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[1]WANG Xiao-yan,LI Zhong-wu,XIU Cheng-xian.Study on Soil Erosion and Its Effect on Different Landuse Types in the Red Soil Hilly Area of South China Based on 137Cs Tracing[J].Research of Soil and Water Conservation,2013,20(02):1-4.

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Study on Soil Erosion and Its Effect on Different Landuse Types in the Red Soil Hilly Area of South China Based on ¹³⁷Cs Tracing

Research of Soil and Water Conservation[ISSN 1005-3409/CN 61-1272/P] Volume: 20 Number of periods: 2013 02 Page number: 1-4 Column: Public date: 2013-04-28

Title:: Study on Soil Erosion and Its Effect on Different Landuse Types in the Red Soil Hilly Area of South China Based on ¹³⁷Cs Tracing

Author(s):: WANG Xiao-yan¹, LI Zhong-wu², XIU Cheng-xian³; 1. School of Civil Engineering Architecture, Changsha University of Science and Technology, Changsha 410114, China;
2. College of Environmental Science and Engineering, Hu’nan University, Changsha 410082, China;
3. Yunfeng Middle School of Laizhou, Shandong Province, Laizhou, Shandong 261400, China

Keywords:: ¹³⁷Cs tracing; red soil hilly area; land utilization; erosion effect

CLC:: S157

DOI:: -

Abstract:: Because of serious soil erosion and degradation, the red soil hilly region has become a fragile ecological area. Based on ¹³⁷Cs tracing technique and soil erosion estimation models, the soil erosion rate and corresponding effect were studied on the representative land utilization of Shaoyang, Hunan province. The result showed that the reference inventory of ¹³⁷Cs in the study area was (1 920±125.6) Bq/m². ¹³⁷Cs concentrations’ distribution had obvious differentiation on the slope with different land use types and on the different parts of slope. The average soil erosion rate was also different, which decreased in the order of barren hill, local pine forest, soil and water conservation forest, citrus orchard, nursery garden changed from citrus orchard, nursery garden. The soil organic matter and other soil physicochemical properties also showed the same variation characteristics as soil erosion rate. On the different parts of slope, the soil erosion rate was relatively smaller on the top while relatively larger rate occurred on the middle and bottom of slope.

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