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Impacts of experimental alteration of water table regime and vascular plant community composition on peat mercury profiles and methylmercury production

机译:实验性改变地下水位和维管植物群落组成对泥炭汞分布和甲基汞生产的影响

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Climate change is expected to alter the hydrology and vascular plant communities in peatland ecosystems. These changes may have as yet unexplored impacts on peat mercury (Hg) concentrations and net methylmercury (MeHg) production. In this study, peat was collected from PEATcosm, an outdoor, controlled mesocosm experiment where peatland water table regimes and vascular plant functional groups were manipulated over several years to simulate potential climate change effects. Potential Hg(II) methylation and MeHg demethylation rate constants were assessed using enriched stable isotope incubations at the end of the study in 2015, and ambient peal total Hg (THg) and MeHg concentration depth profiles were tracked annually from 2011 to 2014. Peat THg and MeHg concentrations and the proportion of THg methylated (%MeHg) increased significantly within the zone of water table fluctuation when water tables were lowered, but potential Hg(II) methylation rate constants were similar regardless of water table treatment. When sedges dominate over ericaceous shrubs, MeHg concentrations and %MeHg became significantly elevated within the sedge rooting zone. Increased desorption of Hg(II) and MeHg from the solid phase peat into pore water occurred with a lowered water table and predominant sedge cover, likely due to greater aerobic peat decomposition. Deeper, more variable water tables and a transition to sedge-dominated communities coincided with increased MeHg accumulation within the zone of water table fluctuation. Sustained high water tables promoted the net downward migration of Hg(II) and MeHg. The simultaneous decrease in Hg(II) and MeHg concentrations in the near-surface peat and accumulation deeper in the peat profile, combined with the trends in Hg(II) and MeHg partitioning to mobile pore waters, suggest that changes to peatland hydrology and vascular plant functional groups redistribute peat Hg(II) and MeHg via vertical hydrochemical transport mechanisms. (C) 2019 Elsevier B.V. All rights reserved.
机译:预计气候变化将改变泥炭地生态系统中的水文和维管植物群落。这些变化可能对泥炭中的汞(Hg)浓度和甲基汞净含量(MeHg)产生尚未开发的影响。在这项研究中,泥炭是从PEATcosm收集的,PEATcosm是一个室外受控的中观宇宙试验,在该试验中,泥炭地的地下水位制度和维管束植物的官能团经过了数年的操纵,以模拟潜在的气候变化影响。在2015年研究结束时,使用富集的稳定同位素孵育评估了潜在的Hg(II)甲基化和MeHg脱甲基化速率常数,并从2011年至2014年每年跟踪环境果皮总Hg(THg)和MeHg浓度深度分布图。泥炭THg当水位降低时,MeHg浓度和甲基化THg的比例(%MeHg)在水位降低的区域内显着增加,但是无论水位如何处理,潜在的Hg(II)甲基化速率常数都相似。当莎草在硬质灌木上占优势时,莎草生根区内的MeHg浓度和%MeHg显着升高。 Hg(II)和MeHg从固相泥炭向孔隙水中的解吸增加,同时地下水位降低和莎草覆盖率降低,这可能是由于好氧泥炭分解的增加。地下水位更深,变化更多,向以莎草为主的群落过渡与地下水位波动区内MeHg积累增加有关。持续的高水位促进了Hg(II)和MeHg的净向下迁移。 Hg(II)和MeHg浓度在近地表泥炭中同时下降并在泥炭剖面中更深处积累,再加上Hg(II)和MeHg分配到流动孔隙水的趋势,表明泥炭地水文学和血管的变化植物官能团通过垂直水化学转运机制重新分配泥炭Hg(II)和MeHg。 (C)2019 Elsevier B.V.保留所有权利。

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