Sensitivity of the initiation of debris flow to initial soil moisture

The initiation of debris flows is commonly attributed either to fluidization as a result of rainfall-induced landslides or to gully erosion induced by concentrated runoffs. A series of flume tests have been performed to show how the initial soil moisture influences the initiation of debris flows. At...

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Bibliographic Details
Published in:Landslides Vol. 12; no. 6; pp. 1139 - 1145
Main Authors: Hu, W., Xu, Q., Wang, G. H., van Asch, T. W. J., Hicher, P.-Y.
Format: Journal Article
Language:English
Published: Berlin/Heidelberg Springer Berlin Heidelberg 01.12.2015
Springer Nature B.V
Springer Verlag
Subjects:
Agriculture
Civil Engineering
Debris flow
Detritus
Earth and Environmental Science
Earth Sciences
Engineering Sciences
Fluidization
Geography
Geology
Gullies
Gully erosion
Landslides
Liquefaction
Natural Hazards
Original Paper
Pore pressure
Risques
Soil erosion
Soil moisture
Soil strength
Surface runoff
Water
Debris flow
Initial moisture
Runoff
Internal erosion
ISSN:1612-510X, 1612-5118
Online Access:Get full text
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Summary:The initiation of debris flows is commonly attributed either to fluidization as a result of rainfall-induced landslides or to gully erosion induced by concentrated runoffs. A series of flume tests have been performed to show how the initial soil moisture influences the initiation of debris flows. At the start of each experiment, surface runoff was generated over loose granular deposits, triggering debris flows. These experimental debris flows enacted different scenarios according to the small variations among the initial soil moistures. In the loose granular deposits with initial soil moistures ranging from 1 to 5 %, most runoff water could infiltrate and trigger a landslide, which accelerated within 1 s to speed over 1 ms −1 and then transformed into a debris flow. In the same soil deposits with initial moistures >5 or <1 %, the debris flow was initiated by slow gully erosion with episodic events of damming and breaching due to small-scale landslides occurring on the side-slopes of the erosion valley. The slope failures were not triggered by positive pore pressure but by a decrease in suction due to the wetting of the soil. This suction decrease in initially unsaturated slopes explains why the transformation of these slope failures into debris flows are due not only to an increase of pore pressure leading to soil liquefaction, which is one of the expected triggering mechanisms, but also to a loss of the cohesive strength of the soil.
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ISSN:1612-510X
1612-5118
DOI:10.1007/s10346-014-0529-2