Laser Interferometers (for GW detection)
Aaron Spector Deutsches Elektronen-Synchrotron (DESY) Hamburg, Germany Transmission Field Cavity Power This configuration additionally avoids co-resonances of End Mirror (via Transmission Port) [North] higher-order cavity modes (HOM) with the fundamental mode. The Gouy phase shift for one-way propagation down the inter- - DARM ferometer arm is Motion Ly~39m L Gouy arctan = 0.806 rad (46.2 ) (6) ⌘ ZR Lx~39m ! Power Recycling End Mirror Any Hermite-Gauss mode, H , attains a round-trip phase ex- =1064nm Mirror [East] mn Input Field cess of
2 kW Laser - mn = 2(1 + m + n) Gouy (7) 1 Watt compared to the propagation of unfocused spherical wave- REFL PD Field - Lp= 20cm fronts. When 2(m+n) Gouy is an integer multiple of 2⇡, the Hmn Reflection Beam DARM Splitter Motion mode will be co-resonant with the fundamental H mode. With Port 00 1.61 rad (92 ) of phase separation between each mode order, Anti-Symmetric 200 mW the lower-order HOM resonances are well-separated from the Photodiode (dark) Port fundamental. The fourth-order mode wraps back near the fun- damental, but the 0.17 rad (10 ) phase separation is >100 times Figure 1: Signal flow diagram of the interferometer static fields, represent- the cavity linewidth. ing the linear system of equations for the interferometer response. The fields are sourced by Elaser. Each reflection and transmission coe cient is given by The power recycling cavity provides not only the resonant r or t, subscripted by its respective optic. F is the optical carrier frequency power enhancement, but also filters noise sidebands from the and the arm lengths are Lx and Ly. The round nodes represent internal states laser. Because of the higher-order-mode separation, di↵erent of the physical system whereas the square nodes are output fields observed transverse modes have di↵erent filtered noise spectra, which in photodetectors, such as the anti-symmetric port field EAS. To fully model the contrast-defect, additional copies of this diagram must be added to rep- beat with residual light at the Michelson anti-symmetric port resent additional transverse modes, with small transfer coe cients arising by readout. The modes then show as noise peaks at the HOM res- defects in the end mirror and beamsplitter shapes. The signal sidebands from onance frequencies in the readout spectra, confirming estimates the end-mirrors are signified with red and blue arrows, which source (unshown) copies of the graph at the modulation frequencies. At each port the optical field of the arm length and Gouy separation. These noise measure- at carrier and sideband frequencies beat together to model the full frequency- ments are described in 6.4.1. FHdependent workshop response. on § 2.2. Instrument Response gravitational waves and With power recycling, the response of the interferometer to 2.1. Power-Recycling Cavity time-varying path length displacements is complicated by the particleThe Michelson physics interferometer, formed by the beamsplitter storage time of the recycling cavity, which imposes a band- and two end mirrors, forms an e↵ective mirror where the losses width limit of approximately 350 Hz on the cavity response. are determined by the fraction of light escaping to the AS port At frequencies 350 Hz, the response at the anti-symmetric ⌧ and the remainder is reflected. The addition of a power recy- port to arm length displacements reflects both a change in the cling mirror (PRM) forms a cavity with this e↵ective mirror. Michelson fringe o↵set and in the cavity storage power. How- The power-recycled interferometers are designed to be nearly ever, at frequencies 350 Hz, arm length displacements occur confocal resonators, folded by the 45 incidence beamsplitter on a shorter time scale than the cavity can respond. In this so that each arm forms a flat-curved cavity. They have an arm limit, the power-recycled interferometer responds equivalently length of L = 39.2 m and an end mirror radius of curvature of to a single-pass Michelson interferometer of the same optical R = 75.1 m, which is matched between the two arms to within power. 10 cm. The resulting waist, with radius Fig. 2 shows the numerically-calculated transfer function of the power-recycled interferometers at several fringe o↵sets. The Holometer operates at an o↵set of approximately 1 nm, and w0 = 2L(2R 2L) 3.57 mm (4) r2⇡ ⇡ all science and calibration signals are measured at frequencies p 1 kHz. At this o↵set, the deviation from a single-pass Michel- lays at the position of the flat PRM. The end mirrors are each son response is 2% above 1 kHz. The third plot, indicating located nearly one Rayleigh range away, the optical sensitivity, shows this di↵erence at the calibration 2 line frequency from the asymptotic response, which is small ⇡w0 ZR = 37.6 m (5) for the 1nm o↵set. Thus, for calibration purposes (see 7.2) ⌘ § the instrument can be modeled as an equivalent high-power, where the beam half-width has grown to w 5 mm. The devi- single-pass interferometer. Neglecting the cavity correction un- 1 ⇡ ation from a pure confocal configuration satisfies the resonator derestimates the instrumental sensitivity. The degradation in stability criterion, R < 2L (for a review of laser resonators, see sensitivity would be relevant for smaller interferometers with [17]). higher bandwidth recycling. For instance in tabletop versions 4 3 Page 6 of 217 LivingRevRelativ(2016)19:3
Fig. 1 Gravitational waves are transverse quadrupole waves. If a wave passes through the ring of test particles that is oriented perpendicular to the direction of wave propagation, the distances between the particles would change periodically as shown in this sketch
Fig. 2 Simplified layout of a Michelson interferometer. The laser provides the input light, which is split into two beams by the central beamsplitters. The beams reflect off the end mirrors and recombine at the beamsplitter. The light power on the main photo detector (PD) changes when the difference between the arm length ∆L L L changes = X − Y
The measurable length change induced by a gravitational-wave depends on the total length being measured. For gravitational waves with wavelength much larger than the Principles of GW detection detector size we get:
Strain • GWs stretch and squeeze space-time ∆L hL, (1.1) = with L the length of the detetor and h the strain amplitude of the gravitational wave. This scaling of the change with the base length led to the construction of interferometers with arm length of several kilometres. Gravitational-wave detectors strive to pick out signals carried by passing gravita- tional waves from a background of self-generated noise. This is challenging because of the extremely small effects produces by the gravitational waves. For example, the
first gravitational wave detected in September 2015 by the LIGO2 detectors (Abbott et al. 2016b), which is considered to be a strong event, reached a strain amplitude of 21 10− .ThissignalcouldnothavebeenmeasuredwithasimpleMichelsoninterferom-
123 3 Page 6 of 217 LivingRevRelativ(2016)19:3
Fig. 1 Gravitational waves are transverse quadrupole waves. If a wave passes through the ring of test particles that is oriented perpendicular to the direction of wave propagation, the distances between the particles would change periodically as shown in this sketch
Fig. 2 Simplified layout of a Michelson interferometer. The laser provides the input light, which is split into two beams by the central beamsplitters. The beams reflect off the end mirrors and recombine at the beamsplitter. The light power on the main photo detector (PD) changes when the difference between the arm length ∆L L L changes = X − Y
The measurable length change induced by a gravitational-wave depends on the total length being measured. For gravitational waves with wavelength much larger than the detectorPrinciples size of we GW get: detection
Interferometers ∆L hL, (1.1) • Phase changes induced by length changes in arms = • Sensitivity determined by response, displacement noise, sensing noise with L the length of the detetor and h the strain amplitude of the gravitational wave. This scaling of the change with the base length led to the construction of interferometers with arm length of several kilometres. Gravitational-wave detectors strive to pick out signals carried by passing gravita- tional waves from a background of self-generated noise. This is challenging because of the extremely small effects produces by the gravitational waves. For example, the first gravitational wave detected in September 2015 by the LIGO detectors (Abbott 3 et al. 2016b), which is considered to be a strong event, reached a strain amplitude of 21 10− .ThissignalcouldnothavebeenmeasuredwithasimpleMichelsoninterferom-
123 Principles of GW detection
[Ringwald, Tamarit, Welling]
GWs in SMASH
GWs from quantum uctuations during in ation
GWs from in aton fragmentation during preheating
GWs from thermal uctuations after preheating
4 Principles of GW detection Space Based (LISA) Ground Based (aLIGO, VIRGO, ET) HF Ground Based • 0.1 mHz - 0.1Hz • 10 Hz - 1 kHz • 1 MHz - 100 MHz km Earth 2.5 million
19 – 23° 60° 1 AU (150 million km) Sun 1 AU Sun 5 ± ± V !"! ∞ =