Abstract
A b s t r a c t. The water conductivity of arctic zone soils derived in different micro-relief forms was determined. The greatest water conductivity at the 0-5 cm depth for the higher values of water potentials (> -7 kJ m -3 ) was shown by tundra polygons (Brunic-Turbic Cryosol, Arenic) – 904-0.09 cm day -1 , whereas the lowest were exhibited by Turbic Cryosols – 95-0.05 cm day -1 . Between -16 and -100 kJ m -3
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