Nizkotyempyeraturnaya dielyektrichyeskaya ryelaksatsiya vo l{cyrillic small soft sign}du: nyezavisimost{cyrillic small soft sign} ot kontsyentratsii primyesyei{cyrillic, short}

Pissis, P; Apekis, L; Boudouris, G

dc.contributor.author	Pissis, P	en
dc.contributor.author	Apekis, L	en
dc.contributor.author	Boudouris, G	en
dc.date.accessioned	2014-03-01T01:06:00Z
dc.date.available	2014-03-01T01:06:00Z
dc.date.issued	1981	en
dc.identifier.issn	03693554	en
dc.identifier.uri	https://dspace.lib.ntua.gr/xmlui/handle/123456789/9111
dc.subject	Dielectric Relaxation	en
dc.subject	Low Temperature	en
dc.subject	Water Use	en
dc.title	Nizkotyempyeraturnaya dielyektrichyeskaya ryelaksatsiya vo l{cyrillic small soft sign}du: nyezavisimost{cyrillic small soft sign} ot kontsyentratsii primyesyei{cyrillic, short}	en
heal.type	journalArticle	en
heal.identifier.primary	10.1007/BF02721284	en
heal.identifier.secondary	http://dx.doi.org/10.1007/BF02721284	en
heal.publicationDate	1981	en
heal.abstract	Polycrystalline ice samples have been investigated by means of the depolarization thermocurrent (DTC) method in the range (90÷240) K in terms of the conductivity of the water used in the range (1.1·10-3÷1.9·10-6) Ω-1 cm-1. The low-temperature DTC peak at about 124 K by a heating rate of 3.5 K/min has been found to be independent of the water purity. There is some evidence that this peak is due to dipolar relaxation in ice. The relaxation mechanism seems to be independent of the concentration of extrinsic defects. It must be considered as an intrinsic property of ice. © 1981 Società Italiana di Fisica.	en
heal.publisher	Società Italiana di Fisica	en
heal.journalName	Il Nuovo Cimento B	en
dc.identifier.doi	10.1007/BF02721284	en
dc.identifier.volume	62	en
dc.identifier.issue	2	en
dc.identifier.spage	365	en
dc.identifier.epage	374	en