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Impacts of land reclamation on tidal marsh 'blue carbon' stocks

机译:土地综合对潮汐沼泽“蓝碳”股的影响

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Tidal marsh ecosystems are among earth's most efficient natural organic carbon (C) sinks and provide myriad ecosystem services. However, approximately half have been 'reclaimed' - i.e. converted to other land uses - potentially turning them into sources of greenhouse gas emissions. In this study, we applied C stock measurements and paleoanalytical techniques to sediments from reclaimed and intact tidal marshes in southeast Australia. We aimed to assess the impacts of reclamation on: 1) the magnitude of existing sediment C stocks; 2) ongoing C sequestration and storage; and 3) C quality. Differences in sediment horizon depths (indicated by ltrax-XRF scanning) and ages (indicated by lead-210 and radiocarbon dating) suggest a physical loss of sediments following reclamation, as well as slowing of sediment accumulation rates. Sediments at one meter depth were between similar to 2000 and similar to 5300 years older in reclaimed cores compared to intact marsh cores. We estimate a 70% loss of sediment C in reclaimed sites (equal to 73 Mg C ha(-1)), relative to stocks in intact tidal marshes during a comparable time period. Following reclamation, sediment C was characterized by coarse particulate organic matter with lower alkyl-o-alkyl ratios and higher amounts of aromatic C, suggesting a lower extent of decomposition and therefore lower likelihood of being incorporated into long-term C stocks compared to that of intact tidal marshes. We conclude that reclamation of tidal marshes can diminish C stocks that have accumulated over millennial time scales, and these losses may go undetected if additional analyses are not employed in conjunction with C stock estimates. (C) 2019 Published by Elsevier B.V.
机译:潮汐沼泽生态系统是地球上最有效的天然有机碳(C)下沉并提供无数的生态系统服务。然而,大约一半被“回收” - 即转换为其他土地用途 - 可能会将它们转化为温室气体排放来源。在这项研究中,我们将C股票测量和古分析技术应用于澳大利亚东南部的回收和完整的潮汐沼泽沉积物。我们旨在评估填海层的影响:1)现有沉积物C股的幅度; 2)持续封存和储存; 3)C质量。沉积物地平线深度的差异(由Ltrax-XRF扫描表示)和年龄(由Lead-210和RadioCarbon Dater表示)表明填海后沉积物的物理损失,以及减慢沉积物积累率。与完整的沼泽核心相比,一米深度的沉积物与2000年相似,类似于再生核心的5300岁。我们估计再生位点(等于73mg C ha(-1))的沉积物C损失的70%,相对于可比较的时间段内的完整潮汐沼泽的股票。填海后,沉淀物C的特征在于具有低烷基-O-烷基比的粗颗粒有机质和较高量的芳族C,表明分解的较低程度,因此与之掺入长期C库存的可能性较低完整的潮汐沼泽。我们得出结论,潮汐沼泽的回收可以减少积累超过千年时间尺度的股票,如果不与C库存估计一起使用额外的分析,这些损失可能会失败。 (c)2019年由elestvier b.v发布。

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