Iron dpa This iron displacement cross section corresponds to the ASTM E693-17 recommended displacement damage function for use in iron and low alloy steels (95% to 100% iron). The response function is useful as an exposure parameter and is used to correlate radiation-induced damage to iron that is related to microstructural changes in the metal, e.g. embrittlement and void swelling. A critical application is in reactor pressure vessel surveillance programs where this correlation is use to relate radiation-induced changes in materials exposed in accelerated surveillance locations to the conditions of the pressure vessel. This response function has units of displacement per atom (dpa). The tabulation uses a histogram representation and is presented in the SAND-II 640-group energy structure. Because use of this functional form is required within the standard, ASTM E693-17 does not report an energy-dependent uncertainty for this response function. The absolute accuracy of the dpa calculation is not important when dpa is used as a correlation parameter for neutron irradiations, so long as the same response function is used by all laboratories in calculating dpa. The absolute uncertainty is estimated to be 40% or more when applied to a light water reactor spectrum. For light water reactor applications, the relative accuracy of the dpa calculation estimated to be less than 10%. This response function was derived using the ENDF/B-VI cross sections (which are identical to the ENDF/B-VII.1 cross sections for the iron isotopes), the Robinson damage partition function, an effective displacement threshold energy of 40 eV, the Norgett-Robinson-Torrens (NRT) treatment in the displacement threshold region, and the beta=0.8 atomic scattering correction factor within the NRT formalism. The NRT equation is used to convert a damage energy into a number of displacements. It applies to naturally occurring iron, i.e. it represents a composite of the isotopic (Fe-54, Fe-56, Fe-57, and Fe-58) microscopic displacement kerma factors properly weighted by the natural abundances.