Thermal dehydroxylation of kaolinite under isothermal conditions

被引:132
作者
Gasparini, Elisa [1 ]
Tarantino, Serena C. [1 ]
Ghigna, Paolo [2 ]
Riccardi, M. Pia [1 ]
Cedillo-Gonzalez, Erika I. [3 ]
Siligardi, Cristina [3 ]
Zema, Michele [1 ]
机构
[1] Univ Pavia, Dipartimento Sci Terra & Ambiente, I-27100 Pavia, Italy
[2] Univ Pavia, Dipartimento Chim, I-27100 Pavia, Italy
[3] Univ Modena & Reggio Emilia, Dipartimento Ingn Mat & Ambiente, I-41100 Modena, Italy
关键词
Kaolinite; Dehydroxylation; Kinetics; X-ray diffraction; FT-IR; Autocorrelation analysis; MULLITE REACTION SEQUENCE; NUCLEAR-MAGNETIC-RESONANCE; OUTSTANDING PROBLEMS; CRYSTAL-CHEMISTRY; KINETIC-ANALYSIS; TRANSFORMATIONS; DECOMPOSITION; TEMPERATURE; BEHAVIOR; SI-29;
D O I
10.1016/j.clay.2013.07.017
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 ; 081704 ;
摘要
The dehydroxylation reaction of kaolinite from the industrial kaolin SI-K (Germany) has been studied by thermal analyses (TG, DTA) and ex situ annealing experiments. Heating experiments were performed at 450, 500, 550 and 600 degrees C. At each working temperature, different heating times were used in order to follow the evolution of the dehydroxylation process with time until completion of the reaction. Every heating run was performed on a new batch of sample, which was weighted before and after the heat-treatment. At the end of the heating run, each sample was characterised by X-ray powder diffraction (XRPD) and FT-infrared attenuated total reflectance spectroscopy (FTIR-ATR). The dehydroxylation process was followed by monitoring the gradual mass loss and the corresponding decrease in intensity of the most significant peaks both in the diffraction patterns (disappearing of kaolinite peaks) and in the FTIR-ATR spectra (disappearing and changes in OH and Si-O-Al bands), as determined by peak-profile and autocorrelation analyses. A kinetic analysis was performed using the Avrami method on the basis of sample mass loss and changes in the intensities of XRPD and FTIR-ATR peaks under isothermal conditions. Two temperature regimes are found, with only the data in range 500-600 degrees C being isokinetic. The activation energy values obtained in this temperature range on the basis of the three measured parameters are comparable and are between 127 and 139 kJ mol(-1). (C) 2013 Elsevier B.V. All rights reserved.
引用
收藏
页码:417 / 425
页数:9
相关论文
共 60 条
[1]  
[Anonymous], 1974, Differential Thermal Analysis: Application and Results in Mineralogy
[2]   In situ powder diffraction studies of temperature induced transformations in minerals [J].
Artioli, G .
NUCLEAR INSTRUMENTS & METHODS IN PHYSICS RESEARCH SECTION B-BEAM INTERACTIONS WITH MATERIALS AND ATOMS, 1997, 133 (1-4) :45-49
[3]   Kinetics of phase change I - General theory [J].
Avrami, M .
JOURNAL OF CHEMICAL PHYSICS, 1939, 7 (12) :1103-1112
[4]  
BAILEY S.W., 1980, Crystal structures of clay minerals and their X-ray identification, P1
[5]  
Balan E, 2001, AM MINERAL, V86, P1321
[6]   Line-broadening effects in the powder infrared spectrum of apatite [J].
Balan, Etienne ;
Delattre, Simon ;
Roche, Damien ;
Segalen, Loic ;
Morin, Guillaume ;
Guillaumet, Maxime ;
Blanchard, Marc ;
Lazzeri, Michele ;
Brouder, Christian ;
Salje, Ekhard K. H. .
PHYSICS AND CHEMISTRY OF MINERALS, 2011, 38 (02) :111-122
[7]   Low-temperature infrared spectroscopic study of OH-stretching modes in kaolinite and dickite [J].
Balan, Etienne ;
Delattre, Simon ;
Guillaumet, Maxime ;
Salje, Ekhard K. H. .
AMERICAN MINERALOGIST, 2010, 95 (8-9) :1257-1266
[8]  
Balek V, 1996, THERMOCHIM ACTA, V283, P385
[9]   Local structure of ferric iron-bearing garnets deduced by IR-spectroscopy [J].
Ballaran, TB ;
Woodland, AB .
CHEMICAL GEOLOGY, 2006, 225 (3-4) :360-372
[10]  
BELLOTTO M, 1995, PHYS CHEM MINER, V22, P207, DOI 10.1007/BF00202253