Abstract
The MnFe differential cross section is measured at MeV\@. The Fe level density obtained from neutron evaporation spectra is compared to the level density extracted from the FeHe,Fe reaction by the Oslo-type technique. Good agreement is found between the level densities determined by the two methods. With the level density function obtained from the neutron evaporation spectra, the Fe -strength function is also determined from the first-generation matrix of the Oslo experiment. The good agreement between the past and present results for the -strength function supports the validity of both methods and is consistent with the low-energy enhancement of the strength below MeV first discovered by the Oslo method in iron and molybdenum isotopes.
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