Introduction of the special issue on “Toward the prediction of shallow landslides induced by heavy rainfalls on tephra-covered slopes”

Goto, Shigeru; Kimura, Takashi

doi:10.3313/jls.56.211

Cited by 5 publications

(3 citation statements)

References 4 publications

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“…Shallow landslides appear frequently on the Aso volcanic mountains. The same sediment disasters have repeatedly occurred in June 1953, July 1990, with the last one occurring at July 12, 2012 (Goto and Kimura., 2019;Higaki et al, 2019;Kimura et al, 2019; when a cumulative rainfall of 508 mm triggered numerous landslides and severe sediment disasters throughout the month. The soil materials in the shallow landslides on the Aso volcanic mountains consist of tephra layers from volcanic activities.…”

Section: Introductionmentioning

confidence: 91%

Slip surface layer estimation of shallow landslides on Aso volcanic mountains in Japan based on tephra layer-soil properties

Ml¹,

Goto²

2020

Preprint

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Shallow landslides are known to appear frequently on the Aso volcanic mountains. The soil material on the Aso volcanic mountains consists of tephra layers obtained from volcanic activities. This study is aimed at determining the soil property factors that correlate with the slip surface of a shallow landslide on the volcanic mountain area. Tephra layers consist of kuroboku and scoria layers and the differences between these layers have been determined using soil property tests. This study determined that the plasticity index and the fine fraction content can be used as factors showing the slip surface indication in the Aso volcanic area.

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Section: Introductionmentioning

confidence: 91%

Slip surface layer estimation of shallow landslides on Aso volcanic mountains in Japan based on tephra layer-soil properties

Ml¹,

Goto²

2020

Preprint

Self Cite

View full text Add to dashboard Cite

show abstract

“…Shallow landslides occur frequently on the Aso volcanic mountains. The same sediment disasters have repeatedly occurred in June 1953, July 1990, with the last one occurring on July 12 th , 2012 (Goto and Kimura, 2019;Higaki et al, 2019;Kimura et al, 2019; when a cumulative rainfall of 508 mm triggered numerous landslides throughout the month. The soil materials in the shallow landslides on the Aso volcanic mountains consist of tephra layers formed by volcanic activities.…”

Section: Introductionmentioning

confidence: 94%

Slip layer estimation of shallow landslides on Aso volcanic mountains in Japan based on tephra layer-physical properties of soil

Istiyanti

Goto

Kimura

et al. 2020

Preprint

Self Cite

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Shallow landslides occur frequently on the Aso volcanic mountains. The soil material on the Aso volcanic mountains consists of tephra layers formed by volcanic activities. This study is aimed at determining the physical properties of soil that correlate with the slip surface of a shallow landslide on the volcanic mountain area. Tephra layers consist of kuroboku and scoria layers and the differences between these layers have been determined using the physical properties of soil methods. This study showed that the plasticity index and the fine fraction content can be used for estimating the slip layer in the Aso volcanic area.

show abstract

“…Shallow landslides occur frequently on the Aso volcanic mountains. Sediment disasters caused by the landslides repeatedly occurred in June 1953, July 1990, with the last one occurring on July 12th, 2012 (Goto and Kimura 2019;Higaki et al 2019;Kimura et al 2019;) when a cumulative rainfall of 508 mm triggered numerous landslides throughout the month. The soil materials in the shallow landslides on the Aso volcanic mountains consist of tephra layers formed by volcanic activities.…”

Section: Introductionmentioning

confidence: 99%

Sliding layer estimation of shallow landslides on Aso volcanic mountains in Japan based on tephra layer-physical properties of soil

Istiyanti

Goto

Kimura

et al. 2020

Geoenviron Disasters

Self Cite

View full text Add to dashboard Cite

Shallow landslides occur frequently on the Aso volcanic mountains. The soil materials on the Aso volcanic mountains consist of tephra layers formed by volcanic activities. This study is aimed to specify the physical properties of soil that correlate with the sliding layer of a shallow landslide on the volcanic mountain area. Tephra layers consist of kuroboku and scoria layers and the differences between these layers were specified using the physical properties of soil methods. Results showed that the plasticity index and the fine fraction content can be used for estimating the sliding layer in the Aso volcanic area.

show abstract

Introduction of the special issue on “Toward the prediction of shallow landslides induced by heavy rainfalls on tephra-covered slopes”

Cited by 5 publications

References 4 publications

Slip surface layer estimation of shallow landslides on Aso volcanic mountains in Japan based on tephra layer-soil properties

Slip surface layer estimation of shallow landslides on Aso volcanic mountains in Japan based on tephra layer-soil properties

Slip layer estimation of shallow landslides on Aso volcanic mountains in Japan based on tephra layer-physical properties of soil

Sliding layer estimation of shallow landslides on Aso volcanic mountains in Japan based on tephra layer-physical properties of soil

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