Articles | Volume 13, issue 10
https://doi.org/10.5194/bg-13-3175-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/bg-13-3175-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
2H and 18O depletion of water close to organic surfaces
Guo Chen
Lehrstuhl für Grünlandlehre, Technische Universität München,
Alte Akademie 12, Freising-Weihenstephan 85354, Germany
Lehrstuhl für Grünlandlehre, Technische Universität München,
Alte Akademie 12, Freising-Weihenstephan 85354, Germany
Hans Schnyder
Lehrstuhl für Grünlandlehre, Technische Universität München,
Alte Akademie 12, Freising-Weihenstephan 85354, Germany
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Cited
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42 citations as recorded by crossref.
- Fire effects on C and H isotopic composition in plant biomass and soil: Bulk and particle size fractions N. Jiménez-Morillo et al. 10.1016/j.scitotenv.2020.141417
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- Isotopic offsets between bulk plant water and its sources are larger in cool and wet environments J. de la Casa et al. 10.5194/hess-26-4125-2022
- Quantitative contribution of cryogenic vacuum extraction and radial water transport to xylem-source water deuterium offsets Y. Li et al. 10.1016/j.agrformet.2023.109837
- The suitability of isotopic methods in identifying water sources of a shallow-rooted herbaceous plant in a desert steppe Y. Song et al. 10.1016/j.scitotenv.2023.166072
- Membrane inlet laser spectroscopy to measure H and O stable isotope compositions of soil and sediment pore water with high sample throughput E. Oerter et al. 10.1002/rcm.7768
- Revisiting streamside trees that do not use stream water: can the two water worlds hypothesis and snowpack isotopic effects explain a missing water source? D. Bowling et al. 10.1002/eco.1771
- Dynamics of competition over water in a mixed oak-pine Mediterranean forest: Spatio-temporal and physiological components J. del Castillo et al. 10.1016/j.foreco.2016.10.025
- Non-destructive estimates of soil carbonic anhydrase activity and associated soil water oxygen isotope composition S. Jones et al. 10.5194/hess-21-6363-2017
- In situ monitoring of H and O stable isotopes in soil water reveals ecohydrologic dynamics in managed soil systems E. Oerter & G. Bowen 10.1002/eco.1841
- The triple oxygen isotope composition of phytoliths as a proxy of continental atmospheric humidity: insights from climate chamber and climate transect calibrations A. Alexandre et al. 10.5194/bg-15-3223-2018
- Flushing or mixing? Stable water isotopes reveal differences in arctic forest and peatland soil water seasonality F. Muhic et al. 10.1002/hyp.14811
- Assessing the isotopic biases of soil water from cryogenic water extraction in different soil types in China P. Zhao et al. 10.1002/hyp.15228
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- The δ18O and δ2H of water in the leaf growth‐and‐differentiation zone of grasses is close to source water in both humid and dry atmospheres H. Liu et al. 10.1111/nph.14549
- Soil water vapour isotopes identify missing water source for streamside trees E. Oerter et al. 10.1002/eco.2083
- 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 N. Brinkmann et al. 10.1111/nph.15255
- Sampling soil water along the pF curve for δ2H and δ18O analysis N. Orlowski & L. Breuer 10.1002/hyp.13916
- Snowmelt-mediated isotopic homogenization of shallow till soil F. Muhic et al. 10.5194/hess-28-4861-2024
- Deuterium depletion in xylem water and soil isotopic effects complicate the assessment of riparian tree water sources in the seasonal tropics C. Duvert et al. 10.1002/eco.2383
- An explanation for the isotopic offset between soil and stem water in a temperate tree species A. Barbeta et al. 10.1111/nph.16564
- Air moisture and soil texture are crucial for the water dynamics of riparian bamboo in a subtropical region G. Chen et al. 10.1007/s11104-020-04696-w
- Effects of Wilting and Dew on the Water Isotope Composition of Detached Grass in Temperate Grassland G. Chen et al. 10.1021/acs.jafc.9b02978
- Oak Transpiration Drawn From the Weathered Bedrock Vadose Zone in the Summer Dry Season W. Hahm et al. 10.1029/2020WR027419
- Radial and axial water movement in adult trees recorded by stable isotope tracing K. Treydte et al. 10.1093/treephys/tpab080
- Bound and mobile soil water isotope ratios are affected by soil texture and mineralogy, whereas extraction method influences their measurement R. Adams et al. 10.1002/hyp.13633
- Plant and root‐zone water isotopes are difficult to measure, explain, and predict: Some practical recommendations for determining plant water sources J. von Freyberg et al. 10.1111/2041-210X.13461
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- The role of soil pH on soil carbonic anhydrase activity J. Sauze et al. 10.5194/bg-15-597-2018
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- Phloem water isotopically different to xylem water: Potential causes and implications for ecohydrological tracing M. Nehemy et al. 10.1002/eco.2417
- Coffee and shade trees show complementary use of soil water in a traditional agroforestry ecosystem L. Muñoz-Villers et al. 10.5194/hess-24-1649-2020
- On the urgent need for standardization in isotope‐based ecohydrological investigations C. Millar et al. 10.1002/hyp.14698
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- Isotopic fractionation induced by a surface effect influences the estimation of the hydrological process of topsoil G. Chen et al. 10.1002/hyp.14019
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- Evidence for distinct isotopic compositions of sap and tissue water in tree stems: consequences for plant water source identification A. Barbeta et al. 10.1111/nph.17857
Latest update: 21 Nov 2024
Short summary
Hydrophilic surfaces influence the structure of water close to them and may thus affect the isotope composition of water. Across a wide range of materials, fractionation became linearly more negative with increasing volumetric solid : water ratio and even exceeded −44 ‰ for 2H. This has major implications for the interpretation of the isotopic composition of extracted water, especially when the solid : water ratio is larger than 0.5 or for processes occurring at the solid–water interface.
Hydrophilic surfaces influence the structure of water close to them and may thus affect the...
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