State Key Laboratory of Atmospheric Boundary Layer Physics and Atmospheric Chemistry (LAPC), Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China.
Sci China Life Sci. 2010 Jul;53(7):766-75. doi: 10.1007/s11427-010-4022-4. Epub 2010 Aug 10.
The present study provides an overview of existing literature on changes in soil organic carbon (SOC) of various terrestrial ecosystems in China. Datasets from the literature suggest that SOC stocks in forest, grassland, shrubland and cropland increased between the early 1980s and the early 2000s, amounting to (71+/-19) Tg x a(-1). Conversion of marshland to cropland in the Sanjiang Plain of northeast China resulted in SOC loss of (6+/-2) Tg x a(-1) during the same period. Nevertheless, large uncertainties exist in these estimates, especially for the SOC changes in the forest, shrubland and grassland. To reduce uncertainty, we suggest that future research should focus on: (i) identifying land use changes throughout China with high spatiotemporal resolution, and measuring the SOC loss and sequestration due to land use change; (ii) estimating the changes in SOC of shrubland and non-forest trees (i.e., cash, shelter and landscape trees); (iii) quantifying the impacts of grassland management on the SOC pool; (iv) evaluating carbon changes in deep soil layers; (v) projecting SOC sequestration potential; and (vi) developing carbon budget models for better estimating the changes in SOC of terrestrial ecosystems in China.
本研究概述了中国各种陆地生态系统土壤有机碳 (SOC) 变化的现有文献。文献中的数据集表明,中国森林、草地、灌丛和农田的 SOC 储量在 20 世纪 80 年代初至 21 世纪初之间有所增加,达到(71+/-19)Tg x a(-1)。同期,中国东北三江平原的沼泽地开垦为耕地,导致 SOC 损失了(6+/-2)Tg x a(-1)。然而,这些估计存在很大的不确定性,特别是对于森林、灌丛和草地的 SOC 变化。为了降低不确定性,我们建议未来的研究应集中于:(i)以高时空分辨率识别中国各地的土地利用变化,并测量土地利用变化导致的 SOC 损失和固存;(ii)估算灌丛和非森林树木(即经济林、防护林和景观林)的 SOC 变化;(iii)量化草地管理对 SOC 库的影响;(iv)评估深层土壤层的碳变化;(v)预测 SOC 固存潜力;(vi)开发碳预算模型,以更好地估计中国陆地生态系统 SOC 的变化。