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Response of a residual soil slope to rainfall

Author
RAHARDJO, H1 ; LEE, T. T1 ; LEONG, E. C1 ; REZAUR, R. B1
[1] NTU-PWD Geotechnical Research Centre, School of Civil and Environmental Engineering, Nanyang Technological University, Blk N1, Nanyang Avenue, Singapore 639798, Singapore
Source

Canadian geotechnical journal. = Revue canadienne de géotechnique. 2005, Vol 42, Num 2, pp 340-351, 12 p ; ref : 19 ref

CODEN
CGJOAH
ISSN
0008-3674
Scientific domain
Civil engineering; Geology; Geophysics
Publisher
National Research Council of Canada, Ottawa, ON
Publication country
Canada
Document type
Article
Language
English
Author keyword
infiltration pression interstitielle ruptures de talus induites par la pluie sol résiduel teneur en eau
Keyword (fr)
Corrélation Courant Direction Eau souterraine Glissement terrain Infiltration Migration Nappe Pluie Pression Ruissellement Rupture Réseau Sol Succion Versant Crète Singapour Asie Europe Europe Sud Extrême Orient Grèce
Keyword (en)
correlation currents direction ground water landslides infiltration migration nappes rainfall pressure runoff rupture networks soils suction slopes Crete Singapore Asia Europe Southern Europe Far East Greece
Keyword (es)
Correlación Dirección Agua subterránea Desmoronamiento tierra Infiltración Migración Manto Lluvia Presión Brillo Ruptura Suelo Succión Declive Cresta Singapur Asia Europa Europa Sur Extremo Oriente Grecia
Classification
Pascal
001 Exact sciences and technology / 001E Earth, ocean, space / 001E01 Earth sciences / 001E01O Engineering and environment geology. Geothermics / 001E01O01 Engineering geology

Discipline
Earth sciences
Origin
Inist-CNRS
Database
PASCAL
INIST identifier
16947514

Sauf mention contraire ci-dessus, le contenu de cette notice bibliographique peut être utilisé dans le cadre d’une licence CC BY 4.0 Inist-CNRS / Unless otherwise stated above, the content of this bibliographic record may be used under a CC BY 4.0 licence by Inist-CNRS / A menos que se haya señalado antes, el contenido de este registro bibliográfico puede ser utilizado al amparo de una licencia CC BY 4.0 Inist-CNRS

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