1887
ASEG2009 - 20th Geophysical Conference
  • ISSN: 2202-0586
  • E-ISSN:

Abstract

Introduction

Since 2000 the .Aarhus Workbench (aarhusgeo, 2008) is constantly developed to meet the research needs of the HydroGeophysics Group (HGG) at the University of Aarhus. It allows you to handle, process, invert and visualize electric and electromagnetic (EM) data on a common GIS platform. Geological data can be shown on the GIS map and on cross-sections for comparison with the geophysical results.

The basic idea of the Aarhus Workbench was to develop a single and integrated software platform for handling a number of different data types. The Workbench uses an open-source client server database to manage data and settings. The benefits of using a databases compared to flat ASCII column files should not be underestimated. Firstly, user-handled input/output is nearly eliminated, thus minimizing the chance of human errors. Secondly, data are stored in a well described and documented format which is well suited for both exchange and storage of data.

The Workbench allows the user to present the output of inversions as point themes or as color contoured thematic maps, such as mean resistivity slices, depth to a conductor etc. Models can also be shown on sections which are linked both to the GIS and to displays of data and forward data. The sections can contain numerous layers representing different data types.

Over the years HGG has developed stable processing and inversion algorithms for airborne and ground-based EM data. The inversion is known as Laterally Constrained inversion (LCI) for quasi 2-D modeling and Spatial Constrained inversion (SCI) for quasi 3-D inversion. The Workbench implements a user friendly interface to these algorithms enabling non-geophysicists to carry out inversion of complicated airborne data sets without having in-depth knowledge about how the algorithm actually works. Just as important is an extensive system for evaluation of inversion results with plots of results like resistivity models, flight height, pitch, roll, residuals etc.

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/content/journals/10.1071/ASEG2009ab062
2009-12-01
2026-01-16
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References

  1. Aarhus Workbench, 2008. www.aarhusgeo.com.
  2. Auken, E., Westergaard, J. A., Christiansen, A. V., and Sørensen, K. I., Processing and inversion of SkyTEM data for high resolition hydrogeophysical surveys. 2007. ASEG 2007 - Perth, Western Australia.
  3. Auken, E., Christiansen, A. V., Jacobsen, B. EL, Foged, N., and Sørensen, K. I., 2005, Piecewise ID Laterally Constrained Inversion of resistivity data: Geophysical Prospecting, 53, 497-506.
  4. Christiansen, A.V. and Auken, E., 2008, Presenting a free, highly flexible inversion code, SEG 2008, expanded abstract, 4p
  5. Sørensen, K. I., Auken, E., Christensen, N. B., and Pellerin, L. An Integrated Approach for Elydrogeophysical Investigations. New Technologies and a Case History. Near-surface Geophysics Part II. 585-603. SEG 2005
  6. Sørensen, K. I. and Auken, E., 2004, SkyTEM - Anew high-resolution helicopter transient electromagnetic system: Exploration Geophysics, 35, 191-199.
  7. Viezzoli, A., Christiansen, A. V., Auken, E. and Sorensen, K. I., 2008, Quasi-3D modeling of airborne TEM data by Spatially Constrained Inversion: Geophysics, 73, F105-F113.
/content/journals/10.1071/ASEG2009ab062
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  • Article Type: Research Article
Keyword(s): AEM; GIS; inversion; processing; QC; SkyTEM
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