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HYDROMETALURGICAL LEACHING EXPERIMENTS ON SELECTED MINERALS AND MATERIALS BY OXALIC ACID
Abstract
To investigate the reactivity of various mineral groups with oxalic acid, a series of long-term beaker experiments were conducted using a saturated solution of oxalic acid dihydrate (~50 g/100 mL) in distilled water, heated to >100 -C to enhance dissolution efficiency. The selected samples represented a broad range of mineralogical classes: brochantite (hydroxy-sulfate), malachite (carbonate hydroxide), pyrite (sulfide), chrysotile (silicate), and a Fe- and Cu-rich metallurgical slag containing complex, heterogeneous mineral phases. Each sample was fully submerged in the solution and left to react for at least 50 days under ambient laboratory conditions. Copper oxalate precipitated from both brochantite and malachite, while chrysotile produced magnesium oxalate dihydrate after extended exposure. No oxalate formation was observed in the pyrite sample. In contrast, the Fe-/Cu-slag yielded iron oxalate dihydrate, likely due to the presence of iron oxyhydroxides such as goethite. Neoformed crystalline phases were identified using Raman spectroscopy with a 785 nm excitation laser. These findings highlight the selective leaching capacity of oxalic acid, particularly for oxidized or hydroxylated mineral phases. The study demonstrates oxalic acid-s potential as a low-cost, selective, and environmentally friendly reagent for metal recovery from mine waste, low-grade ores, and complex industrial residues - offering promising implications for sustainable, scalable, and efficient hydrometallurgical applications in the circular economy.
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