In this experimental study, we simulated the effects of different river flo
oding regimes on soil nutrient availability, decomposition and plant produc
tion in floodplain grasslands. This was done to investigate the influences
of soil water contents on nutrient cycling. Water levels were manipulated i
n mesocosms with intact soil turfs from two French floodplain grasslands. T
hree water levels were established: a 'wet' (water level at the soil surfac
e), an 'intermediate' (water level at -20 cm) and a 'dry' treatment (water
level at -120 cm). With increasing soil moisture, soil pH became more neutr
al, while redox-potential and oxygen concentration decreased. The 'dry' tre
atment showed much lower values for process rates in soil and vegetation th
an the 'intermediate' and 'wet' treatments. Regressions showed that soil C-
evolution and N-mineralization were positively related to soil moisture con
tent. Not all mineralized N was available for plant uptake in the wet treat
ment, as a considerable part was denitrified here. Denitrification was espe
cially high as soil water contents increased to levels above field capacity
, where redox-potentials sharply dropped. Further, soil P availability was
higher under wet conditions. In the 'dry' treatment, soil water content was
close to the wilting point and plant production was low. In the 'intermedi
ate' treatment, plant production was most likely limited by nitrogen. The '
wet' treatment did not result in a further increase in plant production. Da
m construction and river bed degradation can result in lower river levels a
nd summer drought on floodplains. This experimental study suggests that sum
mer drought on floodplain soils reduces decomposition of soil organic matte
r, nutrient availability, denitrification, plant production and nutrient up
take. This can affect the capacity of floodplains to remove or retain nutri
ents from river water in a negative way. (C) 2000 Editions scientifiques et
medicales Elsevier SAS.