Carbon stock and sequestration of planted and natural forests along climate gradient in water-limited area: A synthesis in the China?s Loess plateau*

被引:10
|
作者
Li, Binbin [1 ]
Gao, Guangyao [1 ,4 ]
Luo, Yiqi [2 ]
Xu, Mingxiang [3 ]
Liu, Guobin [3 ]
Fu, Bojie [1 ,4 ]
机构
[1] Chinese Acad Sci, Res Ctr Ecoenvironm Sci, State Key Lab Urban & Reg Ecol, Beijing 100085, Peoples R China
[2] Cornell Univ, Sch Integrat Plant Sci, Ithaca, NY 14853 USA
[3] Chinese Acad Sci & Minist Water Resources, Inst Soil & Water Conservat, State Key Lab Soil Eros & Dryland Farming Loess Pl, Yangling 712100, Peoples R China
[4] Natl Observat & Res Stn Earth Crit Zone Loess Plat, Xian 710061, Peoples R China
基金
中国国家自然科学基金;
关键词
Carbon sequestration; Planted forest; Natural forest; Deep soil profile; Climate gradient; Water-limited area; SOIL ORGANIC-CARBON; LAND-USE; PRECIPITATION GRADIENT; SEMIARID ECOSYSTEMS; AFFORESTATION; ACCUMULATION; STORAGE; DETERMINANTS; PLANTATIONS; VARIABILITY;
D O I
10.1016/j.agrformet.2023.109419
中图分类号
S3 [农学(农艺学)];
学科分类号
0901 ;
摘要
Large-scale afforestation has been widely implemented for restoring the degraded lands and mitigating climate change while naturally regenerated forests should be protected to preserve carbon (C) in land ecosystems. However, a critically needed comparison on the effectiveness of C sequestration between planted forest (PF) and natural forest (NF) in water-limited areas has rarely been conducted at a regional scale. This study synthesized 275 publications to examine the changes of C stock in above-ground biomass (AGB), below-ground biomass (BGB) and deep soils (0-200 cm) between PF and NF in the China's Loess Plateau, a typical water-limited region with extensive afforestation. We found that, NF stored more than twice as much C as did PF in both biomass and soil. But PF allocated relatively higher proportion of C stock to BGB and deep soil layer (> 100 cm) than NF. Moreover, the C sequestration rates in biomass and soil for PF were 1.42 and 1.72 Mg C ha-1 yr-1, respectively, much higher than that of NF (0.13 and -1.38 Mg C ha-1 yr- 1). In addition, afforestation in areas with the mean annual precipitation (MAP) greater than 505 mm may promote both biomass and soil C accumulation without causing severe soil water deficit. Moreover, the increase in mean annual temperature (MAT) could significantly promote the C accumulation in both biomass and soil of PF but accelerated the soil C loss of NF. Overall, our results indicate that afforestation in water-limited areas may exhibit higher potential to sequester C than naturally regeneration, and afforestation is worth promoting with careful consideration of planting density and rainfall zones to avoid causing excessive water depletion. This study has important implications for the forest management in water-limited areas particularly under global climate change.
引用
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页数:13
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