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Planetary g(t) for which resistive atmospheric falling is rising | | H.C. Rosu
; F. Aceves de la Cruz
; | | Date: |
17 Aug 2001 | | Subject: | gr-qc | | Abstract: | 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. The result is a consequence of general, one-parameter-dependent Darboux transformations in mathematical physics | | Source: | arXiv, gr-qc/0108044 | | Services: | Forum | Review | PDF | Favorites | |
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