Cálculo da Componente Difusa entre 30-150keV em 4g.cm2, para um Detector Semi-Unidirecional utilizando o Método de Monte Carlo

Abstract

Results on the propagation of the X-ray diffuse component in the atmosphere, using the Monte Carlo method, are presented. A comparison of this method with the one that assumes only the direct component is performed, showing that the scattered component must be considered in the total flux.