PHYS 3380 - Astronomy Apparent Weight apparent weight

PHYS 3380 - Astronomy Apparent Weight apparent weight

PHYS 3380 - Astronomy Apparent Weight apparent weight - weight force that we actually sense not the downward force of gravity, but the normal (upward) force exerted by the surface we stand on - opposes gravity and prevents us falling to the center of the Earth what is measured by a weighing scale. For a body supported in a stationary position, normal force exactly balances earth's gravitational force - apparent weight has the same magnitude as actual weight. If no contact with any surface to provide such an opposing force - no sensation of weight (no apparent weight). - free-fall - experienced by sky-divers and astronauts in orbit who

feel "weightless" even though their bodies are still subject to the force of gravity - also known as microgravity. A degree of reduction of apparent weight occurs, for example, in elevators. In an elevator, a spring scale will register a decrease in a person's (apparent) weight as the elevator starts to accelerate downwards. This is because the opposing force of the elevator's floor decreases as it accelerates away underneath one's feet. PHYS 3380 - Astronomy Newtons Formulation of Keplers Laws Keplers Laws were based on observation (experimentation). Newtons laws explained Keplers Laws Keplers Second Law

As a planet moves around its orbit, it sweeps out equal areas in equal times - a planet moves slower when it is farther from the Sun and faster when it is closer PHYS 3380 - Astronomy When you swing a ball around, the string exerts a force that pulls the ball inward (gravity for orbiting body). The acceleration is also inward. For a circular orbit: (r = radius of orbit)

The smaller the radius, the greater the speed.The orbital speed is independent of the mass of the orbiting body (m1). As the radius (the distance to the orbiting body) increases, the orbital speed decreases. PHYS 3380 - Astronomy What is the orbital velocity of a satellite near the Earths surface? PHYS 3380 - Astronomy Another Way of Looking at Orbital Velocity Weightlessness - a state of being in free fall towards the Earth. The Earth is round - its surface drops about 5 m for every 8 km of distance. If you were standing at sea level, you would only see the

top of a 5-meter mast on a ship 8000 m away - remember the (false) story of Columbus and the orange. Given h=1/2gt2, if t=1 s then h = 5 m. So if a projectile is fired horizontally at ~8 km/s, it will fall fast enough to keep falling around the Earth - becomes a satellite. So a spacecraft is in free fall around the Earth - free fall is not an absence of gravity. If a satellite is given a velocity greater than 8 km/s, it will overshoot a circular orbit and trace an elliptical path. Cannonball Animation PHYS 3380 - Astronomy Keplers 3rd Law The square of any planet's period of orbital revolution, P, is proportional to

the cube of its mean distance, r, from the sun. From Keplers 2nd Law Speed around orbit: Circumference (2r)/ time P=period, time of 1 orbit PHYS 3380 - Astronomy What is the mass of the Sun? G = 6.67 x 10-11 Nm2/ kg2 r = 1.496 x 1011m - AU P = 3.147 x 107 s So: Msun = 2 x 1030 kg

PHYS 3380 - Astronomy Geosynchronous/Geostationary Orbits A geosynchronous orbit has a period the same as the rotational speed of the Earth - e.g., it orbits in the same amount of time that the Earth rotates - 1 sidereal day. A geostationary orbit is a geosynchronous orbit at the equator it always stays above the same place on the Earth - communications satellites, satellite TV, etc What is the altitude of a geostationary orbit calculated from Newtons formulation of Keplers 3rd Law: G = 6.67 x 10-11 Nm2/ kg2 P = 86,164 s (sidereal day)

MEarth = 5.97 X 1024 kg So: r = 42,164 km above the center of the Earth and the altitude is 35,768 km. PHYS 3380 - Astronomy Another Way of Calculating Geosynchronous Orbit For an orbiting body, the inward and outward forces must equal each other (Newtons 3rd Law) - the centrifugal force from orbital motion has to equal the centripetal force from gravity: is angular velocity - at geosynchronous orbit, of satellite is equal to the angular velocity of the Earth

= 2/86164 (length of sidereal day) M = 5.97 X 1024 kg G= 6.67 x 10-11 Nm2/ kg2 Plug in the numbers a you get r = 42,164 km - same as when we used Keplers 3rd Law PHYS 3380 - Astronomy Escape Velocity If a projectile is fired straight up with a large enough velocity, it will escape the Earths gravity. It will travel slower and slower due to the Earths gravity, but never to zero. Escape velocity - velocity at which gravity can not stop outward motion. Note that the gravitational attraction of Earth never ceases, it just gets

infinitesimally small. Escape velocity is calculated by using conservation of energy - a body achieves escape velocity when the all of its initial gravitational potential energy is converted to kinetic energy. PHYS 3380 - Astronomy Potential energy Gravitational Force - vector r is the unit vector in outward direction Gravitational potential energy at distance r from reference point Kinetic energy

Escape velocity Starting from the surface of the Earth: r = 6.378 X 106 m, M = 5.97 X 1024 kg, G= 6.67 x 10-11 Nm2/ kg2 v= 11,174 m/s PHYS 3380 - Astronomy Types of Orbits Parabolic Elliptical Circular Hyberbolic

PHYS 3380 - Astronomy Center of Mass Note: the previous calculations assumed that the mass of the orbiting body was much smaller that the central body - center of orbit at center of central body Newton showed that two objects attracted to each other by gravity actually orbit about their center of mass - the point at which the objects would balance if they were connected.

Center of Mass - Binary Star This idea is used to find planets orbiting other stars - massive planets cause star to move against background stars PHYS 3380 - Astronomy Einstein 1905 - The Year of Physics Submitted doctoral thesis "A New Determination of Molecular Dimensions Published five pioneering papers in "Annalen der Physik" - revolutionized physics: "On A Heuristic Point of View Concerning the Production and Transformation of Light"

- electromagnetic radiation must consist of quantums or photons - explained the photoelectric effect - became the foundation of quantum theory - what he received the Nobel Prize for in 1921 "On the Electrodynamics of Moving Bodies" - special relativity - new interpretation of the conception of space and time - observer can never detect their uniform motion except relative to other objects - coordinate systems - speed of light constant - independent of motion relative to light source "Does the Inertia of a Body Depend upon its Energy Content?" - the equivalence of mass and energy - E = mc2 PHYS 3380 - Astronomy

General Relativity 1916 published "The Foundation of the General Theory of Relativity - generalized special theory of relativity - observer cannot distinguish between inertial forces due to acceleration and uniform gravitational forces - gravity is curvature of space-time - curvature dependent on mass - acceleration of mass dependent on space-time curvature Numerous implications on astronomy and astrophysics - orbital motion - black holes - big bang - formation and structure of galaxies

PHYS 3380 - Astronomy Proof of General Relativity Theory predicted the deflection of light in a gravitational field Einstein convinced that light deflection by the gravitational field of the sun could be observed during a total solar eclipse - photograph section of sky where eclipse would occur - during eclipse, photograph same section and measure difference in positions - predicted deflection of 1.75 arcseconds for starlight grazing Suns surface

Several failed observations of total solar eclipses before proof in 1919 - observed eclipse in island of Principe in the Gulf of Guinea in western Africa and Sobral, Brazil - found shift in stars outward from Sun - 1.610.30 arcseconds at Principe - 1.980.12 arcseconds at Sobral PHYS 3380 - Astronomy PHYS 3380 - Astronomy Einsteins eclipse . PHYS 3380 - Astronomy

Proof of General Relativity Precession of long axis of Mercurys orbit Newtons formulation predicted precession of 5557.62 arcseconds per century - actually 43.11 arcseconds more - about 29 km past position predicted by Newton per orbit accumulative - 12,000 km per century - easily measured Einstein predicted 43.03 arcseconds per century difference Effect since observed on Venus, Earth, and asteroid Icarus PHS 3380 - Astronomy GPS Satellite clock drift - relativistic effect

satellites move at 3874 m/s - relativistic time dilation means time runs slower on GPS satellite than on Earth ~ 7.2 microseconds per day satellite at 20000 km height exposed to a much weaker field of gravitation than the observer on Earth gravitational time dilation means clock on board of a satellite is running faster than one on Earth this effect about six times stronger than time dilation frequency standard onboard each satellite given rate offset prior to launch makes clock run slightly slower than the desired frequency on Earth at 10.22999999543 MHz instead of 10.23 MHz satellite clock errors are periodically corrected by Control Segment

PHYS 3380 - Astronomy Light PHYS 3380 - Astronomy Light What is light? - A vibration in an electromagnetic field through which energy is transported. The dual nature of light or wave-particle duality: Light as a wave f=c

Light as a particle E = hf photon PHYS 3380 - Astronomy Properties of Waves Period: time to complete one cycle of vibration - from crest to crest or trough to trough Frequency (f): number of crests passing a fixed point per second

Frequency= 1/period Amplitude (a): maximum displacement from equilibrium Wave length ():): distance between successive crests Speed (of a wave) (s)= wave length x frequency s= ): x f PHYS 3380 - Astronomy Light as a Wave Light is a vibration in an electromagnetic field through which energy is transported - a transverse wave - vibration or oscillation is perpendicular to direction of propagation of wave (vs. longitudinal wave - vibration or

oscillation is in the same direction as propagation of wave) So electrons can be manipulated by light. Electrons wiggle up and down as light passes by. PHYS 3380 - Astronomy For a wave, its speed: s = x f But the speed of light is a constant, c. For light: x f = c The higher f is, the smaller is, and vice versa. Our eyes recognize f (or ) as color. Visible light ranges through 7 major colors from long wavelengths (low

frequency - red) to short wavelengths (high frequency - violet) - Red, orange, yellow, green, blue, indigo, violet (Roy G Biv) PHYS 3380 - Astronomy Light as a Particle (Photon) Light propagates as quanta of energy called photons Photons move with speed of light have no mass are electrically neutral Energy of a photon or electromagnetic wave: E = hf = h c/ where h = Plancks constant

f = frequency of a light wave - number of passing a fixed point in 1 second c = velocity of light = wavelength of a light wave Higher frequency/shorter wavelength - higher energy crests PHYS 3380 - Astronomy The Electromagnetic Spectrum Most wavelengths of light can not be seen by the human eye. The visible part of the electromagnetic spectrum lies between ultraviolet

and infrared light (between about 400 and 700 nm). The higher the frequency (shorter the wavelength), the higher the photon energy. Radio waves are at the long wavelength end of the spectrum and gamma rays are at the short wavelength end of the spectrum. PHYS 3380 - Astronomy Light as Information Bearer We can separate light into its different wavelengths (spectrum). Spectrum of a distant object - a spectrum is the amount of energy or intensity at different wavelengths. By studying the spectrum of an object, we can learn its: 1 Composition 2 Temperature

3 Velocity PHYS 3380 - Astronomy Electron Energy Levels Electrons can not have just any energy while orbiting the nucleus. Only certain energy values are allowed. Electrons may only gain or lose certain specific amounts of energy. Each element (atom and ion) has its own distinctive set or pattern of energy levels - holds the key to studying of distant objects in the universe. This diagram depicts the energy levels of Hydrogen.

1 eV (electron volt) = 1.6 X 10-19 J Electron jumps to higher energy levels can only occur with addition of the particular amounts of energy representing differences between possible energy levels. Energy levels are quantized - study of electron energy levels called quantum mechanics. Atom gains this energy either from KE of another atom colliding with it or from absorption of energy carried by light - falls to lower energy level by emitting light or transfer of energy by collision. PHYS 3380 - Astronomy Absorption and Emission. When electrons jump from a low energy shell to a high energy shell, they absorb energy. When electrons jump from a high energy shell to a low energy shell, they emit energy. This energy is either absorbed or emitted at very specific wavelengths, which are different for each atom.

When the electron is in a high energy shell, the atom is in an excited state. When the electron is in the lowest energy shell, the atom is in the ground state. PHYS 3380 - Astronomy Lyman series (UV) Balmer series (V) Rydberg Formula (differences in energy levels in Bohr model of the atom) 1

1 1 2 = 2 2 ( ) Z is the atomic

number, i.e. the number of protons in the atomic nucleus of this Paschen series (IR) element; n is the upper energy level; The Hydrogen Atom. The hydrogen atom is the simplest of atoms. Its nucleus contains only one proton n is the lower which is orbited by only one electron. In going from one energy level; and R is the Rydberg allowed orbit to another, the electron absorbs or emits constant light (photons) at very specific wavelengths. Note wavelength is often written as and the unit used is an (1.09737107 m1) angstrom (A) = 10-8 m

PHYS 3380 - Astronomy Interaction of Light with Matter Hydrogen Emission Spectrum Absorption Spectrum So each electron is only allowed to have certain energies in an atom. Electrons can absorb light

and gain energy or emit light when they lose energy. It is easiest to think of light as a photon when discussing its interaction with matter. Only photons whose energies (colors) match the jump in electron energy levels can be emitted or absorbed. So visible emission spectrum is created when a gas is heated and collisions in gas continually bump electrons to higher energy levels - emit photons of specific wavelength as they fall back to lower levels. Absorption spectrum is produced when white light is passed through cloud of cool gas. Photons of

specific wavelengths absorbed as electrons jump to higher energy levels. PHYS 3380 - Astronomy Emission Spectra Orion Nebula in Ultraviolet The atoms of each element have their own distinctive set of electron energy levels. Each element emits its own pattern of colors, like fingerprints. If it is a hot gas, we see only these colors, called an emission line spectrum.

PHYS 3380 - Astronomy Absorption Spectra Hydrogen If light shines through a cool gas, each element will absorb those photons whose colors match their electron energy levels. The resulting absorption line spectrum has all colors minus those that were absorbed. We can determine which elements are present in an object by identifying emission and absorption lines. PHYS 3380 - Astronomy

Temperature and Thermal Energy Temperature - measure of the average kinetic energy of the particles in a substance particles in box on right have higher temperature - higher velocity = more KE = higher temperature Both boxes have same temperature - particles have same average velocity/KE box on right has more thermal energy - energy contained in a substance - more particles Why does water burn your skin so much quicker than air? Why is falling into a 32 F lake more dangerous than standing outside

naked on a 32 F day? PHYS 3380 - Astronomy This diagram compares three common temperature scales. The Fahrenheit scale is used in the United States, but nearly all other countries use the Celsius scale. Scientists prefer the Kelvin scale because O K represents absolute zero, the coldest possible temperature. PHYS 3380 - Astronomy Thermal/Blackbody Radiation Photons are produced whenever charged particles are accelerated moving charge gives rise to a magnetic field, and if the motion is

changing (accelerated), then the magnetic field varies and in turn produces an electric field - electromagnetic radiation - photons -A In an opaque object or dense gas cloud, photons cant easily escape - they bounce around in the object. This randomizes their radiative energies and resulting photon energies depend only on the bodys temperature - produces a continuous spectrum called a thermal radiation or blackbody spectrum. Blackbody - a hypothetical body that completely absorbs all wavelengths of thermal radiation incident on it - does not reflect light - appears black if temperature low enough so as not to be self-luminous. - all blackbodies heated to a given temperature emit thermal radiation

with the same spectrum - required by thermal equilibrium - distribution of blackbody radiation as a function of wavelength - the Planck law, cannot be predicted using classical physics. - the first motivating force behind the development of quantum mechanics PHYS 3380 - Astronomy Key Features of a Blackbody Spectrum - a dense object produces light at all possible wavelengths if the object is above absolute zero. - since everything in the universe is above 0 K, all dense objects (solids, liquids, thick gases) will produce a thermal spectrum. - the shape of a continuous spectrum depends on only the temperature of the object not its chemical composition.

- as the temperature of an object increases, more light is produced at all wavelengths - as the temperature of an object increases, the peak of thermal spectrum curve shifts to shorter wavelengths (higher frequencies) - -cool things appear red or orange, hotter things appear yellow or white, and very hot things blue or purple. PHYS 3380 - Astronomy Temperature (K) of Black

Body 3 300 3,000 4,000 6,000 8,000 10,000 30,000 300,000 1.5 million 3 billion Wavelength (max) at Which Most Radiation is

Emitted 0.1 cm 0.001 cm 1000 nm 750 nm 500 nm 375 nm 300 nm 100 nm 10 nm 20 nm 0.001 nm Type of Radiation

Radiowaves "Far" Infrared "Near" Infrared Red Light Yellow Light Violet Light "Near" Ultraviolet "Far" Ultraviolet "Soft" X-Rays "hard" x-rays Gamma rays PHYS 3380 - Astronomy Hotter objects emit more total radiation per unit surface area.

E = T4 ( = 5.67 x 10-8 watts/m2 K4) - Stefan-Boltzmann Law Hotter objects emit photons with a smaller wavelength (higher average energy.) max (nm) = 2.8983 x 106 nm-K/T 106 / T(K) [nm] - Wiens Law PHYS 3380 - Astronomy Derivation of the Stefan-Boltzmann Law PHYS 3380 - Astronomy Solid Angle The solid angle subtended by a surface S - the surface area of a unit sphere covered by the surface's projection onto the sphere. This

can be written as where n is a unit vector from the origin, da is the differential area of a surface patch, and r is the distance from the origin to the patch. Written in spherical coordinates with the colatitude (polar angle) and for the longitude (azimuth), this becomes Solid angle is measured in steradians, and the solid angle corresponding to all of space being subtended is 4 steradians. PHYS 3380 - Astronomy PHYS 3380 - Astronomy Consider the solid angle subtended by one face of a cube of side length

centered at the origin. Since the cube is symmetrical and has six sides, one side obviously subtends 4/6 steradians. PHYS 3380 - Astronomy PHYS 3380 - Astronomy PHYS 3380 - Astronomy So, the luminosity of a star depends on temperature and size (surface area). Amount radiated from every square meter equals TT4 (Stefan-Boltzmann Law) - the hotter the star, the more energy radiated per square meter Total amount radiated (luminosity):

L = 4R2TT4 R is star's radius, surface area = 4R2 Stellar luminosities generally given in number of solar luminosities: If we measure L and T, we can estimate R T can be determined using Weins Law

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