Abstract
The delay of the closure of frozen wall occurs frequently due to the excessive groundwater seepage in the construction of deep shaft using artificial freezing technology. The same problem also appears in the freezing construction of new westerly shaft in Pansan Coal Mine of Huainan, whose located stratum suffers from the groundwater seepage of 7.96 m/d. Obviously, the original three-loop pipe freezing scheme under the static water condition is not applicable; it must be optimized to meet the construction requirements. Therefore, the evolution law of temperature field of deep shaft freezing wall under different groundwater seepage velocities was studied based on the coupled equations of temperature and seepage field using COMSOL Multiphysics finite element program. Finally, the optimal freezing scheme of new westerly shaft was proposed and applied to practical engineering. Compared with the original freezing scheme, the optimized freezing scheme shortened the closure time of freezing wall and increased the effective thickness of freezing wall, which ensured the safety of deep shaft construction and produced good social benefit.
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Data availability
The datasets generated and analyzed during the current study are available from the corresponding author upon reasonable request.
Abbreviations
- T :
-
Soil temperature (°C)
- t :
-
Freezing time (d)
- C * :
-
Equivalent volume specific heat (kJ/(m3·°C))
- k * :
-
Equivalent thermal conductivity (W/(m·°C))
- C f :
-
Volumetric heat capacity of frozen soil (kJ/(m3·°C))
- C u :
-
Volumetric heat capacity of unfrozen soil (kJ/(m3·°C))
- C w :
-
Volumetric heat capacity of water (kJ/(m3·°C))
- ρ f :
-
Density of frozen soil (kg/m3)
- ρ u :
-
Density of unfrozen soil (kg/m3)
- ρ w :
-
Density of water (kg/m3)
- c f :
-
Mass specific heat of frozen soil (kJ/(kg·°C))
- c u :
-
Mass specific heat of unfrozen soil (kJ/(kg·°C))
- k f :
-
Thermal conductivity of frozen soil (kJ/(m·d·°C))
- k u :
-
Thermal conductivity of unfrozen soil (kJ/(m·d·°C))
- T d :
-
Freezing temperature (°C)
- T r :
-
Thawing temperature (°C)
- L :
-
Latent heat (kJ/m3)
- T 0 :
-
Initial temperature (°C)
- (x p, y p):
-
Cartesian coordinates of freeze pipe
- T c(t):
-
Surface temperature of freeze pipe (°C)
- ρ l :
-
Density of fluid (kg/m3)
- \(\overrightarrow{u}\) :
-
Relative velocity vector of water flow (m/d)
- K :
-
Permeability coefficient
- P :
-
Osmotic pressure
- α l :
-
Expansion coefficients of water
- α s :
-
Expansion coefficients of soil particle
- Q m :
-
Source sink term of seepage field
- K 0 :
-
Permeability coefficients of frozen zone
- Kf :
-
Permeability coefficients of unfrozen zone
- θ s :
-
Volume content of soil
- θ w :
-
Volume content of water
- θ i :
-
Volume content of ice
- χ :
-
Unfrozen water content
- C eff :
-
Equivalent volume heat capacity
- λ eff :
-
Effective thermal conductivity
- Q 1 :
-
Convective heat
- Q H :
-
Phase change heat
- Q G :
-
Source sink term of temperature field
- ε :
-
Initial porosity of soil
- Re :
-
Reynolds number
- v :
-
Seepage velocity (m/d)
- d 10 :
-
Effective particle size of soil
- η :
-
Dynamic viscosity coefficient (m2/s)
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Funding
This research was supported by the National Natural Science Foundation of China (Grant No. 51778004), Research Activities Funding for Reserve Candidate of Academic and Technical Leaders of Anhui Province, China (Grant No. 2018H170), and Academic Funding for Top-notch Talents in University Disciplines (Majors) of Anhui Province, China (Grant No. gxbjZD10).
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Cai, H., Yao, F., Hong, R. et al. Multi-loop pipe freezing optimization of deep shaft considering seepage effect. Arab J Geosci 15, 153 (2022). https://doi.org/10.1007/s12517-022-09447-y
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DOI: https://doi.org/10.1007/s12517-022-09447-y