Abstract
本報文では, 口坂本地すべりにおける地すべり動態観測データをもとに, 本地すべりの間隙水圧変動機構について考察した。その結果, 下部地すべりブロックにおける間隙水圧の変動は, 降雨が地すべり地塊等に鉛直浸透した後に, 地下水となり水みちや帯水層を通って流動する被圧地下水によると考える。
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