Choose positions in one inertial frame and let . The centre of mass and two-particle relative coordinate are
The lighter body is farther from the centre of mass. Reconstructing both positions from these equations is part of solving the two-body problem; alone describes their separation, not either body's laboratory position.[ref]
Figure 1. . Original illustrative free two-mass spring model, with , equilibrium separation , relative extension , , and . The right plot subtracts both the translating centre of mass and each body's equilibrium offset. It shows internal displacements, not full distances from the centre of mass. Details.
Substitute the reconstructed velocities into the kinetic energy. The result is the exact two-particle instance of kinetic-energy decomposition about the centre of mass:
The mixed dot product has coefficient ; the coefficient of is . This algebra needs constant positive masses but no particular force law. In the stationary centre of mass frame, the fraction of internal kinetic energy carried by body 1 is , and by body 2 is : the lighter body carries more.
For a closed pair with no external forces, write for the force on body 2 and for that on body 1, as required by Newton's third law. Adding and subtracting their Newton's second law equations yields
Thus the centre of mass moves uniformly while the two-particle relative coordinate behaves like one body of reduced mass. Equal-opposite internal forces suffice for these equations. For an internal central force, with , the internal torque vanishes and conservation of angular momentum gives constant . If the central force comes from a time-independent potential energy , then and the internal mechanical energy is conserved. The kinetic energy split alone does not establish either conservation law.
Two-stage rocket with proportional fuel and body masses Created 2026-10-05 Updated 2026-10-06
For zero initial velocity, body masses and fuel masses , the rocket equation gives the displayed final second-stage speed after burning the first-stage fuel, discarding its body without impulse, and burning the second-stage fuel. It assumes and . The speed exceeds the single-stage value when and fuel is positive. Its limit as concerns a surviving second stage of vanishing mass; at no such stage exists.
Underdamping 2026-10-14
For , define the damped angular frequency . The initial value problem has solution
Every nonzero underdamped response crosses equilibrium repeatedly. Its oscillation period is , not . The amplitude envelope decays as , but the actual displacement also changes sign. The envelope coefficient need not equal : initial velocity fixes the oscillation phase as well as that coefficient.
Uniform flow 2026-10-13
A uniform flow has the same velocity at every position. A constant velocity field has zero divergence and zero vorticity; a velocity potential is . It describes the remote ambient flow in idealized obstacle and line vortex problems.
Unsteady Prandtl equation Created 2026-10-06 Updated 2026-10-14
The unsteady form of the Prandtl boundary-layer equation evolves the tangential boundary-layer velocity under advection, outer pressure forcing and normal viscous diffusion. Incompressibility supplies the normal velocity. A stationary wall imposes the no-slip boundary condition, and tangential velocity matches the prescribed outer slip velocity far from the wall. The normal far-field disturbance need not vanish.
Unsteady Stokes equation 2026-10-14
For variations on a time scale , the ratio of local inertia to viscous resistance is . Steady Stokes flow at each instant requires both and . If only the first is small, retain local acceleration:
For an oscillating sphere with angular frequency , the second condition becomes on the radius scale . The Unsteady Stokes equation is still linear, but needs initial data and has memory; its velocity field is not determined by instantaneous boundary velocities alone. See E. J. Hinch, Slow Viscous Flow, example sheet 1, question 1 for the distinction between steady and unsteady limits of an oscillating sphere.
If the galactic distribution function is not restricted to positive relative energy, isotropic velocity integration gives . The same Abel transform argument as Eddington inversion yields the displayed formula, with lower limit . For , substitution gives . An escape-energy truncation changes both the density law and the velocity tails.
In the free-slip Stokes flow temperature model, let the critical temperature be and vertical velocity , . A forced positive second harmonic couples to the negative critical harmonic. Its temperature solvability condition has integrand
The identity follows by substituting and differentiating. Its integral is zero because vanishes on both plates, regardless of the forced boundary value of . Thus the first resonant forcing coefficient vanishes. A generic nonzero conjugate-amplitude term cannot be inferred from wave-number matching alone.
Variable-mass system Created 2026-10-13 Updated 2026-10-14
A body exchanging mass with material of inertial velocity satisfies the displayed momentum conservation law for one stream, with signed positive for entry and negative for exit. The force excludes the incoming or outgoing momentum flux. A short time interval gives , proving the formula. For stationary incoming matter, ; for matter leaving at the body's own velocity, . The rocket equation and accreting-drop motion are applications.
Vector normalization 2026-10-14
Vector normalization converts a nonzero vector in a normed vector space into a unit vector. Absolute homogeneity of a norm gives
The direction is unchanged by multiplying by a positive real scalar. For , and ; for a negative real scalar, . Thus and normalize to the same unit vector, while normalizes to its negative. This decomposition is useful for specifying a direction independently of a force, velocity or displacement magnitude.
In a complex normed vector space, a nonzero complex scalar instead gives . The remaining complex argument is not removed by normalization. For a pure quantum state, vectors differing only by this overall global phase represent the same physical state; vector normalization alone does not identify them.
Velocity Created 2026-09-24 Updated 2026-10-14
Velocity is the vector giving the rate of change of position with time, measured in a specified reference frame. For a differentiable path , its instantaneous velocity and its average velocity between two times are
The displacement in the numerator retains direction. In Cartesian coordinates, each vector component is a derivative, for example ; its sign tells whether the corresponding coordinate is increasing or decreasing. The SI unit of velocity is . [ref]
For a concrete reversal, let for . Its signed velocity is : at it is , at it is zero, and at it is . The opposite endpoint velocities describe opposite directions, although the endpoint speeds agree. The position moves from to and back to .
Recovering displacement from a measured velocity is an integration problem: , with the integral taken component by component. In the reversal example, : the negative and positive contributions cancel. This distinction is useful in navigation, where the final position depends on direction as well as speed.