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• W1484590588 abstract "Recent research has advanced the application of physically-based soil hydrology-slope stability models to elucidate Holocene slope instability processes. Since investigations of past mass movement present particular problems for model parameterisation and validation, contemporary slope failures need to be utilised. One field site, Glen Feshie, has provided model parameterisation data which has enabled investigation of temporal changes in the probability of slope instability resulting from progressive soil development. A second field site, Glen Livet, has allowed some model validation and closer investigation of the hydrological processes which govern slope instability. A third field area on the Mendip Plateau has provided more evidence that slope failure in temperature regions might well be governed by negative rather than by positive pore water pressures. From these investigations, greater emphasis needs to be placed on unsaturated zone hydrology and slope stability. A major issue for future model development involves the inclusion of hydrological and geotechnical processes associated with developing vegetation. Since this largely involves the unsaturated zone of the soil profile, it is suggested that future model development and application needs to concentrate more on detailed and accurate process representation in 1-dimension to overcome some of the inadequacies which currently persist in interpretations of Holocene slope stability. Hence important issues can be highlighted which need to be retained in new models which can handle larger areas and include long time intervals, suitable for elucidating Holocene slope stability." @default.
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• W1484590588 date "2005-10-21" @default.
• W1484590588 modified "2023-09-24" @default.
• W1484590588 title "Exploring the potential for physically-based models and contemporary slope processes to examine the causes of holocene mass movement" @default.
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• W1484590588 doi "https://doi.org/10.1007/bfb0009727" @default.
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