Access the full text.
Sign up today, get DeepDyve free for 14 days.
M. Carson (2010)
Models of Hillslope Development under Mass FailureGeographical Analysis, 1
G. Dury (1972)
Hillslope form and Process. M.A. Carson and M.J. Kirkby, 1972. Cambridge University Press, London, vii + 475 pp., £ 6.60
(2002)
Cause of Fre quent Occurrence of Gravel Slope Landslide and Experiment Simulation
(2003)
Relationship between Occurrence of Debris Flows and Antecedent Precipitation . . . . Taking Jiangjia Gully as an Example
R. Iverson, M. Reid, R. LaHusen (1997)
Debris-flow mobilization from landslidesAnnual Review of Earth and Planetary Sciences, 25
(1990)
Lianq-quan, eta& Debris Flows Observation and Research at J iangjia Ravine o f Yun nan Province
(1997)
Landslides in Hong K o n gPrevention
S. Ellen, R. Fleming (1987)
Mobilization of debris flows from soil slips, San Francisco Bay region, CaliforniaReviews in Engineering Geology, 7
A. Osman, C. Thorne (1988)
RIVERBANK STABILITY ANALYSIS. I: THEORYJournal of Hydraulic Engineering, 114
B. Low, W. Tang (1997)
EFFICIENT RELIABILITY EVALUATION USING SPREADSHEETJournal of Engineering Mechanics-asce, 123
Wang Yuyi, Li Changzhi, Zhou Renyuan (2001)
A study on relationship between erosion of debris flows and critical rain quantity
(1980)
Analysis of the Condition for the Formation of the Debris Flows in jiangjia Ravine, Dong Chuan, Yunnan Province
(1999)
Mechanism for Rainstorm-Induced Soil Slide-Debris Flows in Area with Volcanic Rock Derived Soils
P. Cui, Xiao-qing Chen, Yuyi Waqng, Kai-heng Hu, Yong Li (2005)
Jiangjia Ravine debris flows in south-western China
M. Carson, M. Kirkby (1972)
Hillslope Form and Process
(1980)
Environment and Debris How
M. Crozier (1986)
Landslides: Causes, Consequences and Environment
T. Asch, J. Buma, L. Beek (1999)
A view on some hydrological triggering systems in landslidesGeomorphology, 30
G. Crosta (1998)
Regionalization of rainfall thresholds: an aid to landslide hazard evaluationEnvironmental Geology, 35
To reveal the gravitational erosion process in the headstream area of Jiangjia Ravine, continuous observation was conduced duing the rainy season. The observation and research show that the change of water content of the bank slope lags the precipitation process, the infiltration water concentrates mainly in the shallow layer of the bank slope, also the bank slope was unsaturated, the floods and debris flows in the gully down cut the gully bed, and scour the foot of the bank slope. These results in many collapses, which is the main type of gravitational erosion process, and it provides large amounts of loose solid materials for the eruption of debris flows.
Wuhan University Journal of Natural Sciences – Springer Journals
Published: Jul 1, 2005
Read and print from thousands of top scholarly journals.
Already have an account? Log in
Bookmark this article. You can see your Bookmarks on your DeepDyve Library.
To save an article, log in first, or sign up for a DeepDyve account if you don’t already have one.
Copy and paste the desired citation format or use the link below to download a file formatted for EndNote
Access the full text.
Sign up today, get DeepDyve free for 14 days.
All DeepDyve websites use cookies to improve your online experience. They were placed on your computer when you launched this website. You can change your cookie settings through your browser.