The potential of ground-based 3D GPR imaging: 2D vs. 3D examples from the Yedoma region

• Main Authors: Schennen, Stephan, Tronicke, Jens, Wetterich, Sebastian, Allroggen, Niklas, Schwamborn, Georg, Schirrmeister, Lutz
• Format: Conference Object
• Language: unknown
• Published: Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research International Permafrost Association 2016
• Subjects: Ice; permafrost; Siberia
• Online Access: https://epic.awi.de/id/eprint/42030/; https://hdl.handle.net/10013/epic.48827

Ground-penetrating radar (GPR) reflection imaging is a popular geophysical tool to explore subsurface structures in a non-invasive manner. In terms of GPR, reflective interfaces are defined by contrasts in dielectric permittivity, which result from, for example, variations in soil moisture or ice content. GPR is very suitable for electrically high resistive environments, such as frozen ground (typically > 10,000 m). Here, GPR can be used to explore structural targets at depths up to tens of meters. Furthermore, GPR can be employed to explore more shallow environments where detailed information on the decimeter scale is required. In consequence, 2D GPR reflection profiling is used on different spatial scales in permafrost applications such as active layer characterization and imaging of pingos. However, a 3D strategy might be essential for obtaining a reliable image of subsurface structures, if the geometry of such targets is complex (e.g., structures vary in three dimensions). Additionally, 3D data allow to identify out-of-plane reflection events which might interfere with reflections from target structures. This advantage is especially interesting for the application of GPR in cold environments, where out-of-plane reflections are favored due to a broadened radiation characteristic of GPR antennas on frozen ground compared to unfrozen ground. Here, we present a carefully designed 3D GPR acquisition and processing strategy (Schennen et al., 2016) and employ it to an exemplary data set. Our field site covers an area of approximately 20 m×70 m and is located on top of a Yedoma hill on Bol’shoy Lyakhovsky Island, Northern Siberia. Nearby borehole information provides cryostratigraphic details (up to a depth of approximately 30 m) interpreted in terms of three major stratigraphic units. These comprise two ice complex strata, which enclose a unit of floodplain deposits. Additional ground-truth is available from a 18 m high outcrop of the upper ice complex next to our survey area. Here, we observe large (up to 10 m ...