黄河中游黄土采煤沉陷对坡面水土流失经济损失的影响规律

Influence patterns of coal mining-induced subsidence on economic losses from soil erosion of loess slopes in the middle reaches of the Yellow River

  • 摘要:
    背景 定量评估沉陷坡面水土流失产生的经济损失,不仅是科学制定采煤沉陷区水土流失经济补偿标准的重要依据,也是实现高效治理的重要基础。
    方法 以陕北典型黄土采煤沉陷区内不同形态的沉陷坡面为研究对象,通过野外采样、室内测试、环境经济学分析等方法,构建了采煤沉陷坡面尺度的水土流失经济损失定量评价指标体系,揭示了采煤沉陷坡面水土流失经济损失的变化规律。
    结果和结论 (1)构建了包含4个子系统(土壤水分损失、土壤养分损失、土地废弃损失、泥沙损失)及8个量化指标(土壤水分、有机质、碱解氮、速效磷、土壤速效钾损失量、土地废弃面积、泥沙滞留量、泥沙淤积量)的采煤沉陷坡面水土流失的经济损失定量评价指标体系。(2)黄土沉陷坡面水土流失导致的水分、有机质、碱解氮、速效钾的经济损失均随坡度的增大而明显减小,而泥沙滞留的经济损失会随坡度的增大而明显增大。(3)黄土沉陷坡面土壤水分、有机质、碱解氮、速效磷、速效钾产生的经济损失均在“直线坡+≤5°”时达到最大,而土地废弃、泥沙滞留、泥沙淤积产生的经济损失均在“直线坡+>15°”时达到最大。(4)直线形和凸形、复合形、凹形沉陷坡面水土流失的总经济损失随坡度增大依次呈现“先增后降”“持续下降”“先稳后增”的变化规律。(5)泥沙滞留、土壤有机质损失、土地废弃等3项经济损失总和占黄土沉陷坡面水土流失总经济损失的91.69%,应作为沉陷坡面水土流失事后高效治理和经济补偿的重点。研究结果可为黄河中游采煤沉陷区水土流失的精准治理提供科学依据。

     

    Abstract:
    Background Quantitative assessment of economic losses from soil erosion on subsidence slopes in coal mining-induced subsidence areas can offer a critical basis for formulating scientific economic compensation standards while also laying a solid foundation for efficient governance.
    Methods This study investigated the subsidence slopes with different morphologies in the typical loess area subjected to coal mining-induced subsidence in northern Shaanxi Province. Using methods including field sampling, laboratory tests, and environmental economics analysis, this study constructed an index system for the quantitative assessment of economic losses from soil erosion on coal mining-induced subsidence slopes and revealed the variation patterns of such economic losses.
    Results and Conclusions An index system was constructed for the quantitative assessment of economic losses from soil erosion on coal mining-induced subsidence slopes. This system included four subsystems (i.e., soil moisture loss, soil nutrient loss, land abandonment, and sediment loss) and eight quantitative assessment indices (i.e., soil moisture, organic matter, alkali-hydrolyzable nitrogen, available phosphorus, soil available potassium loss, abandoned land area, sediment retention, and sediment deposition). With an increase in the slope gradient, the economic losses related to soil moisture, organic matter, alkali-hydrolyzable nitrogen, and available potassium caused by soil erosion on subsidence slopes decreased significantly, whereas the economic loss from sediment retention increased significantly. The economic losses related to soil moisture, organic matter, alkali-hydrolyzable nitrogen, available phosphorus, and available potassium peaked in the case of straight slopes at angles of +≤5°. In contrast, the economic losses from land abandonment, sediment retention, and sediment deposition reached the maximum in the case of straight slopes at angles of +>15°. With an increase in the slope gradient, the total economic losses from soil erosion on straight and convex, composite, and concave subsidence slopes exhibited an initial rise followed by a decline, a continuous decrease, and first stabilization followed by an increase, respectively. The sum of the economic losses from sediment retention, soil organic matter loss, and land abandonment accounted for 91.69 % of the total economic losses from soil erosion on subsidence slopes. Therefore, the three indices should be highlighted in the efficient management and economic compensation after soil erosion on subsidence slopes. Overall, the results of this study provide a scientific basis for the precise management of soil erosion in the coal mining-induced subsidence areas in the middle reaches of the Yellow River.

     

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