The influence of rewetting on vegetation development and decomposition in a degraded fen

Citation
M. Richert et al., The influence of rewetting on vegetation development and decomposition in a degraded fen, RESTOR ECOL, 8(2), 2000, pp. 186-195
Citations number
48
Categorie Soggetti
Environment/Ecology
Journal title
RESTORATION ECOLOGY
ISSN journal
10612971 → ACNP
Volume
8
Issue
2
Year of publication
2000
Pages
186 - 195
Database
ISI
SICI code
1061-2971(200006)8:2<186:TIOROV>2.0.ZU;2-I
Abstract
The rewetting technique border irrigation was installed in a degraded fen p eatland in northeastern Germany. Because of the prevailing site conditions, the technique resulted in two different rewetting variants (surface irriga tion and temporary inundation) at the study site. This paper reports on the practicability of this technique and the influence of rewetting on vegetat ion development, decomposition processes and soil nutrient availability, an d the possibilities for renewed peat accumulation. The technique proved to be suited for rewetting fen sites with a continuous slope, deep peat layer with low hydraulic conductivity, and upstream water recharge facilities. A subsidence of the ground-water levels during the summer months, however, co uld not be avoided in dry years. The vegetation changed slowly from species -poor grassland into typical fen plant communities, despite rewetting and s oil tillage. Species richness, however, was higher in the surface irrigatio n than in the temporary inundation variant. A sufficient water supply prove d to be absolutely necessary to retard decomposition processes because high er decomposition of root materials (i.e., higher k values) occurred under t emporary inundated conditions. Generally, the higher water content in the s oil after rewetting led to a lower nitrate-N-to-ammonium-N ratio in the top soil in both rewetting variants. In the surface irrigation variant the mine ral nitrogen content (Nmin) of the topsoil decreased from 7.8 to 4.4 g N/m( 2), which is also correlated with the increase in water content of the soil . The low Nmin levels of fens which were never deeply drained (0.9-2.8 g N/ m(2)), however, were not reached within the observation period of 3 years.