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Pick rd 3 hour stuff! It will first appear in the center of the room before lecture. It will then be moved to the box labeled “3100” outside the planetarium • All 3rd hours will collect there until the end of the semester Scores posted just outside the planetarium (listed by 4-digit ID number) Homework now due at 11:59pm Friday! Extra Credit: see page 41 (25 pts max, 10 must be done before midterm) © Sierra College Astronomy Department 1 25 pts of Extra Credit can be done, 10 pts of these points must be done before midterm (see page 41 of Student Handbook) The Class Web Site: astronomy.sierracollege.edu Mastering Astronomy: masteringastronomy.sierracollege.edu Lecture 4: Newton Motion in a Circle Motion of an object in a circle at constant speed (uniform circular motion) is an example board of acceleration by changing direction. Centripetal (“center-seeking”) force is the force directed toward the center of the curve Circ along which the object is moving. motion What happens if the centripetal force is removed? Demo © Sierra College Astronomy Department 3 Lecture 4: Newton The Law of Universal Gravitation This law states that between every two objects there is an attractive force, the magnitude of which is directly proportional to the mass of each object Grav and inversely proportional to the square of Law the distance between the centers of the objects (inverse square law). In equation form: F = GM1M2 / d 2 Another where G is a constant, M and m are the form masses, and r is the distance between their centers. F = GMm / r 2 © Sierra College Astronomy Department Grav Law2 4 Weight of an object away from Earth 1/16 Grav Law 1/4 1/9 © Sierra College Astronomy Department 5 Lecture 4: Newton The Law of Universal Gravitation According to Newton, gravity not only makes objects fall to Earth but keeps the Moon in orbit around the Earth and keeps the planets in orbit around the Sun. He could therefore explain the planets’ motions and why Kepler’s laws worked. © Sierra College Astronomy Department Cannon Grav Law 6 Lecture 4: Newton The Law of Universal Gravitation Grav Law Testing the Law of Universal Gravitation Because the distance from the center of the Earth to the Moon is about 60 times the distance from the center of the Earth to its surface, the centripetal acceleration of the Moon should be (1/60²) or 1/3600 of the acceleration of gravity on Earth. Newton’s calculations showed this to be the case and confirmed the validity of his theory of gravitation. © Sierra College Astronomy Department 7 Lecture 4: Newton Conservation Laws Demo • Under certain conditions, certain physical quantities will not change in time • These unchanging quantities are said to be conserved • Three important conservation laws for astronomy – (linear) momentum – angular momentum – energy © Sierra College Astronomy Department 8 Lecture 4: Newton Conservation Laws Demo Momentum (Along a Line) and Conservation • The momentum of an object with mass m and velocity v is given as p = mv • The momentum of a system of objects is P = p1 + p2 + … = m1v1 + m2v2 + … • If the absence of external forces acting on the system, P remains constant for all time - this is the Conservation of Momentum • Examples: Rockets and billiard balls • For more than one direction, conservation of momentum is applied in each direction separately © Sierra College Astronomy Department Pool 9 Lecture 4: Newton Demo Conservation of Angular Momentum • Angular Momentum and Conservation – Spinning objects and objects in orbit are said to possess angular momentum – In the absence of a “twisting force” or torque, a spinning object will maintain its angular momentum - this is the Conservation of Angular Momentum – Orbital angular momentum • The orbital angular momentum, J, of an object is the product of that object’s mass m, speed of rotation v, and distance from the center of rotation r: Skater J = mvr • The conservation of J means that (in the absence of an outside torque) as the distance to the spin axis decreases (contraction), the speed increases • This is what Kepler really observed as his 2nd Law of Planetary Motions (the Law of Equal Areas) Orbit © Sierra College Astronomy Department 10 Lecture 4: Understanding Motion, Energy, and Gravity Conservation of Angular Momentum • Angular Momentum and Conservation (continued) – Rotational angular momentum • An object (like the Earth) will continue to spin at the same rate as long as there is no net torque on it – Precession is the result of an external torque (observed for the Earth) • In a system of objects, the total angular momentum can be conserved (no outside torque), but the objects may transfer rotational angular energy between themselves – The slowing of the Earth’s day is due to the transfer of rotational angular momentum of the Earth to orbital angular momentum of the Moon © Sierra College Astronomy Department 11 Lecture 4: Newton Energy is conserved too! • Types of energy: Demo – Kinetic: the energy of moving objects (½ mv2) • Ex: cars in motion, planets going around the sun, molecules jostling in the air • Thermal energy is a important subcategory (next slide) Energy cycle – Radiative: energy carried by light (photons) – Potential: stored energy which may be converted later into kinetic or radiative energy • Ex: A rock perched on a ledge, chemical (or nuclear) bonds in an atom (or nucleus) (more later). • MKS unit for energy: Joule – 4,184 joules are in one food Calorie – Typical adult eats 2500 Calories = 10 million joules © Sierra College Astronomy Department 12 Lecture 4: Newton Temperatures Temperature is the measure of the average kinetic energy of a system of particles • Thermal energy depends on temperature and density Higher Fahrenheit scale: freezing 32°F/boiling 212°F. Lower Kinetic Celsius scale: freezing 0°C/boiling 100°C. Kelvin scale: 0 K = absolute zero (-273°C) 273 K = freezing point of water (0 °C) Thermal dependence 373 K = boiling point of water (100 °C) Note that Kelvin and Celsius degrees are the “same size.” © Sierra College Astronomy Department Temperature scales 13 Lecture 4: Newton Potential Energy in Astronomy Of the many types of potential energy, two are of particular importance in astronomy Gravitational potential energy: How much energy would one get from motions due to gravity? This energy get converted in kinetic energy. Mass-energy: How much energy is stored in the atom or nucleus? E mc © Sierra College Astronomy Department 2 14 Lecture 4: Newton Conservation of Energy Conservation of Energy states that in an isolated system, although energy may change from one form to another, the total amount of energy must remain constant Energy cannot be created nor destroyed, but can be transferred between different types • Ex: As a ball is dropped, its potential energy gets converted to kinetic energy such that the sum of the kinetic and potential energies remains constant The ultimate source of all the energy in the Universe is the Big Bang © Sierra College Astronomy Department 15 Lecture 4: Newton Newton’s Laws and Kepler’s Laws Newton showed mathematically (using calculus) that Kepler’s laws derive from the inverse square law for gravitation and the equation of motion (F = ma). Newton modified Kepler’s third law, showing that the masses are an important factor. 2 p = 3 Ka /(M 1 + M2) where K=4p2/G Objects orbit their center of mass © Sierra College Astronomy Department COM 16 Lecture 4: Newton Examples of Newton’s Laws Orbits: Circular and Escape Speed • Just how much speed does take to orbit the Earth? To leave the Earth? See Mathematical Insight 4.4 GM Vc R 2GM Ve R • Notice that it requires only √2 times the circular velocity to escape from the planet • For the Earth Vc = 8 km/s and Ve = 11 km/s Escape • For comparisons, be careful with M and R © Sierra College Astronomy Department 17 Lecture 4: Newton Examples of Newton’s Laws Feather Hammer Surface Gravity is the gravitational attraction at the surface of a planet or star. It is the acceleration on a mass created by the local gravitational force. GM Acceleration due to gravity at surface (See Mathematical g 2 Insight 4.5): R • Note independence of g with respect to m • For comparisons, be careful with M and R 2 • Notice Weight (W) = mg = GMm/R © Sierra College Astronomy Department 18 Lecture 4: Newton Examples of Newton’s Laws Weightlessness • Weight is the force that counters gravity creating a zero net force • Weightlessness is the absence of the countering force • People in orbit around the Earth feel weightless because gravity is not countered by a surface connected to the Earth Changing Orbits • Objects in orbit around each other do not spontaneously change into other orbital configurations. • The orbital energy of the system must change through: – Gravitational encounters (encounters with a third object) – Atmospheric drag (friction that diverts kinetic energy into other forms) © Sierra College Astronomy Department 19 Lecture 4: Newton The Importance of Newton’s Laws Kepler’s laws can be derived from them. They explain tides and precession. Their use predicted the existence of the planet Neptune. They provide a way to measure things quantitatively and predict the motion of things. Newton laid the foundation for our notion of the Universe. © Sierra College Astronomy Department 20 Lecture 4: Light and the Electromagnetic Spectrum The Wave Nature of Light Spectrum is the order of colors or wavelengths produced when light is dispersed, such as by a prism. Wave Motion in General Wavelength (l) is the distance from a point on a wave to the next corresponding point. Frequency (f or n) is the number of repetitions per unit time There IS a relationship between f and l! Wavel © Sierra College Astronomy Department 21 Lecture 4: Light and the Electromagnetic Spectrum The Wave Nature of Light As a water wave travels along the surface, the wave’s motion in primarily in the vertical direction and not along the direction of the wave. Frequency is given in cycles/second or hertz (Hz). © Sierra College Astronomy Department 22 Lecture 4: Light and the Electromagnetic Spectrum The Wave Nature of Light Light as a Wave wave White light is made up of light of many wavelengths, but all wavelengths travel at photon 300 million meters/second (3.00 X108 m/s). f l = c = speed of light wave 10-9 Nanometer (nm): unit of length = m. Angstrom (Å): unit of length = 10-10 m; it is a non-SI unit. © Sierra College Astronomy Department board 23 Lecture 4: Light and the Electromagnetic Spectrum The Wave Nature of Light 700 nm red light has f = 4.3 X 1014 Hz. 400 nm violet light has f = 7.5 X 1014 Hz. Frequencies range from 102 Hz (low) to 1024 Hz (high). Wavelengths range from 106 m (long) to 10-16 m (short). Based on frequency and/or wavelength, the Electromagnetic (EM) spectrum is usually broken into these regions: radio (AM/FM/microwave), infrared, visible, ultraviolet, X-ray, gamma ray © Sierra College Astronomy Department EM Spec Maxwell 24 © Sierra College Astronomy Department 25 Lecture 4: Light and the Electromagnetic Spectrum The Wave Nature of Light These waves are called “electromagnetic” EM Spec because they consist of combined electric and magnetic waves that result when a charged Windows particle accelerates. Astronomers refer to atomspheric windows in the Earth’s atmosphere that allow certain wavelengths to pass. Electromagnetic Spectrum © Sierra College Astronomy Department 26 Lecture 4: Light and the Electromagnetic Spectrum The Colors of Planets and Stars Color from Reflection - Colors of Planets Planets have their colors because the material on their surfaces or in their clouds absorbs some of the wavelengths of sunlight and reflects a combination of wavelengths that appear, for example, as the rusty red of Mars or the blue of Neptune. © Sierra College Astronomy Department 27 Lecture 4: Light and the Electromagnetic Spectrum The Colors of Planets and Stars Color as a Measure of Temperature An intensity/wavelength graph, a thermal spectrum, of an object emitting electromagnetic radiation can be used to detect its temperature. Therefore, the color of a star tells us about its surface temperature. In Cosmic Calculations 5.1: A quantitative derivation is given by Wien’s Law: Wien’s T = 2,900,000/lmax or lmax= 2,900,000/T where T is the temperature in Kelvin and lm is the wavelength where the thermal spectrum peaks in intensity in nanometers (nm) © Sierra College Astronomy Department EM Spec 28 Lecture 4: Light and the Electromagnetic Spectrum The Colors of Planets and Stars Intensity per square meter How much thermal energy is being emitted (per square meter) from an object with at temperature T ? (see Cosmic Calculations 5.1) Energy per square meter Stefan-Boltzmann constant © Sierra College Astronomy Department T board 4 EM Spec 29 Public Service Anonoucement! Please put your 4-digit ID 3rd hour assignments and anything else you turn in © Sierra College Astronomy Department 30 Lecture 4: Light and the Electromagnetic Spectrum Spectra By using a prism (refraction) or grating (diffraction) one can take the “white” light of a glowing object and spread it out into a spectrum Can be used to study starlight Rainbows are formed from light refracting in water © Sierra College Astronomy Department 700 nm 600 nm 500 nm 400 nm 31 Lecture 4: Light and the Electromagnetic Spectrum Spectra Examined Close Up Continuous spectrum contains an entire range of wavelengths rather than separate, discrete wavelengths. Example of a continuous spectrum is the heated filament of a lamp or a glowing piece of iron in the blacksmith’s forge. © Sierra College Astronomy Department 32 Lecture 4: Light and the Electromagnetic Spectrum Spectra Examined Close Up Kirchhoff’s Laws In 1814 Fraunhofer analyzed the solar spectrum and found a number of dark lines across the continuous spectrum. The dark lines are caused by absorption. Later it was discovered that if gases are heated until they emit light, a spectrum made up of bright lines appears. © Sierra College Astronomy Department Types Of Spectra (basic) 33 Lecture 4: Light and the Electromagnetic Spectrum Spectra Examined Close Up Kirchhoff’s laws summarize how the three types of spectra are produced: Types 1. A hot, dense glowing object (a solid or Of Spectra dense gas) emits a continuous spectrum. (basic) 2. A hot, low-density gas emits light of only Kirchhoff certain wavelengths - a bright line spectrum. 3. When light having a continuous spectrum Demo passes through a cool gas, dark lines appear in the continuous spectrum. © Sierra College Astronomy Department 34 Lecture 4: Light and the Electromagnetic Spectrum The Atom The atom is made of three parts: Atom Structure Proton, electron, neutron The type of atom is determined by the number of protons atoms An isotope of a given atom differs in the number of neutrons # of proton + neutrons = atomic mass number Periodic Table © Sierra College Astronomy Department 36 Lecture 4: Light and the Electromagnetic Spectrum The Bohr Atom Three postulates of the Bohr atom: 1. Electrons in orbit around a nucleus can have only certain specific energies. 2. An electron can move from one energy level to another – changing the energy of the atom. 3. The energy of a photon determines the frequency (or wavelength) of light that is associated with the photon, © Sierra College Astronomy Department Atom Talking Atom Levels Flat Levels 37 Lecture 4: Light and the Electromagnetic Spectrum The Bohr Atom “States” of an electron An electron at it minimum energy level is said to be in its ground state If a photon with just the right amount interacts with the atom, the electron may be raised to a new level, the electron is said to be in an excited state While in an excited state, the electron can “relax” and fall down to a lower energy state releasing a photon © Sierra College Astronomy Department Flat Levels 38 Lecture 4: Light and the Electromagnetic Spectrum The Doppler Effect • Doppler effect is the observed change in wavelength from a source moving toward or away from the observer. • It is most well known as the change in pitch of sound waves when a speeding car or train blowing its horn passes by. • In front of the moving source one hears higher frequency (shorter wavelength) sound. • Behind the source one hears lower frequency (longer wavelength) sound. © Sierra College Astronomy Department EM Spec Doppler 39 Lecture 4: Light and the Electromagnetic Spectrum The Doppler Effect Redshift is the change in wavelength toward longer wavelengths. Blueshift is the change in wavelength toward shorter wavelengths. Except for very distant galaxies, most redshifts or blueshifts caused by the Doppler effect are very small. It is spectral lines in stellar spectra that make the Doppler effect a powerful tool. © Sierra College Astronomy Department Doppler II Doppler In Spectra 40 Lecture 4: Light and the Electromagnetic Spectrum The Doppler Effect In cosmic Calculations 5.2 Doppler Effect as a Measurement Doppler Technique Formula Measuring the amount of the shifting of stellar spectral lines can determine the radial velocity of the star relative to the Earth. Radial velocity is velocity along vt the line of sight, toward or away vrad v from the observer. Tangential velocity is velocity To Earth perpendicular to the line of sight. © Sierra College Astronomy Department 41 Lecture 4: Light and the Electromagnetic Spectrum The Doppler Effect Other Doppler Effect Measurements The rotation rate of the Sun Rotation rates of the planets and the rings of Saturn The motion of some binary stars Doppler The motion of other stars with planets around them Doppler Speeding cars by police radar Formula © Sierra College Astronomy Department 42 Lecture 4: Light and the Electromagnetic Spectrum The Doppler Effect Speed measured by the Doppler effect is the speed of the object relative to the speed of the Earth. All speeds are relative to something. All motion (or non-motion) is relative, too. The understanding of the relativity of motion is called Galilean relativity or Newtonian relativity. © Sierra College Astronomy Department 43 Other Slides © Sierra College Astronomy Department 44 Lecture 4: Light and the Electromagnetic Spectrum The Inverse Square Law Inverse square law of radiation states that radiation spreading from a small Inverse Square source decreases in intensity as the Law inverse square of the distance from the source. Force of gravity also follows an inverse square relationship with distance. © Sierra College Astronomy Department 45 Lecture 3b: Galileo, Newton, and Einstein Beyond Newton to Einstein Newton assumed time was absolute. Einstein’s Special Theory of Relativity showed this was not true. Newton proposed that inertial mass was equivalent to gravitational mass. Subsequent measurements confirmed this coincidence. Einstein in his General Theory of Relativity showed mathematically that the two types of masses are indeed equivalent. © Sierra College Astronomy Department 46 Lecture 3b: Galileo, Newton, and Einstein Beyond Newton to Einstein Principle of equivalence states that the effects of the force of gravity are indistinguishable from those of acceleration. The general theory predicts that light will curve in the presence of a massive object. This prediction, made in 1907, was first confirmed during a solar eclipse in 1919. © Sierra College Astronomy Department D-13 D-14 47 Astronomy Club Meets every Wednesday at 9:30AM in S-202 (Planetarium) Fall 2005