|  Newtonian Gravitation | 
Theory
  > s.a. equivalence principle; models of spacetime structure.
  * Idea: Bodies interact
    through a gravitational force Fg
    = G mg
    m'g/r2
    acting at a distance, and accelerations are proportional to forces with proportionality constant
    equal to the inertial mass, a = F/mi.
  * Masses: The force is proportional to the
    gravitational masses, but as Newton knew mg
    ∝ mi, which makes gravitation similar to
    "inertial" forces, in that the acceleration is independent of each body's
    individual characteristics.
  * Potential: If we define Φ(r)
    = U(r)/r for a test body, then the potential Φ satisfies the Poisson
    equation ∇2Φ = 4πGρ,
Φ(r) = −G ∫ dM |r−r'|−1 = −GM/r − G D · r/r3 − \(1\over2\)G Qij ri rj / r5 + ... ,
    where D = ∫ dM r'
    is the dipole moment of the mass distribution (always zero with respect to the center of mass),
    and Qij = ∫
    dM [3 ri'rj' −
    r' 2 δij]
    the quadrupole moment (vanishes for a spherical mass distribution).
  * Potential energy: For an
    extended body in an external field, U = ∫
    ρ(r) Φ(r)
    d3r; The self-energy is
Uself = \(1\over2\)∫ ρ(r) Φ(r) d3r = (1/8πG) ∫ (∇Φ)3 d3r + ∫ ρ(r) Φ(r) d3r .
@ References: Deser AJP(05)aug-gq/04 [from field theory]; Counihan EJP(07) [basic principles]; Yurtsever et al a1004 [inverse problem]; in Ohanian & Ruffini 13; in Poisson & Will 14; Pereira a1903 [from its empirical basis to the theory].
Special Topics > s.a. cosmology;
  gravitational constant; Newton's
  Theorem; teaching [weightlessness, tides].
  * Tidal forces: A mass m located
    at (x, y, z) with respect to a frame centered at a point a
    distance M, feels a tidal force
Fx = −x (GMm/r03) , Fy = −y (GMm/r03) , Fz = 2z (GMm/r03) ;
    In general relativity the expression is more complicated, uses the equation for geodesic deviation.
  * Other formulations:
    A (slightly generalized) geometric version is the Newton-Cartan theory.
  @ N-body problem: Volchan a0803 [Sundman-Weierstraß theorem of total collapse];
    Farrés et al CMDA(13)-a1208 [high-precision symplectic integrators for the Solar System].
  @ Tidal forces:
    Masi AJP(07)feb [compressive radial];
    Efroimsky & Williams CMDA(09)-a0803 [tidal torques];
    > s.a. Love Number.
  @ Other situations:
    Odagaki & Kawai AJP(98)aug [many-particle statistics];
    Beig & Schmidt PRS(03)gq/02 [self-gravitating extended bodies];
    Teixeira phy/03 [infinite straight line of mass];
    Buchert PLA(06)gq/05 [self-gravitating dust];
    Ridgely EJP(11) [in material media].
  @ Other formulations and issues:
    De Pietri et al gq/92,
    CQG(95)gq/94,
    CQG(95)gq/94 [generalization];
    Nardone JPA(98) [regularization];
    Natário GRG(06)gq/04 [initial-value form, and warp drive];
    Hansen et al PRL(19)-a1807 [action principle, gravitational time dilation];
    Banerjee & Mukherjee PRD(18)-a1810 [geometric].
Phenomenology
  > s.a. cosmological models [Newtonian cosmology];
  phenomenology of gravity; modifications
  and tests of newtonian gravity.
  @ Effects: Abramowicz et al GRG(97) [curvature of space and perihelion precession];
    Ferroglia & Fiolhais AJP(20)dec [tidal locking, pedagogical].
  @ Specific objects: Dittrich a1609 [Dirichlet's massive homogeneous ellipsoid].
  @ Measurement: Kulikov JMO(06)qp/05 [transparency of cold atoms];
    Charrière et al PRA(12) [local g measurements];
    Graney PT(12)sep [Giovanni Battista Riccioli];
    Harms LRR(15)-a1507 [terrestrial gravity fluctuations];
    news sn(19)nov [measuring gravity with trapped atoms];
    > s.a. Eötvös Experiment; fifth force.
  > Related topics: see critical
    collapse; Newton's Theorem [shell theorem]; orbits
    in newtonian gravity.
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  send feedback and suggestions to bombelli at olemiss.edu – modified 2 feb 2021