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Hyung Mok Lee
Department of Physics and Astronomy, Seoul National University
The Third KAGRA International Workshop May 21-22, 2017 Taipei
Terrestrial Detector for Low Frequency GW Based on Full Tensor - - PowerPoint PPT Presentation
KIW3 Terrestrial Detector for Low Frequency GW Based on Full Tensor Measurement Hyung Mok Lee Department of Physics and Astronomy, Seoul National University The Third KAGRA International Workshop May 21-22, 2017 Taipei KIW3
KIW3
Hyung Mok Lee
Department of Physics and Astronomy, Seoul National University
The Third KAGRA International Workshop May 21-22, 2017 Taipei
KIW3
http://rhcole.com/apps/GWplotter by Moore, Cole & Berry
There is a gap here (0.1 - 10 Hz)
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Jun et al. 2015
Measurement by SNU group: are we witnessing the growth of the BH?
Small Mseed (10Mis acceptable if BH accreted at Eddington limit, but larger Mseed is more plausible
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detectors at ~ 0.1 Hz: should be better than 10-20 Hz-1/2 (Harms et
have been considered
interferometer (TOBA)
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Harms et al. 2013
( Amaro-Seone P and Freitag M 2006)
dense star clusters (Fregeau J M et al 2006)
cluster in ultra-compact galaxies (Amaro-Seone P et al 2014)
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d2xi dt2 = −Ri
0j0xj
Ri0j0 ≈ ∂2φ ∂xi∂xj Ri0j0 = −1 2 ∂2hij ∂t2 ≈ 1 2ω2hij
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wave antenna (Johnson & Merkowitz 1993)
polarization
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resonant L-C circuit
circuits
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Test masses are magnetically suspend (fDM ~ 0.01 Hz). 100x higher sensitivity
Six test masses mounted a cube form a tensor gradiometer.
Test masses are levitated by a current induced along a tube.
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Gravitational Radiation Observatory (SOGRO)
Riemann tensor, the source direction and the polarization can be determined
hii(t) = 1 L[x+ii(t) − x−ii(t)] hij(t) = 1 L {[x+ij(t) − x−ij(t)] − [x−ji(t) − x+ji(t)]}
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signal bandwidth (0.1 - 10 Hz)
accelerometer
gravity
hij ∼ 1 ω2 ∂2φ ∂xi∂xj
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combined channels 5 , , 1 1 8 ) (
2 / 1 2 2 2 4 2 p N B N B p D D D B h
n T k T k Q T k ML f S ω β ω ω ω ω ω ! = ⎪ ⎪ ⎭ ⎪ ⎪ ⎬ ⎫ ⎪ ⎪ ⎩ ⎪ ⎪ ⎨ ⎧ ⎟ ⎟ ⎠ ⎞ ⎜ ⎜ ⎝ ⎛ + − + =
Parameter SOGRO aSOGRO Method employed (/aSOGRO) Each test mass M 5 ton 5 ton Nb shell Arm-length L 50 m 50 m Over “rigid” platform Antenna temp T 1.5 K 0.1 K Liquid He / He3-He4 dilution refrigerator Platform temp Tpl 1.5 K 1.5 K Large-scale cryogenics Platform Q factor Qpl 106 107 Square Al tube construction DM frequency fD 0.01 Hz 0.01 Hz Magnetic levitation (horizontal only) DM quality factor 107 108 Surface polished pure Nb Pump frequency fp 50 kHz 50 kHz Tuned capacitor bridge transducer Amplifier noise no. n 20 5 Two-stage dc SQUID cooled to 0.1 K Detector noise Sh1/2(f ) 1 × 10−20 Hz−1/2 3 × 10−21 Hz−1/2 Computed at 1 Hz
▪ aSOGRO requires QD ~ 108 for test masses and Qpl ~ 107 for the platform. ▪ aSOGRO requires improvement by a factor of 2 over best SQUIDs achieved so far.
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▪ At present, the greatest challenge appears to be platform design and construction.
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Seismic noise of underground sites
▪ 20-m pendulum with nodal support ⇒ Passive isolation for f > 0.1 Hz. ▪ Reduction by combining passive and active isolation with CM rejection of the detector can reduce seismic noise below detector noise
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▪ Seismic and atmospheric density modulations cause Newtonian gravity gradient noise. ▪ GWs are transverse and do not have longitudinal components whereas the Newtonian gradient does.
In GW frame,with the wave traveling along the 3rd axis,
GW could be distinguished from near-field Newtonian gravity.
h0(ω) = h+(ω) + h0
NG,11(ω)
h⇥(ω) + h0
NG,12(ω)
h0
NG,13(ω)
h⇥(ω) + h0
NG,12(ω)
−h+(ω) + h0
NG,22(ω)
h0
NG,23(ω)
h0
NG,13(ω)
h0
NG,23(ω)
h0
NG,33(ω)
By combining tensor components, we get Similar expression can be found for hx(ω).
h+(ω) = h0
11(ω) − 2 cot θh0 13(ω) + csc2 θ2πGρ0
ω γR cR exp ✓ ω cR z ◆ X
i
ξ(ω) + csc2 θ4πG ω2 X
i
δρi(ω) sin2 ϑi exp ✓ ω cIS z sin ϑi ◆
Due to Rayleigh Waves Due to Infrasound waves
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NN due to Rayleigh waves removed by using h’13, h’23, h’33, az (CM), plus 7 seismometers with SNR = 103 at the radius of 5 km. NN due to infrasound removed by using h’13, h’23, h’33 and 15 mikes of SNR = 104, 1 at the detector, 7 each at radius 600 m and 1 km.
Harms & Paik, PRD 92, 022001 (2015)
▪ First remove Rayleigh NN by using seismometers only, then remove infrasound NN by using microphones and cleaned-up SOGRO outputs. ▪ SOGRO can remove NN from infrasound for all incident angles.
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Maximum distances to detect IMBH- IMBH binary merger (SOGRO 2)
▪ SOGRO would fill in the missing signal band between eLISA and aLIGO/ Virgo/KAGRA, 0.1 – 10 Hz. ▪ SOGRO is a tensor detector with all-sky coverage and with the ability to locate the source and determine wave polarization. ▪ SOGRO, a full-tensor detector, has an advantage in rejecting NN. ▪ Technical details have to be further studied.
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Paik et al. 2016, 30m and 100 baseline