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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 of soil and water conservation for Lijiang River Basin based on distributed calculation

    • 摘要:
      目的 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。
      方法 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 1)与流域未治理情景相比,漓江流域水土保持增汇量(以 CO2计,下同)为3 661.29万t,其中植被增汇60.18%,土壤增汇39.77%,拦蓄水体增汇0.05%;2)漓江流域水土保持措施保土固碳量411.20万t,林草和耕作措施保土固碳量所占比例分别为91.25%和8.54%,工程措施占0.21%;3)漓江流域水土保持措施减蚀减排量为82.24万t,乔木林地和灌木林地减蚀减排量之和超总量的85%;4)每公顷水土保持林草措施增汇量为45.40 t,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6.26和9.45倍;每公顷水土保持林草措施保土固碳量4.76 t,工程措施4.46 t,耕作措施2.16 t。
      结论 漓江流域水土保持措施增汇量相当于抵消1 408万t标准煤排放,凸显岩溶区生态治理的显著碳中和潜力。

       

      Abstract:
      Objective Soil and water conservation is an important pathway to enhance terrestrial carbon sink capacity. Conducting assessments of soil and water conservation carbon sink capacity is of significant importance for quantitatively evaluating the contribution of regional soil and water conservation to carbon neutrality.
      Methods This study quantitatively assessed the soil and water conservation carbon sink capacity of the Lijiang River Basin in 2024 by establishing a localized assessment indicator system and employing a distributed calculation method that combined remote sensing inversion and field monitoring.
      Results The analysis indicated that: 1) compared with the scenario without watershed management, the carbon sequestration increment amounts (in terms of CO2 equivalent, the same below) from soil and water conservation in the Lijiang River Basin were 36.612 9 million tons, of which vegetation contributed 60.18%, soil contributed 39.77%, and water retention contributed only 0.05%. 2) The soil conservation and carbon sequestration amounts from soil and water conservation measures in the Lijiang River Basin were 4.112 million tons, with vegetation measures and tillage measures accounting for 91.25% and 8.54%, respectively, while engineering measures contributed only 0.21%. 3) Erosion reduction and emission reduction amounts from soil and water conservation measures in the Lijiang River Basin were 0.822 4 million tons, with arbor forest land and shrub forest land together accounting for over 85% of the total. 4) The carbon sequestration increment amounts per hectare of soil and water conservation vegetation measures were 45.40 tons, which was 6.26 and 9.45 times that of slope soil and water conservation engineering measures and soil and water conservation tillage measures, respectively. The soil conservation and carbon sequestration amounts per hectare of vegetation measures were 4.76 tons, while engineering measures achieved 4.46 tons and tillage measures 2.16 tons.
      Conclusions The study demonstrates that the carbon sequestration increment amounts from soil and water conservation measures in the Lijiang River Basin are equivalent to offsetting emissions from 14.08 million tons of standard coal, highlighting the significant carbon neutrality potential of ecological management in karst regions.

       

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