Experimental Study on the Effect of Fines Content on the Frost Swelling Characteristics of Coarse-Grained Soil in Canal Base Under Open System

Author:

Wang Miao123,Hai Mingwei4,Su Anshuang15,Meng Shangjiu6,Mu Hailong7,Guo Yanxiu8

Affiliation:

1. Heilongjiang Province Hydraulic Research Institute , Harbin 150050 , China ;

2. Harbin University of Science and Technology School of Architectural and Civil Engineering, , Harbin 150080 , China ;

3. Harbin Institute of Technology Department of Civil Engineering, , Harbin 150090 , China

4. Harbin University of Science and Technology School of Architectural and Civil Engineering, , Harbin 150080 , China

5. Nanjing Hydraulic Research Institute State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering, , Nanjing 210098 , China

6. Heilongjiang University of Science and Technology College of Architecture and Civil Engineering, , Harbin 154007 , China

7. China Earthquake Administration Institute of Engineering Mechanics, , Harbin 150080 , China

8. Heilongjiang Province Hydraulic Research Institute , Harbin 150050 , China

Abstract

Abstract Engineering usually considers coarse-grained soils as non-frost swelling soils, but serious frost swelling still occurs in coarse-grained canal bases, which is directly related to the recharge conditions and the fine particle content in the soil. Little attention is currently paid to the effect of different fine particle contents on coarse-grained soil frost swelling, especially after the fine particle admixture content exceeds 16%. This paper considers the characteristics of coarse-grained soils in water conservancy projects with fines content between 0% and 50%. The coarse-grained soils with 5%, 15%, 25%, 35%, and 45% fines content were designed for freezing and swelling tests. The evolution of temperature and moisture fields and the amount of freezing and swelling of coarse-grained soils during the freezing process were studied by using servo-type freezing and swelling and thawing tester. The experimental results show that the cooling process of soil samples can be divided into a rapid cooling stage, a slow cooling stage, and a freezing stabilization stage. The cooling rate and the frost heave amount with increasing fines content showed a trend of first increasing and then decreasing.

Funder

China Postdoctoral Science Foundation

Ministry of Water Resources

National Natural Science Foundation of China

Natural Science Foundation of Heilongjiang Province

Postdoctoral Foundation of Hei Long Jiang Province

Publisher

ASME International

Subject

Mechanical Engineering,Ocean Engineering

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