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RESPONSE OF THE EARTH TO GRAVITATIONAL WAVES

Following Schutz(1988), the response of two masses connected by a spring to a gravitational wave with amplitude httxx,00 is controlled by
\begin{displaymath}
\xi_{,00} + 2 \gamma \xi_{,0} + \omega_{0} \xi = \frac{1}{2} l_{0} h^{tt}_{xx,00}\end{displaymath} (5)
where $\xi$ is the displacement, $\gamma$ is the damping factor, $\omega_{0}$is the resonance frequency, and l0 is the length of the spring. $\xi_{,00}$ is the second derivative with respect to time, and $\xi_{,0}$ is the first derivative with respect to time. httxx,00 is the amplitude of the wave as referred to by Schutz(1988).

The solution to this equation when $ h^{tt}_{xx,00} = A \cos\Omega t $is

\begin{displaymath}
\xi = R \cos ( \Omega t - \phi ) \end{displaymath} (6)

where

\begin{displaymath}
R = \frac{ \frac{1}{2} l_{0} \Omega^2 A}{\sqrt{(\omega_{0}-\Omega)^2 + 4 \Omega^2 \gamma^2}} \end{displaymath} (7)

and

\begin{displaymath}
\tan \phi = \frac{2 \gamma \Omega}{\omega_{0}^2 - \Omega^2}\end{displaymath} (8)
$ \Omega $ is the wave's frequency.

If $ \omega_{0}^2 - \Omega^2 $ is large with respect to $ 2 \gamma \Omega $, $ \phi $ will approach zero and $\xi$ will be proportional to httxx.

I make a crude assumption that a column in the earth will react like a spring. Away from resonance, the response of the earth to a gravitational wave will be proportional to the strain $ \cos(2 \phi) \sin^2(\theta)\cos \Omega t $,where $ \phi $ is colatitude and $\theta$ is longitude as given by Hellings (1992). This strain on a sphere for t=0 is shown at an exaggerated scale in Figure  [*].

 
GWresp2
Figure 5
An exaggerated view of the strain on the earth caused by a gravitational wave. The function plotted is $ (\cos(2 \phi) \sin^2(\theta))+2$.
GWresp2
view

If this response is close to the correct response, the strain of the earth recorded by the IDA network can be predicted. Figure [*] shows the response of the earth as it would appear to the available stations to a source at position 43 of the grid in Figure [*], using these approximations.

 
daysrc43
Figure 6
The response of the IDA stations to a gravitational wave source at position 43 of the grid in Figure 11. Each trace corresponds to a station in the IDA array.
daysrc43
view


previous up next print clean
Next: PROCESSING SEQUENCE Up: Abma: Detecting gravitational waves Previous: TARGETED OBJECTS
Stanford Exploration Project
11/17/1997