TY - JOUR
T1 - A Reduced-Order Successive Linear Estimator for Geostatistical Inversion and its Application in Hydraulic Tomography
AU - Zha, Yuanyuan
AU - Yeh, Tian Chyi J.
AU - Illman, Walter A.
AU - Zeng, Wenzhi
AU - Zhang, Yonggen
AU - Sun, Fangqiang
AU - Shi, Liangsheng
N1 - Funding Information:
The present study was supported by the National Natural Science Foundation of China (grants 51779179, 51609173, 51479144, and 51522904). The second author acknowledges funding by CRDF under the award (DAA2–15-61224-1): hydraulic tomography in shallow alluvial sediments: Nile River Valley, Egypt, and the Global Expert award through Tianjin Normal University from the Thousand Talents Plan of Tianjin City. F. Sun would like to acknowledge the Special Fund for Public Industry Research from Ministry of Land and Resources of China (No. 201511047). The authors are grateful for the thoughtful review and suggestions by Alberto Bellin (Associate Editor), Kris Kuhlman, and two anonymous reviewers. The program and the data used in this study can be downloaded from https://doi.org/10.13140/RG.2.2. 11775.71845.
Publisher Copyright:
© 2018. American Geophysical Union. All Rights Reserved.
PY - 2018/3
Y1 - 2018/3
N2 - Hydraulic tomography (HT) is a recently developed technology for characterizing high-resolution, site-specific heterogeneity using hydraulic data (nd) from a series of cross-hole pumping tests. To properly account for the subsurface heterogeneity and to flexibly incorporate additional information, geostatistical inverse models, which permit a large number of spatially correlated unknowns (ny), are frequently used to interpret the collected data. However, the memory storage requirements for the covariance of the unknowns (ny × ny) in these models are prodigious for large-scale 3-D problems. Moreover, the sensitivity evaluation is often computationally intensive using traditional difference method (ny forward runs). Although employment of the adjoint method can reduce the cost to nd forward runs, the adjoint model requires intrusive coding effort. In order to resolve these issues, this paper presents a Reduced-Order Successive Linear Estimator (ROSLE) for analyzing HT data. This new estimator approximates the covariance of the unknowns using Karhunen-Loeve Expansion (KLE) truncated to nkl order, and it calculates the directional sensitivities (in the directions of nkl eigenvectors) to form the covariance and cross-covariance used in the Successive Linear Estimator (SLE). In addition, the covariance of unknowns is updated every iteration by updating the eigenvalues and eigenfunctions. The computational advantages of the proposed algorithm are demonstrated through numerical experiments and a 3-D transient HT analysis of data from a highly heterogeneous field site.
AB - Hydraulic tomography (HT) is a recently developed technology for characterizing high-resolution, site-specific heterogeneity using hydraulic data (nd) from a series of cross-hole pumping tests. To properly account for the subsurface heterogeneity and to flexibly incorporate additional information, geostatistical inverse models, which permit a large number of spatially correlated unknowns (ny), are frequently used to interpret the collected data. However, the memory storage requirements for the covariance of the unknowns (ny × ny) in these models are prodigious for large-scale 3-D problems. Moreover, the sensitivity evaluation is often computationally intensive using traditional difference method (ny forward runs). Although employment of the adjoint method can reduce the cost to nd forward runs, the adjoint model requires intrusive coding effort. In order to resolve these issues, this paper presents a Reduced-Order Successive Linear Estimator (ROSLE) for analyzing HT data. This new estimator approximates the covariance of the unknowns using Karhunen-Loeve Expansion (KLE) truncated to nkl order, and it calculates the directional sensitivities (in the directions of nkl eigenvectors) to form the covariance and cross-covariance used in the Successive Linear Estimator (SLE). In addition, the covariance of unknowns is updated every iteration by updating the eigenvalues and eigenfunctions. The computational advantages of the proposed algorithm are demonstrated through numerical experiments and a 3-D transient HT analysis of data from a highly heterogeneous field site.
KW - Bayesian inversion
KW - Karhunen-Loeve Expansion
KW - geostatistical inverse modeling
KW - hydraulic tomography
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U2 - 10.1002/2017WR021884
DO - 10.1002/2017WR021884
M3 - Article
AN - SCOPUS:85043452735
SN - 0043-1397
VL - 54
SP - 1616
EP - 1632
JO - Water Resources Research
JF - Water Resources Research
IS - 3
ER -