<abstract xml:lang="en" xmlns="http://www.w3.org/1999/xhtml"><p>The succession of vegetation on acidic sandy fields after abandonment was studied and obtained results were compared with similar data from eastern part of Europe. The vegetation changes head towards oligotrophic <italic>Corynephorus</italic>-grasslands, because nutrients from the upper layer of soils are gradually washed out. Dry, occasionally blowing sand enables the growth of psammophytes very well. The paper compares the succession models on abandoned sandy fields, and semi-natural acidic sandy dunes in western part of Slovakia, southern Moravia, Hungary and Croatia. In spite of amazing similarities, some differences are displayed using spectra of life forms and presentation of weeds.</p></abstract>

The succession of vegetation on acidic sandy fields after abandonment was studied and obtained results were compared with similar data from eastern part of Europe. The vegetation changes head towards oligotrophic Corynephorus-grasslands, because nutrients from the upper layer of soils are gradually washed out. Dry, occasionally blowing sand enables the growth of psammophytes very well. The paper compares the succession models on abandoned sandy fields, and semi-natural acidic sandy dunes in western part of Slovakia, southern Moravia, Hungary and Croatia. In spite of amazing similarities, some differences are displayed using spectra of life forms and presentation of weeds.

Succession Model with <italic>Corynephorus Canescens</italic> in Abandoned Sandy Fields (W Slovakia)

Institute of Botany, Slovak Academy of Sciences, Dúbravská cesta 9, SK-845 23 Bratislava, Slovak Republic

Hacquetia

Succession Model with  in Abandoned Sandy Fields (W Slovakia)

The succession of vegetation on acidic sandy fields after abandonment was studied and obtained results were compared with similar data from eastern part of...

Succession Model with Corynephorus Canescens in Abandoned Sandy Fields (W Slovakia)

Publié en ligne: 21 mai 2012

Pages: 5 - 15

DOI: https://doi.org/10.2478/v10028-012-0001-6

Mots clés
obdelana tla, celinske peščene dine, pleveli, Borská nížina

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