Relation between collapse position and water path position in slopes
Yasuyuki Tada, Masaharu Fujita, Daizo Tsutsumi, Kan Koyama,Takayuki Kawai,
Takenobu Okumura and Naomasa Honda
Abstract
In Japan, a lot of hillslope collapses triggered by heavy rainstorm almost every
year. In spite of continuous effort to elucidate the mechanism of landslide occurrence,
sufficient answer explaining why the particular position of the hillslope collapses
have not been obtained. It has been pointed out that there is a close relationship
between the landslide and underground water paths according to observations around
the collapse site; i.e. outlet of soil pipes on the scarp, clouding, stopping
or spouting of spring water just before or after the landslides. However, detail
of these relationships has not been clearly understood yet, partly due to lack
of an effective method to detect the water path within the slope. Recently, a
new method to detect the underground water path positions measuring sound of ground
water flow by a sound sensor "hydrostat" was developed.