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Science 5 August 1983: Vol. 221. no. 4610, pp. 520 - 525 DOI: 10.1126/science.221.4610.520
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Articles
Acid Rain on Acid Soil: A New Perspective
Edward C. Krug 1 and
Charles R. Frink 2
1 Assistant soil scientist in the Department of Soil and Water, The Connecticut Agricultural Experiment Station, New Haven 06504.
2 Chief of the Department of Soil and Water and vice director of The Connecticut Agricultural Experiment Station.
Acid rain is widely believed to be responsible for acidifying soil and water in areas of North America and northern Europe. However, factors commonly considered to make landscapes susceptible to acidification by acid rain are the same factors long known to strongly acidify soils through the natural processes of soil formation. Recovery from extreme and widespread careless land use has also occurred in regions undergoing acidification. There is evidence that acidification by acid rain is superimposed on long-term acidification induced by changes in land use and consequent vegetative succession. Thus, the interactions of acid rain, acid soil, and vegetation need to be carefully examined on a watershed basis in assessing benefits expected from proposed reductions in emissions of oxides of sulfur and nitrogen.
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- C. NEAL, C. J. SMITH, J. WALLS, and C. S. DUNN (1986)
Journal of the Geological Society
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- Mineral weathering processes in podzolic soils on granitic materials and their implications for surface water acidification.
- M. J. WILSON (1986)
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- Acid Rain and Soil Chemistry.
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