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Chemical Transformations in a Snow Cover at Weissfluhjoch, Switzerland, Situated 2500 m.a.s.l.

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Part of the book series: NATO ASI Series ((ASIC,volume 211))

Abstract

During winter 1985/86 three profiles through a snow cover located at the Swiss Snow and Avalanche Research Institute Weissfluhjoch (Davos) at 2540 m.a.s.l. were analysed for the main chemical impurities including hydrogen peroxide. The concentration profiles of NO3 -, SO4 2-, Cl-, HCOO-, H+, NH4 +, Na+, K+ and Ca2+ do not change as long as the temperature in the snow field is below zero degree celsius. Only the H2O2 content decreases considerably. The disintegration rate depends mainly upon the availability of sunlight, thus photolysis is probably the most important decay process. Organic peroxides are not recorded in the snow.

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© 1987 D. Reidel Publishing Company

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Sigg, A., Neftel, A., Zürcher, F. (1987). Chemical Transformations in a Snow Cover at Weissfluhjoch, Switzerland, Situated 2500 m.a.s.l.. In: Jones, H.G., Orville-Thomas, W.J. (eds) Seasonal Snowcovers: Physics, Chemistry, Hydrology. NATO ASI Series, vol 211. Springer, Dordrecht. https://doi.org/10.1007/978-94-009-3947-9_15

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  • DOI: https://doi.org/10.1007/978-94-009-3947-9_15

  • Publisher Name: Springer, Dordrecht

  • Print ISBN: 978-94-010-8251-8

  • Online ISBN: 978-94-009-3947-9

  • eBook Packages: Springer Book Archive

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