Deforestation may increase soil carbon but it is unlikely to be continuous or unlimited.
Deforestation may increase soil carbon but it is unlikely to be continuous or unlimited.
复制标题
森林砍伐可能会增加土壤碳,但不可能持续或无限制。
DOI:
10.1111/gcb.13999
复制
发表时间:
2018
影响因子:
11.6
通讯作者:
Schipper L
中科院分区:
文献类型:
--
作者:
Schipper L
Identifying land uses and management practices that maintain or enhance soil carbon storage are important for sequestering carbon from the atmosphere and improving soil ecosystem services (Herrero et al., 2016). There is debate about how much additional carbon can be stored annually in soil, and for how long, following change in land use or management (Smith, 2014) and resolving this question is important. This is particularly relevant now following the aspirational goal established in the 4 per mille initiative (4p1000, 2017). In a paper titled:“Continuous soil carbon storage of old permanent pastures in Amazonia”, Stahl et al.(2017) purported to show increases in soil carbon when tropical forests are converted to grazed pasture of about 5.3 t C ha À1 year À1 through stock measurements across a chronosequence of sites. They state in the abstract:“... our results show that if sustainable management is applied in tropical pastures coming from deforestation... they can ensure a continuous C storage”, in the discussion:“This result supports the idea that certain ecosystems such as permanent pasture continuously accumulate soil carbon in the long-term (ie several decades).” and later in the conclusions:“Moreover, the humified C stored in the deeper soil layers is likely to provide unlimited C accumulation and conservation of C in the long-term.”(Italics added).Continuous and unlimited accumulation of soil carbon would certainly be of great interest to researchers, policy makers and the broader public as a large contributor to mitigating greenhouse gas emissions, particularly at rates as high as 5 t C ha À1 year À1. However, continuous and unlimited carbon accumulation is not supported by the author’s data or the general literature. Using measurements of soil carbon stocks in a chronosequence of sites converted from forest to pasture, they reported no change in soil carbon for the first 24 years followed by increases in soil carbon between 24 and 36 years at 5 t C ha À1 year À1. From these data, it is not reasonable to extrapolate these increases for 12 years as continuous or unlimited without further justification. In the broader literature, it has been widely observed that carbon reaches a plateau in roughly 30 to 50 years or perhaps 100 years after system perturbation as new equilibrium is reached, and that pastures are not perpetual sinks of carbon (Smith, 2014).