Employing stable isotopes to determine the residence times of soil water and the temporal origin of water taken up by Fagus sylvatica and Picea abies in a temperate forest-Reference-Cited by-同舟云学术

Employing stable isotopes to determine the residence times of soil water and the temporal origin of water taken up by Fagus sylvatica and Picea abies in a temperate forest

Published:2018-06-11 Issue:4 Volume:219 Page:1300-1313
ISSN:0028-646X
Container-title:New Phytologist
language:en
Short-container-title:New Phytol

Author:

Brinkmann Nadine¹²^ORCID,Seeger Stefan³,Weiler Markus³,Buchmann Nina¹,Eugster Werner¹,Kahmen Ansgar²

Affiliation:

1. Institute of Agricultural Sciences; ETH Zürich; Universitätsstrasse 2 Zurich 8092 Switzerland

2. Department of Environmental Sciences - Botany; University Basel; Schönbeinstrasse 6 Basel 4056 Switzerland

3. Faculty of Environment and Natural Resources; University of Freiburg; Fahnenbergplatz 1 Freiburg 79098 Germany

Funder

Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung

Baden-Württemberg Stiftung

Publisher

Wiley

Subject

Plant Science,Physiology

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1111/nph.15255/fullpdf

Reference83 articles.

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3. The δ18O of root crown water best reflects source water delta O-18 in different types of herbaceous species;Barnard;Rapid Communications in Mass Spectrometry,2006

4. Determination of spatiotemporal variability of tree water uptake using stable isotopes (δ18O, δ2H) in an alluvial system supplied by a high- altitude watershed, Pfyn forest, Switzerland;Bertrand;Ecohydrology,2014

5. Spatial distribution of δ18O in meteoric precipitation;Bowen;Geology,2002

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