Spatiotemporal Relationship Between Carbon Emissions and Ecosystem Service Value in Hutuo River Basin

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With the global pursuit of both sustainable development and environmental protection, especially in the context of carbon peaking and carbon neutrality strategies, the importance of ecosystem service in connecting nature and human well-being has become increasingly prominent. Land use change exerts a profound influence on variations of carbon emissions and ecosystem service values (ESV). In-depth exploration of intricate spatio-temporal relationships between land use change, carbon emission and ESV serves as a crucial foundation for promoting green sustainable development strategies. Consequently, taking Hutuo River Basin as the study area, based on five periods of land use and socio-economic data from 2000 to 2020, this research employed the spatial autocorrelation method to investigate the spatiotemporal evolution characteristics and spatial correlation patterns between carbon emissions and ESV in Hutuo River Basin. The results revealed that: ① From 2000 to 2020, Hutuo River Basin was dominated by farmland and grassland, and the conversion area of farmland was as high as 1 241 km2, which was the main driving force for land use change in Hutuo River Basin. ② Over the past two decades, Hutuo River Basin exhibited a significant increase in carbon emissions, with the total emissions rising from 14.029 million tons in 2000 to 57.633 million tons in 2020. In terms of carbon source/sink structures, construction land was the dominant carbon source. The areas with high-intensity carbon emissions were concentrated in the urban areas of Yangquan and Shijiazhuang cities. ③ The proportion of ESV from forest and grassland in Hutuo River Basin was relatively high. The ESV has shown downward trend over the past 20 years, decreasing from 50.25 billion yuan in 2000 to 48.004 billion yuan in 2020. ④ In Hutuo River Basin, there was a significant negative correlation between carbon emission intensity caused by land use and ESV intensity from 2000 to 2020. Specifically, an increase in carbon emission intensity due to land use activities corresponded to a decrease in ESV intensity. These research results can guide decision-making for green transformation and upgrading of industries, environmental protection policies formulation, and sustainable development in Hutuo River Basin.

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  • 10.13227/j.hjkx.202405102
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Impact of Land Urbanization on Carbon Emissions in Urban Agglomerations of the Middle Reaches of the Yangtze River.
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  • Di Zhang + 3 more

The urban agglomerations in the middle reaches of the Yangtze River (MYR-UA) are facing a severe challenge in reducing carbon emissions while maintaining stable economic growth and prioritizing ecological protection. The energy consumption related to land urbanization makes an important contribution to the increase in carbon emissions. In this study, an IPAT/Kaya identity model is used to understand how land urbanization affected carbon emissions in Wuhan, Changsha, and Nanchang, the three major cities in the middle reaches of the Yangtze River, from 2000 to 2017. Following the core idea of the Kaya identity model, sources of carbon emissions are decomposed into eight factors: urban expansion, economic level, industrialization, population structure, land use, population density, energy intensity, and carbon emission intensity. Furthermore, using the Logarithmic Mean Divisia Index (LMDI), we analyze how the different time periods and time series driving forces, especially land urbanization, affect regional carbon emissions. The results indicate that the total area of construction land and the total carbon emissions increased from 2000 to 2017, whereas the growth in carbon emissions decreased later in the period. Energy intensity is the biggest factor in restraining carbon emissions, followed by population density. Urban expansion is more significant than economic growth in promoting carbon emissions, especially in Nanchang. In contrast, the carbon emission intensity has little influence on carbon emissions. Changes in population structure, industrial level, and land use vary regionally and temporally over the different time period.

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  • Research Article
  • Cite Count Icon 6
  • 10.3390/land13040557
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  • Apr 22, 2024
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Land optimization simulation and ecosystem service value (ESV) estimation can better serve land managers in decision-making. However, land survey data are seldom used in existing studies, and land optimization constraints fail to fully consider land planning control, and the optimization at the provincial scale is not fine enough, which leads to a disconnection between academic research and land management. We coupled ESV, gray multi-objective optimization (GMOP), and patch-generating land use simulation (PLUS) models based on authoritative data on land management to project land use and ESV change under natural development (ND), rapid economic development (RED), ecological land protection (ELP), and sustainable development (SD) scenarios in 2030. The results show that construction land expanded dramatically (by 97.96% from 2000 to 2020), which encroached on grassland and cropland. This trend will continue in the BAU scenario. Construction land, woodland, and cropland are the main types of land used for expansion, while grassland and unused land, which lack strict use control, are the main land outflow categories. From 2000 to 2030, the total amount of ESV increases steadily and slightly. The spatial distribution of ESV is significantly aggregated and the agglomeration is increasing. The policy direction and land planning are important reasons for land use changes. The land use scenarios we set up can play an important role in preventing the uncontrolled expansion of construction land, mitigating the phenomenon of ecological construction, i.e., “governance while destruction”, and promoting food security. This study provides a new approach for provincial large-scale land optimization and ESV estimation based on land survey data and provides technical support for achieving sustainable land development.

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