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Degradation of Soil Properties due to Erosion on Sloping Land in Southern Jiangsu Province, China

机译:苏南坡地土壤侵蚀引起的土壤性质退化

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Soil erosion accelerates soil degradation. Some natural soils and cultivated soils on sloping land in southern Jiangsu Province, China were chosen to study soil degradation associated with erosion. Soil erosion intensity was investigated using the ~(137)Cs tracer method. Soil particle-size distribution, soil organic matter (OM), total nitrogen (TN) and total phosphorus (TP) were measured, and the effects of erosion on soil physical and chemical properties were analyzed statistically using SYSTAT8.0. Results indicated that erosion intensity of cultivated soils was greater than that of the natural soils, suggesting that cultivation increased soil loss. Erosion also led to an increase of coarser soil particle proportion, especially in natural soils. In addition, silt was the primary soil particle lost due to erosion. However, in cultivated fields, coarser soil particles over time were attributed not only to soil erosion but also to mechanical eluviation as a result of farming activities. Moreover, erosion caused a decrease in soil OM, TN and TP as well as thinning of the soil layer.
机译:水土流失会加速土壤退化。选择了中国江苏省南部坡地上的一些天然土壤和耕作土壤,以研究与侵蚀相关的土壤退化。使用〜(137)Cs示踪法研究了土壤侵蚀强度。测量土壤粒径分布,土壤有机质(OM),总氮(TN)和总磷(TP),并使用SYSTAT8.0软件统计分析侵蚀对土壤理化性质的影响。结果表明,耕作土壤的侵蚀强度大于天然土壤,表明耕作增加了土壤流失。侵蚀还导致土壤颗粒比重的增加,尤其是在天然土壤中。此外,淤泥是由于侵蚀而损失的主要土壤颗粒。然而,在耕地中,随着时间的推移,土壤颗粒变粗不仅归因于土壤侵蚀,还归因于耕作活动导致的机械淋洗。此外,侵蚀导致土壤OM,TN和TP减少以及土壤层变薄。

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