Hillslope Hydrology And Stability

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

Landslides are caused by a failure of the mechanical balance within hillslopes. This balance is governed by two coupled physical processes: hydrological or subsurface flow and stress. The stabilizing strength of hillslope materials depends on effective stress, which is diminished by rainfall. This book presents a cutting-edge quantitative approach to understanding hydro-mechanical processes across variably saturated hillslope environments and to the study and prediction of rainfall-induced landslides. Topics covered include historic synthesis of hillslope geomorphology and hydrology, total and effective stress distributions, critical reviews of shear strength of hillslope materials and different bases for stability analysis. Exercises and homework problems are provided for students to engage with the theory in practice. This is an invaluable resource for graduate students and researchers in hydrology, geomorphology, engineering geology, geotechnical engineering and geomechanics and for professionals in the fields of civil and environmental engineering and natural hazard analysis.

A complete guide to the behavior of water on graded land Hillslope Hydrology provides a comprehensive introduction to the behavior of water on a slope. Describing the fates of precipitation, the mechanics of runoff, and the calculations involved in assessment, this book clarifies the complex interplay of soils, sediment, subsurface flow, overland flow, saturation, erosion, and more. An ideal resource for graduate students of Earth science, environmental science, civil engineering, architecture, landscape management, and related fields, this informative guide provides the essential information needed to work effectively with graded land or predict outcomes of precipitation.

Hydrology is the branch of science that is concerned with the movement and management of water on the surface of Earth, beneath the surface of Earth, as well as in the atmosphere. Hillslopes make up the flanks of valleys and the margins of eroding uplands. Hillslope hydrology is a scientific study to understand the hillslope runoff processes and the contribution of groundwater to storm runoff. Such hydrologic organization brings in distinct characteristics in soil and vegetation of hilltops, valleys and between sunny and shady slopes. The topographic gradients present on the hillslopes drive water, sediments and biogeochemical fluxes down the hillslopes. Hydrologic processes are traditionally studied at hillslope-to-catchment scales (tens of meters to kilometers). An important area of study in this field is the interplay of sediments, subsurface flow, soil erosion and overland flow. This book provides significant information of this discipline to help develop a good understanding of hillslope hydrology and its related fields. From theories to research to practical applications, case studies related to all contemporary topics of relevance to this field have been included herein. This book will help new researchers by foregrounding their knowledge in this branch.

Hillslope and Watershed Hydrology.

Published by the American Geophysical Union as part of the Water Resources Monograph Series, Volume 11. This monograph compiles research findings on soil mass movement into a format usable by practitioners and students. Applications are stressed in the areas of extensive and management practices rather than engineering earthworks. Examples are included to illustrate various prediction, avoidance, and control measures used in managing unstable terrain. We use the term soil (i.e., soil mass movement) to mean the mantle of unconsolidated or poorly consolidated material of either residual or transported origin, that overlies bedrock and forms the surface of the land. This usage is consistent with the conventional civil engineering use of the word and is synonymous with the geological term regolith and with soil mantle.

This revised and updated edition continues to provide a comprehensive introduction to the subject, exploring the world’s landforms from a broad systems perspective. It covers the basics of Earth surface forms and processes, while reflecting on the latest developments in the field. Fundamentals of Geomorphology begins with a consideration of the nature of geomorphology, including its relation to society, process and form, history, and geomorphic systems, and moves on to discuss: • Structure: structural landforms associated with plate tectonics and those associated with volcanoes, and folds, faults, and joints. • Process and form: landforms resulting from, or influenced by, the exogenic agencies of weathering, running water, flowing ice and meltwater, ground ice and frost, the wind, and the sea; landforms developed on limestone; extraterrestrial landforms; and landscape evolution, a discussion of ancient landforms. Fundamentals of Geomorphology provides a stimulating and innovative perspective on the key topics and debates within the field of geomorphology. Written in an accessible and lively manner, it includes guides to further reading, chapter summaries, and an extensive glossary of key terms. The book is also illustrated throughout with over 200 informative diagrams and attractive photographs, all in colour. It is supported by online resources for students and instructors.