Characteristics of landslides in unwelded pyroclastic flow deposits, southern Kyushu, Japan

Home

Sustainability Research Centre

Research Publications

Characteristics of landslides in unwelded pyroclastic flow deposits, southern Kyushu, Japan

Add to Quick Collection

Description	Size	Format
PDF - Published Version (Open Access)	2 MB	Adobe Acrobat PDF	Download

Title: Characteristics of landslides in unwelded pyroclastic flow deposits, southern Kyushu, Japan
Author/Creator: Yamao, M | Sidle, Roy C | Gomi, T | Imaizumi, F
Description: We investigated 184 landslides that occurred in unwelded pyroclastic flow deposits (Shirasu) on southern Kyushu Island, Japan, that included detailed data on the rainfall characteristics and the timing of slope failure. Localized rainfall intensity, antecedent rainfall, and topography affected the hydrologic processes that triggered landslides. Antecedent rainfall (adjusted for evapotranspiration losses) for large (> 200 mm) storms that triggered landslides was much lower than for smaller (≤ 200 mm) storms. Mean storm intensity and antecedent 7 day rainfall (API7) thresholds of > 5 mm h-1 and ≤ 30 mm (or API30 ≤ 60 mm), respectively, were useful to identify landslides triggered by rapid pore water pressure response, especially for shorter (< 20 h) duration events. During smaller storms with lower intensity, landslides are likely affected by a combined increase in soil weight and loss of suction when API30 ≥ 150 mm; simulations indicated that these weight and suction changes due to rainfall accumulation decreased factor of safety in steep Shirasu slopes, but did not necessarily trigger the landslides. All but two of the 21 landslides that plotted below a general rainfall intensity-duration threshold for landslide initiation had API30 values > 235 mm, indicating that they were highly influenced by the combined effects of the accumulated weight of rainfall and loss of suction. Our findings show that both event rainfall characteristics and antecedent conditions affect the hydrogeomorphic processes that trigger different types of landslides in Shirasu. This knowledge and the thresholds we have identified are useful for predicting the occurrence of different types of landslides in Shirasu deposits and improving sediment disaster prevention practices, including real-time warning systems.
Relation: Natural Hazards and Earth System Sciences / Vol. 3, No. 10, pp.6351-6378
Relation: http://dx.doi.org/10.5194/nhessd-3-6351-2015
Year: 2015
Publisher: Copernicus GmbH
Subject: FoR 0406 (Physical Geography and Environmental Geoscience) | FoR 0403 (Geology) | FoR 0911 (Maritime Engineering) | landslides

Collection(s): Research Publications
Resource Type: Discussion Paper
Identifier: ISSN: 1561-8633
Reviewed

631 Visitors

17 Downloads

USC Research Bank - University of the Sunshine Coast, Queensland, Australia