The hydrology of a Sphagnum mire in the southern Alps was studied during the 1991 growing season by measuring at regular intervals the depth to the water table in a number of water gauges. The thickness of the acrotelm and the thickness of the aerobic layer decrease from dry to wet sites, but the differences between them are not constant along the water-table gradient, being wider the higher are the microsites.
Delimitation of the aerobic peat layer in a Sphagnum mire on the southern Alps
BRAGAZZA, Luca
1996
Abstract
The hydrology of a Sphagnum mire in the southern Alps was studied during the 1991 growing season by measuring at regular intervals the depth to the water table in a number of water gauges. The thickness of the acrotelm and the thickness of the aerobic layer decrease from dry to wet sites, but the differences between them are not constant along the water-table gradient, being wider the higher are the microsites.File in questo prodotto:
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