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Terminologia dotycząca definiowania obszarów zabagnionych : propozycja jej uporządkowania

Bajkiewicz-Grabowska E.

Przegląd Geofizyczny

2005

Z. 1-2

91-102

Boggy areas are the most productive biological ecosystems and appear at all latitudes, ranging from the tundra, temperate and tropic latitudes to the equator. Boggy areas as hydrosphere elements are not only the object of study of such Earth sciences as hydrology, geography, soil geography, pedology or land melioration, but also of biological sciences. This is the reason why the terminology of such objects tends to vary and is often used in a wrong way. Our suggestion is to accept that the synonym of a boggy area is a bog. In case when a bog is strongly wetted, typical boggy peat-forming processes occur and the peat deposits are deep enough, such a bog should be called a. peatbog. When wetting of the bog is unsteady and palustrine, gley or warp processes are the most important in soil formation, then such a bog should be called a marsh. When a bog is situated in the shore lake zone and a sludge blanket spreads from the shore to the centre of the lake or when it is an overgrown water reservoir where water or semi-liquid lake deposits are under a plant blanket, then such bog should be called a quaking bog. The term "bog" is synonymous with "wetland", although a bog is a kind of wetland.