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Effects of drying and rewetting on soluble phosphorus and nitrogen in forest floors : An experiment with undisturbed columns

Title data

Hömberg, Annkathrin ; Matzner, Egbert:
Effects of drying and rewetting on soluble phosphorus and nitrogen in forest floors : An experiment with undisturbed columns.
In: Journal of Plant Nutrition and Soil Science. (2018) . - in press.
ISSN 1436-8730
DOI: https://doi.org/10.1002/jpln.201700380

Abstract in another language

Drying and rewetting (D/W) of soils often resulted in the release of soluble phosphorus (P) and nitrogen (N) thereby changing the availability of both nutrients. Most experiments on D/W have been conducted with disturbed mineral soil samples and with rewetting of the soil samples by abrupt change in the water potential. Here we studied the effect of D/W on the leaching of P and N from undisturbed forest floors of a European beech and a Norway spruce site under near field conditions of desiccation and rewetting. We hypothesized that even under realistic rewetting of undisturbed forest floors, the leaching of P and N is increased after D/W and that the effects are less pronounced for spruce than for beech because of the larger hydrophobicity of the spruce forest floor. Undisturbed forest floor columns were subjected to desiccation at 20°C until a matrix potential of -100 MPa (pF 6.0) was reached, while controls were kept at moist conditions. Columns were irrigated by 22 mm day-1 from day 1-3 and by 10 mm day-1 from day 4-14 given in automated short pulses. Leachates from the soil columns were analyzed for orthophosphate, total P, NH4, NO3 and total N. In the spruce forest floor the concentrations of total P in leachates and the leachate fluxes were strongly increased after D/W. The increase of solute P was less for beech than for spruce coinciding with less actual rewetting of the beech forest floor. Leaching of total N from the spruce forest floor was not affected by D/W, however, concentrations and leaching of NH4 increased while leaching of NO3 decreased. For beech the leaching of total N and NH4 increased after D/W while NO3 leaching decreased. The results indicate that also under realistic conditions, D/W of forest floors increases solute P and leads to changes in the ratio of NH4/NO3 in solution, thereby altering the availability of the nutrients.

Further data

Item Type: Article in a journal
Refereed: Yes
Additional notes: BAYCEER141974
Institutions of the University: Faculties > Faculty of Biology, Chemistry and Earth Sciences > Department of Earth Sciences > Chair Soil Ecology
Faculties > Faculty of Biology, Chemistry and Earth Sciences > Department of Earth Sciences > Former Professors > Chair Soil Ecology - Univ.-Prof. Dr. Egbert Matzner
Research Institutions
Research Institutions > Research Centres
Research Institutions > Research Centres > Bayreuth Center of Ecology and Environmental Research- BayCEER
Faculties
Faculties > Faculty of Biology, Chemistry and Earth Sciences
Faculties > Faculty of Biology, Chemistry and Earth Sciences > Department of Earth Sciences
Result of work at the UBT: Yes
DDC Subjects: 500 Science
Date Deposited: 03 Jan 2018 07:33
Last Modified: 03 Jan 2018 07:33
URI: https://eref.uni-bayreuth.de/id/eprint/41100