文摘
Annual volume-weighted mean (VWM) concentrations in rainwater collected at La Castanya (LC, Montseny Mountains, NE Spain) were analysed from 1983 to 2000 to study the temporal trends in precipitation chemistry, and the causes behind the changes. A significant positive correlation was found between annual rainwater SO4p>2−p> concentrations at LC and Spanish SO2 emissions (r=0.73, P=0.0008) both decreasing remarkably during this period. Rainwater alkalinity increased during the period, shifting from negative values at the beginning (VWM in the 5 initial years=−2.7μeqlp>−1p>) to alkaline values in recent years (VWM in the 5 final years=18.0μeqlp>−1p>). Stepwise regression analysis indicated that 88 % of the variation of alkalinity could be accounted for by the variability of non-marine Cap>2+p> and non-marine SO4p>2−p>, with a more prominent dependence on Cap>2+p>.