Effects of waters of different origin on the formation of intramoraine peatbog habitat near Wilkowo

Great differences were discovered in the trophism of habitats between the boundary zone, formed mainly under the influence of rich delluvial waters, and the middle zone where the effect of these waters decreases and that of precipitation waters increases. Periodically, delluvial flooded also the mid...

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Published inZeszyty Naukowe Akademii Rolniczej we Wroclawiu. Rolnictwo (Poland) no. 300
Main Authors Stepa, S, Tomaszewska, K, Wojtun, B. (Akademia Rolnicza, Wroclaw (Poland). Katedra Botaniki i Fizjologii Roslin)
Format Journal Article
LanguagePolish
Published 1996
Subjects
AGUA DE LLUVIA
AGUA DEL SUELO
AGUAS SUBTERRANEAS
CARACTERISTICAS DEL SITIO
COMMUNAUTE VEGETALE
COMUNIDADES VEGETALES
EAU DE PLUIE
EAU DU SOL
EAU SOUTERRAINE
FACTEUR LIE AU SITE
GROUNDWATER
PEAT SOILS
PEATLAND
PLANT COMMUNITIES
PLANT WATER RELATIONS
POLAND
POLOGNE
POLONIA
RAINWATER
RELACIONES PLANTA AGUA
RELATION PLANTE EAU
SITE FACTORS
SOIL WATER
SOL TOURBEUX
SUELO TURBOSO
TOURBIERE
TURBERA
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Summary:Great differences were discovered in the trophism of habitats between the boundary zone, formed mainly under the influence of rich delluvial waters, and the middle zone where the effect of these waters decreases and that of precipitation waters increases. Periodically, delluvial flooded also the middle part of the peatbog, leaving behind alluvial deposits. In view of the great importance of the object for the natural landscape and in order to preserve the high-bog plant remnats on the deep peat deposit of interesting stratigraphic build, it is advisable to return the bog to its natural state. For that end it would suffice to stop renewing the boundary trench
Bibliography:F40
1998000265
F70
ISSN:0137-1959