Structural-phase transformations in bentonite after acid treatment
Author(s) -
М. Vlasova,
G. DominguezPatiño,
N. G. Kakazey,
Martha Lilia Domínguez-Patiño,
D. Juárez-Romero,
Enríquez Méndez
Publication year - 2003
Publication title -
science of sintering
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.309
H-Index - 25
eISSN - 1820-7413
pISSN - 0350-820X
DOI - 10.2298/sos0303155v
Subject(s) - montmorillonite , bentonite , hydrochloric acid , intercalation (chemistry) , fourier transform infrared spectroscopy , gypsum , materials science , phase (matter) , dehydration , ion exchange , cation exchange capacity , inorganic chemistry , barium , microanalysis , chemistry , nuclear chemistry , chemical engineering , ion , organic chemistry , geology , metallurgy , composite material , biochemistry , soil science , engineering , soil water
The methods of X-ray diffraction, Fourier transform infra-red spectroscopy (FTIR), X-ray microanalysis, electron microscopy, BET and cation exchange capacity (CEC) were used for investigation of the structural-phase transformations in bentonite under the influence of hydrochloric acid and temperature treatment (100-800ºC). It is established that in HCl medium during temperature treatment, dehydration and dehydroxilation of montmorillonite occur. The presence of gypsum and barium chloride results in an intercalation of interlayer space of montmorillonite by Ca and Ba ions Temperature treatment of intercalated montmorillonite leads to the formation of pores
Accelerating Research
Robert Robinson Avenue,
Oxford Science Park, Oxford
OX4 4GP, United Kingdom
Address
John Eccles HouseRobert Robinson Avenue,
Oxford Science Park, Oxford
OX4 4GP, United Kingdom