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The Groundwater Project Foreword
Foreword
Preface
Acknowledgments
2.1 Formation of Karstic Conduit Flow Systems
2.2 Deep Chemically Aggressive Water Forms Interconnected Conduits
2.3 Water Table Decline and Fluctuation Forms Interconnected Conduits
2.4 Summary of Formation of Conduit Flow
3.1 Karst Drainage System
3.2 Karst Occurrence where Soluble and Less Soluble Units Occur Together
3.3 Multiple Porosity and Permeability Structure
3.4 Variance in Surface-Water and Spring Discharge in Karst Aquifers
3.5 Conduit Drainage Patterns
3.6 Subsurface Piracy and Karst Drainage Basins
3.7 Vulnerability of Karst Aquifers to Contamination
3.8 Karst Aquifer Flow Characteristics Compared with Aquifers Composed of Other Rock Types
4.1 Limitations of Darcy’s Law for Application to Karst Aquifers
4.2 Reynolds Number as an Indicator of Flow Regime
4.3 Investigation of Onset of Turbulent Flow in Rock Samples
4.4 Fluid Mechanics of Pipes and Open Channels
5.1 Hydrogeologic Mapping
5.2 Borehole Testing
5.3 Water Tracing Tests
5.4 Aquifer Tests
5.5 Use of Water Chemistry Data
6.1 Fitting Models
6.2 Lumped Parameter Models
6.3 Distributed Parameter Models
Exercise 1
Exercise 2
Exercise 3
Exercise 4
Exercise 5
Exercise 6
Exercise 7
Exercise 8
Exercise 9
Exercise 10
Exercise 11
Exercise 12
Exercise 13
Exercise 14
Exercise 15
Exercise 16
Exercise 17
Exercise 18
Exercise 19
Exercise 20
Exercise 21
Exercise 22
Box 1 Stages from Fracture Flow to Conduit Flow
Exercise 1 Solution
Exercise 2 Solution
Exercise 3 Solution
Exercise 4 Solution
Exercise 5 Solution
Exercise 6 Solution
Exercise 7 Solution
Exercise 8 Solution
Exercise 9 Solution
Exercise 10 Solution
Exercise 11 Solution
Exercise 12 Solution
Exercise 13 Solution
Exercise 14 Solution
Exercise 15 Solution
Exercise 16 Solution
Exercise 17 Solution
Exercise 18 Solution
Exercise 19 Solution
Exercise 20 Solution
Exercise 21 Solution
Exercise 22 Solution
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Introduction to Karst Aquifers Copyright © 2022 by Eve L. Kuniansky, Charles J. Taylor, and Frederick Paillet. All Rights Reserved.