Changing pH shifts the microbial sourceas well as the magnitude of N2O emission from soil
Author:
Publisher
Springer Science and Business Media LLC
Subject
Soil Science,Agronomy and Crop Science,Microbiology
Link
http://link.springer.com/content/pdf/10.1007/s00374-010-0484-6.pdf
Reference54 articles.
1. Acton SD, Baggs EM (2010) Interactions between N application rate, CH4 oxidation and N2O production in soil. Biogeochem. doi: 10.1007/s10533-010-9442-5
2. Allison SM, Prosser JI (1991) Urease activity in neutrophilic autotrophic ammonia-oxidising bacteria isolated from acid soils. Soil Biol Biochem 23:45–51
3. Allison SM, Prosser JI (1993) Ammonia oxidation at low pH by attached populations of nitrifying bacteria. Soil Biol Biochem 25:935–941
4. Avrahami S, Bohannan BJM (2009) N2O emission rates in a California meadow soil are influenced by fertilizer level, soil moisture and the community structure of ammonia-oxidizing bacteria. Glob Chang Biol 15:643–655
5. Bååth E, Anderson TH (2003) Comparison of soil fungal/bacterial ratios in a pH gradient using physiological and PLFA-based techniques. Soil Biol Biochem 35:955–963
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