Head and flux variability in heterogeneous unsaturated soils under transient flow conditions

Marco Ferrante, Tian-Chyi J Yeh

Research output: Contribution to journalArticle

26 Citations (Scopus)

Abstract

A numerical model for the analysis of uncertainty propagation in flow through unsaturated soils is developed. This model is based on a first-order Taylor series expansion of the discretized Richards equation. Soil hydrologic properties (the saturated hydraulic conductivity and the pore size distribution parameter) are assumed to be stochastic processes in space. The surface boundary conditions can be considered as deterministic variables in time or stochastic time series. Spectral analysis and Monte Carlo simulations were used to verify this numerical model for flow under both steady and transient conditions. The model is then used to examine the effect of uncertainty in boundary conditions and the effect of heterogeneity on the pressure head and flux variance profiles at various times for one-dimensional vertical flow cases. Dependence of pressure head variance on the flow conditions (drying or wetting) is examined. On the basis of the analysis it is found that the propagation of the head variance is similar to that of the concentration variance for solute transport in saturated aquifers. The head variance is proportional to the mean pressure gradient, and thus large head variances are associated with the wetting and the drying front of a moisture pulse. The peak head variance is smaller at the wetting front than it is at the drying front. This difference is attributed to the difference in the magnitude of mean hydraulic gradient and should not necessarily be interpreted as a hysteresis effect. In addition, it is shown how the variance of the flux of a moisture pulse increases with depth.

Original languageEnglish (US)
Pages (from-to)1471-1479
Number of pages9
JournalWater Resources Research
Volume35
Issue number5
DOIs
StatePublished - 1999

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transient flow
Wetting
Drying
Fluxes
Soils
Numerical models
Moisture
wetting
Boundary conditions
Solute transport
soil
boundary condition
Taylor series
Hydraulic conductivity
moisture
Pressure gradient
Random processes
Aquifers
wetting front
Spectrum analysis

ASJC Scopus subject areas

  • Environmental Science(all)
  • Environmental Chemistry
  • Aquatic Science
  • Water Science and Technology

Cite this

Head and flux variability in heterogeneous unsaturated soils under transient flow conditions. / Ferrante, Marco; Yeh, Tian-Chyi J.

In: Water Resources Research, Vol. 35, No. 5, 1999, p. 1471-1479.

Research output: Contribution to journalArticle

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