Probing Shallow Aquifers in Hyper-Arid Dune Fields Using VHF Sounding Radar

• Published in: IEEE transactions on geoscience and remote sensing 2023-08, p.1-1
• Main Authors: Heggy, Essam, Normand, Jonathan C. L., Palmer, Elizabeth M., Scabbia, Giovanni, Al-Maktoumi, Ali K. S., Mazzoni, Annamaria, Blanton, Lee, Schaefer, Sophie J. N., Avouac, Jean-Philippe
• Format: Article
• Language: English
• Subjects: Airborne radar; Desert regions; Geophysical measurements; Ground penetrating radar; Hydrology; Losses; Radar; Soil; Spaceborne radar; Surveys; VHF radar; Water resources
• ISSN: 0196-2892
• DOI: 10.1109/TGRS.2023.3306286

Large-scale characterization of water table depth in shallow aquifers in hyper-arid areas provides crucial insights into groundwater dynamics under increasing anthropogenic discharge and climatic fluctuations. Due to their penetration capabilities into arid soils, airborne VHF sounding radars can achieve this objective under specific system design, topographic and geophysical constraints, superseding sporadic well logs and ground-based surveys that provide compromised assessments of the distribution and depth of these water bodies. One of the least constrained ambiguities limiting the design of such systems, however, is the maximum penetration depth in desiccated sandy soils, which cover a sizeable fraction of desert landscapes. To constrain the latter, we perform a ground survey using 50-and-80-MHz GPRs with effective dynamic ranges of ~80-dB at the surface to probe the unconfined aquifer under desiccated linear dunes in the Wahiba Sands in Oman. Our survey resolves the water table down to at least 69-m depth, the deepest achieved at VHF frequencies in hyper-arid terrains. We observe the average two-way plane-wave subsurface radar attenuation, accounting for both dielectric and scattering losses, to range from 0.1-to-1.4-dB/m through these sandy formations. Dielectric and scattering losses can be of equal magnitude depending on the sounding frequency and stratigraphic setting of the subsurface. Penetration depths to the water table are validated with TDEM measurements and well-log data. Additionally, we identify shallow paleochannels from L-band SAR observations that suggest modern meteoritic recharge of the probed aquifer, creating shallow localized anomalous losses in the radar signal in the first few meters. We conclude that the minimum requirements for an airborne VHF sounding radar to probe shallow aquifers at depths of tens of meters in sandy formations in hyper-arid areas are an SNR of 55-dB at the surface, a bandwidth of 10-MHz, and a surface h rms not exceeding 2 m.