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

O. Pinto Jr., W.D. Gonzalez

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.



Keywords


componente difusa; semi-unidirecional; método de monte carlo



DOI: http://dx.doi.org/10.22564/rbgf.v4i1.1033







 

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