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L. Gelhar (1986)
Stochastic subsurface hydrology from theory to applicationsWater Resources Research, 22
R. Hoeksema, P. Kitanidis (1984)
An Application of the Geostatistical Approach to the Inverse Problem in Two-Dimensional Groundwater ModelingWater Resources Research, 20
Weimer Weimer, Land Land (1972)
Lyons Formation (Permian), Jefferson County, Colorado: A fluvial depositMt. Geol., 9
Howard Howard (1966)
Patterns of sediment dispersal in the Fountain Formation of ColoradoMt. Geol., 3
Hubert Hubert (1960)
Petrology of the Fountain and Lyons Formations, Front Range, ColoradoQ. Colo. Sch. Mines, 55
M. Hill (1992)
A computer program (MODFLOWP) for estimating parameters of a transient, three-dimensional ground-water flow model using nonlinear regression
Journel Journel (1986)
Constrained interpolation and qualitative informationMath. Geol., 18
E. Isaaks, R. Srivastava (1988)
Spatial continuity measures for probabilistic and deterministic geostatisticsMathematical Geology, 20
H. Olsen, Garsten Ploug, U. Nielsen, K. Sørensen (1993)
Reservoir Characterization Applying High‐Resolution Seismic Profiling, Rabis Creek, DenmarkGround Water, 31
J. Davis, R. Lohmann, F. Phillips, John Wilson, D. Love (1993)
Architecture of the Sierra Ladrones Formation, central New Mexico: Depositional controls on the permeability correlation structureGeological Society of America Bulletin, 105
A. Desbarats, R. Srivastava (1991)
Geostatistical characterization of groundwater flow parameters in a simulated aquiferWater Resources Research, 27
E. Poeter, S. McKenna (1995)
Reducing Uncertainty Associated with Ground‐Water Flow and Transport PredictionsGround Water, 33
D. Hyndman, J. Harris, S. Gorelick (1993)
Coupled seismic and tracer test inversion for aquifer property characterization
B. James, R. Freeze (1993)
The worth of data in predicting aquitard continuity in hydrogeological designWater Resources Research, 29
J. Brannan, J. Haselow (1993)
Compound random field models of multiple scale hydraulic conductivityWater Resources Research, 29
R. Kulkarni (1984)
Bayesian Kriging in Geotechnical Problems
A. Journel (1986)
Constrained interpolation and qualitative information—The soft kriging approachMathematical Geology, 18
Moline Moline, Bahr Bahr, Drzewiecki Drzewiecki, Shepherd Shepherd (1992)
Identification and characterization of pressure seals through the use of wireline logs: A multivariate statistical approachLog Anal., 33
J. Davis, John Wilson, F. Phillips (1994)
A Portable Air‐Minipermeameter for Rapid In Situ Field MeasurementsGround Water, 32
M. Anderson (1989)
Hydrogeologic facies models to delineate large-scale spatial trends in glacial and glaciofluvial sedimentsGeological Society of America Bulletin, 101
Hua Zhu, A. Journel (1993)
Formatting and Integrating Soft Data: Stochastic Imaging via the Markov-Bayes Algorithm
J. Howard (1966)
PAtterns of Sediment Dispersal in the Fountain Formation of ColoradoThe mountain Geologist
C. Deutsch, A. Journel (1993)
GSLIB: Geostatistical Software Library and User's Guide
A. Journel (1991)
Fundamentals of geostatistics in five lessons
G. Moline, P. Drzewiecki, J. Bahr (1991)
Identification and characterization of pressure seals through the use of wireline logs: A multivariate statistical approachAAPG Bulletin, 75
R. Weimer, C. Land (1972)
Lyons Formation (Permian), Jefferson County, Colorado: A Fluvial DepositThe mountain Geologist
Y. Rubin, G. Dagan (1988)
Stochastic analysis of boundaries effects on head spatial variability in heterogeneous aquifers: 1. Constant head boundaryWater Resources Research, 24
McKenna McKenna, Poeter Poeter (1995)
Subsurface characterization through cross‐borehole seismic tomographyGround Water
Application of data fusion to characterization of the Fountain and Lyons Formations at a field site incorporates geologic knowledge, geophysical log data, cross‐hole seismic tomography, hydraulic test data, and observations of head to reduce uncertainty associated with subsurface interpretation. These formations consist of channel and overbank deposits that have undergone variable diagenesis, resulting in more hydrofacies than would have been encountered in the original, unaltered deposits. The disparate types of available data are integrated to yield a coherent hydrofacies classification through use of discriminant analysis and soft data techniques. This data fusion improves definition of the complex hydrofacies and increases knowledge of their spatial correlation. Two hundred multiple‐indicator, conditional, stochastic simulations of the site are generated, 100 with only hard data and 100 with both hard and soft data. Forward groundwater flow modeling using estimates of hydraulic conductivity from field testing yields smaller head residuals for realizations which include soft data. Inverse modeling is used to eliminate hydrofacies realizations that do not honor hydraulic data and to estimate hydrofacies hydraulic conductivity ranges for the hard and hard/soft data ensembles. Inverse parameter estimation substantially decreases head residuals for both ensembles. Standard deviations of hydraulic conductivities estimated through inverse modeling are smaller when both hard and soft data are used to generate the simulations, even though head residuals are similar within the two ensembles when these estimated hydraulic conductivities are used.
Water Resources Research – Wiley
Published: Dec 1, 1995
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