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Extra resources for Atmospheric Chemistry: Report of the Dahlem Workshop on Atmospheric Chemistry, Berlin 1982, May 2 – 7
The pH values obtained are con- siderably higher than those either observed today in the 27 Factors Governing pH and Oxidation Capacity of Rain northeast US or calculated for 1955-56 (11) from charge balances. Geographical relation to sources of acid and basic emissions and the transport-transformatjon times from source locations are generally recognized to be among the factors governing pH of rain. hout further interpretation. , pH, metal ion, ligand, and complexes in both rain and aquatic systems depends on absolute input concentrations or acid-base components and redox components.
Tellus 31: 421-431. J. 1980. Spatial variations of acid precipitation in Southern California. Env. Sci. Technol. 15: 333-339. J. 1982. Chemical source, equilibrium and kinetic models of acid precipitation. In Energy and Environmental Chemistry: Acid Rain, ed. H. Keith, vol. 2. Ann Arbor: Ann Arbor Science. Dry and wet removal of sulphur Atmos. Env. 12: 349-362. J. Morgan (14) Od~n, S. 1976. The acidity problem - an outline of concepts. Water, Air, Soil Poll. ~: 137-166. J. 1979. The importance of atmospheric ozone and hydrogen peroxide in oxidizing sulfur dioxide in cloud and rainwater.
J. Soil Res. 2: 187-210. I. 1976. Rain as a source of fertilizer in Australia. Research Project Series No. 16. Victoria: Department of Agriculture. , and Rodhe, H. 1982. Factors controlling the acidity of natural rainwater. Nature 295: 683-685. A. 1978. Ionic composition of rain during sixteen convective showers. Atmos. Env. 12: 1991-1999. , ed. 1981. 9, Summary Report 1980. S. Department of Commerce. (9) Douglas, I. 1968. The effects of precipitation chemistry and catchment area lithology on the quality of river water in selected catchments in eastern Australia.