Müller, H; von Dobeneck, Tilo; Hilgenfeldt, Christian; SanFelipo, Bill; Rey, Daniel; Rubio, Belen (2012): (Figure 3) Modeled GEM-3 susceptibility and conductivity response under decreasing water depth [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.775957, In supplement to: Müller, H et al. (2012): Mapping the magnetic susceptibility and electric conductivity of marine surficial sediments by benthic EM profiling. Geophysics, 77(1), E43-E56, https://doi.org/10.1190/GEO2010-0129.1
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Comment:
This model result assumes that the sensor emerges from an infinite seawater half-space (kappa w = -9 x 10**-6 and Sigma w = 3 S/m; susceptibility in SI-units).
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | DEPTH, water | Depth water | m | Geocode | ||
2 | Magnetic susceptibility, volume | kappa | 10-6 SI | Müller, H | modelled | |
3 | Conductivity | Cond | mS/cm | Müller, H | modelled | 525Hz quadrature component |
4 | Conductivity | Cond | mS/cm | Müller, H | modelled | 2025Hz quadrature component |
5 | Conductivity | Cond | mS/cm | Müller, H | modelled | 4775Hz quadrature component |
6 | Conductivity | Cond | mS/cm | Müller, H | modelled | 16025Hz quadrature component |
7 | Conductivity | Cond | mS/cm | Müller, H | modelled | 525Hz in-phase component |
8 | Conductivity | Cond | mS/cm | Müller, H | modelled | 2025Hz in-phase component |
9 | Conductivity | Cond | mS/cm | Müller, H | modelled | 4775Hz in-phase component |
10 | Conductivity | Cond | mS/cm | Müller, H | modelled | 16025Hz in-phase component |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
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18000 data points
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