7 resultados para Jaina


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On Pārśvanātha, 8th century B.C., 23rd Jaina Tīrthaṅkara.

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The influence of MnO2, CuO, and NiO on the thermal decomposition and explosivity of arylammonium perchlorates has been studied by differential thermal analysis (DTA) and explosive sensitivity measurements. The metal oxides considerably sensitize both decomposition and explosion and the sensitizing effect is in the order NiO < CuO < MnO2. The accelerated decomposition or explosion seems to occur via the formation of an intermediate, metal perchlorate arylamine complex. The experimental evidence for the mechanism put forward has been included.

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The paper is an essay in the comparative metaphysics of nothingness that begins by pondering why Leibniz thought of the opposite question as the preeminent one. In Eastern philosophical thought, like the numeral ‘zero’ (śānya) that Indian mathematicians first discovered, nothingness as non-being looms large and serves as the first quiver on the imponderables they seem to have encountered (e.g. ‘In the beginning was neither non-being nor being’ RgVeda X.129). The concept of non-being and its permutations of nothing, negation, nullity, receive more sophisticated treatment in the works of grammarians, ritual hermeneuticians, logicians, and their dialectical adversaries, variously across Jaina and Buddhist schools, in respect of the function of negation /the negative copula, nãn, fraying into ontologies of non-existence and extinction; not least also the suggestive tropes that tend to arrest rather than affirm the inexorable being-there of something. After some passing references to interests in non-being and nothingness in contemporary (Western) thinking, the paper dwells at some length on Heidegger’s extensive treatment of nothingness in his 1927 inaugural lecture ‘Was ist Metaphysik?’, published later as What is Metaphysics? The essay however distances itself from any pretensions toward a doctrine of Nihilism.

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The Global River Discharge (RivDIS) data set contains monthly discharge measurements for 1018 stations located throughout the world. The period of record varies widely from station to station, with a mean of 21.5 years. These data were digitized from published UNESCO archives by Charles Voromarty, Balaze Fekete, and B.A. Tucker of the Complex Systems Research Center (CSRC) at the University of New Hampshire. River discharge is typically measured through the use of a rating curve that relates local water level height to discharge. This rating curve is used to estimate discharge from the observed water level. The rating curves are periodically rechecked and recalibrated through on-site measurement of discharge and river stage.

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Cataloged from cover.