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    东北平原旱地土壤侵蚀的空间变异及其土壤养分流失的潜在格局

    Spatial variation of soil erosion and potential pattern of soil nutrient loss in dryland in the Northeast plain

    • 摘要: 在国家重要粮食生产基地东北平原,近年来土壤侵蚀加剧,导致土壤养分流失与质量退化,直接威胁到国家粮食安全。笔者基于RUSLE模型和GIS技术,分析2010—2018年东北平原3大子平原(辽河平原、松嫩平原、三江平原)旱地的平均土壤侵蚀强度及其0~30 cm土壤养分流失的空间变异特征,阐明土壤侵蚀空间变异对土壤养分流失的影响。结果表明:1)东北平原旱地土壤侵蚀以微度侵蚀为主;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3大子平原中部、西部和南部地区。2)东北平原旱地土壤有机碳(SOC)和全氮(TN)含量呈由西南到东北递增,全磷(TP)含量呈由中部向四周辐射增大,全钾(TK)含量呈由中部向四周辐射减小的分布趋势;土壤SOC、TN、TP含量均是三江平原 > 松嫩平原 > 辽河平原,而土壤TK含量则是松嫩平原 > 三江平原 > 辽河平原。3)东北平原旱地土壤SOC、TN、TP、TK总流失量分别为2.95 × 107、3.24 × 106、1.67 × 106和6.24 × 107 t;土壤养分流失量呈西高东低格局,辽河平原土壤养分流失量高于松嫩平原和三江平原;随侵蚀强度加剧,各土壤养分平均单位面积流失量在3大平原呈显著增大趋势,总流失量呈先增大后减小再剧烈增大趋势;剧烈侵蚀区养分总流失量最大、轻度侵蚀区次之;辽河平原出现土壤养分“低含量–高流失”的矛盾特征。综上所述,东北平原3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。本研究阐明了东北平原旱地土壤侵蚀空间变异对土壤多养分流失的影响,可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。

       

      Abstract:
      Background As a critical national grain production base, the Northeast China plain has experienced intensified soil erosion in recent years. This leads to the loss of soil nutrients and degradation of soil quality, posing a direct threat to national food security. However, the specific extent of multi-nutrient loss from the soil caused by erosion in the upland soils of the Northeast China plain remains unclear. Furthermore, identifying which areas characterized by specific erosion intensities require prioritized attention and protective measures is an urgent research need.
      Methods Utilizing the RUSLE model integrated with GIS-based spatial analysis, this study analyzed the spatial variation characteristics of mean soil erosion intensity and associated 0–30 cm soil nutrient loss fluxes (including SOC, TN, TP, and TK) in drylands across the contiguous Liaohe, Songnen, and Sanjiang plains during 2010—2018. We further elucidated the mechanistic controls of soil erosion spatial heterogeneity on multi-nutrient depletion patterns.
      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 three sub-plains. 2) SOC and TN of dryland in the Northeast plain increased from the southwest to the northeast, TP increased from the center to the surroundings, and TK decreased 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. 3) 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. 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. The contradiction of "low content-high loss" of soil nutrients appeared in the Liaohe plain.
      Conclusions This study quantified multi-nutrient losses from erosion in the Northeast plain’s upland soils, elucidating the impact of spatial variability in soil erosion on multi-nutrient loss. It identified priority control zones—severe and slight erosion areas across its three sub-plains—with very severe erosion zones in the Liaohe plain demanding urgent intervention. These findings provide a scientific foundation for effective soil resource management and sustainable conservation in the region.

       

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