Related Experiment Video
Updated: May 9, 2026

08:02
Reservoir Condition Pore-scale Imaging of Multiple Fluid Phases Using X-ray Microtomography
Published on: February 25, 2015
A method for conducting simultaneous convergent tracer tests in multilayered aquifers
Richard B Greswell1, Véronique Durand, Maria F Aller
1Water Sciences (Hydrogeology), School of Geography, Earth and Environmental Sciences, University of Birmingham, Edgbaston, Birmingham B15 2TT, UK.
Ground Water
|July 31, 2013
Summary
This study introduces a new multilevel sampling system for simultaneous forced gradient tracer tests. This method enhances the identification of groundwater flow paths in aquifers, improving contaminant transport studies.
Area of Science:
- Hydrogeology
- Environmental Science
- Geochemistry
Background:
- Forced gradient tracer tests are crucial for understanding contaminant transport and aquifer properties at the field scale.
- Traditional full-depth tests yield complex breakthrough curves, hindering the identification of specific flow paths.
- Level-specific aquifer tests are often costly and do not guarantee pathway identification.
Purpose of the Study:
- To present a novel method for conducting simultaneous, multilevel tracer tests.
- To overcome limitations of traditional tracer testing methods in identifying subsurface flow pathways.
- To enable high-frequency and cumulative sampling for detailed transport analysis.
Main Methods:
- Development and application of a novel multilevel sampling system for simultaneous tracer tests.
- Conducting forced gradient tracer tests between two boreholes.
- Utilizing fluorescein as a tracer in a multilayered sandstone aquifer.
Main Results:
- Successful simultaneous execution of multiple tracer tests across the full borehole depth.
- Generation of six well-defined tracer breakthrough curves.
- Demonstration of the system's capability for high-frequency and cumulative sampling.
Conclusions:
- The novel multilevel sampling system effectively facilitates simultaneous tracer tests.
- This method significantly improves the ability to delineate groundwater flow paths and study contaminant transport.
- The technique offers a more efficient and informative approach to aquifer characterization.

