共 4 条
ERT data assimilation to characterize aquifer hydraulic conductivity heterogeneity through a heat-tracing experiment
被引:2
|作者:
Shariatinik, Benyamin
[1
,3
]
Gloaguen, Erwan
[1
]
Raymond, Jasmin
[1
]
Boutin, Louis-Charles
[1
]
Fabien-Ouellet, Gabriel
[2
]
机构:
[1] Inst Natl Rech Sci INRS, Ctr Eau Terre Environm, Quebec City, PQ, Canada
[2] Polytech Montreal, Dept Civil Geol & Min Engn, Montreal, PQ, Canada
[3] Inst Natl Rech Sci INRS, Ctr Eau Terre Environm, Quebec City, PQ G1K 9A9, Canada
基金:
加拿大自然科学与工程研究理事会;
关键词:
electrical resistivity tomography;
ensemble Kalman filter;
heat-tracing experiment;
heterogeneity;
hydraulic conductivity;
D O I:
10.1002/nsg.12288
中图分类号:
P3 [地球物理学];
P59 [地球化学];
学科分类号:
0708 ;
070902 ;
摘要:
Geothermal energy systems, such as heat pumps relying on aquifers, use renewable sources of energy that are accessible in urban areas. It is necessary to characterize the subsurface hydraulic properties prior to the installation of such systems. In this context, a heat-tracing experiment is a typical field test that can help with the characterization of the subsurface. During a heat-tracing experiment, monitoring with downhole temperature sensors, water-level pressure transducers and electrical resistivity tomography (ERT) can be used to help characterize the hydrogeological properties. Previous monitoring tools have shortcomings, such as low-resolution data and over-smoothing; thus, they fail to reproduce the heterogeneity of hydrogeological properties. Ensemble Kalman filter (EnKF) is a promising tool that can overcome the over-smoothing problem to replicate the hydrogeological property heterogeneity. In this work, we proposed a new procedure to assimilate time-lapse cross-borehole ERT data into a numerical model of groundwater flow and heat transfer, where the groundwater is extracted and heated water is reinjected into an unconfined sandy-gravel aquifer. The finite element model (FEFLOW 7.3) of groundwater flow and heat transfer is integrated with petrophysical relationship and electrical forward modelling (ResIPy) to estimate cross-borehole ERT measurements. Then, the estimated apparent resistivity is assimilated to update the hydraulic conductivity model using EnKF. The results of the application of the proposed approach to an experimental site located in Quebec City (Canada) demonstrate that the heterogeneity of K is correctly reproduced as the updated K model is reasonably consistent with the lithological log. In addition, the proposed approach was able to replicate the cross-borehole ERT field and temperature measurements. The comparison between prior and posterior distribution of K with slug test results shows that the EnKF made the final (assimilated) distribution of K move towards K values inferred with slug tests.
引用
收藏
页码:358 / 371
页数:14
相关论文