Project Title Virginia Beach Shallow Ground-Water Study Number VA113 Location Virginia Beach Cooperating Agency City of Virginia Beach Department of Public Utilities  Project Chief Barry Smith Period of Project 1996 to present

Virginia Beach Shallow Ground-Water Study

The City of Virginia Beach

Virginia Beach is a growing city in southeastern Virginia with a limited supply of fresh water. Most of the city’s drinking water, up to 45 million gallons per day, comes from Lake Gaston. The Lake Gaston pipeline supplies water for the northern half of Virginia Beach, but the southern rural boroughs rely solely on ground water (Johnson, 1999).

Privately owned wells also provide water from shallow depths throughout Virginia Beach. Supplies of ground water are limited, however, because of high concentrations of iron, manganese, chloride and (or) sulfide ions in some areas. The shallow aquifers are also dewatered by several open-pit mines. At depths greater than approximately 200 ft, the water is generally too saline to drink.

The purpose of the Virginia Beach shallow aquifer study is to better understand the distribution of fresh ground water, its susceptibility to contamination, and to its sustainability as a long-term water supply.

The city of Virginia Beach has a progressive interest in preserving the limited supply of usable ground water in the shallow aquifers for drinking water, irrigation, lawn watering, heat pumps, and potentially for desalination. The U.S. Geological Survey in cooperation with the City of Virginia Beach Department of Public Utilities began a cooperative study of the shallow aquifer system in 1996. 

Virginia Beach land use

During the study,  the USGS collected continuous cores and geophysical logs from the shallow aquifer system, established a water-level and water-quality network in the city, and revised the conceptual hydrogeologic framework of the shallow aquifer system (Smith and Harlow, 2002). The USGS also simulated ground-water flow and the distribution of saline water, as indicated by chloride concentration, in the shallow aquifers of the southern watersheds of Virginia Beach (Smith, 2003). Slow, but steady movement of chloride concentrations toward a hypothetical well field pumping from the York-Eastover aquifer was simulated, as well as, drawdowns around hypothetical open-pit mines in the Columbia aquifer.