Non‐exchangeable stable hydrogen isotope ratios in clay minerals and soil clay fractions: A method test
Author:
Affiliation:
1. Institute of Geography and Geoecology, Karlsruhe Institute of Technology (KIT) Karlsruhe Germany
2. Geoecology, University of Tübingen Tübingen Germany
Funder
Deutsche Forschungsgemeinschaft
Publisher
Wiley
Subject
Soil Science
Link
https://onlinelibrary.wiley.com/doi/pdf/10.1111/ejss.13289
Reference89 articles.
1. Determination of the cation exchange capacity of clays with copper complexes revisited
2. Analytical methods for the measurement of hydrogen isotope composition and water content in clay minerals by TC/EA
3. An extended revision of the interlayer structures of one- and two- layer hydrates of Na- vermiculite
4. Baseline Studies of the Clay Minerals Society Source Clays: Cation Exchange Capacity Measurements by the Ammonia-Electrode Method
5. Iodide, caesium and strontium adsorption by organophilic vermiculite
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1. Impacts of chemical pre-treatments on the hydrogen isotope composition of clay minerals: Determining potential effects in the absence of impurities;Applied Clay Science;2024-01
2. Global distribution of nonexchangeable stable hydrogen isotope ratios of topsoil clay fractions;Geochimica et Cosmochimica Acta;2023-04
3. Equilibrium isotope fractionation factors of H exchange between steam and soil clay fractions;Rapid Communications in Mass Spectrometry;2023-03-23
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