Temperature Dependence of Nickel Stabilization in Inorganic Oxide Matrices: Fid-Bau Portal

Temperature Dependence of Nickel Stabilization in Inorganic Oxide Matrices

Wei, Yu-Ling / Huang, Hui-Chin / Wang, Hsi-Chih / Yang, Yao-Wen / Lee, Jyh-Fu

Scanning electron microscopy, X‐ray diffractometry, X‐ray absorption spectroscopy, and other means are used to investigate the effect of thermal treatment temperature, 105–1100 °C, on the immobilization of nickel (Ni) by the inorganic oxides of latosol. Ni is more firmly immobilized by the latosol with increasing temperature. Spectral analyses indicate that a shoulder toward the edge‐jump appears in the spectra of X‐ray absorption near‐edge structure for the samples heated at 900 and 1100 °C. Moreover, the intensity of the main peak at the edge increases with higher temperature; this information indicates the distortion of the divalent nickel [Ni(II)] environment in the samples heated at 900 and 1100 °C. Nevertheless, the distortion is absent from the samples heated at 105 and 500 °C. The fact of the distortion of the Ni(II) environment suggests the occurrence of a chemical reaction between the Ni compound and the inorganic matrices of the latosol soil during the heating process at 900 and 1100 °C. In addition, the extended X‐ray absorption fine structure results correspond well to the X‐ray absorption near‐edge structure results; the former are supportive of the occurrence of a distorted Ni(II) environment in the samples heated at 900 and 1100 °C. The wet‐chemistry results show that the samples heated at 900–1100 °C leach less Ni than the 105–500 °C samples do. The change of the Ni environment is related to the observation that less Ni is leached from the samples heated at 900–1100 °C. Furthermore, the pore closing phenomenon is observed only in the 1100 °C sample; this phenomenon corresponds with the fact that the 1100 °C sample leaches less Ni than the 900 °C sample does.