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[在灌注亚硝酸盐的土壤柱中实现完全硝化作用]

[Complete nitrification in soil columns perfused with nitrite].

作者信息

Marengo G W, Petenello M C

机构信息

Cátedra de Microbiología, Facultad de Ciencias Agrarias, Universidad Nacional de Rosario, Argentina.

出版信息

Rev Argent Microbiol. 1990 Jul-Sep;22(3):146-9.

PMID:2102014
Abstract

Four columns of the same soil were put under the continuous flow of a NaNO2 solution [50 ppm N], so as to follow the evolution of nitrification. The soil, the columns as well as the solution continuous flow regulating system, were prepared as in the previous experiments. The columns, with the exception of No1 (control), contained also the following substances: No2 and 4: 2% de CaCO3 and No3 and 4:0.0015% SO - 4-S. Since the eight day of perfusion all the effluents had an important concentration of nitrate (Figure 1), exceeding in them, the sum of [No-2-N] an [NO-3-N] (Table 1) the concentration of th NO-2-N of the perfusion solution. Finally, the [NO-2-N] was reduced importantly in the effluents, and the (NO-3N), in all of them, stabilized itself as values nearing 50 ppm. Its suggested that at the beginning of the experiment, an endogenous source of NO-2 was functioning, which could explain the observed phenomenon, and that later it ceased to do so. The populational density of NO-2 oxidizers increased, during the experiment, 49 times (Table 2). An increase was also measured in the populational density of NH+4 oxidizers, which amounted to 41 times. This later fact contributes to support the existence of an endogenous provision of NO-2 during the initial part of the experiment.

摘要

将四组相同的土壤置于[50 ppm氮]的NaNO₂溶液持续流动下,以跟踪硝化作用的演变。土壤、柱体以及溶液连续流动调节系统的制备方法与之前的实验相同。除1号柱体(对照)外,其他柱体还含有以下物质:2号和4号柱体含有2%的CaCO₃,3号和4号柱体含有0.0015%的SO₄²⁻ - S。自灌注第八天起,所有流出物中的硝酸盐浓度都很高(图1),其中[NO₂⁻ - N]和[NO₃⁻ - N]的总和超过了灌注溶液中NO₂⁻ - N的浓度(表1)。最后,流出物中的[NO₂⁻ - N]大幅降低,并且所有流出物中的(NO₃⁻ - N)稳定在接近50 ppm的值。这表明在实验开始时,存在一个内源性的NO₂来源,这可以解释观察到的现象,而后来它不再起作用。在实验过程中,NO₂氧化菌的种群密度增加了49倍(表2)。NH₄⁺氧化菌的种群密度也有所增加,达到了41倍。后一个事实有助于支持在实验初期存在内源性NO₂供应的观点。

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