Toward real-time three-dimensional mapping of surficial aquifers using a hybrid modeling approach

被引:1
作者
Friedel, Michael J. [1 ,2 ]
Esfahani, Akbar [3 ]
Iwashita, Fabio [4 ]
机构
[1] GNS Sci, Dept Hydrogeol, Lower Hutt 5040, New Zealand
[2] Univ Colorado, Math & Stat Sci, Denver, CO 80217 USA
[3] Univ Calif Los Angeles, Ctr Hlth Policy Res, Los Angeles, CA 90024 USA
[4] Univ Florence, I-5 Florence, Italy
关键词
Airborne geophysics; Geostatistics; Heterogeneity; Machine-learning; USA; SELF-ORGANIZING MAP; IMPUTATION; WATER; PRECIPITATION; INVERSION; NETWORKS; SOM;
D O I
10.1007/s10040-015-1318-2
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
A hybrid modeling approach is proposed for near realtime three-dimensional (3D) mapping of surficial aquifers. First, airborne frequency-domain electromagnetic (FDEM) measurements are numerically inverted to obtain subsurface resistivities. Second, a machine-learning (ML) algorithm is trained using the FDEM measurements and inverted resistivity profiles, and bore-hole geophysical and hydrogeologic data. Third, the trained ML algorithm is used together with independent FDEM measurements to map the spatial distribution of the aquifer system. Efficacy of the hybrid approach is demonstrated for mapping a heterogeneous surficial aquifer and confining unit in northwestern Nebraska, USA. For this case, independent performance testing reveals that aquifer mapping is unbiased with a strong correlation (0.94) among numerically inverted and ML-estimated binary (clay-silt or sand-gravel) layer resistivities (5-20 ohm-m or 21-5,000 ohm-m), and an intermediate correlation (0.74) for heterogeneous (clay, silt, sand, gravel) layer resistivities (5-5,000 ohm-m). Reduced correlation for the heterogeneous model is attributed to over-estimating the under-sampled high-resistivity gravels (about 0.5 % of the training data), and when removed the correlation increases (0.87). Independent analysis of the numerically inverted andML-estimated resistivities finds that the hybrid procedure preserves both univariate and spatial statistics for each layer. Following training, the algorithms can map 3D surficial aquifers as fast as leveled FDEM measurements are presented to the ML network.
引用
收藏
页码:211 / 229
页数:19
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