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Topographic position and water chemistry of fens in a Dutch river plain
Author(s) -
Wassen Martin J.,
Barendregt Aat
Publication year - 1992
Publication title -
journal of vegetation science
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.1
H-Index - 115
eISSN - 1654-1103
pISSN - 1100-9233
DOI - 10.2307/3235801
Subject(s) - hydrology (agriculture) , environmental science , wetland , vegetation (pathology) , surface water , species richness , productivity , peat , groundwater , ecology , geology , biology , medicine , geotechnical engineering , macroeconomics , pathology , environmental engineering , economics
. On the Vecht river plain (western Netherlands), small fens, remnants of a large mesotrophic wetland bordering a moraine, of 1 to 5 ha are found in a man‐made matrix of lakes and pastures. The regional position of the fens, local position of sampling sites, composition of the vegetation and local hydrological variables were measured. Polders in the river plain produce a complex hydrology obscuring the regional zonation between moraine and river. Water supply and species composition are determined more by a site's regional than local position. High‐productivity reedlands are abundant close to the river. Carex paniculata reedlands receive large amounts of river water, which gives their fen water a high K + concentration. Low‐productivity C. diandra fens and litter fens have their optimum closer to the moraine. C. diandra fens are fed mainly by inflowing nutrient‐poor ground‐ or surface water; litter fens receive primarily rainwater. Nutrients in fen water and in peat are lowest in C. diandra and C. lasiocarpa fens, but do not differ significantly between the communities. In both, iron seems to be more important than calcium in reducing phosphate solubility. Iron richness in the C. diandra fens is caused by present inflows of ground‐ or surface water, while in C. lasiocarpa fens, which succeed the former, iron richness is the result of historical inflows.