Li Shuaifeng, Su Jianrong, Liu Wande, Lang Xuedong, Huang Xiaobo, Jia Chengxinzhuo, Zhang Zhijun, Tong Qing
Research Institute of Resource Insects, Chinese Academy of Forestry, Kunming, China; The Pu`er Forest Eco-system Research Station, State Forestry Bureau, Kunming, China.
Research Institute of Resource Insects, Chinese Academy of Forestry, Kunming, China.
PLoS One. 2015 Sep 23;10(9):e0135946. doi: 10.1371/journal.pone.0135946. eCollection 2015.
The objectives of this study were to estimate changes of tree carbon (C) and soil organic carbon (SOC) stock following a conversion in land use, an issue that has been only insufficiently addressed. For this study, we examined a chronosequence of 2 to 54-year-old Pinus kesiya var. langbianensis plantations that replaced the original secondary coniferous forest (SCF) in Southwest China due to clearing. C stocks considered here consisted of tree, understory, litter, and SOC (0-1 m). The results showed that tree C stocks ranged from 0.02±0.001 Mg C ha-1 to 141.43±5.29 Mg C ha-1, and increased gradually with the stand age. Accumulation of tree C stocks occurred in 20 years after reforestaion and C stock level recoverd to SCF. The maximum of understory C stock was found in a 5-year-old stand (6.74±0.7 Mg C ha-1) with 5.8 times that of SCF, thereafter, understory C stock decreased with the growth of plantation. Litter C stock had no difference excluding effects of prescribed burning. Tree C stock exhibited a significant decline in the 2, 5-year-old stand following the conversion to plantation, but later, increased until a steady state-level in the 20, 26-year-old stand. The SOC stocks ranged from 81.08±10.13 Mg C ha-1 to 160.38±17.96 Mg C ha-1. Reforestation significantly decreased SOC stocks of plantation in the 2-year-old stand which lost 42.29 Mg C ha-1 in the 1 m soil depth compared with SCF by reason of soil disturbance from sites preparation, but then subsequently recovered to SCF level. SOC stocks of SCF had no significant difference with other plantation. The surface profile (0-0.1 m) contained s higher SOC stocks than deeper soil depth. C stock associated with tree biomass represented a higher proportion than SOC stocks as stand development proceeded.
本研究的目的是评估土地利用转换后树木碳(C)和土壤有机碳(SOC)储量的变化,这一问题此前研究较少。本研究中,我们考察了一个2至54年生的思茅松人工林时间序列,这些人工林是由于砍伐而取代了中国西南地区原有的次生针叶林(SCF)。这里考虑的碳储量包括树木、林下植被、凋落物和土壤有机碳(0-1米)。结果表明,树木碳储量范围为0.02±0.001 Mg C ha-1至141.43±5.29 Mg C ha-1,并随林分年龄逐渐增加。造林后20年内树木碳储量持续积累,且碳储量水平恢复到次生针叶林水平。林下植被碳储量最大值出现在5年生林分(6.74±0.7 Mg C ha-1),是次生针叶林的5.8倍,此后,林下植被碳储量随人工林生长而减少。除规定火烧影响外,凋落物碳储量无差异。转换为人工林后,2年生和5年生林分的树木碳储量显著下降,但随后增加,直至在20年生和26年生林分达到稳定状态水平。土壤有机碳储量范围为81.08±10.13 Mg C ha-1至160.38±17.96 Mg C ha-1。造林显著降低了2年生人工林的土壤有机碳储量,由于整地造成的土壤扰动,与次生针叶林相比,1米土壤深度处损失了42.29 Mg C ha-1,但随后又恢复到次生针叶林水平。次生针叶林的土壤有机碳储量与其他人工林无显著差异。表层土壤(0-0.1米)的土壤有机碳储量高于深层土壤。随着林分的发育,与树木生物量相关的碳储量占比高于土壤有机碳储量。