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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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 |
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HighWire Press (Stanford University) |
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English |
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Articles WILSON, J. WARREN Observations on Net Assimilation Rates in Arctic Environments: With two Figures in the Text |
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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 |
_version_ |
1766313888256622592 |