Planetary Astronomy
PIRA classification 8A
8A05. Historical Astronomy
PIRA # |
Demonstration Name |
Subsets |
Abstract |
8A05.10 |
Calender Wheels |
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Native American celestial calendar wheels and how to construct them. See TPT 37(8), 476 |
8A05.15 |
Stonehenge |
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Many models of this famous megalith are available. |
8A05.16 |
Megaliths |
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Some historical background on megalithic astronomy. See AJP 45(2), 125 |
8A05.20a |
Constellations |
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Constellations used to interpret historical legends. See TPT, 31(6), 383 |
8A05.20b |
Constellations |
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The Big Dipper used to tell time. See TPT, 29(2), 80 |
8A05.30a |
Eratosthenes measurement of Earth's radius |
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Eratosthenes determination of the circumference of the Earth updated by doing the experiment from an aircraft. See TPT 25(8), 500 |
8A05.30b |
Eratosthenes measurement of Earth's radius |
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Eratosthenes experiment redone using meter sticks instead of wells. See TPT 26(3), 154 |
8A05.30c |
Measurement of Earth's radius |
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The calculation done using feet and miles. Also several other neat problems using Earth's radius as a starting point. See TPT 31(9), 519 |
8A05.30d |
Measurement of Earth's diameter |
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A GPS is used to calculate the diameter of the Earth. See TPT 38(6), 360 |
8A05.30e |
Eratosthenes measurement of Earth's radius |
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Trying to calculate the radius of the Earth by watching the Sun set twice, once from the bottom and then from the top of a tall building. See TPT 31(7), 440 |
8A05.30f |
Eratosthenes - scale of Earth/Moon/Sun system |
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Using Eratosthenes calculation of the diameter of the Earth to calculate the size of the Moon. See TPT 38(3), 179 |
8A05.33 |
Eudoxus: homocentric spheres models |
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Two homocentric models of Eudoxus: one shows the motion of the Sun, the other shows retrograde motion. See AJP, 31(6),456 |
8A05.35 |
Ptolemaic and Copernican orbits |
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An analog computer (circuit given) displays orbits and epicycles on an oscilloscope. See AJP, 30(9),615 |
8A05.40a |
Kepler and planetary orbits |
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A photographic solution to Kepler's laws. See AJP, 69(4), 481 |
8A05.40b |
Kepler and planetary orbits |
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An unusual verification of Kepler's first law. See AJP, 69(10), 1036 |
8A05.40c |
Kepler and planetary orbits |
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A graphical representation of Kepler's third law. See TPT 36(4), 212 |
8A05.40d |
Kepler and planetary orbits |
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Kepler's third law calculations without a calculator. See TPT 42(9), 530 |
8A05.40e |
Kepler and planetary orbits |
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Kepler's third law and the rise time of stars. See TPT 25(8), 493 |
8A05.40f |
Kepler and planetary orbits |
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Applying Kepler's third law to elliptical orbits. See TPT 34(1), 42 |
8A05.40g |
Kepler and planetary orbits |
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Measuring an asteroids orbit to test Kepler's first and second law. See TPT 36(1), 40 |
8A05.50 |
Sundial |
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A Plexiglas model of a sundial. See AJP 52(2),185 |
8A05.50 |
Sundial |
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Detailed descriptions, pictures, and how to time correct a sundial. See TPT 10(3), 117 |
8A05.50 |
Sundial, solar pocket watch |
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Picture of a portable sundial (solar pocket watch) dated 1573. See TPT 41(5), 268 |
8A05.50 |
Sundial |
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Constructing a portable sundial. See TPT 37(2), 113 |
8A05.50 |
Sundial, solar pocket watch |
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Additional observations on TPT 41(5), 268. |
8A05.55 |
Horizontal sundial |
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An analytic solution for determining the markings on a sundial and a description of construction. See AJP 42(5),372 |
8A05.60 |
Cross-staff |
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Cut a meter stick into 57 1/3 cm and 42 2/3 cm. (At 57 1/3 cm one degree equals one cm.) Some refinements. See AJP 33(2),165 |
8A05.70 |
Sextant |
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Pictures of and directions for sextants. |
8A05.70 |
Sextant |
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An easily constructed mini-sextant and directions for it's use. See TPT 38(4), 238 |
8A05.80 |
Artificial Horizon |
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A mercury filled dish that is used for an artificial horizon when taking measurements with a sextant during times when the real horizon is obscured. |
8A05.85 |
Chronometer |
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An accurate ships time piece used in conjunction with the sextant to determine longitude and latitude. |
8A05.90 |
Heliostat |
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Picture of a heliostat. See AJP 38(3),391 |
8A10. Solar System Mechanics
PIRA # |
Demonstration Name |
Subsets |
Abstract |
8A10.05 |
Origin of the Solar System |
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Discussion on how the Solar System was formed. See TPT 5(8), 363 |
8A10.06 |
Planetary nebula |
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On the formation of planetary nebula. See TPT 29(5), 268 |
8A10.10a |
Orrery model |
pira200 |
A motor-driven model of the Sun, Moon, Earth system. The size is not to scale, the periods of orbit are scaled. |
8A10.10b |
Orrery model |
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A mechanical model of the inner planets. |
8A10.15 |
Scale of the Solar System - Video |
|
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8A10.15 |
Inflatable Solar System |
|
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8A10.15 |
Solar System on a String |
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8A10.15 |
Scale model of the Solar System |
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The scale model of the Solar System as a hallway demo. See TPT 16(4), 223 |
8A10.15 |
Scale model of the Solar System |
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The 1:10 billion Colorado Scale-Model Solar System on the University of Colorado-Boulder campus. See TPT 29(6), 371 |
8A10.15 |
Scale model of the Solar System |
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Globes and balloons used to model the planets of the Solar System. See TPT 27(1), 38 |
8A10.16 |
Scale of the orbital radii of the planets |
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A hat pin, roll of tape, and some markers used to scale the orbital radii of the planets. See TPT 43(2), 120 |
8A10.20 |
Locating stars |
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A simple analytical method at the descriptive astronomy level for locating stars. See AJP 53(6),591 |
8A10.20 |
Locating stars |
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Using the stars of the Big Dipper to teach vectors. See TPT 44(3), 168 |
8A10.22 |
Tracking stars, Sun, and Moon |
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Construction of an electromechanical device that automatically and continually tracks celestial objects. See AJP 78 (11), 1128 |
8A10.25 |
Diurnal motion |
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Punch holes in a can bottom in the big dipper pattern and place over a point source of light. Rotate the can. See AJP 43(1),113 |
8A10.30 |
Planispheric planetarium |
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Description of a homemade planetarium. |
8A10.30 |
Small planetarium |
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Description of a small homemade planetarium dome. |
8A10.33 |
Day & night |
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8A10.35 |
Local zenith |
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8A10.40 |
Sidereal time |
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An explanation of how a sidereal day differs from a solar day and how to calculate the difference. See TPT 29(5), 265 |
8A10.42 |
Sidereal day |
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A simple method to measure the length of the sidereal day. See TPT 30(9), 558 |
8A10.44 |
Sidereal year |
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Use orbital mechanics and centripetal force to calculate the sidereal year. See TPT 32(2), 111 |
8A10.50 |
Precession of the equinox graph |
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A graph that shows the precession of the equinox from 1890 to 2000 and a discussion of its pedagogical value. See AJP 55(9),848 |
8A10.60 |
Apparent motion of the sun |
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The autumn and spring equinoxes do not have equal length days and nights. Index of refraction through the atmosphere makes the day about 9 minutes longer than the night. See TPT 35(3), 167 |
8A10.70 |
Distortion due to refraction by Earth atmosphere |
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On the flatness of the setting sun. See AJP 71(4), 379 |
8A10.70 |
Distortion due to refraction by Earth atmosphere |
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A demonstration using sugar water to show why the Sun appears elliptical instead of round when viewed through the atmosphere. See TPT 29(9), 566 |
8A10.70 |
Distortion due to refraction by Earth atmosphere |
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The appearance of the flattening of the solar disk and the appearance of the "anti-Sun" captured on film. See TPT 35(9), 553 |
8A10.70 |
Distortion due to refraction by Earth atmosphere |
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The apparent ellipticity of the setting Sun. See TPT 20(6), 404 |
8A10.75 |
Distortion due to refraction by Earth atmosphere |
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A complete explanation of distortions produced by the atmosphere. See TPT 39(2), 92 |
8A10.80 |
Geochron |
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The standard Geochron is used to show analemma, the part of the Earth lit by the Sun at any given time, etc. See [http://scitation.aip.org/tpt/ |
8A10.80 |
Subsolar point |
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An experiment plotting the subsolar point (the place on Earth where the Sun is directly overhead at solar noon). See TPT 29(5), 318 |
8A10.80 |
Analemma |
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Additional comments on TPT 34(1), 58 |
8A10.80 |
Analemma |
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A good explanation of how the analemma couples the seasonal declination changes of the Sun with the "Equation of Time". See TPT 34(6), 355 |
8A10.80 |
Analemma |
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Analemma used to show why sunrise can be at the same time for several weeks while the length of the day increases. See TPT 34(1), 58 |
8A10.80 |
Analemma |
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How to plot and demonstrate the noncircularity of the Earth's orbit around the Sun. See TPT 38(9), 570 |
8A10.80 |
Analemma, clocks, apparent motion of the Sun |
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Explains why the length of the morning and afternoon do not increase in the same proportion as the length of the day gets longer. See TPT 23(2), 85 |
8A10.90 |
Apparent motion of the Sun |
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A formula for the number of days between the winter solstice and the latest sunrise. See AJP, 71(12), 1242 |
8A10.90 |
Apparent motion of the Sun |
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Using simple equipment to measure the length of the solar day. See TPT 34(6), 351 |
8A10.90 |
Apparent motion of the Sun |
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Using the apparent motion of the Sun to teach vectors and scalar products. See TPT 35(5), 310 |
8A20. Earth-Moon Mechanics
PIRA # |
Demonstration Name |
Subsets |
Abstract |
8A20.05 |
Earth's Seasons |
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Showing the Earth's seasons with a 3-D model. See TPT 31(7), 419 |
8A20.07 |
Seasonal Tilt |
|
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8A20.08 |
Tilt of the Earth - Video |
|
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8A20.15 |
Phases of the moon - terminator line demo |
pira200 |
View a ball illuminated by a distant light with a TV camera as the source is rotated around the ball. |
8A20.15 |
Phases of the moon |
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How the view of the crescent moon changes from the northern to southern hemisphere. See TPT 38(6), 371 |
8A20.15 |
Phases of the moon |
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An exercise in Moon watching and observation of phases of the Moon. See TPT 32(2), 126 |
8A20.15 |
Phases of the moon |
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Phases of the moon shown with a styrofoam ball, light source, and a CCD camera. See TPT 34(6), 360 |
8A20.15 |
Phases of the moon |
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A handy way to teach "Moon Phases". See TPT 31(3), 178 |
8A20.17 |
Phases models |
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Illuminated models for showing the phases of Venus and the Moon. See TPT 3(6),263 |
8A20.19 |
Phases of planets |
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Calculating the phases of the outer planets. See TPT 37(9), 528 |
8A20.20 |
Albedo |
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8A20.20 |
Brightness of the Moon |
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Two methods to determine the brightness of the Moon. See TPT 23(5), 293 |
8A20.22 |
Eccentricity of the Moon's orbit |
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A piece of cardboard with a hole slid up and down a yardstick is used to determine the eccentricity of the Moon's orbit. See AJP 78 (8), 834 |
8A20.25 |
Eclipse model |
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An eclipse model built from Hoola Hoops to show the eclipse seasons. See TPT 34(6), 376 |
8A20.30 |
Solar eclipse |
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Preparations and observation of the March 7, 1970 eclipse. See TPT 9(5), 276 |
8A20.30 |
Solar eclipse |
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The path of the February 26, 1998 solar eclipse. See TPT 35(9), 515 |
8A20.31 |
Solar eclipse |
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Using a solar eclipse to estimate the Earth-Moon distance. See TPT 34(4), 232 |
8A20.32 |
Solar eclipse, pinhole images |
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Using pinholes and natural phenomenon to view a solar eclipse. See TPT 32(6), 347 |
8A20.35 |
Lunar eclipse |
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Why the Moon appears red during a lunar eclipse. See TPT 44(3), 181 |
8A20.37 |
Umbra, penumbra |
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Why there are crisp, dark or fuzzy shadows during eclipses. |
8A20.40 |
Transit - Mercury & Venus |
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8A20.45 |
Occultations |
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Occultation used to determine the diameter of a planet. See AJP 45(10), 914 |
8A20.45 |
Occultations |
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Lunar geography shown determined by grazing occultation. See TPT 21(4), 218 |
8A20.45 |
Occultations |
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Occultation used to determine the diameter of the Moon. See TPT 30(5), 290 |
8A20.50 |
Earth/Moon system |
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The Earth-Moon system orbits the Sun at its center of mass or barycenter. See TPT 44(1), 48 |
8A20.55 |
Earth/Moon system |
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Using Earth-Moon communication to calculate the speed of light. See TPT, 44(7), 414 |
8A20.60 |
Earth/Moon distance |
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Retroreflector arrays and laser pulses to measure the Earth/Moon distance. See TPT 33(2), 90 |
8A20.60 |
Earth/Moon distance |
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How to determine the distance to the Moon. See TPT 10(1), 40 |
8A20.64 |
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A 10" globe, a painted tennis ball, and a 100 W bulb are used to represent the Earth-Moon-Sun system |
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8A20.70 |
Pinhead Earth |
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8A20.70 |
Scale model of the Earth/Moon/Sun system |
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Using a basketball and a push pin to model the Sun-Earth system. See TPT 38(2), 115 |
8A20.70 |
Scale model of the Earth/Moon/Sun system |
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Pinholes used to enhance a 1:2 billion scale model of the Earth/Moon/Sun system. See TPT 11(8), 489 |
8A20.80 |
Moon & Tides |
|
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8A30. Views From Earth
PIRA # |
Demonstration Name |
Subsets |
Abstract |
8A30.10 |
Horizon astronomy model |
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8A30.10 |
Cratering |
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8A30.10 |
Horizon calculations |
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A method for calculating the distance to the horizon. |
8A30.10 |
Estimating the distance to the horizon |
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An analysis for calculating the distance to the horizon as a function of the altitude of the observer. Also takes into account the variation of atmospheric refractive index with height. See AJP 50 (9), 795 |
8A30.10 |
Estimating the distance to the horizon |
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How to accurately estimate the distance to the horizon. See TPT 38(9), 528 |
8A30.13 |
Estimating the distance to the horizon |
|
How to accurately estimate the distance to the horizon when at sea. |
8A30.20 |
Cinhelium |
|
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8A30.30 |
Retrograde motion model |
pira200 |
Two balls, connected with a rod fixed through one ball and sliding through the other, orbit on a common focus. |
8A30.30 |
Retrograde motion model |
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Two balls driven by independent clock motors are connected with a rod fixed through one ball and sliding through the other. See AJP 54(11),1021 |
8A30.32 |
Retrograde motion |
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Three methods to plot retrograde motion, one is simpler than the others. See AJP 43(7), 639 |
8A30.32 |
Retrograde motion |
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Using retrograde motion to understand and determine orbital parameters of a planet using only geometry and trigonometry. See 73(11), 1023 |
8A30.32 |
Retrograde motion of Mars |
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How to plot the retrograde motion of Mars on paper. See TPT 37(6), 342 |
8A30.32 |
Retrograde motion |
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A method of plotting retrograde motion on a large scale to be done outdoors with twine and students. See TPT 30(5), 302 |
8A30.32 |
Retrograde motion |
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Plotting retrograde motion in a manner that gives a better diagram. See TPT 21(4), 252 |
8A30.34 |
Retrograde motion |
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Retrograde motion and epicycles are shown using polar graph paper and a fender washer. See TPT 35(9), 554 |
8A30.40 |
Epicycles |
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An Orrery carries a small flashlight on a rod between Earth and Jupiter to project epicycloidal motion. |
8A30.40 |
Epicycles |
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An elliptical Lucite dish has two arms attached to one foci. Place some ball bearings between the two arms and rotate the rear arm at constant angular velocity. |
830.40 |
Epicycles |
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A diagram of how to make a fairly simple crank device to trace out elliptical through cusped figures with a penlight. |
8A30.50 |
Synodic period |
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Using calculations to show that the conjuction and opposition of a planet are not "perfect" due to non-circular orbits. See TPT 19(2), 116 |
8A30.50 |
Synodic period |
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Use relative angular velocity to calculate the synodic period. See TPT 23(3), 154 |
8A30.60 |
Tidal locking |
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Why the same side of the Moon always faces the Earth. See TPT 41 (6), 363 |
8A30.60 |
Tidal locking |
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A demonstration on how the Moon and other moons become tidally locked. See TPT 35(6), 379 |
8A30.70 |
Parallax |
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Have students measure the distance to objects in the classroom by parallax using a camera to better understand stellar parallax. See AJP 45(5), 490 |
8A30.70 |
Parallax |
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Another simple photographic experiment to help students understand parallax. See AJP 45(12), 1221 |
8A30.70 |
Parallax |
|
Measuring the distance to an outer planet by parallax with a camera. See TPT 35(1), 34 |
A30.72 |
Parallax |
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A laboratory model to calculate stellar distances by parallax and relative magnitude. See AJP 45(11), 1124 |
8A30.80 |
Autoresonance |
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3:2 and 2:1 resonances of the planets and asteroids. See AJP, 69(10), 1096 |
8A30.90 |
Roche Limit |
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A calculation of the Roche limit of a Jovian planet and a simulated experiment to test the calculation. See TPT, 44(6), 381 |
8A35. Views From Earth 2
PIRA # |
Demonstration Name |
Subsets |
Abstract |
8A35.10 |
Celestial sphere |
pira200 |
A simple model celestial sphere is made from a round bottom flask. Pictures. |
8A35.10 |
Celestial sphere |
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8A35.15 |
Celestial sphere |
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Modifying the Replogle Model 15620 celestial sphere. See TPT 18(6), 465 |
8A35.16 |
Celestial sphere |
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Making your own celestial sphere by locating stars. See TPT 25(7), 438 |
8A35.18 |
Celestial sphere |
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Introducing students to the celestial sphere should always be done with a companion Earth-Sun model. See AJP 73(11), 1030 |
8A35.18 |
Celestial sphere |
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Difficulties teaching concepts with a celestial sphere may be simplified by construction of a mechanical Armillary. See TPT 10(2), 96 |
8A35.30 |
Satellite orbits |
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Plotting the orbits of the planets from existing data and charts. See TPT, 45(6), 369 |
8A35.30 |
Satellite orbits |
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Orbital periods of Mercury, Venus, and the Earth simulated using a whirligig setup. See TPT 31(2), 122 |
8A35.30 |
Satellite orbits |
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Calculating how long it takes for a planet to fall into the Sun if its orbital motion is arrested and relating that to the orbital period of the planet. See TPT 36(2), 122 |
8A35.32 |
Satellite orbits |
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The orbital motion of the Moon explained by projectile motion. See TPT 19(3), 181 |
A35.35 |
Satellite orbits |
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Calculation showing that an orbiting satellite is in freefall. See TPT 23(1), 29 |
8A35.35 |
Satellite orbit model |
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Making a satellite/Earth system model from glass tubing, a model rocket, nylon thread, a support stand, wooden sphere, and hooked masses. See TPT 46(4), 237 |
8A35.40 |
Satellite orbits |
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The effect of atmospheric drag and temperature on satellite orbits. See TPT 43(7), 452 |
8A35.50 |
Slingshot effect |
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A simple explanation of the "slingshot effect" or "gravity assist". See TPT 23(8), 466 |
8A40. Planetary Properties: Globes, Hemispheres, & Maps
PIRA # |
Demonstration Name |
Subsets |
Abstract |
8A40.10 |
Globes |
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Globes of Earth, the Moon, Mercury, Venus, Mars, etc. See University of Minnesota Handbook - 8A20.10 |
8A40.20 |
Globes and hemispheres |
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The angles of any triangle on a sphere or hemisphere always add up to more than 180 degrees. See TPT 32(8), 506 |
8A40.20 |
The minimum path length joining two points on a sphere's surface is a segment of a "great circle". |
|
Globes and hemispheres. See TPT 26(5), 280 |
8A50. Planetary Properties 2: The Planets
PIRA # |
Demonstration Name |
Subsets |
Abstract |
8A50.10 |
Mercury |
|
|
8A50.12 |
Mercury's Orbit |
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Plotting Mercury's orbit from data in The Astronomical Almanac. See The Physics Teacher - TPT 29(6), 346 |
8A50.15 |
Perihelion of Mercury |
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The precession of the perihelion of Mercury's orbit calculated using the LaPlace-Runge-Lenz vector.. See American Journal of Physics - AJP 73(8), 730 |
8A50.15 |
Perihelion of Mercury |
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A Lagrangian yielding the same equations of motion that Einstein derived for the precession of the perihelion of Mercury. See American Journal of Physics - AJP 70(5), 498 |
8A50.20 |
Venus |
|
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8A50.30 |
Earth |
|
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8A50.30 |
Earth's Rotation |
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Does the Earth rotate? Seven "proofs" for the rotation of the Earth. See The Physics Teacher - TPT 25(2), 86 |
8A50.30 |
Earth's Rotation |
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Several other experiments carried out that proved the Earth rotates. See The Physics Teacher - TPT 25(7), 418 |
8A50.30 |
Earth's Rotation |
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One more "proof" the Earth rotates. See The Physics Teacher - TPT 30(4), 196 |
8A50.30 |
Earth's Rotation |
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Additional experiments on how we sense the Earth rotates. See The Physics Teacher - TPT 30(2), 111 |
8A50.30 |
Earth's Rotation |
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Leeuwenhoek's "Proof" of the Earth's rotation. See The Physics Teacher - TPT 33(3), 144 |
8A50.30 |
Earth's Rotation |
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Emperical evidence the Earth rotates by marking the length of a shadow of a rod in two minute intervals starting 20 minutes before midday and ending 20 minutes after midday. See The Physics Teacher - TPT 33(2), 116 |
8A50.34 |
Geological Timeline - Earth |
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|
8A50.35 |
The Moon |
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A calculation of how high you can jump on the Moon. See The Physics Teacher - TPT 11(1), 43 |
8A50.35 |
The Moon |
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What information it takes to calculate the size of the Moon. See The Physics Teacher - TPT 38(3), 179 |
8A50.36 |
The Moon's orbit |
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How to observe the Moon's path with a cross-staff and plot its path. See The Physics Teacher - TPT 29(3), 160 |
8A50.38 |
Moonquakes |
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Detection and analysis of moonquakes by the seismometers left on the Moon by the Apollo astronauts. See The Physics Teacher - TPT 38(9), 522 |
8A50.39 |
The Moon's offset center-of-mass |
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Comments on the center-of -mass offset of the Moon. See American Journal of Physics - AJP 46(7),762 |
8A50.40 |
Mars |
|
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8A50.41 |
Mars Missions, Orbital Timing |
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The problems, physics principles, and timing involved in a mission from Earth to Mars. See The Physics Teacher - TPT, 43(5), 293 |
8A50.42 |
Aerobraking at Mars |
|
The physics of aerobraking at Mars. See The Physics Teacher - TPT 36(3), 154 |
8A50.45 |
Mars' moons |
|
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8A50.50 |
Jupiter |
|
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8A50.52 |
Jupiter |
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Looking at the Solar System from Jupiter's reference frame. See The Physics Teacher - TPT 35(3), 178 |
8A50.55 |
Jupiter's moons / Galilean Satellites |
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|
8A50.55 |
Io |
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The volcanos on Io. See The Physics Teacher - TPT 19(6), 402 |
8A50.55 |
Europa's Ocean |
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An exercise exploring the effect of freefall acceleration on buoyancy and waves. See The Physics Teacher - TPT 25(8), 508 |
8A50.55 |
Galileo's discovery of Jupiter's moons |
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A look at the challenges Galileo faced during his observation of the Jovian moons. See The Physics Teacher - TPT 30(2), 103 |
8A50.60 |
Saturn |
|
|
8A50.65 |
Saturn's Moons |
|
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8A50.65 |
Mimas |
|
Statistics about Mimas and the view of Saturn from Mimas. See The Physics Teacher - TPT 26(4), 207 |
8A50.70 |
Uranus |
|
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8A50.75 |
Uranus' Moons |
|
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8A50.80 |
Neptune |
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8A50.85 |
Neptune's Moons |
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8A60. Planetary Properties 3: Planetoids, Minor Objects
PIRA # |
Demonstration Name |
Subsets |
Abstract |
8A60.10 |
Pluto/Charon |
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The history and process that resulted in Pluto's demotion from a planet to a minor object. See The Physics Teacher - TPT 45(1), 14 |
8A60.20 |
Asteroids |
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8A60.25 |
Asteroids |
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Describes the trajectory of an asteroid as it approaches a planet of much greater mass. Values are given for Earth, Mars, Jupiter, and Saturn. See American Journal of Physics - AJP 74(8), 717 |
8A60.25 |
Asteroids |
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Estimates of catastrophic asteroid and comet impacts on the Earth. See American Journal of Physics - AJP 74(9), 789 |
8A60.25 |
Asteroids |
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How asteroid or comet impacts is not the cause of and would not significantly change the eccentricity of Earth's orbit. See American Journal of Physics - AJP 71(7), 687 |
8A60.25 |
Asteroids |
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The physics of asteroid/Earth collisions. See The Physics Teacher - TPT 40(8), 487 |
8A60.30 |
Meteorites |
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Mass spectroscopy of meteorites. See The Physics Teacher - TPT 5(1), 5 |
8A60.35 |
Meteors |
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"Observing" a meteors ionized trail by using radio. See The Physics Teacher - TPT 37(2), 123 |
8A60.40 |
Outer Solar System Objects |
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|
8A60.50 |
The Kuiper Belt |
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|
8A60.60 |
Extra-Solar Planets |
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The precision it takes to detect extra-solar planets. See The Physics Teacher - TPT 39(7), 400 |
8A60.60 |
Extra-Solar Planets |
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Teaching about data and detection of extra-solar planets by asking how our solar system would look if viewed by an observer from far away using the same detection methods. See The Physics Teacher - TPT 42(4), 208 |
8A60.60 |
Extra-Solar Planets |
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Teaching about and helping with the search for extra-solar planets. See The Physics Teacher - TPT 39(2), 120 |
8A60.70 |
Matter from Outside Our Solar System |
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Using cosmic rays to study matter in the galaxy outside our solar system. See The Physics Teacher - TPT 20(4), 222 |
8A70. Planetary Properties 4: Planetary Characteristics
PIRA # |
Demonstration Name |
Subsets |
Abstract |
8A70.05 |
Geological Samples |
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Assortments of rocks, minerals, or gemstones. |
8A70.10 |
Planetary Magnetism |
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|
8A70.10 |
Earth's Magnetic Field |
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An elementary model of Earth's magnetic field capturing some features of the geodynamo. See The Physics Teacher - TPT 45(3), 168 |
8A70.20 |
Refraction/Twinkling |
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Refer to 6A40.47 to demonstrate how observing planets and stars through the atmosphere makes them appear to twinkle. |
8A70.20 |
Thickness of Earth's Atmosphere |
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A method of estimating the thickness of the atmosphere by light scattering. See American Journal of Physics - AJP 71(10), 979 |
8A70.20 |
Effective Depth of Earth's Atmosphere |
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Using "The Old Farmers Almanac" to calculate the effective depth of the atmosphere. See The Physics Teacher - TPT 35(2), 90 |
8A70.20 |
Earth's Atmosphere |
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The interaction of radiation from the Sun and the Earth's atmosphere determines the Earth's climate. See The Physics Teacher - TPT 26(5), 266 |
8A70.22 |
Sounding Balloon Experiment |
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Atmospheric measurements using sounding balloons. See The Physics Teacher - TPT 43(9), 578 |
8A70.30 |
Sprites |
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Exotic lightening that takes place above thunderstorms. See American Journal of Physics - AJP 74(9), 804 |
8A70.40 |
Greenhouse Effect |
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See 4B50.60 for demonstrations of the greenhouse effect. |
8A70.45 |
Cloud Formation |
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See 4B70.20 for cloud in a bottle demonstrations. |
8A70.48 |
IR Telescope Model |
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Construction of a simple IR telescope. |
8A70.50 |
Gaseous Planets |
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|
8A70.50 |
Gaseous Planet Atmospheres |
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Float bubbles on layers of Freon, CO2, or other heavy gases in the bottom of a fish tank. See The Physics Teacher - TPT 16(7), 490 |
8A70.55 |
Rotational Banding |
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Rheoscopic fluid in a round bottom flask placed on a turntable will show rotational banding when turned for a few seconds. |
8A70.55 |
Planetary Atmospheres |
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A demonstration that can be used to explain rotational banding in planetary atmospheres. See The Physics Teacher - TPT 35(7), 391 |
8A70.55 |
Planetary Atmospheres |
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The composition of the atmospheres of the planets and the moon Titan. How would acoustic waves travel in these atmospheres. See The Physics Teacher - TPT 40(4), 239 |
8A70.60 |
Precipitation in the Solar System |
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Descriptions of the types of precipitation that fall on the other planets and moons in the Solar System. Some of these can be brought into the classroom. See The Physics Teacher - TPT 45(8), 502 |
8A70.65 |
Aurora |
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Historical and detailed explanation of Earth's aurora. See The Physics Teacher - TPT 17(4), 228 |
8A70.65 |
Aurora |
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A brief description of aurora and how to photograph them. See The Physics Teacher - TPT 44(2), 68 |
8A70.65 |
Auroral Measurements |
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How to obtain and plot auroral data in the classroom. See The Physics Teacher - TPT 33(1), 34 |
8A70.70 |
Lightening Whistlers |
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Ionospherice whistlers at radio frequencies. |
8A70.70 |
Culvert Whistlers |
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See 3B25.67 for acoustical examples, demonstrations, and comparisons to ionospheric whistlers. |
8A70.75 |
Planetary Density Model |
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Add abstract in Handbook.FM |
8A70.78 |
Planetary Gravities |
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Use pennies and soda cans to show how a can of soda would feel on different planets. Mercury = 38 pennies, Venus = 101, Earth = 1 can of soda or 100 pennies, the Moon = 12, Mars = 38, Jupiter = 293, Saturn = 119, Uranus and Neptune = 133, Pluto = 0. |
8A70.80 |
Red Hot Ball |
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Heat a small metal ball until it glows red hot. Watch it cool with a black and white camera or an IR camera. Observe that it still glows in the camera even though the eye can no longer see it. A match may be lit off the apparently non-glowing ball for effect. |
8A70.80 |
Earth's Glow |
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The Earth glows from nuclear processes in the interior. See The Physics Teacher - TPT 35(4), 230 |
8A70.85 |
Earthquakes |
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Student participation in P-wave and S-wave demonstrations. See The Physics Teacher - TPT 16(7), 479 |
8A70.90 |
Cratering |
|
Drop ball bearings into a pan of glass beads or flour. Illuminate with a lamp from the side of the pan to provide contrast. See University of Minnesota Handbook - 8A20.30 |
8A70.90 |
Cratering |
|
Impact cratering studied in the laboratory using a marble for the meteorite, salt for the target, and a video camera to record the impact. Frame by frame analysis. See American Journal of Physics - AJP 68(8), 771 |
8A70.91 |
Cratering |
|
High speed photography and analysis of milk drops falling into coffee that can be applied to cratering. See The Physics Teacher - TPT 27(2), 118 |
8A80. Planetary Properties 5: Comets and the Search for Life
PIRA # |
Demonstration Name |
Subsets |
Abstract |
8A80.10 |
Make a Comet |
|
Add abstract in Handbook.FM |
8A80.10 |
Ed's Comet |
|
Add abstract in Handbook.FM |
8A80.20 |
Comet Orbit |
|
|
8A80.20 |
Comet Orbits |
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The erroneous view that in Newton's Principia one can find a proof that inverse-square central forces implies a conic-section orbit. See The Physics Teacher - TPT 23(1), 6 |
8A80.30 |
Halley's Comet |
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About Halley's comet. See The Physics Teacher - TPT 22(8), 488 |
8A80.30 |
Halley's Comet |
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Preparing to observe Halley's comet in 1986. See The Physics Teacher - TPT 15(2), 110 |
8A80.30 |
Halley's Comet |
|
Making a Halley's comet orbit model. See The Physics Teacher - TPT 23(8), 490 |
8A80.30 |
Halley's Comet |
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Making sense of the apparent path of Halley's comet. See The Physics Teacher - TPT 23(8), 485 |
8A80.40 |
Comet Hale-Bopp |
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A computer preview of comet Hale-Bopp. See The Physics Teacher - TPT 34(9), 558 |
8A80.40 |
Comet Hale-Bopp |
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Photographs and data review of comet Hale-Bopp. See The Physics Teacher - TPT 35(6), 348 |
8A80.80 |
Comets Emit X-Rays |
|
Surprise, comets emit x-rays. See The Physics Teacher - TPT 35(4), 247 |
8A80.90 |
Creating Life in the Classroom |
|
Spoof the creation of life in the classroom by putting the necessary ingredients in a tank, add UV light and lightening, and voila. |
8A80.95 |
Life on Other Planets |
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Searching for life on other planets. What to look for. See The Physics Teacher - TPT 20(2), 90 |