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Theories of the origin of the solar system 1956-1985

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Attempts to find a plausible naturalistic explanation of the origin of the solar system began about 350 years ago but have not yet been quantitatively successful. The period 1956--1985 includes the first phase of intensive space research; new results from lunar and planetary exploration might be expected to have played a major role in the development of ideas about lunar and planetary formation. While this is indeed the case for theories of the origin of the moon (selenogony), it was not true for the solar system in general, where ground-based observations (including meteorite studies) were frequently more decisive. During this period most theorists accepted a monistic scenario: the collapse of a gas-dust cloud to form the sun with surrounding disk, and condensation of that disk to form planets, were seen as part of a single process. Theorists differed on how to explain the distribution of angular momentum between sun and planets, on whether planets formed directly by condensation of gaseous protoplanets or by accretion of solid planetesimals, on whether the solar nebula'' was ever hot and turbulent enough to vaporize and completely mix its components, and on whether an external cause such as a supernova explosion triggered'' the initial collapse of the cloud. Only in selenogony was a tentative consensus reached on a single working hypothesis with quantitative results.

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Attempts of applying stellar polarization spectra to evaluation of magnetic fields of some types of stars are described.
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There is an ancient Irish folk-tale, rewritten by Padraic Colum in a book called The King of Ireland’s Son, about a prince who goes out into the world to find the secret of his own childhood—the beginning and the end of the Unique Tale. His companion on the quest is Gilly of the Goatskin; and in the end, it appears that the boyhood of neither can be understood without the other.
Article
La naissance de la Lune lors de l'impact d'un objet unique massif, de la taille de Mars, avec la Terre peut expliquer le moment angulaire specifique et les caracteristiques orbitales du systeme Terre-Lune. Les differences chimiques et de densite de la Terre et de son Satellite sont alors liees a la composition du manteau de l'impacteur. On discute de la validite de cette hypothese en montrant qu'il est possible de former un tel impacteur dans la nebuleuse proto-solaire interne
Article
In the 1950's and 60's there arose a plethora of claims that the structure of evolutionary theory was intrinsically different from the structures of the theories of physics—and thus from the structure that philosophers of science claimed to be the structure of scientific theories. There were claims: 1) that evolutionary theory had no laws (Smart 1963); 2) that evolutionary concepts were so peculiar that their definitions violated the ordinary standards for definitions (Beckner 1959); 3) that evolutionary theory was not axiomatizable (Beckner 1959); 4) that evolutionary theory made no falsifiable predictions (Scriven 1959, Manser 1965, Smart 1963); 5) that evolutionary biology relied on teleological explanations which violated the deductive-nomological explanation form (Hempel 1965); and 6) that evolutionary biology made significant use of narrative explanations which also violated the deductive-nomological explanation form (Goudge 1961)
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Science is accorded high value in our culture because, unlike many other intellectual endeavors, it appears capable of producing increasingly reliable knowledge. During the last quarter century a group of historians and philosophers of science (known variously as ‘theorists of scientific change’, the ‘post-positivist school’ or the ‘historical school’) has proposed theories to explain progressive change in science. Their concepts and models have received such keen attention that terms like ‘paradigm’ have passed from obscurity to common speech. In this volume, we subject key claims of some of the theorists of scientific change to just that kind of empirical scrutiny that has been so characteristic of science itself. Certain claims emerge unscathed — the existence and importance of large-scale theories (guiding assumptions) in the physical sciences for example. Others, such as the supposed importance of novel predictions or the alleged insignificance of anomalies, seem to be without foundation. We conclude that only by engaging in testing of this sort will the study of science be able to make progress.
Article
We live in a society which sets great store by science. Scientific ‘experts’ play a privileged role in many of our institutions, ranging from the courts of law to the corridors of power. At a more fundamental level, most of us strive to shape our beliefs about the natural world in the ‘scientific’ image. If scientists say that continents move or that the universe is billions of years old, we generally believe them, however counter-intuitive and implausible their claims might appear to be. Equally, we tend to acquiesce in what scientists tell us not to believe. If, for instance, scientists say that Velikovsky was a crank, that the biblical creation story is hokum, that UFOs do not exist, or that acupuncture is ineffective, then we generally make the scientist’s contempt for these things our own, reserving for them those social sanctions and disapprobations which are the just deserts of quacks, charlatans and con-men. In sum, much of our intellectual life, and increasingly large portions of our social and political life, rest on the assumption that we (or, if not we ourselves, then someone whom we trust in these matters) can tell the difference between science and its counterfeit.
Article
The dynamics of two dimensional jetstreams have been studied by following the evolution of simulation particle populations for different collision models. Collisions, independent of details of the collision model, rapidly lead to the establishment of a distribution of perihelion vectors of the form ~exp(-α(P-η)2), the characteristic time for this process being of the order of magnitude equal to the mean free collision time. Under appropriate conditions a radial focusing takes place. In terms of the varians of semi-major axis a focusing exceeding a factor 2 has been achieved. Necessary conditions for the existence of this radial focusing are a sufficient degree of inelasticity and the requirement that the dominant part of the velocity change in a typical collision is along the pre-collisional relative velocity vector. The properties of grazing collisions are especially important in this respect.
Article
Nucleosynthesis associated with explosive carbon burning is reexamined, with the aim of providing a realistic prediction of the abundance of /sup 26/Al formed under such conditions. The sensitivities of the /sup 26/Al//sup 27/Al production ratio to variations in the temperature, the initial composition, and the degree of neutron competition from heavy nuclei are explored. Ratios of /sup 26/Al//sup 27/Al in the range 4 x 10/sup -4/ to 2 x 10/sup -3/ are found to result for the range of conditions considered. For a primordial solar-system ratio /sup 26/Al//sup 27/Alapprox. =6 x 10/sup -5/ (Lee, Papanastassiou, and Wasserburg), these production ratios imply that primitive solar matter was influenced by a nucleosynthesis event which could not have occurred more than a few million years prior to condensation.
Article
At the end of the nineteenth century, Lord Kelvin's upper limit of only 20 or 30 million years for the age of the Earth was challenged by the American geologist T. C. Chamberlin, who showed that Kelvin's model of an Earth gradually cooling from an initial molten state was not the only possible one. Kelvin's limit was soon afterwards repealed by the new science of radioactivity, which yielded ages of a few billion years. While some geologists resisted this expanded time-scale, Chamberlin was the only one who could provide a comprehensive cosmogonical theory that did not submit to the epistemological superiority of physics and astronomy. In the 1940s, as radiometric age determinations improved in accuracy, they came into conflict with the expanding-universe cosmology — a conflict which the cosmologists eventually avoided by expanding their distance and time scales. In 1953, Patterson announced the result 4.5 billion years, which is still accepted as the best estimate for the age of the Earth. But geologists, liberated from Kelvin's limit, define the epoch of the Earth's formation as being outside the scope of their science, and their textbooks rarely give credit to the person who established the number that once seemed so important to accounts of the Earth's history.
Article
In mixed leukocyte cultures prepared ’ from pairs of normal unrelated donors, some of the lymphocytes became transformed to large cells capable of mitosis. Subsequent experiments indicated that transformation was stimulated by genetically determined factors in leukocytes. A relationship to transplantation immunity was suggested. [The SCI ® indicates that this paper has been cited over 505 times since 1964.]
Article
DOI:https://doi.org/10.1103/RevModPhys.28.53
Article
Comments are given concerning a paper by Bonsack and Greenstein (1960) on the abundance of lithium in T Tauri stars and on the origin of the solar system. The lithium evidence strongly suggests that planetary materials once were part of the sun as an outer envelope that was later thrown off; and then, perhaps through magnetic interaction, regained almost all the angular momentum initially present in the sun. The inference was drawn that T Tauri stars must be capable of manufacturing lithium, and it was estimated that there was at least ten times more lithium per gram of material on the surfaces of the stars than in the surrounding nebular material. (B.O.G.)
Article
In the Preplanetary dust cloud, particle adhesion and aggregation Would have been most effective for magnetic grains. Enrichment of iron in the region of the inner planets could have occurred by a particle-size fractionation, the outward dispersal of small, metal-poor aggregates leaving behind only the larger aggregates enriched in magnetic particles of iron.
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Article
In considering our space program, it is well to study objects that arrive from extraterrestrial sources quite without any effort or expense on our part. It is my purpose to discuss recent and older observations of meteorites and to draw some tentative conclusions from them. Meteorites are objects of variable structure and chemical composition, and a complete review of their properties is impossible in a brief time; therefore, this discussion will be limited to some specific features from which certain conclusions will be drawn. I believe that these conclusions will not be contrary to evidence that is not reviewed.
Article
A survey of the abundances of elements in the ocean and sedimentary rocks as compared to their abundances in the weathered igneous rocks shows that carbon, nitrogen, oxygen as water, chlorine, bromine and boron are highly concentrated in the surface materials and that thicknesses of from 17 to 89 km of the outer part of the earth would be required to produce these elements if all of them now present in the igneous rocks were removed. A study of the available information indicates that many other elements would be concentrated at the earth's surface if chlorine, bromine and boron were concentrated there by a high-temperature volatilization process either from volcanoes or in an original high-temperature atmosphere of the earth. It is concluded that the removal of these elements from the outer parts of the earth occurred through solution in water at low or moderate temperatures (\sim 100 degrees C or less), since they are soluble and other elements are not. Iodine should belong to this group, but its position is uncertain because of doubtful analytical data. Sulphur may belong in some degree with the volatiles, i.e. carbon as methane or carbon dioxide, nitrogen as ammonia or molecular nitrogen, and water. It is shown that the low abundances of mercury and arsenic in the sediments are inconsistent with a temperature of formation of the earth's surface regions higher than a few hundred degrees centigrade. The presence of appreciable quantities of nitrogen in the igneous rocks indicates that this element was present in condensed phases during the earth's formation, and a survey of the conditions of stability of such compounds indicates temperatures of about 200 degrees C or less. It has not been possible to decide whether liquid water was present on the primitive earth.
Article
Data on the composition of the satellites of the outer planets and the composition and structure of planetary atmospheres are briefly reviewed in light of simple models for the origin of the solar system and the planets. Some crucial tests of present theories are suggested.