N tracing model AOA Boreal coniferous forest a b s t r a c tThe forest-floor organic layer of the boreal coniferous forest is generally characterized by large mineral-N pools (especially ammonium), high rates of gross N mineralization, and low rates of autotrophic nitrification and nitrate immobilization. As atmospheric N deposition increases in boreal regions, it is expected to increase N losses from the forest-floor organic layer, which could affect the N status and microbial N cycling of the underlying mineral soil. To test this possibility, we conducted a long-term experiment, starting in 2010, consisting of three N addition levels (0, 20, and 40 kg NH 4 CleN ha À1 yr
À1) in a boreal Larix gmelinii forest in the Great Xing'an Mountain, China. We measured mineral N concentrations (2012e2014), the in-situ net N-cycling rates (2012 and 2013), the gross N transformation rates (2014), and microbial abundance (2014) in mineral soil (0e10 cm) in the peak growing season. The gross rates of N transformations were quantified via a laboratory,
15N tracing experiment with a processbased 15 N tracing model. NO 3 À concentration, in-situ net nitrification, heterotrophic nitrification, gross nitrification, NO 3 À immobilization, and dissimilatory NO 3 À reduction to NH 4 þ (DNRA) neither increased nor decreased, suggesting that NO 3 À loss, production and retention were not affected by continual NH 4 þ additions. However, the NH 4 þ concentration and in-situ net ammonification rates increased under continued high NH 4 þ additions, reflecting a change in soil NH 4 þ status. As a result, microbial NH 4 þ cycling was in uncoupled state in the high N addition plots (NH 4 þ immobilization rates were incomparable to gross N mineralization rates), but this was not the case for the control and low N addition plots. Interestingly, the NH 4 þ oxidation rates decreased rather than increased with decreased NH 4 þ immobilization rates in the high N addition plots. However, the decreased NH 4 þ oxidation rates were paralleled by a reduction in ammonia-oxidizing archaea (AOA) abundance. Our results indicate that for this boreal coniferous forest, enhanced NH 4 þ deposition could alter mineral soil NH 4 þ status and NH 4 þ consumption. We show that NH 4 þ fertilization could inhibit NH 4 þ oxidation in forest soils.