马来西亚土壤相关因素控制侵蚀和滑坡

Q3 Earth and Planetary Sciences
Paramananthan S, Nurfashareena Muhamad, J. Pereira
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引用次数: 3

摘要

马来西亚的高温和降雨导致强烈的热带风化,根据母质的不同,所形成的土壤可以有深或浅的土壤剖面。因此,可以形成具有不同质地(粘土含量)、结构和孔隙度的各种土壤。在高降雨条件下,地形陡峭的土壤在暴露时容易发生地表侵蚀,雨水渗入土壤剖面后容易发生滑坡。控制土壤侵蚀和滑坡的关键土壤相关因素包括当地气候、土壤母质和风化剖面深度。坡度和地貌、植被和土地利用以及土地管理做法也会影响侵蚀和滑坡。用于控制土壤侵蚀和稳定斜坡的措施需要更好地了解陡峭地形上的土壤风化、侵蚀、滑坡及其联系。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Soil Related Factors Controlling Erosion And Landslides In Malaysia
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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来源期刊
Bulletin of the Geological Society of Malaysia
Bulletin of the Geological Society of Malaysia Earth and Planetary Sciences-Earth and Planetary Sciences (miscellaneous)
CiteScore
1.60
自引率
0.00%
发文量
15
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