Reports

Estimation of areas contributing recharge to selected public-supply wells in designated Metro Core Areas of Upper Wicomico River and Rockawalking Creek Basins, Maryland

2001, Andreasen, D.C. and Fewster, T.B.

Open File Report 2001-02-14

Key Results

Contributing areas of existing and hypothetical public-supply wells screened in the unconfined Salisbury aquifer in the Upper Wicomico River Basin and th e Metro Core Area west of that basin (Rockawalking Creek study area) were determined using two separate finite-difference , ground-water-flow models (MODFLOW) and a particle-tracking routine (MODPA TH). The contributing area of a pumping well is the area supplying recharge to the well from precipitation. The Salisbury aquifer, which is a shallow, water-table aquifer with relatively high transmissivity, is vulnerable to contamination. The mapped contributing areas can be used in the development of a well-head protection plan to protect s upply wells from contamination. The wells selected for analysis include ity of Salisbury Park.wells 17 and 18, other public-supply wells serving 25 people or more such as mobile-home parks and some commercial wells, and hypothetical production wells. Contributing areas of all other public-supply wells operated by U1e City of Salisbury were determined in an earlier study. The key results of the study include:

UPPER WICOMICO RIVER BASIN

• The 50-year contributing area of City of Salisbury Park wells 17 and 18, pumping at a simulated rate of0.36 million gallons per day, form an elongated pattern that extends approximately4 miles from the wells in an eastnortheast direction. Minimum travel time was 242 and 425 days for wells 17 and 18, respectively. (p. 8)
• The 50-year contributing area of 14 public-supply wells or well fields range in length from 0.25 to 3.2 miles and width from 0.1 to 0.5 miles and are either contiguous with the wells or occur at distances up to 1.8 miles from the wells. (p. 10)
• The 50-year contributing area of three hypothetical wells pumped simultaneously at 2 million gallons per day and located in the paleochannel range in length from 1.3 to 4 miles and width from 0.3 to 1 miles. The 50-year contributing area of a hypothetical well pumped at 0.36 million gallons per day and located in the Park well field was 3.5 miles long and less than 0.2 miles wide. (p. 11)
• Particles tracked forward from the West Road rubble landfill and an application area of waste-water sludge are intetcepted by Paleochannel well 1 after 26 and 7 years, respectively. Particles tracked forward from two hazardous-waste sites are not intercepted by public-water supply wells. (p. 11)

ROCKAWALKING CREEK STUDY AREA

• Currently there are no public-supply wells pumping from the Salisbury aquifer in the Rockawalking Creek study area. The 50-year contributing area of three hypothetical wells pumped independently at 0.25 million gallons per day range in length from 0. 7 to 1.6 miles and width from 0.5 to 0.65 miles. Minimum particle travel time ranged from 62 to 95 days. (p. 33) When the pumping rate is increased two-fold (0.5 million gallons per day) the 50-year contributing area expands down-gradient (southward) an additional 0.28 miles. (p. 33)
• Water for potable use in the Salisbury aquifer is currently limited to domestic supply from individual wells. The 20-year contributing area for clustered domestic wells within subdivisions are generally localized, occurring within 500 to 2,500 feet from withdrawal sites determined by particles backtracked from the midpoint of the aquifer. The average particle travel time was 6.8 years. (p. 37)

Downloads and Data

Open-File Report 2001-02-14 (pdf, 23 MB)

(Plates 1 - 3 are not currently available)