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TitleHydrogeological implications of paleo-fluvial architecture for the Paskapoo Formation, sw Alberta, Canada: a stochastic analysis
AuthorBurns, E R; Bentley, L R; Hayashi, M; Grasby, S E; Hamblin, A P; Smith, D G; Wozniak, P R J
SourceJournal of Hydrology vol. 18, 2010 p. 1375-1390, https://doi.org/10.1007/s10040-010-0608-y
Year2010
Alt SeriesEarth Sciences Sector, Contribution Series 20090388
PublisherElsevier
Documentserial
Lang.English
Mediapaper; on-line; digital
File formatpdf
ProvinceAlberta
NTS82O/01; 82O/02; 82O/07; 82O/08; 82P/04; 82P/05
AreaCalgary
Lat/Long WENS-115.0000 -113.5000 51.5000 51.0000
Subjectshydrogeology; mathematical and computational geology; groundwater; groundwater flow; groundwater movement; groundwater regimes; statistical analyses; statistics; modelling; models; Paskapoo Formation
Illustrationstables; location maps; plots
ProgramAquifer Assessment & support to mapping, Groundwater Geoscience
AbstractFluvial systems tend to deposit sediment in well-defined relational geometries and in vertically and laterally repeating patterns. These sedimentary deposits are preserved to varying degrees depending on how much the fluvial system reworks the deposits. The Paskapoo bedrock aquifer system in southern Alberta, Canada, was deposited in a foreland depositional basin during uplift of the Rocky Mountains, and both the geomorphic model and field evidence indicate that the upper 100m of the local aquifer system contains well-preserved, highly connected paleo-channels and associated overbank deposits. In order to evaluate the value of different types of data, a simplified stochastic-numerical groundwater flow model was developed to examine the sensitivity of results to model parameters. Parameters examined include: fraction of the formation made up of channel sands; meander and sinuosity factors; width-to-depth ratios of preserved channels; and crevasse splay conductivity. In all cases examined, the system exhibited anisotropic behavior with the along-channel flow direction being the most permeable and the vertical direction being least permeable. In general, the strongest control on the resulting effective anisotropic hydraulic conductivities was channel fraction, but geometric factors that control between-channel connectivity (e.g., channel sinuosity) had an appreciable effect on the across-channel flow direction effective permeability.
GEOSCAN ID261622