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Updated: May 20, 2025

Measurement of the Potential Rates of Dissimilatory Nitrate Reduction to Ammonium Based on 14NH4+/15NH4+ Analyses via Sequential Conversion to N2O
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Measurement of the Potential Rates of Dissimilatory Nitrate Reduction to Ammonium Based on 14NH4+/15NH4+ Analyses via Sequential Conversion to N2O

Published on: October 7, 2020

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的可用性和降水的变化改变微生物介导的NO和N2O排放量从Pinyon-Juniper干地

Sharon Zhao1, Alexander H Krichels1,2, Elizah Z Stephens1

  • 1Department of Environmental Sciences, University of California, Riverside, California, USA.

Global change biology
|March 27, 2025
PubMed
概括

改变降水模式会影响 (N) 循环和微量气体排放. 干旱增加了土壤N,导致降雨恢复时释放更多的氧化 (NO) 和氧化 (N2O),影响气候变化.

关键词:
改变了降水情况.氧化氨的古生物学家.氨氧化细菌是一种氨氧化细菌.气候变化 气候变化 气候变化化化化化化化气循环是指气循环的循环.

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