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Estimation of total erosion in cultivated Black soils in northeast China from vertical profiles of soil organic carbon

机译:从土壤有机碳垂直剖面估算东北黑土耕作的总侵蚀量

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It is difficult to estimate soil thickness eroded from annual erosion rates in cultivated Black soils in northeast China because of the uncertainty of the time when the soil was first cultivated for agricultural crops. Assuming soil organic carbon (SOC) profile curves for cultivated sites are the same as virgin sites before cultivation, it may be possible to estimate the total thickness of surface soils lost by erosion by vertical movement of plotted SOC profiles until those for the virgin and cultivated soils are superimposed. We collected pairs of soil samples (0-1 m) with one sample in each pair from a virgin site and the other from a nearby cultivated site in Heilongjiang province, northeast China. In undulating areas where soil erosion was moderate, the shapes of SOC distribution curves below 40 cm depth were nearly identical for both cultivated and virgin soils, but were offset vertically. This offset was attributed to the loss of surface soil by erosion in the cultivated land. By moving the distribution curve of SOC in cultivated soil downwards by 12.7 cm, we found nearly coincident curves below 45 cm for the virgin and cultivated soils. This thickness (12.7 cm) was believed to be the depth of soils that had been eroded since the onset of cultivation in Black soils in northeast China. We concluded that the amount of surface soil lost by erosion could be estimated from comparison of the vertical distribution of SOC in cultivated and virgin soils.
机译:由于最初用于农作物种植的时间不确定,因此很难估算东北地区已耕种的黑色土壤的年侵蚀率所侵蚀的土壤厚度。假设耕地的土壤有机碳(SOC)曲线与耕种前的处女地相同,则可以通过绘制SOC曲线的垂直运动直到原始和耕种的土壤剖面来估算由于侵蚀而损失的表层土壤总厚度。土壤被叠加。我们收集了成对的土壤样本(0-1 m),每对样本中一个来自原始站点,另一个来自附近的黑龙江省耕地。在土壤侵蚀适度的起伏地区,耕作土壤和原始土壤的SOC分布曲线在40 cm深度以下的形状几乎相同,但垂直偏移。这种抵消归因于耕地侵蚀造成的表层土壤流失。通过将耕作土壤中SOC的分布曲线向下移动12.7 cm,我们发现原始土壤和耕作土壤中45 cm以下的曲线几乎重合。该厚度(12.7厘米)被认为是自中国东北黑土耕种开始以来被侵蚀的土壤深度。我们得出的结论是,通过比较耕作土壤和原始土壤中SOC的垂直分布,可以估算出侵蚀造成的表层土壤损失量。

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