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Original Research ARTICLE Provisionally accepted The full-text will be published soon. Notify me

Front. For. Glob. Change | doi: 10.3389/ffgc.2019.00066

Divergent patterns of carbon, nitrogen, and phosphorus mobilization in forest soils

  • 1Swiss Federal Institute for Forest, Snow and Landscape Research (WSL), Switzerland
  • 2Department of Soil Science and Soil Protection,Martin Luther University Halle-Wittenberg, Germany

Carbon (C), nitrogen (N), and phosphorus (P) become released in inorganic or organic forms during decomposition of soil organic matter (SOM), often at varying rates. Our study aimed at identifying the individual patterns and controls of C, N, and P mobilization in soils under beech forests. We exposed organic and mineral horizons sampled along a nutrient availability gradient in Germany to either permanent moist conditions or to dry spells in microcosms and quantified the release of inorganic and organic C, N, and P. In the moist control treatment, releases of DOC, DON and DOP were interrelated and depended on the C:N:P ratio of SOM, whilst net mineralization rates of C, N and P were poorly correlated. Mineralization of C decreased with soil depth from Oi to A horizons, reflecting the increasing SOM stability. Net mineralization of N and P showed divergent depth patterns. In the Oi horizon, microbial immobilization was more pronounced for N than for P. In A horizons, net mineralization of P was less than of N, very likely because of strong sorption of released phosphate by mineral phases. Counterintuitively, net P mineralization in A horizons increased towards P-poor sites, probably due to decreasing contents of clay and pedogenic oxides, and thus, declining P sorption. Drying and rewetting caused stronger mobilization of inorganic and organic P, and organic N than of inorganic C and inorganic N, most likely by lysis of microbial biomass with tight C:N:P ratios. Due to the divergent patterns in N and P cycling, the organic layer is more important for the mineralization of P than the mineral soil; for N the mineral soil is most relevant. Consequently, the loss of the organic layer would deteriorate P nutrition, in particular at nutrient-poor sites. Overall, our results indicate that the cycling of C, N, and P is not directly coupled due to the different microbial processing and, in the mineral soil, differential sorption of N and P. This may ultimately cause imbalances in the N and P nutrition of forests.

Keywords: Drying-rewetting, Dissolved organic matter (DOM), Immobilization, mineralization, nutrient availability, stoichiometry, sorption, Temperate beech forest

Received: 12 Jul 2019; Accepted: 11 Oct 2019.

Copyright: © 2019 Brödlin, Kaiser and Hagedorn. This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) and the copyright owner(s) are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms.

* Correspondence: Mx. Frank Hagedorn, Swiss Federal Institute for Forest, Snow and Landscape Research (WSL), Birmensdorf, Switzerland,