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Titlebook: Acidic Precipitation; Soils, Aquatic Proce S. A. Norton,S. E. Lindberg,A. L. Page Book 1990 Springer Science+Business Media New York 1990 E

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Hans Joachim Schwanitz M.D., Ph.D.nions associated with strong acids on the chemical composition of the soil solution, as they are likely to be highly nonlinear with respect to the capacity factors. These include pH, aluminum mobilization, and loss of alkalinity in the soil solution, which in turn may result in acidification of drai
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John Rawles BSc, MB, BS, FRCP, FRCP (Edin)ly as much as 0.5 to 1.5 pH units. No acidification trends were observed in regions currently receiving low deposition of strong acids (e.g., Rocky Mountains and Sierra Nevada in the western United States, northwestern Norway, and northwestern Scotland). Slight or no trends toward decreasing pH were
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Front Matterheast Asian countries and China and the transboundary haze problem emanating from Indonesia. The efforts to manage each of them are imagined as constituting a mediation regime, and its effectiveness is assessed in terms of good governance. Among the findings of the book is that the measures of manoe
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