PENELOPE 2003 - OECD Nuclear Energy Agency
PENELOPE 2003 - OECD Nuclear Energy Agency
PENELOPE 2003 - OECD Nuclear Energy Agency
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192 Chapter 6. Structure and operation of the code system<br />
(iii) Angular distributions of transmitted and backscattered particles.<br />
(iv) Depth-dose distribution (i.e. deposited energy per unit depth).<br />
(v) Depth-distribution of deposited charge.<br />
(vi) Distribution of energy deposited into the slab.<br />
Each simulated continuous distribution is printed on a separate file (as a histogram),<br />
with a heading describing its content and in a format ready for visualization with a<br />
plotting program. The code computes and delivers the statistical uncertainties (3σ) of<br />
all evaluated quantities and distributions. Many authors quote these uncertainties as<br />
one standard deviation, which means that the probability for the actual value to lie<br />
outside the error bar is 0.317. We prefer to be more conservative and stay at the 3σ<br />
level, for which the probability of “missing the real value” is only 0.003.<br />
The program PENSLAB and its predecessors have been intensively used during the<br />
last years to analyze the reliability of penelope. They have been applied to a variety<br />
of experimental situations, covering a wide energy range. Benchmark comparisons with<br />
experimental data have been published elsewhere (Baró et al., 1995; Sempau et al.,<br />
1997).<br />
WARNING: In the output files of PENSLAB (and also in those of the program PENCYL<br />
described below), the terms “transmitted” and “backscattered” are used to denote particles<br />
that leave the material system moving upwards (W > 0) and downwards (W < 0),<br />
respectively. Notice that this agrees with the usual meaning of these terms only when<br />
primary particles impinge on the system coming from below (i.e. with W > 0).<br />
6.2.2 Program PENCYL<br />
The program PENCYL simulates electron and photon transport in multilayered cylindrical<br />
structures. The material system consists of one or several layers of given thicknesses.<br />
Each layer contains a number of concentric homogeneous rings of given compositions and<br />
radii (and thickness equal to that of the layer). The layers are perpendicular to the z-axis<br />
and the centre of the rings in each layer is specified by giving its x and y coordinates.<br />
When all the centres are on the z-axis, the geometrical structure is symmetrical under<br />
rotations about the z-axis (see fig. 6.3).<br />
Primary particles of a given kind, KPARP, are emitted from the active volume of<br />
the source, either with fixed energy SE0 or with a specified (histogram-like) energy<br />
spectrum. The initial direction of the primary particles is sampled uniformly inside a<br />
cone of (semi-) aperture SALPHA and with central axis in the direction (STHETA, SPHI).<br />
Thus, SALPHA = 0 defines a monodirectional source and SALPHA = 180 deg corresponds<br />
to an isotropic source.<br />
The program can simulate two different types of sources:<br />
a) An external point or extense (cylindrical) homogeneous source, defined separately<br />
from the geometry of the material system, with its centre at the point (SX0, SY0, SZ0).