[Spatiotemporal variation and future scenario simulation of ecosystem carbon storage in the Hulun Lake Basin, Inner Mongolia, China].

Q3 Environmental Science
Qi Wang, Nan Shan, Nan-Nan Li, Zhao-Yong Zhang, Quan Li, Rui Diao, Wen-Lin Wang, Yu-Bing Qu
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引用次数: 0

Abstract

Carbon storage in terrestrial ecosystems plays a crucial role in climate change and the global carbon cycle. To investigate the spatiotemporal variations of carbon storage in the Hulun Lake Basin, we combined the InVEST and PLUS models to systematically analyze the impacts of land use changes from 1990 to 2020 on carbon storage, and simulate land use patterns and spatial distribution of carbon storage under different scenarios for 2030. The results indicated that the Hulun Lake Basin experienced significant changes in land use distribution during 1990-2020. The area of cultivated land, forest, bare land, and built-up land increased, while the area of grassland, water, and wetlands decreased. Total carbon storage in the basin increased by 1.48×107 t, with a growth rate of 1.0%. Carbon storage in forest and cultivated land increased by 7.18×107 and 6.7×106 t, while that in grassland, water, and wetlands decreased by 6.01×107, 1.8×106, and 1.7×106 t, respectively. Carbon storage in the basin exhibited significant spatial heterogeneity, with higher carbon storage areas mainly distributed in the eastern hilly areas of the basin and lower carbon storage areas mainly located in the northeastern part of the basin and around Hulun Lake. The spatial differentiation showed a strong coupling relationship with land use patterns. Under the four scenarios for 2030, including natural development, urban development, cropland protection, and ecological conservation,carbon storage in the Hulun Lake Basin showed an increasing trend, with the ecological conservation scena-rio demonstrating the most significant growth of 6.19×106 t and a growth rate of 0.4%. Our findings would provide important references for optimizing land use pattern and enhancing carbon storage capacity in the Hulun Lake Basin.

内蒙古呼伦湖流域生态系统碳储量时空变化及未来情景模拟[j]。
陆地生态系统的碳储量在气候变化和全球碳循环中起着至关重要的作用。为探讨呼伦湖流域碳储量的时空变化特征,结合InVEST和PLUS模型,系统分析了1990 - 2020年土地利用变化对流域碳储量的影响,并模拟了2030年不同情景下的土地利用格局和碳储量空间分布。结果表明:1990—2020年,呼伦湖流域土地利用格局发生了显著变化。耕地、森林、裸地和建设用地面积增加,草地、水域和湿地面积减少。流域总碳储量增加1.48×107 t,增长率为1.0%。森林和耕地碳储量分别增加7.18×107和6.7×106 t,草地、水体和湿地碳储量分别减少6.01×107、1.8×106和1.7×106 t。流域碳储量具有显著的空间异质性,高碳储量区主要分布在盆地东部丘陵地带,低碳储量区主要分布在盆地东北部和呼伦湖周边。空间分异与土地利用方式存在较强的耦合关系。2030年自然发展、城市发展、农田保护、生态涵养4个情景下,呼伦湖流域碳储量均呈现增加趋势,其中生态涵养情景增长最为显著,为6.19×106 t,增长率为0.4%。研究结果可为优化呼伦湖流域土地利用格局,提高流域碳储量提供重要参考。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
应用生态学报
应用生态学报 Environmental Science-Ecology
CiteScore
2.50
自引率
0.00%
发文量
11393
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