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내삼리 땅밀림형 산사태의 발생특성에 관한 분석(2) -발생원인을 중심으로-
박재현 ( Bak Jae Hyeon ),최경 ( Choe Gyeong ),마호섭 ( Ma Ho Seob ),이종학 ( Lee Jong Hag ),우보명 ( U Bo Myeong ) 한국산림과학회 2003 한국산림과학회지 Vol.92 No.6
This study was carried out to analyze rainfall events, geo-topographical characteristics at the landsliding area of about 3. lha in Nasamri, Juchonmyeon, Gimhaesi, Gyeongsangnam-do. There were many cracks and soil burying. Most rainfall was infiltrated from the surface layer to the subsurface layer. We found that subsurface water in the area was sprang out to the surface areas in the bottom of landsliding area. Heavily continued rainfall above 350㎜ which led to rapid shift of soil mass was one of the dominant factors in this landslide. We conclude that the occurrence of landslide was closely related to geo-topographical characteristics, hydrological conditions and rainfall mass events.