Why does a comet's tail bend away from its path? Released dust keeps the comet's orbital velocity. Sunlight then reduces the inward force on small grains more than on large ones, so their new orbits spread into a curved tail. An ion tail follows a different process driven by the solar wind and magnetic field.
Drag the nucleus around the Sun or change a grain's size. Watch released dust form a three-dimensional fan, then separate months of radiation pressure from millennia of Poynting–Robertson drift.
Interactive modelComet Dust Tails and Radiation Pressure
Radiation pressure / solar gravity0.191
Nucleus–Sun distance1.27AU
Farthest grain from nucleus0.711AU
Circular one-AU PR reference time2090yr
Release history and slow energy loss answer different questions
Ideal orbital-plane offsets from the nucleus
Gold is the synthetic cloud; coloured curves are ideal zero-launch-velocity release families. The orbital-plane axes share one scale.
Read the release families
Gold: teaching cloud. White arrow: antisolar direction, with schematic length. Violet, cyan and pink: zero-launch-velocity synchrones released thirty, sixty-five and one hundred percent of the oldest age ago. Both axes use AU and the same scale; they rotate with the model orbit, not the sky.
Δyorb[AU]
Δxorb[AU]
A different experiment: bound circular PR drift
Bound circular-orbit reference with the physical speed of light. Near-Sun survival is outside this model.
Circular reference assumptions
A hypothetical grain starts on a circular orbit under reduced gravity at one AU. Its radius follows the orbit-averaged law at the physical speed of light; the formal zero-radius endpoint lies outside the near-Sun survival model. This is not the fate of every escaping comet grain.
a(t)[AU]
t[yr]
The observed ISON image belongs to the separate tutorial. Its sectors are measured from real pixels. The synthetic interactive cloud explores release geometry; the tutorial carries out the separate observed-direction comparison.
Physics tutorial
Follow the dust after it leaves the comet
BackgroundDust leaves a comet with almost the same orbital velocity as the nucleus. Solar gravity bends both trajectories; radiation pressure makes the grain's inward acceleration smaller. Different grain sizes and release times spread these trajectories into a tail.
Why it mattersA comet's dust tail records its recent release history and our viewing angle. Its direction can differ from both the antisolar direction and the direction opposite its velocity.
Start with the essentials
Focus question
Which changes come from grain size, release age and projection?
One-sentence intuition
A grain inherits velocity before light changes its acceleration. Reduced inward attraction can produce a wide or escaping orbit without any outward net central force.
Core mathematical model
Size sets the adopted force ratio
β=16πcGM⊙ρs3L⊙Qpr
The stage fixes spherical-grain density at one thousand kilograms per cubic metre and pressure efficiency at one. The inverse-size scaling follows from these assumptions; real material efficiencies can vary with size and wavelength.
Preserve the release velocity
vd=vc+vej,r¨d=−GM⊙(1−β)rd3rd
The nucleus and grain are propagated from the same release event to the same observing time. With zero beta and zero launch velocity they coincide. The cyan reference grain always has zero launch velocity.
Read the slow circular reference
a(t)2=a02−c4βGM⊙t
This orbit-averaged PR relation describes a bound, initially circular reference at one AU with physical light speed. Escaping comet grains can have a different future. The stage treats neutral dust with central pressure, and the separate curve treats this defined bound PR reference.
Common difficulties
Separating from the nucleus does not require outward force
Typical misconceptionIf dust falls behind or outside the nucleus, sunlight must exceed gravity.
Better mental modelBoth objects can accelerate inward at different rates. An inherited velocity also allows escape under an inward force. Check release energy as well as beta.
A curve match can have several histories
Typical misconceptionMatching one projected ridge uniquely gives its grain age and size.
Better mental modelDifferent release ages and sizes can project almost together. The real-image tutorial shows actual overlapping alternatives; brightness and additional epochs would add information.
Run the experiment
01
Change one reference grain
Pause and drag the cyan grain. Predict whether a smaller radius increases or decreases the separation before checking beta.
What to observe: A smaller grain has a larger force ratio under the adopted material assumptions. Its inherited motion bends less sharply inward.
02
Separate age from size
Compare the one-burst and one-size presets. Then increase the launch-speed scale and rotate the camera.
What to observe: Release history changes the family curve; launch velocities give the dust real depth. The lower colored synchrones omit launch velocities for comparison.
03
Test the zero-force limit and the two clocks
Choose the zero-force preset, reset, then compare the fan with the circular PR reference's year axis.
What to observe: With no pressure or launch velocity the grains coincide with the nucleus. Restoring physical pressure makes a tail in months; the separate PR circular clock spans far longer times.
Related experiments and articles
Sunlight shapes comet dust tails · Reading path
Sunlight shapes comet dust tails
Articles on this path that use this experiment, followed by the other experiments they suggest.