Two perpendicular sliding constraints
Coordinates are in the transverse upward–depth plane, with the input center at the origin.
Spatial mechanisms · Parallel offset
Connect parallel shafts that do not share a center. Inspect the perpendicular tongue-and-groove faces, follow the floating disc around its orbit, and compare constant output speed with changing sliding speed.
Physics tutorial
BackgroundCouplings carry rotation between shafts whose axes do not coincide.
Why it mattersWatch the connecting geometry before reading the speed curve.
Start with the essentials
Coordinates are in the transverse upward–depth plane, with the input center at the origin.
The center orbit has radius half the axis offset; it is not either shaft orbiting.
Travel is signed from the corresponding shaft center along its own groove direction.
No frictional loss or inertial power is included.
Typical misconceptionOne output turn per input turn guarantees constant speed.
Better mental modelA universal joint has a varying instantaneous ratio; an ideal parallel Oldham coupling has a constant ratio.
Typical misconceptionA smooth animation establishes acceptable bearing loads and wear.
Better mental modelInput motion is prescribed, and the connecting parts are massless and frictionless. Dynamic inertia, real clearances and contact forces require a different model.
Select aligned shafts and play one turn.
What to observe: Both shaft phase markers agree and the speed ratio stays unity.Increase the offset and compare the two slide-speed curves.
What to observe: The center goes around twice per input turn. Sliding speeds are in quadrature while shaft speeds stay equal.Reverse the signed load and export the cycle.
What to observe: Torque and power change sign; the prescribed motion does not.Theory & apparatus: Carnegie Mellon · Universal Joint · Ruland · Oldham Coupling