Total suspended sediment (TSS) concentrations and their nutrient composition were studied in discharges from seven contiguous small watersheds on the Atlantic Coastal Plain in Maryland for up to 22 yr. AU watersheds were equipped with V-notch weirs and volumeintegrating, Dow-proportional samplers. Spot samples were also taken for analysis of TSS concentrations and the composition of dissolved and particulate nutrients at known water discharge rates. Interannual variations in annual and seasonal precipitation during this study spanned approximately the range of 160-yr weather records in the vicinity. Mean annual TSS fluxes were 263,546, 134, and 92 kg ha-1 for the area-weighted mean of the overall Rhode River watershed, and for subwatersheds that were primarily-cropland, completely forested, and grazed, respectively. TSS fluxes were highest in the summer, foUowed by spring, winter, and faD. Regressions ofTSS Dux vs precipitation were used to calculate TSS fluxes for seasons and years with average, above and below the average precipitation. TSS Dux from the Rhode River watershed was 12-fold higher in very wet years than in very dry years and 271-fold higher in very wet summers than in very dry summers. At base Dow, TSS had high nutrient content, but as Dow rates increased TSS nutrient content rapidly declined. At base Dow, most of the totai-P, TPi, TKN, and organic-C was in the dissolved phase, while at higher flows, most of these nutrients were in the TSS phase.T HE DISCHARGE of total suspended sediment (TSS) from watersheds into receiving waters can become a serious problem when natural vegetation is replaced by agriculture or urbanization Reid and Frostick, 1994). TSS is, by weight, the most important aquatic pollutant and also contains large amounts of nutrients and other pollutants, some of which may later be released into the water column of the receiving waters. Many studies have measured the fluxes of TSS from small watersheds dominated by cropland (e.g., Alberts et al., 1978;Burwell et al., 1977; Schuman et al., 1973a,b ), pasture land (e.g., Doran et al., 1981;Owens et al., 1982Owens et al., , 1983a Owens et al., ,b, 1989 Schuman et al., 1973a,b;Smith, 1992), and forest (e.g., McDowell and Asbury, 1994;Naiman, 1982;Owens et al., 1983aOwens et al., , 1989. Other studies have measured TSS fluxes from larger mixed land use watersheds (e.g., Haith and Shoemaker, 1987;Jordan et al., 1986;Kronvang, 1992 Many studies also have examined the nitrogen and phosphorus content of the TSS discharged from study watersheds and compared this with the discharge of dissolved nutrients (e.g., Alberts et al., 1978; Cooke, 1988a,b;Duffy et al., 1978;McDowell and Asbury, 1994; Schuman et al., 1973a,b ). Some studies also measured the organic-C content of the TSS (e.g., Mulholland, 1981;Naiman, 1982;McDowell and Asbury, 1994). These studies concluded that most of the organic-P, TPi, and organic-N is discharged in the TSS. Many of these studies also developed regression models to describe the relationships among wat...