https://nova.newcastle.edu.au/vital/access/ /manager/Index en-au 5 https://nova.newcastle.edu.au/vital/access/ /manager/Repository/uon:42988 Wed 13 Mar 2024 11:24:24 AEDT ]]> https://nova.newcastle.edu.au/vital/access/ /manager/Repository/uon:52113 Thu 28 Sep 2023 14:57:20 AEST ]]> https://nova.newcastle.edu.au/vital/access/ /manager/Repository/uon:37319 Thu 12 Aug 2021 11:45:49 AEST ]]> https://nova.newcastle.edu.au/vital/access/ /manager/Repository/uon:42912 -1 and ∼33,000 to ∼150 μg L^-1, respectively. This trend was interrupted by a sharp rise in aqueous As(III) and Fe(II) caused by reductive dissolution of As-bearing Fe(III) phases in a sediment retention pond. Attenuation of Fe and As mobility occurred via formation of As(V)-rich schwertmannite, As(V)-rich jarosite, and amorphous ferric arsenate (AFA), resulting in solid-phase As concentrations spanning ∼13 to ∼208 g kg-1. Schwertmannite and jarosite retained As(V) predominantly by structural incorporation involving AsO₄-for-SO₄ substitution at up to ∼40 and ∼22 mol %, respectively. Arsenic strongly influenced Fe(III) mineral formation, with high As(V) concentrations causing formation of AFA over schwertmannite. Arsenic also strongly influenced Fe(III) mineral evolution over time. In particular, increasing levels of As(V) incorporation within schwertmannite were shown, for the first time, to enhance the transformation of schwertmannite to jarosite. This significant discovery necessitates a re-evaluation of the prevailing paradigm that As(V) retards schwertmannite transformation.]]> Thu 02 Nov 2023 14:53:12 AEDT ]]> https://nova.newcastle.edu.au/vital/access/ /manager/Repository/uon:47561 Mon 23 Jan 2023 13:04:35 AEDT ]]>