# Steady-State Convection in a Saturated Porous Medium Heated from Above

Note

To view this project in FLAC3D, use the menu command . Choose “Thermal/NaturalAdvection” and select “NaturalAdvection.prj” to load. The project’s main data files are shown at the end of this example.

This example shows the effect of temperature-dependent density on the pore-pressure distribution for heating applied from above a saturated porous layer of large lateral extent. The thickness of the layer is \(b\). The temperature is fixed at \(T_1\) at the base of the layer and at \(T_0 > T_1\) at the top. The boundaries are impermeable to fluid flow; the problem is one-dimensional. For zero specific discharge, the steady-state temperature solution is

where \(x\) is measured down, from the top of the layer. Assuming no fluid flow, we have

Using \(\rho = \rho_0[1 - \beta (T - T_r)]\), where \(T_r\) is a reference temperature and \(T\) is given by the temperature solution (Equation (1)), integration of this equation gives

where \(p_0\) is a reference pressure.

To simulate the problem with FLAC3D, we first establish the temperature field and cycle in flow mode
until the steady-state pore pressure solution is reached. For the case treated, the relative
pore-pressure error calculated at the end of the simulation is negligible (less than 10^{-5}%;
see Figure 1).

Data File

```
model new
model title 'conduction and natural convection in a porous layer'
fish automatic-create off
model config fluid thermal
program call "fishFunctions"
[setup]
; --- geometry ---
zone create brick size 5 5 10 point 0 (-5e3,-5e3,-5e3) ...
point 1 (5e3,-5e3,-5e3) ...
point 2 (-5e3,5e3,-5e3) ...
point 3 (-5e3,-5e3,5e3)
; --- thermal and fluid models ---
zone thermal cmodel advection-conduction
zone fluid cmodel assign isotropic
; --- properties ---
; (mechanical)
zone initialize density 2000
; (thermal)
zone thermal property conductivity=[_condu] specific-heat=[_mspec]
zone thermal property conductivity-fluid=[_fcond] specific-heat-fluid=[_fspec]
zone thermal property expansion-fluid=[_fthex] expansion=[_thexp]
zone thermal property temperature-reference=[_T1]
; (fluid)
zone fluid property porosity=[_poros] permeability=[_mobil]
zone fluid property biot=1 undrained-thermal-coefficient=0
zone fluid biot off
zone gridpoint initialize fluid-modulus=2e5
zone gridpoint initialize fluid-tension=-1e10
zone initialize fluid-density=[_fdens]
; --- initial conditions ---
; --- boundary conditions ---
zone face apply temperature [_T1] range position-z -5e3
zone face apply temperature [_T0] range position-z 5e3
; --- settings ---
model gravity 0 0 -10.0
model mechanical active off
; --- conduction solution ---
zone initialize fluid-density=0.0
model fluid active off
model thermal active on
model step 500
zone initialize fluid-density=[_fdens]
model thermal active off
model fluid active on
model step 500
[ref_pp]
fish list [err_pp] [err_t]
[_makeTables]
```

⇐ One-Dimensional Solution of Thermal Transport by Forced Convection and Conduction | Steady-State Convection in a Saturated Porous Medium Heated from Below ⇒

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