Both the inorganic nitrogen pool and environmental factors controlling
the spatial and temporal variability of nitrite concentration were mo
nitored in the River Lahn at two sites with different sediment composi
tion (coarse gravel/fine gravel and fine sediments). The field studies
were conducted both in the free flowing and the interstitial water. A
ccumulation of nitrite in the River Lahn occurred in correlation to wa
ter temperatures over a range of 13 degrees C during the warmer season
and coincided with high concentrations of ammonium. An annual as well
as daily variations of the concentrations could be determined with th
e highest data in the summer and lower values at the beginning of the
colder season. Maxima were measured from May until July 1993, especial
ly in the hours around noon, sometimes in ecotoxicologically critical
concentrations (greater than or equal to 0.3 mg NO(2)(-)Nl(-1)). A spa
tial variability depending on the depth of the interstitial strata (8-
28 cm) was only found at a muddy study site. Here the concentration of
nitrite was four to sixfold of that in the free flowing water. At the
other study-site consisting of coarse gravel, no accumulation of nitr
ite could be detected. In order too assess the importance of abiotic f
actors, e.g. temperature, on the nitrification process, laboratory exp
eriments were also conducted. Nitrifying biofilms of a defined substra
te from the River Lahn were used as a model for patterns and processes
in the river-bed. The results indicate a critical temperature domain
(16-22 degrees C) in which the activity of Nitrobacter seems to be mor
e inhibited than the nitritation by Nitrosomonas, resulting in a trans
ient build-up of nitrite. (C) 1998 Elsevier Science Ltd. All rights re
served.