Dielectric study of dispersed ice microcrystals by the depolarization thermocurrent technique

Pissis, P; Apekis, L; Christodoulides, C; Boudouris, G

dc.contributor.author	Pissis, P	en
dc.contributor.author	Apekis, L	en
dc.contributor.author	Christodoulides, C	en
dc.contributor.author	Boudouris, G	en
dc.date.accessioned	2014-03-01T02:40:47Z
dc.date.available	2014-03-01T02:40:47Z
dc.date.issued	1983	en
dc.identifier.issn	0022-3654	en
dc.identifier.uri	https://dspace.lib.ntua.gr/xmlui/handle/123456789/30227
dc.subject.classification	Chemistry, Physical	en
dc.title	Dielectric study of dispersed ice microcrystals by the depolarization thermocurrent technique	en
heal.type	conferenceItem	en
heal.identifier.primary	10.1021/j100244a006	en
heal.identifier.secondary	http://dx.doi.org/10.1021/j100244a006	en
heal.language	English	en
heal.publicationDate	1983	en
heal.abstract	Dispersions of ice microcrystals obtained from the breakdown of water-in-oil emulsions were investigated by means of the depolarization thermocurrent (DTC) technique in the temperature range 85-250 K. Two predominant peaks were observed at temperatures of about 140 and 225 K. The low-temperature DTC peak at 140 K was studied extensively with different kinds of electrodes. Its position and shape were found to change in the course of time. The characteristics of the low-temperature DTC peak in dispersions of ice microcrystals at advanced states of evolution with time are discussed in relation to those of the low-temperature DTC in macroscopic pure ice. Our results provided more evidence that the low-temperature DTC peak in dispersions of ice microcrystals is due to dipolar absorption in ice. © 1983 American Chemical Society.	en
heal.publisher	AMER CHEMICAL SOC	en
heal.journalName	Journal of Physical Chemistry	en
dc.identifier.doi	10.1021/j100244a006	en
dc.identifier.isi	ISI:A1983RM39800006	en
dc.identifier.volume	87	en
dc.identifier.issue	21	en
dc.identifier.spage	4034	en
dc.identifier.epage	4037	en