During the 1994-1997 water years, a hydrogeological study was carried out o
n the alluvial aquifer of Sparta in the Peloponnese, where the concentratio
n of nitrate ions in groundwater, as NO3- is well over the highest recommen
ded WHO limits of 50 mg l(-). Under specific hydrological and chemical cond
itions with high amounts of dissolved oxygen, the migration of nitrate ions
in the aquifer, seems to be unaffected by any hydrological process, chemic
al substance or reaction. Examination of the relationship between nitrate c
oncentration and aquifer properties shows that maximum nitrate concentratio
n values follow the main axes of groundwater movement, while zones of incre
ased recharge coincide with zones of diluted nitrate concentration.
Profiles of the evolution of chemical parameters vs depth, show that the ma
in process causing nitrate increase in groundwater, is the oxidation of amm
onia originating from the rapid leaching of inorganic fertilizers applied t
o cultivated areas. (C) 2000 Elsevier Science Ltd. All rights reserved.