Current annual measurements of the average pH of precipitation in the northern hemisphere range from about 4.0 to 7.0. The lower, highly acidic values occur primarily over and immediately downwind of industrialized areas in northeastern North America and Europe. Higher pH values are found over less industrialized regions where the atmosphere contains larger amounts of alkaline dust. The primary cause of low pH in precipitation over northeastern North America is sulphuric acid (H2SO4) resulting from industrial and urban emissions of sulphur dioxide (SO2). Nitric acid (HNO3) generated from emissions of nitrogen oxides (NOx) is a significant contributing factor in this region. Current annual emissions of SO2 amount to about 20 million t in the US and about 2 million t in Canada. Coal-fired thermal electric power plants produce about 70% of US emissions and about 20% of Canadian emissions. Nonferrous smelters, producing such metals as nickel and copper, account for about 50% of Canada's SO2 emissions. The acid rain precursors, SO2 and NOx, can be transported thousands of kilometres through the atmosphere, returning to earth as dry deposition or in wet acid form.
Acidity Scale The pH scale measures the degree of acidity (artwork by Michael Lee). |
read more
No comments:
Post a Comment