267-6 How Do Soil Properties Affect the Efficacy of Nitrification Inhibitors On Nitrous Oxide Emission and Distribution of Ammonia Oxidizers?.

Poster Number 1817

See more from this Division: SSSA Division: Soil Biology & Biochemistry
See more from this Session: Microbial Community Diversity: II

Tuesday, November 5, 2013
Tampa Convention Center, East Exhibit Hall

Rui Liu, Royal Parade Cnr and Tin Alley, Parkville, Melbourne School of Land and Environment, The University of Melbourne, Melbourne, VIC, AUSTRALIA, Deli Chen, School of Agriculture and Food, University of Melbourne, Victoria, VIC, AUSTRALIA, Helen Charlotte Suter, Agriculture and Food Systems, Melbourne School of Land and Environment, The University of Melbourne, Parkville, Victoria, 3010, Australia and Helen Hayden, Biosciences Research Division - Department of Primary Industries, Melbourne, Australia
Poster Presentation
  • Rui Liu Poster for ASA conference.pdf (1.0 MB)
  • Abstract:
    Nitrification is an important nitrogen (N) transformation process in soils, which converts relatively immobile ammonium (NH4+) and ammonia (NH3) into more mobile nitrate (NO3-). The NO3- can then be subjected to losses by leaching and as gaseous emissions (N2O or N2) from subsequent denitrification. Nitrous oxide (N2O) is a potent greenhouse gas with a global warming potential 300 times that of carbon dioxide (CO2). The application of nitrification inhibitors is one strategy to reduce these N losses as they inhibit the bacterial ammonia monooxygenase (amoA) enzyme that is involved in the oxidation of NH3 to NH2OH, the first step of nitrification. Previous studies have indicated that the efficiency of nitrification inhibitors is variable both spatially and temporally, and this depends greatly on the environmental conditions and soil properties.

    Some studies have verified that ammonia oxidizers can directly regulate N2O production. Ammonia-oxidizing bacteria (AOB) are generally believed to be the most important contributors to nitrification in agricultural soils, but ammonia-oxidizing archaea (AOA) can also be present in large numbers. Inhibition of nitrification after application of fertilizers treated with nitrification inhibitors has been observed for soil AOB populations but not for AOA populations. Differences in soil properties seems to be a key parameter responsible for the variation in their distributions, however there is no clearly identified soil chemical or physical parameter that is most important, and limited data exists regarding the importance of the soil microbial community.  Therefore, we undertook a laboratory incubation experiment aimed at evaluating the efficiency of the nitrification inhibitors 3, 4- dimethylpyrazol phosphate (DMPP) and acetylene in reducing N2O production from three soils of different physical and chemical properties, and their impact on the dynamics of AOB and AOA abundance.

    The results showed that the application of DMPP and acetylene can significantly reduce N2O emission from all three soils. DMPP inhibited N2O emissions better than acetylene in the neutral clay loam soil, less effectively in the acid loam soil, and equally well in the alkaline clay loam soil. It was concluded that soil pH is a key parameter influencing the effectiveness of the nitrification inhibitors.

    Further studies are currently being undertaken to quantify the amoA gene from bacteria and archaea in our soils to test if there is a direct relationship between these nitrifiers and soil properties that can influence N2O production from nitrification.

    See more from this Division: SSSA Division: Soil Biology & Biochemistry
    See more from this Session: Microbial Community Diversity: II