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Impact of nitrogen compounds on fungal and bacterial contributions to codenitrification in a pasture soil

机译:氮化合物对牧草土壤中共硝化作用的真菌和细菌的影响

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摘要

Ruminant urine patches on grazed grassland are a significant source of agricultural nitrous oxide (N2O) emissions. Of the many biotic and abiotic N2O production mechanisms initiated following urine-urea deposition, codenitrification resulting in the formation of hybrid N2O, is one of the least understood. Codenitrification forms hybrid N2O via biotic N-nitrosation, co-metabolising organic and inorganic N compounds (N substrates) to produce N2O. The objective of this study was to assess the relative significance of different N substrates on codenitrification and to determine the contributions of fungi and bacteria to codenitrification. 15N-labelled ammonium, hydroxylamine (NH2OH) and two amino acids (phenylalanine or glycine) were applied, separately, to sieved soil mesocosms eight days after a simulated urine event, in the absence or presence of bacterial and fungal inhibitors. Soil chemical variables and N2O fluxes were monitored and the codenitrified N2O fluxes determined. Fungal inhibition decreased N2O fluxes by ca. 40% for both amino acid treatments, while bacterial inhibition only decreased the N2O flux of the glycine treatment, by 14%. Hydroxylamine (NH2OH) generated the highest N2O fluxes which declined with either fungal or bacterial inhibition alone, while combined inhibition resulted in a 60% decrease in the N2O flux. All the N substrates examined participated to some extent in codenitrification. Trends for codenitrification under the NH2OH substrate treatment followed those of total N2O fluxes (85.7% of total N2O flux). Codenitrification fluxes under non-NH2OH substrate treatments (0.7–1.2% of total N2O flux) were two orders of magnitude lower, and significant decreases in these treatments only occurred with fungal inhibition in the amino acid substrate treatments. These results demonstrate that in situ studies are required to better understand the dynamics of codenitrification substrates in grazed pasture soils and the associated role that fungi have with respect to codenitrification.
机译:放牧草地上反刍的尿片是农业一氧化二氮(N2O)排放的重要来源。在尿-尿素沉积之后引发的许多生物和非生物N2O产生机制中,导致硝化N2O形成的共硝化是了解最少的一种。共氮化通过生物N-亚硝化作用形成杂化N2O,共同代谢有机和无机N化合物(N种底物)以产生N2O。这项研究的目的是评估不同氮底物对共硝化的相对重要性,并确定真菌和细菌对共硝化的贡献。在没有尿液存在或存在细菌的情况下,在模拟尿液事件发生八天后,分别将 15 N标记的铵盐,羟胺(NH2OH)和两个氨基酸(苯丙氨酸或甘氨酸)应用于筛分过的土壤中膜和真菌抑制剂。监测土壤化学变量和N2O通量,并确定共硝化N2O通量。真菌抑制使N2O通量降低了约两种氨基酸处理均占40%,而细菌抑制仅使甘氨酸处理的N2O通量降低14%。羟胺(NH2OH)产生最高的N2O通量,仅通过真菌或细菌抑制即可降低,而综合抑制则使N2O通量降低60%。所有检查的N种底物都在一定程度上参与了共硝化作用。 NH2OH底物处理下共氮化的趋势遵循总N2O通量的趋势(占总N2O通量的85.7%)。在非NH 2 OH底物处理下的共硝化通量(占总N 2 O通量的0.7–1.2%)降低两个数量级,并且仅在这些处理中显着降低在氨基酸底物处理中发生真菌抑制。这些结果表明,需要就地研究以更好地了解牧草土壤中共硝化底物的动力学以及真菌对共硝化的相关作用。

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