Determination of thе soil-permafrost border in two maritime Antarctic regions on thе base of vertical electric sounding data

The deepness of soil-permafrost layer was measured bу vertical electrical resistivity sounding. It has been revealed that the deepness of active layer оn the Point Thomas oasis , King George lsland is in average about 100-150 cm, while оn the Argentine lslands it is 40-50 cm, which is caused bу clim...

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Bibliographic Details
Main Authors: E.V. Abakumov, I. Yu. Parnikoza
Format: Article
Language:English
Published: State Institution National Antarctic Scientific Center 2016-01-01
Series:Український антарктичний журнал
Subjects:
Online Access:http://uaj.uac.gov.ua/index.php/uaj/article/view/182