Carbon pools in forest systems and new estimation based on an investigation of carbon sequestration

Bin Wang; Guoce Xu; Zhanbin Li; Yuting Cheng; Fengyou Gu; Mingzhu Xu; Yixin Zhang

doi:10.1016/j.jenvman.2024.121124

Carbon pools in forest systems and new estimation based on an investigation of carbon sequestration

J Environ Manage. 2024 May 10:360:121124. doi: 10.1016/j.jenvman.2024.121124. Online ahead of print.

Authors

Bin Wang¹, Guoce Xu², Zhanbin Li¹, Yuting Cheng³, Fengyou Gu¹, Mingzhu Xu¹, Yixin Zhang¹

Affiliations

¹ State Key Laboratory of Eco-hydraulics in Northwest Arid Region, Xi'an University of Technology, Xi' An, 710048, Shaanxi, China.
² State Key Laboratory of Eco-hydraulics in Northwest Arid Region, Xi'an University of Technology, Xi' An, 710048, Shaanxi, China. Electronic address: xuguoce@xaut.edu.cn.
³ State Key Laboratory of Eco-hydraulics in Northwest Arid Region, Xi'an University of Technology, Xi' An, 710048, Shaanxi, China; Geology and Environment, Xi'an University of Science and Technology, Xi' An, 710048, Shaanxi, China.

PMID: 38733838
DOI: 10.1016/j.jenvman.2024.121124

Abstract

Forests, the ancient wooden giants, are both symbols of natural beauty and reservoirs of carbon stocks. The current climate crisis has created an urgent need for an in-depth study of forest ecosystems and carbon stocks. Based on forest inventory data from field surveys and four bioclimatic zones [Zone 1 (Z1, humid forest), Zone 2 (Z2, semi-humid forest), Zone 3 (Z3, semi-humid to semi-arid forest-grassland), and Zone 4 (Z4, semi-arid typical grassland)], two methods [Method 1 (M1) and Method 2 (M2)] were used to estimate carbon stocks in forest ecosystems in Shaanxi Province, China, and explored the spatial patterns of carbon pools and potential influences. The total forest ecosystem carbon pool amounted to 520.80 Tg C, of which 53.60% was stored aboveground, 17.16% belowground, and 29.24% in soil (depth of 0-10 cm). Spatially, there were marked north-south gradients in both biomass (Z2 > Z3 > Z1 > Z4) and soil organic carbon densities (Z1 > Z2 > Z3 > Z4). The differences between aboveground and belowground biomass carbon density across broadleaf, needle-leaf, and broadleaf and needle-leaf mixed forest were not pronounced, while soil organic carbon density had the order of broadleaf (18.38 Mg C/ha) > needle-leaf (11.29 Mg C/ha) > broadleaf and needle-leaf mixed forest (10.33 Mg C/ha). Under an ideal scenario that excludes external factors, mainly forest growth, the sequestration potential of forest biomass by 2032 was estimated by M1 as 85.43 Tg, and by M2 to be substantially higher at 176.21 Tg. As of 2062, M1 estimated 155.97 Tg of sequestration potential for forest biomass. The spatial patterns of forest biomass and soil carbon density were closely related to climatic factors, and these relationships allowed the spatial division into two distinct climatic regions. Moreover, biomass carbon density was significantly correlated with the normalized difference vegetation index, soil silt, and elevation. This study provides key information for promoting the strategic shift from light-green to deep-green forest systems in Shannxi Province and updates the estimation methods of forest ecosystems' carbon pools based on field surveys.

Keywords: Carbon stock; Estimation; Factors influences; Field surveys; Forest ecosystem.