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首页> 外文期刊>Ecological Modelling >Changes in soil organic carbon stocks of wetlands on China's Zoige plateau from 1980 to 2010
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Changes in soil organic carbon stocks of wetlands on China's Zoige plateau from 1980 to 2010

机译:1980-2010年中国若尔盖高原湿地土壤有机碳储量的变化

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China's Zoige Plateau, located in the northeastern part of the Qinghai-Tibet plateau, has the largest alpine peat wetland in the world. However, little is known about how the soil organic carbon (SOC) stock of these wetlands has been influenced by human activities. In this study, we quantified the changes in the SOC stock in two counties (i.e., Hongyuan and Ruoergai) in the Zoige Plateau wetlands between 1980 and 2010 in response to progressive drainage of the wetlands and increased grazing intensity using the Environmental Policy Integrated Climate (EPIC) model. The results indicate that wetlands accumulate large amounts of SOC (>300 t C ha(-1)) in the upper 1 m of the soil in the study area. Wetland soils sequestered similar to 0.25 t C ha(-1) yr(-1) despite the degradation that has occurred due to drainage and grazing. Drainage was one of the main driving factors for SOC loss in the wetlands. Conversion of wetlands to grassland via drainage since 1980 led to a loss of approximately 4 t C ha(-1) from the SOC stock. On the other hand, grazing might have positive impact on root biomass accumulation, thus enhancing the SOC stock. As estimated by EPIC, more intensive grazing slightly increased the SOC stock. However, grazing is also a reason why wetlands were drained with all the negative effects on the SOC pool. The potential SOC sequestration of intensive grazing was offseted by the negative effect of drainage. The outcomes suggest not only to limit drainage and restore wetland, but also to control grazing which will in turn decrease drainages to sustain the ecosystem service of carbon sequestration provided by the Zoige wetlands. (C) 2016 Elsevier B.V. All rights reserved.
机译:中国的Zoige高原位于青藏高原的东北部,拥有世界上最大的高山泥炭湿地。然而,人们对于这些湿地的土壤有机碳(SOC)储量如何受到人类活动的影响知之甚少。在这项研究中,我们使用环境政策综合气候(Environmental Policy Integrated Climate),量化了1980年至2010年之间在佐伊格高原湿地的两个县(即宏远县和若尔盖)的SOC储量变化,以响应湿地的逐步排水和放牧强度增加( EPIC)模型。结果表明,湿地在研究区域的土壤上部1 m积累了大量的SOC(> 300 t C ha(-1))。尽管由于排水和放牧而发生了退化,但湿地土壤的固存量与0.25 t C ha(-1)yr(-1)相似。排水是湿地SOC损失的主要驱动因素之一。自1980年以来,通过排水将湿地转变为草地,导致SOC储量损失约4 t C ha(-1)。另一方面,放牧可能会对根系生物量积累产生积极影响,从而增加SOC储量。根据EPIC的估计,更密集的放牧会稍微增加SOC的存量。但是,放牧也是湿地被排水而对SOC池产生所有负面影响的原因。排水的负面影响抵消了集约化放牧的潜在SOC隔离。结果表明,不仅要限制排水和恢复湿地,而且要控制放牧,这将减少排水,以维持佐伊格湿地提供的碳固存的生态系统服务。 (C)2016 Elsevier B.V.保留所有权利。

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