INFLUENCE OF PRECIPITATION COMPOSITION ON THE CHEMISTRY OF STREAMS DRAINING FROM PEAT EXAMINED USING NA-CA-MG RATIO

It is hypothesised that, since precipitation chemistry regulates the c onstitution of the base cations occupying the cation exchange sites of peat soils, and the latter in turn directly regulates the relative ab undance of the corresponding base cations in drainage waters, the rati os of base cations in precipitation and drainage waters from peats sho uld be very similar. The hypothesis is confirmed using data for 45 str eams in western Scotland sampled under baseflow conditions, and for th ree streams in northeastern Scotland sampled along their length under baseflow conditions and also throughout a sequence of three successive storms. During the latter, as the soils became progressively wetter, and flow through or over surface organic horizons started to make an i ncreasing relative contribution to total discharge, the difference bet ween cation ratios in precipitation and river water was reduced. The e ffects of changing hydrological pathway in the three catchments were c onfirmed by changes in Al:Ca:Mg ratios between baseflow and storm wate r samples. (C) 1997 Elsevier Science Ltd.