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A timelike vector field assigns a timelike vector continuously or smoothly to every event in its domain. A globally defined such field gives a time orientation, but it need not be a Killing vector field or a timelike geodesic vector field.
The matrix in time reversal of a Dirac field depends on the convention for the spin-flip phases and on the sign of the spinor identity used when relabeling the mode expansion of a Dirac field. If and , the relabelled coefficient is , giving . A common phase changes but leaves its gamma matrix conjugation property and the induced fermion bilinear transformation unchanged. The antiunitary operator acts on both numerical coefficients and creation or annihilation operators.
A time-ordered product sorts operator insertions from latest time on the left to earliest time on the right. Reordering odd fermionic operators contributes the sign of their permutation. For bosonic , . Vacuum expectations of free time-ordered products are evaluated by the Wick theorem.
For bounded linear operators between Hilbert spaces with and , the operator is coercive and invertible for . The reconstruction uniquely minimizes . Testing its normal equation for coercive Tikhonov regularization by gives . If is injective, exact-data consistency and , give norm convergence to .
For a bounded linear operator between Hilbert spaces, the spectral regularization method for quadratic Tikhonov regularization has scalar coefficient . Since , this coefficient is at most . The spectral theorem for normal operators transfers this scalar bound to the operator norm, providing the noise term in the noise-bias decomposition for linear regularization.
The reconstruction operator in Tikhonov regularization has scalar gain . Its maximum over is , so a data perturbation of norm at most changes the solution by at most . A convergent noisy-data parameter choice satisfies and . Fixed-parameter stability is distinct from stability of the unregularized inverse.
For a singular system of a compact operator with , Tikhonov regularization gives , where and the inner product is linear in the first argument. The bounded gain yields a norm-convergent reconstruction; components in are discarded and no component in is introduced.
For a bounded linear operator between Hilbert spaces, a quadratic penalty givesIts first variation in direction is in the real case; use the real part of the pairing in the complex case. Dividing stationarity by two gives . Thus the derivative of the displayed penalty itself is , while its contribution to the normalized normal equation for a linear inverse problem is .
The positive quadratic term makes the objective strongly convex and coercive, yielding a unique minimizer. In a singular system of a compact operator, the data-to-solution coefficient is instead of . Small singular values are suppressed, trading approximation bias against amplification of measurement noise. This is Tikhonov regularization, rather than exact minimization of the residual alone.
For a point-mass companion at separation , subtract the constant and linear terms of its Newtonian gravitational potential in a frame accelerating with the target's center. The leading residual isIt is degree two in spherical harmonics. In a circular orbit with angular frequency , its time-dependent components force at in a frame with no spin; there is also a static component. This is the leading approximation in , and the tidal amplitude may be absorbed into a harmonic-dependent constant.
Differential gravitational acceleration, multiplied by the affected mass, across a spatially extended body. In the linear approximation the acceleration difference is , where is the tidal tensor. Stellar tidal forces limit the domain of a circumplanetary orbit; sufficiently strong ones can produce tidal disruption.
To isolate a tidal force, subtract the gravitational acceleration shared by the body as a whole. Let a reference test particle follow , and let another have position . In a translating accelerated reference frame with parallel, nonrotating axes,for a source point mass, when . Here is its standard gravitational parameter and the last term uses Big O notation. This Taylor expansion removes the common inward pull and keeps the spatial variation. The near side has an excess pull toward the source; the far side has a deficit of inward pull, which is an outward relative acceleration. Both sides can stretch apart while both still accelerate toward the source.[ref]
Chapter 7: The Theory of Gravitation. §7–4, discussion of stronger near-side and weaker far-side attraction
Subtracting common gravitational acceleration reveals radial stretching and transverse squeezing
. Blue arrows show the exact Newtonian gravitational field at several positions near a reference point. Orange arrows show its linear residual, calculated with the tidal tensor. Arrow lengths use separate scales in the two panels; this is a comparison of direction and spatial variation, not two equal-magnitude fields. Details.For a material element of mass , the residual external force in this translating accelerated reference frame is . Actual deformation also depends on elasticity, pressure and self-gravity. A rigid body approximation suppresses deformation but can still have internal forces that resist the tidal force. The point-mass tidal stretching and squeezing pattern describes freely falling, noninteracting test particles, rather than promising the same shape for every solid, star or ocean. A rotating reference frame introduces centrifugal acceleration and Coriolis acceleration, which must be included separately.
Disruption of a self-gravitating body when differential gravitational acceleration across it exceeds its binding acceleration. For a body of radius , mass at distance from a much more massive body , the competing scales are and ; their equality gives , up to geometry and internal-structure factors. The tidal tensor gives the directional differential acceleration. A tidal disruption event near a black hole is a specific astronomical application.
Subtracting the constant and uniform-acceleration terms from the point-mass relative potential gives , with force convention . Its tidal tensor is . This is the leading term for target size small compared with separation.
Tidal dissipation converts mechanical energy associated with a time-varying tidal deformation into heat. It can reduce orbital eccentricity, drive synchronous rotation, and contribute deep planetary heating. A circular orbit with exact synchronous rotation, perpendicular spin axis and no additional forcing has a static tidal deformation in the body's frame and need not sustain substantial tidal heating.
For ,If , its contribution to is . Since , summing over the prime factors proves the bound. Here is Dirichlet convolution and is the Von Mangoldt function.
The Euler product and Mertens second theorem give . The log-weighted convolution bound for three to the prime omega, with the Chebyshev estimate , then gives . A direct bound for the full range follows from , where :
For the three-to-one spatially forced amplitude equation with forcing , put . The real phase constant belongs inside the factor of . If and the phase has been chosen so that , the scaling , gives the displayed canonical amplitude equation, with and . A negative cubic saturation coefficient cannot give the same cubic sign under a forward-time normalization; zero forcing or zero cubic coefficient requires another scaling.
The canonical three-to-one spatially forced amplitude equation has nonzero equilibrium points satisfying and . Thus . Each positive amplitude has three phases separated by : two amplitude branches normally mean six complex equilibrium points. For the larger branch is asymptotically stable and the smaller consists of saddle equilibria, except that its zero-amplitude root at is not a nonzero equilibrium point. Equality gives a saddle-node bifurcation. This phase locking breaks continuous translation symmetry down to threefold symmetry.
For small positive forcing-frame frequency , use , and in the three-to-one spatially forced amplitude equation. The leading system is . Writing gives the Hamiltonian system and the displayed first integral. The origin is a center equilibrium; three saddle equilibria at and lie on . The factorization reveals a triangular heteroclinic cycle, containing closed periodic orbits for every .
Every triple of subspaces is a direct sum of one-dimensional membership blocks and two-dimensional three-line blocks. Split off the triple intersection, then the pairwise intersections using projections killing the third subspace. Next split complements to , using projections killing the other two subspaces. The remaining subspaces are pairwise disjoint and each lies in the sum of the other two. Their sum is , with the graph of an isomorphism . A graph basis splits this into two-dimensional blocks. A complement to the total span supplies zero-membership blocks. This elementary argument classifies the three-subspace quiver.
For a compact oriented three-manifold, the integral relative class has norm the minimum of over properly embedded oriented topological surfaces representing . Homogeneity and continuity extend it to real relative homology. It is a seminorm, since spheres, disks, annuli and tori have zero cost.
Pinned article: Introduction to the OurBigBook Project
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Intro to OurBigBook
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