임기광산 폐석적치장의 수리침투특성 분석

  • 지상우 (한국지질자원연구원 지질환경재해연구부) ;
  • 정영욱 (한국지질자원연구원 지질환경재해연구부) ;
  • 임길재 (한국지질자원연구원 지질환경재해연구부)
  • Published : 2004.09.01

Abstract

This study was carried out to plan the prevention of the generation and discharge of acid mine drainage (AMD). Hydraulic characteristics were tested with the disk tension infiltrometer around the waste rock dump of the Imgi abandoned pyrophyllite mine in Busan, Korea. Because the waste rock dump of the Imgi mine have very low infiltration rate, most of rain was expected flowing into adjoined stream through the slope or plane as surface flow rather then throughflow or ground water. But slopes of the waste rock dump have many 'V' type erosion gullies and consist multi-layers. These gullies and multi-layers have coarse clastic particle layer which have very large hydraulic conductivity. So through these coarse clastic particle layers a large part of rain flow into ground. And also these layers could be played a function of aeration path, which induced oxidation of sulfide minerals and generation of AMD continuously.tinuously.

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