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Soil Related Factors Controlling Erosion And Landslides In Malaysia
Author(s) -
S. Paramananthan,
Nurfashareena Muhamad,
Joy Jacqueline Pereira
Publication year - 2021
Publication title -
bulletin of the geological society of malaysia
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.441
H-Index - 12
eISSN - 2637-109X
pISSN - 0126-6187
DOI - 10.7186/bgsm72202113
Subject(s) - landslide , weathering , erosion , soil water , terrain , geology , vegetation (pathology) , soil production function , environmental science , rainwater harvesting , hydrology (agriculture) , soil science , geomorphology , geotechnical engineering , pedogenesis , geography , medicine , ecology , cartography , pathology , biology
The high temperature and rainfall in Malaysia results in intensive tropical weathering and depending on the parent material, the resultant soil can have deep or shallow soil profiles. Thus, a variety of soils can form with different textures (clay content), structure and porosity. With the high rainfall, soils in steep terrain are subjected to surface erosion when exposed or landslides if the rainwater percolates into the soil profile. Key soil-related factors controlling soil erosion and landslides include local climate, parent material of soils and depth of the weathered profile. Slope and geomorphology, vegetation and land use as well as land management practices also influence erosion and landslides. Measures used to control soil erosion and stabilize slopes require improved understanding of soil weathering, erosion, landslide and their linkages in steep terrain.

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