Published May 1983 | Version public
Journal Article

Saurer Regen, eine Folge der Störung hydrogeochemischer Kreisläufe

  • 1. ROR icon Swiss Federal Institute of Aquatic Science and Technology
  • 2. ROR icon California Institute of Technology
  • 3. ROR icon University of Iowa

Abstract

The occurrence of acid precipitation in regions of the northern hemisphere results from the anthropogenic disturbance of cycles that couple land, water and atmosphere. The oxidation of C, S and N resulting mostly from fossil fuel burning rivals oxidation processes induced by photosynthesis; the acidity of rain is a consequence of these redox processes in the atmosphere and in the rain. In evaluating the impact of aqueous acidity upon the environment and vice versa, it is essential to distinguish between free H⁺ acidity and the H⁺ reservoir (base-neutralizing capacity). The acidification of lakes, streams and soils is influenced by hydrology, biota, geology and weathering rates.

Additional Information

© 1983 Springer. Diese Arbeit entstand, während J.J.M. und J.L.S. als Gastwissenschafter an der EAWAG/ETH weilten.

Additional details

Identifiers

Eprint ID
107124
DOI
10.1007/bf00405438
Resolver ID
CaltechAUTHORS:20201216-122930373

Related works

Describes
10.1007/bf00405438 (DOI)

Dates

Created
2020-12-16
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Updated
2021-11-16
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