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XRD, FTIR, and thermal analysis of bauxite ore-processing waste (Red Mud) exchanged with heavy metals

Castaldi, Paola and Silvetti, Margherita and Santona, Laura and Enzo, Stefano and Melis, Pietro (2008) XRD, FTIR, and thermal analysis of bauxite ore-processing waste (Red Mud) exchanged with heavy metals. Clays and Clay Minerals, Vol. 5 (4), p. 461-469. eISSN 1552-8367. Article.

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DOI: 10.1346/CCMN.2008.0560407


The present work shows the results of X-ray diffraction (XRD), Fourier transform infrared (FTIR), and thermal analysis of untreated (RMnt) and acid-treated red mud (RMa), a bauxite ore-processing waste, exchanged with Pb2+, Cd2+, and Zn2+ cations. These studies were performed in order to investigate the changes in the sorbent structure caused by the exchange with metals of different ionic radii.

The XRD pattern of RMnt, analyzed according to the Rietveld method, showed a mixture of eight different phases. However, just three phases made up 78 wt.% of the RMnt: cancrinite (33 wt.%), hematite (29 wt.%), and sodalite (16 wt.%). X-ray diffraction patterns of RMnt exchanged with Pb2+ and Cd2+ cations revealed two additional phases, namely hydrocerussite [Pb3 (CO3)2 (OH) 2 (10 wt.%)] and octavite [CdCO3 (8 wt.%)].

These two phases probably originated from the carbonate precipitation processes which were due to the decarbonation of cancrinite. Hydrocerussite and octavite were not found in the case of acid-treated red mud samples.

In the FTIR spectra, the introduction of cations caused a distinct shift to higher wavenumbers in the peak at ~1100 cm–1, which is attributed to the asymmetric stretch of Si–O–Al. This effect may be associated with the Pb2+, Cd2+, and Zn2+ adsorbed by the red muds which caused a deformation of the initial structure.

Thermal analysis data of the red mud samples were obtained by thermogravimetric/differential thermogravimetric analysis, and these methods were employed to evaluate the desorption behavior of water and to clarify the thermal stability of the chemical phases of the different red mud samples. The loss of metal-bound water in the red mud samples was found to depend on the size of non-framework cations and water loss consistently followed the order: Zn2+>Cd2+>Pb2+.

Item Type:Article
ID Code:4934
Uncontrolled Keywords:Cancrinite, cations of Pb2+, Cd2+ and Zn2+, Hydrocerussite, Octavite, red muds, Sodalite
Subjects:Area 03 - Scienze chimiche > CHIM/02 Chimica fisica
Area 07 - Scienze agrarie e veterinarie > AGR/13 Chimica agraria
Divisions:001 Università di Sassari > 01 Dipartimenti > Chimica
001 Università di Sassari > 01 Dipartimenti > Scienze ambientali agrarie e biotecnologie agro-alimentari
Publisher:Clay Minerals Society
Deposited On:24 Nov 2010 10:08

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