Biochemical oxygen demand modeling in a river involves derivation and
solution of the governing partial differential equation which describe
s concentration change with time and space brought on by convective, d
ispersive, and decay processes and the loading function. In this study
, a sinusoidal variation in waste discharge concentration is considere
d. The governing partial differential equation is solved analytically
by a transform method and by assuming that the solution varies periodi
cally in time. The concepts of memory length and memory time are used
to indicate when the solution becomes quasi-steady (periodic). The ana
lytical solution is compared with two other solutions. The three solut
ions produce comparable results. However, the analytical solution is m
uch easier to apply. The analytical solution extends the number of bou
ndary conditions which a modeler can apply to describe real engineerin
g problems.