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40 COSMOS.is manifested during <strong>the</strong> twenty-five days immedia'.ely pro»ceding and succeeding <strong>the</strong> comet's perihelion passage. Thevalue of <strong>the</strong> constant is <strong>the</strong>refore somewhat different, becausein <strong>the</strong> neighborhood of <strong>the</strong> sun <strong>the</strong> highly attenuated butstill gravitating strata of <strong>the</strong> resisting fluid -are denser. Gibersmaintained"^ that this fluid could not be at rest, butmust rotate directly round <strong>the</strong> sun, and <strong>the</strong>refore <strong>the</strong> resistanceoffered to retrograde comets, like Halley's, must differwholly from that opposed to those comets having a directcourse, like Encke's. The perturbations of comets havinglong periods of revolution; and <strong>the</strong> difference of <strong>the</strong>ir magnitudes and sizes, complicate <strong>the</strong> results, and render it dilf?-cult to determine what is ascribable to individual forces.The gaseous matter constituting <strong>the</strong> belt of <strong>the</strong> zodiacallight may, as Sir John Herschelf expresses it, be merely <strong>the</strong>denser portion of this comet-resisting medium. Although itmay be shown that all nebulae are crowded stellar masses,indistinctly visible, it is certain that innumerable comets fill<strong>the</strong> regions of space with matter through <strong>the</strong> evaporation of<strong>the</strong>ir tails, some of which have a length of 56,000,000 ofmiles. Arago has ingeniously shown, on optical grounds, $that <strong>the</strong> variable stars which always exhibit white lightwithout any change of color in <strong>the</strong>ir periodical phases, mightafford a means of determining <strong>the</strong> superior hmit of <strong>the</strong> densityto be assunaed for cosmic al e<strong>the</strong>r, if we supposeit to beequal to gaseous terrestrial fluids in itspower of refraction.The question of <strong>the</strong> existence of an e<strong>the</strong>real fluid filling<strong>the</strong> regions of space is closely connected with one warmlyagitated by "Wollaston,^ in reference to <strong>the</strong> definite limit of<strong>the</strong> atmosp<strong>here</strong>— a limit which must necessarily exist at <strong>the</strong>elevation w<strong>here</strong> <strong>the</strong> specific elasticity of <strong>the</strong> air is equipoisedby <strong>the</strong> force of gravity. Faraday's ingenious experiments on* Olbers, in Schum., Asir. NacJir., No. 268, s. 58.t Outlines of Astronomy , ^ 55G, 597.X ^^ En assimilant la watiere tres rare qui rempllt les espaces cilesteiquant a ses proprietes refringcntes aux gas terrestres, la density de cettimatiere nz saurait depasscr nne certaine limite dont les observations deeiloilcs chcngeantes, p. e. cellcs d'' Algol ou de (3 de Persic, peuvent assignerla valeur?^— Arago, in <strong>the</strong> Annnaire pour 1842, p. 336-345." On comparing <strong>the</strong> extremely rare matter occupying <strong>the</strong> regions oif space withterrestrial gases, in respect to its refractive properties, we shall find that<strong>the</strong> density of this matter can not exceed a definite limit, whose valuemay be obtained from observations of variable stars, as, for instance,Algol or (3 Tersei."i <strong>See</strong> WoWaRton, Philos. Transact, for 1822. p 80' Sir.Tnlin TIerschelcyp. cU., ^M, 36.

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