Abstract
Abstract Iron(III) colloids are known to act as carriers for toxic elements in nature, which can cause retardation or even acceleration of their migration. In this study the adsorption of UO22+ on iron(III) (oxy)hydroxides (2-line ferrihydrite, 6-line ferrihydrite, goethite, and maghemite) were compared through adsorption isotherm measurements. The normalized adsorption amounts on goethite were larger than those of the other minerals over a wide range of free UO22+ concentration in spite of the relatively small site density of goethite.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
