Abstract
Abstract. Ground-penetrating radar (GPR) reflection tomography algorithms allow
non-invasive monitoring of water content changes resulting from flow in the
vadose zone. The approach requires multi-offset GPR data that are
traditionally slow to collect. We automate GPR data collection to reduce the
survey time significantly, thereby making this approach to hydrologic
monitoring feasible. The method was evaluated using numerical simulations
and laboratory experiments that suggest reflection tomography can provide
water content estimates to within 5 % vol vol−1–10 % vol vol−1 for the
synthetic studies, whereas the empirical estimates were typically within
5 %–15 % of measurements from in situ probes. Both studies show larger
observed errors in water content near the periphery of the wetting front,
beyond which additional reflectors were not present to provide data
coverage. Overall, coupling automated GPR data collection with reflection
tomography provides a new method for informing models of subsurface
hydrologic processes and a new method for determining transient 2-D soil
moisture distributions.
Funder
Division of Earth Sciences
Subject
General Earth and Planetary Sciences,General Engineering,General Environmental Science
Cited by
19 articles.
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