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The linearized-wave approximation regime and an ideal two-body detector with a prescribed finite arm path

Physical scope

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 (M,g,N)=(R4,η,∂0) be the flat model with its inertial chart and let c>0 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 Ω⊆R4 be a nonempty open set and let K⊆Ω be a nonempty compact set. Fix a length scale L>0, and use the numerical threshold δ0=1/16 and chart control functional BK 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 K,L. A linearized-wave datum on K consists of:

The parameter λ is dimensionless, and in the adopted SI length coordinates Sab, Gab(1)(h) and Λhab have units m−2, whereas Tab has energy-density units and κTab has units m−2 (SI unit and coordinate conventions of the classical gravitational framework). The BK and δ0 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, BK, δ0 and CK,L are real control numbers and CK,LBK2/L2 has the residual component unit m−2 for L in metres. The datum is a linearized vacuum wave datum when S=0 and Λ=0. If in addition the perturbation is a TT planar perturbation with amplitudes A+,A× (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

D(λ,K):=max⁡a,b sup⁡p∈K∣Gab(η+λh)(p)+Λ gab(λ)(p)−κ Tab(λ,p)∣,

where G is the Einstein tensor of the exact metric η+λh; this is the residual against the specified exact stress-energy family, not against its first-order coefficient alone. In length coordinates it has units m−2. The datum is within the quadratic approximation when ∣λ∣BK(h)≤δ0. This uses the chosen threshold rather than an unspecified existential δ0/BK(h), and also covers BK(h)=0. 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 J⊆R, a spatial point x0∈R3, and a nonzero spatial vector δ∈R3 with Euclidean norm ∣δ∣>0 (The Euclidean inner product ⟨x,y⟩=∑k<nxkyk on Rn). Require the coordinate tube

AJ,δ:={(cs, x0+qδ):s∈J, q∈[0,1]}

to lie in Ω. For q∈[0,1] define the smooth curves γq:J→Ω by γq(s):=(cs, x0+qδ), and require g(λ) to be Lorentzian on a neighborhood of AJ,δ; the reference worldline is γ0 and the companion worldline is γ1. 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 (x0,δ) is the ideal two-body detector. Its arm direction is eδ:=δ/∣δ∣, the spatial unit vector in the chosen inertial chart.

In SI length coordinates, the components of x0 and δ and the arm length ∣δ∣ are in metres, while eδ is dimensionless.

(c) Finite arm length and strain. For s∈J the prescribed spatial arm path is σs:[0,1]→Ω, σs(q):=γq(s), with tangent σ˙s(q)=δi∂i. Its metric arm length is the metric length of this spacelike coordinate segment,

Lδ(s):=∫01g(λ)σs(q)(σ˙s(q),σ˙s(q)) dq,

whenever the radicand is positive for every q∈[0,1]; the root is the nonnegative square root of Rational powers ar 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 Sδ(s):=Lδ(s)/∣δ∣−1. For a TT linearized-wave datum put

aδ(s,q):=δiδjhij(cs, x0+qδ)∣δ∣2.

Since g0i=0 and gij=δij+λhij, wherever 1+λaδ(s,q)>0 for every q∈[0,1] one has

Lδ(s)=∣δ∣∫011+λaδ(s,q) dq,Sδ(s)=∫011+λaδ(s,q) dq−1.

In the adopted SI length coordinates Lδ has units metres and Sδ is dimensionless.

The first-order strain response is

Sδ(1)(s):=∂λSδ(s)∣λ=0=12∫01aδ(s,q) dq,

which is the parameter derivative of this finite-path length ratio; the response theorem gives a uniform remainder estimate. If δ3=0, the phase u=cs−x03−qδ3 is constant along the arm, so the integrand is constant in q and the formula reduces to the usual single-point TT strain.

(d) Reading and scope. In the TT metric, g(γq′,γq′)=−c2, so s=x0/c 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

Depends on

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