Physic Labs

Newtonian mechanics

Gravity and weight

Measure the attraction between two masses as m₁, m₂, and distance r vary. Verify the law of gravitation F=G m1m2/r2F=G\,m_1m_2/r^2 and follow its effect on the orbit.

Middle school

Equipment

  • 3D model of two attracting bodies and their orbit
  • Mass 1, Mass 2, and Distance sliders
  • Virtual force readout and Pause button

Procedure

  1. Test the inverse-square law

    Hold m₁ = 12, m₂ = 5 and sweep «Distance» through 2, 4, 8. Read the force each time: doubling r quarters F. Quickly plot F against 1/r21/r^2 — the points fall on a straight line, evidence for F∝1/r2F\propto 1/r^2.

  2. Test linearity in each mass

    Hold r = 5, vary «Mass 1» from 1 to 20, then «Mass 2» similarly; record F each step. F is proportional to each mass, giving F=G m1m2/r2F=G\,m_1m_2/r^2 — estimate G from the slope of F versus m1m2/r2m_1m_2/r^2.

  3. Watch the orbit as masses change

    Toggle «Pause» to follow mass 2 orbiting mass 1. Raising m₂ or shrinking r strengthens the pull and curves the path more; note both bodies move about the common center of mass — the point closer to the heavier body.

  4. Relate to weight at Earth's surface

    Predict the free-fall acceleration of a small body near a heavy one: g=GM/R2g=GM/R^2 with R the distance to the center. Check: double the distance and g quarters — which is why weight measured atop a mountain is less than at its base (though the effect is tiny).

Simulation

Experiment history

Newton published the law of universal gravitation in the Principia (1687): every pair of particles attracts with F=Gm1m2/r2F=Gm_1m_2/r^2. The falling-apple legend marks the insight that one force both holds the Moon in orbit and pulls objects down — Newton verified it by comparing the Moon's acceleration with g at Earth's surface. G was too small to measure in a laboratory until 1798, when Henry Cavendish used a torsion balance to «weigh the Earth»: he measured the attraction between lead spheres and inferred Earth's density within about 1% of the modern value. Newton's law predicted planetary orbits superbly; the small precession of Mercury's perihelion was only explained by Einstein's general relativity in 1915.

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