Nitrification in acid soils: solving the paradox, possibly
Ammonia oxidation in soil was, until recently, thought to be dominated by autotrophic, chemolithotrophic proteobacteria. These organisms gain energy from oxidation of ammonia to nitrite and perform the first step in nitrification. All cultivated ammonia oxidising bacteria show no or very poor growth in liquid batch culture below pH 7. Paradoxically, nitrification occurs in acid soils at rates that are often faster than those in apparently more favourable neutral and alkaline soils. Understanding acidophilic ammonia oxidation is important globally and economically. Approximately 30% of the world’s soils are acidic (pH<5), including 50% of arable soils, and up to 70% of ammonia-based nitrogen fertiliser is lost through nitrification and leaching or denitrification of nitrate. Potential mechanisms for acidophilic ammonia oxidation include urea hydrolysis, protection in biofilms and aggregates and heterotrophic nitrification, but could also be due to acidophilic or acidotolerant ammonia oxidisers. Assessment of selection for such groups in acid soils was impossible…