Pre-Phase A Report - Lisa - Nasa
Pre-Phase A Report - Lisa - Nasa
Pre-Phase A Report - Lisa - Nasa
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1.1 Theory of gravitational radiation 13<br />
field, by the equivalence principle. Detectors work only because they sense the changes<br />
in this acceleration across them. If two parts of a detector are separated by a vector L,<br />
then it responds to a differential acceleration of order<br />
L ·∇(∇Φ) ∼ LΦ/λ 2 . (1.3)<br />
SincewehaveseenthatΦ∼ hc 2 (dropping the indices of hαβ in order to simplify this<br />
order-of-magnitude argument), the differential acceleration is of order Lω 2 h.<br />
If the detector is a solid body, such as the bar detectors described in Section 2.2.1,<br />
the differential acceleration will be resisted by internal elastic stresses, and the resulting<br />
mechanical motion can be complex. Bars are made so that they will “ring” for a long<br />
time after a gravitational wave passes, making detection easier. If the detector consists<br />
of separated masses that respond to the gravitational wave like free particles, then the<br />
situation is easier to analyse. This is the case for interferometers, including LISA.<br />
For two free masses separated by the vector L, the differential acceleration given by<br />
Equation 1.3 leads to an equation for the change in their separation δ L,oforder<br />
d2δL dt2 ∼ Lω2h. Since the time-derivatives on the left-hand-side just bring down factors of ω, we arrive at<br />
the very simple equation δL/L ∼ h. A careful derivation shows that this is exact with a<br />
further factor of 2:<br />
δL 1<br />
= h. (1.4)<br />
L<br />
Here we make contact with the geometrical interpretation of general relativity. The distances<br />
L and δL should be interpreted as proper distances, the actual distances that a<br />
meter-stick would measure at a given time. Then we see that h is indeed a metric, a distance<br />
measure: as a gravitational wave passes, it stretches and shrinks the proper distance<br />
between two free bodies. This equation also explains why interferometric detectors should<br />
be made large: the technical problem is always to measure the small distance change δL,<br />
and for a given wave amplitude h this distance change increases in proportion to L.<br />
Polarization of gravitational waves. We have managed to discover much about gravitational<br />
waves by ignoring all the indices and the full complexity of the field equations,<br />
but this approach eventually reaches its limit. What we cannot discover without indices<br />
is how the differential accelerations depend on the direction to the source of the wave.<br />
Here there are two important results that we simply quote without proof:<br />
2<br />
• Gravitational waves are transverse. Like electromagnetic waves, they act only in<br />
a plane perpendicular to their direction of propagation. This means that the two<br />
separated masses will experience the maximum relative distance change if they are<br />
perpendicular to the direction to the source; if they lie along that direction there<br />
will be no change δL.<br />
• In the transverse plane, gravitational waves are area preserving. This means that<br />
if a wave increases the proper distance between two free masses that lie along a given<br />
direction, it will simultaneously decrease the distance between two free masses lying<br />
along the perpendicular direction in the transverse plane. The consequence of this<br />
is illustrated in the standard polarization diagram, Figure 1.1 .<br />
Corrected version 2.08 3-3-1999 9:33