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Adverse Effects of Ammonia on Nitrification Process: the Case of Chinese Shallow Freshwater Lakes

机译:氨对硝化过程的不利影响-以中国浅层淡水湖泊为例

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摘要

Nitrification is a process in which ammonia is oxidized to nitrite (NO_2~-) that is further oxidized to nitrate (NO_3~-). The relations between these two steps and ambient ammonia concentrations were studied in surface water of Chinese shallow lakes with different trophic status. For the oxidations of both ammonia and NO_2~-, more eutrophic lakes generally showed significantly higher potential and actual rates, which was linked with excessive ammonia concentrations. Additionally, both potential and actual rates for ammonia oxidation were higher than those for NO_2~-oxidation in the more eutrophic lakes, while in the lakes with lower trophic status, both potential and actual rates for ammonia oxidation were almost equivalent to those for NO_2~- oxidation. This can be explained by the excessive unionized ammonia (NH_3) concentration that inhibits nitrite-oxidizing bacteria in the more eutrophic lakes. The laboratory experiment with different ammonia concentrations, using the surface water in a eutrophic lake, showed that ammonia oxidation rates were proportional to the ammonia concentrations, but NO_2~- oxidation rates did not increase in parallel. Furthermore, NO_2~- oxidation was less associated with particles in natural water of the studied lakes. Without effective protection, it would be selectively inhibited by the excessive ammonia in hypereutrophic lakes, resulting in NO_2~- accumulation. Shortly, the increased concentrations of ammonia cause a misbalance between the NO_2~--producing and the NO_2~--consuming processes, thereby exacerbating the lake eutrophication.
机译:硝化是将氨氧化为亚硝酸盐(NO_2〜-),再将其氧化为硝酸盐(NO_3〜-)的过程。研究了不同营养状态下中国浅水湖泊地表水中这两个步骤与环境氨浓度之间的关系。对于氨和NO_2〜-的氧化,富营养化湖泊通常显示出明显更高的电势和实际速率,这与氨浓度过高有关。此外,在富营养化湖泊中,氨氧化的电位和实际速率都高于NO_2〜-氧化,而在营养状态较低的湖泊中,氨氧化的电位和实际速率几乎与NO_2〜相等。 -氧化。这可以用过度富集的氨水(NH_3)的浓度来解释,该浓度会抑制富营养化湖泊中的亚硝酸盐氧化细菌。使用富营养化湖泊中的地表水在不同氨浓度下进行的实验室实验表明,氨氧化速率与氨浓度成正比,但NO_2〜-氧化速率并没有平行增加。此外,在被研究的湖泊中,NO_2〜-氧化与天然水中颗粒物的联系较少。没有有效的保护,富营养化湖泊中的过量氨会选择性地抑制它,导致NO_2〜-的积累。不久,氨浓度的升高会导致产生NO_2〜的过程和消耗NO_2〜的过程之间的失衡,从而加剧湖泊富营养化。

著录项

  • 来源
    《Water, air and soil pollution》 |2010年第4期|P.297-306|共10页
  • 作者单位

    Institute of Hydrobiology, The Chinese Academy of Sciences, 7 Donghu Nan Road, Wuhan, Hubei 430072, China Graduate School of the Chinese Academy of Sciences, 19 Yuquan Road, Beijing 100049, China;

    rnInstitute of Hydrobiology, The Chinese Academy of Sciences, 7 Donghu Nan Road, Wuhan, Hubei 430072, China;

    rnInstitute of Hydrobiology, The Chinese Academy of Sciences, 7 Donghu Nan Road, Wuhan, Hubei 430072, China;

    rnInstitute of Hydrobiology, The Chinese Academy of Sciences, 7 Donghu Nan Road, Wuhan, Hubei 430072, 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

    nitrification process; ammonia concentration; nitrite accumulation; chinese shallow lakes;

    机译:硝化过程氨浓度亚硝酸盐积累中国浅湖;

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