Chemical characteristics of soils and pore waters of three wetland sites dominated by Phragmites australis: relation to vegetation composition and reed performance
H. Cizkova et al., Chemical characteristics of soils and pore waters of three wetland sites dominated by Phragmites australis: relation to vegetation composition and reed performance, AQUATIC BOT, 69(2-4), 2001, pp. 235-249
Chemical characteristics of soils and soil pore waters, plant species compo
sition and horizontal stand structure were investigated for three reed stan
ds in the Trebon Basin (Czech Republic): Branna sand pit and two littoral s
tands of Rozmberk fishpond (Rozmberk East and Rozmberk West). Phragmites st
ands were expanding, stable and retreating at the three sites, respectively
. The elemental soil composition (especially of C, N, P, and K) indicated t
he lowest trophic conditions at Branna, intermediate at Rozmberk East and t
he highest at Rozmberk West. This corresponded well also with concentration
s of ammonium nitrogen, dissolved reactive phosphate and total phosphorus i
n the soil pore water. In contrast, Branna had by far the highest level of
total nitrogen, determined by nitrate nitrogen (20 mg l(-1)), and the highe
st level of total dissolved solids (concentrations of NO3-, SO42-, Ca2+ and
Mg2+) of all three sites. No conspicuous differences were found among the
three stands in biomass and its allocation. The vegetation composition corr
esponded more closely to elemental soil composition than to total nitrogen
or total dissolved solids in the pore water. It is concluded that Branna pr
ovides an example of a site subjected to an initiating but dramatic and fas
t eutrophication while conditions at the two Rozmberk sites indicate a slow
er but longer lasting eutrophication. Owing to continuous heavy organic loa
ding, Rozmberk West represents a hypertrophic site characterised by the hig
hest levels of organic matter and associated characteristics (soil C, N, P,
K, dissolved P), but also by the most severe lack of oxygen of the three s
ites. (C) 2001 Elsevier Science B.V. All rights reserved.