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Input (pre-processing)

Further options of the HYDRUS code

The HYDRUS-1D code contains options that its interface does not offer (INPUT.FOR: "New Options – Not supported by GUI"). The computational module opens a file Options.in for them but never reads it, so HYDRUS-1D always runs with the defaults. Rusteau offers them on this page and stores them in the project; a HYDRUS-1D project cannot hold them. HYDRUS defaults resets them.

The page Further options.
The page Further options.

Water flow

OptionDescription
Extrapolation of the heads (lExtrap, default on)each time step starts from heads extrapolated linearly from the two previous steps; off: from the heads of the previous step
Non-equilibrium water flow (TauW)the water content approaches the equilibrium water content of the pressure head with the time constant τw Ross and Smettem (2000) (theory)

Centrifuge (lCentrif)

Flow in a centrifuge: the gravity term becomes ω²(R + depth)/g with the rotation speed [rpm] and the distance R of the soil surface from the axis (theory). With a time-variable bottom boundary condition the hBot column gives the speed and the bottom pressure head is 0, as in HYDRUS.

Density-dependent flow (lDensity)

The density and the viscosity of the solution are cubic polynomials of the liquid concentration of solute 1: ρ/ρ0 = a0 + a1 c + a2 c² + a3 c³ (HYDRUS: 1 + 0.75 c) and μ/μ0 likewise (HYDRUS: 1). The conductivity scales with ρ/μ, the gravity term and the storage with ρ (theory).

Vapor flow

OptionDescription
Enhancement factor of the thermal vapor flux (iEnhanc, default on)the thermal vapor flux is multiplied by the enhancement factor of Cass et al. (1984); off: factor 1 (vapor flow)
Non-equilibrium water flow, the centrifuge and density-dependent flow are not available with the dual-permeability model.

Literature cited in this topic

  • Cass, A., G. S. Campbell, and T. L. Jones (1984). Enhancement of thermal water vapor diffusion in soil. Soil Science Society of America Journal 48(1): 25–32. doi:10.2136/sssaj1984.03615995004800010005x
  • Ross, P. J., and K. R. J. Smettem (2000). A simple treatment of physical nonequilibrium water flow in soils. Soil Science Society of America Journal 64(6): 1926–1930. doi:10.2136/sssaj2000.6461926x

All sources: References.