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Nitrogen loads alter the N_2 production between denitrification and anammox in Min River Estuary, a highly impacted estuary in southeast China

机译:氮负载改变了闽河河口中硝化和厌氧毒素之间的N_2生产,这是中国东南部受到高度影响的河口

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摘要

Estuarine sediment denitrification and anammox in response to increased nitrogen (N) loads remain poorly understood. In this study, we used N isotope tracer approach to investigate the spatial distribution of denitrification and anammox and identified the crucial controls on the partitioning of dinitrogen gas (N-2) production along the Min River Estuary (MRE), a highly impacted estuary in southeast China. The results indicated that denitrification and anammox rates ranged from 10.5 to 70.7 nmol g(-1) h(-1) and from 0.44 to 4.31 nmol g(-1) h(-1), respectively. Relative contribution of anammox to N-2 production (R-a) was in a range of 1.04-15.1%, tending to increase toward estuary mouth. Denitrification rates were significantly higher in upper (high N loads) than in lower estuary (low N loads), while anammox rates and R-a showed inverse distributions along the MRE. Wastewater discharge caused the N point pollution triggering denitrification but inhibiting anammox. The best predictor of the variations in denitrification rates was total nitrogen, whereas pH and NH4+ could explained the variations in anammox rates across the estuary. The crucial predictors for the partitioning of N-2 production between denitrification and anammox were NH4+ and NOx. These results suggest that the increase in human activities intensity can alter the partitioning of N-2 production between denitrification and anammox, and the magnitude of this switch can be predicted by N loads in MRE and other highly impacted estuaries. (c) 2021 Elsevier Ltd. All rights reserved.
机译:返回亚硝酸盐沉积物反硝化和厌氧毒素响应于增加的氮气(n)载荷仍然是较差的理解。在这项研究中,我们使用了N同位素示踪方法来研究反硝化和厌氧的空间分布,并确定了沿着Min River Entuary(MRE)沿着Min River Entuary(MRE)的二煤气(N-2)生产分配的关键管制东南部。结果表明,除硝化和厌氧速率分别为10.5至70.7 nmol g(-1)H(-1),分别为0.44至4.31nmol G(-1)H(-1)。 Anammox对N-2生产(R-A)的相对贡献在1.04-15.1%的范围内,趋于增加河口口。上层(高负荷)的脱氮率明显高于河口(低N负载),而厌氧速率和R-A沿着MRE显示逆分布。废水放电导致N点污染触发反硝化但抑制厌氧毒素。反硝化率变化的最佳预测因子是总氮,而pH和NH4 +可以解释河口厌氧率的变化。用于脱氮和厌氧之间的N-2产生分配的关键预测因子是NH 4 +和NOx。这些结果表明,人类活性的增加可以改变反硝化和厌氧之间的N-2产生的分配,并且可以在MRE和其他高度撞击的河口中预测该开关的大小。 (c)2021 elestvier有限公司保留所有权利。

著录项

  • 来源
    《Environmental Pollution》 |2021年第5期|116757.1-116757.8|共8页
  • 作者单位

    East China Normal Univ State Key Lab Estuarine & Coastal Res Shanghai 200241 Peoples R China|Fujian Normal Univ Key Lab Humid Subtrop Ecogeog Proc Minist Educ Fuzhou 350007 Peoples R China;

    East China Normal Univ State Key Lab Estuarine & Coastal Res Shanghai 200241 Peoples R China;

    East China Normal Univ State Key Lab Estuarine & Coastal Res Shanghai 200241 Peoples R China;

    Fujian Normal Univ Key Lab Humid Subtrop Ecogeog Proc Minist Educ Fuzhou 350007 Peoples R China;

    East China Normal Univ Sch Geog Sci Key Lab Geog Informat Sci Minist Educ Shanghai 200241 Peoples R China;

    Fujian Normal Univ Key Lab Humid Subtrop Ecogeog Proc Minist Educ Fuzhou 350007 Peoples R China;

    Fujian Normal Univ Key Lab Humid Subtrop Ecogeog Proc Minist Educ Fuzhou 350007 Peoples R China;

    Fujian Normal Univ Key Lab Humid Subtrop Ecogeog Proc Minist Educ Fuzhou 350007 Peoples R China;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);美国《生物学医学文摘》(MEDLINE);美国《化学文摘》(CA);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    N loads; Denitrification; Anammox; Land use; Min river estuary;

    机译:n负载;反硝化;anammox;土地使用;闽河口;

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