Abstract
AbstractDie Kinetik der O2‐Oxidation von Chalkocit, Cu2S, zu CuS in gepufferter wäßriger NH3‐ Lösung bei pH 10.5 und 30°C kann modellmäßig durch einen schrumpfenden Cu2S‐ Kern innerhalb einer sich verdickenden Schale aus CuxS (x 1) beschrieben werden.
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