CRWA in the NewsCRWA
creates a water budget CRWA was selected to perform a statewide
water budget analysis for the Executive Office of Environmental Affairs
for 351 towns in Massachusetts. Our ground-breaking work in water
budgeting began in the Charles River watershed, but is applicable in other
watersheds as well. A water budget, comparable to balancing a checkbook,
accounts for the amount of water that enters or leaves a watershed while
quantifying the human impact on streamflow. This project, which commenced
in November 2005 and will continue until June 2007, dovetails with
CRWA’s flow trading efforts. Statewide maps of streamflow stress will
aid in prioritizing restoration efforts and could form the basis for
initiating a trading program using water banking. For several years CRWA scientists have
calculated water use patterns for all the months and all sub-watersheds
ranging in size from one to five square miles. This water budget approach
includes water lost from well withdrawals, transfers via water supply and
wastewater pipes, and evaporation from irrigation. Also accounted for is
reduced recharge from impervious surfaces (roads, parking lots, buildings)
as well as flows returned to the ground from septic systems. CRWA
scientists compare these water losses against data on natural streamflow
in each sub-watershed to determine the level of human impact on rivers and
streams. CRWA maps these results, which graphically depict river flow
variations from month-to-month and the magnitude and timing of the human
impact on all the sub-watersheds. CRWA applied this
specialized methodology to the Town of Blackstone to help prioritize
recharge sites since the Blackstone River sub-watershed is impacted by
water withdrawals, a large amount of impervious area, and wastewater
losses. The town´s water budget calculation identified the Lower Mill
River and the Quick River as the most stressed sub-watersheds in the town,
primarily because the public water wells are in, or near, their
sub-watersheds. The impacts of impervious surfaces and sewering were
greatest in the spring since high groundwater levels aid infiltration into
sewer pipes, and runoff from impervious surfaces is not absorbed by
adjacent soil. The impacts of pumping and irrigation peak in the summer.
Streamflow impacts were greater in the summer when streamflows are
naturally low. But with more development there will be more withdrawals,
irrigation losses, impervious areas, and sewered areas, which will further
reduce streamflows in the town. Newton is different from Blackstone in a number of
ways. Newton does not have any public water supply wells so there is no
direct local impact in any sub-basin from a public water withdrawal well.
There are a number of small golf course wells but their cumulative
withdrawal volume is small. The impact of the evaporation losses from
irrigated lawns is likely to be somewhat larger because, even though both
communities have similar summer-to-winter ratios of water use, there are
many more residential lots in Newton. Newton is on the MWRA water supply
and sewer system so more water leaves as wastewater than is supplied. This
apparent anomaly is because groundwater and stormwater leak into the sewer
system and augment the outgoing wastewater flow. The net amount of water
lost could be fairly large because of Newton´s large population. Newton
is also more highly paved than Blackstone so more recharge is blocked from
entering the groundwater. Nigel Pickering, Senior Engineer and
Project Manager, is CRWA´s computer modeling and mapping expert. He
earned his PhD in Agricultural Engineering from Cornell University. |