This invention discloses a slope model
moisture migration testing device under freeze-thaw cycles, comprising: a model box containing a soil-
rock slope model, with the bottom of the model connected to an automatic water replenishment device. The automatic water replenishment device includes a
sample water replenishment tank, a
pressure balance pipe, and a Mariotte
bottle. A
fluorescent tracer is added to the
sample water replenishment tank to allow for
direct observation of the
moisture migration process within the slope. The freeze-thaw cycle
system of this device includes an upper cold bath plate, a cold bath device, a lower ambient temperature plate, an ambient temperature water pump, and connecting pipelines to simulate the freeze-thaw cycle of a slope caused by actual atmospheric environmental changes. The device includes a
laser displacement meter, a temperature sensor, a
data acquisition instrument, a computer, an
ultraviolet lamp, and a
digital camera to collect data on physical quantities such as displacement and temperature during the deformation process of the slope model, providing a quantitative analysis basis for the required research. By simulating the temperature rise and fall effects of the atmospheric environment on the slope model through the freeze-thaw cycle
system, the deformation and internal
moisture migration process of the slope model under freeze-thaw cycles are observed. This provides a basis for the mechanism research and prediction and early warning of geological disasters on slopes in cold regions.