2002
DOI: 10.1002/app.10846
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Characterization of polyethylene/kaolin composites by polymerization filling with Cp2ZrCl2/MAO catalyst system

Abstract: ABSTRACT:In this work, the preparation and characterization of metallocene-catalyzed polyethylene (PE)/kaolin composites were presented. The composites was prepared by the so-called polymerization-filling method in which the PE matrix was formed directly on the kaolin surface by ethylene polymerization with the prefixed Cp 2 ZrCl 2 /methylaluminoxane (MAO) catalyst system on the kaolin surface. SEM, FTIR, and DMA were carried out to characterize the composites. The experimental results showed the new composite… Show more

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Cited by 6 publications
(3 citation statements)
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“…The intrinsic viscosity [η] of the PE constituent was determined in decalin at 135 °C after being extracted from the PE nanocomposites by hot xylene at elevated temperatures. M w was calculated from the following formula:24 …”
Section: Characterization Of the Pe Nanocompositesmentioning
confidence: 99%
“…The intrinsic viscosity [η] of the PE constituent was determined in decalin at 135 °C after being extracted from the PE nanocomposites by hot xylene at elevated temperatures. M w was calculated from the following formula:24 …”
Section: Characterization Of the Pe Nanocompositesmentioning
confidence: 99%
“…In comparison with metals and ceramics, polymers are much more inferior in mechanical properties Anjana et al [6]. The layered silicates (clay minerals) commonly used for the preparation of polymer composites belong to the family of 2:1 phyllosilicates, with kaolinite being one of the most common of such clay minerals Fowden et al, [7]. Their layered tetrahedral silica sheets are linked through oxygen atoms to the octahedral alumina sheets Fowden et al, [7].…”
Section: Introductionmentioning
confidence: 99%
“…The layered silicates (clay minerals) commonly used for the preparation of polymer composites belong to the family of 2:1 phyllosilicates, with kaolinite being one of the most common of such clay minerals Fowden et al, [7]. Their layered tetrahedral silica sheets are linked through oxygen atoms to the octahedral alumina sheets Fowden et al, [7]. These layers are separated by galleries where cations such as Na 1 , K 1 , etc., are present to counterbalance the negative charge of the aluminosilicate sheets arising from isomorphic substitution of Al or Si with other metals.…”
Section: Introductionmentioning
confidence: 99%