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