The widespread use in medicine and biology of radioactive nuclides emitting beta particles has focused attention on the problem of the dose distribution in tissue corresponding to non-uniform distributions of the radioactivity. The problem has two aspects. First, the distribution of absorbed energy (i.e., dose) about a point source of beta particles must be inferred in some fashion. Second, this point-source energy-distribution function must be integrated over some distributed source, real or hypothetical, to get the dose distribution. For purposes of radiation dosimetry, it would clearly be convenient if the point-source distribution could be described by a reasonably simple mathematical function. The purpose of this paper is first to present such a function, then to indicate the extent to which this function fits available experimental data, and last to discuss the application of this function to beta sources distributed in tissue. Experimentally, the problem has been approached in two ways, indirect and direct. The first experimental work was done with the indirect method (5), which consisted in attempts to deduce the point-source distribution function from the appropriate mathematical manipulation of measurements made on plane sources in polystyrene. Some of the results by this method have already been reported (6). The direct experimental approach consists in measurements on point sources of beta particles in air. Such measurements have been made by Sommermeyer and Waechter in Germany (10, 11), Clark, Brar, and Marinelli in Chicago (1), and Emery in England (2). The data from these three sets of observers give a relatively complete and consistent picture of the point-source distribution in air. When representing the experimental data with a function for dosimetry purposes, it is quite satisfactory to account for 90 or 95 per cent of the energy, with reasonable accuracy. The remainder of the energy, distributed over the last quarter or third of the beta-particle range, will, in general, be of little biological significance. This allows the function to be run to infinity, which greatly simplifies the mathematics. The measurements on point beta-particle sources in air can be represented, with this degree of accuracy, by the following function: (1) This can be somewhat more conveniently written in terms of the dimensionless variable r = μx, and c = μx1. Then Equation 1 becomes (2) Now I is the point-source distribution function, that is, the absorbed energy per gram per disintegration, at a distance r = μx from a point source of beta particles.
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