Temperature deformations of frozen soils caused by rapid changes in temperature


如何引用文章

全文:

开放存取 开放存取
受限制的访问 ##reader.subscriptionAccessGranted##
受限制的访问 订阅存取

详细

The results of the study of the temperature deformations for different types of frozen soils due to rapid temperature variations in cooling–heating cycles have been described. The difference in the patterns of the temperature deformation for step-like and single variations of temperature has been established. The dependence of the temperature deformation of frozen soil on the soil type, the total moisture, and the number of the cooling–heating cycles has been studied.

作者简介

S. Volokhov

Department of Geology

编辑信件的主要联系方式.
Email: volokhov@geol.msu.ru
俄罗斯联邦, Moscow, 119991

I. Nikitin

Department of Geology

Email: volokhov@geol.msu.ru
俄罗斯联邦, Moscow, 119991

D. Lavrov

LLC GeoProject Survey

Email: volokhov@geol.msu.ru
俄罗斯联邦, Moscow, 111024

补充文件

附件文件
动作
1. JATS XML

版权所有 © Allerton Press, Inc., 2017