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基于土地利用变化的洞庭湖地区碳储量时空演变及情景模拟OA

Spatiotemporal evolution and scenario simulation of carbon storage in Dongting Lake area based on land use change

中文摘要英文摘要

[目的]探讨区域土地利用变化与生态系统碳储量的关系,预测不同情景下未来碳储量时空分布,为优化土地利用格局,提高区域碳储量和"双碳"战略目标的实现提供科学支撑.[方法]利用PLUS-InVEST模型分析洞庭湖地区2000-2020年碳储量的时空演变特征,并结合16个驱动因子,预测研究区域在不同情景下,2040年土地利用和碳储量变化趋势.[结果](1)2000-2020年洞庭湖地区土地利用类型以耕地和林地为主,二者占总面积接近80%.耕地、林地、草地、水体呈现减少趋势,建设用地和未利用地呈增长趋势.(2)2000-2020年洞庭湖地区总碳储量呈减少趋势,2000年、2005年、2010年、2015年、2020年总碳储量分别为7.455×108 t,7.436×108 t,7.414×108 t,7.402×108 t和7.389×108 t,其中林地为主要碳源.(3)土地利用类型转化直接影响碳储量,2000-2020年耕地转出、林地转出分别引起碳储量减少了6.3×105 t,1.56×107 t,草地转出、水体转出分别引起碳储量增加了5.8×105 t,5.8×106 t,建设用地转出、未利用地转出引起碳储量增加了2.7×105 t,8.5×105 t.(4)预测2040年,自然发展、耕地保护、经济发展、生态保护4种情景下的碳储量分别为7.352×108 t,7.363×108 t,7.347×108 t,7.398×108 t,其中生态保护情景总碳储量相比2020年有所增加,其他3种情景均为减少趋势.[结论]洞庭湖地区碳储量减少的主要原因是林地、耕地等高碳储地类向建设用地等低碳储地类转变,未来需优化国土空间规划布局,提高区域碳储量.

[Objective]This study aims to investigate the relationship between regional land use changes and ecosystem carbon storage,and to predict the spatiotemporal distribution of future carbon storage under different scenarios,thereby providing scientific support for optimizing land use patterns,enhancing regional carbon storage,and achieving the"dual carbon"strategic goals.[Methods]The PLUS-InVEST model was used to analyze the spatiotemporal evolution characteristics of carbon storage in the Dongting Lake area from 2000 to 2020.Combined with 16 driving factors,this study predicted land use and carbon storage change trends in the study area under different scenarios for 2040.[Results](1)From 2000 to 2020,the main land use types in the Dongting Lake area were cultivated land and forest land,together accounting for nearly 80%of the total area.Cultivated land,forest land,grassland,and water bodies showed a decreasing trend,while construction land and unused land exhibited an increasing trend.(2)From 2000 to 2020,the total carbon storage in the Dongting Lake area showed a decreasing trend.The total carbon storage in 2000,2005,2010,2015,and 2020 were 7.455×108 t,7.436×108 t,7.414×108 t,7.402×108 t,and 7.389×108 t,respectively,with forest land being the primary carbon source.(3)The conversion of land use types directly affected carbon storage.From 2000 to 2020,the transfer of cultivated land and forest land resulted in decreases in carbon storage of 6.3×105 t and 1.56×107 t,respectively.The transfer of grassland and water bodies caused carbon storage to increase by 5.8×105 t and 5.8×106 t,respectively.The transfer of construction land and unused land caused carbon storage to increase by 2.7×105 t and 8.5×105 t,respectively.(4)It was predicted that by 2040,the carbon storage under the four scenarios of natural development,cultivated land protection,economic development,and ecological protection would be 7.352×108 t,7.363×108 t,7.347×108 t,and 7.398×108 t,respectively.Among these,the total carbon storage under the ecological protection scenario was predicted to increase compared to 2020,while the other three scenarios showed a decreasing trend.[Conclusion]The main reason for the decrease in carbon storage in the Dongting Lake area is the conversion of high carbon storage land types such as forest land and cultivated land to low carbon storage land types such as construction land.In the future,it is necessary to optimize territorial spatial planning to increase regional carbon storage.

申海建;郭荣中;张阔;刘华平

湖南省测绘科技研究所,长沙 410007||湖南省自然资源调查与监测工程技术研究中心,长沙 410007长沙环境保护职业技术学院,长沙 410004||自然资源部南方丘陵区自然资源监测监管重点实验室,长沙 410118长沙环境保护职业技术学院,长沙 410004湖南省国土资源规划院,长沙 410118

资源环境

土地利用变化洞庭湖地区碳储量情景模拟

land use changeDongting Lake areacarbon storagescenario simulation

《水土保持研究》 2026 (3)

266-276,11

湖南省自然科学基金项目(2024JJ8363,2023JJ60253)自然资源部南方丘陵区自然资源监测监管重点实验室开放基金课题(NRMSSHR2022Y11)湖南省教育厅科研项目(23C1058)

10.13869/j.cnki.rswc.2026.03.029

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