Seasonal variation of δ18O and δ2H in leaf water of Fagus sylvatica L. and related water compartments

Copyright © 2018 Elsevier GmbH. All rights reserved.

Bibliographische Detailangaben
Veröffentlicht in:Journal of plant physiology. - 1979. - 227(2018) vom: 19. Aug., Seite 56-65
1. Verfasser: Plavcová, Lenka (VerfasserIn)
Weitere Verfasser: Hronková, Marie, Šimková, Marie, Květoň, Jiří, Vráblová, Martina, Kubásek, Jiří, Šantrůček, Jiří
Format: Online-Aufsatz
Sprache:English
Veröffentlicht: 2018
Zugriff auf das übergeordnete Werk:Journal of plant physiology
Schlagworte:Journal Article Fagus Irradiance Leaf water Seasonal course Soil Water isotopes Oxygen Isotopes Water 059QF0KO0R mehr... Deuterium AR09D82C7G
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100 1 |a Plavcová, Lenka  |e verfasserin  |4 aut 
245 1 0 |a Seasonal variation of δ18O and δ2H in leaf water of Fagus sylvatica L. and related water compartments 
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500 |a Date Completed 30.08.2018 
500 |a Date Revised 30.09.2020 
500 |a published: Print-Electronic 
500 |a Citation Status MEDLINE 
520 |a Copyright © 2018 Elsevier GmbH. All rights reserved. 
520 |a The study aims to assess variability in leaf water isotopic enrichment occurring in the field under natural conditions. We focused on seasonal variation and difference between sun-exposed and shaded leaves. Isotopic composition (δ18O, δ2H) of leaf water was monitored in a beech tree (Fagus sylvatica L.) growing in the forest-meadow ecotone together with δ18O (2H) of water compartments which are in close relation to this signal, namely twig and soil water. The sampling was carried out in approximately two-week intervals during five consecutive vegetation seasons. The δ18O (2H) data showed a distinct seasonal pattern and a consistency in relative differences between the seasons and sample categories. Leaf water was the most isotopically enriched water compartment. The leaf water enrichment decreased toward the autumn reflecting the change in δ18O (2H) of source water and evaporative demands. The soil and twig water isotopic signal was depleted against current precipitation as it partly retained the isotopic signature from winter precipitation however the seasonal pattern of soil and twig water followed that of precipitation. No significant differences between sun-exposed and shaded samples were detected. Nevertheless, the observed strong seasonal pattern of isotope composition of leaf, twig and soil water should be taken into account when using leaf water enrichment for further calculations or modeling 
650 4 |a Journal Article 
650 4 |a Fagus 
650 4 |a Irradiance 
650 4 |a Leaf water 
650 4 |a Seasonal course 
650 4 |a Soil 
650 4 |a Water isotopes 
650 7 |a Oxygen Isotopes  |2 NLM 
650 7 |a Water  |2 NLM 
650 7 |a 059QF0KO0R  |2 NLM 
650 7 |a Deuterium  |2 NLM 
650 7 |a AR09D82C7G  |2 NLM 
700 1 |a Hronková, Marie  |e verfasserin  |4 aut 
700 1 |a Šimková, Marie  |e verfasserin  |4 aut 
700 1 |a Květoň, Jiří  |e verfasserin  |4 aut 
700 1 |a Vráblová, Martina  |e verfasserin  |4 aut 
700 1 |a Kubásek, Jiří  |e verfasserin  |4 aut 
700 1 |a Šantrůček, Jiří  |e verfasserin  |4 aut 
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773 1 8 |g volume:227  |g year:2018  |g day:19  |g month:08  |g pages:56-65 
856 4 0 |u http://dx.doi.org/10.1016/j.jplph.2018.03.009  |3 Volltext 
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