Huitong Experimental Station of Forest Ecology, Institute of Applied Ecology, Chinese Academy of Sciences, Shenyang 110016, China; Huitong National Research Station of Forest Ecosystem, Huitong 418307, China.
College of Bioscience and Biotechnology, Hunan Agricultural University, Changsha 410128, China.
Sci Total Environ. 2017 Jun 1;587-588:296-304. doi: 10.1016/j.scitotenv.2017.02.140. Epub 2017 Feb 27.
The conversion from natural forest to plantation has been widely applied, with consequences on ecosystem carbon pool. The experimental results of changes of soil carbon stocks after forest conversion are often contradictory. Moreover, the recovery time of soil carbon stocks after forest conversion varies among different sites. To examine the changes of soil carbon stocks following the forest conversions in the long-term and to estimate the recovery time, we selected 116 subtropical forests, including 29 pair-wise replicates for evergreen broadleaved forests (EBF, 40-100-year-old), young Chinese fir plantations (Cunninghamia lanceolata) (YCP, 4-8-year-old), middle-aged Chinese fir plantations (MACP, 13-20-year-old), and mature Chinese fir plantations (MCP, 23-32-year-old), and estimated soil carbon stocks. Soil carbon stocks of YCP and MACP decreased in average 12.5 and 28.7Mgha compared with EBF, and showed no variation between MCP and EBF. Soil carbon stocks were positively correlated to soil total nitrogen stocks and C:N ratio. Our results showed that the forest conversions didn't cause a variation of soil carbon stocks in the long-term, although there was a short-term decline after conversion. The recovery time of soil carbon stock is 27years. These results indicate that the conversion from evergreen broadleaved forests to Chinese fir plantations in subtropical region of China causes soil carbon release in early stage, but has no effect on soil carbon stocks in the long-term. Prolonging the rotation period (>27years) would offset the adverse effects of the forest conversion on soil carbon stocks, and be critical in alleviating global climate change.
从天然林向人工林的转换已经得到广泛应用,对生态系统碳库产生了影响。森林转换后土壤碳储量变化的实验结果往往存在矛盾。此外,森林转换后土壤碳储量的恢复时间在不同地点也有所不同。为了长期研究森林转换后土壤碳储量的变化并估计恢复时间,我们选择了 116 个亚热带森林,包括 29 对常绿阔叶林(EBF,40-100 年)、年轻的杉木人工林(Cunninghamia lanceolata)(YCP,4-8 年)、中年杉木人工林(MACP,13-20 年)和成熟杉木人工林(MCP,23-32 年)的成对样本,估计了土壤碳储量。与 EBF 相比,YCP 和 MACP 的土壤碳储量平均减少了 12.5 和 28.7Mgha,而 MCP 与 EBF 之间没有变化。土壤碳储量与土壤全氮储量和 C:N 比呈正相关。我们的研究结果表明,尽管在转换后存在短期下降,但森林转换在长期内不会导致土壤碳储量发生变化。土壤碳储量的恢复时间为 27 年。这些结果表明,在中国亚热带地区从常绿阔叶林向杉木人工林的转换会在早期导致土壤碳释放,但从长期来看对土壤碳储量没有影响。延长轮伐期(>27 年)将抵消森林转换对土壤碳储量的不利影响,这对缓解全球气候变化至关重要。