Evolution of Retisol impacted by artificial drainage: What can we learn from stable Fe isotope ratios?-Reference-Cited by-同舟云学术

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Evolution of Retisol impacted by artificial drainage: What can we learn from stable Fe isotope ratios?

Published:2021-02 Issue: Volume:384 Page:114771
ISSN:0016-7061
Container-title:Geoderma
language:en
Short-container-title:Geoderma

Author:

Fekiacova Z.,Montagne D.,Duvivier A.,Guihou A.,Deschamps P.,Cornu S.

Publisher

Elsevier BV

Subject

Soil Science

Reference46 articles.

1. Iron stable isotopes: beyond biosignatures;Anbar;Earth Planet. Sci. Lett.,2004

2. Notice de la carte des sols de l'Yonne à 1/50000, feuille Joigny;Baize,1988

3. Iron isotope fractionation during microbially stimulated Fe(II) oxidation and Fe(III) precipitation;Balci;Geochim. Cosmochim. Acta,2006

4. Beard, B. L. and Johnson, C. M. (2004) Reviews in Mineralogy & Geochemistry 10A Vol. 55, 319-357.

5. Iron isotope biosignatures;Beard;Science,1999

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1. Impact of Flooding–Drainage Alternation on Fe Uptake and Transport in Rice: Novel Insights from Iron Isotopes;Journal of Agricultural and Food Chemistry;2024-01-02

2. Iron isotope fractionation during the formation of ferromanganese nodules under different conditions of hydromorphism;Geoderma;2023-02

3. Glossic planosols in the postglacial landscape of central europe: Modern polygenetic soils or subaerial palaeosols?;Geoderma;2022-11

4. The use of stable isotopes in soil science: Metals;Reference Module in Earth Systems and Environmental Sciences;2022

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