-
(Figure 10b, 11) Benthic electromagnetic profile of GeoB130106 on the northwe...
Porosity is derived from Archie's law with constants m = 1.6, a = 1 and 14.4% offset (susceptibility with 37.7 offset; based on Figure 9). -
(Figure 10a, 11, 12) Benthic electromagnetic profile of GeoB130124 on the nor...
Porosity is derived from Archie's law with constants m = 1.6, a = 1 and 14.4% offset (susceptibility with 37.7 offset; based on Figure 9). -
(Figure 9b) Correlation of EM and sediment core susceptibility
This dataset has no description
-
(Figure 9a) Correlation of EM and sediment core porosity
EM Porosity is derived from Archie's law with constants m = 1.6 and a = 1. -
(Figure 7b) Apparent susceptibility profiles by various available sensor size...
Assumption: magnetite dissolution sets in at depths of 0.2-0.8 m and is completed 0.2 m deeper. -
(Figure 7a) Simulations of apparent susceptibility and conductivity profiles ...
This dataset has no description
-
(Figure 6b) Horizontal footprint diameter (90% of the total signal) and half-...
This dataset has no description
-
(Figure 6a) Lateral response of GEM-3 sensor (96 cm coil) for susceptibility ...
This dataset has no description
-
(Figure 5c) In-phase and quadrature responses of GEM-3 sensor at various oper...
The models are based on 0.1% perturbations of an homogenous seafloor model with seawater (and sediment) conductivities/susceptibilities of 3 S/m and -9 x 10-6 (1 S/m and 100 x... -
(Figure 5b) Vertical sensor characteristics of GEM-3 (96 cm coil) for quadrat...
The models are based on 0.1% perturbations of an homogenous seafloor model with seawater (and sediment) conductivities/susceptibilities of 3 S/m and -9 x 10-6 (1 S/m and 100 x... -
(Figure 4a) Relative contribution of the magnetic response to total in-phase ...
This dataset has no description
-
(Figure 3) Modeled GEM-3 susceptibility and conductivity response under decre...
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). -
(Figure 2) Primary magnetic field intensity distribution of EM sensor
DISTANCE [cm] = vertical distance -
Sediment electric conductivity profiles of benthic EM profiler NERIDIS during...
Sediment-physical properties of the seabed mapped with the MARUM benthic EM profiler NERIDIS III during HEINCKE cruise HE537. The profiler was towed in contact with the seabed... -
Sediment electric conductivity profiles of benthic EM profiler NERIDIS during...
Sediment-physical properties of the seabed mapped with the MARUM benthic EM profiler NERIDIS III during HEINCKE cruise HE537. The profiler was towed in contact with the seabed... -
Sediment electric conductivity profiles of benthic EM profiler NERIDIS during...
Sediment-physical properties of the seabed mapped with the MARUM benthic EM profiler NERIDIS III during HEINCKE cruise HE537. The profiler was towed in contact with the seabed... -
Magnetic susceptibility and electric conductivity of marine surficial sedimen...
Distribution, accumulation and diagenesis of surficial sediments in coastal and continental shelf systems follow complex chains of localized processes and form deposits of great... -
Permanent Magnetotelluric Reference Station Wittstock, Germany
Magnetotellurics (MT) is a passive geophysical method which uses natural variations of electromagnetic fields generated by global lightning discharges and ionospheric current... -
Electromagnetic induction of horizontally oriented dipole from CMD Explorer (...
This dataset has no description
-
Electromagnetic induction of horizontally oriented dipole from CMD Explorer (...
This dataset has no description
