Stream nutrient retention was examined in three adjacent agricultural catch
ments (Cherokee Creek, Cloud Creek, and Dry Creek) in the Ozark Plateau. Re
tention efficiency was measured using short-term nutrient and tracer inject
ions to estimate nutrient uptake length (S-w) during summer 1999 and winter
2000. A one-dimensional transport model was used to estimate dispersion, t
ransient storage size, and exchange. Soluble reactive P (SRP) and NO3-N con
centrations were least in the stream with the lowest proportion of pasture
in the upland (Dry Creek), whereas concentrations and land use were similar
in Cherokee Creek and Cloud Creek. Water column SRP concentrations were si
milar between seasons in all streams, but NO3-N concentrations varied signi
ficantly. Injected NO3-N was not significantly retained in these systems, p
robably because the streams were saturated by ambient NO3-N concentrations
(greater than 0.1 mg L-1). Phosphorus was retained during summer injections
(S-W ranged from 200-900 m), but S-W regressions were not significant in w
inter Variation in catchment land use was not a major determinant in P rete
ntion during summer, but stream hydrology, such as discharge and transient
storage, was a regulating factor Therefore, land use changes that alter str
eam hydrology may have a greater impact on P retention in these streams.