Some notes on clay minerals in Podzol profiles in Fennoscandia
Montmorillonite is found to be a predominant clay mineral in the < 2/z fraction of the A2 horizon of podzol profiles in Fennoscandia, even when these are only 300 years old. Irt fractions between 2/ ~ and 20/ ~ vermiculite and. hydrobiotite predominate, but are rarely detected in the fraction coa...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.559.8983 2023-05-15T16:11:35+02:00 Some notes on clay minerals in Podzol profiles in Fennoscandia O. Gjems The Pennsylvania State University CiteSeerX Archives 1960 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.559.8983 http://www.minersoc.org/pages/Archive-CM/Volume_4/4-24-208.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.559.8983 http://www.minersoc.org/pages/Archive-CM/Volume_4/4-24-208.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.minersoc.org/pages/Archive-CM/Volume_4/4-24-208.pdf text 1960 ftciteseerx 2016-01-08T11:57:20Z Montmorillonite is found to be a predominant clay mineral in the < 2/z fraction of the A2 horizon of podzol profiles in Fennoscandia, even when these are only 300 years old. Irt fractions between 2/ ~ and 20/ ~ vermiculite and. hydrobiotite predominate, but are rarely detected in the fraction coarser than 20/z. Vermiculite and hydrobiotite are also found in the finer fractions of the B horizon, but are only rarely detected in the C horizon where their presence is apparently due to contamination with inter-glacial or older products of weathering. The presence of kaolinite in some profiles is explicable in the same way. Text Fennoscandia Unknown |
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ftciteseerx |
language |
English |
description |
Montmorillonite is found to be a predominant clay mineral in the < 2/z fraction of the A2 horizon of podzol profiles in Fennoscandia, even when these are only 300 years old. Irt fractions between 2/ ~ and 20/ ~ vermiculite and. hydrobiotite predominate, but are rarely detected in the fraction coarser than 20/z. Vermiculite and hydrobiotite are also found in the finer fractions of the B horizon, but are only rarely detected in the C horizon where their presence is apparently due to contamination with inter-glacial or older products of weathering. The presence of kaolinite in some profiles is explicable in the same way. |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
O. Gjems |
spellingShingle |
O. Gjems Some notes on clay minerals in Podzol profiles in Fennoscandia |
author_facet |
O. Gjems |
author_sort |
O. Gjems |
title |
Some notes on clay minerals in Podzol profiles in Fennoscandia |
title_short |
Some notes on clay minerals in Podzol profiles in Fennoscandia |
title_full |
Some notes on clay minerals in Podzol profiles in Fennoscandia |
title_fullStr |
Some notes on clay minerals in Podzol profiles in Fennoscandia |
title_full_unstemmed |
Some notes on clay minerals in Podzol profiles in Fennoscandia |
title_sort |
some notes on clay minerals in podzol profiles in fennoscandia |
publishDate |
1960 |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.559.8983 http://www.minersoc.org/pages/Archive-CM/Volume_4/4-24-208.pdf |
genre |
Fennoscandia |
genre_facet |
Fennoscandia |
op_source |
http://www.minersoc.org/pages/Archive-CM/Volume_4/4-24-208.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.559.8983 http://www.minersoc.org/pages/Archive-CM/Volume_4/4-24-208.pdf |
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Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
_version_ |
1765996728914280448 |