Pre-Phase A Report - Lisa - Nasa
Pre-Phase A Report - Lisa - Nasa
Pre-Phase A Report - Lisa - Nasa
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2.4 Spacecraft tracking 43<br />
2.4 Spacecraft tracking<br />
<strong>Pre</strong>cise, multi-frequency transponding of microwave signals from interplanetary probes,<br />
such as the ULYSSES, GALILEO and CASSINI spacecraft, can set upper limits on<br />
low-frequency gravitational waves. These appear as irregularities in the time-ofcommunication<br />
residuals after the orbit of the spacecraft has been fitted. The irregularities<br />
have a particular signature. Searches for gravitational waves have produced only<br />
upper limits so far, but this is not surprising: their sensitivity is far short of predicted<br />
wave amplitudes. This technique is inexpensive and well worth pursuing, but will be<br />
limited for the forseeable future by some combination of measurement noise, the stability<br />
of the frequency standards, and the uncorrected parts of the fluctuations in propagation<br />
delays due to the interplanetary plasma and the Earth’s atmosphere. Consequently, it is<br />
unlikely that this method will realise an rms strain sensitivity much better than 10 −17 ,<br />
which is six orders of magnitude worse than that of a space-based interferometer.<br />
2.5 Space interferometer<br />
The LISA measurement concept is, in essence, a space-borne implementation of a Michelson<br />
interferometer for the purpose of measuring the fluctuations in the distance between<br />
widely separated mirrors. There is, however, a fundamental distinction between LISA<br />
and the ground-based interferometers: LISA will search for the distinctively low-frequency<br />
(milli-hertz) gravitational waves (Chapter 1) which will probably never be detectable by<br />
any terrestrial detectors — existing or planned — because of unshieldable gravitational<br />
disturbances. These disturbances are due to the motion of bulk matter in the Earth and<br />
the atmospere which will pull gravitationally on the interferometer mirrors, producing<br />
undesirable phase shifts. Since gravity can not be shielded, and there does not seem to<br />
be a feasible way of independently measuring the gravitational effects of seismicity, these<br />
effects impose a strict lower limit on the gravitational wave frequencies observable on<br />
Earth. With its wide separation from Earth, LISA is completely free from these terrestrial<br />
disturbances.<br />
2.6 Early concepts for a laser interferometer in space<br />
The earliest concept for a laser gravitational wave detector in space appears to have<br />
been a Shuttle-launched monolithic Gravity Wave Interferometer (GWI). R. Weiss was<br />
informed in 1974 about NASA studies of producing such a device with up to 1 km arm<br />
lengths by using an orbiting machine to extrude aluminium beams. A NASA publication<br />
in March 1978 [72] described an interferometer with a total launch mass of 16.4 t, which<br />
included four 1000 kg test masses at the ends of a cross-shaped device (see Figure 2.3).<br />
The GWI’s sensitivity was calculated as δl/l =10−21 in the frequency range from 10−1 to<br />
102 Hz. The total cost of the project was estimated at that time to be $ 49.5 M.<br />
The idea of a monolithic space gravitational wave interferometer presented to Weiss<br />
started discussions in 1974 with P.L. Bender, R.W.P. Drever and J.E. Faller of a much<br />
larger space interferometer. The approach considered was to send laser beams between<br />
Corrected version 2.08 3-3-1999 9:33