Animal manures are an important source of N for crop production. Effic
ient use of manure is necessary to increase N recycling, eliminate exc
essive purchase of fertilizer N, and reduce N loss to the environment.
An estimate of the annual rate of organic N mineralization in manure
is a necessary prerequisite to efficient manure N management. A minera
lization or decay series for the organic N in dairy manure was estimat
ed for corn (Zea mays L.) production from several field experiments ov
er a 5- to 8-yr period. Four rates of sidedressed fertilizer N (0, 56,
112, and 224 kg N ha-1) were superimposed over several spring-applied
manure treatments ranging from 0 to 168 Mg ha-1 yr-1. Ammonia volatil
ization from manure was encouraged, to allow for an assessment of the
fertilizer N equivalence of the more stable organic N fraction. Based
on silage dry matter yield and N uptake, a decay series of 0.16, 0.10,
0.03, 0.03 and 0.02, and 0.21, 0.09, 0.03, 0.03 and 0.02, respectivel
y, described the fertilizer N equivalence of organic N. The first numb
er in the decay series estimates the fraction of organic N that is ava
ilable for crop use during the year of application, and the second to
fifth numbers are estimates of available N from residual N in Years 2
through 5. An independent set of field data was used to evaluate the a
ccuracy of the decay series. The predicted decay series, based on dry
matter yield (R2 = 0.16) was more variable than the corresponding deca
y series based on N uptake (R2 = 0.72). The non-N effects of manure we
re insignificant, and therefore yield and N uptake were directly relat
ed to the N contribution.