Iron isotope fingerprints of redox and biogeochemical cycling in the soil-water-rice plant system of a paddy field-Reference-Cited by-同舟云学术

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Iron isotope fingerprints of redox and biogeochemical cycling in the soil-water-rice plant system of a paddy field

Published:2017-01 Issue: Volume:574 Page:1622-1632
ISSN:0048-9697
Container-title:Science of The Total Environment
language:en
Short-container-title:Science of The Total Environment

Author:

Garnier J.,Garnier J-M.,Vieira C.L.,Akerman A.,Chmeleff J.,Ruiz R.I.,Poitrasson F.

Funder

LMI-OCE

7th European Community Framework Programme

CNRS-INSU

CLIM-AMAZON European Laboratory

CNPq

Publisher

Elsevier BV

Subject

Pollution,Waste Management and Disposal,Environmental Chemistry,Environmental Engineering

Reference55 articles.

1. Isotopic fingerprint of Fe cycling in an equatorial soil-plant-water system: the Nsimi watershed, South Cameroon;Akerman;Chem. Geol.,2014

2. Theoretical investigation of iron isotope fractionation between Fe(H2O)63+ and Fe(H2O)62+: implications for iron stable isotope geochemistry;Anbar;Geochim. Cosmochim. Acta,2005

3. Iron and zinc isotope fractionation during uptake and translocation in rice (Oryza sativa) grown in oxic and anoxic soils;Arnold;C.R. Geoscience,2015

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

5. Iron uptake and loading into rice grains;Bashir;Rice,2010

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