数字农科院2.0

Residue cover and rainfall intensity effects on runoff soil organic carbon losses

文献类型： 外文期刊

作者： Jin, K.;Wu, H. J.;Cai, D. X.;Jin, J. Y.;Jin, K.;Wu, H. J.;Cai, D. X.;Jin, J. Y.;Jin, K.;Cornelis, W. M.;Gabriels, D.;Baert, M.;Schiettecatte, W.;De Neve, S.;Hartmann, R.;Hofman, G.

作者机构：

关键词： soil erosion;rainfall intensity;residue cover;runoff soil organic carbon loss

期刊名称： CATENA

ISSN：

年卷期：

页码：

收录情况： SCI

摘要： Soil cover and rainfall intensity (RI) are recognized to have severe impacts on soil erosion and an interaction exists between them. This study investigates the effect of rainfall intensity (RI) and soil surface cover on losses of sediment and the selective enrichment of soil organic carbon (SOC) in the sediment by surface runoff. A field rainfall simulator was used in the laboratory to produce 90 min rainfall events of three rainfall intensities (65, 85 and 105 mm h(-1)) and four cover percentages (0%, 25%, 50% and 75%) on soil material at 9% slope. A strong negative exponential relation was observed between cover percentage and RI on sediment loss under 85 and 105 mm h(-1) of rain, while under RI of 65 mm h(-1), the highest sediment loss was observed under 25% cover. Overall, higher RI and lower cover produced higher sediment and consequently higher nutrient loss, but resulted in a lower SOC enrichment ratio (ERSOC) in the sediment. The amount of runoff sediment rather than the ERSOC in the sediment was the determinant factor for the amount of nutrients lost. The values of ERSOC were high and positively correlated with the ER values of particles smaller than 20 mu m (p<0.01). Although the sediment contained substantially more fine fractions (fine silt and clay, <20 mu m), the original soil and runoff sediment were still of the same texture class, i.e. silt clay loam.

分类号： S15

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