Conference paper
Automatic generation of groundwater model hydrostratigraphy from AEM resistivity and boreholes
Regional hydrological models are important tools in water resources management. Model prediction uncertainty is primarily due to structural (geological) non-uniqueness which makes sampling of the structural model space necessary to estimate prediction uncertainties. Geological structures and heterogeneity, which spatially scarce borehole lithology data may overlook, are well resolved in AEM surveys.
This study presents a semi-automatic sequential hydrogeophysical inversion method for the integration of AEM and borehole data into regional groundwater models in sedimentary areas, where sand/ clay distribution govern groundwater flow. The coupling between hydrological and geophysical parameters is managed using a translator function with spatially variable parameters followed by a 3D zonation.
The translator function translates geophysical resistivities into clay fractions and is calibrated with observed lithological data. Principal components are computed for the translated clay fractions and geophysical resistivities. Zonation is carried out by k-means clustering on the principal components.
The hydraulic parameters of the zones are determined in a hydrological model calibration using head and discharge observations. The method was applied to field data collected at a Danish field site. Our results show that a competitive hydrological model can be constructed from the AEM dataset using the automatic procedure outlined above.
Language: | English |
---|---|
Publisher: | European Association of Geoscientists and Engineers |
Year: | 2014 |
Proceedings: | 20th European Meeting of Environmental and Engineering Geophysics |
ISBN: | 9462820279 and 9789462820272 |
Types: | Conference paper |
ORCIDs: | Marker, Pernille Aabye , Bauer-Gottwein, Peter , 0000-0001-5829-2913 and 0000-0002-5397-4832 |