Requirements for a multi-scale, ultra wide-band National Geoelectromagnetic Facility (Invited)

Advances in data acquisition technology and modeling make it possible to image the electrical properties of the near surface, crust and mantle in 3D. A generation of investigators is emerging whose research depends on application of complementary methods including magnetotelluric (MT) [micro-Hz to kHz sampling frequencies], natural audio (AMT) and controlled source and radio-frequency magnetotellurics (CSAMT, RFMT) [1 Hz-300 kHz], time-domain (TDEM) EM, as well as DC resistivity, induced polarization and ground-penetrating radar. Different process studies involve different depths and spatial scales, requiring target illumination by signals of different frequency content, and application of one or more of the methods above. Current practice often assumes that near surface and deeper crustal imaging problems can be decoupled by treating shallower heterogeneities in e.g. electrical conductivity structure as surface distortions that can be dealt with either through tensor stripping techniques or thin sheet modeling. Such methods are based on parametric models with implicit or explicit assumptions that may not in all cases be satisfied by the physics of the situation. Large-scale EM imaging programs such as EarthScope/USArray's magnetotelluric (MT) component seek to reconstruct the electrical conductivity structure of the US on the crustal-to-upper mantle scale. A variety of PI-led investigations seek to increase the resolving power of this effort through a combination of targeted, finer-spaced arrays, and by pushing into a higher frequency domain. As these efforts continue, great care has to be made in dealing with the impact of near surface heterogeneities. There is no national or regional scale set of near surface conductivity maps that one could use to strip near surface effects from deeper studies. National radio propagation/absorption maps were assembled by the FCC in the 1950's, and maps of ground-penetrating radar soil suitability provide a rough guide to surface conductance. Such information is insufficient to remove near surface effects for those imaging upper-to-mid crustal electrical properties. In order to obtain field measurements that can span near-surface through crust and upper mantle problems, an initiative to establish a multi-institutional National Geoelectromagnetic Facility has been proposed as part of a Virtual Institute for EM methods. An academic-industry partnership is designing a flexible, ultra wide-band system capable of being configured to obtain most of the data types indicated above. The system is specified to to provide between 100 dB - 130 dB dynamic range for sample rates from DC up to 2.5 MHz. A hybrid magnetic field sensor employing both induction coils and fluxgates, and a flexible arrangement of electric field sensors completes the specified receivers. The systems can be configured for sustained, low-power autonomous operation, or for higher power high frequency, active source operations. A series of controlled source transmitter systems is also specified. As financial support for the National Geoelectromagnetic Facility is being aligned, an organizational framework is being developed to permit efficient scheduling, data flow and archiving of resulting data sets. Education and outreach efforts are intrinsic to this, with close interactions with SAGE and other projects planned from the outset.