Abstract

The Patuxent River flows into the Chesapeake Bay from its western shore. Historically, the river has been implicated as having been contaminated with copper since the mid-1960's when a steam electric generating plant was built at Chalk Point, 35 km from the mouth of the river . Greening of oysters was noted by Roosenberg (1969) who reported copper levels in oysters from trays set close to the outfall in excess of 1000 μg g dry weight ' . It was claimed that the copper contamination derived from the coppernickel condenser tubing used for cooling two of the four generating units at the Chalk Point Plant . Units 3 and 4 used cooling towers for cooling purposes . In the early 1980's, a detailed study of copper output from the plant was undertaken in this laboratory and by Abbe & Sanders (1986) . The Abbe and Sanders (1986) study was confined to the immediate vicinity of Chalk Point, whereas the current study was extended from Holland Cliff (River Km 45) to Solomons, 3 km from the river mouth. Data describing dissolved and particulate copper concentrations in Patuxent River water have been described in a companion paper (Wright & Zamuda, 1990), which creates a budget for copper input to the river . In the current paper, we describe the bioavailable copper in the Patuxent River as defined by body burdens in

Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call