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Investigations of Faraday Rotation Maps of Extended Radio Sources ...

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60 CHAPTER 3. MEASURING MAGNETIC FIELD POWER SPECTRA<br />

100<br />

A 2634<br />

A 400<br />

Hydra A<br />

(8π) 1/2 [µG]<br />

10<br />

1<br />

0.1<br />

0.01 0.1 1 10 100<br />

k c [kpc -1 ]<br />

Figure 3.4: Magnetic field strength B dependent on the upper k-cut<strong>of</strong>f in the integration<br />

<strong>of</strong> Eq. (3.29). The equivalent beamsizes k beam are represented as vertical lines.<br />

displays the magnetic field strength B = √ 8π〈ε B 〉 estimated from<br />

ε B (k < k c ) =<br />

∫ kc<br />

0<br />

dk ε B (k). (3.55)<br />

3.4.4 Test the model and assess the influence <strong>of</strong> the window function<br />

The various possibilities to test the window function and to assess its influences on the<br />

results outlined in Sects. 3.3.3 and 3.3.4 were also applied to the data. The χ 2 -function<br />

was derived by radially averaging the χ 2 (⃗x ⊥ ) distribution resulting from Eq. (3.38),<br />

where for the magnetic autocorrelation length λ B the value derived in the Fourier<br />

analysis was used since this approach seems to be more accurate. The resulting radially<br />

binned distributions are shown in Fig. 3.5 determined for the three clusters. There is no<br />

apparent spatial large scale trend visible for Abell 400 and Abell 2634 which indicates<br />

a reasonable model for the window function. In the case <strong>of</strong> Hydra A, there appears<br />

to be a trend <strong>of</strong> higher values for χ 2 (x ⊥ ) towards larger r, comparable to small scale<br />

trends seen in the χ 2 (x ⊥ ) distribution <strong>of</strong> Abell 2634 and Abell 400.<br />

Furthermore, the χ 2 (⃗x ⊥ ) distribution was integrated following Eq. (3.40) and χ 2 av<br />

was calculated to be 1.0 for Abell 2634, 1.2 for Abell 400 and 1.6 for Hydra A. A<br />

refinement <strong>of</strong> the model describing parameter does not seem to be required for Abell<br />

2634 and Abell 400.<br />

Since the value for χ 2 av <strong>of</strong> 1.6 for Hydra A is deviating from 1, the geometry <strong>of</strong> the<br />

source was varied, i.e. the inclination angle θ between source and observer plane was

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