In magnetic fields above 10 tesla or so additional plateaus of the Hall conductivity at with are observed.
2.
Measurements of the thermal Hall conductivity are used to distinguish between the electronic and lattice contributions to thermal conductivity.
3.
Pedersen and Hall conductivities reach maximum values near 120 to 140 km altitudes with numbers of about 1 mS / m during sunlit conditions.
4.
This leads to oscillations in the observed energy of the highest occupied level, and hence in many physical properties ( including Hall conductivity, resistivity, and susceptibility ).
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