terrestrial detector for low frequency gw based on full

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Hyung Mok Lee Department of Physics and Astronomy, Seoul National University Collaborators: H. Paik, Vol Moody, Cornelius Griggs, Ettore Majorana, Jan Harms, C. Kim, A. Nielsen KCK Meeting, Dec. 14, 2015 Beijing Terrestrial Detector for Low Frequency GW Based on Full Tensor Measurement

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Page 1: Terrestrial Detector for Low Frequency GW Based on Full

Hyung Mok Lee Department of Physics and Astronomy, Seoul National University

Collaborators: H. Paik, Vol Moody, Cornelius Griggs, Ettore Majorana, Jan Harms, C. Kim, A. Nielsen

KCK Meeting, Dec. 14, 2015 Beijing

Terrestrial Detector for Low Frequency GW Based on Full Tensor

Measurement

Page 2: Terrestrial Detector for Low Frequency GW Based on Full

2015 KCK, Dec. 14-16, Beijing HMLee

Gravitational Waves in Wide Spectral Range

http://rhcole.com/apps/GWplotter by Moore, Cole & Berry

}

There is a gap here (0.1 - 10 Hz)

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Page 3: Terrestrial Detector for Low Frequency GW Based on Full

2015 KCK, Dec. 14-16, Beijing HMLee

Terrestrial Detector Concepts for Low Frequencies

• Astrophyiscal requirement for detectors at ~ 0.1 Hz: should be better than 10-20 Hz-1/2 (Harms et al. 2013)

• Following Detector Concepts have been considered 1. Atom-laser interferometer 2. Torsional bar with laser interferometer (TOBA)

3. Michelson interferometer

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Page 4: Terrestrial Detector for Low Frequency GW Based on Full

2015 KCK, Dec. 14-16, Beijing HMLee

Gravity Gradiometer as a GW Detecror

•Geodesic deviation equation:

• In weak field limit

• Strain Amplitude

d

2x

i

dt

2= �R

i0j0x

j

Ri0j0 ⇡ @

2�

@x

i@x

j

Ri0j0 = �1

2

@2hij

@t2⇡ 1

2!2hij

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Page 5: Terrestrial Detector for Low Frequency GW Based on Full

2015 KCK, Dec. 14-16, Beijing HMLee

• Truncated icosahedral gravitational wave antenna (Johnson & Merkowitz 1993)

• Omni-directional

• Measure direction and polarization

• Spherical Resonant Detectors

• MiniGRAIL (Leiden)

• Schenberg (Sao Paulo)

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Full Tensor Detectors

Page 6: Terrestrial Detector for Low Frequency GW Based on Full

2015 KCK, Dec. 14-16, Beijing HMLee

Tunable Free Mass GW Detector (Wagoner et al. 1979)• The relative motion of two masses induces driving emf of

resonant L-C circuit • The relative momentum is determined by the current in the

circuits • Can be tuned over a wide frequency range

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Page 7: Terrestrial Detector for Low Frequency GW Based on Full

2015 KCK, Dec. 14-16, Beijing HMLee

Superconducting Tensor Gravity Gradiometer (Univ. of Maryland)

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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Page 8: Terrestrial Detector for Low Frequency GW Based on Full

2015 KCK, Dec. 14-16, Beijing HMLee

Superconducting tensor GW Detector

• Superconducting Omni-directional Gravitational Radiation Observatory (SOGRO)

• By detecting all six components of 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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Page 9: Terrestrial Detector for Low Frequency GW Based on Full

2015 KCK, Dec. 14-16, Beijing HMLee

Requirements and Philosophy

• Extremely low detector noise is required • Low temperature, high Q and quantum limited detector

• Test mass suspension frequency should be lowered to below the signal bandwidth (0.1 - 10 Hz) • Almost free test masses by magnetic levitation

• Seismic noise is more difficult to isolate at low frequencies • High CM rejection in a superconducting differential

accelerometer • Newtonian noise increases sharply below 10 Hz

• Tensor detector which can discriminate against the near-field gravity

hij ⇠1

!

2

@

2�

@x

i@x

j

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Page 10: Terrestrial Detector for Low Frequency GW Based on Full

2015 KCK, Dec. 14-16, Beijing HMLee

Basic Design of SOGRO

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Page 11: Terrestrial Detector for Low Frequency GW Based on Full

2015 KCK, Dec. 14-16, Beijing HMLee

Suspension• Go underground to reduce seismic and gravity gradient

noise

• Nodal support in order to suppress the odd harmonics

• 25m pendulum gives fp=0.1 Hz for two horizontal modes and fr <0.001 Hz for three angular modes

• passive isolation for high frequencies

• Triangulate with thin wall tubes to make the platform rigid

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Page 12: Terrestrial Detector for Low Frequency GW Based on Full

2015 KCK, Dec. 14-16, Beijing HMLee

Magnetic Levitation• Field required to levitate 5 ton mass:

• The biggest challenges: • To obtain symmetry, vertical DM resonance frequencies

must also reduced to 0.01 Hz. • Employ “push-pull levitation”

B2

2µ0A = Mg, B =

✓2µ0Mg

A

◆1/2

⇡ 0.16T

(Moody, Chan and Paik, JAP, 1986)

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Page 13: Terrestrial Detector for Low Frequency GW Based on Full

2015 KCK, Dec. 14-16, Beijing HMLee

Tuned Capacity-Bridge Transducer

•Capacitor bridge coupled to a near quantum-limited SQUID thru S/C transformer.

•LC resonance increases energy coupling β by Qp .

•Oscillator noise is rejected by the bridge balance. • Maintain precise

balance by feedback.

EN (f) =kBT!D

QD+

|!2 � !2D|

!p

✓1 +

1

�2

◆1/2

kBTN

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Page 14: Terrestrial Detector for Low Frequency GW Based on Full

2015 KCK, Dec. 14-16, Beijing HMLee

Achievable detector noiseFor CW signal impedance matched bridge transducer

Parameter SOGRO 1 SOGRO 2 Method Employed (SOGRO 1 / 2)Each mass M 5 ton 5 ton Nb square tubeSeparation L 30 m 100 m Over “rigid” mounting platformAntenna temp T 1.5 K 0.1 K Superfluid He / dilution refrigeratorDM frequency fD 0.01 Hz 0.01 Hz Magnetic levitation w/ negative springDM quality factor QD 108 109 Surface polished pure NbSignal frequency f 0.1-10 Hz 0.1-10 Hz Detector noise computed at 1 HzPump frequency fp 50 kHz 50 kHz Tuned capacitor bridge transducerAmplifier noise no. n 200 10 Near-quantum-limited SQUIDDetector noise S 1/2(f )

h 2×10�20 Hz�1/2 2×10�21 Hz�1/2 Two phase development

Sh(!) =8

ML2!4

(kB!D

QD+

|!2 � !2D|

!p

✓1 +

1

�2

◆1/2

kBTN

), kBTN = n!p

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Page 15: Terrestrial Detector for Low Frequency GW Based on Full

2015 KCK, Dec. 14-16, Beijing HMLee

Seismic noise

Seismic noise of underground sites

▪ 20-m pendulum with nodal support ⇒ Passive isolation for f > 0.1 Hz. ▪ 110 dB reduction by combining passive

and active isolation with CM rejection of the detector.

Seismic background

Active isolation

Axis alignment and scale factor match

Error compensation

Paik 14

SOGRO 1 sensitivity

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Page 16: Terrestrial Detector for Low Frequency GW Based on Full

Major challenges: ▪ Large-scale cryogenics. ▪ Mitigation of Newtonian noise. 13

Sensitivity goals of SOGRO

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Page 17: Terrestrial Detector for Low Frequency GW Based on Full

2015 KCK, Dec. 14-16, Beijing HMLee

Newtonian gravity noise (NN)▪ 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(!) =

0

@h+(!) + h0

NG,11(!) h⇥(!) + h0NG,12(!) h0

NG,13(!)h⇥(!) + h0

NG,12(!) �h+(!) + h0NG,22(!) h0

NG,23(!)h0NG,13(!) h0

NG,23(!) h0NG,33(!)

1

A

By combining tensor components, we get

Similar expression can be found for hx(ω).

h+(!) = h011(!)� 2 cot ✓h0

13(!) + csc

2 ✓2⇡G⇢0

!

�RcR

exp

✓!

cRz

◆X

i

⇠(!)

+ csc

2 ✓4⇡G

!2

X

i

�⇢i(!) sin2 #i exp

✓!

cISz sin#i

Due to Rayleigh Waves

Due to Infrasound waves

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Page 18: Terrestrial Detector for Low Frequency GW Based on Full

2015 KCK, Dec. 14-16, Beijing HMLee

Removal of Newtonian noise

Tensor + 8 microphones 100 m ( 100m, SNR 105)

Harms and Paik, PRD (2015)

Tensor + ver CM (0 noise)

Ω

Meets sensitivity goal of SOGRO 1.

Tensor + ver CM (SNR 106

+7 seisemometers (5km, SNR 103)

Tensor + 15 microphones(0, 0.6, 1 km, SNR 104)

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Page 19: Terrestrial Detector for Low Frequency GW Based on Full

2015 KCK, Dec. 14-16, Beijing HMLee

Summary

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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