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(ed.). Gravitational waves (IOP, 2001)(422s).

(ed.). Gravitational waves (IOP, 2001)(422s).

(ed.). Gravitational waves (IOP, 2001)(422s).

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18.5 cmThe SA suspension and requirements on the control 109to the previousstagecrossbarmagnetsmagnetscenteringwirescenteringwiresbellowbellow moving element bladecenteringwiresto the nextstagecentralcolumnbladehinge70 cmFigure 9.5. The filter.parts: the vessel, roughly speaking a cylinder with a hole in the centre and amovable part, compos<strong>ed</strong> of a piece call<strong>ed</strong> ‘cross’ attach<strong>ed</strong> to a tube call<strong>ed</strong> ‘centralcolumn’, rigidly connect<strong>ed</strong> together. The ‘central column’ is free to move alongthe vertical inside the vessel, for about a centimetre. The upper wire is attach<strong>ed</strong>to the vessel, while the lower is attach<strong>ed</strong> to the column. The two pieces areconstrain<strong>ed</strong> to move along the vertical by means of centring wires. The baseof each blade is rigidly attach<strong>ed</strong> to the outer diameter of the vessel, while the tipsare connect<strong>ed</strong> to the central column. When the filter is load<strong>ed</strong> the blades act as aspring, and are free to move for several millimetres, with a resonant frequencyabove 1 Hz. In order to decrease the vertical resonant frequency a magneticantispring acts between the vessel and the ‘cross’, in parallel with the blades.It is compos<strong>ed</strong> of an array of permanent magnets attach<strong>ed</strong> to the ‘cross’, plac<strong>ed</strong>in front of an equal array of magnets attach<strong>ed</strong> to the vessel; the two array aread hoc built in order to make repulsive force, proportional to the vertical offset,for a few millimetres. The effective elastic constant is the difference between theblade spring and the magnetic antispring, and each filter is tun<strong>ed</strong> to oscillate at∼400 mHz. In figure 9.3 with the other noise sources, the seismic motion of theVirgo test masses is shown [14], it is possible to see that it dominates below 2 Hz,and the resonance peaks of the SA are visible.Ground motion can be of the order of hundr<strong>ed</strong>s of micrometres, due to tidaldeformation of the Earth’s crust and thermal effects on the surface. In order to

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