Typical diurnal variations of lagoon surface temperature and ammonia flux were observed during both the experimental periods. Also, an exponentially increasing flux with increasing lagoon surface temperature was observed. A simple linear regression relationship between the logarithm of ammonia flux and lagoon surface temperature was obtained, in good agreement with a similar relationship obtained earlier by some of the co-authors from measurements made at another farm(Farm 10) in eastern North Carolina. On closer examination of our new data, however, the difference, D, between the air temperature and the lagoon surface temperature was found to also influence the ammonia flux, especially when D > 0. This "hot air" effect is included in the multiple regression model obtained in this study. Some of the farm-related differences in the ammonia flux were eliminated or minimized in our statistical/observational model by considering the total emission from the lagoon, normalized by the total live animal weight at the farm.
Relationships between the lagoon ammonia flux/emission and relevant chemical parameters, such as pH and total kjeldahl nitrogen(TKN) were also examined. The lagoon pH stayed within a relatively narrow range from 7.7 to 8.5 during our fall and winter field campaigns, and no statistically significant correlation between ammonia flux and pH was found. Although, the TKN concentration was positively correlated with the lagoon ammonia flux, this correlation was confounded by significant seasonal variability of TKN concentration, with lower TKN values observed in fall with higher ammonia fluxes, and higher TKN concentrations observed in winter with lower ammonia fluxes.