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    基于分布式测算的漓江流域水土保持碳汇能力评估

    Assessment of Carbon Sink Capacity in Soil and Water Conservation for Lijiang River Basin Based on Distributed Calculation

    • 摘要: 水土保持是增强陆地碳汇能力的重要途径。开展水土保持碳汇能力评估,对于量化评价区域水土保持碳中和贡献具有重要意义。本文以漓江流域为研究对象,基于水土保持碳汇能力评价指标体系本地化构建,结合遥感反演与实地监测,采用分布式测算方法对漓江流域2024年水土保持碳汇能力进行量化评估。结果表明:1)与流域未治理情景相比,漓江流域现状水土保持增汇量为3661.29万 t CO2,其中植被增汇占比 60.18%,土壤增汇占比39.77%,拦蓄水体增汇量仅占0.05%;2)漓江流域水土保持措施保土固碳量为411.20万 t CO2,林草、耕作措施保土固碳量占比分别为91.25%和8.54%,工程措施占比仅0.21%;3)漓江流域水土保持措施减蚀减排量为82.24万 t CO2,乔木林地和灌木林地减蚀减排量之和超总量的85%;4)单位面积水土保持林草措施增汇量为40.16 t CO2/公顷,分别是坡面水土保持工程措施和水土保持耕作措施增汇量的5.85倍和8.37倍;单位面积水土保持林草措施保土固碳量为4.51 t CO2/公顷,工程措施为4.46 t CO2/公顷,耕作措施为2.16 t CO2/公顷。研究表明漓江流域水土保持措施年增汇量相当于抵消1408万吨标准煤排放,凸显岩溶区生态治理的显著碳中和潜力。

       

      Abstract: [Background]Soil and water conservation is an important pathway to enhance terrestrial carbon sink capacity. Conducting evaluations of soil and water conservation carbon sink capacity is of significant importance for quantifying and assessing the contribution of regional soil and water conservation to carbon neutrality. [Methods]This study takes the Lijiang River Basin as the research object. Based on the localized construction of an evaluation index system for soil and water conservation carbon sink capacity, combined with remote sensing inversion and field monitoring, a distributed calculation method was used to quantitatively assess the carbon sink capacity of soil and water conservation in the Lijiang River Basin in 2024. [Results]The results show that: 1) Compared with the unmanaged scenario of the basin, the current soil and water conservation measures in the Lijiang River Basin have increased carbon sinks by 36.6129 million tons of CO2, of which vegetation accounts for 60.18%, soil accounts for 39.77%, and the carbon sink from stored water accounts for only 0.05%; 2) The soil conservation and carbon sequestration amount of soil and water conservation measures in the basin is 4.1120 million tons of CO2, with forest and grass measures and tillage measures accounting for 91.25% and 8.54% respectively, while engineering measures account for only 0.21%; 3) The erosion reduction and emission reduction amount of soil and water conservation measures in the basin is 0.8224 million tons of CO2, with the combined reduction from arbor and shrub forest lands exceeding 85% of the total; 4) The carbon sink increment per unit area of forest and grass measures for soil and water conservation is 40.16 tons of CO2 per hectare, which is 5.85 times and 8.37 times that of slope engineering measures and tillage measures for soil and water conservation respectively; the soil conservation and carbon sequestration amount per unit area of forest and grass measures is 4.51 tons of CO2 per hectare, compared with 4.46 tons for engineering measures and 2.16 tons for tillage measures. [Conclusions]The study indicates that the annual carbon sink increment from soil and water conservation measures in the Lijiang River Basin is equivalent to offsetting the emissions from 14.08 million tons of standard coal, highlighting the significant carbon neutrality potential of ecological governance in karst areas. Keywords: carbon sink of soil and water conservation; carbon neutrality; carbon sink capacity assessment; Lijiang River Basin; distributed calculation method.

       

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