Starter track
Step 3 of 50 / 5 completeGravity and Orbits
Earlier steps still set up Circular Orbits and Orbital Speed.
Previous step: Gravitational Potential and Potential Energy.
Concept module
See why a circular orbit needs the right sideways speed, how gravity supplies the centripetal acceleration, and how source mass and radius together set orbital speed and period on one bounded live model.
Interactive lab
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Progress
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Stable links
Starter track
Step 3 of 50 / 5 completeEarlier steps still set up Circular Orbits and Orbital Speed.
Previous step: Gravitational Potential and Potential Energy.
Why it behaves this way
A circular orbit is not a place where gravity turns off. It is a special free-fall case where gravity already points inward and the sideways speed is exactly the value that keeps the radius from shrinking or growing.
This bounded lab keeps one source mass, one chosen reference radius, one speed factor, one live path, and the linked radius, speed, and acceleration-balance graphs on the same state. That makes the orbit condition honest: gravity supplies the centripetal acceleration, and the circular speed changes whenever you change source mass or radius.
Key ideas
Frozen walkthrough
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View plans4 kg
1.6 m
1. Start from the circular-orbit balance
2. Solve for the circular speed
3. Compute the live circular speed
Required circular speed
Orbit-balance checkpoint
Make a prediction before you reveal the next step.
Check your reasoning against the live bench.
Common misconception
A satellite in orbit is floating because gravity is basically absent there.
Orbit still needs gravity. The gravitational pull is the inward acceleration that keeps the path curved instead of straight.
What changes is not whether gravity exists, but whether the sideways speed matches the circular-orbit requirement at that radius.
Quick test
Reasoning
Question 1 of 4
Use the live bench to test the result before moving on.
Accessibility
The simulation shows one fixed source mass at the center of the stage, a moving satellite launched from the right side of a chosen reference radius, and optional overlays for the dashed reference orbit, the live radius line, the tangent velocity vector, the inward gravity vector, and the trajectory trail.
Changing source mass, reference orbit radius, or speed factor updates the same orbit path, live readouts, and linked graphs together. Compare mode overlays a second setup without switching to a separate orbit model.
The displayed units use a bounded one-source gravity model with G = 1. A minimum sample radius keeps the stage and graphs finite and readable while preserving the correct inward and inverse-square trends.
Graph summary
The radius-history graph compares the live radius with the chosen circular reference radius over time. Hovering or scrubbing the graph previews the same instant on the orbit stage.
The speed-history graph compares the live speed with the circular speed required at the current radius, and the acceleration-balance graph compares gravity with the turning requirement v squared over r on that same live path.
Carry the orbit bridge forward
Open the next concept, route, or track only when you want the current model to widen into a larger branch.
Compare circular orbits around one source mass and see why larger orbits take longer: the path is longer, the circular speed is lower, and the same live model makes the period law visible without hiding the gravity-speed link.
Launch outward from one bounded gravity source and see how source mass, launch radius, and total specific energy decide whether the object escapes or eventually returns.
See one source mass create a negative potential well, compare how potential and potential energy change with distance, and connect the downhill slope of phi to the gravitational field on the same live model.