2020
DOI: 10.1007/978-3-030-60319-9_7
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Pressure Head Dynamics on a Natural Slope in Eastern Iburi Struck by the 2018 Hokkaido Earthquake

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“…The LWD is thought to have moved up to approximately >200 m in the river channel accompanied by landslide debris in the upstream area, despite the landslides occurring without the direct involvement of rainfall. In this area, the volcanic ejecta, which is the soil layer above the sliding surface, is constantly close to saturation (Aoki et al, 2021). Soil tests conducted after the earthquake showed that the natural water content of En-a was close to the liquid limit (Osanai et al, 2019).…”
Section: Discussion Lwd Budget and Dynamics During The Earthquakementioning
confidence: 91%
“…The LWD is thought to have moved up to approximately >200 m in the river channel accompanied by landslide debris in the upstream area, despite the landslides occurring without the direct involvement of rainfall. In this area, the volcanic ejecta, which is the soil layer above the sliding surface, is constantly close to saturation (Aoki et al, 2021). Soil tests conducted after the earthquake showed that the natural water content of En-a was close to the liquid limit (Osanai et al, 2019).…”
Section: Discussion Lwd Budget and Dynamics During The Earthquakementioning
confidence: 91%