So, what we have seen in today's lecture are a coupled volumetric liquid model based on a mechanistic approach has been presented in terms of ground water flow, which are temperature dependence, and you have a transient phenomenon and the liquid transport and the vapour transfer they all can be coupled together to give a realistic simulation and we also stressed the importance of thermo-physical properties, because the hydraulic conductivity is quite a non-linear function of ql, which is, and also the capillary potential, which also are a non-linear potential of ql.
Therefore we need to measure those parameters experimentally, and we have also seen that the literature the variation has been quite non-linear for variety of soil conditions. And we also said that the mathematical formulation that we proposed has been validated with the results from heating experiment.