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Effects of grazing exclusion on carbon sequestration in China's grassland

机译:放牧排除对中国草原碳封存的影响

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摘要

Globally, grazing exclusion (GE) is an effective management practice to restore degraded grasslands and improve carbon (C) stock. However, the C dynamics in grasslands ecosystem with GE have not been well characterized. The results of 145 sites published in 118 recent literatures were synthesized to examine the dynamics of plant and soil C sequestrations in grassland ecosystem after GE, and with the recovery age > 27 years under the China's 'Returning Grazing Land to Grassland' Project. Results showed a positive impact of GE on vegetation and soil C stock at most sites. The mean rate of aboveground biomass carbon stock (AGBC) change was 10.64 g m(-2) yr(-1), and the mean rate of belowground biomass (0-30 cm) carbon stock (BGBC) change was 32.14 g m(-2) yr(-1) after GE. The mean rate of soil C stock change was 0.27, 0.23, 0.18, 0.09 Mg ha(-1) yr(-1) in 0-10 cm, 10-20 cm, 20-30 cm, and 30-100 cm (equivalent to 10 cm), respectively. And Grass-dominated grasslands present a higher C sequestration ability than forb-dominated grasslands. Soil C stock rates and vegetation biomass C changes showed an Exponential Decay trend since GE, and the AGBC changes reached a steady state (when the rate at the equilibrium point) first, followed by BGBC, and then soil C. The AGBC and BGBC both had opposite views on soil C changes in the top 30 cm soil layers. Soil N is a key factor in the regulation of soil C sequestration since long term GE ( > 20 years). The large scale of GE under 'Returning Grazing Land to Grassland' Project significantly increased grassland C stocks. Meanwhile, increased soil N supply to grasslands with GE at the latter recovery stage may enhance ecosystem C sequestration capacity.
机译:在全球范围内,放牧排除(GE)是一种有效的管理实践,可以恢复退化的草原并改善碳(C)库存。然而,GE的草原生态系统中的C动态并未得到很好的表征。 145个地点发表于118位最近的文献的遗址,综合,以检查GE后草原生态系统的植物和土壤C序列的动态,恢复时代>在中国“回归草地上的草地”项目下的恢复时代> 27年。结果对GE对大多数地点的植被和土壤C库存显示出积极影响。地上生物质碳股(AGBC)变化的平均速率为10.64克(-2)Yr(-1),下面的生物质(0-30cm)碳股(BGBC)变化为32.14克(-2 GE之后的YR(-1)。土壤C含量的平均速率为0.27,0.23,0.18,0.09mg ha(-1)Yr(-1),0-10cm,10-20cm,20-30cm和30-100厘米(相同分别为10厘米。和草丛主导的草原呈现比Forb主导的草原更高的C螯合能力。土壤C股率和植被生物量C变化显示出自GE以来的指数衰减趋势,并且AGBC变化达到稳态(当均衡点的速率)首先,其次是BGBC,然后土壤C. AGBC和BGBC两者对土壤C的相反看法,顶层30厘米的土壤层。土壤N是自GE(> 20年)长期以来土壤C螯合调节的关键因素。 “将放牧地放牧到草地”项目下的大规模大规模越来越大。同时,在后一期恢复期的GE的草地上增加了土壤N供应量可以增强生态系统C螯合能力。

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