Modification of river flow from engineering activities often affects salini
ty and the mixing of fresh and saltwater in tidal rivers. In this study, an
empirical relation between subtidal salinity and gradually varying freshwa
ter inflow at a given station in the Apalachicola River, Florida, was devel
oped and tested with field observations. A time series of subtidal salinity
was obtained by low-pass filtering of the instantaneous salinity to elimin
ate the tidal signal. Based on the one-dimensional balance theory between a
dvection and diffusion of salt, the time series of subtidal salinity was di
rectly correlated to the gradually varying freshwater input by an exponenti
al equation. With field observations obtained from the Apalachicola River,
the empirical constants were obtained by regression. The correlation betwee
n observations and the results from the empirical equation were very good.
This simple empirical relation may be used by water resource engineers and
managers in preliminary studies to quickly estimate the potential impact of
water resource planning on subtidal salinity at a given location in a tida
l river.