DARK WELL‐DRAINED SOILS OF TUNDRA REGIONS IN WESTERN ALASKA
Summary Four dark well‐drained soils in tundra areas near the Bering Sea coast of Alaska have similar morphology, but physical and chemical properties reflect those of the parent materials. Three of the soils are extremely acid and have low base‐status. These, together with comparable soils in the a...
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Online Access: | http://dx.doi.org/10.1111/j.1365-2389.1966.tb01472.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1365-2389.1966.tb01472.x http://onlinelibrary.wiley.com/wol1/doi/10.1111/j.1365-2389.1966.tb01472.x/fullpdf |
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crwiley:10.1111/j.1365-2389.1966.tb01472.x 2024-06-02T08:01:52+00:00 DARK WELL‐DRAINED SOILS OF TUNDRA REGIONS IN WESTERN ALASKA RIEGER, S. 1966 http://dx.doi.org/10.1111/j.1365-2389.1966.tb01472.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1365-2389.1966.tb01472.x http://onlinelibrary.wiley.com/wol1/doi/10.1111/j.1365-2389.1966.tb01472.x/fullpdf en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Journal of Soil Science volume 17, issue 2, page 264-273 ISSN 0022-4588 journal-article 1966 crwiley https://doi.org/10.1111/j.1365-2389.1966.tb01472.x 2024-05-03T10:44:14Z Summary Four dark well‐drained soils in tundra areas near the Bering Sea coast of Alaska have similar morphology, but physical and chemical properties reflect those of the parent materials. Three of the soils are extremely acid and have low base‐status. These, together with comparable soils in the arctic and in high mountains at lower latitudes, are classified as Cryumbrepts. One, from basic rock, with slight acidity and fairly high base‐status is classified as a Cryoboroll. These soils have some characteristic in common with Cryandepts and Cryorthods of adjacent areas, but can readily be distinguished from them in the field. Article in Journal/Newspaper Arctic Bering Sea Tundra Alaska Wiley Online Library Arctic Bering Sea Journal of Soil Science 17 2 264 273 |
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Wiley Online Library |
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crwiley |
language |
English |
description |
Summary Four dark well‐drained soils in tundra areas near the Bering Sea coast of Alaska have similar morphology, but physical and chemical properties reflect those of the parent materials. Three of the soils are extremely acid and have low base‐status. These, together with comparable soils in the arctic and in high mountains at lower latitudes, are classified as Cryumbrepts. One, from basic rock, with slight acidity and fairly high base‐status is classified as a Cryoboroll. These soils have some characteristic in common with Cryandepts and Cryorthods of adjacent areas, but can readily be distinguished from them in the field. |
format |
Article in Journal/Newspaper |
author |
RIEGER, S. |
spellingShingle |
RIEGER, S. DARK WELL‐DRAINED SOILS OF TUNDRA REGIONS IN WESTERN ALASKA |
author_facet |
RIEGER, S. |
author_sort |
RIEGER, S. |
title |
DARK WELL‐DRAINED SOILS OF TUNDRA REGIONS IN WESTERN ALASKA |
title_short |
DARK WELL‐DRAINED SOILS OF TUNDRA REGIONS IN WESTERN ALASKA |
title_full |
DARK WELL‐DRAINED SOILS OF TUNDRA REGIONS IN WESTERN ALASKA |
title_fullStr |
DARK WELL‐DRAINED SOILS OF TUNDRA REGIONS IN WESTERN ALASKA |
title_full_unstemmed |
DARK WELL‐DRAINED SOILS OF TUNDRA REGIONS IN WESTERN ALASKA |
title_sort |
dark well‐drained soils of tundra regions in western alaska |
publisher |
Wiley |
publishDate |
1966 |
url |
http://dx.doi.org/10.1111/j.1365-2389.1966.tb01472.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1365-2389.1966.tb01472.x http://onlinelibrary.wiley.com/wol1/doi/10.1111/j.1365-2389.1966.tb01472.x/fullpdf |
geographic |
Arctic Bering Sea |
geographic_facet |
Arctic Bering Sea |
genre |
Arctic Bering Sea Tundra Alaska |
genre_facet |
Arctic Bering Sea Tundra Alaska |
op_source |
Journal of Soil Science volume 17, issue 2, page 264-273 ISSN 0022-4588 |
op_rights |
http://onlinelibrary.wiley.com/termsAndConditions#vor |
op_doi |
https://doi.org/10.1111/j.1365-2389.1966.tb01472.x |
container_title |
Journal of Soil Science |
container_volume |
17 |
container_issue |
2 |
container_start_page |
264 |
op_container_end_page |
273 |
_version_ |
1800746363522121728 |