Theoretical and Computational Development of a Hydrobiogeochemical Model

by
Gour-Tsyh (George) Yeh
Department of Civil and Environmental Engineering
The Pennsylvania State University
University Park, PA 16802
Presented at
Fifth SIAM Conference on Mathematical and
Computational Issues in Geosciences
San Antonio, Texas
March 24-27, 1999

Outline


Introduction

The most important issues among others in modeling reactive chemical transport are:

Consistency of a Reactive Transport System

Once a reactive system is defined (we say a system is defined when the number of species, M, and number of reactions, Nr, are specified), we can check the consistency of the system even before we assess whether the proposed rate laws are adequate. We do the analysis by diagonalizing the reaction matrix.

Example

    H + NTA <-->  HNTA                    with rate R1 = infinity         (R1)
    Co + NTA <--> CoNTA                with rate R2 = infinity          (R2)
    CoNTA + H <--> Co + HNTA       with rate R3 = finite     (R3)
    HNTA + H <--> M                        with rate R4 = finite     (R4)

Formulation of Rate Laws and Parameter Determination

 Example: Bio-degradation of Bi-reactants

Formulation of Rate Laws and Parameter Determination


Reactive Transport Formulation -Transport Velocities

To simplify the discussion, let us consider advective transport under single phase flow conditions without the loss of generality,

where [A] is the diagonal matrix, [B] is the diagonal matrix with zero diagonal entries corresponding to immobile species. Applying the Gauss-Jordan Elimination, we have
From NC component equations with those rows that the reduced [A] is different from the reduced [B]. Vt = (C/T)Vf
From (NI - Ne) transport-reaction equations with those rows that the reduced [A] is the same as the reduced [B]. Vt is not easy to define.
From (NI - Ne) transport-reaction equations with those rows that the reduced [A] is different from the reduced [B]. Vt is not easy to define.
NOTE: If the system of Eq. (18) is reducible to the system of Type 0, Type I, and Type II, then the transport can be completely decoupled from reactions. Under such circumstances, "true" transport velocities for chemical components are just the fluid velocity and the "true" transport velocities for chemical species are unnecessary to know. We would like to know what kind of properties the reaction matrix [] must have in order to render the system of Eq. (18) reducible. If Type V equations are not created, then the diagonalized approach is always superior to the conventional approach.
NOTE: The conventional approach contains Type I (for surface species) and Type IV (for aqueous species) equations only.
Now let us consider the reactive system given previously, but subject to transport.

First Decomposition

Second Decomposition

Numerical Methods for Reactive Transport

A 2-D Linear Transport Benchmark Problem by Peter C. Lichtner

This benchmark problem compares 1st order upwinding with the TVD scheme for nonreactive flow at 45o angle to the grid. Parameters used in the calculation are: a fluid flow velocity of 15.768 m y-1 along the positive x- and y-axes, diffusion coefficient equal to 10-5 cm2 s-1, and 100% porosity. The grid consists of 50 nodes in the x- and y-directions with an equal spacing of 0.2 m. This gives a grid Peclet number of 100. The initial condition consists of a concentration mound of unit concentration with a width of 2 m occupying the square region 1-3 m by 1-3 m corresponding to nodes 5-15 in each direction. The concentration is zero everywhere else. Zero gradient boundary conditions are imposed around the periphery of the domain. A Courant number of 0.1 is used in the TVD calculation. The calculation is carried out for 5 x 106 s.
The result for upwinding are shown in Figure 1 along with the initial condition. In Figure 2 is shown the result of the TVD calculation. Both calculations conserve mass essentially exactly. Clearly the TVD scheme does a much better job compared to the upwinding scheme whcih reapidly disperses the concentration mound with time. The TVD scheme is able to very accurately track the mound without spreading it out as in the upwinding scheme, although some distortion can be seen perpendicular to the direction of flow.

Peter C. Lichtner's Problem Solved with LEZOOMPC

Cases 1A and 1E

Peter C. Lichtner's Problem Solved with LEZOOMPC

Cases 1D and 1H
 

A 2-D Nonlinear Reactive Transport Problem by A. Chilakapati


Conclusion