A fluidized landslide on a natural slope by artificial rainfall

被引:159
作者
Ochiai, Hirotaka [2 ]
Okada, Yasuhiko [1 ]
Furuya, Gen [3 ]
Okura, Yoichi [2 ]
Matsui, Takuro [2 ]
Sammori, Toshiaki [2 ]
Terajima, Tomomi [4 ]
Sassa, Kyoji
机构
[1] Forestry & Forest Prod Res Inst, Tsukuba, Ibaraki 3058687, Japan
[2] Natl Res Inst Earth Sci & Disaster Prevent, Tsukuba, Ibaraki 3050006, Japan
[3] Kyoto Univ, Disaster Prevent Res Inst, Res Ctr Landslide, ICL, Kyoto 6110011, Japan
[4] Chiba Univ, Chiba 2638522, Japan
关键词
Natural slope; Sliding surface formation; Stereo photogrammetry; Soil surface movement; Landslide-fluidization;
D O I
10.1007/s10346-004-0030-4
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
An experiment to induce a fluidized landslide by artificial rainfall was conducted on a natural slope at Mt. Kaba-san in the village of Yamato, Ibaraki Prefecture, Japan. The experimental slope was 30 m long, 5 m wide, and the average slope gradient was 33 degrees. A landslide initiated 24,627.5 s (410 m/27.5 s) after the start of sprinkling at a rainfall intensity of 78 mm/h. The landslide mass was 14 m long and 1.2 m deep (at maximum). It first slid, then fluidized, and changed into a debris flow. The travel distance was up to 50 m in 17s. The apparent friction angle of the fluidized landslide was 16.7 degrees. Formation of the sliding surface was detected by soil-strain probes. Motion of the surface of the failed landslide mass was determined by stereo photogrammetry.
引用
收藏
页码:211 / 219
页数:9
相关论文
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