Gravity from one source mass
In this bounded lab with displayed units using $G = 1$, the inward gravitational acceleration is set by source mass and radius.
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.
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. At t = 0 s, the satellite is 1.6 m from the source mass. Its speed is 1.58 m/s, while the local circular speed is 1.58 m/s. Gravity supplies 1.56 m/s² inward and the current turn would need 1.56 m/s². The chosen speed matches the circular-orbit condition closely, so gravity keeps turning the path without pulling it inward or letting it drift outward.
Interactive lab
Keep the stage, graph, and immediate control feedback in one working view.
Time
0.00 s / 7.63 sLivePause to inspect a specific moment, then step or scrub through it.Circular Orbits and Orbital Speed
Keep the speed factor at 1.00 to match the circular-orbit condition. Move away from 1.00 to see the same gravity law bend the path inward or let it drift outward.
Graphs
Switch graph views without breaking the live stage and time link.
Radius over time
Compares the live radius with the chosen reference circular-orbit radius over the same time window.
Controls
Adjust the physical parameters and watch the motion respond.
Changes the mass creating the inward gravity.
Sets the dashed reference circle used for the circular-orbit target.
1.00 means the actual speed equals the circular-orbit speed for the chosen mass and radius.
More tools
Secondary controls, alternate presets, and less-used toggles stay nearby without crowding the main bench.
More presets
Presets
Predict -> manipulate -> observe
Keep the active prompt next to the controls so each change has an immediate visible consequence.
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Equation map
Select a symbol to highlight the matching control and the graph or overlay it most directly changes.
Strengthens the inward gravity everywhere, so the circular speed and circular angular speed both rise at the same reference radius.
Equations in play
Choose an equation to sync the active symbol, control highlight, and related graph mapping.
More tools
Detailed noticing prompts, guided overlays, and challenge tasks stay available without taking over the main bench.
What to notice
Use one prompt at a time. The clearest thing to watch changes depending on whether the orbit is close to circular, too slow, too fast, or being compared against another setup.
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Why it matters
Guided overlays
Focus one overlay at a time to see what it represents and what to notice in the live motion.
Overlay focus
Shows the dashed circle for the chosen circular-orbit target.
What to notice
Why it matters
It separates the chosen circular target from the actual path taken when the speed factor is too low or too high.
Challenge mode
Tune one bounded gravity source into orbit-balance targets. The checks read the same live orbit state, overlays, and graphs instead of a detached answer sheet.
2 of 12 checks
Suggested start
The checklist updates from the live simulation state, active graph, overlays, inspect time, and compare setup.
Gravity from one source mass
In this bounded lab with displayed units using $G = 1$, the inward gravitational acceleration is set by source mass and radius.
Turning requirement
Any path with speed v and radius r needs this inward acceleration to keep turning.
Circular-orbit speed
Matching gravity to the turning requirement gives the speed for a stable circular orbit at the chosen radius.
Circular angular speed
The angular speed follows from $\omega = v/r$ once the circular speed is fixed.
Circular period
At larger radius the period grows strongly, while heavier source mass shortens the period.
Progress
Not startedMastery: NewLocal-firstStart exploring and Open Model Lab will keep this concept's progress on this browser first. Challenge mode has 3 compact tasks ready. No finished quick test, solved challenge, or completion mark is saved yet.
Try this setup
Copy the live bench state and reopen this concept with the same controls, graph, overlays, and compare context.
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.
Short explanation
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
Live orbit checks
4 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
Prediction prompt
Check your reasoning
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
Choose one answer to reveal feedback, then test the idea in the live system if a guided example is available.
Accessible description
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
These suggestions come from the concept registry, so the reason label reflects either curated guidance or the fallback progression logic.
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.