The effect of drought between summer 1995 and 1997 on stream and river nitr
ate concentrations was investigated using sites close to the long-running m
eteorological station in Oxford, UK. Nitrate concentrations in the River Wi
ndrush were relatively low during the drought, but after it had ended reach
ed the highest level since records began in 1973. The low concentrations du
ring the drought probably reflect a reduced contribution from agricultural
runoff. High nitrate concentrations were found in a field drain at Wytham E
nvironmental Change Network site during and after the drought, but discharg
e was greatly reduced. A woodland stream at Wytham had much lower nitrate c
oncentrations than the field drain but these similarly increased during and
after the drought. There was evidence that both a concentrating effect of
low water volumes and enhanced soil nitrogen mineralization and nitrificati
on rates were causing concentrations to rise. The effects of mineralization
and nitrification were more important in woodland than agricultural land.
Nitrate load over the course of a year was determined largely by discharge,
but steeper gradients for the relationship between cumulative load and cum
ulative discharge were seen during and after the drought than before, refle
cting the higher concentrations.