GRAVITATIONAL WAVES FROM NS INTERIORS C. Peralta, M. Bennett, M. - - PowerPoint PPT Presentation

gravitational waves from ns interiors
SMART_READER_LITE
LIVE PREVIEW

GRAVITATIONAL WAVES FROM NS INTERIORS C. Peralta, M. Bennett, M. - - PowerPoint PPT Presentation

GRAVITATIONAL WAVES FROM NS INTERIORS C. Peralta, M. Bennett, M. Giacobello, A. Melatos, A. Ooi, A. van Eysden, S. Wyithe (U. Melbourne and AEI) 1. Superfluid turbulence 2. Post-glitch relaxation 3. Rigorous model parametrised template


slide-1
SLIDE 1

GRAVITATIONAL WAVES FROM NS INTERIORS

  • C. Peralta, M. Bennett, M. Giacobello, A. Melatos, A. Ooi,
  • A. van Eysden, S. Wyithe (U. Melbourne and AEI)

1. Superfluid turbulence 2. Post-glitch relaxation 3. Rigorous model → parametrised template → nuclear physics (viscosity, compressibility)

slide-2
SLIDE 2

CONTINUOUS SOURCE

Long-lived (days → years) periodic signal

  • Superfluid turbulence as pulsar spins down (Re ≈ 1011)
  • Post-glitch relaxation (Ekman pumping)
  • Follows burst signal of glitch itself (msec?)

Not discussed here...

  • R-modes continuously excited in core (Andersson et al. 99;

Nayyar & Owen 06); cf. ocean r-modes (Heyl 04)

  • Amplitude and threshold probe superfluid core and

viscous crust-core boundary layer (Lindblom & Mendell 99;

Bildsten & Ushomirsky 00; Levin & Ushomirsky 01)

C-C diff. rotation (glitches)→ nonaxisymmetric superfluid flows

slide-3
SLIDE 3

SUPERFLUID CIRCULATION

Differential rotation → meridional circulation

  • superfluid → HVBK two-fluid model (3D)
  • Quantised vortices ↔ mutual friction
  • scillating

hydro torque Re=104 EKMAN PUMPING (Peralta et al. 05, 06, 07)

slide-4
SLIDE 4

MACRO SF TURBULENCE

HERRINGBONE & SPIRAL TURBULENCE TAYLOR VORTEX

slide-5
SLIDE 5
slide-6
SLIDE 6

POST-GLITCH RELAXATION

  • Ekman: fluid spun up in radially expanding boundary

layer (meridional → Coriolis)

  • TEkman = (2E1/2Ω)−1 with E = ν(2ΩR2)−1 ≈ Re−1
  • Buoyancy inhibits meridional flow less/more according

to compressibility K

  • Brunt-Vaisala frequency: N2=g2(ceq

−2−K−2)

  • Incompressible: K → ∞. Unstratified: N → 0
  • Nonaxisymmetric perturbation ∝ exp(imφ)
  • Wave strain:

(van Eysden & Melatos 07, Bennett & Melatos 07)

slide-7
SLIDE 7

GW SPECTRUM

  • Lorentzian: measure width & peak frequency
  • Extract two of E, N, K if Ω known (X-rays)
  • Width ratio independent of E (i.e. viscosity)
  • Amplitude depends on distance, orientation, ∆Ω, and

compressibilities… but not E

  • Pol’n ratio: orientation to line of sight (also N, K)

2 2 11

) ( ) ( Ω − + =

2 ×

f E f f h ω

2 2 21

) 2 ( ) ( Ω − + =

2 +

f E f f h ω

EQUATORIAL OBSERVER (van Eysden & Melatos 07, Bennett & Melatos 07)

slide-8
SLIDE 8

h+(f) h×(f) f f

Ν = 1 K = 1

K = 0.1 K = 3 K = 1 K = 0.3 N = 0.3 N = 0.1 N = 1 N = 3

(van Eysden & Melatos 07)

slide-9
SLIDE 9

EXTRACTING NUCLEAR PHYSICS

N i E K

Total signal including current quadrupole

i i E N N K K E

(Bennett & Melatos 07)

slide-10
SLIDE 10

PHYSICS TO WORRY ABOUT

  • Microscopic turbulence
  • DGI → tangle of quantized vortices
  • Affects the mutual friction coupling ↓
  • Macroscopic turbulence (Kolmogorov

“eddies”)

  • Do large or small eddies dominate the

GW signal?

(Peralta et al 05, 06; Andersson et al 06, 07)

slide-11
SLIDE 11

WHAT WILL LIGO TEACH US?

SF turbulence

  • Is the core superfluid?
  • Mutual friction & entrainment parameter
  • Viscosity
  • Crust-core coupling
slide-12
SLIDE 12

Glitches

  • Measure ceq and K for nuclear matter
  • Do glitches happen faster or slower than one

rotation period?

  • Probe “seismic” (avalanche) dynamics
  • Spectrum of non-axisymmetric excitation

NO OTHER GOOD WAY TO LEARN SUCH THINGS!