IMPROVING DRINKING WATER QUALITY BY BETTER UNDERSTANDING GROUND-WATER/SURFACE-WATER INTERACTION
This study focuses on improved assessment of the degree of hydraulic connection and contribution of surface water to well discharge using a combination of chemical, physical and biological indicators at a public-supply well site located within 100 feet of a stream-fed pond, not currently classified as GWUDI. Hydraulic head data confirm the development of a pronounced downward gradient in the pond bottom when the well is activated. Temperature profiles, measured in the pond sediments, suggest that infiltration is occurring, however, some of the temperature signature may be attributable to heat conduction rather than water flow. Chemical indicators including chloride, sodium, and calcium suggest the potential for surface water infiltration at this site. A mass-balance mixing model, using oxygen isotopes, confirms that a small percentage of the well water is derived from surface water. Results from two microscopic particulate analyses reveal that surface-water organisms are present in the well water. All together, if the surface water body became contaminated, this well's water quality would be impacted. Hence, the conjunctive use of these methods provides a better understanding of the degree and nature ground-water/surface-water interaction and would further strengthen the approach to public-supply protection.