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UNIVERSIDADE ESTADUAL PAULISTA "JÚLIO DE MESQUITA FILHO" CAMPUS DE GUARATINGUETÁ TIAGO FRANCISCO LINS LEAL PINHEIRO Estudo da sailboat para sistemas binários Guaratinguetá 2016 Tiago Francisco Lins Leal Pinheiro Estudo da sailboat para sistemas binários Trabalho de Graduação apresentado ao Conselho de Curso de Graduação em Bacharel em Física da Faculdade de Engenharia do Campus de Gua- ratinguetá, Universidade Estatual Paulista, como parte dos requisitos para obtenção do diploma de Graduação em Bacharel em Física . Orientador: Profo Dr. Rafael Sfair Guaratinguetá 2016 Pinheiro, Tiago Francisco Lins Leal L654e Estudo da sailboat para sistemas binários / Tiago Francisco Lins Leal Pinheiro– Guaratinguetá, 2016. 57 f.: il. Bibliografia: f. 53 Trabalho de Graduação em Bacharelado em Física – Universidade Estadual Paulista, Faculdade de Engenharia de Guaratinguetá, 2016. Orientador: Prof. Dr. Rafael Sfair 1. Planetas - Orbitas 2. Sistema binário (Matematica) 3. Metodos de simulação I. Título . CDU 523. DADOS CURRICULARES TIAGO FRANCISCO LINS LEAL PINHEIRO NASCIMENTO 03/06/1993 - Lorena / SP FILIAÇÃO Roberto Carlos Pinheiro Jurema Lins Leal Pinheiro 2012 / 2016 Bacherelado em Física Faculdade de Engenharia de Guaratin- guetá - UNESP 2011 Bacherelado em Engenharia de Produção Centro Universitário Salesiano de São Paulo - UNISAL 2008 / 2010 Ensino Médio Instituto Santa Teresa AGRADECIMENTOS Em primeiro lugar agradeço a Deus, fonte da vida e da graça. Agradeço pela minha vida, minha inteligência, minha família e meus amigos, ao meu orientador, Prof. Dr. Rafael Sfair que jamais deixou de me incentivar. Sem a sua orientação, dedicação e auxílio, o estudo aqui apresentado seria praticamente impossível. aos meus pais Roberto Carlos Pinheiro e Jurema Lins Leal Pinheiro, e irmãos Maria Teresa, Daniel, Gabriel e Rafael, que apesar das dificuldades enfrentadas, sempre incentivaram meus estudos. -
Universidade Estadual Paulista "Júlio De Mesquita Filho" Campus De Guaratinguetá
UNIVERSIDADE ESTADUAL PAULISTA "JÚLIO DE MESQUITA FILHO" CAMPUS DE GUARATINGUETÁ TIAGO FRANCISCO LINS LEAL PINHEIRO Estudo da estabilidade de anéis em exoplanetas Guaratinguetá 2019 Tiago Francisco Lins Leal Pinheiro Estudo da estabilidade de anéis em exoplanetas Trabalho Mestrado apresentado ao Conselho da Pós Graduação em Mestrado em Física da Faculdade de Engenharia do Campus de Guaratinguetá, Univer- sidade Estatual Paulista, como parte dos requisitos para obtenção do diploma de Mestre em Mestrado em Física . Orientador: Profo Dr. Rafael Sfair Guaratinguetá 2019 Pinheiro, Tiago Francisco Lins Leal P654E Estudo da estabilidade de anéis em exoplanetas / Tiago Francisco Lins Leal Pinheiro – Guaratinguetá, 2019. 57 f : il. Bibliografia: f. 54 Dissertação (Mestrado) – Universidade Estadual Paulista, Faculdade de Engenharia de Guaratinguetá, 2019. Orientador: Prof. Dr. Rafael Sfair 1. Exoplanetas. 2. Satélites. 3. Métodos de simulação. I. Título. CDU 523.4(043) Luciana Máximo Bibliotecária/CRB-8 3595 DADOS CURRICULARES TIAGO FRANCISCO LINS LEAL PINHEIRO NASCIMENTO 03/06/1993 - Lorena / SP FILIAÇÃO Roberto Carlos Pinheiro Jurema Lins Leal Pinheiro 2012 / 2016 Bacharelado em Física Universidade Estadual Paulista "Júlio de Mesquita Filho" 2017 / 2019 Mestrado em Física Universidade Estadual Paulista "Júlio de Mesquita Filho" Dedico este trabalho aos meus pais, Roberto e Jurema, aos meus irmãos, Maria Teresa, Daniel, Gabriel e Rafael, a minha sobrinha Giovanna Maria e amigos. AGRADECIMENTOS Em primeiro lugar agradeço a Deus, fonte da vida e da graça. Agradeço pela minha vida, minha inteligência, minha família e meus amigos, ao meu orientador, Prof. Dr. Rafael Sfair que jamais deixou de me incentivar. Sem a sua orientação, dedicação e auxílio, o estudo aqui apresentado seria praticamente impossível. -
How Earth Got Its Moon Article
FEATURE How Earth Got its MOON Standard formation tale may need a rewrite By Thomas Sumner he moon’s origin story does not add up. Most “Multiple impacts just make more sense,” says planetary scientists think that the moon formed in the earli- scientist Raluca Rufu of the Weizmann Institute of Science in est days of the solar system, around 4.5 billion years Rehovot, Israel. “You don’t need this one special impactor to Tago, when a Mars-sized protoplanet called Theia form the moon.” whacked into the young Earth. The collision sent But Theia shouldn’t be left on the cutting room floor just debris from both worlds hurling into orbit, where the rubble yet. Earth and Theia were built largely from the same kind of eventually mingled and combined to form the moon. material, new research suggests, and so had similar composi- If that happened, scientists expect that Theia’s contribution tions. There is no sign of “other” material on the moon, this would give the moon a different composition from Earth’s. perspective holds, because nothing about Theia was different. Yet studies of lunar rocks show that Earth and its moon are “I’m absolutely on the fence between these two opposing compositionally identical. That fact throws a wrench into the ideas,” says UCLA cosmochemist Edward Young. Determining planet-on-planet impact narrative. which story is correct is going to take more research. But the Researchers have been exploring other scenarios. Maybe answer will offer profound insights into the evolution of the the Theia impact never happened (there’s no direct evidence early solar system, Young says. -
What Is the Color of Pluto? - Universe Today
What is the Color of Pluto? - Universe Today space and astronomy news Universe Today Home Members Guide to Space Carnival Photos Videos Forum Contact Privacy Login NASA’s New Horizons spacecraft captured this high-resolution enhanced color view of http://www.universetoday.com/13866/color-of-pluto/[29-Mar-17 13:18:37] What is the Color of Pluto? - Universe Today Pluto on July 14, 2015. Credit: NASA/JHUAPL/SwRI WHAT IS THE COLOR OF PLUTO? Article Updated: 28 Mar , 2017 by Matt Williams When Pluto was first discovered by Clybe Tombaugh in 1930, astronomers believed that they had found the ninth and outermost planet of the Solar System. In the decades that followed, what little we were able to learn about this distant world was the product of surveys conducted using Earth-based telescopes. Throughout this period, astronomers believed that Pluto was a dirty brown color. In recent years, thanks to improved observations and the New Horizons mission, we have finally managed to obtain a clear picture of what Pluto looks like. In addition to information about its surface features, composition and tenuous atmosphere, much has been learned about Pluto’s appearance. Because of this, we now know that the one-time “ninth planet” of the Solar System is rich and varied in color. Composition: With a mean density of 1.87 g/cm3, Pluto’s composition is differentiated between an icy mantle and a rocky core. The surface is composed of more than 98% nitrogen ice, with traces of methane and carbon monoxide. Scientists also suspect that Pluto’s internal structure is differentiated, with the rocky material having settled into a dense core surrounded by a mantle of water ice. -
The Solar System Cause Impact Craters
ASTRONOMY 161 Introduction to Solar System Astronomy Class 12 Solar System Survey Monday, February 5 Key Concepts (1) The terrestrial planets are made primarily of rock and metal. (2) The Jovian planets are made primarily of hydrogen and helium. (3) Moons (a.k.a. satellites) orbit the planets; some moons are large. (4) Asteroids, meteoroids, comets, and Kuiper Belt objects orbit the Sun. (5) Collision between objects in the Solar System cause impact craters. Family portrait of the Solar System: Mercury, Venus, Earth, Mars, Jupiter, Saturn, Uranus, Neptune, (Eris, Ceres, Pluto): My Very Excellent Mother Just Served Us Nine (Extra Cheese Pizzas). The Solar System: List of Ingredients Ingredient Percent of total mass Sun 99.8% Jupiter 0.1% other planets 0.05% everything else 0.05% The Sun dominates the Solar System Jupiter dominates the planets Object Mass Object Mass 1) Sun 330,000 2) Jupiter 320 10) Ganymede 0.025 3) Saturn 95 11) Titan 0.023 4) Neptune 17 12) Callisto 0.018 5) Uranus 15 13) Io 0.015 6) Earth 1.0 14) Moon 0.012 7) Venus 0.82 15) Europa 0.008 8) Mars 0.11 16) Triton 0.004 9) Mercury 0.055 17) Pluto 0.002 A few words about the Sun. The Sun is a large sphere of gas (mostly H, He – hydrogen and helium). The Sun shines because it is hot (T = 5,800 K). The Sun remains hot because it is powered by fusion of hydrogen to helium (H-bomb). (1) The terrestrial planets are made primarily of rock and metal. -
Pluto and Charon
National Aeronautics and Space Administration 0 300,000,000 900,000,000 1,500,000,000 2,100,000,000 2,700,000,000 3,300,000,000 3,900,000,000 4,500,000,000 5,100,000,000 5,700,000,000 kilometers Pluto and Charon www.nasa.gov Pluto is classified as a dwarf planet and is also a member of a Charon’s orbit around Pluto takes 6.4 Earth days, and one Pluto SIGNIFICANT DATES group of objects that orbit in a disc-like zone beyond the orbit of rotation (a Pluto day) takes 6.4 Earth days. Charon neither rises 1930 — Clyde Tombaugh discovers Pluto. Neptune called the Kuiper Belt. This distant realm is populated nor sets but “hovers” over the same spot on Pluto’s surface, 1977–1999 — Pluto’s lopsided orbit brings it slightly closer to with thousands of miniature icy worlds, which formed early in the and the same side of Charon always faces Pluto — this is called the Sun than Neptune. It will be at least 230 years before Pluto history of the solar system. These icy, rocky bodies are called tidal locking. Compared with most of the planets and moons, the moves inward of Neptune’s orbit for 20 years. Kuiper Belt objects or transneptunian objects. Pluto–Charon system is tipped on its side, like Uranus. Pluto’s 1978 — American astronomers James Christy and Robert Har- rotation is retrograde: it rotates “backwards,” from east to west Pluto’s 248-year-long elliptical orbit can take it as far as 49.3 as- rington discover Pluto’s unusually large moon, Charon. -
Precision Astrometry for Fundamental Physics – Gaia
Gravitation astrometric tests in the external Solar System: the QVADIS collaboration goals M. Gai, A. Vecchiato Istituto Nazionale di Astrofisica [INAF] Osservatorio Astrofisico di Torino [OATo] WAG 2015 M. Gai - INAF-OATo - QVADIS 1 High precision astrometry as a tool for Fundamental Physics Micro-arcsec astrometry: Current precision goals of astrometric infrastructures: a few 10 µas, down to a few µas 1 arcsec (1) 5 µrad 1 micro-arcsec (1 µas) 5 prad Reference cases: • Gaia – space – visible range • VLTI – ground – near infrared range • VLBI – ground – radio range WAG 2015 M. Gai - INAF-OATo - QVADIS 2 ESA mission – launched Dec. 19th, 2013 Expected precision on individual bright stars: 1030 µas WAG 2015 M. Gai - INAF-OATo - QVADIS 3 Spacetime curvature around massive objects 1.5 G: Newton’s 1".74 at Solar limb 8.4 rad gravitational constant GM 1 cos d: distance Sun- 1 1 observer c2d 1 cos M: solar mass 0.5 c: speed of light Deflection [arcsec] angle : angular distance of the source to the Sun 0 0 1 2 3 4 5 6 Distance from Sun centre [degs] Light deflection Apparent variation of star position, related to the gravitational field of the Sun ASTROMETRY WAG 2015 M. Gai - INAF-OATo - QVADIS 4 Precision astrometry for Fundamental Physics – Gaia WAG 2015 M. Gai - INAF-OATo - QVADIS 5 Precision astrometry for Fundamental Physics – AGP Talk A = Apparent star position measurement AGP: G = Testing gravitation in the solar system Astrometric 1) Light deflection close to the Sun Gravitation 2) High precision dynamics in Solar System Probe P = Medium size space mission - ESA M4 (2014) Design driver: light bending around the Sun @ μas fraction WAG 2015 M. -
Solar System Planet and Dwarf Planet Fact Sheet
Solar System Planet and Dwarf Planet Fact Sheet The planets and dwarf planets are listed in their order from the Sun. Mercury The smallest planet in the Solar System. The closest planet to the Sun. Revolves the fastest around the Sun. It is 1,000 degrees Fahrenheit hotter on its daytime side than on its night time side. Venus The hottest planet. Average temperature: 864 F. Hotter than your oven at home. It is covered in clouds of sulfuric acid. It rains sulfuric acid on Venus which comes down as virga and does not reach the surface of the planet. Its atmosphere is mostly carbon dioxide (CO2). It has thousands of volcanoes. Most are dormant. But some might be active. Scientists are not sure. It rotates around its axis slower than it revolves around the Sun. That means that its day is longer than its year! This rotation is the slowest in the Solar System. Earth Lots of water! Mountains! Active volcanoes! Hurricanes! Earthquakes! Life! Us! Mars It is sometimes called the "red planet" because it is covered in iron oxide -- a substance that is the same as rust on our planet. It has the highest volcano -- Olympus Mons -- in the Solar System. It is not an active volcano. It has a canyon -- Valles Marineris -- that is as wide as the United States. It once had rivers, lakes and oceans of water. Scientists are trying to find out what happened to all this water and if there ever was (or still is!) life on Mars. It sometimes has dust storms that cover the entire planet. -
The Trans-Neptunian Haumea
Astronomy & Astrophysics manuscript no. main c ESO 2018 October 22, 2018 High-contrast observations of 136108 Haumea? A crystalline water-ice multiple system C. Dumas1, B. Carry2;3, D. Hestroffer4, and F. Merlin2;5 1 European Southern Observatory. Alonso de Cordova´ 3107, Vitacura, Casilla 19001, Santiago de Chile, Chile e-mail: [email protected] 2 LESIA, Observatoire de Paris, CNRS. 5 place Jules Janssen, 92195 Meudon CEDEX, France e-mail: [email protected] 3 European Space Astronomy Centre, ESA. P.O. Box 78, 28691 Villanueva de la Canada,˜ Madrid, Spain 4 IMCCE, Observatoire de Paris, CNRS. 77, Av. Denfert-Rochereau, 75014 Paris, France e-mail: [email protected] 5 Universit Paris 7 Denis Diderot. 4 rue Elsa Morante, 75013 Paris, France e-mail: [email protected] Received 2010 May 18 / Accepted 2011 January 6 ABSTRACT Context. The trans-neptunian region of the Solar System is populated by a large variety of icy bodies showing great diversity in orbital behavior, size, surface color and composition. One can also note the presence of dynamical families and binary systems. One surprising feature detected in the spectra of some of the largest Trans-Neptunians is the presence of crystalline water-ice. This is the case for the large TNO (136 108) Haumea (2003 EL61). Aims. We seek to constrain the state of the water ice of Haumea and its satellites, and investigate possible energy sources to maintain the water ice in its crystalline form. Methods. Spectro-imaging observations in the near infrared have been performed with the integral field spectrograph SINFONI mounted on UT4 at the ESO Very Large Telescope. -
Stellium Handbook Part
2 Donna Cunningham’s Books on the Outer Planets If you’re dealing with a stellium that contains one or more outer planets, these ebooks will help you understand their role in your chart and explore ways to change difficult patterns they represent. Since The Stellium Handbook can’t cover them in the depth they deserve, you’ll gain a greater perspective through these ebooks that devote entire chapters to the meanings of Uranus, Neptune, or Pluto in a variety of contexts. The Outer Planets and Inner Life volumes are $15 each if purchased separately, or $35 for all three—a $10 savings. To order, go to PayPal.com and tell them which books you want, Donna’s email address ([email protected]), and the amount. The ebooks arrive on separate emails. If you want them sent to an email address other than the one you used, let her know. The Outer Planets and Inner Life, V.1: The Outer Planets as Career Indicators. If your stellium has outer planets in the career houses (2nd, 6th, or 10th), or if it relates to your chosen career, this book can give you helpful insights. There’s an otherworldly element when the outer planets are career markers, a sense of serving a greater purpose in human history. Each chapter of this e-book explores one of these planets in depth. See an excerpt here. The Outer Planets and Inner Life, v.2: Outer Planet Aspects to Venus and Mars. Learn about the love lives of people who have the outer planets woven in with the primary relationship planets, Venus and Mars, or in the relationship houses—the 7th, 8th, and 5th. -
Taxonomy of Trans-Neptunian Objects and Centaurs As Seen from Spectroscopy? F
A&A 604, A86 (2017) Astronomy DOI: 10.1051/0004-6361/201730933 & c ESO 2017 Astrophysics Taxonomy of trans-Neptunian objects and Centaurs as seen from spectroscopy? F. Merlin1, T. Hromakina2, D. Perna1, M. J. Hong1, and A. Alvarez-Candal3 1 LESIA – Observatoire de Paris, PSL Research University, CNRS, Sorbonne Universités, UPMC Univ. Paris 06, Univ. Paris Diderot, Sorbonne Paris Cité, 5 place Jules Janssen, 92195 Meudon, France e-mail: [email protected] 2 Institute of Astronomy, Kharkiv V. N. Karin National University, Sumska Str. 35, 61022 Kharkiv, Ukraine 3 Observatorio Nacional, R. Gal. Jose Cristino 77, 20921-400 Rio de Janeiro, Brazil Received 4 April 2017 / Accepted 19 May 2017 ABSTRACT Context. Taxonomy of trans-Neptunian objects (TNOs) and Centaurs has been made in previous works using broadband filters in the visible and near infrared ranges. This initial investigation led to the establishment of four groups with the aim to provide the mean colors of the different classes with possible links with any physical or chemical properties. However, this taxonomy was only made with the Johnson-Cousins filter system and the ESO J, H, Ks filters combination, and any association with other filter system is not yet available. Aims. We aim to edit complete visible to near infrared taxonomy and extend this work to any possible filters system. To do this, we generate mean spectra for each individual group, from a data set of 43 spectra. This work also presents new spectra of the TNO (38628) Huya, on which aqueous alteration has been suspected, and the Centaur 2007 VH305. -
Atmospheres and Surfaces of Small Bodies and Dwarf Planets in the Kuiper Belt
EPJ Web of Conferences 9, 267–276 (2010) DOI: 10.1051/epjconf/201009021 c Owned by the authors, published by EDP Sciences, 2010 Atmospheres and surfaces of small bodies and dwarf planets in the Kuiper Belt E.L. Schallera Lunar and Planetary Laboratory, University of Arizona, Tucson, AZ 85721, USA Abstract. Kuiper Belt Objects (KBOs) are icy relics orbiting the sun beyond Neptune left over from the planetary accretion disk. These bodies act as unique tracers of the chemical, thermal, and dynamical history of our solar system. Over 1000 Kuiper Belt Objects (KBOs) and centaurs (objects with perihelia between the giant planets) have been discovered over the past two decades. While the vast majority of these objects are small (< 500 km in diameter), there are now many objects known that are massive enough to attain hydrostatic equilibrium (and are therefore considered dwarf planets) including Pluto, Eris, MakeMake, and Haumea. The discoveries of these large objects, along with the advent of large (> 6-meter) telescopes, have allowed for the first detailed studies of their surfaces and atmospheres. Visible and near-infrared spectroscopy of KBOs and centaurs has revealed a great diversity of surface compositions. Only the largest and coldest objects are capable of retaining volatile ices and atmospheres. Knowledge of the dynamics, physical properties, and collisional history of objects in the Kuiper belt is important for understanding solar system formation and evolution. 1 Introduction The existence of a belt of debris beyond Neptune left over from planetary accretion was proposed by Kuiper in 1951 [1]. Though Pluto was discovered in 1930, it took over sixty years for other Kuiper belt objects (KBOs) to be detected [2] and for Pluto to be recognized as the first known member of a larger population now known to consist of over 1000 objects (Fig.