Articles | Volume 24, issue 1
Hydrol. Earth Syst. Sci., 24, 159–167, 2020
Hydrol. Earth Syst. Sci., 24, 159–167, 2020

Research article 14 Jan 2020

Research article | 14 Jan 2020

Reflection tomography of time-lapse GPR data for studying dynamic unsaturated flow phenomena

Adam R. Mangel et al.

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Cited articles

Baysal, E., Kosloff, D., and Sherwood, J.: Reverse Time Migration, Geophysics, 48, 1514–1524,, 1983. 
Bradford, J. H.: Applying reflection tomography in the postmigrated domain to multifold ground-penetrating radar data, Geophysics, 71, K1–K8,, 2006. 
Bradford, J. H.: Measuring water content heterogeneity using multifold GPR with reflection tomography, Vadose Zo. J., 7, 184–193,, 2008. 
Bradford, J. H., Clement, W. P., and Barrash, W.: Estimating porosity with ground-penetrating radar reflection tomography: A controlled 3-D experiment at the Boise Hydrogeophysical Research Site, Water Resour. Res., 45, 1–11,, 2009. 
Brosten, T. R., Bradford, J. H., McNamara, J. P., Gooseff, M. N., Zarnetske, J. P., Bowden, W. B., and Johnston, M. E.: Multi-offset GPR methods for hyporheic zone investigations, Near Surf. Geophys., 7, 244–257, 2009. 
Short summary
Water flows through soils in an incredibly complex network of pathways. Understanding these pathways is critical to sustainable use of water resources. Ground-penetrating radar (GPR) can image water in near-surface soils the same way an X-ray is used to image the human body. Utilizing innovative ways of collecting and processing the GPR data, we can image complex water flow in space and through time, which allows for the continued development of our ideas and models of subsurface water flow.