<HashMap><database>biostudies-literature</database><scores/><additional><submitter>Abernathy MJ</submitter><funding>National Institute of Environmental Health Sciences</funding><funding>NIEHS NIH HHS</funding><funding>National Institute of Food and Agriculture</funding><funding>University of California, Riverside</funding><pagination>11703-11712</pagination><full_dataset_link>https://www.ebi.ac.uk/biostudies/studies/S-EPMC11938697</full_dataset_link><repository>biostudies-literature</repository><omics_type>Unknown</omics_type><volume>55(17)</volume><pubmed_abstract>Vanadium is a redox-active metal that has been added to the EPA's Contaminant Candidate List with a notification level of 50 μg L&lt;sup>-1&lt;/sup> due to mounting evidence that V&lt;sup>V&lt;/sup> exposure can lead to adverse health outcomes. Groundwater V concentration exceeds the notification level in many locations, yet geochemical controls on its mobility are poorly understood. Here, we examined the redox interaction between V&lt;sup>IV&lt;/sup> and birnessite (MnO&lt;sub>2&lt;/sub>), a well-characterized oxidant and a scavenger of many trace metals. In our findings, birnessite quickly oxidized sparingly soluble V&lt;sup>IV&lt;/sup> species such as häggite [V&lt;sub>2&lt;/sub>O&lt;sub>3&lt;/sub>(OH)&lt;sub>2&lt;/sub>] into highly mobile and toxic vanadate (H&lt;i>&lt;sub>n&lt;/sub>&lt;/i>VO&lt;sub>4&lt;/sub>&lt;sup>(3-&lt;i>n&lt;/i>)-&lt;/sup>) in continuously</pubmed_abstract><journal>Environmental science &amp; technology</journal><pubmed_title>Oxidation of V(IV) by Birnessite: Kinetics and Surface Complexation.</pubmed_title><pmcid>PMC11938697</pmcid><funding_grant_id>T32 ES018827</funding_grant_id><funding_grant_id>CA-R-ENS-5151-H</funding_grant_id><pubmed_authors>Vessey CJ</pubmed_authors><pubmed_authors>Liu H</pubmed_authors><pubmed_authors>Schaefer MV</pubmed_authors><pubmed_authors>Abernathy MJ</pubmed_authors><pubmed_authors>Ying SC</pubmed_authors></additional><is_claimable>false</is_claimable><name>Oxidation of V(IV) by Birnessite: Kinetics and Surface Complexation.</name><description>Vanadium is a redox-active metal that has been added to the EPA's Contaminant Candidate List with a notification level of 50 μg L&lt;sup>-1&lt;/sup> due to mounting evidence that V&lt;sup>V&lt;/sup> exposure can lead to adverse health outcomes. Groundwater V concentration exceeds the notification level in many locations, yet geochemical controls on its mobility are poorly understood. Here, we examined the redox interaction between V&lt;sup>IV&lt;/sup> and birnessite (MnO&lt;sub>2&lt;/sub>), a well-characterized oxidant and a scavenger of many trace metals. In our findings, birnessite quickly oxidized sparingly soluble V&lt;sup>IV&lt;/sup> species such as häggite [V&lt;sub>2&lt;/sub>O&lt;sub>3&lt;/sub>(OH)&lt;sub>2&lt;/sub>] into highly mobile and toxic vanadate (H&lt;i>&lt;sub>n&lt;/sub>&lt;/i>VO&lt;sub>4&lt;/sub>&lt;sup>(3-&lt;i>n&lt;/i>)-&lt;/sup>) in continuously</description><dates><release>2021-01-01T00:00:00Z</release><publication>2021 Sep</publication><modification>2025-07-04T03:05:52.767Z</modification><creation>2025-07-04T03:05:52.767Z</creation></dates><accession>S-EPMC11938697</accession><cross_references><pubmed>34488349</pubmed><doi>10.1021/acs.est.1c02464</doi></cross_references></HashMap>