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Koehler G, McNeill G, Hobson KA. The stable isotope hydrology of Sable Island, Nova Scotia, Canada with implications for evaluating the water budget of wild horses. ISOTOPES IN ENVIRONMENTAL AND HEALTH STUDIES 2024; 60:122-140. [PMID: 38372972 DOI: 10.1080/10256016.2024.2316584] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 11/03/2023] [Accepted: 01/08/2024] [Indexed: 02/20/2024]
Abstract
We investigated the stable isotope hydrology of Sable Island, Nova Scotia, Canada over a five year period from September, 2017 to August, 2022. The δ2H and δ18O values of integrated monthly precipitation were weakly seasonal and ranged from -66 to -15 ‰ and from -9.7 to -1.9 ‰, respectively. Fitting these monthly precipitation data resulted in a local meteoric water line (LMWL) defined by: δ2H = 7.22 ± 0.21 · δ18O + 7.50 ± 1.22 ‰. Amount-weighted annual precipitation had δ2H and δ18O values of -36 ± 11 ‰ and -6.1 ± 1.4 ‰, respectively. Deep groundwater had more negative δ2H and δ18O values than mean annual precipitation, suggesting recharge occurs mainly in the winter, while shallow groundwater had δ2H and δ18O values more consistent with mean annual precipitation or mixing of freshwater with local seawater. Surface waters had more positive values and showed evidence of isolation from the groundwater system. The stable isotopic compositions of plant (leaf) water, on the other hand, indicate plants use groundwater as their source. Fog had δ2H and δ18O values that were significantly more positive than those of local precipitation, yet had similar 17O-excess values. δ2H values of horsehair from 4 individuals lacked seasonality, but had variations typical to those of precipitation on the island. Differences in mean δ2H values of horsehair were statistically significant and suggest variations in water use may exist between spatially disparate horse communities. Our results establish an important initial framework for ongoing isotope studies of feral horses and other wildlife on Sable Island.
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Affiliation(s)
- Geoff Koehler
- NHRC Stable Isotope Laboratory, Environment and Climate Change Canada, Saskatoon, Canada
| | - Gina McNeill
- Department of Biology, University of Western Ontario, London, Canada
| | - Keith A Hobson
- Department of Biology, University of Western Ontario, London, Canada
- Wildlife and Landscape Science Directorate, Environment and Climate Change Canada, Saskatoon, Canada
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Haberstroh S, Kübert A, Werner C. Two common pitfalls in the analysis of water-stable isotopologues with cryogenic vacuum extraction and cavity ring-down spectroscopy. ANALYTICAL SCIENCE ADVANCES 2024; 5:2300053. [PMID: 38827022 PMCID: PMC11142394 DOI: 10.1002/ansa.202300053] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Grants] [Track Full Text] [Download PDF] [Figures] [Subscribe] [Scholar Register] [Received: 10/21/2023] [Revised: 01/08/2024] [Accepted: 01/11/2024] [Indexed: 06/04/2024]
Abstract
Water stable isotopologue analysis is widely used to disentangle ecohydrological processes. Yet, there are increasing reports of measurement uncertainties for established and emerging methods, such as cryogenic vacuum extraction (CVE) or cavity ring-down spectroscopy (CRDS). With this study, we investigate two pitfalls, that potentially contribute to uncertainties in water-stable isotopologue research. To investigate fractionation sources in CVE, we extracted pure water of known isotopic composition with cotton, glass wool or without cover and compared the isotopologue results with non-extracted reference samples. To characterise the dependency of δ2H and δ18O on the water mixing ratio in CRDS, which is of high importance for in-situ applications with large natural variations in mixing ratios, we chose samples with a large range of isotopic compositions and determined δ2H and δ18O for different water mixing ratios with two CRDS analysers (Picarro, Inc.). Cotton wool had a strong fractionation effect on δ2H values, which increased with more 2H-enriched samples. δ2H and δ18O values showed a strong dependency on the water mixing ratio analysed with CRDS with differences of up to 34.5‰ (δ2H) and 3.9‰ (δ18O) for the same sample at different mixing ratios. CVE and CRDS, now routinely applied in water stable isotopologue research, come with pitfalls, namely fractionation effects of cover materials and water mixing ratio dependencies of δ2H and δ18O, which can lead to erroneous isotopologue results and thus, invalid conclusions about (ecohydrological) processes. These practical issues identified here should be reported and addressed adequately in water-stable isotopologue research.
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Affiliation(s)
- Simon Haberstroh
- Ecosystem PhysiologyFaculty of Environment and Natural ResourcesInstitute of Earth and Environmental SciencesUniversity FreiburgFreiburgGermany
| | - Angelika Kübert
- Ecosystem PhysiologyFaculty of Environment and Natural ResourcesInstitute of Earth and Environmental SciencesUniversity FreiburgFreiburgGermany
- Institute for Atmospheric and Earth System Research (INAR)University of HelsinkiHelsinkiFinland
| | - Christiane Werner
- Ecosystem PhysiologyFaculty of Environment and Natural ResourcesInstitute of Earth and Environmental SciencesUniversity FreiburgFreiburgGermany
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Zhang J, Xu Z. Vacuum extraction of high-salinity water for the determination of oxygen and hydrogen isotopic compositions using cavity ring-down spectroscopy. Microchem J 2023. [DOI: 10.1016/j.microc.2023.108678] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 04/04/2023]
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Cui X, Li Y, Jiang C, Yuan Z, Zhou S, Chen W, Yu B. In situ measurement of water vapor isotope ratios in air with a laser-based spectrometer. SPECTROCHIMICA ACTA. PART A, MOLECULAR AND BIOMOLECULAR SPECTROSCOPY 2022; 283:121762. [PMID: 35985233 DOI: 10.1016/j.saa.2022.121762] [Citation(s) in RCA: 1] [Impact Index Per Article: 0.5] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Subscribe] [Scholar Register] [Received: 05/03/2022] [Revised: 08/04/2022] [Accepted: 08/11/2022] [Indexed: 06/15/2023]
Abstract
Simultaneous measurement of H217O/H216O, H218O/H216O, and HDO/H216O in air with a compact spectrometer based on a mid-infrared distributed feedback (DFB) laser was described. The obtained mixing ratios of H216O, H217O, and H218O agreed reasonably well with those measured by a hygrometer. The precision and repeatability of the spectrometer were analyzed. Indoor air tests demonstrated that its 220-s precision was 0.08 ‰, 0.06 ‰, and 0.14 ‰ for δ18O, δ17O, and δ2H respectively. The measured values of δ18O, δ17O, and δ2H in indoor air were highly correlated with the water vapor mixing ratios. The compact spectrometer provides in situ measurements of water vapor isotopes with high precision and fast time response, which opens new possibilities for its application in atmospheric and hydrological research in the future.
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Affiliation(s)
- Xiaojuan Cui
- Information Materials and Intelligent Sensing Laboratory of Anhui Province, Institutes of Physical Science and Information Technology, Anhui University, 230601 Hefei, China; Key Laboratory of Opto-Electronic Information Acquisition and Manipulation of Ministry of Education, Anhui University, 230601 Hefei, China.
| | - Yafan Li
- Information Materials and Intelligent Sensing Laboratory of Anhui Province, Institutes of Physical Science and Information Technology, Anhui University, 230601 Hefei, China; Key Laboratory of Opto-Electronic Information Acquisition and Manipulation of Ministry of Education, Anhui University, 230601 Hefei, China
| | - Chaochao Jiang
- Information Materials and Intelligent Sensing Laboratory of Anhui Province, Institutes of Physical Science and Information Technology, Anhui University, 230601 Hefei, China; Key Laboratory of Opto-Electronic Information Acquisition and Manipulation of Ministry of Education, Anhui University, 230601 Hefei, China
| | - Zijian Yuan
- Information Materials and Intelligent Sensing Laboratory of Anhui Province, Institutes of Physical Science and Information Technology, Anhui University, 230601 Hefei, China
| | - Sheng Zhou
- Information Materials and Intelligent Sensing Laboratory of Anhui Province, Institutes of Physical Science and Information Technology, Anhui University, 230601 Hefei, China; Key Laboratory of Opto-Electronic Information Acquisition and Manipulation of Ministry of Education, Anhui University, 230601 Hefei, China
| | - Weidong Chen
- Laboratoire de Physicochimie de l'Atmosphère, Université du Littoral Côte d'Opale, 189A Avenue, Maurice Schumann, 59140 Dunkerque, France
| | - Benli Yu
- Information Materials and Intelligent Sensing Laboratory of Anhui Province, Institutes of Physical Science and Information Technology, Anhui University, 230601 Hefei, China; Key Laboratory of Opto-Electronic Information Acquisition and Manipulation of Ministry of Education, Anhui University, 230601 Hefei, China
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Voigt C, Vallet-Coulomb C, Piel C, Alexandre A. 17 O-excess and d-excess of atmospheric water vapor measured by cavity ring-down spectrometry: Evidence of a matrix effect and implication for the calibration procedure. RAPID COMMUNICATIONS IN MASS SPECTROMETRY : RCM 2022; 36:e9227. [PMID: 34845759 DOI: 10.1002/rcm.9227] [Citation(s) in RCA: 1] [Impact Index Per Article: 0.5] [Reference Citation Analysis] [Abstract] [Track Full Text] [Subscribe] [Scholar Register] [Received: 07/21/2021] [Revised: 11/22/2021] [Accepted: 11/22/2021] [Indexed: 06/13/2023]
Abstract
RATIONALE Producing robust high-frequency time series of raw atmospheric water vapor isotope data using laser spectrometry requires accurate calibration. In particular, the chemical composition of the analyzed sample gas can cause isotope bias. This study assesses the matrix effect on calibrated δ17 O, δ18 O, δ2 H, 17 O-excess, and d-excess values of atmospheric water vapor. METHODS A Picarro L2140-i cavity ring-down spectrometer with an autosampler and a vaporizer is used to analyze δ17 O, δ18 O, δ2 H, 17 O-excess, and d-excess of two water standards. Isotope data obtained using synthetic air and dry ambient air as carrier gas at water mixing ratios ranging from 2000 to 30 000 ppmv are compared. Based on the results, atmospheric water vapor measurements are calibrated. The expected precision is estimated by Monte Carlo simulation. RESULTS The dry air source strongly impacts raw isotope values of the two water standards but has no effect on the mixing ratio dependency functions. When synthetic air is used, δ17 O, δ18 O, and 17 O-excess of calibrated atmospheric water vapor are overestimated by 0.6‰, 0.7‰, and 217 per meg, respectively, whereas δ2 H and d-excess are underestimated by 1.5‰ and 7.3‰. Optimum precisions for the calibrated δ17 O, δ18 O, δ2 H, 17 O-excess, and d-excess values and 12 min integration time are 0.02‰, 0.03‰, 0.4‰, 14 per meg, and 0.4‰, respectively. CONCLUSIONS Regarding the obtained results, recommendations for the calibration of atmospheric water vapor isotope measurements are presented. The necessity to use dry ambient air as dry air source when running the standards for calibration is pointed out as a prerequisite for accurate atmospheric water vapor 17 O-excess and d-excess measurements.
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Affiliation(s)
- Claudia Voigt
- Aix Marseille Univ, CNRS, IRD, INRAE, CEREGE, Aix-en-Provence, France
| | | | - Clément Piel
- ECOTRON Européen de Montpellier, UAR 3248, Centre National de la Recherche Scientifique (CNRS), Campus de Baillarguet, Montferrier-sur-Lez, France
| | - Anne Alexandre
- Aix Marseille Univ, CNRS, IRD, INRAE, CEREGE, Aix-en-Provence, France
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Gessler A, Bächli L, Rouholahnejad Freund E, Treydte K, Schaub M, Haeni M, Weiler M, Seeger S, Marshall J, Hug C, Zweifel R, Hagedorn F, Rigling A, Saurer M, Meusburger K. Drought reduces water uptake in beech from the drying topsoil, but no compensatory uptake occurs from deeper soil layers. THE NEW PHYTOLOGIST 2022; 233:194-206. [PMID: 34610146 PMCID: PMC9293437 DOI: 10.1111/nph.17767] [Citation(s) in RCA: 18] [Impact Index Per Article: 9.0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 08/03/2021] [Accepted: 09/26/2021] [Indexed: 06/02/2023]
Abstract
The intensity and frequency of droughts events are projected to increase in future with expected adverse effects for forests. Thus, information on the dynamics of tree water uptake from different soil layers during and after drought is crucial. We applied an in situ water isotopologue monitoring system to determine the oxygen isotope composition in soil and xylem water of European beech with a 2-h resolution together with measurements of soil water content, transpiration and tree water deficit. Using a Bayesian isotope mixing model, we inferred the relative and absolute contribution of water from four different soil layers to tree water use. Beech took up more than 50% of its water from the uppermost 5 cm soil layer at the beginning of the 2018 drought, but then reduced absolute water uptake from the drying topsoil by 84%. The trees were not able to quantitatively compensate for restricted topsoil water availability by additional uptake from deeper soil layers, which is related to the fine root depth distribution. Absolute water uptake from the topsoil was restored to pre-drought levels within 3 wk after rewetting. These uptake patterns help to explain both the drought sensitivity of beech and its high recovery potential after drought release.
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Affiliation(s)
- Arthur Gessler
- Research Unit Forest DynamicsSwiss Federal Research Institute for Forest, Snow and Landscape Research WSL8903BirmensdorfSwitzerland
- Institute of Terrestrial EcosystemsETH Zurich8092ZurichSwitzerland
| | - Lukas Bächli
- Research Unit Forest DynamicsSwiss Federal Research Institute for Forest, Snow and Landscape Research WSL8903BirmensdorfSwitzerland
| | | | - Kerstin Treydte
- Research Unit Forest DynamicsSwiss Federal Research Institute for Forest, Snow and Landscape Research WSL8903BirmensdorfSwitzerland
| | - Marcus Schaub
- Research Unit Forest DynamicsSwiss Federal Research Institute for Forest, Snow and Landscape Research WSL8903BirmensdorfSwitzerland
| | - Matthias Haeni
- Research Unit Forest DynamicsSwiss Federal Research Institute for Forest, Snow and Landscape Research WSL8903BirmensdorfSwitzerland
| | - Markus Weiler
- Hydrology, Faculty of Environment and Natural ResourcesUniversity of Freiburg79098FreiburgGermany
| | - Stefan Seeger
- Hydrology, Faculty of Environment and Natural ResourcesUniversity of Freiburg79098FreiburgGermany
| | - John Marshall
- Department of Forest Ecology and ManagementSwedish University of Agricultural SciencesUmeå90283Sweden
| | - Christian Hug
- Research Unit Forest DynamicsSwiss Federal Research Institute for Forest, Snow and Landscape Research WSL8903BirmensdorfSwitzerland
| | - Roman Zweifel
- Research Unit Forest DynamicsSwiss Federal Research Institute for Forest, Snow and Landscape Research WSL8903BirmensdorfSwitzerland
| | - Frank Hagedorn
- Research Unit Forest Soils and BiogeochemistrySwiss Federal Research Institute for Forest, Snow and Landscape Research WSL8903BirmensdorfSwitzerland
| | - Andreas Rigling
- Research Unit Forest DynamicsSwiss Federal Research Institute for Forest, Snow and Landscape Research WSL8903BirmensdorfSwitzerland
- Institute of Terrestrial EcosystemsETH Zurich8092ZurichSwitzerland
| | - Matthias Saurer
- Research Unit Forest DynamicsSwiss Federal Research Institute for Forest, Snow and Landscape Research WSL8903BirmensdorfSwitzerland
| | - Katrin Meusburger
- Research Unit Forest Soils and BiogeochemistrySwiss Federal Research Institute for Forest, Snow and Landscape Research WSL8903BirmensdorfSwitzerland
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Wassenaar L, Terzer-Wassmuth S, Douence C. Progress and challenges in dual- and triple-isotope (δ 18 O, δ 2 H, Δ 17 O) analyses of environmental waters: An international assessment of laboratory performance. RAPID COMMUNICATIONS IN MASS SPECTROMETRY : RCM 2021; 35:e9193. [PMID: 34490664 DOI: 10.1002/rcm.9193] [Citation(s) in RCA: 1] [Impact Index Per Article: 0.3] [Reference Citation Analysis] [Abstract] [Track Full Text] [Subscribe] [Scholar Register] [Received: 06/04/2021] [Revised: 08/31/2021] [Accepted: 09/02/2021] [Indexed: 06/13/2023]
Abstract
RATIONALE Stable isotope analyses of environmental waters (δ2 H, δ18 O) are an important assay in hydrology and environmental research with rising interest in δ17 O, which requires ultra-precise assays. We evaluated isotope analyses of six test water samples for 281 laboratory submissions measuring δ2 H and δ18 O along with a subset analyzing δ17 O and Δ17 O by laser spectrometry and isotope ratio mass spectrometry (IRMS). METHODS Six test waters were distributed to laboratories spanning a wide δ range of natural waters for δ2 H, δ18 O and δ17 O and Δ17 O. One sample was a blind duplicate to test reproducibility and claims of analytical precision. RESULTS Results showed that ca 83% of the submissions produced acceptable δ18 O and δ2 H results within 0.2‰ (mUr) and 1.6‰ of the benchmark values, respectively. However, 17% of the submissions gave questionable to unacceptable results. A blind duplicate revealed many laboratories reported overly optimistic precision, and many could not replicate within their claimed precision. For Δ17 O, dual-inlet results for IRMS using quantitative O2 conversion were accurate and highly precise, but the results for laser spectrometry ranged by ca 200 per meg (μUr) for each sample, with ca 70% unable to replicate the duplicate to their claimed Δ17 O precision. One complicating factor is the lack of certified primary reference waters for δ17 O. CONCLUSIONS No single factor or combination of factors was identifiable for poor or good performance, and underperformance came from issues like data normalization including inadequate memory and drift corrections, compromised working reference materials and underperforming instrumentation. We recommend isotope laboratories include high and low δ value controls of known isotope composition in each run. Progress in Δ17 O analyses by laser spectrometry requires extraordinary proof of performance claims and would benefit from the development of adoptable and systematic advanced data processing procedures to correct for memory and drift.
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Affiliation(s)
- Leonard Wassenaar
- Department of Nuclear Sciences and Applications, Division of Physical and Chemical Sciences, Isotope Hydrology Laboratory, International Atomic Energy Agency, Vienna, Austria
| | - Stefan Terzer-Wassmuth
- Department of Nuclear Sciences and Applications, Division of Physical and Chemical Sciences, Isotope Hydrology Laboratory, International Atomic Energy Agency, Vienna, Austria
| | - Cedric Douence
- Department of Nuclear Sciences and Applications, Division of Physical and Chemical Sciences, Isotope Hydrology Laboratory, International Atomic Energy Agency, Vienna, Austria
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