State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Northwest A&F University, Yangling, Shaanxi, 712100, China.
Glob Chang Biol. 2014 Nov;20(11):3544-56. doi: 10.1111/gcb.12508. Epub 2014 May 16.
The establishment of either forest or grassland on degraded cropland has been proposed as an effective method for climate change mitigation because these land use types can increase soil carbon (C) stocks. This paper synthesized 135 recent publications (844 observations at 181 sites) focused on the conversion from cropland to grassland, shrubland or forest in China, better known as the 'Grain-for-Green' Program to determine which factors were driving changes to soil organic carbon (SOC). The results strongly indicate a positive impact of cropland conversion on soil C stocks. The temporal pattern for soil C stock changes in the 0-100 cm soil layer showed an initial decrease in soil C during the early stage (<5 years), and then an increase to net C gains (>5 years) coincident with vegetation restoration. The rates of soil C change were higher in the surface profile (0-20 cm) than in deeper soil (20-100 cm). Cropland converted to forest (arbor) had the additional benefit of a slower but more persistent C sequestration capacity than shrubland or grassland. Tree species played a significant role in determining the rate of change in soil C stocks (conifer < broadleaf, evergreen < deciduous forests). Restoration age was the main factor, not temperature and precipitation, affecting soil C stock change after cropland conversion with higher initial soil C stock sites having a negative effect on soil C accumulation. Soil C sequestration significantly increased with restoration age over the long-term, and therefore, the large scale of land-use change under the 'Grain-for-Green' Program will significantly increase China's C stocks.
将退化耕地转变为林地或草地,已被提议作为一种减缓气候变化的有效方法,因为这些土地利用类型可以增加土壤碳(C)储量。本文综合了 135 篇近期出版物(181 个地点的 844 个观测值),这些出版物主要集中在中国从耕地向草地、灌丛或森林的转变,即广为人知的“退耕还林”计划,以确定哪些因素正在推动土壤有机碳(SOC)的变化。结果强烈表明,耕地转化对土壤 C 储量有积极影响。0-100cm 土层土壤 C 储量的时间变化模式表明,在植被恢复之前,土壤 C 会在早期(<5 年)先减少,然后增加到净碳增益(>5 年)。表层(0-20cm)土壤的 C 变化速率高于深层土壤(20-100cm)。耕地转化为森林(乔木)具有比灌丛或草地更慢但更持久的碳固存能力的额外好处。树种在决定土壤 C 储量变化率方面起着重要作用(针叶树<阔叶树,常绿树<落叶林)。与温度和降水相比,恢复年龄是影响耕地转化后土壤 C 储量变化的主要因素,初始土壤 C 储量较高的地点对土壤 C 积累有负面影响。土壤 C 固存随着恢复年龄的增加而显著增加,因此,“退耕还林”计划下的大规模土地利用变化将显著增加中国的 C 储量。