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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Main Author: O. Gjems
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Published: 1960
Subjects:
Fennoscandia
Online Access: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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spelling 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
institution Open Polar
collection Unknown
op_collection_id 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
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
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