An analytical solution for estimating percolation rate by fitting temperature profiles in the vadose zone.
We present a simple analytical solution for one-dimensional steady heat transfer with convection and conduction through a multilayer system such as a vadose zone. We assume that each layer is homogeneous and has a constant thermal diffusivity. The mass/heat flow direction is perpendicular to the layers, and the mass flow rate is a constant. The analytical solution presented in this study also assumes constant known temperatures at the two boundaries of the system. Although the analytical solution gives the temperature as a function of a few parameters, we focus on the inverse application to estimate the percolation rate in a vadose zone. Example applications have shown that with reliable field observation data, the solution can be used to determine the percolation rate to high degree of accuracy (e.g., to mm/year). In some other cases, the solution may also be helpful in characterizing potential lateral flow along layer divides.
Shan
Chao
C
Earth Sciences Division, Lawrence Berkeley National Laboratory, 90-1116, 1 Cyclotron Road, Berkeley, CA 94720, USA. c_shan@lbl.gov
Bodvarsson
Gudmundur
G
D008962:Models, Theoretical; D012987:Soil; D013696:Temperature; D014872:Water Movements
D012987:Soil