[Temporal and Spatial Variation Characteristics of Carbon Storage in the Source Region of the Yellow River Based on InVEST and GeoSoS-FLUS Models and Its Response to Different Future Scenarios].

Jian-Kun Hou, Jian-Jun Chen, Kai-Qi Zhang, Guo-Qing Zhou, Hao-Tian You, Xiao-Wen Han
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引用次数: 6

Abstract

Regional land use change is the main cause of carbon storage changes in ecosystems. Predicting the impact of future land use changes on carbon storage is of great significance for the sustainable development of carbon storage functions. In recent years, under the combined action of natural and human factors, the land use in the source region of the Yellow River has changed significantly, and its carbon storage function has also changed accordingly. This study combined InVEST and GeoSoS-FLUS models to evaluate land use change and its impact on carbon storage in the source region of the Yellow River from 2000 to 2020 and from 2020 to 2040 under different scenarios. The results showed that:① from 2000 to 2020, the carbon storage in the source region of the Yellow River showed an overall upward trend, with a total increase of 11.59×106 t. ② Over the past 20 years, the land use changes in the source region of the Yellow River included mainly the increase in the area of low-coverage grassland, construction land, and wetland and the decrease in the area of high-coverage grassland, medium-coverage grassland, and unused land, as well as the large-scale reduction of unused land and the reduction of grassland. The increase in the area of wetlands was the main reason for the increase in carbon storage. ③ Under the natural change scenario in 2040, the ecosystem carbon storage in the source region of the Yellow River was 871.34×106 t, an increase of 3.92×106 t compared with that in 2020. Under the ecological protection scenario, carbon storage increased significantly, with an increase of 13.53×106 t compared with that in 2020. The results of this study can provide a scientific reference for the decision-making of land use management and the sustainable development of carbon storage function in the source region of the Yellow River.

基于InVEST和GeoSoS-FLUS模型的黄河源区碳储量时空变化特征及其对未来不同情景的响应[j]。
区域土地利用变化是生态系统碳储量变化的主要原因。预测未来土地利用变化对碳储量的影响,对碳储量功能的可持续发展具有重要意义。近年来,在自然和人为因素的共同作用下,黄河源区土地利用发生了显著变化,其碳储量功能也发生了相应的变化。本研究结合InVEST和GeoSoS-FLUS模型,对2000 - 2020年和2020 - 2040年不同情景下黄河源区土地利用变化及其对碳储量的影响进行了评价。结果表明:①2000—2020年,黄河源区碳储量总体呈上升趋势,总增幅为11.59×106 t。②近20年,黄河源区土地利用变化主要表现为低覆盖度草地、建设用地和湿地面积的增加,高覆盖度草地、中覆盖度草地和未利用地面积的减少;以及未利用土地的大规模减少和草地的减少。湿地面积的增加是碳储量增加的主要原因。③在2040年自然变化情景下,黄河源区生态系统碳储量为871.34×106 t,比2020年增加3.92×106 t。生态保护情景下,碳储量显著增加,与2020年相比增加13.53×106 t。研究结果可为黄河源区土地利用管理决策和碳汇功能可持续发展提供科学参考。
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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