Nitrification gene ratio and free ammonia explain nitrite and nitrous oxide production in urea-amended soils

被引:71
作者
Breuillin-Sessoms, Florence [1 ]
Venterea, Rodney T. [2 ,3 ]
Sadowsky, Michael J. [1 ,2 ]
Coulter, Jeffrey A. [4 ]
Clough, Tim J. [5 ]
Wang, Pang [1 ]
机构
[1] Univ Minnesota, Inst Biotechnol, St Paul, MN 55108 USA
[2] Univ Minnesota, Dept Soil Water & Climate, St Paul, MN 55108 USA
[3] USDA ARS, Soil & Water Management Res Unit, St Paul, MN 55108 USA
[4] Univ Minnesota, Dept Agron & Plant Genet, St Paul, MN 55108 USA
[5] Lincoln Univ, Fac Agr & Life Sci, POB 85084, Canterbury 7647, New Zealand
关键词
LONG-TERM FERTILIZATION; OXIDIZING BACTERIA; N2O EMISSIONS; HUMIC SUBSTANCES; ARCHAEA; OXIDATION; ACCUMULATION; RESPONSES; KINETICS; MECHANISMS;
D O I
10.1016/j.soilbio.2017.04.007
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
The atmospheric concentration of nitrous oxide (N2O), a potent greenhouse gas and ozone-depleting chemical, continues to increase, due largely to the application of nitrogen (N) fertilizers. While nitrite (NO2-) is a central regulator of N2O production in soil, NO2- and N2O responses to fertilizer addition rates cannot be readily predicted. Our objective was to determine if quantification of multiple chemical variables and structural genes associated with ammonia (NH3)- (AOB, encoded by amoA) and NO2--oxidizing bacteria (NOB, encoded by nxrA and nxrB) could explain the contrasting responses of eight agricultural soils to five rates of urea addition in aerobic microcosms. Significant differences in NO2- accumulation and N2O production by soil type could not be explained by initial soil properties. Biologically-coherent statistical models, however, accounted for 70-89% of the total variance in NO2- and N2O. Free NH3 concentration accounted for 50-85% of the variance in NO2- which, in turn, explained 62-82% of the variance in N2O. By itself, the time-integrated nxrA:amoA gene ratio explained 78 and 79% of the variance in cumulative NO2- and N2O, respectively. In all soils, nxrA abundances declined above critical urea addition rates, indicating a consistent pattern of suppression of Nitrobacter-associated NOB due to NH3 toxicity. In contrast, Nitrospira-associated nxrB abundances exhibited a broader range of responses, and showed that long-term management practices (e.g., tillage) can induce a shift in dominant NOB populations which subsequently impacts NO2- accumulation and N2O production. These results highlight the challenges of predicting NO2- and N2O responses based solely on static soil properties, and suggest that models that account for dynamic processes following N addition are ultimately needed. The relationships found here provide a basis for incorporating the relevant biological and chemical processes into N cycling and N2O emissions models. Published by Elsevier Ltd.
引用
收藏
页码:143 / 153
页数:11
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