X iv : g r - qc / 0 10 80 44 v 2 2 3 A ug 2 00 1 Planetary g ( t ) for which resistive atmospheric falling is rising
نویسنده
چکیده
A Darboux-transformed surface gravitational acceleration of the constant gravitational acceleration for a body endowed with an atmospheric layer is shown to turn the atmospheric free fall with quadratic resistance in the opposite motion, i.e., a free rising. Although the atmosphere of such a body may look completely normal, it is the time dependence of its gravitational field that produces this type of motion. This result is a consequence of general, one-parameter-dependent Darboux transformations in mathematical physics.
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ar X iv : g r - qc / 0 10 80 44 v 1 1 7 A ug 2 00 1 Planetary g ( t ) for which resistive atmospheric falling is rising
A Darboux-transformed surface gravitational acceleration of the constant gravitational acceleration for a body endowed with an atmospheric layer is shown to turn the atmospheric free fall with quadratic resistance in the opposite motion, i.e., a free rising. Although the atmosphere of such a body may look completely normal, it is the time dependence of its gravitational field that produces this...
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