Observations on the corrosion potential in alpine caves

Several hundreds of water samples have been collected in Austrian alpine caves. It was possible to differientiate between karst waters in common sense and condensing waters. Due to lower temperatures at higher elevations the soil-biological activity is decreasing, hypercompensating the higher solubi...

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Bibliographic Details
Published inBulletin (Société géographique de Liège) Vol. 29
Main Author Pavuza, R. (Museum of Natural History, Vienna (Austria). Karstund Hoehlenkundliche Abteilung)
Format Journal Article
LanguageEnglish
Published Liege (Belgium) La Societe Geographique de Liege 1993
Université de Liège
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Summary:Several hundreds of water samples have been collected in Austrian alpine caves. It was possible to differientiate between karst waters in common sense and condensing waters. Due to lower temperatures at higher elevations the soil-biological activity is decreasing, hypercompensating the higher solubility of CO2. Therefore, the carbonate dissolution is lower. The opposite effect can be observed with the condensing waters as there is a higher uptake of CO2 during condensation according to lower condensing temperatures in high alpine caves. Thus the mineralisation of condensing waters tends to increase with altitude. As the dissolution of common karst waters is more than compensated by the increase of precipitation with altitude, it can be concluded on the whole that a higher carbonate-dissolution is currently taking place in high alpine karst regions.
Bibliography:9401442
P10
29 (1993/2) - Spéléologie physique et karstologie
ISBN:2872980040
9782872980048
ISSN:0770-7576
2507-0711