Measurements of the sea-level μ-meson momentum spectrum made during the last decade utilizing conventional air gap spectrometers have indicated that the differential intensity is approximately proportional to 1/(momentum)3. For a study of the high-momentum region therefore, the instrument concerned not only must have a high angular resolution but also be able to accumulate data at a significant rate. These requirements can only be met with difficulty when conventional air gap magnets are used. This paper is concerned with the characteristics of a μ-meson spectrometer in which the air gap magnet is replaced by a block of lagnetized iron. Methods are given for computing the effects of energy loss and scattering in the material and it is shown that the angular scattering distribution produced by the iron in the unmagnetized state can be accurately predicted. Further since the magnetic material acts as a filter for nuclear active particles this type of instrument has all the advantages of operating underground while retaining the convenience of working at sea-level.
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