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A holistic framework integrating plant-microbe-mineral regulation of soil bioavailable nitrogen.
Daly, Amanda B; Jilling, Andrea; Bowles, Timothy M; Buchkowski, Robert W; Frey, Serita D; Kallenbach, Cynthia M; Keiluweit, Marco; Mooshammer, Maria; Schimel, Joshua P; Grandy, A Stuart.
Afiliación
  • Daly AB; Department of Natural Resources and the Environment, University of New Hampshire, 56 College Road, Durham, NH 03824 USA.
  • Jilling A; Department of Plant and Soil Sciences, Oklahoma State University, Stillwater, OK USA.
  • Bowles TM; Department of Environmental Science, Policy, and Management, University of California Berkeley, Berkeley, CA USA.
  • Buchkowski RW; Department of Biology, University of Western Ontario, London, ON Canada.
  • Frey SD; Department of Natural Resources and the Environment, University of New Hampshire, 56 College Road, Durham, NH 03824 USA.
  • Kallenbach CM; Department of Natural Resource Sciences, McGill University, Montreal, Canada.
  • Keiluweit M; School of Earth & Sustainability and Stockbridge School of Agriculture, University of Massachusetts, Amherst, MA USA.
  • Mooshammer M; Department of Environmental Science, Policy, and Management, University of California Berkeley, Berkeley, CA USA.
  • Schimel JP; Department of Ecology, Evolution, and Marine Biology, University of California, Santa Barbara, CA USA.
  • Grandy AS; Department of Natural Resources and the Environment, University of New Hampshire, 56 College Road, Durham, NH 03824 USA.
Biogeochemistry ; 154(2): 211-229, 2021.
Article en En | MEDLINE | ID: mdl-34759436
ABSTRACT
Soil organic nitrogen (N) is a critical resource for plants and microbes, but the processes that govern its cycle are not well-described. To promote a holistic understanding of soil N dynamics, we need an integrated model that links soil organic matter (SOM) cycling to bioavailable N in both unmanaged and managed landscapes, including agroecosystems. We present a framework that unifies recent conceptual advances in our understanding of three critical steps in bioavailable N cycling organic N (ON) depolymerization and solubilization; bioavailable N sorption and desorption on mineral surfaces; and microbial ON turnover including assimilation, mineralization, and the recycling of microbial products. Consideration of the balance between these processes provides insight into the sources, sinks, and flux rates of bioavailable N. By accounting for interactions among the biological, physical, and chemical controls over ON and its availability to plants and microbes, our conceptual model unifies complex mechanisms of ON transformation in a concrete conceptual framework that is amenable to experimental testing and translates into ideas for new management practices. This framework will allow researchers and practitioners to use common measurements of particulate organic matter (POM) and mineral-associated organic matter (MAOM) to design strategic organic N-cycle interventions that optimize ecosystem productivity and minimize environmental N loss. SUPPLEMENTARY INFORMATION The online version contains supplementary material available at 10.1007/s10533-021-00793-9.
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Texto completo: 1 Colección: 01-internacional Base de datos: MEDLINE Idioma: En Revista: Biogeochemistry Año: 2021 Tipo del documento: Article

Texto completo: 1 Colección: 01-internacional Base de datos: MEDLINE Idioma: En Revista: Biogeochemistry Año: 2021 Tipo del documento: Article