Kepler's Laws
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Modern Astronomical Optics - Observing Exoplanets 2
Modern Astronomical Optics - Observing Exoplanets 2. Brief Introduction to Exoplanets Olivier Guyon - [email protected] – Jim Burge, Phil Hinz WEBSITE: www.naoj.org/staff/guyon → Astronomical Optics Course » → Observing Exoplanets (2012) Definitions – types of exoplanets Planet (& exoplanet) definitions are recent, as, prior to discoveries of exoplanets around other stars and dwarf planets in our solar system, there was no need to discuss lower and upper limits of planet masses. Asteroid < dwarf planet < planet < brown dwarf < star Upper limit defined by its mass: < 13 Jupiter mass 1 Jupiter mass = 317 Earth mass = 1/1000 Sun mass Mass limit corresponds to deuterium limit: a planet is not sufficiently massive to start nuclear fusion reactions, of which deuterium burning is the easiest (lowest temperature) Lower limit recently defined (now excludes Pluto) for our solar system: has cleared the neighbourhood around its orbit Distinction between giant planets (massive, large, mostly gas) and rocky planets also applies to exoplanets Habitable planet: planet on which life as we know it (bacteria, planets or animals) could be sustained = rocky + surface temperature suitable for liquid water Formation Planet and stars form (nearly) together, within first few x10 Myr of system formation Gravitational collapse of gas + dust cloud Star is formed at center of disk Planets form in the protoplanetary disk Planet embrios form first Adaptive Optics image of Beta Pic Large embrios (> few Earth mass) can Shows planet + debris disk accrete large quantity of -
Measuring Gravity
Physics Measuring Gravity Sir Isaac Newton told us how important gravity is, but left some gaps in the story. Today scientists are measuring the gravitational forces on individual atoms in an effort to plug those gaps. This is a print version of an interactive online lesson. To sign up for the real thing or for curriculum details about the lesson go to www.cosmoslessons.com Introduction: Measuring Gravity Over 300 years ago the famous English physicist, Sir Isaac Newton, had the incredible insight that gravity, which we’re so familiar with on Earth, is the same force that holds the solar system together. Suddenly the orbits of the planets made sense, but a mystery still remained. To calculate the gravitational attraction between two objects Newton needed to know the overall strength of gravity. This is set by the universal gravitational constant “G” – commonly known as “big G” – and Newton wasn't able to calculate it. Part of the problem is that gravity is very weak – compare the electric force, which is 1040 times stronger. That’s a bigger di혯erence than between the size of an atom and the whole universe! Newton's work began a story to discover the value of G that continues to the present day. For around a century little progress was made. Then British scientist Henry Cavendish got a measurement from an experiment using 160 kg lead balls. It was astoundingly accurate. Since then scientists have continued in their attempts to measure G. Even today, despite all of our technological advances (we live in an age where we can manipulate individual electrons and measure things that take trillionths of a second), di혯erent experiments produce signicantly di혯erent results. -
Cavendish Weighs the Earth, 1797
CAVENDISH WEIGHS THE EARTH Newton's law of gravitation tells us that any two bodies attract each other{not just the Earth and an apple, or the Earth and the Moon, but also two apples! We don't feel the attraction between two apples if we hold one in each hand, as we do the attraction of two magnets, but according to Newton's law, the two apples should attract each other. If that is really true, it might perhaps be possible to directly observe the force of attraction between two objects in a laboratory. The \great moment" when that was done came on August 5, 1797, in a garden shed in suburban London. The experimenter was Lord Henry Cavendish. Cavendish had inherited a fortune, and was therefore free to follow his inclinations, which turned out to be scientific. In addition to the famous experiment described here, he was also the discoverer of “inflammable air", now known as hydrogen. In those days, science in England was often pursued by private citizens of means, who communicated through the Royal Society. Although Cavendish studied at Cambridge for three years, the universities were not yet centers of scientific research. Let us turn now to a calculation. How much should the force of gravity between two apples actually amount to? Since the attraction between two objects is proportional to the product of their masses, the attraction between the apples should be the weight of an apple times the ratio of the mass of an apple to the mass of the Earth. The weight of an apple is, according to Newton, the force of attraction between the apple and the Earth: GMm W = R2 where G is the \gravitational constant", M the mass of the Earth, m the mass of an apple, and R the radius of the Earth. -
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. -
Gravity and Coulomb's
Gravity operates by the inverse square law (source Hyperphysics) A main objective in this lesson is that you understand the basic notion of “inverse square” relationships. There are a small number (perhaps less than 25) general paradigms of nature that if you make them part of your basic view of nature they will help you greatly in your understanding of how nature operates. Gravity is the weakest of the four fundamental forces, yet it is the dominant force in the universe for shaping the large-scale structure of galaxies, stars, etc. The gravitational force between two masses m1 and m2 is given by the relationship: This is often called the "universal law of gravitation" and G the universal gravitation constant. It is an example of an inverse square law force. The force is always attractive and acts along the line joining the centers of mass of the two masses. The forces on the two masses are equal in size but opposite in direction, obeying Newton's third law. You should notice that the universal gravitational constant is REALLY small so gravity is considered a very weak force. The gravity force has the same form as Coulomb's law for the forces between electric charges, i.e., it is an inverse square law force which depends upon the product of the two interacting sources. This led Einstein to start with the electromagnetic force and gravity as the first attempt to demonstrate the unification of the fundamental forces. It turns out that this was the wrong place to start, and that gravity will be the last of the forces to unify with the other three forces. -
Probing Gravity at Short Distances Using Time Lens
Probing Short Distance Gravity using Temporal Lensing Mir Faizal1;2;3, Hrishikesh Patel4 1Department of Physics and Astronomy, University of Lethbridge, Lethbridge, AB T1K 3M4, Canada 2Irving K. Barber School of Arts and Sciences, University of British Columbia Okanagan Campus, Kelowna, V1V1V7, Canada 3Canadian Quantum Research Center, 204-3002, 32 Ave, Vernon, BC, V1T 2L7, Canada 4Department of Physics and Astronomy, University of British Columbia, 6224 Agricultural Road, Vancouver, V6T 1Z1, Canada Abstract It is known that probing gravity in the submillimeter-micrometer range is difficult due to the relative weakness of the gravitational force. We intend to overcome this challenge by using extreme temporal precision to monitor transient events in a gravitational field. We propose a compressed ultrafast photography system called T-CUP to serve this purpose. We show that the T-CUP's precision of 10 trillion frames per second can allow us to better resolve gravity at short distances. We also show the feasibility of the setup in measuring Yukawa and power-law corrections to gravity which have substantial theoretical motivation. 1 Introduction General Relativity (GR) has been tested at large distances, and it has been arXiv:2003.02924v2 [gr-qc] 29 Jun 2021 realized that we need a more comprehensive model of gravity that aligns with our measurements of gravity at long distances and short distances. Several ad- vances have been made in trying to understand gravity at long distances since the advent of multi-messenger astronomy [1, 2]. However, it is possible to relate the large distance corrections to the short distance corrections. In fact, several theories like MOND [3, 4] have been proposed to explain the large distance corrections to gravitational dynamics due to small accelerations. -
Oil, Earth Mass and Gravitational Force
A peer reviewed version is published at: https://doi.org/10.1016/j.scitotenv.2016.01.127 Oil, Earth mass and gravitational force Khaled Moustafa Editor of the Arabic Science Archive (ArabiXiv) E-mail: [email protected] Highlights Large amounts of fossil fuels are extracted annually worldwide. Would the extracted amounts represent any significant percentage of the Earth mass? What would be the consequence on Earth structure and its gravitational force? Modeling the potential loss of Earth mass might be required. Efforts for alternative renewable energy sources should be enhanced. Abstract Fossil fuels are intensively extracted from around the world faster than they are renewed. Regardless of direct and indirect effects of such extractions on climate change and biosphere, another issue relating to Earth’s internal structure and Earth mass should receive at least some interest. According to the Energy Information Administration (EIA), about 34 billion barrels of oil (~4.7 billion metric tons) and 9 billion tons of coal have been extracted in 2014 worldwide. Converting the amounts of oil and coal extracted over the last 3 decades and their respective reserves, intended to be extracted in the future, into mass values suggests that about 355 billion tons, or ~ 5.86*10−9 (~ 0.0000000058) % of the Earth mass, would be ‘lost’. Although this is a tiny percentage, modeling the potential loss of Earth mass may help figuring out a critical threshold of mass loss that should not be exceeded. Here, I briefly discuss whether such loss would have any potential consequences on the Earth’s internal structure and on its gravitational force based on the Newton's law of gravitation that links the attraction force between planets to their respective masses and the distances that separate them. -
Universal Gravitational Constant EX-9908 Page 1 of 13
Universal Gravitational Constant EX-9908 Page 1 of 13 Universal Gravitational Constant EQUIPMENT 1 Gravitational Torsion Balance AP-8215 1 X-Y Adjustable Diode Laser OS-8526A 1 45 cm Steel Rod ME-8736 1 Large Table Clamp ME-9472 1 Meter Stick SE-7333 INTRODUCTION The Gravitational Torsion Balance reprises one of the great experiments in the history of physics—the measurement of the gravitational constant, as performed by Henry Cavendish in 1798. The Gravitational Torsion Balance consists of two 38.3 gram masses suspended from a highly sensitive torsion ribbon and two1.5 kilogram masses that can be positioned as required. The Gravitational Torsion Balance is oriented so the force of gravity between the small balls and the earth is negated (the pendulum is nearly perfectly aligned vertically and horizontally). The large masses are brought near the smaller masses, and the gravitational force between the large and small masses is measured by observing the twist of the torsion ribbon. An optical lever, produced by a laser light source and a mirror affixed to the torsion pendulum, is used to accurately measure the small twist of the ribbon. THEORY The gravitational attraction of all objects toward the Earth is obvious. The gravitational attraction of every object to every other object, however, is anything but obvious. Despite the lack of direct evidence for any such attraction between everyday objects, Isaac Newton was able to deduce his law of universal gravitation. Newton’s law of universal gravitation: m m F G 1 2 r 2 where m1 and m2 are the masses of the objects, r is the distance between them, and G = 6.67 x 10-11 Nm2/kg2 However, in Newton's time, every measurable example of this gravitational force included the Earth as one of the masses. -
Physics 100: Homework 5 Solutions 1) Somewhere Between the Earth
Physics 100: Homework 5 Solutions 1) Somewhere between the Earth and the moon, the gravitational force on a space shuttle would cancel. Is this location closer to the moon or to the Earth? Explain your answer. The gravitational force on the shuttle due to the moon is proportional to the shuttle’s mass, the moon’s mass, and inversely proportional to the square of the shuttle-moon distance. That due to the Earth is proportional to the shuttle’s mass, the Earth’s mass, and inversely proportional to the square of the shuttle-Earth distance. Since Earth mass >> moon mass, the shuttle must be much closer to the moon in order for the two attractions to cancel. 2) Which is greater, the gravitational pull of the moon on the Earth or that of the sun on the Earth? Which has a greater effect on our ocean tides, the sun or the moon? Explain your answers. The gravitational pull of the Sun on the Earth is greater than the gravitational pull of the Moon, about 180 times as large due its much greater mass, as explained in class. The tides, however, are caused by the differences in gravitational forces by the Moon on opposite sides of the Earth. The difference in gravitational forces by the Moon on opposite sides of the Earth is greater than the corresponding 2 difference in forces by the stronger pulling but much more distant Sun. The difference, 1/(d+Dearth) – 2 1/d , where Dearth is the diameter of Earth, is greater for the moon (smaller d) than it is for the sun (larger d), which is the math-way of saying what we said in class about the inverse-law flattening out… 3 a) A particular atom contains 47 electrons, 61 neutrons, and 47 protons. -
Observing the Gravitational Constant G Underneath Two Pump Storage Reservoirs Near Vianden (Luxembourg)
Universität Stuttgart Geodätisches Institut Observing the gravitational constant G underneath two pump storage reservoirs near Vianden (Luxembourg) Function fit 1012 10 5 Function value 0 0 5 510 505 10 500 Water temperature 15 495 Water level Bachelorarbeit im Studiengang Geodäsie und Geoinformatik an der Universität Stuttgart Tobias Schröder Stuttgart, September 2017 Betreuer: Prof. Dr.-Ing. Nico Sneeuw Universität Stuttgart Prof. Dr. Olivier Francis Université du Luxembourg Erklärung der Urheberschaft Ich erkläre hiermit an Eides statt, dass ich die vorliegende Arbeit ohne Hilfe Dritter und ohne Benutzung anderer als der angegebenen Hilfsmittel angefertigt habe; die aus fremden Quellen direkt oder indirekt übernommenen Gedanken sind als solche kenntlich gemacht. Die Arbeit wurde bisher in gleicher oder ähnlicher Form in keiner anderen Prüfungsbehörde vorgelegt und auch noch nicht veröffentlicht. Stuttgart, 30. September 2017 Unterschrift III Abstract The aim of this thesis is to extract the gravitational constant G from relative gravity measure- ments underneath two artificial reservoirs in Vianden (Luxembourg). If one wants to deter- mine the Newtonian constant G from measurements many variables play a role, like water level, density and temperature. All of them are measured, while the gravimeter is measuring the gravitational attraction. To extract the gravitational constant G it is important to know the gravitational attraction of each point inside the reservoir. For this calculation the 3D models of the lakes are filled with tiny cubes, from which the exact integral to calculate their gravitational attraction to the gravimeter is known. Calculated values are compared to the measured ones which makes it possible to extract the searched gravitational constant G. -
The Cavendish Experiment
The Cavendish Experiment 1 Introduction In 1687 Newton published the Principia in which he presented a mathematical de- scription of the gravitational force. In Newton’s theory of gravitation the gravitational attraction, F , exerted by one object on another is expressed according to the relation- ship m m F = G l s : (1.1) R2 The quantities ml and ms are the masses of two objects whose spatial separation is R. The value of the constant of proportionality, G, was not known to Newton and, in fact, was not accurately determined until the latter half of the nineteenth century. The calculation of its value was based on the results of an experiment to determine the density of the earth performed by Henry Cavendish, and published in 1798.1 The purpose of this experiment is to perform a modern version of the Cavendish experiment, determine the gravitational constant, G, and compare it to its accepted value. 2 Theory The primary apparatus used to perform this experiment is the torsion balance which is shown in Figure 1. The torsion balance is depicted in Figure 2 with relevant compo- nents labeled for illustrative purposes. Initially, the internal boom is at rest. Then the two large masses are put in place and attract the two smaller masses causing a torque to be exerted on the internal boom so that the it rotates from its initial point of equilib- rium. As the boom rotates, the thin wire which is fixed at the top twists until the wire exerts a counter torque on the boom. If the rotational kinetic energy is dissipated, the boom will come to rest at a new point of equilibrium so that the following relationship for the the torques is satisfied: 2F d = kθD : (2.1) The term on the right of the equality is the counter torque resulting from the wire. -
Gravity on Earth
National Grade Level Science 9-12 Foundation GRAVITY ON EARTH Did you know that your weight is different This slice of the Earth’s surface shows a mountain, an ocean, and the depending on where you are on the surface atmosphere. Section A is two thirds rock and one third air while Section of the Earth? While the Earth has an average B is one quarter rock, one quarter water, and one half air. The sections gravitational force, different locations on are the same size but Section A has more mass in the space so it has a Earth have gravitational forces that are larger stronger gravitational pull. or smaller than average. This is because each location has more or less mass than the average. Density of: A B Gravity is a physical force of attraction between Air objects. Objects with a small mass have a weak gravitational force while those with a large mass have a strong force. Water You are held down to the Earth’s surface because it has a strong gravitational force. You Rock actually exert a gravitational force on the Earth, but because your mass is many times smaller than the Earth’s mass, your pull is much less than the Earth’s. These differences in gravity are tiny so scientists have to use very sensitive satellites to measure differences around the world. These satellites can Gravity is measured as how fast objects even detect dense features deep within the earth that increase the accelerate towards each other. The average gravitational pull at the surface.