Research Article

Simulating the Evolution of Fluid Underpressures in the Great Plains, by Incorporation of Tectonic Uplift and Tilting, with a Groundwater Flow Model

Table 1

Correlation of sections of the paper with FE elements of the flow chart of the modeling process in Figure 13 that they refer to.

Section titleFlow chart of the modeling process Figure 13, Element #

Abstract
1. Introduction
2. The Geologic Setting
3. Methodology
 3.1. Understanding the Geology and Quantifying Structural Changes
 3.2. Assembling the present-day geofluid underpressure data
 3.3. Creating and Calibrating the Hydrologic Model to SimulateFE#’s ; (4b), (9), (2b), (4a), (5b); (2a),
   Structurally Driven Underpressures(4a), (5a), (7b), (7a)
  3.3.1. Uplift, Deposition, And ErosionFE#
  3.3.2. Hydraulic Conductivity and Specific StorageFE# (6), Appendix C, (2a), (8), (5a), (4b), (7a)
   Darcy’s equation (2)FE#’s: (4a), (5a), (4b), (7a)
  3.3.3. Boundary Conditions (BCs) for the Sequence ofFE#’s: (2b), (4a), (8), (5b), (4b), (7a), (7b); FE’s: ,
      Models arrows of FE# (3)
   3.3.4. Initial Heads for the Sequence of ModelsFE#’s (3a), (3b), (3i); ’s under FE#’s
  3.3.5. Transience While Running the Sequence of 9 MODFLOWFE# (3), FE# (3a)
     Models
  3.3.6. Sensitivity Analysis
  3.3.7. Model Limitations
4. Results and Discussion
5. Summary and Conclusions
A. Theoretical Basis of Underpressure
B. Expanded Geologic Setting
C. Permeability and Hydraulic Conductivity Values from Other Sources
Definitions of Terms
Acknowledgements
References