Frost Heave Characteristics of Lined Canals with Sand-Gravel Replacement in Seasonally Frozen Regions

Xinjian Fan (), Fei Ye, Li Qin, Yupei Yan, Lirong Wang and Jiafang Wei
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Xinjian Fan: School of Civil and Hydraulic Engineering, Lanzhou University of Technology, Lanzhou 730050, China
Fei Ye: School of Civil and Hydraulic Engineering, Lanzhou University of Technology, Lanzhou 730050, China
Li Qin: Gansu Provincial Institute of Water Resources Science, Lanzhou 730050, China
Yupei Yan: Gansu Jingtaichuan Electric Power Irrigation Water Resource Utilization Center, Baiyin 730499, China
Lirong Wang: School of Civil and Hydraulic Engineering, Lanzhou University of Technology, Lanzhou 730050, China
Jiafang Wei: School of Civil and Hydraulic Engineering, Lanzhou University of Technology, Lanzhou 730050, China

Sustainability, 2025, vol. 17, issue 21, 1-18

Abstract: To address the frost heave damage issue of the trapezoidal lined canals in seasonally frozen regions and further ensure the stable operation of canals while reducing operation and maintenance costs, this study conducted a gradient sand-gravel cushion replacement experiment on the main canal of the Jingdian Irrigation District, China. For the experiment, east–west and north–south-oriented canal sections were selected, with frost heave meters and soil temperature-humidity meters installed. Dynamic changes in canal ground temperature, moisture content, and frost heave were monitored over two full freeze–thaw cycles. The results indicate the following: (1) The variation of ground temperature lags behind air temperature by 2–3 days; the ground temperature change on the canal slope is more pronounced than that at the canal bottom; and for the east–west-oriented canal, the ground temperature on the sunny slope is higher than that on the shady slope, while the ground temperatures on the two slopes of the north–south-oriented canal are similar. (2) The moisture content of the east–west-oriented canal changes drastically during the freezing period, showing a decreasing trend in the early freezing stage and a significant increasing trend in the thawing stage, whereas the moisture content of the north–south-oriented canal fluctuates slightly. (3) Canals with different orientations exhibit spatial differences in frost heave due to variations in solar radiation distribution. (4) The frost heave is negatively correlated with ground temperature, and its variation lags behind ground temperature by 1–2 days. (5) Increasing the replacement thickness of sand-gravel can significantly reduce the frost heave, with a reduction rate exceeding 50%. Under the action of freeze–thaw cycles, canals with gradient sand-gravel exhibit remarkable anti-frost effects. Thus, for trapezoidal lined canals in seasonally frozen regions, a gradient replacement scheme is recommended: For east–west canals, the replacement thickness is 40–100 cm for shady slopes and 30–70 cm for sunny slopes; for north–south canals, the replacement thickness is 30–70 cm for both slopes. In conclusion, gradient sand-gravel replacement is an effective anti-frost heave measure, providing a theoretical basis for the design of sand-gravel replacement for lined canals in seasonally frozen regions.

Keywords: seasonally frozen regions; trapezoidal lined canal; sand-gravel replacement; frost heave characteristics; anti-frost effect; field test; freeze–thaw cycle; hydrothermal migration (search for similar items in EconPapers)
JEL-codes: O13 Q Q0 Q2 Q3 Q5 Q56 (search for similar items in EconPapers)
Date: 2025
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