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The tidal Love number kâ‚‚ can be approximated from planet mass (m) by the formula "kâ‚‚ = 2e24m^0.82" for smaller terrestrial worlds, "kâ‚‚ = 5e25m^2.03" for earth-like worlds, and "kâ‚‚ = 2e28m^3.5" for giant planets. These formulas are extrapolated from the above data.
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The following paper was submitted in 1908, then read early 1909. It is available as a free .pdf from Roy Soc. LOVE, A. E. H., 1909. "The yielding of the earth to disturbing forces". Proc. Roy. Soc. London, A 82, pp. 73 – 88.
471:) 11:53, 24 February 2020 (UTC) The Love numbers h and k are first introduced at the end of section 3 of Love's 1909 paper “The Yielding of the Earth to Disturbing Forces”. That paper was submitted on 18 Nov 1908.
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The first numbers are the ones that I decided are probably the most correct, and the ones in parentheses are others I found online.
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Measures the rigidity of a planetary body and its susceptibility to change shape in response to a tidal potential.
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on
Knowledge. If you would like to participate, please visit the project page, where you can join
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resource. If you would like to participate, you can choose to edit this article, or visit the
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Tidal Love
Numbers (kâ‚‚) of Solar System Objects (plus notes, analysis and empirical formulas)
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Io: 0.09 (or as much as 0.5 with a very high melt fraction, i.e. magma ocean)
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500:Moon: 0.024±0.002 (0.02405, 0.0222, 0.02664)
598:Start-Class physics articles of Low-importance
538:More homogenous interior = higher love number
8:
541:More stratified interior = lower love number
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503:Mercury: 0.485±0.04 (0.0965, 0.52, 0.45)
512:Jupiter: 0.58±0.07 (0.525, 0.565, 0.66)
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533:Higher mantle mass = lower love number
530:Higher core mass = higher love number
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308:This article is within the scope of
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38:It is of interest to the following
506:Venus: 0.275±0.02 (0.295, 0.254)
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518:Saturn: 0.36±0.03 (0.341, 0.39)
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521:Titan: 0.47±0.1 (0.36, 0.57)
509:Mars: 0.168 (0.168, 0.0712)
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404:I found the definition of k
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