template<class Scalar>
class Dumux::ThermalConductivitySomertonThreeP< Scalar >
Somerton (three fluid phases)
The Somerton method [77] computes the thermal conductivity of dry and the wet soil material. It is extended here to a three phase system of water (w), NAPL (n) and gas (g). It uses a root function of the water and NAPL saturation to compute the effective thermal conductivity for a three-phase fluidsystem. The individual thermal conductivities are calculated as geometric mean of the thermal conductivity of the porous material and of the respective fluid phase.
The effective thermal conductivity of ThermalConductivitySomertonThreeP
is given by
\[ \lambda_\text{eff} = \lambda_\text{g,eff} + \sqrt{S_\text{w}} \left(\lambda_\text{w,eff} - \lambda_\text{g,eff}\right) + \sqrt{S_\text{n}} \left(\lambda_\text{n,eff} - \lambda_\text{g,eff}\right) \]
with \( S_\text{w} \) the water saturation, \( S_\text{n} \) the NAPL saturation, the effective phase saturations given by \( \lambda_{\alpha,\text{eff}} = (\lambda_\text{s})^{\left(1-\phi\right)} (\lambda_\alpha)^\phi, \alpha \in \{\text{w,n,g}\}\) (geometric mean) and \( \lambda_\text{s} \) is the thermal conductivity of the solid phase.