Effect of vegetation type on throughfall deposition and seepage flux.
2008
de Schrijver, A. | Staelens, J. | Wuyts, K. | van Hoydonck, G. | Janssen, N. | Mertens, J. | Gielis, L. | Geudens, G. | Augusto, Laurent | Verheyen, Kris | Laboratory of Forestry ; Universiteit Gent = Ghent University (UGENT) | Haskoning Belgium BVBA ; Partenaires INRAE | Natuurpunt | Transfert Sol-Plante et Cycle des Eléments Minéraux dans les Ecosystèmes Cultivés (TCEM) ; Institut National de la Recherche Agronomique (INRA)-École Nationale d'Ingénieurs des Travaux Agricoles - Bordeaux (ENITAB)
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Mostrar más [+] Menos [-]Inglés. This paper compares different vegetation types (coniferous and deciduous forest, grassed and pure heathland) in terms of input (throughfall deposition) and output (seepage flux) in a region with intermediate nitrogen load (+/-20 kg N ha(-1) y(-1) via bulk precipitation) in comparable conditions in north Belgium. Coniferous forest (two plots Pinus sylvestris and two plots Pinus nigra) received significantly higher nitrogen and sulphur throughfall deposition than deciduous forest and heathland. Grassed and pure heathland had significantly highest throughfall quantities of Ca2+ and Mg2+, respectively. The observed differences in throughfall deposition between the different vegetation types were not univocally reflected in the ion seepage flux. Considerable seepage fluxes of NO3-, SO42-, Ca2+ and Al(III) were only found under the P. nigra plots. We discuss our hypothesis that the P. nigra forests already evolved to a situation of N saturation, while the other vegetation types did not. (C) 2007 Elsevier Ltd. All rights reserved.
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