Starter track
Step 1 of 50 / 5 completeGravity and Orbits
Next after this: Gravitational Potential and Potential Energy.
This concept is the track start.
Concept module
See how one source mass creates an inward gravitational field, how source mass and distance set the field strength, and how a probe mass turns that field into force without changing the field itself.
Interactive lab
Loading the live simulation bench.
Progress
Not startedMastery: NewLocal-firstStart exploring and Open Model Lab will keep this concept's progress on this browser first. Challenge mode has 2 compact tasks ready. No finished quick test, solved challenge, or completion mark is saved yet.
Try this setup
Jump to a named bench state or copy the one you are looking at now. Shared links reopen the same controls, graph, overlays, and compare context.
Saved setups
Premium keeps named exact-state study setups in your account while stable concept links stay public below.
Checking saved setup access.
This concept can keep using stable links while the saved-setups capability resolves for this browser.
Copy current setup
Stable concept and section links stay public below while exact-state setup sharing stays behind premium.
Stable links
Starter track
Step 1 of 50 / 5 completeNext after this: Gravitational Potential and Potential Energy.
This concept is the track start.
Why it behaves this way
A gravitational field tells you what one kilogram of probe mass would feel at a point before you imagine any actual probe there. In this bounded lab, one source mass sits at the origin, the field always points inward toward that mass, and the size of the field follows the inverse-square distance trend.
The same source mass, probe position, and probe mass drive the stage arrows, scan graphs, compare mode, prediction prompts, worked examples, challenge checks, and quick test. That keeps field direction, field strength, and force on a test mass attached to one honest live model instead of drifting into separate rules.
Key ideas
Frozen walkthrough
Premium unlocks saved study tools, exact-state sharing, and the richer review surfaces that support this guided flow.
View plans2 kg
1.6 m
1.2 m
1. Measure the live source-to-probe distance
2. Apply the one-mass field relation
3. Resolve the current field components
Gravitational field
Inverse-square checkpoint
Make a prediction before you reveal the next step.
Check your reasoning against the live bench.
Common misconception
A heavier probe mass makes the gravitational field at that point stronger.
The gravitational field at a point is set by the source mass and the source-to-probe distance. The probe mass is only responding to that field.
Making the probe mass larger increases the force because F = m_test g, but the inward field arrow and the field graph stay the same until you change the source mass or the probe position.
Quick test
Reasoning
Question 1 of 4
Use the live bench to test the result before moving on.
Accessibility
The simulation shows one source mass fixed at the origin, a movable probe mass in a bounded two-dimensional field region, and optional overlays for a coarse field grid, the live field arrow at the probe, the force arrow on the probe mass, equal-distance rings, and the horizontal scan line used by the graphs.
Dragging the probe changes the sampled field location directly on the stage. The focused probe handle also responds to arrow keys for small position changes, and sliders provide the same controls for source mass, probe position, and probe mass.
Very near the source mass, the field display uses a minimum sampling radius so the drawn arrows and response graphs stay finite and readable. This keeps the visualization bounded while preserving the correct trend that gravitational field strength grows rapidly near the source.
Graph summary
The field-components graph plots the horizontal and vertical gravitational field components along the current horizontal scan line. Hovering the graph previews the same x-location on the stage.
The strength-response graph plots the field magnitude and the probe-force magnitude along that same scan line. Changing the probe mass rescales the force curve, but the field curve remains a source-mass and distance readout.
Bridge this into orbits
Open the next concept, route, or track only when you want the current model to widen into a larger branch.
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.
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.
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.