A method to assess whether ‘preferential use’ occurs after 15N ammonium addition; implication for the 15N isotope dilution technique

The robustness of the assumption of equilibrium between native and added N during 15N isotope dilution has recently been questioned by Watson et al. (Soil Biol Biochem 32 (2000) 2019–2030). We re-analyzed their raw data using equations that consider the added and native NH4+ and NO3− pools as separate state variables. Gross mineralization rates and first-order rate constants for NH4+ and NO3− consumption were obtained by combining analytical integration of the differential equations with a non-linear fitting procedure. The first-order rate constants for NH4+ consumption and NO3− immobilization for the added NH4+ and NO3− pool were used to estimate gross mineralization rates and first-order rate constants for nitrification of native NH4+. The latter were 2–4 times lower than the first-order rate constants derived from the added N pool. This discrepancy between first-order rate constants for nitrification implies that one or more process rates estimated for the added N pools cannot be applied to the native N pools. Preferential use of the added N resulted in an overestimation of the gross mineralization by 1.5–2.5-fold, emphasizing the need for critical evaluation of the assumption of equilibrium before gross mineralization rates are calculated.