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Soil Crevice Formation and Erosion in Yuanmou Dry-Hot Valley, Yunnan Province, China

Soil Crevice Formation and Erosion in Yuanmou Dry-Hot Valley, Yunnan Province, China
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摘要 The basic characteristics, X-ray analysis and micromorphology of soil developed from the parent rubified soil is probed. Results show that there are similarities among different types of the rubified soils. The soil clay (D〈0.002 mm) contents (Co) are relatively higher between 29.16% and 80.03%. In addition, organic matter contents are lower between 2.2-6.6 g/kg. The clay minerals in the rubified soils have a high content of 2:l type swelling minerals, e.g., smectite and vermiculite, which are the basic causes of formation of soil cracks and crevices. Soil micromorphology characteristics show that microcosmic crevices universally distributed within the tight and compact soil microstructure are the microcosmic characteristics of crevices formation. The soil cracks and crevices change the erosion process. Obviously, well developed soil crevice carries a significant connection with strong soil erosion in Yuanmou, Yunnan province, China. The term "soil crevice erosion" was coincided with the viewpoint put forward that soil crevice erosion plays a dominant role in regional and violent soil erosion in this area. The basic characteristics, X-ray analysis and micromorphology of soil developed from the parent rubified soil is probed. Results show that there are similarities among different types of the rubified soils. The soil clay (D〈0.002 mm) contents (Co) are relatively higher between 29.16% and 80.03%. In addition, organic matter contents are lower between 2.2-6.6 g/kg. The clay minerals in the rubified soils have a high content of 2:l type swelling minerals, e.g., smectite and vermiculite, which are the basic causes of formation of soil cracks and crevices. Soil micromorphology characteristics show that microcosmic crevices universally distributed within the tight and compact soil microstructure are the microcosmic characteristics of crevices formation. The soil cracks and crevices change the erosion process. Obviously, well developed soil crevice carries a significant connection with strong soil erosion in Yuanmou, Yunnan province, China. The term "soil crevice erosion" was coincided with the viewpoint put forward that soil crevice erosion plays a dominant role in regional and violent soil erosion in this area.
出处 《Wuhan University Journal of Natural Sciences》 CAS 2009年第1期87-91,共5页 武汉大学学报(自然科学英文版)
基金 Supported by the Knowledge Innovation Program of the Chinese Academy of Sciences(KZCX2-YW-409) the National Key Tech-nology R&D Program of China ( 2006BAC01A11)
关键词 soil crevice erosion soil characteristics soil micromorphology Yuanmou dry-hot valley soil crevice erosion soil characteristics soil micromorphology Yuanmou dry-hot valley
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