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From Adsorption to Precipitation of U(VI): What is the Role of pH and Natural Organic Matter?
Journal article   Peer reviewed

From Adsorption to Precipitation of U(VI): What is the Role of pH and Natural Organic Matter?

Carmen A Velasco, Adrian J Brearley, Jorge Gonzalez-Estrella, Abdul-Mehdi S Ali, María Isabel Meza, Stephen E Cabaniss, Bruce M Thomson, Tori Z Forbes, Juan S Lezama Pacheco and José M Cerrato
Environmental science & technology, Vol.55(23), pp.16246-16256
12/07/2021
DOI: 10.1021/acs.est.1c05429
PMCID: PMC8680647
PMID: 34797046
url
https://www.ncbi.nlm.nih.gov/pmc/articles/8680647View
Open Access

Abstract

We investigated interfacial reactions of U(VI) in the presence of Suwannee River natural organic matter (NOM) at acidic and neutral pH. Laboratory batch experiments show that the adsorption and precipitation of U(VI) in the presence of NOM occur at pH 2 and pH 4, while the aqueous complexation of U by dissolved organic matter is favored at pH 7, preventing its precipitation. Spectroscopic analyses indicate that U(VI) is mainly adsorbed to the particulate organic matter at pH 4. However, U(VI)-bearing ultrafine to nanocrystalline solids were identified at pH 4 by electron microscopy. This study shows the promotion of U(VI) precipitation by NOM at low pH which may be relevant to the formation of mineralized deposits, radioactive waste repositories, wetlands, and other U- and organic-rich environmental systems.
Adsorption Dissolved Organic Matter Hydrogen-Ion Concentration Radioactive Waste Uranium - analysis

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