Journal article

Soil nitrogen conservation mechanisms in a pristine south Chilean Nothofagus forest ecosystem


Authors listHuygens, D; Rütting, T; Boeckx, P; Van Cleemput, O; Godoy, R; Müller, C

Publication year2007

Pages2448-2458

JournalSoil Biology and Biochemistry

Volume number39

Issue number10

ISSN0038-0717

DOI Linkhttps://doi.org/10.1016/j.soilbio.2007.04.013

PublisherElsevier


Abstract
A N-15 tracing study was carried out to identify microbial and abiotic nitrogen (N) transformations in a south Chilean Nothofagus betuloides forest soil which is characterized by low N inputs and absence of human disturbance. Gross N transformation rates were quantified with a 15 N tracing model in combination with a Markov chain Monte Carlo sampling algorithm for parameter estimation. The 15 N tracing model included five different N pools (ammonium (NH4'), nitrate (NOD, labile (N-lab) and recalcitrant (N,,) soil organic matter and adsorbed NH4+), and ten gross N transformation rates. The N dynamics in the N. betuloides ecosystem are characterized by low net but high gross mineralization rates. Mineralization in this soil was dominated by turnover of Ntab, while immobilization of NH4+ predominantly entered the N-rec,, pool. A fast exchange between the NH4+ and the adsorbed NH4+ pool was observed, possibly via physical adsorption on and release from clay lattices, providing an effective buffer for NH4+. Moreover, high NH4+ immobilization rates into the Nrec pool ensure a sustained ecosystem productivity. Nitrate, the most mobile form of N in the system, is characterized by a slow turnover and was produced in roughly equal amounts from NH4+ oxidation and organic N oxidation. More than 86% of the NO3- produced was immediately consumed again. This study showed for the first time that dissimilatory nitrate reduction to ammonium (DNRA) was almost exclusively (> 99%) responsible for NO3- consumption. DNRA rather than N03 immobilization ensures that NO3 is transformed into another available N form. DNRA may therefore be a widespread N retention mechanism in ecosystems that are Nlimited and receive high rainfalls. (c) 2007 Elsevier Ltd. All rights reserved.



Citation Styles

Harvard Citation styleHuygens, D., Rütting, T., Boeckx, P., Van Cleemput, O., Godoy, R. and Müller, C. (2007) Soil nitrogen conservation mechanisms in a pristine south Chilean Nothofagus forest ecosystem, Soil Biology and Biochemistry, 39(10), pp. 2448-2458. https://doi.org/10.1016/j.soilbio.2007.04.013

APA Citation styleHuygens, D., Rütting, T., Boeckx, P., Van Cleemput, O., Godoy, R., & Müller, C. (2007). Soil nitrogen conservation mechanisms in a pristine south Chilean Nothofagus forest ecosystem. Soil Biology and Biochemistry. 39(10), 2448-2458. https://doi.org/10.1016/j.soilbio.2007.04.013


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