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Analysis of Changes in Vegetation Carbon Storage and Net Primary Productivity as Influenced by Land-Cover Change in Inner Mongolia, China

Author

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  • Linye Zhu

    (Inner Mongolia Research Institute, China University of Mining and Technology (Beijing), Ordos 017004, China)

  • Mingming Shi

    (Urumqi Comprehensive Survey Center on Natural Resources, China Geological Survey, Urumqi 830057, China)

  • Deqin Fan

    (Inner Mongolia Research Institute, China University of Mining and Technology (Beijing), Ordos 017004, China)

  • Kun Tu

    (Inner Mongolia Research Institute, China University of Mining and Technology (Beijing), Ordos 017004, China)

  • Wenbin Sun

    (Inner Mongolia Research Institute, China University of Mining and Technology (Beijing), Ordos 017004, China)

Abstract

Exploring the influence of vegetation carbon stocks over land-cover change and the relationship between land-cover change and net primary production (NPP) is of great practical importance for achieving China’s carbon neutrality target. Therefore, this paper analyses the spatio-temporal distribution of land-cover change and NPP change in Inner Mongolia from 2000 to 2020 and explores the vegetation carbon stock change caused by land-cover change, the relationship between land cover and NPP, and the relationship between land-cover change and NPP change. The results show that the main land-cover change in Inner Mongolia during 2000–2020 was the conversion from other land-cover types to grassland, with the conversion of bare land to grassland from 2000 to 2010 covering an area of 20,634.87 km 2 . During the period of 2000–2020, the high values of NPP were mainly located in northeastern Inner Mongolia, and the low values were mainly distributed in southwestern Inner Mongolia. The total carbon storage changes in vegetation affected by land-cover change during 2000–2010 and 2010–2020 were 10,736,986.11 t and 3,894,272.41 t. The mean values of NPP for different land covers were, in descending order, forest > cultivated land > wetland > grassland > artificial surfaces > shrubland > water bodies > bare land. Between 2000 and 2010, the change in land-cover type to water bodies was the main cause of the decrease in NPP, and the increase in NPP was mainly due to the conversion of other land-cover types to cultivated land, forest, and grassland. The implementation of appropriate conservation and management measures (e.g., the construction of forest and grass ecological protection), planting, and the protection of high-vegetation carbon storage plants and other means can improve the level of vegetation carbon sequestration and protect the ecological environment of Inner Mongolia.

Suggested Citation

  • Linye Zhu & Mingming Shi & Deqin Fan & Kun Tu & Wenbin Sun, 2023. "Analysis of Changes in Vegetation Carbon Storage and Net Primary Productivity as Influenced by Land-Cover Change in Inner Mongolia, China," Sustainability, MDPI, vol. 15(6), pages 1-18, March.
    • Handle: RePEc:gam:jsusta:v:15:y:2023:i:6:p:4735-:d:1090178
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    Cited by:

    1. Linye Zhu & Yonggui Zhang & Kewen Chen & Qiang Liu & Wenbin Sun, 2023. "Exploring Land-Cover Types and Their Changes in the Open-Pit Mining Area of Ordos City Using Sentinel-2 Imagery," Sustainability, MDPI, vol. 15(19), pages 1-14, September.
    2. Yi Cao & Xingping Wen & Yixiao Wang & Xuanting Zhao, 2024. "The Analysis of NPP Changes under Different Climatic Zones and under Different Land Use Types in Henan Province, 2001–2020," Sustainability, MDPI, vol. 16(18), pages 1-22, September.

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