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the link does not work any more Ra-raisch ( talk) 20:34, 4 February 2019 (UTC)
I found the definition of kL = 3J2vo²/vt² in [1] with J2=(Jz-Jx)/r²m, vt²=ω²r² and vo²=Gm/r. Ra-raisch ( talk) 18:31, 10 February 2019 (UTC)
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. King of Tea Tree ( talk) 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. King of Tea Tree ( talk) 07:28, 1 March 2020 (UTC)
Measures the rigidity of a planetary body and its susceptibility to change shape in response to a tidal potential.
The first numbers are the ones that I decided are probably the most correct, and the ones in parentheses are others I found online.
The tidal Love number k₂ can be approximated from planet mass (m) by the formula "k₂ = 2e24m^0.82" for smaller terrestrial worlds, "k₂ = 5e25m^2.03" for earth-like worlds, and "k₂ = 2e28m^3.5" for giant planets. These formulas are extrapolated from the above data.
SnailsAttack ( talk) 15:09, 30 June 2021 (UTC)
![]() | This article is rated Start-class on Wikipedia's
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the link does not work any more Ra-raisch ( talk) 20:34, 4 February 2019 (UTC)
I found the definition of kL = 3J2vo²/vt² in [1] with J2=(Jz-Jx)/r²m, vt²=ω²r² and vo²=Gm/r. Ra-raisch ( talk) 18:31, 10 February 2019 (UTC)
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. King of Tea Tree ( talk) 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. King of Tea Tree ( talk) 07:28, 1 March 2020 (UTC)
Measures the rigidity of a planetary body and its susceptibility to change shape in response to a tidal potential.
The first numbers are the ones that I decided are probably the most correct, and the ones in parentheses are others I found online.
The tidal Love number k₂ can be approximated from planet mass (m) by the formula "k₂ = 2e24m^0.82" for smaller terrestrial worlds, "k₂ = 5e25m^2.03" for earth-like worlds, and "k₂ = 2e28m^3.5" for giant planets. These formulas are extrapolated from the above data.
SnailsAttack ( talk) 15:09, 30 June 2021 (UTC)