Abstract
The suspended sediment discharged by the Susquehanna River at Havre de Grace, Maryland, during the year 1 April 1966 through 31 March 1967 is estimated to be about 0.60×106 metric tons. This estimate is based on daily river discharge records from the Conowingo Hydroelectric Plant, and on 34 determinations of the depth distribution of suspended sediment at a station in the Susquehanna River off Havre de Grace. Approximately 70% of this total of 0.60×106 tons, or about 0.42×106 tons, was discharged during the period of peak river flow in February and March.
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Contribution No. 117 from the Chesapeake Bay Institute and the Department of Oceanography, The Johns Hopkins University. This work was supported by the Department of Chesapeake Bay Affairs and the Bureau of Commercial Fisheries, Department of Interior, under Public Law 88-309.
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Schubel, J.R. Suspended sediment discharge of the Susquehanna River at Havre de Grace, Maryland, during the period 1 April 1966 through 31 March 1967. Chesapeake Science 9, 131–135 (1968). https://doi.org/10.2307/1351255
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DOI: https://doi.org/10.2307/1351255