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Coherent Backscattering from Multiple Scattering Systems - KOPS ...

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5.2 The coherent backscattering cone in high resolution<br />

intensity [a.u.]<br />

4000<br />

3000<br />

2000<br />

1000<br />

data profiles (f = 43%)<br />

data average (f = 43%)<br />

n water<br />

= 1.334 , n particle<br />

= 1.519 .<br />

n water<br />

= 1.334 , n particle<br />

= 1.520<br />

n water<br />

= 1.334 , n particle<br />

= 1.521<br />

n water<br />

= 1.334 , n particle<br />

= 1.522<br />

n water<br />

= 1.334 , n particle<br />

= 1.523<br />

n water<br />

= 1.333 , n particle<br />

= 1.519<br />

n water<br />

= 1.333 , n particle<br />

= 1.520<br />

n water<br />

= 1.333 , n particle<br />

= 1.521<br />

n water<br />

= 1.333 , n particle<br />

= 1.522<br />

n water<br />

= 1.333 , n particle<br />

= 1.523<br />

0<br />

−1000<br />

−2000<br />

0 0.1 0.2 0.3 0.4 0.5 0.6 0.7 0.8<br />

scattering angle θ CCD<br />

[deg]<br />

Figure 5.17: Measured data and calculated Mie distributions. Due to non-uniform<br />

background lighting the data vary strongly for angles larger than 0.3 ◦ and can not be<br />

fitted properly. To get a reliable scaling, the Mie distributions were scaled to fit the first<br />

order minimum and maximum of the azimuthally averaged data, whose heights are<br />

marked in the graph. The first maximum of the calculated Mie distributions is shifted<br />

towards smaller scattering angles, which shows that the particle size distribution used<br />

for the calculations is slightly wrong.<br />

65

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