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- W3022341792 abstract "Hydrotalcites are a class of Mg-Al layered double hydroxide minerals with the ideal 3:1 Mg:Al endmember chemical composition Mg6Al2(A)(OH)16.n(H2O) (A = CO3 2- , SO4 2- , Cl - , etc). Hydrotalcites may occur naturally and are a common secondary mineral formed in soils during natural attenuation of acidic, metal-laden contaminated sites. Many acidic wastewaters generated during mineral processing often contain either Mg and/or Al in sufficient abundance that the potential exists for hydrotalcite formation providing there is addition of alkali to achieve a pH >5 and Mg and/or Al to attain a Mg:Al ratio between 2:1 and 3:1. Some Fe, typically present in acidic wastewaters, may also be accommodated within the hydrotalcite structure. Advantageously, hydrotalcites form rapidly and readily dewater. The utility of hydrotalcites, which could be precipitated as part of managing mine wastewaters, lies in their ability to incorporate a wide range of cationic (Cu" @default.
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- W3022341792 date "2010-01-01" @default.
- W3022341792 modified "2023-09-24" @default.
- W3022341792 title "Hydrotalcite formation for contaminant removal from mining wastewaters" @default.
- W3022341792 hasPublicationYear "2010" @default.
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