Príspevok k problematike veku a vývoja illimerizovaných pôd na Slovensku

Rok, strany: 1976, 310 - 322

The age and development of illimerized soils in Slovakia Is a result of interaction of soil-creating substrata, bioclimatic oscillations during Holocene and since the end of Atlantic also of antropical influences. The most favourable conditions for decalcification of soil-creating substrata were during the Atlantic, for illimerization during the Epiatlantic. Therefore, the age of the discussed soils most often varies within the span of 6,000 to 3,500 years. The period since Subatlantic till the present has been prevailingly favourable for medium intensive decalcification and illimerization, the result of which are further smaller areas of illimerized soils. The present results of antropic influences, depending on several factors, may be very different.

ISO 690:

Obr, F. 1976. Príspevok k problematike veku a vývoja illimerizovaných pôd na Slovensku. In Geografický časopis, vol. 28, no.4, pp. 310-322. 0016-7193.

APA:

Obr, F. (1976). Príspevok k problematike veku a vývoja illimerizovaných pôd na Slovensku. Geografický časopis, 28(4), 310-322. 0016-7193.

Vydavateľ: Geografický ústav SAV/Institute of Geography of the Slovak Academy of Sciences