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    东北平原旱地土壤侵蚀空间分布对土壤养分流失的潜在影响

    Potential impact of soil erosion spatial distribution on soil nutrient loss of dryland in the Northeast Plain

    • 摘要: 目的研究东北平原旱地土壤侵蚀对土壤养分流失的影响,将为东北平原土壤资源的有效管理和合理保护提供科学依据。方法基于RUSLE模型和GIS技术,本文分析了2010-2018年东北平原旱地的平均土壤侵蚀强度和0~30 cm深土壤养分(有机碳、全氮、全磷、全钾)的空间变化特征,阐明了土壤侵蚀空间分布对土壤养分流失的影响。结果(1)东北平原旱地土壤侵蚀均以微度侵蚀为主,但侵蚀强度辽河平原>松嫩平原>三江平原。中度以上侵蚀主要分布在辽河平原的中部、西部和南部地区,松嫩平原的中部和西南部地区,三江平原的中部和南部地区。(2)东北平原旱地土壤有机碳、全氮均呈由西南到东北增大的空间分布趋势,土壤全磷呈由中部向四周辐射增大的分布趋势,而土壤全钾则呈由中部向四周辐射减小的分布趋势。三大子平原旱地的土壤有机碳、全氮、全磷含量,均是三江平原>松嫩平原>辽河平原,而土壤全钾含量则是松嫩平原>三江平原>辽河平原。三大子平原旱地土壤的养分含量均随区域土壤侵蚀强度增强呈持续降低趋势。(3)东北平原旱地土壤养分流失量呈西高东低、辽河平原高于松嫩平原和三江平原的格局。旱地有机碳、全氮、全磷、全钾的总流失量分别为2.95×107 t、3.24×106 t、1.67×106 t和6.24×107 t,四种养分总流失量达到9.68×107 t。随着侵蚀强度加剧,三大子平原各养分单位面积平均流失量呈现显著增大趋势;各养分总流失量呈现先增大后减小再剧烈增大的趋势,剧烈侵蚀区养分总流失量最大、轻度侵蚀区次之。在极强烈以上侵蚀区,各养分总流失量均是辽河平原>松嫩平原>三江平原。结论三大子平原的剧烈侵蚀区和轻度侵蚀区,尤其是辽河平原的极强烈以上侵蚀区,应是东北平原旱地土壤侵蚀和养分流失防治的重点关注区。

       

      Abstract: Purpose This study delineated the impact of soil erosion on nutrient loss of dryland in the Northeast Plain, aiming to provide a scientific basis for the effective management and rational protection of soil resources in the region. Methodology Utilizing the RUSLE model and GIS technology, this study analyzed the spatial variation characteristics of soil erosion intensity and soil nutrients content (SOC, TN, TP and TK) in the 0-30 cm depth of dryland soil, and clarified the impact of erosion spatial distribution on soil nutrient loss of dryland in the Northeast Plain during 2010-2018. Results (1) Soil erosion was primarily characterized as slight, with the following ranking of erosion intensity: Liaohe Plain>Songnen Plain>Sanjiang Plain. Moderate to severe erosion was mainly distributed in the central, western and southern parts of the Liaohe Plain, the central and southwestern parts of the Songnen Plain, and the central and southern parts of the Sanjiang Plain. (2) The spatial distribution of SOC and TN of dryland in the Northeast Plain increased from southwest to northeast, while TP showed a radially increasing trend from the center to the surroundings and TK exhibited a radially decreasing trend from the center to the surroundings. The content of SOC, TN and TP in the three sub-plains was in the order of Sanjiang Plain>Songnen Plain>Liaohe Plain, whereas the content of TK was in the order of Songnen Plain>Sanjiang Plain>Liaohe Plain. The nutrient content of dryland in the three sub-plains showed a continuous decreasing trend with increasing soil erosion intensity. (3) The soil nutrient loss of dryland in the Northeast Plain showed a pattern of being higher in the west and lower in the east, where the loss in the Liaohe Plain was higher than that in the Songnen Plain and Sanjiang Plain. The total loss of SOC, TN, TP and TK was 2.95×107 t, 3.24×106 t, 1.67×106 t and 6.24×107 t respectively, and the total loss of the four nutrients reached 9.68×107 t. With the intensification of erosion, the average loss per unit area of each nutrient showed a significant increasing trend in the three sub-plains, while the total loss of each nutrient exhibited a trend of initial increase, followed by a decrease, and then a sharp increase. The total loss of each nutrient was the largest in the area of severe erosion, followed by that in the area of slight erosion. In areas with very strong erosion and severe erosion, the total loss of each nutrient was in the order of Liaohe Plain>Songnen Plain>Sanjiang Plain. Conclusion The areas of severe and slight erosions in the three sub-plains, especially the areas of very strong erosion and severe erosion of the Liaohe Plain, should be prioritized for the prevention and control of soil erosion and nutrient loss of dryland in the Northeast Plain.

       

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