Observations on Net Assimilation Rates in Arctic Environments: With two Figures in the Text

Examination of the net assimilation rate ( E ) during the growing season in arctic regions by a detached-leaf method revealed no differences between species or with soil richness, but showed a reduction of E with exposure to wind–probably resulting from cooling–and a tendency for E to fall towards t...

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Main Author: WILSON, J. WARREN
Format: Text
Language:English
Published: Oxford University Press 1960
Subjects:
Online Access:http://aob.oxfordjournals.org/cgi/content/short/24/3/372
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spelling fthighwire:oai:open-archive.highwire.org:annbot:24/3/372 2023-05-15T14:42:11+02:00 Observations on Net Assimilation Rates in Arctic Environments: With two Figures in the Text WILSON, J. WARREN 1960-07-01 00:00:00.0 text/html http://aob.oxfordjournals.org/cgi/content/short/24/3/372 en eng Oxford University Press http://aob.oxfordjournals.org/cgi/content/short/24/3/372 Copyright (C) 1960, Oxford University Press Articles TEXT 1960 fthighwire 2007-06-24T04:58:03Z Examination of the net assimilation rate ( E ) during the growing season in arctic regions by a detached-leaf method revealed no differences between species or with soil richness, but showed a reduction of E with exposure to wind–probably resulting from cooling–and a tendency for E to fall towards the later part of the growing season. E generally lay in the range 0·5 to o·8 g./dm.2/week. E for detached leaves ignores respiratory losses in other parts of the plant and is not comparable with E for whole plants; failure to appreciate this confused a previous comparison of E under arctic and temperate environments. E for detached leaves in temperate summer conditions is normally around 1·1 to 1·5 g./dm.2/week. Thus E is reduced in arctic environments to about half the value in temperate conditions. This reduction is due mainly to the cold climate. Text Arctic HighWire Press (Stanford University) Arctic
institution Open Polar
collection HighWire Press (Stanford University)
op_collection_id fthighwire
language English
topic Articles
spellingShingle Articles
WILSON, J. WARREN
Observations on Net Assimilation Rates in Arctic Environments: With two Figures in the Text
topic_facet Articles
description Examination of the net assimilation rate ( E ) during the growing season in arctic regions by a detached-leaf method revealed no differences between species or with soil richness, but showed a reduction of E with exposure to wind–probably resulting from cooling–and a tendency for E to fall towards the later part of the growing season. E generally lay in the range 0·5 to o·8 g./dm.2/week. E for detached leaves ignores respiratory losses in other parts of the plant and is not comparable with E for whole plants; failure to appreciate this confused a previous comparison of E under arctic and temperate environments. E for detached leaves in temperate summer conditions is normally around 1·1 to 1·5 g./dm.2/week. Thus E is reduced in arctic environments to about half the value in temperate conditions. This reduction is due mainly to the cold climate.
format Text
author WILSON, J. WARREN
author_facet WILSON, J. WARREN
author_sort WILSON, J. WARREN
title Observations on Net Assimilation Rates in Arctic Environments: With two Figures in the Text
title_short Observations on Net Assimilation Rates in Arctic Environments: With two Figures in the Text
title_full Observations on Net Assimilation Rates in Arctic Environments: With two Figures in the Text
title_fullStr Observations on Net Assimilation Rates in Arctic Environments: With two Figures in the Text
title_full_unstemmed Observations on Net Assimilation Rates in Arctic Environments: With two Figures in the Text
title_sort observations on net assimilation rates in arctic environments: with two figures in the text
publisher Oxford University Press
publishDate 1960
url http://aob.oxfordjournals.org/cgi/content/short/24/3/372
geographic Arctic
geographic_facet Arctic
genre Arctic
genre_facet Arctic
op_relation http://aob.oxfordjournals.org/cgi/content/short/24/3/372
op_rights Copyright (C) 1960, Oxford University Press
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