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Grain size tunes microbial community assembly and nitrogen transformation activity under frequent hyporheic exchange: A column experiment

机译:晶粒尺寸在频繁的低于交换下调整微生物群落组件和氮转化活性:列实验

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摘要

Hyporheic zones (HZ) are hotspots for biogeochemical reactions where groundwater and surface water mix. River dam buildings and other hydrologic controls alter the sediment grain size distribution and modify the downstream hyporheic exchange, with cascading effects on geochemical and microbial processes in river corridors. In this lab-scale column experiment, the N transformations in HZ filled with sediments in different grain sizes were investigated with a focus on understanding the interplay among variational hydraulic connectivity, microbial community structure, functional potential under frequent groundwater-surface water exchange. Porosity was identified as the main driver determining bacterial community assembly in HZ sediments. Significant microbial zonation was observed along the columns and the degree of co-occurrence of bacterial communities in the Fine column was lower than that in the Coarse and Mix columns. The Coarse column allowed for almost 2.47 times the exchange flux relative to the Fine column, and generates the fastest DO consumption rate (-6.52 mu g O-2/L.s). The enrichment of nitriflers, i.e., Cytophagaceae and Bacillaceae and nitrification functional genes, i.e., amoA_AOA and amoA_AOB revealed the higher nitrification potential in column filled with coarse sediments. In com- parison, the highest NH4+ production rates (2.4 x 10(-3) mu g N/L.s) took place in Fine column. The higher abundancies of denitriflers such as Comamonadaceae and Lysobacter and enrichment of functional genes of nirK and nirS interestingly suggested the elevated denitrification potential in Fine column in a more anaerobic environment. The results implied that variations in microbial functional potential and associated nitrogen transformation may occur in size-fractioned HZ to dynamic hyporheic exchange, which added new knowledge to the underlying biogeochemical and ecological processes in regulated river corridors. (C) 2020 Elsevier Ltd. All rights reserved.
机译:Hyporheic区(HZ)是地球化学反应的热点,地下水和地表水混合。河坝建筑物和其他水文控制改变了沉积物粒度分布和修改下游低管交换,对地球化学和河流走廊的微生物过程的级联影响。在该实验室规模的柱实验中,研究了填充不同粒度沉积物的Hz中的N变化,专注于理解变分液态连接,微生物群落结构,在频繁地下水表面水交换下的功能潜力之间的相互作用。孔隙率被鉴定为Hz沉积物中的主要驾驶员确定细菌群落组件。沿柱观察显着的微生物区段,细柱中的细菌群落的共发生程度低于粗柱和混合柱的程度。粗柱允许相对于细柱的交换通量近2.47倍,并产生最快的消耗率(-6.52μgo-2 / L.)。富含氮的富集,即细胞学造香和硝酸杆菌和硝化官能基因,即AmOA_AOA和AmOa_Aob在填充有粗沉积物的柱中揭示了较高的硝化电位。在Com-parison中,最高的NH4 +生产率(2.4 x 10(-3)mu g n / l)发生在细柱中。诸如Comamonadaceae和粘附杆菌的较高的越野越高,疯子和牢房的功能基因的富集有趣地表明在更厌氧环境中细柱的脱硝潜力升高。结果暗示了微生物功能电位和相关氮转化的变化可能在尺寸分馏的Hz中发生动态低于过度交换,这增加了对受监管河流走廊中的潜在生物地球化学和生态过程的新知识。 (c)2020 elestvier有限公司保留所有权利。

著录项

  • 来源
    《Water Research》 |2020年第1期|116040.1-116040.11|共11页
  • 作者单位

    Hohai Univ Coll Environm Key Lab Integrated Regulat & Resource Dev Shallow Minist Educ Nanjing 210098 Jiangsu Peoples R China;

    Hohai Univ Coll Environm Key Lab Integrated Regulat & Resource Dev Shallow Minist Educ Nanjing 210098 Jiangsu Peoples R China;

    Hohai Univ Coll Environm Key Lab Integrated Regulat & Resource Dev Shallow Minist Educ Nanjing 210098 Jiangsu Peoples R China;

    Hohai Univ Coll Environm Key Lab Integrated Regulat & Resource Dev Shallow Minist Educ Nanjing 210098 Jiangsu Peoples R China;

    Hohai Univ Coll Environm Key Lab Integrated Regulat & Resource Dev Shallow Minist Educ Nanjing 210098 Jiangsu Peoples R China;

    Hohai Univ Coll Environm Key Lab Integrated Regulat & Resource Dev Shallow Minist Educ Nanjing 210098 Jiangsu Peoples R China;

    Hohai Univ Coll Environm Key Lab Integrated Regulat & Resource Dev Shallow Minist Educ Nanjing 210098 Jiangsu Peoples R China;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Hyporheic exchange; Grain size; Hydraulic conductivity; Microbial community assembly; Nitrogen transformation;

    机译:过度的交换;晶粒尺寸;液压导电性;微生物群落组装;氮转化;

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