Related Experiment Videos
Deriving TDS values in coarse sediments from long normal and electromagnetic logs.
1Ghent University, Department of Geology and Soil Science Krijgslaan, 281 (S8)B-9000 Ghent, Belgium. Nathalie.VanMeir@erdw.ethz.ch
Ground Water
|January 21, 2003
Summary
This study establishes a link between electromagnetic (EM) borehole logs and total dissolved solids (TDS) in groundwater. This method enables effective salinity monitoring in coastal aquifers, offering advantages over traditional logging techniques.
Area of Science:
- Geophysics
- Hydrogeology
- Environmental Science
Background:
- Accurate groundwater salinity assessment is crucial for coastal resource management.
- Traditional logging methods like long normal (LN) logs have limitations in monitoring and data acquisition.
- Electromagnetic (EM) logging offers potential advantages for continuous and detailed subsurface characterization.
Purpose of the Study:
- To develop an empirical relationship between EM borehole recordings and total dissolved solids (TDS) in pore water.
- To adapt existing resistivity-based TDS estimation methods for EM log data.
- To establish a framework for enhanced groundwater salinity monitoring in the Belgian coastal plain.
Main Methods:
- Linking long normal (LN) logs to electromagnetic (EM) logs.
- Rewriting established relationships between LN resistivity and TDS for EM recordings.
- Utilizing Archie's Law to derive the formation factor from groundwater analyses and LN logs.
Main Results:
- An empirical relationship was established, enabling TDS estimation from EM borehole recordings.
- EM logging demonstrated advantages including measurement in PVC-cased wells and high vertical resolution.
- EM logging is not hindered by the invasion zone and allows for time-dependent data collection.
Conclusions:
- The developed technique provides a robust method for estimating groundwater TDS using EM logs.
- This approach facilitates the establishment of effective salinity monitoring networks in coastal areas.
- The method allows for historical salinity comparison and monitoring of freshwater-saltwater evolution over time.