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 |
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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 |
| _version_ | 1818173524145078272 |
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| author | E.V. Abakumov I. Yu. Parnikoza |
| author_facet | E.V. Abakumov I. Yu. Parnikoza |
| author_sort | E.V. Abakumov |
| collection | DOAJ |
| description | 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 climatic conditions. Weak soils of the Argentine Islands are connected to permafrost via the massive rock, while in case of Point Thomas oasis (King-George Island) fine-coarsy gravel soils are underlayed directly bу permafrost. |
| first_indexed | 2024-12-11T19:29:52Z |
| format | Article |
| id | doaj.art-86168862733d4ac89e48c31caba875f7 |
| institution | Directory Open Access Journal |
| issn | 1727-7485 2415-3087 |
| language | English |
| last_indexed | 2024-12-11T19:29:52Z |
| publishDate | 2016-01-01 |
| publisher | State Institution National Antarctic Scientific Center |
| record_format | Article |
| series | Український антарктичний журнал |
| spelling | doaj.art-86168862733d4ac89e48c31caba875f72022-12-22T00:53:18ZengState Institution National Antarctic Scientific CenterУкраїнський антарктичний журнал1727-74852415-30872016-01-011413814210.33275/1727-7485.14.2015.182182Determination of thе soil-permafrost border in two maritime Antarctic regions on thе base of vertical electric sounding dataE.V. Abakumov0I. Yu. Parnikoza1Saint-Petersburg State University, Saint-Petersburg, RussiaInstitute of Molecular Biology and Genetics, National Academy of Sciences of Ukraine, Zabolotnogo Str., 150, Kyiv, 03680, UkraineThe 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 climatic conditions. Weak soils of the Argentine Islands are connected to permafrost via the massive rock, while in case of Point Thomas oasis (King-George Island) fine-coarsy gravel soils are underlayed directly bу permafrost.http://uaj.uac.gov.ua/index.php/uaj/article/view/182electric resistivitypermafrostsoilsmaritime antarcticaactive layer |
| spellingShingle | E.V. Abakumov I. Yu. Parnikoza Determination of thе soil-permafrost border in two maritime Antarctic regions on thе base of vertical electric sounding data Український антарктичний журнал electric resistivity permafrost soils maritime antarctica active layer |
| title | Determination of thе soil-permafrost border in two maritime Antarctic regions on thе base of vertical electric sounding data |
| title_full | Determination of thе soil-permafrost border in two maritime Antarctic regions on thе base of vertical electric sounding data |
| title_fullStr | Determination of thе soil-permafrost border in two maritime Antarctic regions on thе base of vertical electric sounding data |
| title_full_unstemmed | Determination of thе soil-permafrost border in two maritime Antarctic regions on thе base of vertical electric sounding data |
| title_short | Determination of thе soil-permafrost border in two maritime Antarctic regions on thе base of vertical electric sounding data |
| title_sort | determination of thе soil permafrost border in two maritime antarctic regions on thе base of vertical electric sounding data |
| topic | electric resistivity permafrost soils maritime antarctica active layer |
| url | http://uaj.uac.gov.ua/index.php/uaj/article/view/182 |
| work_keys_str_mv | AT evabakumov determinationofthesoilpermafrostborderintwomaritimeantarcticregionsonthebaseofverticalelectricsoundingdata AT iyuparnikoza determinationofthesoilpermafrostborderintwomaritimeantarcticregionsonthebaseofverticalelectricsoundingdata |