Soil and tree stem xylem water isotope data from two pan-European sampling campaigns

The stable isotope ratios of hydrogen (δ2H) and oxygen (δ18O) are useful for studying ecohydrological dynamics in forests. However, most isotope-based eco-hydrological studies are limited to single sites, resulting in a lack of large-scale isotope data for understanding tree water uptake. Here, we provide a first systematic isotope dataset for soil and stem xylem water collected during two pan-European sampling campaigns at 40 beech (Fagus sylvatica), spruce (Picea abies), or mixed beech-spruce forest sites in spring and summer 2023 (https://doi.org/10.16904/envidat.542, Lehmann et al., 2024). The dataset is complemented by additional site-, soil-, and tree-specific metadata. The samples and metadata were collected by different researchers across Europe following a standardized protocol. Soil samples were taken at up to 5 depths (ranging from 0 to 90 cm) and stem xylem samples from the trunks of three beech and/or spruce trees per site. All samples were sent to a single laboratory, where all analytical work was conducted. Water was extracted using cryogenic vacuum distillation and analyzed with an isotope laser spectrometer. Additionally, a subset of the samples was analyzed with an isotope ratio mass spectrometer. Data quality checks revealed a high mean total extraction efficiency, mean water amount (>1 mL), accuracy, and precision. The isotopic signature of soil and stem xylem water varied as a function of the geographic origin and changed from spring to summer across all sites. While δ2H and δ18O were strongly correlated, the soil water data plotted closer to the Global Meteoric Water Line (GMWL) than the stem xylem water. Specifically, the δ2H values of the xylem water were more enriched than those of the soil water, leading to a systematic deviation from the GMWL. Isotopic enrichment of the stem xylem water at mixed forest sites was larger for spruce trees than for beech trees. This dataset is particularly useful for large-scale studies on plant water use, ecohydrological model testing, and isotope mapping across Europe.

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Publication Details

Journal
Universität Zürich, ZORA
Published
2025-11-14
DOI
https://doi.org/10.5167/uzh-282300
Primary Topic
Plant Water Relations and Carbon Dynamics
Type
article
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article

Soil and tree stem xylem water isotope data from two pan-European sampling campaigns

Frank Hagedorn, Alberto Iraheta, Fabio Ercoli, Marius G. Floriancic et al.
Universität Zürich, ZORA
Plant Water Relations and Carbon Dynamics
article

Soil and tree stem xylem water isotope data from two pan-European sampling campaigns

Frank Hagedorn, Alberto Iraheta, Fabio Ercoli, Marius G. Floriancic, Frédéric Huneau, Pertti Ala‐aho, David Dubbert, Christophe Hissler, Fabian Bernhard, Josie Geris, Youri Rothfuss, Matteo Verdone, Lukrecija Butorac, Natalie Ceperley, Mátyás Árvai, Alise Babre, Teresa Gimeno, Nerantzis Kazakis, Alicia Correa, Ilja van Meerveld, Alligin Ghazoul, Haoyu Diao, Marco M. Lehmann, et al., Damien Gounelle, Daniele Penna, Simon D. Carrière, Philippe Balandier, Maren Dubbert, Zuosinan Chen, Tamara Jakovljević
article en

Abstract

The stable isotope ratios of hydrogen (δ2H) and oxygen (δ18O) are useful for studying ecohydrological dynamics in forests. However, most isotope-based eco-hydrological studies are limited to single sites, resulting in a lack of large-scale isotope data for understanding tree water uptake. Here, we provide a first systematic isotope dataset for soil and stem xylem water collected during two pan-European sampling campaigns at 40 beech (Fagus sylvatica), spruce (Picea abies), or mixed beech-spruce forest sites in spring and summer 2023 (https://doi.org/10.16904/envidat.542, Lehmann et al., 2024). The dataset is complemented by additional site-, soil-, and tree-specific metadata. The samples and metadata were collected by different researchers across Europe following a standardized protocol. Soil samples were taken at up to 5 depths (ranging from 0 to 90 cm) and stem xylem samples from the trunks of three beech and/or spruce trees per site. All samples were sent to a single laboratory, where all analytical work was conducted. Water was extracted using cryogenic vacuum distillation and analyzed with an isotope laser spectrometer. Additionally, a subset of the samples was analyzed with an isotope ratio mass spectrometer. Data quality checks revealed a high mean total extraction efficiency, mean water amount (>1 mL), accuracy, and precision. The isotopic signature of soil and stem xylem water varied as a function of the geographic origin and changed from spring to summer across all sites. While δ2H and δ18O were strongly correlated, the soil water data plotted closer to the Global Meteoric Water Line (GMWL) than the stem xylem water. Specifically, the δ2H values of the xylem water were more enriched than those of the soil water, leading to a systematic deviation from the GMWL. Isotopic enrichment of the stem xylem water at mixed forest sites was larger for spruce trees than for beech trees. This dataset is particularly useful for large-scale studies on plant water use, ecohydrological model testing, and isotope mapping across Europe.

Universität Zürich, ZORA
Clean water and sanitation
Openalex Percentile: Top 33%
Plant Water Relations and Carbon Dynamics
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