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Deformation and compaction of frozen soils
Luleå tekniska universitet, Institutionen för samhällsbyggnad och naturresurser, Geoteknologi.ORCID-id: 0000-0001-8739-2219
Luleå tekniska universitet, Institutionen för samhällsbyggnad och naturresurser, Geoteknologi.ORCID-id: 0000-0002-1365-8552
1994 (engelsk)Inngår i: Ground freezing 94: proceedings of the seventh International Symposium on Ground Freezing, Nancy, France, 24-28 October 1994 / [ed] Michel Fremond, Rotterdam: Balkema Publishers, A.A. / Taylor & Francis The Netherlands , 1994, s. 109-116Konferansepaper, Publicerat paper (Fagfellevurdert)
Abstract [en]

Frozen soils compaction are understood to give fills with low densities. Thus, relatively large deformations often occur when such fills melts. The most important factors influencing the obtained dry density, and consequently the thaw deformations, are compaction effort, temperature, water/ice content and soil type. A laboratory investigation was conducted in order to quantify the different factors influencing the obtained degree of compaction, as well as related thaw deformation. The results indicated that the water content of the soil is the most important factor for the obtained dry densities and for the thaw compressions

sted, utgiver, år, opplag, sider
Rotterdam: Balkema Publishers, A.A. / Taylor & Francis The Netherlands , 1994. s. 109-116
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URN: urn:nbn:se:ltu:diva-31723Lokal ID: 5fb19fd0-fc03-11dc-a946-000ea68e967bISBN: 90-5410-518-6 (tryckt)OAI: oai:DiVA.org:ltu-31723DiVA, id: diva2:1004957
Konferanse
International Symposium on Ground Freezing : 24/10/1994 - 28/10/1994
Merknad
Godkänd; 1994; 20080327 (cira)Tilgjengelig fra: 2016-09-30 Laget: 2016-09-30 Sist oppdatert: 2018-06-26bibliografisk kontrollert

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Totalt: 47 treff
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