Sequential and joint hydrogeophysical inversion using a field-scale groundwater model with ERT and TDEM data
- 1Technical University of Denmark, Dept. of Environmental Engineering, Miljøvej, Building 113, 2800, Kgs. Lyngby, Denmark
- 2Flinders University, National Centre for Groundwater Research and Training, G.P.O. Box 2100, Adelaide, SA 5001, Australia
- 3Aarhus University, Dept. of Earth Sciences, Høegh-Guldbergs Gade 2, 8000, Aarhus C, Denmark
- 4University of Palermo, Dept. of Mathematics and Computer Science, Palermo, Italy
Abstract. Increasingly, ground-based and airborne geophysical data sets are used to inform groundwater models. Recent research focuses on establishing coupling relationships between geophysical and groundwater parameters. To fully exploit such information, this paper presents and compares different hydrogeophysical inversion approaches to inform a field-scale groundwater model with time domain electromagnetic (TDEM) and electrical resistivity tomography (ERT) data. In a sequential hydrogeophysical inversion (SHI) a groundwater model is calibrated with geophysical data by coupling groundwater model parameters with the inverted geophysical models. We subsequently compare the SHI with a joint hydrogeophysical inversion (JHI). In the JHI, a geophysical model is simultaneously inverted with a groundwater model by coupling the groundwater and geophysical parameters to explicitly account for an established petrophysical relationship and its accuracy. Simulations for a synthetic groundwater model and TDEM data showed improved estimates for groundwater model parameters that were coupled to relatively well-resolved geophysical parameters when employing a high-quality petrophysical relationship. Compared to a SHI these improvements were insignificant and geophysical parameter estimates became slightly worse. When employing a low-quality petrophysical relationship, groundwater model parameters improved less for both the SHI and JHI, where the SHI performed relatively better. When comparing a SHI and JHI for a real-world groundwater model and ERT data, differences in parameter estimates were small. For both cases investigated in this paper, the SHI seems favorable, taking into account parameter error, data fit and the complexity of implementing a JHI in combination with its larger computational burden.