Airborne Electromagnetic Surveys
A special issue of Remote Sensing (ISSN 2072-4292). This special issue belongs to the section "Remote Sensing in Geology, Geomorphology and Hydrology".
Deadline for manuscript submissions: closed (31 July 2021) | Viewed by 26647
Special Issue Editors
Interests: airborne geophysics; airborne electromagnetics; groundwater and soil surveys
Interests: frequency and time domain airborne electromagnetics; semi-airborne electromagnetics
Special Issue Information
Dear Colleagues,
Airborne geophysical devices are being increasingly applied to quickly investigate large areas of subsurface at relatively low costs. From the most common airborne methods currently used, airborne electromagnetics (AEM) contributes most to high-resolution spatial subsurface investigations. AEM links areal remote sensing applications with local in-situ measurements. As the principal parameter investigated, the electrical conductivity, depends on various sources such as pore water salinity, clay content, or metals, AEM can be used for groundwater, soil, or mineral exploration studies.
We are interested in receiving high quality submissions that use large-scale AEM surveys to study the subsurface conductivity distribution and further applications derived from AEM results. In particular, we are looking for contributions that combine multiple parameters to investigate the near surface. Thus, joint interpretations of results of remote sensing, airborne- and ground-based surveys, as well as in-situ measurements are welcome. We are also interested in receiving submissions that use modern interpretation techniques such as cluster analyses and neuronal networks or further machine learning applications.
We look forward to receiving your manuscript.
Sincerely,
Dr. Bernhard Siemon
Dr. Annika Steuer
Dr. Andrea Viezzoli
Guest Editors
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Keywords
- Airborne geophysical surveys
- Electrical conductivity/resistivity
- Near-surface applications
- Large-scale soil mapping
- Large-scale groundwater mapping
- Large-scale geological mapping
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