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![]() It is notable how much static electricity can build up from the falling of various sized water droplets in a thunderstorm. Basic questions: What are the electrical conductivity properties of the both the solid and liquid cores at such high temperatures and pressures? Are there significant differences in the electrical properties of the two types of core and intermediates? What are the electircal properties of the junctions between the liquid metal core and the semisolid magma mantle? Is magma at such high temperatures and pressures still going to be an insulator? What about magma with a high level of liquid metal embedded in it possibly as a metal droplet ('aerosol'?) or as metal complexes with partially dissolved magma impurities. Is magma going to be be withdrawing electric charge from the liquid metal core, or adding charge to it? Are the electrical junctions at the magma-core boundary significant when it comes to the earth's magnetic field? What would be the likely electrical and magnetic properties of magma particles flowing and being carried by the physical movement of the liquid metal in the outer liquid metal core? Is the magma-core boundary significant when it comes to geomagnetism? On a non-electrical side note, is the more solid inner metal core generally plastic? Would it allow the migration of heavier metal components further toward the center. (Effectively concentrating lead, uranium, and the heavier metals toward the furthest and lowest interior?) |
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