Bayesian approach for three-dimensional aquifer characterization at the Hanford 300 Area

被引:31
|
作者
Murakami, H. [2 ]
Chen, X. [1 ]
Hahn, M. S. [1 ]
Liu, Y. [1 ]
Rockhold, M. L. [3 ]
Vermeul, V. R. [3 ]
Zachara, J. M. [3 ]
Rubin, Y. [1 ]
机构
[1] Univ Calif Berkeley, Dept Civil & Environm Engn, Berkeley, CA 94720 USA
[2] Univ Calif Berkeley, Dept Nucl Engn, Berkeley, CA 94720 USA
[3] Pacific NW Natl Lab, Richland, WA 99352 USA
关键词
PUMPING TEST DATA; HYDRAULIC TOMOGRAPHY; HETEROGENEOUS AQUIFERS; CONDUCTIVITY; INFERENCE; INVERSE; MOMENTS; TESTS; SITE;
D O I
10.5194/hess-14-1989-2010
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
This study presents a stochastic, three-dimensional characterization of a heterogeneous hydraulic conductivity field within the Hanford 300 Area, Washington, USA, by assimilating large-scale, constant-rate injection test data with small-scale, three-dimensional electromagnetic borehole flowmeter (EBF) measurement data. We first inverted the injection test data to estimate the transmissivity field, using zeroth-order temporal moments of pressure buildup curves. We applied a newly developed Bayesian geostatistical inversion framework, the method of anchored distributions (MAD), to obtain a joint posterior distribution of geostatistical parameters and local log-transmissivities at multiple locations. The unique aspects of MAD that make it suitable for this purpose are its ability to integrate multi-scale, multi-type data within a Bayesian framework and to compute a nonparametric posterior distribution. After we combined the distribution of transmissivities with depth-discrete relative-conductivity profile from the EBF data, we inferred the three-dimensional geostatistical parameters of the log-conductivity field, using the Bayesian model-based geostatistics. Such consistent use of the Bayesian approach throughout the procedure enabled us to systematically incorporate data uncertainty into the final posterior distribution. The method was tested in a synthetic study and validated using the actual data that was not part of the estimation. Results showed broader and skewed posterior distributions of geostatistical parameters except for the mean, which suggests the importance of inferring the entire distribution to quantify the parameter uncertainty.
引用
收藏
页码:1989 / 2001
页数:13
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