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   <subfield code="a">Interaction of Magnesium-Iron-Carbonic-Layered Double Hydroxides with As(III)</subfield>
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   <subfield code="c">[Susanta Paikaray, M. Hendry]</subfield>
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   <subfield code="a">Hydrotalcite-like compounds (HTlcs) are of potential environmental significance due to a reactive interlayer that may act as a natural sink during precipitation under ambient conditions or after interaction with contaminants. This study focused on the partitioning of As(III) on MgFeCO3-type HTlcs, in consideration of the predominance of both Mg2+ and Fe3+ in CO2-equilibrated natural settings. Sequestration of As(III) during HTlc precipitation was several orders of magnitude greater compared to interaction with pre-existing HTlc precipitates. This is attributed to the participation of As(III)-oxyanion species in the maintenance of surface charge neutrality during active precipitation. The degree of crystallinity, crystallite size, and interlayer thickness of the Mg-FeCO3-type HTlc all decreased slightly upon As(III) incorporation; metal-metal coordination was largely unaffected. Ambient interaction of the HTlc with As(III) caused CO3 2− incorporation into the interlayer from atmospheric CO2 even in the absence of a dissolved CO3 2− source. The interlayer occupancy of entrapped As(III) constituted a minor fraction of the total mass sequestered, resulting in a low intensity Raman spectral vibration at ∼810cm−1. Minimal changes in the thermal stability due to As(III) incorporation were measured. However, total mass loss occurred through multiple stages in As(III)-incorporated HTlcs compared to pure HTlc due to excess H2O absorption onto the surface and structural incorporation of CO3 2−.</subfield>
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