3.1. Effect of Excretion Conditions on Frost Heave Force
In order to explore the freezing process of the voided water behind the lining and the formation mechanism of frost heave force, a frost heave test of voided water behind the lining was carried out. The test model is composed of two concrete specimens with dimensions of 0.4 m × 0.4 m × 0.2 m, and the size of the hollow cavity is set to 0.2 m × 0.2 m × 0.1 m, as shown in
Figure 2. A temperature sensor is embedded in the model to monitor whether the water in the cavity is frozen; a film pressure sensor is also installed to test the frost heave force.
Set the test conditions according to the tunnel emptying form, that is:
Working condition 1: During the freezing process of type I emptying water, the water supply and discharge channels do not freeze;
Working condition 2: During the freezing process of type II emptying water, the water supply and drainage channels are frozen first, and the water body in the model freezes later.
By freezing the bottom of the specimen, it was found that: in working condition 1, the freezing process of the water body in the cavity develops from the bottom upward, and the frost heave force in the cavity is almost zero; in working condition 2, the freezing process of the water body in the cavity Also developing upward from the bottom of the cavity, a large frost heave force is generated in the cavity, with the average pressure reaching 0.16 MPa.
3.2. Frost-Heaving Mechanism of Voided Water behind Lining under Short-Period Fluctuation Conditions
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Numerical simulation plan
This article uses FLUENT simulation software and based on the Solidification/Melting model to analyze the process of freezing of the dewatered water behind the lining under the condition of short-period fluctuations in lining surface temperature. Considering that tunnel vault voids often occur at the highest point of each mold lining near the end formwork, and the void cavities formed by concrete pouring are mostly circular wedge and flying saucer shapes, circular wedge and flying saucer shaped void models were established.
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Boundary conditions
According to the monitoring results of the tunnel temperature field, considering the situation where the short-period temperature amplitude of the tunnel reaches 15 ℃ under extreme conditions, the short-period fluctuation function of T0=-5+15×sin(2πt/24+φ) is used as the temperature loading on the lining surface function, the lining surface adopts a convective boundary.
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Supply and excretion conditions
Based on the supply and discharge conditions of groundwater, two working conditions of top channel and lateral channel are designed. As shown in
Figure 3 and
Figure 4, the left side shows the shape of the hollow cavity, and the right side shows the location of the supply and excretion channels. In the x-y cross-sectional view of Figure 6, the drainage channel is located at the top of the hollow cavity, which corresponds to the working conditions in which water seeps into the cavity after the waterproof panel on the tunnel vault is damaged; in the y-z cross-section of
Figure 3 and
Figure 4, the drainage channel is located on the side of the cavity, corresponding to the tunnel arch waist and other parts. Water seepage, water seepage enters the vault cavity along the waterproof board.
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Grid and parameters
The concrete and water-filled cavity within the void range of the vault are selected as the research object. The longitudinal length of the circular wedge-shaped and flying saucer-shaped voids is 2.0 m, and the maximum height of the void is 20 cm. The parameters selected for simulation are shown in
Table 1.
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Freezing and thawing analysis of empty accumulated water
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Freezing process of water inside the void
Figure 5 and
Figure 6 show the freezing process of water accumulation in circular wedge-shaped voids and flying saucer-shaped voids in the tunnel lining respectively.
It can be seen from
Figure 5 that during the cooling process, the freezing of the voided water behind the lining starts from the edge of the voided cavity and develops from the thinnest part of the voided cavity to the thicker part; during the freezing process, the freezing of the voided water at the side of the voided cavity The excretory channels (y-z cross-section) freeze first, and the channels at the top of the void freeze last (x-y cross-section).
It can be seen from
Figure 6 that the freezing process of the voided water behind the lining also starts from the edge of the voided cavity and develops from the thinnest part of the voided cavity to the thicker part; during the freezing process, the freezing process is located at the side of the voided cavity (x-y cross-sectional view ) and the excretory channels at the top (y-z section view) are frozen first.
In general, the freezing sequence of water in the cavity is related to the height of the cavity and has nothing to do with temperature fluctuations. The smaller the thickness of the water body in the cavity, the easier it is for the water body to freeze. Under short-period fluctuation conditions, temperature fluctuations only affect the freezing rate of water and have no effect on the sequence of frozen parts.
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Melting process of water inside the void
Under short-period fluctuation conditions, when a positive temperature occurs in the lining structure, the ice formed starts to melt from the thinnest part, and then develops to the thicker part. This is the same as the freezing development process, that is, the ice that freezes first when cooling. place, it is also the first to melt when the temperature rises, as shown in
Figure 7.
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The formation mechanism of frost heave force within the void
For Type I voiding, the freeze-thaw cycle basically does not produce frost heave force. Since the hollowed-out top surface is the initial support, it can be considered that the entire top surface is a drainage channel. Under the condition of short-term temperature fluctuations, whether it is freezing or thawing, the groundwater supply and drainage channels will remain open, and frost heaving will basically not occur. force.
For type II voiding, the frost-heaving force in the cavity will gradually increase under freeze-thaw cycles. Since the top surface of the hollow is a waterproof layer, the water accumulated in it is the seepage of groundwater flowing through the contact surface of the lining and waterproof layer into the hollow cavity. The groundwater infiltration channels are located at the edge of the hollow cavity, where the thickness of the water body in the cavity is the largest. Thin, it is the first part to be frozen during the freezing process. Therefore, under the condition of short-term temperature fluctuations, when the temperature drops and freezes, the drainage channel freezes first, causing frost heaving force in the cavity; when the temperature rises and melts, the drainage channel melts first, and the cavity volume increases due to frost heaving of accumulated water, and the new water body along the channel into the cavity. When freezing again, the excretion channel is also frozen first, causing frost heaving force in the cavity and causing the cavity volume to increase again. That is, under the condition of short-term temperature fluctuations, the water body in the cavity will undergo a cyclic process of frost heaving - melting, water supply - and then frost heaving. This will lead to the frost heaving force of the structure under the conditions of short-term temperature fluctuations gradually increasing, and lining cracks will occur., or even blockage, collapse and other diseases.