Take as particle proper time, dots as , and with . In the equatorial plane the geodesic Lagrangian is
The cyclic coordinates give and . Set the resulting constants to and respectively. The explicit second-order equations are
The polar equation is satisfied by , , consistently with spherical symmetry. The proper-time normalization supplies the third first integral:
The normalization is ; it is distinct from choosing an arbitrary affine tangent's norm.
Stationarity and axial symmetry make the covariant time and azimuthal momenta constant. For physical momentum and coordinate in seconds, and . Thus is the conserved energy normalized at infinity and is the signed axial angular momentum. This is Killing energy with positive time signature; a convention with negative timelike norm uses the opposite contraction sign. The supplied covariant-momentum form of the geodesic equation makes these cyclic constants immediate, but its parametrization must be understood: for it is exactly as written. For physical , proper-time differentiation instead gives ; equivalently, the displayed mass-free form uses . This affine momentum normalization does not change either conservation law.
Multiply the normalization equation by and substitute the two cyclic integrals. Rearrangement gives the radial energy equation
For radial marginal escape and the future-directed constant is , because the speed at infinity vanishes. Choose the outward root:
Hence the marginal escape geodesic in Schwarzschild spacetime has
The constant has units of length to the power divided by time. This radius is an areal coordinate, not accumulated local proper distance.
A Schwarzschild static observer at exterior radius uses local radial rulers and a local clock . Therefore the local radial speed of a Schwarzschild geodesic is
For the marginal trajectory this gives
Its equality to is particular to ; the local definition, rather than that accidental equality, is the required observer measurement. The Schwarzschild-coordinate velocity is instead .
For nonzero asymptotic speed , the same energy constant is . Combining the radial equation with the local-ruler relation gives radial Schwarzschild escape with asymptotic speed
The positive root describes the outward particle, at radii on its trajectory with . Independently, a static observer has four-velocity in these coordinates, giving relative Lorentz factor and the same speed. As it tends to ; for it gives the preceding result. Its limiting value approaches as , but that is a limit through exterior observers: no static timelike observer exists on or inside the horizon.
Figure 1.
Original comparison of local static-observer and Schwarzschild-coordinate radial speeds, for illustrative asymptotic speeds
. Details.
Nearby freely falling particles can accelerate relative to one another even though each follows a geodesic. A local inertial frame removes the common gravitational acceleration at one event; it cannot remove the variation across an extended laboratory. That variation is a tidal force, measured covariantly by geodesic deviation.
Let be the reference four-velocity and an infinitesimal separation to a neighboring geodesic, with matching affine parameters. With the convention ,
This relates measured relative acceleration to the Riemann curvature tensor. Reversing the curvature-tensor convention reverses the displayed curvature sign, without changing the physical relative motion.
In a small freely falling frame outside a spherical mass, the weak-field tidal tensor has radial and transverse components proportional to . Thus
An initially spherical cloud stretches radially and compresses in both transverse directions. Two separated test masses, with their changing separation measured by light, form the basic idea of a gravity gradiometer; the common falling motion drops out. A uniform apparent acceleration in an accelerated laboratory can occur even in flat Minkowski spacetime, so it is the separation-dependent tidal response that diagnoses curvature.
Figure 1.
Radial stretching and transverse compression from geodesic deviation
. Original local schematic of the weak-field tidal tensor around a freely falling reference particle. Arrows show relative acceleration, with radial direction horizontal; the cloud deformation is exaggerated and is not a trajectory calculation. Details.
Let denote coordinate acceleration and use for four-acceleration, to distinguish these two objects. Applying the chain rule to the Lorentz factor gives
Since , differentiation of the four-velocity with respect to proper time yields
This is also , as required.
The invariant Minkowski norm of the four-velocity is . Differentiating this identity gives . In the instantaneous rest frame, , so and the spatial components equal the physically experienced proper acceleration . Therefore in the metric signature.
For a direct calculation, put and expand the temporal and spatial squares:
The last step uses . This proper acceleration from coordinate velocity and acceleration also reads , providing the familiar one-dimensional limit . Each expression has units .
Local equivalence and tides. In Newtonian mechanics, inertial mass measures the response to a force, whereas passive gravitational mass couples to an imposed Newtonian gravitational field. A freely falling body obeys
The observed composition independence of free fall says that this ratio is universal. With a common choice of units it is one. This is the Newtonian content of the weak equivalence principle for test particles; it does not by itself specify all nongravitational physics.
The Einstein equivalence principle further says that local nongravitational experiments in a sufficiently small freely falling laboratory have the form predicted by special relativity, independently of the laboratory's location and motion. In such a local inertial frame, the metric tensor is locally the Minkowski metric and the Christoffel symbols vanish at the selected event. The strong equivalence principle extends the universality claim to local gravitational experiments and bodies with significant gravitational self-energy. None of these statements removes measurable tidal forces across a finite apparatus.
In an ideal small freely falling lift, a released ball initially floats relative to the cabin, because both undergo the same free fall. Two separated balls, however, need not retain their separation: they sample different parts of the gravitational field. For a point source, linearizing across a small separation gives the tidal tensor prediction
A radial separation stretches with coefficient , whereas a transverse separation is compressed with coefficient . Initially parallel velocities therefore develop relative motion even though the individual bodies experience zero proper acceleration.
The relativistic statement is geodesic deviation. With the Riemann curvature tensor convention
a connecting vector between neighboring freely falling worldlines satisfies
Here is the covariant derivative along the reference geodesic, and its four-velocity. Curvature can be nonzero where the Christoffel symbols have been made zero. In the weak, static, slow-motion limit this equation reduces to , recovering the tidal tensor above. A finite falling lift can detect gravity through these relative accelerations; local equivalence does not imply a globally uniform field.
Weak-field connection and potential. Take and the metric signature. There is an index error in the printed formula for the Christoffel symbols: its first differentiated metric component must be , not . The correctly contracted expression is
The offending term vanishes under the stipulated time independence, so this correction does not change the intended calculation. Write and treat both and its derivatives as first order. To that order , , and . A stationary metric tensor gives
For the temporal component the inverse-metric coefficient is already first order, so
For a spatial component the zeroth-order inverse metric contributes:
The time component of the approximate geodesic equation says that is constant to the retained order. In its spatial component, convert the proper time derivatives to coordinate-time derivatives and cancel :
Comparison with the Newtonian equation identifies . For an isolated source, choose the gravitational potential to tend to zero at infinity and normalize the time coordinate there, giving . Thus
The quantity is the Newtonian gravitational potential, or gravitational potential energy per unit mass, in . For a point source, . A static clock has , connecting the Newtonian limit with gravitational time dilation.
Frequency of the orbiting source. Treat the gas blob as a test particle on a timelike circular Schwarzschild geodesic, with pressure and other nongravitational forces negligible. Treat our very distant location as infinity, so the observer's own gravitational potential is negligible. These are the assumptions that make a unique answer in terms of possible.
Put and use a local static observer at the emission point as an intermediate measuring frame. The remote observer lies on the symmetry axis of the orbit. A ray arriving on that axis has zero conserved axial angular momentum, so its local direction is perpendicular to the emitter's azimuthal velocity. Bending within a meridional plane does not alter this orthogonality. The transverse relativistic Doppler effect therefore gives
where is the orbital speed measured by that local static observer. The gravitational redshift between static Schwarzschild observers then gives
A gravitational circular orbit has in the weak-field limit, so . Expanding both factors,
Solving for the emitted frequency gives
The gravitational part is and the transverse kinematic time dilation contributes another ; the absence of line-of-sight motion does not remove this second effect.
As an exact check, the local speed on a timelike circular Schwarzschild geodesic satisfies , where . Therefore the face-on frequency shift of a circular Schwarzschild source is
whose expansion agrees with the boxed answer. If the gas is supported or accelerated by pressure or magnetic stresses rather than following a geodesic, its orbital speed is not fixed by the mass and radius alone; the appropriate first-order result is instead , with supplied independently.
For motion along one spatial axis, introduce the rapidity so that the four-velocity is . Its four-acceleration is
A constant signed proper acceleration therefore gives , hence . Differentiating the four-velocity twice yields
The zero transverse components also satisfy this equation. The constant acceleration measured on board is the proper acceleration, rather than a constant coordinate acceleration in the laboratory.
Use signature and local inertial coordinates . Write and , where is rest mass density. The perfect fluid in general relativity has components
Here is energy density, is energy flux, is momentum density, and is the flux of the th momentum component through a surface normal to . In the local rest frame these reduce to energy density , zero energy and momentum flow, and isotropic pressure . The equation expresses local stress-energy conservation. Its temporal and spatial components give energy and momentum balance; in flat coordinates, for example, .
For relativistic dust, . Contracting its divergence with , and using metric compatibility together with , gives
Consequently . Substituting this continuity equation back into the divergence leaves . Wherever matter is present,
so the individual particles follow geodesics.
The electromagnetic four-force law must preserve the particle's rest mass. Thus , and requiring this for arbitrary timelike four-velocities makes the electromagnetic field tensor antisymmetric. Its six independent components comprise the electric field and magnetic field. With the stated signature and , one consistent convention is
It gives the spatial force and energy transfer . Under a Lorentz transformation, transforms as a rank-two contravariant tensor; its electric and magnetic components consequently mix. A four-potential supplies , unchanged by . The Maxwell equations are
These combine the source equations and the homogeneous equations into covariant tensor statements; is the four-current.
For charged relativistic dust, the matter tensor exchanges four-momentum with the electromagnetic field: , while their total stress-energy tensor is conserved. Identical particles of rest mass and electric charge have . Contraction with again gives mass continuity because . Removing that term gives
Using zero divergence for the matter tensor alone in this last step would omit the electromagnetic Lorentz force.
Write , with . On the equatorial plane, the geodesic Lagrangian is
The coordinates and are cyclic, giving . The conserved physical energy per unit rest mass is , while is the signed angular momentum per unit rest mass. The radial Euler-Lagrange equation, with , is
These are the requested geodesic equations. The equatorial condition is consistent with the polar equation by the spherical symmetry of the Schwarzschild metric.
The normalization of the four-velocity is . Insert the two conserved quantities and multiply by to obtain
This is a one-dimensional radial energy equation. Half of its left side is radial kinetic energy per unit mass plus an effective potential: the Newtonian centrifugal and gravitational terms acquire the extra attractive contribution .
A timelike circular Schwarzschild geodesic requires . Equivalently, set the derivative of to zero. At this gives , and substitution in the radial energy equation yields
Such timelike circular orbits require . Their coordinate angular velocity satisfies , and their proper clock rate is .
For the static North-Pole clock, . Consecutive overhead passages occur one coordinate orbital period apart, and the repeated Earth-satellite geometry gives equal signal travel delays. The comparison of circular-orbit and static Schwarzschild clocks therefore gives
This includes both gravitational and orbital-motion effects; a separate Newtonian time-dilation correction must not be added again.
For an estimate, Kepler's third law gives . The same approximate geostationary radius and period give . Expanding the ratio to first order,
The satellite clock consequently gains about over a three-hour orbit in this approximation. The surface observer is taken to be static, and the spacetime model is the spherical Schwarzschild metric specified in the problem.
For rest mass and electric charge , the generally covariant Lorentz force law is
Here is the electromagnetic field tensor for the chosen electromagnetic four-potential normalization, and the covariant derivative includes the spacetime Levi-Civita connection. Antisymmetry of ensures , preserving the four-velocity norm and the particle's rest mass. An uncharged particle follows a geodesic.
An affine geodesic has constant squared tangent norm, but that constant depends on the scale of its parameter. Write
Using in the line element gives
The affine normalization in a Kaluza-Klein geodesic reduction matters: the specific formula requested in the paper uses , namely equal to the positive five-dimensional arclength. With that normalization,
A timelike four-dimensional projection has , requiring in this normalization. At the projection is null and has no proper-time four-velocity. For an arbitrary affine parameter the first boxed relation, with retained, is the general result.
For coordinates the inverse metric is , . Only is nonzero, giving the Christoffel symbols
with all remaining components zero.
On the specified constant- worldline, assume . The four-velocity is , , and its norm is , so is indeed proper time. The coordinate components are constant, but the covariant acceleration is nonzero:
The proper acceleration of a static Rindler observer is
The acceleration has constant components in this accelerated chart and constant invariant magnitude. It is not a covariantly constant vector: its inertial-frame components change along the hyperbolic trajectory. For , the magnitude is , with the appropriate choice of future time orientation.
A fundamental observer follows the coarse-grained cosmological matter, with fixed comoving coordinates. The cosmological principle asserts spatial homogeneity and cosmological isotropy on large scales for this family of observers. A moving observer generally sees a preferred direction, for example a Doppler dipole in the cosmic microwave background, even when the underlying cosmology is isotropic.
In an FLRW metric, these worldlines are orthogonal to homogeneous spatial slices. Synchronize their clocks to define cosmic time , which is their proper time. Along a fixed spatial label, , giving . Orthogonality of the spatial coordinate directions to the observers' four-velocity gives . Thus, in the metric signature,
where the spatial matrix is negative definite. Spatial homogeneity and cosmological isotropy further restrict it to , with a constant-curvature spatial metric.
For radial motion, use the geodesic Lagrangian
The Euler-Lagrange equation for gives . Since is a cyclic coordinate, its conjugate momentum is constant. Hence
For a massive particle, take as proper time; the four-velocity normalization is . For a photon, use an affine parameter rather than proper time, and the corresponding tangent is a null vector. Therefore
The normalization of the null affine parameter remains arbitrary.
At any event on a massive observer's worldline, choose an orthonormal tetrad with timelike basis vector . Its components obey , so locally : the Minkowski metric. A local inertial frame can also remove the Christoffel symbols at that event. Curvature cannot be removed on a finite region, and a frame following an accelerated observer need not remain inertial in its neighbourhood.
In general coordinates, labels the trajectory, while the four-velocity and four-acceleration are
Coordinate values are not themselves a vector under arbitrary nonlinear coordinate changes; their tangent is. For fixed rest mass , the four-momentum is and the four-force is . With the metric signature,
where is the proper acceleration. The middle identity follows by differentiating the constant velocity norm; in the instantaneous rest frame, and , proving the last identity.
The proper time normalization of the astronaut's four-velocity gives . In the light-cone coordinates this is
The four-acceleration has squared norm , because is the constant proper acceleration. The same coordinate change therefore gives
Equivalently write , . Their second derivatives give , so the rapidity form of one-dimensional proper acceleration makes , with sign fixing the acceleration direction.
Differentiate each segment and express the four-velocity using a continuous rapidity:
At both rapidities are ; at both are . Hence the four-velocity is continuous at both junctions. This expression also gives everywhere, so the parameter remains proper time on the later segments.
Away from the junctions,
with successively . The rapidity is continuous but its slope reverses. Thus the four-acceleration has a finite jump to its negative at each junction, while its magnitude stays on either side. There is no velocity jump; the idealized path is continuously differentiable but not twice differentiable at the switching events.
Take spacetime coordinates . Differentiating the initial segment gives the four-velocity
The identity gives , and . The proper time element therefore satisfies , with the future orientation selecting . Thus is proper time along this path.
Use the metric and four-velocity . Its derivative with respect to proper time is the four-acceleration. Since
a purely transverse laboratory acceleration has . With ,
The invariant proper acceleration is the magnitude measured in the instantaneous rest frame, . Consequently,
For longitudinal acceleration the factor is instead multiplying the laboratory acceleration. The distinction matters for circular storage-ring motion, where the acceleration is centripetal and transverse even though its magnitude is nonzero.
Regard as a scalar field evaluated on a specified worldline . The ordinary multivariable chain rule gives
This is the directional derivative along the four-velocity. With , it reads . The spatial term is present because the worldline moves through the field; it would be lost by identifying a total derivative along the particle with a partial derivative at a fixed spatial position. For a scalar the contracted expression has the same value in all coordinate systems. For a tensor field the analogous covariant derivative also transports its indices.
Use and a constant Minkowski metric. Vary the velocity-dependent square root before imposing the proper-time normalization. Equivalently, vary a reparametrization-invariant worldline action first and then choose proper time. Its canonical covector momentum is
The coordinate derivative at fixed velocity is . The Euler-Lagrange equation and the chain rule from a therefore give
Define the antisymmetric field tensor by
The particle equation becomes
Antisymmetry ensures , so the force is orthogonal to the four-velocity and preserves . The worldline variation before proper-time normalization is essential: substituting into the Lagrangian before taking its velocity derivative would turn the kinetic term into a constant and incorrectly remove the inertial momentum. The normalization is a property of the proper-time solution, not permission to discard the variational dependence.
Take the kaon decay as the common origin. A pion traveling freely with constant momentum has lab decay time and position . The supplied proper survival times therefore give
Consequently the separation from the first decay event to the second is
The requested distance is the separation of the two events, not the sum of the two individual pion path lengths.
Here , so the separation is a spacelike separation. There is an inertial frame in which the events are simultaneous; in that frame their distance equals the invariant spacelike length:
One such frame moves along with , of speed . The simultaneity condition is then .
The spacelike distance between daughter decay events provides an independent invariant check: the daughter four-velocity contraction gives
It produces the same distance without using the particular kaon laboratory boost. A simultaneous frame exists only when this expression is positive, as it is for these two survival times.