Retention of U(VI) by the Formation of Fe Precipitates from Oxidation of Fe(II)-Reference-Cited by-同舟云学术

Retention of U(VI) by the Formation of Fe Precipitates from Oxidation of Fe(II)

Published:2018-08-07 Issue:10 Volume:2 Page:968-976
ISSN:2472-3452
Container-title:ACS Earth and Space Chemistry
language:en
Short-container-title:ACS Earth Space Chem.

Author:

Mei Huiyang¹²,Tan Xiaoli¹²^ORCID,Tan Liqiang¹,Meng Yuedong²,Chen Changlun²^ORCID,Fang Ming¹^ORCID,Wang Xiangke¹³^ORCID

Affiliation:

1. School of Environment and Chemical Engineering, North China Electric Power University, Beijing 102206, People’s Republic of China

2. CAS Key Laboratory of Photovoltaic and Energy Conservation Materials, Institute of Plasma Physics, Chinese Academy of Sciences (CAS), Post Office Box 1126, Hefei, Anhui 230031, People’s Republic of China

3. Collaborative Innovation Center of Radiation Medicine of Jiangsu Higher Education Institutions, Suzhou, Jiangsu 215123, People’s Republic of China

Funder

Ministry of Education of the People's Republic of China

National Natural Science Foundation of China

Priority Academic Program Development of Jiangsu Higher Education Institutions

Collaborative Innovation Center of Radiation Medicine of Jiangsu Higher Education Institutions

Science Challenge Project

Publisher

American Chemical Society (ACS)

Subject

Space and Planetary Science,Atmospheric Science,Geochemistry and Petrology

Link

https://pubs.acs.org/doi/pdf/10.1021/acsearthspacechem.8b00055

Reference55 articles.

1. Sorption Speciation of Lanthanides/Actinides on Minerals by TRLFS, EXAFS and DFT Studies: A Review

2. The influence of dissolved Si on Ni precipitate formation at the kaolinite water interface: Kinetics, DRS and EXAFS analysis

3. Bonding properties of humic acid with attapulgite and its influence on U(VI) sorption

4. Interaction mechanism of radionickel on Na-montmorillonite: Influences of pH, electrolyte cations, humic acid and temperature

5. Effect of Silicate on the Formation and Stability of Ni–Al LDH at the γ-Al2O3 Surface

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