Patricius' Phenomenological Theory of Tides and Its Modern Relativistic
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Geometry, Mathematics, and Dialectic Beyond Aristotelian Science
Studies in History and Philosophy of Science 40 (2009) 243–257 Contents lists available at ScienceDirect Studies in History and Philosophy of Science journal homepage: www.elsevier.com/locate/shpsa Francesco Patrizi’s two books on space: geometry, mathematics, and dialectic beyond Aristotelian science Amos Edelheit De Wulf-Mansion Centre for Ancient, Medieval, and Renaissance Philosophy, Institute of Philosophy, Catholic University of Louvain, Kardinaal Mercierplein 2, BE-3000 Leuven, Belgium article info abstract Keywords: Francesco Patrizi was a competent Greek scholar, a mathematician, and a Neoplatonic thinker, well Francesco Patrizi known for his sharp critique of Aristotle and the Aristotelian tradition. In this article I shall present, in Space the first part, the importance of the concept of a three-dimensional space which is regarded as a body, Geometry as opposed to the Aristotelian two-dimensional space or interval, in Patrizi’s discussion of physical space. Mathematics This point, I shall argue, is an essential part of Patrizi’s overall critique of Aristotelian science, in which Aristotle Epicurean, Stoic, and mainly Neoplatonic elements were brought together, in what seems like an original Proclus theory of space and a radical revision of Aristotelian physics. Moreover, I shall try to show Patrizi’s dia- lectical method of definition, his geometrical argumentation, and trace some of the ideas and terms used by him back to Proclus’ Commentary on Euclid. This text of Proclus, as will be shown in the second part of the article, was also important for Patrizi’s discussion of mathematical space, where Patrizi deals with the status of mathematics and redefines some mathematical concepts such as the point and the line accord- ing to his new theory of space. -
Of Universal Gravitation and of the Theory of Relativity
ASTRONOMICAL APPLICATIONS OF THE LAW OF UNIVERSAL GRAVITATION AND OF THE THEORY OF RELATIVITY By HUGH OSCAR PEEBLES Bachelor of Science The University of Texas Austin, Texas 1955 Submitted to the faculty of the Graduate School of the Oklahoma State University in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE August, 1960 ASTRONOMICAL APPLICATIONS OF THE LAW OF UNIVERSAL GRAVITATION AND OF THE THEORY OF RELATIVITY Report Approved: Dean of the Graduate School ii ACKNOWLEDGEMENT I express my deep appreciation to Dr. Leon w. Schroeder, Associate Professor of Physics, for his counsel, his criticisms, and his interest in the preparation of this study. My appre ciation is also extended to Dr. James H. Zant, Professor of Mathematics, for his guidance in the development of my graduate program. iii TABLE OF CONTENTS Chapter Page I. INTRODUCTION. 1 II. THE EARTH-MOON T"EST OF THE LAW OF GRAVITATION 4 III. DERIVATION OF KEPLER'S LAWS OF PLAN.ET.ARY MOTION FROM THE LAW OF UNIVERSAL GRAVITATION. • • • • • • • • • 9 The First Law-Law of Elliptical Paths • • • • • 10 The Second Law-Law of Equal Areas • • • • • • • 15 The Third Law-Harmonic Law • • • • • • • 19 IV. DETERMINATION OF THE MASSES OF ASTRONOMICAL BODIES. 20 V. ELEMENTARY THEORY OF TIDES. • • • • • • • • • • • • 26 VI. ELEMENTARY THEORY OF THE EQUATORIAL BULGE OF PLANETS 33 VII. THE DISCOVERY OF NEW PLANETS. • • • • • • • • • 36 VIII. ASTRONOMICAL TESTS OF THE THEORY OF RELATIVITY. 40 BIBLIOGRAPHY . 45 iv LIST OF FIGURES Figure Page 1. Fall of the Uoon Toward the Earth • • • • • • • • • • 6 2. Newton's Calculation of the Earth's Gravitational Ef- fect on the Moon. -
«Legato Con Amore in Un Volume, Ciò Che Per L'universo Si Squaderna»
FLORILEGIO DI EDIZIONI DANTESCHE «legato con amore in un volume, ciò che per l’universo si squaderna» LIBRERIA PHILOBIBLON - LIBRERIA PREGLIASCO «legato con amore in un volume, ciò che per l’universo si squaderna» (Paradiso XXXIII, 86-87) Et per mia opinione questo commento e di un Jacopo Bolognese, che secondo il medesimo Landino scrisse nella patria lingua: per che ci sono molte parole Bolognesi, et si mostra molto informato delle cose di Bologna. V. B. (Postilla manoscritta di Vincenzo Buonanni apposta all’esemplare dell’edizione di Venezia, Vindelino da Spira, 1477; cfr scheda n. 1) Questo Florilegio dantesco, realizzato in collaborazione tra la Libreria Philobiblon e la Libreria Pregliasco, non è che una scelta dei libri di maggior pregio di una collezione dantesca di oltre mille opere, il cui catalogo completo vedrà senz’altro la luce prima del 690° anniversario della morte del Poeta. Comprenderà quasi tutte le edizioni critiche del Poema e delle opere cosiddette “minori”, nonché quattrocento volumi monografici ed opuscoli in varie lingue sui più variegati aspetti della figura di Dante. N.B. L’illustrazione in copertina si riferisce al n. 32, Suite acquerellata di Zatta. 1 Libreria PHILOBIBLON Libreria Antiquaria PREGLIASCO Piazza S. Simpliciano, 7 Via Accademia Albertina, 3 bis 20121 Milano 10123 Torino Tel. (+39) 02 89076643 Tel. (+39) 011.8177114 - Telefax (+39) Fax (+39) 02 89076644 011.8179214 Palazzo Massimo - Piazza dei Massimi, 3 e-mail: [email protected] 00186 Roma www.preliber.com Tel. (+39) 06 45555970 Fax (+39) 06 45555991 e-mail: [email protected] www.philobiblon.org redazione e responsabilità - Arturo e Umberto Pregliasco - Filippo Rotundo grafica - Francesco Pregliasco stampa - GRAFART CONDIZIONI DI VENDITA I libri sono garantiti completi e in buono stato, salvo indicazione contraria. -
Chapter 5 Water Levels and Flow
253 CHAPTER 5 WATER LEVELS AND FLOW 1. INTRODUCTION The purpose of this chapter is to provide the hydrographer and technical reader the fundamental information required to understand and apply water levels, derived water level products and datums, and water currents to carry out field operations in support of hydrographic surveying and mapping activities. The hydrographer is concerned not only with the elevation of the sea surface, which is affected significantly by tides, but also with the elevation of lake and river surfaces, where tidal phenomena may have little effect. The term ‘tide’ is traditionally accepted and widely used by hydrographers in connection with the instrumentation used to measure the elevation of the water surface, though the term ‘water level’ would be more technically correct. The term ‘current’ similarly is accepted in many areas in connection with tidal currents; however water currents are greatly affected by much more than the tide producing forces. The term ‘flow’ is often used instead of currents. Tidal forces play such a significant role in completing most hydrographic surveys that tide producing forces and fundamental tidal variations are only described in general with appropriate technical references in this chapter. It is important for the hydrographer to understand why tide, water level and water current characteristics vary both over time and spatially so that they are taken fully into account for survey planning and operations which will lead to successful production of accurate surveys and charts. Because procedures and approaches to measuring and applying water levels, tides and currents vary depending upon the country, this chapter covers general principles using documented examples as appropriate for illustration. -
Durham Research Online
Durham Research Online Deposited in DRO: 10 February 2011 Version of attached le: Accepted Version Peer-review status of attached le: Peer-reviewed Citation for published item: Banks, K.. (2007) 'Space and light : cinian neoplatonism and Jacques Peletier Du Mans's 'Amour des Amours'.', Biblioth equed'humanisme et renaissance., 69 (1). pp. 83-101. Further information on publisher's website: http://www.droz.org/fr/livre/?GCOI=26001100835230 Publisher's copyright statement: Additional information: Use policy The full-text may be used and/or reproduced, and given to third parties in any format or medium, without prior permission or charge, for personal research or study, educational, or not-for-prot purposes provided that: • a full bibliographic reference is made to the original source • a link is made to the metadata record in DRO • the full-text is not changed in any way The full-text must not be sold in any format or medium without the formal permission of the copyright holders. Please consult the full DRO policy for further details. Durham University Library, Stockton Road, Durham DH1 3LY, United Kingdom Tel : +44 (0)191 334 3042 | Fax : +44 (0)191 334 2971 https://dro.dur.ac.uk Space and Light: Ficinian Neoplatonism and Jacques Peletier Du Mans’s Amour des amours Jacques Peletier Du Mans‟s Amour des amours of 1555 uses the fiction of a cosmic voyage inspired by love in order to join together a collection of love poems with a series of meteorological and planetary ones: the latter represent the poet‟s discoveries upon flying into the cosmos -
Equilibrium Model of Tides Highly Idealized, but Very Instructive, View of Tides
Tides Outline • Equilibrium Theory of Tides — diurnal, semidiurnal and mixed semidiurnal tides — spring and neap tides • Dynamic Theory of Tides — rotary tidal motion — larger tidal ranges in coastal versus open-ocean regions • Special Cases — Forcing ocean water into a narrow embayment — Tidal forcing that is in resonance with the tide wave Equilibrium Model of Tides Highly Idealized, but very instructive, View of Tides • Tide wave treated as a deep-water wave in equilibrium with lunar/solar forcing • No interference of tide wave propagation by continents Tidal Patterns for Various Locations 1 Looking Down on Top of the Earth The Earth’s Rotation Under the Tidal Bulge Produces the Rise moon and Fall of Tides over an Approximately 24h hour period Note: This is describing the ‘hypothetical’ condition of a 100% water planet Tidal Day = 24h + 50min It takes 50 minutes for the earth to rotate 12 degrees of longitude Earth & Moon Orbit Around Sun 2 R b a P Fa = Gravity Force on a small mass m at point a from the gravitational attraction between the small mass and the moon of mass M Fa = Centrifugal Force on a due to rotation about the center of mass of the two mass system using similar arguments The Main Point: Force at and point a and b are equal and opposite. It can be shown that the upward (normal the the earth’s surface) tidal force on a parcel of water produced by the moon’s gravitational attraction is small (1 part in 9 million) compared to the downward gravitation force on that parcel of water caused by earth’s on gravitational attraction. -
Waves and Tides the Preceding Sections Have Dealt with the Types Of
CHAPTER XIV Waves and Tides .......................................................................................................... Introduction The preceding sections have dealt with the types of motion in the ocean that bring about transport of water massesin a definite direction during a considerable length of time. They have also dealt with the random motion, the turbulence, which is superimposed upon the general flow. Besidesthese types, one has also to consider the oscillating motion characteristic of waves. In general, this motion manifests itself to the observer more by the riseand fall of the sea surface than by the motion of the individual water particles. Waves have attracted attention since before the beginning of recorded history, and in recent years they have been the subject of extensive theoretical studies. Surveys of our knowledge as to the character of ocean waves have been presented by Cornish (1912, 1934), Krtimmel (1911), Patton and Mariner (1932) and by Defant (1929). Lamb (1932) has discussed the hydrodynamic theories of waves, and Thorade (1931) has given a comprehensive review of the theoretical studies of ocean waves and has compiled a long list of literature covering the period from 1687 to 1930. Our understanding of the waves of the ocean, how they are formed and how they travel, is as yet by no means complete. The reason is, in the first place, that actual observations at sea are so difficult that the characteristicsof the waves cannot easily be determined. In the second place, the theories that serve to bring the observed sequence of events in nature into intimate connection with experience gained by other methods of study are still incomplete, particularly because most theories are based on classicalhydrodynamics, which deal with wave motion in an idealized fluid. -
UNDERGRADUATE STUDY PROGRAMME Philosophy (Double-Major)
UNIVERSITYOFSPLIT FACULTY OF HUMANITIES AND SOCIAL SCIENCES UNDERGRADUATE STUDY PROGRAMME Philosophy (double-major) Class: 602-04/16-02/0002 Reg. No: 2181-190-02-2/1-16-0002 Split, December 2015 Undergraduate study programme Philosophy (double major) 1 GENERAL INFORMATION OF HIGHER EDUCATION INSTITUTION Name of higher education Faculty of Humanities and Social Sciences in Split institution Address Poljička cesta 35, 21000 Split, Croatia Phone Dean's Office: (021) 384 144 Fax (021) 329 288 E.mail [email protected] Internet address www.ffst.unist.hr GENERAL INFORMATION OF THE STUDY PROGRAMME Name of the study Undergraduate university study programme Philosophy (double- programme major) Provider of the study Faculty of Humanities and Social Sciences programme Other participants Type of study programme Vocational study programme☐ University study programmeX UndergraduateX Graduate☐ Integrated☐ Level of study programme Postgraduate☐ Postgraduate specialist☐ Graduate specialist☐ Academic/vocational title Bachelor (baccalaureus/baccalaurea) of Arts (BA) in Philosophy earned at completion of study (univ.bacc.phil.) Undergraduate study programme Philosophy (double major) 2 1. INTRODUCTION 1.1. Reasons for starting the study programme The idea of organizing Philosophy studies has been present ever since the foundation of the Department of Humanities in Split. The development of the Humanities and Social Studies was unthinkable without philosophy and the foundation of the Faculty of Humanities and Social Sciences in Split became meaningful upon establishing Philosophy studies. The study of philosophy is further justified by the fact that, apart from Split, the most southern city providing the opportunity of studying philosophy is Zadar which is at the very north of the Middle Dalmatia. -
Mental Models in Galileo's Early Mathematization of Nature
Stud. Hist. Phil. Sci. 34 (2003) 229–264 www.elsevier.com/locate/shpsa Mental models in Galileo’s early mathematization of nature Paolo Palmieri UCL London, Department of Science and Technology Studies, Gower Street, London WC1E 6BT, UK Received 21 June 2001; received in revised form 7 May 2002 1. Introduction: the question of Galileo’s early mathematization of nature Distinguishing between the mathematical followers of Archimedes, notably Gali- leo, and the Aristotelians of the late sixteenth century, William R. Shea asserted that ‘[m]athematicians, under the guidance of Euclid and Archimedes, viewed the world in terms of geometric shapes which obeyed mathematically expressible laws’.1 In my judgement, Shea’s view should be accepted, even though it was not only Euclid and Archimedes who escorted Galileo into new territories such as, for instance, Two New Sciences, or the Discourse on Buoyancy. A more complex picture has gradually emerged thanks to a number of studies that have examined in detail Galileo’s accept- ance of the Euclidean theory of proportions (or proportional reasoning) as the langu- age of early mathematized physics.2 Yet no research has so far been devoted to the cognitive mechanisms underlying Galileo’s mathematization of nature. This paper addresses some questions related to this theme by adopting a cognitive history perspective which relies on the theory of mental models (on mental models, see Sect. 2, Pt. I; on cognitive history, see Sect. 2, Pt. II). Moreover, through a discussion of Galileo’s alleged use of thought experi- ments the paper suggests how a cognitive history perspective might complement E-mail address: [email protected] (P. -
European Latin Drama of the Early Modern Period in Spain, Portugal and Latin America
1 European Latin Drama of the Early Modern Period in Spain, Portugal and Latin America Joaquín Pascual Barea Introduction In the Hispanic Neo-Latin theatre, ancient drama converged with cultured and popular medieval genres such as elegiac comedy, debates and religious performances, as well as humanistic comedy from Italy and from the Low Countries, and other dramatic, poetic and oratorical genres from the Modern Age. Before a historical survey, we also analyze the influence of Aristotle’s and Horace’s poetics and of ancient drama on Neo-Latin drama, paying particular attention to the structure, the number of acts, the characters, the use of prose or verse, and the main dramatic genres. The History of Neo-Latin drama in Iberia and Latin America has been divided into four periods. During the reign of the Catholic Kings (1479–1516), the first Latin eclogues and dialogues produced in Spain, and the works of Hercules Florus and Johannes Parthenius de Tovar in the Kingdom of Aragon deserve our interest. Under the King and Emperor Charles (1516–1556), we consider the main authors of Neo-Latin drama: Joannes Angelus Gonsalves and Joannes Baptista Agnesius in Valencia, and Franciscus Satorres in Catalonia; Joannes Maldonatus in Salamanca and Burgos; Joannes Petreius at the University of Alcalá de Henares, and Franciscus Cervantes de Salazar in Mexico, as well as Didacus Tevius in Portugal under John III (1521–1557). A few months before the reign of King Sebastian in Portugal and King Philip in Spain (1556–1598), the Society of Jesus started their dramatic activity in the different provinces of Iberia: Portugal, Andalusia, Castile, Toledo and Aragon. -
Thompson/Ocean 420/Winter 2005 Tide Dynamics 1
Thompson/Ocean 420/Winter 2005 Tide Dynamics 1 Tide Dynamics Dynamic Theory of Tides. In the equilibrium theory of tides, we assumed that the shape of the sea surface was always in equilibrium with the forcing, even though the forcing moves relative to the Earth as the Earth rotates underneath it. From this Earth-centric reference frame, in order for the sea surface to “keep up” with the forcing, the sea level bulges need to move laterally through the ocean. The signal propagates as a surface gravity wave (influenced by rotation) and the speed of that propagation is limited by the shallow water wave speed, C = gH , which at the equator is only about half the speed at which the forcing moves. In other t = 0 words, if the system were in moon equilibrium at a time t = 0, then by the time the Earth had rotated through an angle , the bulge would lag the equilibrium position by an angle /2. Laplace first rearranged the rotating shallow water equations into the system that underlies the tides, now known as the Laplace tidal equations. The horizontal forces are: acceleration + Coriolis force = pressure gradient force + tractive force. As we discussed, the tide producing forces are a tiny fraction of the total magnitude of gravity, and so the vertical balance (for the long wavelength appropriate to tidal forcing) remains hydrostatic. Therefore, the relevant force, the tractive force, is the projection of the tide producing force onto the local horizontal direction. The equations are the same as those that govern rotating surface gravity waves and Kelvin waves. -
Bibliotheca Platonica V1 N2 Nov-Dec 1889
VOL. 1. XO Vj EM BE R - D E C E M B E R , XO. 1 B ib l io t h e c a P latonica An Exponent of tf[e Platonic Philosophy. •^EDITED B Y * THOS. M. JOHNSON. D amabkios on Fir st Principles P hilosophic Morality—Alexander Wilder ON HOLINK88 P lato and His W ritings -Thus. M. Johnson Pi.atonic Cel ebration E cstasy—T U . Klimt P latonic Theory ok Educat ion—T. M. J. T eaching Morality—D avid m tcr L etter pr o m B. S t . H il a ir e M isc e l l a ne a B ibl io g r a ph ic a l Notes OSCEOLA, MO., U. S. A BIBLIOTHECA PLATONICA: rum .[sued bi-monthly. A philosophical aud philological exponent of the writings of Plato and his School. The chief aim of the B ibl io t h e c a Platonica will be the critical and philosophic examination and interpretation of the writings of Plato, Aristotle, and the Neoplatonists. The literary history and characteristics of the Platonic writings, philological researches, emen dations of the text; philosophical analyses and interpretations, discus sions and book reviews—all will receive appropriate treatment. Many important Platonic suggestions, notes, emendations and ex positions, made by European and American scholars, never see the light for want of a proper organ. The B ibl io t hec a Platonica will be we hope a medium through which Platonic students the world over may communicate for the common benefit the results of their labors, alike philological and philosophical.