Concrete strain is an important physical quantity for quantitative characterization of concrete deterioration under freeze-thaw cycling

but previous freeze-thaw test methods are difficult to reflect the strain evolution law of unsaturated concrete under different minimum freeze-thaw temperatures. We design and conduct sealed freeze-thaw tests and water-freeze-thaw tests on the hydraulic concrete specimens in four different saturation ranges (70 - 80%

85 - 91.7%

91.7 - 95%

and 95 - 100%) and three different freeze-thaw cycling temperature ranges (-18 to 6 ℃

-10 to 6 ℃

and -5 to 6 ℃). Based on the strain measured by strain sensors embedded in the specimen

we examine the strain evolving process of hydraulic concrete during a full cycle

including variations in its residual strain

thermal expansion coefficient

and frost heave coefficient at different saturations and different minimum freeze-thaw temperatures. The results reveal that as the cycling number increases

a continuous and irreversible deterioration leads to the freeze-thaw damage of unsaturated sealed freeze-thaw specimens and water-freeze-thaw specimens. And the residual strain of the latter specimen set is larger than that of the former set

and the higher the saturation

the greater the residual strain. The thermal expansion coefficient varies slightly with the cycling number

and the freeze-heave coefficient increases with saturation and the cycling number. The difference of these two sets in thermal expansion coefficients is relatively small

while the frost heave coefficient of the water-freeze-thaw set is significantly greater.