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Frederick B. Gay

Publications and source records attributed to Frederick B. Gay.

10 recordsLinked to original sources

Distribution of polychlorinated biphenyls in the Housatonic River and adjacent aquifer, Massachusetts

Polychlorinated biphenyls (PCB's) are sorbed to the fine-grained stream-bottom sediments along the Housatonic River from Pittsfield, Massachusetts, southward to the Massachusetts-Connecticut boundary. The highest PCB concentrations, up to 140,000 micrograms per kilogram, were found in samples of bottom material from a reach of the river between Pittsfield and Woods Pond Dam in Lee, Massachusetts. Sediments in Woods Pond have been estimated to contain about 11,000 pounds of PCB's. Approximately 490 pounds per year of PCB's have also been estimated to move past the Housatonic River gaging station at Great Barrington. The distribution of hydraulic heads, water temperatures, and concentrations of dissolved oxygen, ammonia, nitrate, iron, and manganese in ground water shows that industrial water-supply wells in a sand and gravel aquifer adjacent to a stretch of the river called Woods Pond have been inducing ground-water recharge through the PCB-contaminated bottom sediments of the pond since late 1956. These data indicate that, at one location along the shore of the pond, the upper 40 feet of the aquifer contains water derived from induced infiltration. However, this induced recharge has not moved PCB's from the bottom sediments into a vertical section of the aquifer located 5 feet downgradient from the edge of Woods Pond. Samples taken at selected intervals in this section showed that no PCB's sorbed to the aquifer material or dissolved in the ground water within the detection limits of the chemical analyses.

Water Supply Paper

Hydrologic data of the lower Merrimack River basin, Massachusetts, from Concord River, Lowell, to Plum Island, Newburyport

The lower Merrimack River basin study area drains approximately 180 square miles along the New Hampshire border in northeastern Massachusetts. This area includes parts of the Merrimack River basin within Massachusetts east of the Beaver Brook and Concord River basins, except for the Shawsheen River basin. Even though the Blackwater River basin within Massachusetts isn't part of the lower Merrimack River basin, it has been included in this report. Principal tributaries to the Merrimack River, which discharges to the Atlantic Ocean at Newburyport, Massachusetts, are: Bare Meadow, Bartlett, Cobbler Creek, Fish, Richardson, and Trull Brooks, Artichoke, East Meadow, Indian, Little, Powwow, and Spicket Rivers, and Johnson Creek.

Massachusetts

Hydrologic data of the Shawsheen River basin, Massachusetts

The Shawsheen River basin drains a 77-square-mile area northwest of metropolitan Boston in eastern Massachusetts and discharges into the Merrimack River. Principal tributaries to the Shawsheen River are: Content, Elm, Heath, Hussey, Kiln, Rogers, Spring, Strong Water, Vine, and Webb Brooks.

Massachusetts

Hydrologic data of the Lake Cochituate drainage basin, Framingham-Natick, Massachusetts

Lake Cochituate is about 16 miles due west of Boston, Massachusetts, in the southeastern part of Middlesex County. The drainage basin is 17.7 mi 2 at the outlet of Lake Cochituate in Framingham. Principal tributaries to the lake are Beaverdam, Course, Pegan, and Snake Brooks. Beaverdam and Course Brooks flow into Fisk Pond, which empties into Lake Cochituate, whereas Pegan and Snake Brooks flow directly into Lake Cochituate. Surface drainage from the outlet of Lake Cochituate flows along Cochituate Brook into the Sudbury River at Framingham. The Cochituate Basin is in the center of the Sudbury River basin, which flows northeastward into the Concord River, a tributary of the Merrimack River.

Massachusetts