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Runoff Processes in Southeast Asia: Role of Soil, Regolith, and Rock Type
Abstract
Runoff processes govern the river hydrograph form, location of return-flow and
biogeochemical water quality of tropical forest watersheds. This study reviews the
literature on runoff processes from tropical rainforests and applies it to the situation in
tropical Southeast Asia. The impact of clay mineralogy on permeability and thence water
pathways within the soil, and the role of deep pathways with unconsolidated geological
materials (regolith) or permeable rock (solid geology) are emphasised, and a new
perceptual model, DELTAmodel, presented. Lastly, the implications of these findings for
runoff processes within the Mekong Basin are discussed.