By Harrie Stewart Wilson Massey, E. H. S. Burhop
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Additional resources for Electronic and Ionic Impact Phenomena I
In regard to the second requirement, however, our detailed knowledge of reaction crosssections at all energies of the different radiations is imperfect, in particular for neutrons. This knowledge gap introduces errors into the calculated values of the geophysical parameters. Consequently, the desirability of each available approach to solving the direct problem will be determined by the nature of the problem. Frequently, the best approach is to use a mixture of different modelling strategies appropriate to the application sought.
The diffusion length or the photoelectric cross-section) serve as the inputs for the computations. The calculations made for these parameters are an essential part of the algorithmic process for resolving the interpretational relationships and are based on what is known beforehand about the properties of the particular material. The computations must also take into account the variation of the reaction cross-sections with the energy of the radiation. The first requirement presents neither a disadvantage nor a problem.
G. the diffusion length). g. the iron concentration in manganese ore). g. the porosity of water saturated pure sandstone samples and the neutron slowing-down length. g. the diffusion length or the photoelectric cross-section) serve as the inputs for the computations. The calculations made for these parameters are an essential part of the algorithmic process for resolving the interpretational relationships and are based on what is known beforehand about the properties of the particular material.