Most measurements of dairy manure nitrogen (N) availability depend on net changes in soil inorganic N concentration over time, which overlooks the cycling of manure N in the soil. Gross transformations of manure N, including mineralization (m), immobilization (i), and nitrification (n), can be quantified using 15 N pool dilution methods. This research measures gross m, n, and i resulting from application of four freeze-dried dairy manures that had distinctly different patterns of N availability. A sandy loam soil (coarse-loamy, mixed, frigid Typic Haplorthod) was amended with four different freeze-dried dairy manures and incubated at 258C with optimal soil water content. The dilution of 15 ammonium (NH4 þ ) during a 48-h interval (7-9 d and 56-58 d after manure application) was used to estimate m, whereas the dilution of 15 nitrate (NO 3 2 ) was used to estimate n. Gross immobilization was calculated as gross minus net mineralization. Gross mineralization in the unamended soil was similar at 7-to 9-d and 56-to 58-d intervals and was significantly increased by the application of manures. For both amended and unamended soil, m was much greater (i.e., three-to nine-fold) than estimated net mineralization, illustrating the degree to which manure N can be cycled in soil. At the early interval, both m and i were directly related to the manure C input, demonstrating the linkage between substrate C availability and N utilization by soil microbes. This research clearly shows that the application of dairy manures stimulates gross N transformation rates in the soil, improving our understanding of the impact of manure application on soil N cycling.