Premium
Dynamics of Gross Nitrogen Transformations in an Old‐Growth Forest: The Carbon Connection
Author(s) -
Hart Stephen C.,
Nason G. E.,
Myrold David D.,
Perry David A.
Publication year - 1994
Publication title -
ecology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.144
H-Index - 294
eISSN - 1939-9170
pISSN - 0012-9658
DOI - 10.2307/1939413
Subject(s) - nitrification , mineralization (soil science) , autotroph , heterotroph , incubation , nitrogen cycle , cycling , ecology , ammonium , environmental chemistry , biomass (ecology) , nitrogen , soil water , biology , chemistry , zoology , forestry , bacteria , biochemistry , genetics , organic chemistry , geography
We conducted a 456—d laboratory incubation of an old—growth coniferous forest soil to aid in the elucidation of C controls on N cycling processes in forest soils. Gross rates of N mineralization, immobilization, and nitrification were measured by 1 5 N isotope dilution, and net rates N mineralization and nitrification were calculated from changes in KCl—extractable inorganic N and NO 3 — @ ON pool sizes, respectively. Changes in the availability of C were assessed by monitoring rates of CO 2 evolution and the sizes of extractable organic C and microbial biomass pools. Net and gross rates of N mineralization (r 2 = 0.038, P = .676) and nitrification (r 2 = 0.403, P = .125) were not significantly correlated over the course of the incubation, suggesting that the factors controlling N consumptive and productive processes do not equally affect these processes. A significant increase in the NO 3 — pool size (net nitrification) only occurred after 140 d, when the NO 3 — pool size increased suddenly and massively. However, gross nitrification rates were substantial throughout the entire incubation and were poorly correlated with these changes in NO 3 — pool sizes. Concurrent decreases in the microbial biomass suggest that large increases in NO 3 — pool sizes after prolonged incubation of coniferous forest soil may arise from reductions in the rate of microbial immobilization of NO 3 — , rather than from one of the mechanisms proposed previously (e.g., sequestering of NH 4 + by microbial heterotrophs, the deactivation of allelopathic compounds, or large increases in autotrophic nitrifier populations). Strong correlations were found between rates of CO 2 evolution and gross N mineralization (r 2 = 0.974, P < .0001) and immobilization (r 2 = 0.980, P < .0001), but not between CO 2 evolution and net N mineralization rates. Microbial growth efficiency, determined by combining estimates of gross N immobilization, CO 2 evolution, and microbial biomass C and N pool sizes, declined exponentially over the incubation. These results suggest the utilization of lower quality substrates as C availability declined during incubation. Results from this research indicate the measurement of gross rates of N transformations in soil provides a powerful tool for assessing C and N cycling relationships in forests.