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Thermal stability of hypercrosslinked polystyrene

As mentioned above, heating of hypercrosslinked polystyrene to 325°C for at least 1 h under protective argon atmosphere does not affect the porous structure and the apparent specific surfrce area of the material. StiU, this temperature should be considered as the material s upper stability limit. [Pg.287]

Interestingly, the presence of residual chlorine in the hypercrosslinked polymer enhances the yield of the final carbonizate (plot 1 in Fig. 7.48). It was found that the presence of carboxyl or sulfonic substituents in the aromatic rings of the polymer also enhances the yield of final carbons [207]. In fact it has been known [208] that sulfbnated styrene—DVB copolymers can be used for the preparation of carbonaceous adsorbing materials. However, because of the ehmination of heavy sulfonic substituents (over 40% of the material weight), the final yield of carbons is by no means hi er than in the [Pg.288]

This suggestion is directly corroborated by the emergence of very intensive signals of unpaired electrons in the electron paramagnetic (EPR) spectra of products pyrolyzed at 500-600°C [209]. Rupture of a stressed bond unavoidably results in a change of the conformation of the broken mesh, which places the formed radicals in positions unsuitable for their [Pg.289]

In general, pyrolysis of certain hypercrosslinked polystyrene materials at a temperature of about 600°C may result in interesting carbonaceous adsorbing materials with a yield of up to 55-60% within 50-60 min. The products maintain the spherical form of the initial materials and their overall texture, and acquire an exceptional mechanical strength of up to 8 kg per bead. They are basically nanoporous and show size-dependent adsorbing properties [207, 210]. In particular, they efficiently separate mineral ions in accordance with the new frontal ion size exclusion process [Pg.290]

The desweUing anomaly is particularly characteristic of the macroporous poly-DVB XAD-4, also containing a significant firaction of meso- and [Pg.291]


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