Geostatistics and Bayesian Updating for Transmissivity Estimation in a Multiaquifer System in Manitoba, Canada

• Published in: Ground water Vol. 40; no. 3; pp. 273 - 283
• Main Authors: Kennedy, Paula L., Woodbury, Allan D.
• Format: Journal Article
• Language: English
• Published: Oxford, UK Blackwell Publishing Ltd 01-05-2002; National Ground Water Association; Ground Water Publishing Company
• Subjects: Aquifers; Bayes Theorem; Bayesian analysis; Bayesian statistical decision theory; Canada; Canada, Manitoba; Geology; Geology - statistics & numerical data; Groundwater; Groundwater flow; Hydrology; Soil; Statistical methods; Water Movements; Water Supply; Manitoba; Manitoba Canada; PNW, Canada, Manitoba
• ISSN: 0017-467X; 1745-6584
• DOI: 10.1111/j.1745-6584.2002.tb02655.x

In ground water flow and transport modeling, the heterogeneous nature of porous media has a considerable effect on the resulting flow and solute transport. Some method of generating the heterogeneous field from a limited dataset of uncertain measurements is required. Bayesian updating is one method that interpolates from an uncertain dataset using the statistics of the underlying probability distribution function. In this paper, Bayesian updating was used to determine the heterogeneous natural log transmissivity field for a carbonate and a sandstone aquifer in southern Manitoba. It was determined that the transmissivity in m2/sec followed a natural log normal distribution for both aquifers with a mean of ‐7.2 and ‐ 8.0 for the carbonate and sandstone aquifers, respectively. The variograms were calculated using an estimator developed by Li and Lake (1994). Fractal nature was not evident in the variogram from either aquifer. The Bayesian updating heterogeneous field provided good results even in cases where little data was available. A large transmissivity zone in the sandstone aquifer was created by the Bayesian procedure, which is not a reflection of any deterministic consideration, but is a natural outcome of updating a prior probability distribution function with observations. The statistical model returns a result that is very reasonable; that is homogeneous in regions where little or no information is available to alter an initial state. No long range correlation trends or fractal behavior of the log‐transmissivity field was observed in either aquifer over a distance of about 300 km.