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The linearized-wave approximation regime and an ideal two-body detector with a prescribed finite arm path
Modelling definitions inside the classical gravitational framework: the class of flat linearized-wave data with an explicitly scaled smooth stress-energy family and a fixed quadratic threshold, and an ideal detector consisting of two freely falling test-body worldlines plus the metric length of their prescribed chart-straight spatial arm at equal chart time. The arm length is path-dependent and is not asserted to be the shortest spatial distance between its endpoints. The definitions exclude rigid bodies, elasticity, internal resonances, noise, light propagation, readout and any measured signal, and assert no observation and no property of any laboratory apparatus.
Definition
Let be the flat model with its inertial chart and let be the parameter of SI unit and coordinate conventions of the classical gravitational framework. All objects below are component families in this chart.
(a) Linearized-wave datum. Let be a nonempty open set and let be a nonempty compact set. Fix a length scale , and use the numerical threshold and chart control functional defined in Linearized field equations as the first-order consequence of the adopted field law, with the harmonic-gauge wave reduction and the quadratic residual control clause (d) for this . A linearized-wave datum on consists of:
- a flat linearized family over with perturbation (Flat linearized perturbations: families, trace reversal, gauge transformation and harmonic gauge) such that in the chart control functional of that clause;
- the real cosmological parameter and a smooth family of stress-energy tensor fields on for , with component fields smooth jointly in (Stress-energy tensor field of a model);
- the zeroth-order compatibility condition , where ; define the linearized source field, with curvature units, by , and require in the sense of Plane-wave perturbations of the flat linearization: planar profiles, wave covectors, amplitudes, TT form and the linearized field equations clause (e);
- a nonzero real amplitude with for which is a Lorentzian metric of signature on a neighborhood of .
The parameter is dimensionless, and in the adopted SI length coordinates , and have units , whereas has energy-density units and has units (SI unit and coordinate conventions of the classical gravitational framework). The and values in the chart Taylor estimate are numerical controls: evaluate component functions and their coordinate derivatives as SI numerical values in this fixed length-coordinate chart, then form the displayed real-valued functional. It is not a physical observable or an intrinsic norm. In this fixed numerical convention, , and are real control numbers and has the residual component unit for in metres. The datum is a linearized vacuum wave datum when and . If in addition the perturbation is a TT planar perturbation with amplitudes (Plane-wave perturbations of the flat linearization: planar profiles, wave covectors, amplitudes, TT form and the linearized field equations clause (b)), the datum is a TT linearized-wave datum. Its approximation defect is
where is the Einstein tensor of the exact metric ; this is the residual against the specified exact stress-energy family, not against its first-order coefficient alone. In length coordinates it has units . The datum is within the quadratic approximation when . This uses the chosen threshold rather than an unspecified existential , and also covers . Whether a datum satisfies any of these conditions is a property of the given data; this definition names the data, the condition and the defect and asserts neither existence nor a bound.
(b) Ideal two-body detector. Let a TT linearized-wave datum be given. Choose a nonempty open interval , a spatial point , and a nonzero spatial vector with Euclidean norm (The Euclidean inner product on ). Require the coordinate tube
to lie in . For define the smooth curves by , and require to be Lorentzian on a neighborhood of ; the reference worldline is and the companion worldline is . Whenever these endpoint curves are the ideal freely falling worldlines assigned by the postulate of Adopted clock, free-fall and light-ray assumptions of the classical gravitational framework, their pair with is the ideal two-body detector. Its arm direction is , the spatial unit vector in the chosen inertial chart.
In SI length coordinates, the components of and and the arm length are in metres, while is dimensionless.
(c) Finite arm length and strain. For the prescribed spatial arm path is , , with tangent . Its metric arm length is the metric length of this spacelike coordinate segment,
whenever the radicand is positive for every ; the root is the nonnegative square root of Rational powers of a positive base. This is the length along the prescribed chart-straight path, not the infimum over spatial paths and not a tangent-vector norm between finite-separated endpoints. The strain function is . For a TT linearized-wave datum put
Since and , wherever for every one has
In the adopted SI length coordinates has units metres and is dimensionless.
The first-order strain response is
which is the parameter derivative of this finite-path length ratio; the response theorem gives a uniform remainder estimate. If , the phase is constant along the arm, so the integrand is constant in and the formula reduces to the usual single-point TT strain.
(d) Reading and scope. In the TT metric, , so is proper time along each endpoint curve; their geodesic and free-fall properties are established in the response theorem of this page. The detector is the two ideal endpoint bodies plus the defined path length along a chosen coordinate segment at equal inertial-chart time; the length depends on the chosen path and chart and is not asserted to be a geodesic distance. Rigid bodies, elasticity, internal resonances, the propagation and readout of light, noise and calibration are outside this definition; no reading of a real apparatus is defined here, and no fact about nature is asserted.
Remarks
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Why the regime conditions are separate from the detector. Clause (a) packages the approximation hypotheses — a linearized family, a length scale, a source and parameter, a compact set and an amplitude — so that later theorems can quantify the approximation defect and the response without repeating them. When and the specified family satisfies identically, the quadratic residual bound is the content of Linearized field equations as the first-order consequence of the adopted field law, with the harmonic-gauge wave reduction and the quadratic residual control clause (d) and TT plane waves with arbitrary bounded profiles solve the linearized vacuum equations, are in harmonic gauge, and give Lorentzian small-amplitude metrics with a quadratic Einstein-tensor residual clause (c). Merely having allows higher-order terms in , for which no residual bound is asserted here; the definition itself only names the defect.
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Simultaneity and the arm path are chart-defined. The length is the metric length along the prescribed coordinate segment at equal inertial-chart time . It is not an intrinsic shortest distance between the endpoints or a statement about how any apparatus records a duration or length; its path and frame dependence are part of the model definition.
Depends on
Plane-wave perturbations of the flat linearization: planar profiles, wave covectors, amplitudes, TT form and the linearized field equations
The wave screen of an observer and propagation direction, and the transverse-traceless projection of a symmetric two-tensor
Flat linearized perturbations: families, trace reversal, gauge transformation and harmonic gauge
The flat model spacetime: the Minkowski metric on R^4 and its inertial chart
Smooth covariant 2-tensor fields on a smooth manifold
Stress-energy tensor field of a model
Timelike worldlines, proper time, length and four-velocity on a Lorentzian four-manifold
Proper time is well defined and reparametrization invariant; the four-velocity is its proper-time tangent
TT plane waves with arbitrary bounded profiles solve the linearized vacuum equations, are in harmonic gauge, and give Lorentzian small-amplitude metrics with a quadratic Einstein-tensor residual
Linearized field equations as the first-order consequence of the adopted field law, with the harmonic-gauge wave reduction and the quadratic residual control
Adopted clock, free-fall and light-ray assumptions of the classical gravitational framework
Adopted Einstein field equation in the direct-equation presentation
SI unit and coordinate conventions of the classical gravitational framework
The Euclidean inner product on
Rational powers of a positive base
Order on the reals
Squares of nonzero elements are positive
Open cover, subcover, and compact topological space; a compact subset is a subspace that is compact in its own right
Dependency tree · 2 levels
Sources
- S. M. Carroll, Lecture Notes on General Relativity, arXiv:gr-qc/9712019v1 (1997), Ch. 6 (6.58)-(6.66): geodesic deviation of slowly moving test particles in a plane wave and the oscillating separation S_1 = (1 + (1/2) C_+ e^{i k.x}) S_1(0), printed pp. 152-153 (PDF pp. 159-160)
- D. Tong, General Relativity (Cambridge Part III Mathematical Tripos, Michaelmas 2019), sections 5.2.2-5.2.3: the bobbing of neighbouring geodesics in a passing wave, the circle-to-ellipse deformation and the interferometer arm response L' = L(1 +/- H_+/2), printed pp. 212-215 (PDF pp. 219-222)
- H. S. Reall, Part III General Relativity (Cambridge, October 12, 2022 revision), section 7.3: the parallelly transported frame of an observer, the geodesic deviation of nearby test particles and the corresponding changes in separation caused by + and x polarized waves, printed pp. 79-81 (PDF pp. 80-82)