Loading…

Increased strength and related mechanisms for mortars at cryogenic temperatures

•Compressive and flexural strengths of mortars at 20 °C to −170 °C were tested.•Water content is the main factor influencing the cryogenic strength increase.•The freezing of capillary water leads to rapid increase of strength.•Both ice formed in capillary pores and gel pores contributes to the cryog...

Full description

Saved in:
Bibliographic Details
Published in:Cryogenics (Guildford) 2018-09, Vol.94, p.5-13
Main Authors: Zhengwu, Jiang, Zilong, Deng, Xinping, Zhu, Wenting, Li
Format: Article
Language:English
Subjects:
Citations: Items that this one cites
Items that cite this one
Online Access:Get full text
Tags: Add Tag
No Tags, Be the first to tag this record!
Description
Summary:•Compressive and flexural strengths of mortars at 20 °C to −170 °C were tested.•Water content is the main factor influencing the cryogenic strength increase.•The freezing of capillary water leads to rapid increase of strength.•Both ice formed in capillary pores and gel pores contributes to the cryogenic strength increase. Properties of cement-based materials at cryogenic temperatures are quite different from those at room temperatures. The strength of mortars at cryogenic temperatures was experimentally studied and an empirical model was established. The freezing thermodynamic process of pore water and pore size distribution in mortars were characterized by differential scanning calorimeter (DSC) and thermoporometry (TPM), respectively. The relationship between the increased cryogenic strength and pore ice formation was discussed. The results showed that flexural strength of mortars increased at a higher rate than compressive strength. Water content and initial strength at room temperatures were the main factors influencing the cryogenic strength. Higher water content and higher initial strength resulted in higher cryogenic strength. Ice formation in pores is one of the main reasons for the mortar’s cryogenic strength increase. Nearly half of the water remained unfrozen in pores with radius less than 40 nm at −40 °C. Both ice formed in capillary pores and gel pores contributes to the strength increase observed at cryogenic temperatures.
ISSN:0011-2275
1879-2235
DOI:10.1016/j.cryogenics.2018.06.005