The reduction behavior of two Ni, Fe-rich dioctahedral smectite clays has been investigated by temperature-programmed reduction (TPR). For both clays, the reduction process of the transition metal elements occurs in two steps. At about 400 degrees C, Fe3+ is first reduced to Fe2+. At higher temperatures, further reduction of iron and reduction of nickel are achieved. Samples reduced at 400 degrees C and 700 degrees C have been characterized by X-ray diffraction (XRD), X-ray photoelectron spectroscopy (XPS), and Mossbauer spectroscopy (MS), and transmission electron microscopy (TEM). After a treatment at 700 degrees C, metallic particles deposited on the silicates has been evidenced by TEM and confirmed with the other techniques. (C) 2000 Elsevier Science B.V. All rights reserved.
Coelho, A., Ladrière, J., & Poncelet, G. (2000). Nickel, iron-containing clay minerals from Niquelandia deposit, Brazil 2. Behaviour under reducing conditions. Applied Clay Science, 17(3-4), 183-204. https://doi.org/10.1016/S0169-1317(00)00013-2 (Original work published 2000)