Development of a Regional-Scale Model to Simulate Groundwater Flow and Nitrogen Loading in Watersheds Along the Connecticut Coast of Long Island Sound

Science Center Objects

In 2018 USGS began work on the development of a regional-scale groundwater flow model of areas along the Connecticut coast. The model will be used as a quantitative tool to evaluate groundwater flow and nitrogen loading to Long Island Sound.

Junction of the Yantic and Shetucket Rivers, Norwich, Connecticut

Photograph of the junction of the Yantic and Shetucket Rivers, where they combine to make the Thames River Estuary, Norwich, Connecticut.

(Courtesy of the Office of Long Island Sound Programs, Bureau of Water Protection and Land Reuse, and Connecticut Department of Energy and Environmental Protection)

    Aquatic systems in and around Long Island Sound (LIS) provide a variety of ecological and economic benefits such as flood and storm protection, water filtration, recreation, commercially and recreationally important fish and bird populations, and carbon sequestration. In 1985, the U.S. Environmental Protection Agency, States of Connecticut and New York, and other organizations formed the Long Island Sound Study to protect and restore LIS. In 1994, the LISS developed a Comprehensive Conservation and Management Plan (CCMP) to guide LIS restoration efforts. Reducing nitrogen loads to surface waters is identified in the CCMP as a priority for the region. Although measurable improvements in water quality have been made through controls on major point sources such as wastewater treatment plants, the CCMP identified reduction of nitrogen contamination from sources that are smaller, more diffuse, or more distant from LIS as an ongoing major challenge. Disposal of domestic wastewater to septic systems and application of inorganic fertilizers are the major nonpoint sources of nitrogen in the watersheds draining to LIS. Nonpoint source nitrogen can run off directly to streams and other surface-water bodies during storm events, or infiltrate to groundwater, affecting surface waters over longer periods of time. Legacy nitrogen loads from groundwater, directly to LIS and to stream networks in the watersheds draining to LIS, are difficult to estimate and relatively poorly understood.  

Watersheds along the Connecticut coast of Long Island Sound

Preliminary study area.

    A significant fraction of historical releases of nitrogen to watersheds in Connecticut may be present in the groundwater flow system because groundwater residence times (or travel times) in surficial aquifers can exceed 100 years and, consequently, may result in a multiyear lag between recharge at the water table and discharge to receiving waters. Lags can be evaluated by calculating travel times through groundwater flow systems to surface-water discharge points such as streams, ponds, or coastal embayments.

    In this study a groundwater flow model of the watersheds draining to LIS along the Connecticut coast is being developed to provide a regional tool to evaluate the groundwater flow systems in these watersheds. The model will serve as a framework for understanding the groundwater component of flow to the coastal embayments of LIS and for conducting more-detailed assessments of priority areas (for example, groundwater discharge rates, travel times, and nitrogen loading to coastal embayments in primary tier watersheds). Calculating groundwater discharge rates along with residence times will greatly enhance the ability of resource managers to prioritize nitrogen reduction strategies to the areas where the loads from groundwater are highest and the application of these strategies will be most beneficial.

    This study was initiated in late 2018 and will be completed by the end of 2020. It is being conducted in cooperation with the U.S. Environmental Protection Agency, Long Island Sound Program, and the Connecticut Department of Energy and Environmental Protection.