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Before we can measure planets, we work out the basic law of photometry: as the distance from the lamp increases, the detector receives less and less light.
Tools:
Photometer
Lamp
Tape Measure
Procedure:
Measure the irradiance every 10 cm at distances from the lamp: ten readings between 10 and 110 cm
Sketch to explain the quadratic law:
The initial energy is distributed over growing spherical shells of area 4 pi r².
(The circles need to be imagined as spheres.)
Finally, we let the orbit pass around the lamp and measure the light intensity as a function of time. Whenever the orbit passes in front of the lamp, the brightness goes down a little, but does not become zero: a very good analogy to the planetary transit.
Test it!
Around christmas time, some gadget stores sell tiny christmas-trains. With one of them orbitting extremely closely, and with all of its wagons making the “planet” train really big, I simulated a hot Jupiter (or even brown dwarf) in narrow orbit.
Note that battery-powered trains typically do not allow to regulate their speed, except for slowing them down with more load (more waggons/ increased mass – e.g. modelling clay) attached.
Mass Density is a measure of its composition: rock planets have a higher density than gas planets (roughly spoken). We convince ourselves that this principle works by “weighing” some “test planets” with a transparent surface where we can see the inner composition.
With highschool students, we can even compute the density.
With primary school students, we just weigh them and compare the masses of ball with same size.