Long-Term Thermal Performance of Group of Energy Piles in Unsaturated Soils under Cyclic Thermal Loading
Abstract
:1. Introduction
2. Finite Element Modelling
2.1. Soil Moisture Transfer Mechanism
2.2. Dry Air Transfer Mechanism
2.3. Soil Heat Transfer Mechanism
2.4. Numerical Modelling
2.4.1. Geometry Description
2.4.2. Initial Conditions
2.4.3. Boundary Conditions
2.5. Material Parameters
2.5.1. Thermal Conductivity
2.5.2. Soil-Water Characteristic Curve and Unsaturated Hydraulic Conductivity
3. Numerical Simulation
3.1. Case 1: Heating and Cooling of All the GEPs in the Group
3.2. Case 2: Heating and Cooling of Alternate GEPs in the Group
4. Numerical Simulation
4.1. Case 1: Heating and Cooling of All the GEPs in the Group
4.1.1. Temperature Evolution
4.1.2. Radial Temperature Distribution
4.1.3. Temperature Distribution with Depth
4.1.4. Degree of Saturation with Depth
4.2. Case 2: Heating and Cooling of Alternate GEPs in the Group
4.2.1. Temperature Evolution
4.2.2. Radial Temperature Distribution
4.2.3. Temperature Distribution with Depth
4.2.4. Degree of Saturation with Depth
5. Conclusions
- The maximum temperature magnitude in all the simulations were observed at point B, i.e., the mid-point for all the group of GEPs. This could be as a result of the contribution of heat radiating from all the four GEPs towards the centre (point B). In addition, the temperature magnitude at this location and all the other locations decreases as the initial degree of saturation of the soil increases from 0% to 100% in the sand and the clay soils.
- Similarly, the temperature magnitudes at locations A, B, and C were observed to be higher in the sand than in clays. This phenomenon can be described based on the thermal conductivity of the two soils: sand and clay. The lower thermal conductivity values in clays permit the development of greater temperature magnitude around the GEPs and prevent heat from radiating away to greater distances in the soil domain. In contrast, in the case of sand, its thermal conductivity was about twice that of the clay as the two soils approach full saturation. This allows the sand to easily transfer heat to greater distances within the soil whilst preventing the development of greater temperature magnitudes at the regions close to the GEPs. Similarly, soil permeability is another factor that is greater in sands and allows heat to be easily transferred via convection due to its high porosity.
- The continuous heating and cooling cycles of the GEPs, during the 10 years of numerical simulations, resulted in a continuous decrease in temperature trend at all the observed locations (i.e., A, B, and C, respectively). This could be as a result of the continuous heat injection and extraction mode without allowing the system any opportunity to recover throughout the period of the numerical simulations. However, adopting intermittent heating and cooling mode of operation permits the soil domain to naturally recover and prevent excessive heat build-up or deficit in the soil [46]. This is important in safeguarding the long-term thermal performance of the system.
- In addition, thermally activating some selected and alternate GEPs in the group results in lower temperature magnitude at all the observed locations in the soil domain, and the temperature change decreases with an increase in soil saturation. This is a result of the increase in the spacing between the GEPs that are thermally activated, thus allowing greater soil volume for heat rejection and solicitation. This is especially important where the structural pile foundation elements are situated close to each other and/or where they are installed in problematic clays. This could lead to the heaving or contraction of the clays and the GEPs due to excessive heat injection or extraction. Thus, thermally activating alternate GEPs offers an alternative approach towards installing an energy-efficient GEP system, and ensure the longevity of the system.
- Furthermore, temperatures that are well below freezing were observed at some point during the simulations. It is strongly advised that the application of any temperature magnitude that could result in extreme changes to the soil and pile(s) should be avoided. Because the superimposition of extreme heating and cooling loads results in the expansion and contraction of the pile(s). This phenomenon has a negative consequence on the structural integrity of the pile(s).
- Lastly, future investigations should employ a 3D modelling approach to investigate the effect of thermally activating all the GEPs and alternate ones and compare with the findings here. In addition, the application of equal total thermal load on the GEPs in both cases should be investigated.
Author Contributions
Funding
Data Availability Statement
Conflicts of Interest
Nomenclature
Abbreviation | |
GSHP | Ground source heat pump |
GEP | Geothermal energy pile |
HCF | Heat carrier fluid |
HDPE | High density poly-ethylene |
DTN | Dynamic Thermal Network |
LCA | Life cycle analysis |
FEM | Finite element modelling |
TH | Thermo-hydraulic |
COMPASS | COde for Modelling PArtially Saturated Soils |
THM-C | Thermo-Hydraulic-Mechanical and Chemical |
SWCC | Soil water characteristic curve |
PVC | Polyvinyl chloride |
Parameters | |
Cps | Specific heat capacity of solid soil particles [J/(kg K)] |
Cpl | Specific heat capacity of liquid [J/(kg K)] |
Cpv | Specific heat capacity of vapour [J/(kg K)] |
Cpda | Specific heat capacit of dry air [J/(kg K)] |
Datms | Molecular diffusivity of vapour through air |
h | Relative humidity (%) |
Hs | Henry’s volumetric coefficient of solubility |
kl | Intrinsic permeability (m/s) |
Kl | Unsaturated hydraulic conductivity (m/s) |
ksat | Saturated hydraulic conductivity (m/s) |
L | Latent heat of vaporisation (J/kg) |
n | Soil porosity |
q | Heat flux (W/m2) |
Q | Heat flow per unit length (W/m) |
s | Suction (MPa) |
Sa | Degree of saturation of pore air (%) |
Sl | Degree of saturation of pore water (%) |
t | time (seconds) |
T | temperature (K) |
Ti | Reference temperature (K) |
Pore air pressure (Pa) | |
Pore water pressure (Pa) | |
va | Velocities of air (m/s) |
vl | Velocities of liquid (m/s) |
vv | Velocities of vapour (m/s) |
Mass flow factor | |
z | Elevation (m) |
Greek Symbols | |
γl | Unit weight of liquid (kN/m3) |
∂V | Incremental volume (m3) |
δ, ε, φ, ϕ | Constant fitting parameter |
θ | Volumetric moisture content |
θa | Volumetric air content |
θl | Volumetric liquid content |
θlr | Residual volumetric liquid water content |
θls | Saturated volumetric liquid water content |
λs | Coefficient of thermal conductivity of unsaturated soil [W/(m·K)] |
λdry | Coefficient of thermal conductivity of dry soil [W/(m·K)] |
λsat | Coefficient of thermal conductivity of saturated soil [W/(m·K)] |
μl | Absolute viscosity of pore liquid (Pas) |
ρd | Dry density (Kg/m3) |
ρda | Density of dry air (kg/m3) |
ρl | Density of liquid water (kg/m3) |
ρo | Saturated vapour density (kg/m3) |
ρs | Density of solid soil particles (Kg/m3) |
ρv | Density of water vapour (kg/m3) |
Ω | Heat content |
∇ | Gradient operator |
Microscopic pore temperature gradient factor |
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GEP (m) | Element Size in Soil Domain | No. of Elements | ||
---|---|---|---|---|
Along Radial Axis (m) | Along Depth (m) | |||
case A | 1 | 1 | 1 | 2350 |
case B | 0.1 | 1 | 1 | 3200 |
case C | 0.05 | 0.5 | 0.2 | 24,320 |
case D | 0.15 | 0.5 | 0.5 | 9400 |
case E | 0.1 | 0.5 | 0.2 | 17,000 |
case F | 0.1 | 0.5 | 0.5 | 10,700 |
case G | 0.1 | 0.5 | 1 | 5350 |
Initial Temperature, To (K) | Saturation, Sl (%) | Soil suction, s (MPa) | |
---|---|---|---|
286.55 | Sand | Clay | |
0 | 1 | 103 | |
30 | 2.5 × 10−3 | 2.3 | |
60 | 2.4 × 10−3 | 0.8 | |
100 | 0 | 0 |
Parameter | Sand | Clay | Concrete |
---|---|---|---|
Hydraulic Parameters | |||
ksat (m/s) | 1.3 × 10−3 | 1.02 × 10−10 | 1.02 × 10−10 |
Kl (m/s) | Kl = (Sl)δ ksat; δ = 3 | – | |
Sl (%) | ranges from 0–100% | ||
van Genuchten [40] fitting parameters | φ = 0.645 | φ = 0.015 | – |
ε = 5.905, | ε = 1.9, | ||
ϕ = 0.831, | ϕ = 0.474, | ||
θlr = 0.0025, | θlr = 0.0001, | ||
θls = 0.356 | θls = 0.38 | ||
Thermal Parameters | |||
λ (W/m K) | λs = f (Sl) | 1.62 | |
Cps (J/kg K) | 700 | 800 | 800 |
Cpv (J/kg K) | 1870 | 1870 | 1870 |
Cpw (J/kg K) | 4200 | 4200 | 4200 |
Other Parameters | |||
ρd (Kg/m3) | 2570 | 2630 | 2630 |
n | 0.356 | 0.38 | 0.38 |
L (J/kg) | 2,400,000 | ||
Hs | 0.02 |
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Sani, A.K.; Singh, R.M. Long-Term Thermal Performance of Group of Energy Piles in Unsaturated Soils under Cyclic Thermal Loading. Energies 2021, 14, 4122. https://doi.org/10.3390/en14144122
Sani AK, Singh RM. Long-Term Thermal Performance of Group of Energy Piles in Unsaturated Soils under Cyclic Thermal Loading. Energies. 2021; 14(14):4122. https://doi.org/10.3390/en14144122
Chicago/Turabian StyleSani, Abubakar Kawuwa, and Rao Martand Singh. 2021. "Long-Term Thermal Performance of Group of Energy Piles in Unsaturated Soils under Cyclic Thermal Loading" Energies 14, no. 14: 4122. https://doi.org/10.3390/en14144122