FastFind »   Lastname: doi:10.1029/ Year: Advanced Search  

AGU: Water Resources Research

 

Keywords

  • transition probability
  • Markov chain
  • sediment layering structure
  • soil textural class
  • injection experiment

Index Terms

  • Hydrology: Modeling
  • Hydrology: Soil moisture
  • Hydrology: Stochastic hydrology
  • Hydrology: Uncertainty assessment
Abstract
Cited By (0)
 

Abstract

A Markov chain model for characterizing medium heterogeneity and sediment layering structure

Ming Ye

Department of Scientific Computing, Florida State University, Tallahassee, Florida, USA

Raziuddin Khaleel

Fluor Government Group, Richland, Washington, USA

By leveraging use of “soft” data (e.g., initial moisture content, θ i ), this study applies the transition probability (TP) based Markov chain (MC) model to sediment textural classes for characterizing the medium heterogeneity and sediment layering structure. The TP/MC method is evaluated by simulating the vadose zone moisture movement at a field site, where the stratigraphy consists of imperfectly stratified soil layers. Soil heterogeneity is characterized via spatial variability of the geometry of soil textural classes. When the θ i measurements, which carry signature about medium heterogeneity and stratigraphy, are not included in the TP/MC model, it is not possible to identify the horizontal TP. The θ i measurements, when transformed into soil classes, are necessary in mapping the soil layering structure prevalent at the site. The soil hydraulic parameters for each soil class are treated deterministically and are estimated on the basis of core samples. To evaluate uncertainty in characterizing geometry of the soil classes, multiple conditional realizations of the soil classes are generated. A Monte Carlo simulation shows that the simulated mean moisture contents agree well with corresponding field observations. The observed splitting of the moisture plume in a coarse sand layer that is sandwiched between two fine-textured layers, the southeastward movement of the plume during the redistribution period, and the near-zero fluid flux below the bottom fine layer are adequately simulated. Spatial variability of the field-measured moisture content is sufficiently captured by the 95% confidence intervals calculated from the Monte Carlo simulations. Investigating the effect of data conditioning on the simulated results shows that a reduction of conditioning data does not necessarily deteriorate simulation results if other conditioning data exist within the mean length of the soil classes. The TP/MC method is flexible so that other types of site characterization data (e.g., geophysical data) can be incorporated as they become available.

Received 15 February 2008; accepted 24 June 2008; published 20 September 2008.

Citation: Ye, M., and R. Khaleel (2008), A Markov chain model for characterizing medium heterogeneity and sediment layering structure, Water Resour. Res., 44, W09427, doi:10.1029/2008WR006924.

Cited By

Please wait one moment ...