Agricultural pollution is a matter of political and scientific concern throughout the world. Intensive agriculturecan cause nutrient contamination of groundwater and surface water. Nutrient pollution causes eutrophicationin freshwater and estuarine ecosystems. A secondary effect of agricultural intensification is river acidification.Oxidation of chemical fertilizers such as ammonium (NH4+) to nitrate (NO3-) produces H+ ions that causeleaching of cations from soil and deeper material to maintain charge balance. Monitoring of various rivers inBrittany (western France) revealed that agriculture intensification has led to increased cation export starting in the1980s. From the cation ratios, we deduced that cation increase comes approximately equally from dissolution ofcarbonate added to soil (liming practices) and silicate dissolution. Cation export represented about 30% of the soilcation exchange potential. If compensated by liming, it may constitute a non-negligible source to atmosphericCO2 (Aquilina et al., 2012).We further investigated the potential for silicate dissolution through the use of groundwater dating in various sitesof Brittany. Coupling chemical analyses to groundwater ages in a large range of aquifers and a large range ofdepths (down to 110m) allowed us to reconstruct a chronicle for the last 50 yrs of the cation concentrations ofgroundwater. It clearly shows a contemporaneous increase in sodium and nitrate and a decrease in calcium, withthe most dramatic changes occurring during the 70s and 80s.Using groundwater dating, we were also able to determine a silica production geochronometer. A tight and linearrelationship between silica concentration and groundwater age (Figure) was observed and allowed a productionrate in groundwater to be determined. Except for short residence-times (Kerrien), the silica production rate fordifferent granitic catchments was consistent, ranging from 0.3 to 0.4 mg.L-1.yr-1.To assess the role of anthropogenic activity in silica production rate, we compared production rates from Brittanywith catchments in the Vosges Mountains, a relatively pristine area. Dissolution rates were much higher in theBrittany catchments, indicating the effect of human activities on chemical weathering and cation export at thecatchment scale.Aquilina L. et al., 2012 - Long-term effects of high nitrogen loads on cation and carbon riverine export inagricultural catchments. Env. Sci & Technology 46-17, 9447-9455..