The Influence of Groundwater on Nitrogen Delivery to the Chesapeake Bay
By Scott W. Phillips and Bruce D. Lindsey
Summary of Major Findings:
- Resource
managers need to understand the "lag time"
between the implementation of management practices
and improvement in water quality in the Chesapeake
Bay to help develop future nutrient- and sediment-reduction
strategies. One factor affecting the lag time
is the influence of Groundwater on the transport
of nitrogen to streams in the Bay watershed.
- Groundwater supplies a significant amount (about half)
of water and nitrogen to streams in the watershed
and is therefore an important pathway for nitrogen
to reach the Chesapeake Bay.
- The
age of Groundwater in shallow aquifers in the
Chesapeake Bay watershed ranges from modern
(less than 1 year) to more than 50 years, with
a median age of 10 years.
- In
addition to Groundwater, stream water will
be influenced by surface runoff and soil water.
Runoff and soil water both have very young ages
(hours to months) and supply, on average, about
half of the water to a stream.
- Proposed water-quality criteria in the Bay probably will not be met by 2010 due to the time needed to implement management practices and the effects of Groundwater and other watershed properties on nutrient transport.
