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Hillslope hydrology and stability /

A cutting-edge quantitative approach to understanding hydro-mechanical processes behind rainfall-induced landslides, for graduate students, researchers and professionals.

Detalles Bibliográficos
Clasificación:Libro Electrónico
Autores principales: Lu, Ning, 1960- (Autor), Godt, Jonathan W. (Autor)
Formato: Electrónico eBook
Idioma:Inglés
Publicado: Cambridge, UK ; New York : Cambridge University Press, 2013.
Temas:
Acceso en línea:Texto completo

MARC

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082 0 4 |a 551.43/6  |2 23 
049 |a UAMI 
100 1 |a Lu, Ning,  |d 1960-  |e author.  |1 https://id.oclc.org/worldcat/entity/E39PCjHYcWcfRGqdjxPd7pY4WP 
245 1 0 |a Hillslope hydrology and stability /  |c Ning Lu, Jonathan W. Godt. 
260 |a Cambridge, UK ;  |a New York :  |b Cambridge University Press,  |c 2013. 
300 |a 1 online resource (xxiv, 437 pages, 16 unnumbered pages of plates (chiefly color)) :  |b illustrations (some color), maps (some color) 
336 |a text  |b txt  |2 rdacontent 
337 |a computer  |b c  |2 rdamedia 
338 |a online resource  |b cr  |2 rdacarrier 
504 |a Includes bibliographical references (pages 406-429) and index. 
588 0 |a Print version record. 
505 0 |a Foreword; Preface; Symbols; PART I Introduction and state of the art; 1 Introduction; 1.1 Landslide overview; 1.2 Landslide classification; 1.2.1 Landslide velocity; 1.2.2 Illustration of landslide classification; 1.3 Landslide occurrence; 1.3.1 Landslide triggering mechanisms; 1.3.2 Frequency and magnitude of landslide events; 1.4 Socio-economic impacts of landslides; 1.4.1 Types of costs; 1.4.2 Historical examples of widespread landslide events in North America; 1.4.3 Direct economic loss in the San Francisco Bay region in 1997-8; 1.5 Rainfall-induced landslides. 
505 8 |a 1.5.1 Evidence of shallow landslide occurrence in the unsaturated zone1.5.2 Role of precipitation characteristics in triggering shallow landslides; 1.5.3 Role of infiltration and unsaturated flow within hillslopes; 1.6 Scope and organization of the book; 1.6.1 Why does rainfall cause landslides?; 1.6.2 Organization of the book; 1.7 Problems; 2 Hillslope geomorphology; 2.1 Hillslope hydrologic cycle; 2.1.1 Global patterns of precipitation and evaporation; 2.1.2 Orographic precipitation enhancement; 2.1.3 Atmospheric rivers; 2.1.4 Monsoons; 2.1.5 Tropical cyclones; 2.1.6 El Niño and La Niña. 
505 8 |a 2.1.7 Trends in extreme precipitation2.2 Topography; 2.2.1 General topographic features; 2.2.2 Digital landscapes; 2.2.3 DEM methods for landslide analysis; 2.3 Soil classification; 2.3.1 Soil stratigraphy; 2.3.2 Commonly used classification systems; 2.4 Hillslope hydrology and stream flow generation; 2.4.1 Runoff and infiltration; 2.4.2 Subsurface flow processes and runoff generation; 2.4.3 Subsurface stormflow; 2.4.4 Subsurface stormflow and landslide initiation; 2.5 Mechanical processes in hillslopes; 2.5.1 Stress variation mechanisms; Seismic shaking; Weight of water. 
505 8 |a Saturated pore-water diffusionUnsaturated soil suction diffusion; 2.5.2 Strength reduction mechanisms; Weathering; Mineral dissolution or precipitation; Slickenside; Soil creep; Root growth and decay; 2.5.3 Combined change in stress and strength; Erosion; Tensile cracking; Shrink-swell; 2.6 Problems; PART II Hillslope hydrology; 3 Steady infiltration; 3.1 Water movement mechanisms; 3.1.1 Introduction; 3.1.2 Gravitational potential; 3.1.3 Pressure potential; 3.1.4 Osmotic potential; 3.1.5 Water vapor potential; 3.1.6 Chemical potential equilibrium principle in multi-phase media. 
505 8 |a 3.1.7 Pressure profiles under hydrostatic conditions3.2 Darcy's law; 3.2.1 Darcy's experiments; 3.2.2 Darcy's law in three-dimensional space; 3.2.3 Hydraulic properties; 3.3 Capillary rise; 3.3.1 Height of capillary rise in soils; 3.3.2 Rate of capillary rise in soils; 3.4 Vapor flow; 3.5 Vertical flow; 3.5.1 One-layer system; Case i: sandy soil layer; Case ii: silty soil layer; Case iii: clayey soil layer; 3.5.2 Two-layer system; Case iv: sand-silt system; Case v: sand-clay system; Case vi: silt-clay system; Case vii: silt-sand system; Case viii: clay-sand system; Case ix: clay-silt system. 
520 |a A cutting-edge quantitative approach to understanding hydro-mechanical processes behind rainfall-induced landslides, for graduate students, researchers and professionals. 
590 |a ProQuest Ebook Central  |b Ebook Central Academic Complete 
650 0 |a Mountain hydrology. 
650 0 |a Slopes (Physical geography) 
650 0 |a Soil erosion. 
650 0 |a Soil mechanics. 
650 0 |a Landslides. 
650 0 |a Groundwater flow. 
650 6 |a Hydrologie de montagne. 
650 6 |a Pentes et versants (Géographie physique) 
650 6 |a Sols  |x Érosion. 
650 6 |a Mécanique des sols. 
650 6 |a Eau souterraine  |x Écoulement. 
650 7 |a soil mechanics.  |2 aat 
650 7 |a SCIENCE  |x Earth Sciences  |x Geography.  |2 bisacsh 
650 7 |a SCIENCE  |x Earth Sciences  |x Geology.  |2 bisacsh 
650 7 |a Groundwater flow  |2 fast 
650 7 |a Landslides  |2 fast 
650 7 |a Mountain hydrology  |2 fast 
650 7 |a Slopes (Physical geography)  |2 fast 
650 7 |a Soil erosion  |2 fast 
650 7 |a Soil mechanics  |2 fast 
650 7 |a Hang  |2 gnd 
650 7 |a Erdrutsch  |2 gnd 
650 7 |a Hydrologie  |2 gnd 
700 1 |a Godt, Jonathan W.,  |e author. 
758 |i has work:  |a Hillslope hydrology and stability (Text)  |1 https://id.oclc.org/worldcat/entity/E39PCGyGFHjT3RgbqD97f4yQmb  |4 https://id.oclc.org/worldcat/ontology/hasWork 
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