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Newton’s theory of tail formation can be regarded as the Achilles’ heel of his theory of comets. The process that Newton introduced for tail formation was based on the function of the rarified and receding particles of the ether, which carried along the particles of cometary atmosphere. This assumption, as illustrated in chapter four and five of the present work, was unable to answer some challenging questions proposed even by Newton’s disciples. These questions can be classified into three groups based on (1) the role of different agents in the formation of a tail; (2) the interaction of the ethereal particles and the particles of the comet’s atmosphere; and (3) the interaction of the cometary atmosphere and the atmosphere of the sun.

In the first category, the questions were related to the basic factors responsible for triggering tail formation. Since some comets with perihelia around the orbit of Venus produced tails long before and after their closest approaches to the sun, it was a dilemma why the inner planets – including the earth – did not produce tails. In other words, it was a key question whether the amount of heat a comet received or the quality of its atmosphere was the main agent in the formation of a tail.

The second group of questions considered some sophisticated problems regarding the nature and function of the ethereal particles. Defined as the most subtle corpuscles in the cosmos, the ethereal particles had to carry along the atmospheric particles of a comet that undoubtedly were heavier and bigger. The insufficiency of the theory became more evident when it was found that the process had to be performed in a situation where the comet’s head was moving at a speed of a few thousands of miles per minute. Thus, the heating and rarifying of the ethereal particles were taking place in such a manner that they could move away the cometary particles with a speed more than the orbital speed of the comet and continue to recede for millions of miles. Furthermore, it was not known why Newton did not assign a role for the sun’s rays to act on the highly rarified particles of cometary tails.

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  95. The underlying social factors in development of astronomy were not only different in England and France, but also the diverse approaches of the British and the Continental mathematicians to analysis and mechanics brought about different levels of advancement in the calculus-related parts of mathematics. For the differences between the Newtonian calculus and that of Leibniz (which was maintained by the Continental mathematicians) see: Katz, A History of Mathematics, pp. 503–531; Boyer, A History of Mathematics, pp. 391–414; D. T. Whiteside, “Patterns of Mathematical Thought in the Late Seventeenth Century”, Archive for the History of Exact Sciences 1 (1961), pp. 173–388; Curtis Wilson, “The problem of perturbation analytically treated: Euler, Clairaut, d’Alembert”, in R. Taton and C. Wilson (eds.), The General History of Astronomy, vol. 2B, pp. 89–94;Craig Fraser, “Mathematics”, in Roy Porter (ed.), The Cambridge History of Science, Volume 4: Eighteenth-Century Science (Cambridge: Cambridge University Press, 2003), pp. 305–327; For a history of mathematics in Britain in the eighteenth century see Niccolò Guicciardini, The Development of Newtonian Calculus in Britain, 1700–1800 (Cambridge: Cambridge University Press, 1989); For a social history of science in France during the second half of the seventeenth century see: Roger Hahn, The Anatomy of a Scientific Institution, The Paris Academy of Sciences, 1666–1803 (Berkeley: University of California Press, 1971).

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  97. Regarding the uncertainties in the planetary masses, the perturbative effects of the undiscovered planets, and the problems in the method of approximation, Clairaut’s calculations had a fairly small error. See Yeomans, Comets, pp. 111–139; Pannekoek, A History of Astronomy, pp. 302–303; Curtis Wilson, “Clairaut’s Calculation of the Eighteenth-Century Return of Halley’s Comet”, Journal for the History of Astronomy 24 (1993), 1–15; Craig B. Waff, “Predicting the mid-eighteenth-century return of Halley’s Comet”, in R. Taton and C. Wilson, eds., The General History of Astronomy, vol. 2B, pp. 69–82; Peter Broughton, “The First Predicted Return of Comet Halley”, Journal for the History of Astronomy 16 (1985), 123–133; For a history of return of Halley’s comet in 1759 see: Simon Schaffer, “ Halley, Delisle, and the Making of the Comet”, in Norman J. W. Thrower, eds., Standing on the Shoulders of Giants, pp. 254–298; Craig B. Waff, “The First International Halley Watch: Guiding the Worldwide Search for Comet Halley, 1755–1759”, Ibid., pp. 373–411; Idem, Comet Halley’s First Expected Return: English Public Apprehensions, 1755–1758”, Journal for the History of Astronomy 17 (1986), 1–37; Ruth Wallis, “The Glory of Gravity–Halley’s Comet 1759”, Annals of Science 41 (1984), 279–286; Phillip Stewart, “Science and superstition: Comets and the French public in the eighteenth century”, American Journal of Physics 54 (1986), 16–24.

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(2008). Non-Newtonian Theories of Comets. In: A History of Physical Theories of Comets, From Aristotle to Whipple. Archimedes: New Studies In The History And Philosophy Of Science And Technology, vol 19. Springer, Dordrecht. https://doi.org/10.1007/978-1-4020-8323-5_6

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