@misc{Kruk_Marek_Types_1987,
 author={Kruk, Marek},
 editor={Polska Akademia Nauk. Instytut Ekologii},
 copyright={Creative Commons Attribution BY 3.0 PL license},
 address={Warszawa},
 howpublished={online},
 year={1987},
 language={eng},
 abstract={Several hydrological types of basins without drainage have been identified. An important relationship has been found between the magnitude of seasonal fall of the water level in a mire situated in a basin without run off and the proportion of the mire surface area in the total area of the basin. In a hummocky lakeland landscape there are basins with mires in them, as well as whole areas without surface drainage where seasonal retention of water and its long-term storage are favoured to a variable extent.},
 type={Text},
 title={Types of basins without drainage and factors affecting the water cycle in them in the present-day landscape of the Masurian Lakeland},
 URL={http://rcin.org.pl/miiz/Content/80101/PDF/WA058_87749_P2840-T35_Eko-Pol-A-Nr-3-4.pdf},
 volume={35},
 number={3-4},
 journal={Ekologia Polska},
 publisher={Polish Scientific Publishers},
 keywords={basin without drainage (run off), mire, minerotrophic fens, ombrotrophic bogs, ground-water table, water retention},
}