渝东南喀斯特地区碳储量时空变化、驱动因素及其对碳减排的贡献

    Spatio-temporal changes of carbon storage, driving factors and their contribution to carbon emission reduction in karst area, southeast Chongqing

    • 摘要:
      研究目的 渝东南喀斯特地区是中国西南岩溶生态系统核心区域和长江上游重要的生态屏障,开展陆地生态碳储量时空变化、驱动因素的研究分析,对喀斯特地区生态环境保护和碳减排具有重要意义。
      研究方法 基于多源遥感数据,运用GeoSOS-FLUS、InVEST模型和地理探测器,动态评估1990—2020年渝东南喀斯特地区的碳储量变化特征,并对渝东南喀斯特地区2030年3种不同情景下碳储量的时空变化情况进行模拟。
      研究结果 ①1990—2020年,研究区土地利用类型以林地为主,占比超过区域总面积的65%,受人为活动的干扰耕地成为土地流转面积最大的地类,建设用地成为整体变化率最显著的地类。②在30年时间跨度内,研究区生态系统总碳储量从26.0051×107 t增长至26.7063×107 t,增长率为2.70%,总体呈现持续增加的趋势。③植被生长状况、地形、温度是影响研究区碳储量时空变化的主要因素,在生态保护情景下2030年研究区碳储量为26.7408×107 t,碳储量高于自然增长情景的26.6816×107 t和城市发展情景的26.6041×107 t。
      结论 1990—2020年,渝东南喀斯特地区碳储量呈增长趋势,驱动因素主要为土地利用变化。未来的研究应该更加关注土地利用变化对碳储量影响的长期监测和评估,以及如何通过政策干预优化土地利用结构,从而实现区域碳储量的最大化和生态系统的可持续性。

       

      Abstract:
      Objective The karst area in the southeast of Chongqing is a core region of the karst ecosystem in southwest China and an important ecological barrier in the upper Yangtze River. Conducting research and analysis on the spatio−temporal changes and driving factors of terrestrial ecological carbon storage is of great significance for the ecological environment protection and carbon emission reduction in karst areas. Conducting research and analysis on the spatiotemporal changes and driving factors of terrestrial ecological carbon storage is of great significance for ecological environment protection and carbon reduction in karst areas.
      Methods Based on multi−source remote sensing data, GeoSOS−FLUS, InVEST model and geographical detectors to dynamically assess the characteristics of carbon stock changes in the southeast Chongqing karst region from 1990 to 2020, and simulated the spatio−temporal changes of carbon stocks in the southeast Chongqing karst region in 2030 under three different scenarios.
      Results ① during the period of 1990−2020, the land use type in the study area is dominated by forest land, which accounts for more than 65% of the total area of the region, and cropland in the study area is the land type with the largest area of land transfer due to the disturbance of anthropogenic activities, and construction land is the land type with the most significant rate of change in the whole. ② In the 30−year time span, the total carbon stock in the study area increased from 26.0051×107 t to 26.7063×107 t, with a growth rate of 2.70%, and the overall trend showed a continuous increase.③Vegetation growth condition, topography, and temperature are the main factors affecting the spatial and temporal changes of carbon stock in the study area, and the carbon stock in the study area in 2030 under the ecological protection scenario is 26.7408×107 t, which is higher than that in the natural growth scenario (26.6816×107 t) and the urban development scenario (26.6041×107 t).
      Conclusions From 1990 to 2020, the carbon storage in the karst area of southeastern Chongqing showed an increasing trend, and the driving factors were mainly land use change.Future research should pay more attention to the long−term monitoring and assessment of the impact of land use change on carbon stock, and how to optimize the land use structure through policy intervention, so as to achieve the maximization of regional carbon stock and the sustainable development of the ecosystem.

       

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