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THE EGS5 CODE SYSTEM

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Hence,<br />

so that<br />

ln [1.13 + 3.76(αZ i ) 2 ] = ln 1.13 + ln[1 + 3.34(αZ i ) 2 ] . (2.320)<br />

ln χ 2 α =<br />

[<br />

Z S ln<br />

(<br />

m<br />

2<br />

e e 4 )<br />

]<br />

1.13<br />

p 2¯h 2 + Z<br />

(0.885) 2 X − Z E ZS −1 , (2.321)<br />

χ 2 α = m2 ee 4 1.13 e Z X/Z S<br />

p 2¯h 2 (0.885) 2 e Z E/Z S<br />

, (2.322)<br />

Now, recalling that Equations 2.297 through 2.299 are equivalent to<br />

χ 2 c = N aρ<br />

M<br />

and using Equations 2.302, 2.303, 2.322 and 2.323, we obtain<br />

Ω 0 =<br />

N aρ<br />

M<br />

(<br />

4πr2 0Z S t m 2 ec 2 /E 2 β 4) , (2.323)<br />

4πr2 0 Z Stm 2 e c4 (E 2 β 2 /c 2 )¯h 2 (0.885) 2 e Z E/Z S<br />

m 2 e (r2 0 m2 e c4 )e Z X /Z SE 2 β 4 (1.167)(1.13)<br />

= ‘6680 ′ [<br />

ρZS e Z E/Z S<br />

Me Z X/Z S<br />

]<br />

t<br />

β 2 (2.324)<br />

= b c t/β 2 . Q.E.D.<br />

Molière’s B parameter is related to b by the transcendental Equation 2.290. For a given value<br />

of b, the corresponding value of B may be found using Newton’s iteration method. As a rough<br />

estimate, B = b+ln b. It can be seen that b, and hence B, increases logarithmically with increasing<br />

transport distance.<br />

The intuitive meaning of Ω 0 is that it may be thought of as the number of scatterings that take<br />

place in the slab. If this number is too small, then the scattering is not truly multiple scattering and<br />

various steps in Molière’s derivation become invalid. In Molière’s original paper[107], he considered<br />

his theory valid for<br />

Ω 0 (his Ω b ) ≥ 20 , (2.325)<br />

which corresponds to<br />

From Equations 2.325 and 2.325 we arrive at the condition<br />

B ≥ 4.5, and b ≥ 3 . (2.326)<br />

t/β 2 ≥ 20/b c = (t eff ) 0 .<br />

Another restriction on the validity of Equation 2.279 is mentioned by Bethe[23], namely,<br />

χ 2 c B < 1 . (2.327)<br />

Resuming our presentation of the method used to sample Θ, we return now to the problem of<br />

sampling θ from f r (θ) given by Equation 2.281. It might at first appear that f r (θ) is already<br />

decomposed into sub-distribution functions. However, f (1) (θ) and f (2) (θ) are not always positive,<br />

87

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