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Tidal Radius, Hills Mass, and Direct Capture

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A close stellar encounter has three qualitatively different outcomes: the star can lose an envelope, be fully disrupted, or cross the relativistic capture boundary before producing escaping debris. The useful organizing comparison is therefore not “tidal radius versus horizon.” It is stellar response versus the spin-, inclination-, and orbit-dependent capture separatrix. This page derives the scale competition and identifies where the Newtonian estimate stops deciding the outcome. Generic stellar dynamics and exact geodesic derivations are outside scope.

Required background. Geodesics and Jacobi Fields supplies the geodesic-deviation and tidal-tensor language used to compare disruption with capture.

Helpful background. Black-Hole Geometry and Mechanics supplies horizon and capture concepts; Relativistic Matter and Compact Objects supplies stellar structure and self-gravity; and Black-Hole Astrophysics supplies the source environment and transient interpretation.

From the tidal tensor to a disruption scale

Section titled “From the tidal tensor to a disruption scale”

Let the black hole have physical mass MBHM_{\rm BH} and the star have mass M∗M_* and radius R∗R_*. Across a star whose size is small compared with its orbital radius rr, the Newtonian potential Φ=−GMBH/r\Phi=-GM_{\rm BH}/r produces the tidal tensor

Cij=−∂i∂jΦ=GMBHr3(−δij+3ninj).C_{ij}=-\partial_i\partial_j\Phi =\frac{GM_{\rm BH}}{r^3} \left(-\delta_{ij}+3n_i n_j\right).

Its radial stretching eigenvalue is 2GMBH/r32GM_{\rm BH}/r^3; order-unity conventions differ according to whether one balances that maximum eigenvalue, a mean force, or an actual stellar response. Equating the characteristic tidal acceleration GMBHR∗/r3GM_{\rm BH}R_*/r^3 with surface self-gravity GM∗/R∗2GM_*/R_*^2 gives

rt=R∗(MBHM∗)1/3.r_t=R_*\left(\frac{M_{\rm BH}}{M_*}\right)^{1/3}.

The cancellation of GG is a useful check: the estimate compares two accelerations governed by the same gravitational coupling. It is also a mean-density statement, since rt3/MBH=R∗3/M∗r_t^3/M_{\rm BH}=R_*^3/M_*. Rossi and collaborators derive the estimate from the tidal tensor and then replace it by a curvature tensor projected on a parallel-propagated tetrad when the encounter is relativistic (Rossi et al. 2021, §2, Eqs. 1–9).

Define the penetration factor

β≡rtrp,\beta\equiv\frac{r_t}{r_p},

where rpr_p is the center-of-mass pericenter in the stated orbital model. A value β=1\beta=1 is not a universal full-disruption threshold. A centrally concentrated star can retain a core at larger β\beta than a diffuse polytrope, while stellar spin, prior evolution, encounter duration, and relativistic compression change the response. Hydrodynamic calculations therefore supply structure-dependent partial- and full-disruption thresholds βp\beta_{\rm p} and βd\beta_{\rm d} rather than a single sharp number.

Capture must be tested before observability

Section titled “Capture must be tested before observability”

For a parabolic Schwarzschild orbit, the marginally bound circular orbit lies at the Boyer–Lindquist radius rmb=4GMBHr_{\rm mb}=4GM_{\rm BH} in the site units. An orbit below the corresponding angular-momentum separatrix plunges; the horizon radius 2GMBH2GM_{\rm BH} is too late a comparison. In Kerr spacetime, both the capture separatrix and the tidal eigenvalues depend on a∗=J/(GMBH2)a_*=J/(GM_{\rm BH}^2), orbital inclination, energy, axial angular momentum, and Carter constant.

The distinction can be checked without a stellar model. In Schwarzschild spacetime, a timelike geodesic arriving marginally bound from infinity has specific energy E=1\mathcal E=1 and specific angular momentum ℓ\ell. Its radial equation is

(drdτ)2=1−(1−2GMBHr)(1+ℓ2r2).\left(\frac{dr}{d\tau}\right)^2 =1-\left(1-\frac{2GM_{\rm BH}}{r}\right) \left(1+\frac{\ell^2}{r^2}\right).

A turning point therefore obeys ℓ2=2GMBHr2/(r−2GMBH)\ell^2=2GM_{\rm BH}r^2/(r-2GM_{\rm BH}). The minimum of this expression occurs at r=4GMBHr=4GM_{\rm BH}, giving ℓcap=4GMBH\ell_{\rm cap}=4GM_{\rm BH}. Below that angular momentum there is no outer turning point: a plunging orbit has no actual pericenter outside the horizon. At equality the ideal geodesic approaches the unstable circular orbit asymptotically. Thus the commonly drawn “capture radius” is shorthand for a boundary in orbital constants, not a material surface that every trajectory crosses at its closest approach.

The invariant procedure is:

  1. specify the incoming constants of motion in the black-hole rest frame;
  2. determine whether the geodesic crosses the capture separatrix;
  3. along a noncaptured orbit, project curvature onto the star’s freely falling tetrad;
  4. evolve a stellar model under those tides and classify surviving core, full disruption, and escaping debris.

Kesden treats geodesic capture and the relativistic tidal tensor for generically oriented Kerr orbits, comparing instantaneous tidal stretching with the star’s Newtonian self-gravity. This is a disruption criterion, not a hydrodynamic evolution of the star in step 4. The calculation shows that direct capture becomes a major rate correction above MBH∼107M⊙M_{\rm BH}\sim10^7M_\odot (Kesden 2012, §§II–IV, Eqs. 10–11 and Figs. 3–4). A coordinate pericenter can still label a calculation, but it is not itself the physical disruption criterion.

This is also the seam with finite-size orbital theory. The worldline-breakdown treatment asks when a controlled multipole expansion ceases to approximate an extended body. Here the additional question is astrophysical: whether the resulting matter is captured, remains in a core, or returns as observable debris.

Write a schematic capture radius as

rcap=κ(a∗,ι,E) GMBH,r_{\rm cap}=\kappa(a_*,\iota,\mathcal E)\,GM_{\rm BH},

where κ=4\kappa=4 for the marginally bound parabolic Schwarzschild comparison and ι\iota is orbital inclination. Setting rt=rcapr_t=r_{\rm cap} gives

MH=1κ3/2G3/2(R∗3M∗)1/2.M_{\rm H} =\frac{1}{\kappa^{3/2}G^{3/2}} \left(\frac{R_*^3}{M_*}\right)^{1/2}.

Temporarily restoring cc multiplies the numerator by c3c^3. For a solar-type star and κ=4\kappa=4, this estimate is about 4×107M⊙4\times10^7M_\odot; relativistic tidal response and the precise observable-debris criterion move the coefficient by factors of a few. The scaling is more trustworthy:

MH∝ρˉ∗−1/2κ−3/2.M_{\rm H}\propto \bar\rho_*^{-1/2}\kappa^{-3/2}.

A puffier giant can be disrupted by a more massive black hole, while a compact white dwarf requires a much smaller one. Favorable prograde Kerr orbits reduce κ\kappa and raise the limiting mass; retrograde or inclined orbits generally do less well. Fully relativistic calculations extend solar-type disruptions toward several 108M⊙10^8M_\odot for nearly maximal favorable spin, but the existence of a disruption is not yet the existence of a detectable flare (Rossi et al. 2021, §5, Eq. 33 and the discussion following it).

The scale comparison can be summarized without pretending that its boundaries are exact.

Ordering or responsePhysical outcomeWhat still must be modeled
rp>rtr_p>r_tweak tides or tidal excitationrepeated passages, mode damping, and orbital diffusion
rcap<rp≲rtr_{\rm cap}<r_p\lesssim r_t with a surviving corepartial strippingstellar profile, spin, kick, and subsequent orbit
rcap<rp≲rtr_{\rm cap}<r_p\lesssim r_t with no corefull disruptiondebris energy distribution and hydrodynamics
Incoming orbital constants lie on the plunging side of the capture separatrixdirect plunge or prompt capture; an exterior turning-point rpr_p need not existKerr separatrix and whether any debris escapes before capture

The Newtonian calculation assumes R∗/rp≪1R_*/r_p\ll1, a nearly parabolic center-of-mass orbit, and a point-mass black-hole field. It cannot determine the order-unity disruption threshold, relativistic compression, nuclear burning in a deep encounter, or the mass of an escaping debris tail. In particular, comparing rtr_t only with the horizon both overcounts observable events and erases the strong spin-orientation dependence near the Hills scale.

A solar-type star approaches a nonspinning 108M⊙10^8M_\odot black hole on a nearly parabolic orbit. Use the Newtonian rtr_t and compare it first with the horizon 2GMBH2GM_{\rm BH} and then with the marginally bound capture scale 4GMBH4GM_{\rm BH}. Which comparison is physically relevant, and what may be concluded?

Solution

For a solar-type star,

rtGMBH=R∗GM∗(M∗MBH)2/3≈2.2.\frac{r_t}{GM_{\rm BH}} =\frac{R_*}{GM_*} \left(\frac{M_*}{M_{\rm BH}}\right)^{2/3} \approx2.2.

Thus rtr_t lies slightly outside the Schwarzschild horizon but well inside the 4GMBH4GM_{\rm BH} marginally bound capture scale. The horizon-only comparison would incorrectly advertise room for disruption. The capture comparison says that a parabolic Schwarzschild orbit reaching the Newtonian tidal scale plunges first, so it does not yield the standard returning-debris flare. Because the estimate uses a Newtonian tide in a strong field, it establishes the correct regime choice rather than a percent-level boundary; a Kerr tidal-tensor calculation is required for spin or inclined orbits.

  • Kesden, M. “Tidal-Disruption Rate of Stars by Spinning Supermassive Black Holes.” Physical Review D 85, 024037 (2012). DOI.
  • Rossi, E. M., Stone, N. C., Law-Smith, J. A. P., et al. “The Process of Stellar Tidal Disruption by Supermassive Black Holes: The First Pericenter Passage.” Space Science Reviews 217, 40 (2021). DOI.