| sir George Biddell Airy - 1826 - 208 páginas
.... 2 ' V - sin t rnIZ ' -l_ 1 N hence — - 1 = - - - = D (n + 1), suppose ; and This determines w, that is, the ratio of the mass of the Earth to the mass of the Moon. If we calculate the values of C and 2" T D with the values of t, — , and — , already given, n + l= rx 47,52- 177,56.... | |
| George Biddell Airy, Sir George Biddell Airy - 1831 - 442 páginas
.../ 3 . , \ T2 1 sm % \ \ 2 ) a T°~(n+l) hence — — l = — = D (n + 1), suppose ; bC T2fl--sin " This determines n, that is, the ratio of the mass...the Earth to the mass of the Moon. If we calculate the values of C and 7* T D with the values of i, — , and — , already given, n+l = -.47,52 — 177,56.... | |
| Cambridge univ, exam. papers - 1856 - 252 páginas
...precessional movement. How will the amount of precession, as deduced from observation, aid in determining the ratio of the mass of the Earth to the mass of a pound weight ? 7. What is meant by secular variations of planetary elements ? Shew how to find the... | |
| 1877 - 420 páginas
...M' * -=-= =319824,* the ratio of the mass of the Sun to the •"* mass of the Earth. ^ = X = 81'5, the ratio of the mass of the Earth to the •"* mass of the Moon. Number of seconds in the mean annual Solar Precession = 2w x 206265 x ^ = 2w x 206265 xf - . ~ cosw... | |
| Arthur Gordon Webster - 1904 - 612 páginas
...the ratio of the attraction of the sphere and cone to that of the sphere alone, and from this we get the ratio of the mass of the earth to the mass of the mountain. Such a determination was carried out by Mendenhall, on Fujiyama, Japan, in 1880, giving 5.77... | |
| Royal Astronomical Society - 1925 - 1104 páginas
...±o* -005. The value of the solar parallax derived in this way is dependent upon the value assumed for the ratio of the mass of the Earth to the mass of the Moon, but this ratio is now known with sufficient accuracy for its effect on the solar parallax to be practically... | |
| United States. Army. Corps of Engineers - 1940 - 318 páginas
...equilibrium tide. — Assigning to the constants in equation (16) their numerical values, the ratio, M/E, of the mass of the earth to the mass of the moon is 1/81.45; a, the mean radius of the earth, 3,959 statute miles; R, the mean distance to the moon,... | |
| United States. Army. Corps of Engineers - 1940 - 312 páginas
...equilibrium tide. — Assigning to the constants in equation (16) their numerical values, the ratio, M/E, of the mass of the earth to the mass of the moon is 1/81.45; a, the mean radius of the earth, 3,959 statute miles; R, the mean distance to the moon,... | |
| George Bigelow Pillsbury - 1940 - 308 páginas
...equilibrium tide. — Assigning to the constants in equation (16) their numerical values, the ratio, M/E, of the mass of the earth to the mass of the moon is 1/81.45; a, the mean radius of the earth, 3,959 statute miles; R, the mean distance to the moon,... | |
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