DOSE CALCULATIONS IN PROTON-BEAMS - RANGE STRAGGLING CORRECTIONS AND ENERGY SCALING

Citation
Kr. Russell et al., DOSE CALCULATIONS IN PROTON-BEAMS - RANGE STRAGGLING CORRECTIONS AND ENERGY SCALING, Physics in medicine and biology, 40(6), 1995, pp. 1031-1043
Citations number
43
Categorie Soggetti
Radiology,Nuclear Medicine & Medical Imaging
ISSN journal
00319155
Volume
40
Issue
6
Year of publication
1995
Pages
1031 - 1043
Database
ISI
SICI code
0031-9155(1995)40:6<1031:DCIP-R>2.0.ZU;2-G
Abstract
Three-dimensional dose planning systems employing accurate proton tran sport algorithms are essential for calculating absorbed dose distribut ions in proton therapy. In this paper, a pencil beam algorithm for the transport of protons in materials of interest for radiation therapy i s developed. The Fermi-Eyges multiple-scattering theory is used to der ive transport equations for calculating proton fluence and absorbed do se distributions. The multiple-scattering theory of Moliere is used to predict mean square scattering angles and to develop an expression fo r calculating the root mean square (RMS) radial spread of a proton pen cil beam, as a function of depth, in an arbitrary scattering material. A correction factor is suggested to account for the decrease in the r adial spread at the end of the range due to range straggling. The effe cts of neglecting large-angle scattering events and the possibility of incorporating such events into the pencil beam algorithm are discusse d. An energy scaling technique for determining the water-equivalent su rface energy at a given depth in a heterogeneous scattering medium is developed. The water-equivalent energy, giving the same Moliere scatte ring parameter B in water, is determined and the 1/e angle in water is scaled to the appropriate width in the scattering material. By using stored analytically or Monte Carlo calculated pencil beam distribution s in water, the large-angle single-scattering events may be incorporat ed by approximating the scattering in an arbitrary material by the sca ttering in water for protons of the appropriate water-equivalent surfa ce energy.