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Substantial net N mineralization during the dormant season in temperate forest soils

Title data

Schütt, Marianne ; Borken, Werner ; Stange, Claus Florian ; Matzner, Egbert:
Substantial net N mineralization during the dormant season in temperate forest soils.
In: Journal of Plant Nutrition and Soil Science. Vol. 177 (2014) Issue 4 . - pp. 566-572.
ISSN 1436-8730
DOI: https://doi.org/10.1002/jpln.201300644

Abstract in another language

In temperate forest soils, nitrogen (N) net mineralization has been extensively investigated during the growing season, whereas N cycling during winter was barely addressed. Here, we quantified net ammonification and nitrification during the dormant season by in situ and laboratory incubations in soils of a temperate European beech and a Norway spruce forest. Further, we compared temperature dependency of N net mineralization in in situ field incubations with those from laboratory incubations at controlled temperatures.From November to April, in situ N net mineralization of the organic and upper mineral horizons amounted to 10.9 kg N ha-1 6 months-1 in the spruce soil and to 44.3 kg N ha-1 6 months-1 in the beech soil, representing 65% (beech) and 26% (spruce) of the annual above ground litterfall. N net mineralization was largest in the Oi/Oe horizon and lowest in the A and EA horizons. Net nitrification in the beech soil (1.5 kg N ha-1 6 months-1) was less than in the spruce soil (5.9 kg N ha-1 6 months-1). In the range of soil temperatures observed in the field (0 – +4°C), the temperature dependency of N net mineralization was low in the spruce soil. In the beech soil, the apparent temperature dependency of N net mineralization was much larger than in spruce and more pronounced in laboratory incubations than in the in situ incubations.In temperate forest soils N net mineralization during the dormant season contributes substantially to the annual N cycling, especially in deciduous sites with large amounts of litterfall immediately before the dormant season. High Q10 values of N net mineralization at low temperatures suggest a huge effect of future increasing winter temperature on the N cycle especially in deciduous forests.

Further data

Item Type: Article in a journal
Refereed: Yes
Additional notes: BAYCEER119608
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 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
Research Institutions
Research Institutions > Research Centres
Result of work at the UBT: Yes
DDC Subjects: 500 Science
Date Deposited: 07 Aug 2015 06:59
Last Modified: 07 Aug 2015 06:59
URI: https://eref.uni-bayreuth.de/id/eprint/17640