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Gravitational Waves - The Sound of the Dark Universe

Summary of the Pro ISSI talk by Karsten Danzmann (edited by H.Schlaepfer)

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son interferometer. For a gravitational<br />

wave detector, <strong>the</strong> mirrors<br />

are <strong>the</strong> test masses, so that any<br />

change <strong>of</strong> <strong>the</strong> distance between<br />

<strong>the</strong>m due to a gravitational wave<br />

changes <strong>the</strong> length <strong>of</strong> <strong>the</strong> light<br />

path, which in turn is measured by<br />

interference with <strong>the</strong> o<strong>the</strong>r beam.<br />

For instance, as <strong>the</strong> wavelength <strong>of</strong><br />

red light is in <strong>the</strong> order <strong>of</strong> 0.6 µm,<br />

displacements <strong>of</strong> less than say 0.1<br />

µm can be resolved.<br />

Yet, this value is still a long way <strong>of</strong>f<br />

from resolving <strong>the</strong> tiny shifts caused<br />

by gravitational waves. In order to<br />

enhance a Michelson interferometer’s<br />

capabilities, interferometers<br />

nowadays make use <strong>of</strong> an invention<br />

by Charles Fabry 16 and Alfred<br />

Perot 17 who added fur<strong>the</strong>r optical<br />

elements constituting Fabry-Perot<br />

cavities (not shown in Fig. 5). <strong>The</strong><br />

idea is to allow <strong>the</strong> two beams between<br />

<strong>the</strong> beam splitter and <strong>the</strong> respective<br />

mirrors to pass several hundred<br />

times back and forth instead<br />

<strong>of</strong> just once. This multiplies <strong>the</strong> effective<br />

displacement <strong>of</strong> <strong>the</strong> mirrors<br />

by <strong>the</strong> same factor <strong>the</strong>reby greatly<br />

enhancing <strong>the</strong> sensitivity <strong>of</strong> <strong>the</strong><br />

system.<br />

Yet, with increasing sensitivity,<br />

spurious noise tends to appear that<br />

can mask <strong>the</strong> signal caused by gravitational<br />

waves. For instance, <strong>the</strong><br />

light produced by a laser consists<br />

<strong>of</strong> a flow <strong>of</strong> photons. However,<br />

<strong>the</strong>y come at random, just like <strong>the</strong><br />

droplets <strong>of</strong> a rainfall. This leads to<br />

high-frequency noise in <strong>the</strong> output<br />

<strong>of</strong> <strong>the</strong> detector. In addition, for<br />

sufficiently high laser power, <strong>the</strong><br />

photons reflected by <strong>the</strong> mirrors<br />

Fig 5: <strong>The</strong> basic configuration <strong>of</strong> a Michelson Interferometer. A light source<br />

(today mostly lasers) emits light in <strong>the</strong> direction <strong>of</strong> <strong>the</strong> beam splitter. This element<br />

produces two beams, <strong>of</strong> which one travels ahead in <strong>the</strong> same direction as before,<br />

while <strong>the</strong> second is reflected by 90°. Both beams travel towards <strong>the</strong> mirrors, which<br />

reflect <strong>the</strong>m back towards <strong>the</strong> beam splitter, which acts on <strong>the</strong> beams again. Finally,<br />

both beams travel towards <strong>the</strong> detector where <strong>the</strong>y interfere. <strong>The</strong> test masses’ surfaces<br />

act as mirrors, so that any displacement <strong>of</strong> <strong>the</strong> test cubes causes a change in<br />

<strong>the</strong> path lengths <strong>of</strong> <strong>the</strong> beams. <strong>The</strong> difference between <strong>the</strong> two optical paths makes<br />

<strong>the</strong> interference pattern change and <strong>the</strong> detector deliver an output.<br />

on <strong>the</strong> test masses transfer a random<br />

momentum, which tends to<br />

disguise a signal at lower frequencies.<br />

External effects, such as seismic<br />

turbulences and o<strong>the</strong>r forms <strong>of</strong><br />

environmental vibrations acting on<br />

<strong>the</strong> test masses, are sources <strong>of</strong> detector<br />

noise. In order to suppress<br />

this type <strong>of</strong> noise, two (or more)<br />

widely spaced sites are used. <strong>The</strong><br />

stochastic environmental noise<br />

will be different at each site so that<br />

appropriate algorithms are able to<br />

suppress it to some extent. On <strong>the</strong><br />

o<strong>the</strong>r hand, any gravitational wave<br />

signal will be <strong>the</strong> same at all sites<br />

(aside from an eventual time shift).<br />

All <strong>the</strong>se – and many o<strong>the</strong>r – effects<br />

must be taken into account<br />

before an observatory becomes<br />

able to monitor gravitational<br />

waves. As an engineer said: <strong>The</strong><br />

16<br />

Maurice Paul Auguste Charles Fabry, 1867, Marseille – 1945, Paris, French physicist.<br />

17<br />

Jean-Baptiste Alfred Perot, 1863, Metz, France – 1925, Paris, French physicist.<br />

SPATIUM 39 10

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