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Abstrakty
The work presents some properties of eutrophic fen soils and the impact of their spatial location, the kind of bedrock and oxygen concentration in fen feed-water. The depth of peat horizons and the degree of peat decomposition in these horizons depends on the gradient of the land and the oxygen levels in the waters feeding the fens. The calcium carbonate content in the soils studied and their pH depended on the kind of bedrock on which the soil was formed.
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Tom
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Opis fizyczny
p.39-47,fig.,ref.
Twórcy
autor
- Agricultural University of Krakow, Al.Mickiewicza 21, 31-120 Krakow, Poland
autor
Bibliografia
Typ dokumentu
Bibliografia
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Identyfikator YADDA
bwmeta1.element.agro-article-38ca8843-a9d7-4a72-b34f-0f0ec21874bd