Room acoustics - Building Acoustics - page 134

source method . The models implemented in software programs are, however, given
special names depending on the specific algorithm used and furthermore, there exist
hybrid types combining principles from ray-tracing and image-source modelling. A
review on computer modelling of sound fields is given a journal special issue (see Naylor
(1993)).
4.6.1 Ray-tracing models
A pioneering work on computer modelling using the ray-tracing method is from
Krokstad et al. (1968). Calculation involving ray tracing is based on simulating a point
source emitting a large number of “rays” evenly distributed per unit solid angle. Each ray
then represents a given solid angle part of the spherical wave emitted from the source.
The rays are “followed” on their way through the room, either through a sufficiently long
time span or until they hit a surface defined as totally absorbing (see Figure 4.13 ). The
seating area in, for example, a concert hall, is a surface of the latter type. What is a
“sufficiently” long time if such a surface does not exist? Pragmatically, one may choose
the time according to the energy left in the ray after a certain time interval but there are
also implementations where the last surface point hit is defined as a new source, in its
turn emitting the rest energy of the ray, contributing to the reverberant energy in the
room.
Figure 4.13 The principle of ray tracing.
A major problem using ray tracing is that a ray, per definition, has no extent, i.e. in
practice it almost never hits a receiving point. This implies that the detectors
(“microphones”), which shall record the rays hitting a given surface and thereby the
magnitude and direction of the intensity, must be quite large. One may apply spherical
microphones having a diameter in the range of one metre. Certainly, applying a very
large number of rays, one may reduce the diameter but there is also the question of
calculating time. There are alternative measures, such as using a beam having the shape
of a cone of pyramid, but in effect, these are models of a hybrid type (see below).
One will also encounter the notion of “sound particle” instead of the ray and
thereby the concept of sound particle tracing (see e.g. Stephenson (1990)). The algorithm
to calculate the trajectories is the same; the sound particles or phonons propagate along
rays. The differences are found on the receiving side; i.e. how the detectors are arranged
and how the energy is calculated. In principle, however, it is still a ray-tracing method.