The Scientific Papers of Sir George Darwin 2009
DOI: 10.1017/cbo9780511703515.008
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Address to the International Congress of Mathematicians at Cambridge in 1912

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Cited by 7 publications
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“…where R p is the radius of the planet and q p and q s are the mean densities of the planet and moon respectively; while M P is the mass of the planet and f is a numerical factor which for a rigid spherical satellite is f ¼ 2 1 3 ¼ 1:26 (Scharf 2006); while for a fluid-like body it is given by f = 2.44, (Darwin 1908). A moon moving inside this limit would either collide with the planet or be torn apart very rapidly by the tidal forces exerted by the planet (see Donnison and Williams 1975 for an estimate of the likely dispersal timescale).…”
Section: Stability Limitsmentioning
confidence: 99%
“…where R p is the radius of the planet and q p and q s are the mean densities of the planet and moon respectively; while M P is the mass of the planet and f is a numerical factor which for a rigid spherical satellite is f ¼ 2 1 3 ¼ 1:26 (Scharf 2006); while for a fluid-like body it is given by f = 2.44, (Darwin 1908). A moon moving inside this limit would either collide with the planet or be torn apart very rapidly by the tidal forces exerted by the planet (see Donnison and Williams 1975 for an estimate of the likely dispersal timescale).…”
Section: Stability Limitsmentioning
confidence: 99%
“…A rapid phase of mass loss from the more evolved star may occur, leading to the engulfment of its companion provided that the less-evolved companion rapidly expands to fill its own Roche lobe (see Kippenhahn & Meyer-Hofmeister 1977) in response to mass accretion. An alternative evolutionary channel to the common envelope phase can take place as a result of a tidal instability (Darwin 1908) if there is insufficient orbital angular momentum in the system for the evolved star to be in a state of synchronous rotation with its companion. This occurs when…”
Section: Primary Main-sequence Evolutionmentioning
confidence: 99%
“…The researches of George Darwin were the most detailed in the evaluation of specific results. 6 He introduced a principal-axis frame and derived equations of motion for this frame. He was able to show that a movement of the poles of 8 deg would require one half of the Earth's surface to be deflected by nearly 2 miles.…”
Section: Floating Frames For Deformable Bodiesmentioning
confidence: 99%