Référence : S1999-24
Karst modelling
Auteur(s) : Arthur N. Palmer, Margaret V. Palmer, and Ira D. Sasowsky - K W I - 1999
Proceedings of the symposium held February 27 through 27, 1999, Charlottesville, Virginia (USA). - only available on CD-Rom
Table of Contents
INTRODUCTION
A. N. Palmer 1
CONCEPTUAL MODELS 10
Conceptual models for karstic aquifers
W. B. White 11
Perspectives in karst hydrogeology and cavern genesis
D. C. Ford 17
A comprehensive strategy for understanding flow in carbonate aquifers
S. R. H. Worthington 30
Structural effects on carbonate aquifers
I. D. Sasowsky 38
The surface-subsurface interface and the influence of geologic structure in karst
E. H. Kastning 43
A conceptual view of carbonate island karst
J. E. Mylroie and H. L. Vacher 48
Toward a suitable conceptual model of the northern Guam lens aquifer
J. W. Jenson 58
A model of karst drainage basin evolution, Interior Low Plateaus, USA
J. A. Ray 58
Origin and attributes of paleocave carbonate reservoirs
R. G. Loucks 59
From a conceptual model of karst hydrological systems to water-vulnerability mapping
P. -Y. Jeannin, F. Zwahlen, and N. Doerfliger 65
ANALYTICAL MODELS 70
Patterns of dissolution porosity in carbonate rocks
A. N. Palmer 71
Karstic permeability: organized flow pathways created by circulation
P. W. Huntoon 79
Interpreting flow using permeability at multiple scales
T. Halihan, J. M. Sharp, Jr., and R. E. Mace 82
Linear systems approach to modeling groundwater flow and solute transport through karstic basins
C. M. Wicks and J. A. Hoke 97
Toward understanding transport in the Floridan karst
D. Loper 102
DIGITAL MODELS 105
Dynamics of the early evolution of karst
W. Dreybrodt, F. GabrovÓek, and J. Siemers 106
Potential influence of aperture variability on the dissolutional enlargement of fissures
H. Rajaram, W. Cheung, and B. Hanna 120
Enhancement of early karstification by subterranean sources of carbon dioxide
F. GabrovÓek and W. Dreybrodt 131
The initiation of hypogene caves in fractured limestone by rising thermal water:
investigation of a parallel series of competing fractures
K. A. Dumont, H. Rajaram, and D. A. Budd 132
On predicting contaminant transport in carbonate terrains: Behavior and prediction
W. K. Annable and E. A. Sudicky 133
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Table of Contents
Karst Modeling
Karst Waters Institute Special Publication 5
Subsidiary conduit systems: A hiatus in aquifer monitoring and modeling
C. C. Smart 146
Solutionally enhanced leakage rates of dams in karst regions
S. Bauer, S. Birk, R. Liedl, M. Sauter 158
Quantitative analysis of tracer breakthrough curves from tracing tests in karst aquifers
M. S. Field 163
Nonequilibrium solute-transport modeling in karst aquifers
M. S. Field 172
Modeling breakthrough curves of tracing experiments in a karst environment
P. -Y. Jeannin, M. Hauns, and O. Atteia 173
Hydrologic insights from a finite-element model of the
Yigo-Tumon sub-basin, northern Guam lens aquifer
J. M. U. Jocson, J. W. Jenson and D. N. Contractor 174
Simulated effect of a karstic vadose zone above the northern Guam lens on well-water levels
D. N. Contractor and J. W. Jenson 175
SCALE MODELS 176
Bench-scale karst models
L. J. Florea and C. M. Wicks 177
STATISTICAL MODELS 182
Entranceless and fractal caves revisited
R. L. Curl 183
Fractal characteristics of conduit systems
W. D. Howcroft and J. W. Hess 186
Volumetric fractal dimension as a quantitative descriptor for saturated cave morphology
T. R. Kincaid 186
A statistical evaluation of the structural influence on solution-conduit patterns
A. N. Palmer 187
ACQUISITION AND APPLICATION OF FIELD DATA 196
Bridging the gap between real and mathematically simulated karst aquifers
C. Groves, J. Meiman, and A. D. Howard 197
The development of basin-scale conceptual models of the active-flow conduit system
J. Meiman and M. T. Ryan 203
Role of cave information in environmental site characterization
M. Jancin 213
Variation of karstic permeability between unconfined and confined aquifers,
Grand Canyon region, Arizona
P. W. Huntoon 222
Anisotropy in carbonate aquifers
A. N. Palmer 223
Modern dye-tracing data as fundamental input for karst modeling
T. Aley 228
On the importance of stock dye concentrations for accurate preparation of calibration standards
M. S. Field 229
Delineation of source-protection zones for carbonate springs in the Bear River Range, northeastern Utah
L. E. Spangler 230
Geochemical and isotopic evidence for multiple residence times in the same aquifer
E. C. Alexander, Jr., S. C. Alexander, S. R. Grow, B. J. Wheeler, R. A. Jameson,
L. Guo, and D. H. Doctor 233
Mass balance as a tool for the modeling of mixing zones at karst springs,
using Manitou Springs And Cave of the Winds, Colorado, as an example
F. Luiszer 235
Geochemistry of the springs of Missouri
C. M. Wicks 235
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Table of Contents
Karst Modeling
Karst Waters Institute Special Publication 5
Temperature as a natural tracer of short residence times for groundwater in karst aquifers
J. B. Martin and R. W. Dean 236
Using temperature variation at springs to characterize flow in carbonate aquifers
G. J. Davies and S. W. Jones 243
Delineation and characterization of the groundwater basins of four cave systems of
southwestern Illinois' sinkhole plain
S. V. Panno and C. P. Weibel 244
Karst inventory of the northern Guam lens aquifer
D. Taborosi 244
The Kentucky karst atlas: a cooperative project by Kentucky Division of Water
and Kentucky Geological Survey
J. A. Ray 245
How did the Fiborn karst form in only 5000 years?
R. L. Curl 245
The Hydrogeology Consortium
D. Loper 246
The Savoy Experimental Watershed -- early lessons for hydrogeologic modeling
from a well-characterized karst research site
J. V. Brahana, P. D. Hays, T. M. Kresse, T. J. Sauer, and G. P. Stanton 247
Methodology to study the effects of animal production in mantled karst aquifers of the southern Ozarks
J. Funkhouser, P. Little, J. V. Brahana, T. Kresse, M. Anderson, S. Formica and T. Huetter 255
Pump tests of wells at the National Training Center near Shepherdstown, West Virginia
W. K. Jones 259
FIELD TRIP TO ENDLESS CAVERNS, NEW MARKET, VIRGINIA
W. K. Jones 262
AUTHOR INDEX 265
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