Prince William County encompasses approximately 44% of the Occoquan Watershed. More importantly, the watershed covers over two-thirds of the county’s land. Therefore, decisions made within Prince William County have wide-reaching consequences for all Fairfax Water customers and nearby groundwater users. Protecting the Occoquan Watershed and the regional water supply requires a thorough understanding of the impacts of ongoing and planned development.
The Occoquan Watershed Model was developed over several
decades to assess how land use changes affect the water quality of the Occoquan
Reservoir. It is currently being updated and new The Northern Virginia Regional Commission has operated this model
and plans to release its findings later this year. Despite this, the Board of
County Supervisors recently approved comprehensive plan changes that eliminated
the Rural Crescent and made sweeping land use changes without considering the
potential impacts on the water supply.
Rising Salinity and Its Implications
Salinity levels in the Occoquan Reservoir have been steadily
increasing and may be approaching a critical threshold. This rise in salt is
primarily attributed to watershed runoff—especially from road salting during
wet weather—and reclaimed water from the Upper Occoquan Service Authority
(UOSA) during dry weather. The sodium content in reclaimed water from UOSA
exceeds that of outflows from the two watersheds. As paved areas expand, salt
runoff into the watershed also increases.
The removal of salt from the drinking water supply would
require a major investment in desalination technology at regional water
treatment plants, which currently lack this capability. The estimated cost of
adding treatment lines at Fairfax Water to keep the Occoquan potable is between
$1 and $2 billion, a financial burden that would ultimately fall on water rate
payers, including the 350,000 public water users in Prince William County.
Urbanization and Watershed Health
The Occoquan watershed is frequently described as the most
urbanized watershed in the nation. Although more heavily urbanized areas exist
in the United States, these do not have functioning watersheds. Historically,
cities like New York, Philadelphia, Baltimore, and Washington have confined and
subsumed countless streams, erasing them and destroying their watersheds.
Scientific studies indicate that when 5–10% of a watershed
is developed, it begins to decline, though restoration is still possible for a
time. However, if urban land use surpasses this tipping point, water quality
ceases to respond to restoration efforts. Once a watershed is destroyed,
restoration may be impossible.
To avoid irreversible harm to the local ecology and regional
drinking water supply, it is essential to understand the impacts of planned
changes. The cost of restoring the basin and treating the water could reach
billions of dollars, a financial responsibility for residents. The Occoquan
Reservoir is a vital and irreplaceable component of the region’s water supply.
Average Water Flows to the Reservoir
|
Source |
Percentage (%) |
|
Bull Run Watershed |
25% |
|
Occoquan
River Watershed |
48% |
|
Groundwater and Other
Watershed |
20% |
|
UOSA
Reclamation Facility |
6% |
Initial development of previously open areas mainly causes erosion and sediment transport via stormwater into local streams. After development, the primary concern shifts to higher stormwater volume and velocity, resulting from loss of tree canopy and replacement of pervious surfaces with impervious ones such as roads, parking lots, rooftops, driveways, and patios. This leads to the disappearance of small streams and a reduction in groundwater recharge. Current stream monitoring by the Conservation District already shows troubling signs of declining tributary health.
Connection Between Surface Water and Groundwater
The US Geological Survey emphasizes that virtually all
surface-water features—streams, lakes, reservoirs, wetlands, and
estuaries—interact with groundwater. All water is interconnected, and
groundwater flow and storage are dynamic, constantly changing due to human and
climatic stress. Altering the land changes both the quality and quantity of
groundwater and streamflow.
Land use changes that increase impervious cover beyond 5–10%
from roads, pavement, and buildings have two significant effects: they reduce
open areas where rain and snow can infiltrate the ground and recharge
groundwater, and they increase stormwater velocity, preventing water from
percolating into the earth. This leads to more frequent flooding and less
groundwater recharge.
Over time, reduced groundwater levels transform perennial
streams into ephemeral ones, disconnecting groundwater from the surface water
network. Once watershed hydrology is destroyed by development, restoration is
extremely difficult, if not impossible. The Occoquan watershed is essential for
the region’s drinking water supply.
Emerging Water Quality Issues
According to Dr. Stanley Grant, emerging water quality
issues are mainly a result of the built environment. Ongoing development within
the Occoquan Watershed threatens the sustainability of the water supply for up
to one million people in northern Virginia. Population density increases lead
to a rapid rise in impervious surfaces once the density reaches 100 people per
square mile, accelerating the decline of the most urbanized watershed in the
United States.
Water’s Journey Through the Region