MICROSTRUCTURE OF HDTMA+-MODIFIED MONTMORILLONITE AND ITS INFLUENCE ON SORPTION CHARACTERISTICS

dc.contributor.authorHe H.
dc.contributor.authorZhou Q.
dc.contributor.authorMartens W.N.
dc.contributor.authorKloprogge T.J.
dc.contributor.authorYuan P.
dc.contributor.authorXi Yu.
dc.contributor.authorZhu J.
dc.contributor.authorFrost R.L.
dc.date.accessioned2024-09-22T02:54:14Z
dc.date.available2024-09-22T02:54:14Z
dc.date.issued2006
dc.description.abstractA series of organoclays with monolayers, bilayers, pseudotrilayers, paraffin monolayers and paraffin bilayers were prepared from montmorillonite by ion exchange with hexadecyltrimethylammonium bromide (HDTMAB). The HDTMAB concentrations used for preparing the organoclays were 0.5, 0.7, 1.0, 1.5, 2.0 and 2.5 times the montmorillonite cation exchange capacity (CEC). The microstructural parameters, including the BET-N2 surface area, pore volume, pore size, and surfactant loading and distribution, were determined by X-ray diffraction, N2 adsorption-desorption and high-resolution thermogravimetric analysis (HRTG). The BET-N2 surface area decreased from 55 to 1 m2/g and the pore volume decreased from 0.11 to 0.01 cm3/g as surfactant loading was increased from Na-Mt to 2.5CEC-Mt. The average pore diameter increased from 6.8 to 16.3 nm as surfactant loading was increased. After modifying montmorillonite with HDTMAB, two basic organoclay models were proposed on the basis of HRTG results: (1) the surfactant mainly occupied the clay interlayer space (0.5CEC-Mt, 0.7CEC-Mt, 1.0CEC-Mt); and (2) both the clay interlayer space and external surface (1.5CEC-Mt, 2.0CEC-Mt, 2.5CEC-Mt) were modified by surfactant. In model 1, the sorption mechanism of p-nitrophenol to the organoclay at a relatively low concentration involved both surface adsorption and partitioning, whereas, in model 2 it mainly involved only partitioning. This study demonstrates that the distribution of adsorbed surfactant and the arrangement of adsorbed HDTMA+ within the clay interlayer space control the efficiency and mechanism of sorption by the organoclay rather than BET-N2 surface area, pore volume, and pore diameter.
dc.identifierhttps://www.elibrary.ru/item.asp?id=51641174
dc.identifier.citationClays and Clay Minerals, 2006, 54, 6, 689-696
dc.identifier.doi10.1346/ccmn.2006.0540604
dc.identifier.issn0009-8604
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/45335
dc.subjectBET-N2 SURFACE AREA
dc.subjectHDTMA+
dc.subjectORGANOCLAY
dc.subjectPORE SIZE
dc.subjectPORE VOLUME
dc.subjectSORPTION EFFICIENCY
dc.subjectSURFACTANT LOADING
dc.subjectSORPTION MECHANISM
dc.titleMICROSTRUCTURE OF HDTMA+-MODIFIED MONTMORILLONITE AND ITS INFLUENCE ON SORPTION CHARACTERISTICS
dc.typeСтатья

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