as in the case of area B, shows gravity anomaly that has close relation with the prelandfill topography. Magnetic data show the variation of total field intensity varies in the range of 46600~51000 nT, and reach maximum anomaly of 4400 nT. The overall pattern of magnetic anomaly well reflects the distribution of magnetic materials in the landfill. The result of VLF survey reveals several low resistivity zones, which may serve as underground passages for contaminant flow, in the area C located near the small Village.

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Acknowledgement

Supported by : 기초과학연구소