首页> 外文期刊>Soil Biology & Biochemistry >Nitrite production by Nitrosomonas europaea and Nitrosospira sp. AV in soils at different solution concentrations of ammonium.
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Nitrite production by Nitrosomonas europaea and Nitrosospira sp. AV in soils at different solution concentrations of ammonium.

机译:亚硝酸盐沼和亚硝基螺菌亚硝酸盐的生产。不同浓度铵溶液在土壤中的AV。

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Although it remains unclear why NH3-oxidizing bacteria (AOB) of the genus Nitrosospira dominate soil environments, and why Nitrosomonas spp. are less common, virtually no studies have compared their behavior in soil. In this study, the NH3 oxidation rates of Nitrosomonas europaea (ATCC 19718) and Nitrosospira sp. AV were compared in three differently textured soils containing a range of extractable NH4+ contents (2-11 micro g NH4+-N g-1 soil). Soils were adjusted to pH 7.0-7.4 with CaCO3 and sterilized with gamma -radiation. Cell suspensions of each bacterium were inoculated into the soils to bring them to two-third of water-holding capacity and cell densities ~2.5x106 g-1 soil. In virtually all cases, rates of NO2- production for both N. europaea and Nitrosospira sp. AV were linear over 48 h, and represented between 13 and 75%, respectively, of the maximum rates achieved in soil-free bacterial suspensions. Soil solution NH4+ concentrations that supported these rates ranged between 0.2 and 1.5 mM. Addition of 21-36 micro g NH4+-N g-1 soil raised soil solution NH4+ levels to 1.8-2.5 mM and stimulated NO2- production to a greater extent in N. europaea (3.3-6.6-fold) than in Nitrosospira sp. AV (1-2.1-fold). Maximum rates of NO2- production were obtained by raising soil solution NH4+ levels to 3-4 mM with a supplement of ~80-90 micro g NH4+-N g-1 soil. Ks values in soil for Nitrosospira sp. AV and N. europaea were estimated as 0.14 and 1.9 mM NH4+, respectively, and estimates of Vmax were about 3.5-times higher for N. europaea (0.007 pmol h-1 cell-1) than for Nitrosospira sp. AV (0.002 pmol h-1 cell-1). The cell density of N. europaea increased in sterile Steiwer soil independent of supplemental NH4+. In the case of treatments receiving supplemental NH4+, growth yields of N. europaea calculated from either NO2- produced or NH4+ consumed were similar to those reported in literature (3.5x106-6x106 cells micro mol-1 NH4+). A higher growth yield was measured in the case of zero added NH4+ (2.7x107 cells micro mol-1 NH4+), indicating that use of organic carbon compounds might have occurred and resulted in some energy sparing. Our results suggest that Nitrosospira spp. with a Ks similar to Nitrosospira sp. AV may have an advantage for survival in soil environments where soil solution NH4+ levels are less than 1 mM. However, it is apparent that AOB like N. europaea are poised to take advantages of modest increases in extractable NH4+ that raise soil solution NH4+ levels to about 2.0-2.5 mM..
机译:尽管尚不清楚为什么亚硝基螺菌属的NH3氧化细菌(AOB)在土壤环境中占主导地位,以及为什么亚硝基梭菌属(Nitrosomonas spp。)仍然存在。较少见,几乎没有研究比较它们在土壤中的行为。在这项研究中,欧洲亚硝化单胞菌(ATCC 19718)和亚硝基螺菌的NH3氧化速率。在包含一定范围可提取NH4 +含量的3种不同质地的土壤(2-11微克NH4 + -N g-1土壤)中比较了AV。用CaCO 3将土壤的pH调节至7.0-7.4,并用γ射线灭菌。将每种细菌的细胞悬液接种到土壤中,使它们的持水能力和细胞密度达到2.5x106 g-1土壤的三分之二。在几乎所有情况下,欧洲猪笼草和亚硝基螺菌的NO2-产生率均较高。 AV在48小时内呈线性,分别代表无土细菌悬浮液中获得的最大比率的13%至75%。支持这些速率的土壤溶液中NH4 +浓度在0.2至1.5 mM之间。加入21-36微克NH4 + -N g-1土壤可使土壤溶液中的NH4 +水平提高到1.8-2.5 mM,并比硝化螺菌更能刺激欧洲猪笼草的NO2-产生(3.3-6.6倍)。 AV(1-2.1倍)。通过将土壤溶液中的NH4 +水平提高至3-4 mM,并补充约80-90 micro g NH4 + -N g-1土壤,可获得最大的NO2-产生速率。亚硝基螺菌在土壤中的Ks值。 AV和欧洲猪笼草的NH4 +估计分别为0.14和1.9 mM NH4 +,而欧洲猪笼草(0.007 pmol h-1 cell-1)的Vmax估计值比亚硝基螺菌菌种高约3.5倍。 AV(0.002 pmol h-1 cell-1)。在无菌Steiwer土壤中,欧洲猪笼草的细胞密度增加,独立于补充NH4 +。在接受补充NH4 +的处理的情况下,根据产生的NO2或消耗的NH4 +计算得出的欧洲猪笼草的生长产量与文献报道的相似(3.5x106-6x106细胞微摩尔-1 NH4 +)。在零添加的NH4 +(2.7x107细胞micro mol-1 NH4 +)的情况下测得更高的生长产量,表明可能已经发生了有机碳化合物的使用,并导致了一些能源节约。我们的结果表明,亚硝基螺旋体。具有与Nitrosospira sp。类似的Ks。 AV在土壤溶液中NH4 +含量小于1 mM的土壤环境中的生存可能具有优势。但是,很明显,像欧洲猪笼草这样的AOB有望利用适度增加的可提取NH4 +的优势,从而将土壤溶液中NH4 +的水平提高到约2.0-2.5 mM。

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