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Tracking
Water Movement
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Art Gold, Professor
Department of Natural Resources Science
Art Gold's research focuses on coastal watersheds
and water quality, in particular, the role of riparian wetlands
on the export of nitrate from coastal watersheds. As head of URI's
Cooperative Extension Water Quality Program, he oversees community-based
watershed education.
Peter Groffman, Scientist
Institute of Ecosystem Studies
Peter Groffman is a terrestrial microbial ecologist
at the Institute of Ecosystem Studies in Milbrook, New York. His
research interests include nutrient cycling and transformation of
environmental pollutants in wetlands, forests, agro-ecosystems,
and groundwater.
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We are on the verge of a new
frontier in watershed science. Watersheds are now recognized by local, state,
and federal decisionmakers as natural units that bind and integrate seemingly
disparate lands, communities, and ecosystems. In the near future, we can
expect to see an increase in the deliberate coordination of watershed activities
with the expectation of measurable improvement in the value or function
of a particular watershed. This new recognition of the value and importance
of the watershed approach represents a huge challenge to scientists. Over
the next decade or so, scientists who study processes at a watershed scale
(watershed scientists) will be called upon to provide solutions to real
and complex problems using the tools and knowledge that have been developed
over the last 30 to 40 years of watershed research.
It will not be easy to find these solutions.
Nitrogen delivery to coastal waters provides an excellent illustration of
the complexity of environmental science and management and shows how environmental
problems require multidisciplinary solutions. Because these problems are
created and driven by human behavior, our solutions are ultimately constrained
by human values and decisions that are difficult to predict and manage.
A major focus of estuarine managers is the
control and reduction of nitrogen from coastal watersheds. In the Chesapeake
Bay, Puget Sound, and Rhode Island's salt ponds, nitrogen inputs from the
watershed degrade water quality. The nitrogen generates excessive algal
blooms that create a cascade of events resulting in depletion of dissolved
oxygen, buildup of organic deposits, and a loss of valuable aquatic habitat.
At first glance, it would appear that scientists and managers have a simple
and forthright method to evaluate the outcome of their watershed nitrogen
control strategies. We can measure the changes in nitrogen output of estuarine
tributaries in relationship to changes in management.
However, watersheds continue to baffle us.
In a recent study, Thomas Jordan and his colleagues at the Smithsonian Environmental
Research Center in Edgewater, Maryland, examined nitrogen inputs and outputs
from 17 small (100 to 2,000 hectares) subwatersheds that contribute to the
Chesapeake Bay. Although they found that nitrogen discharge increased as
the anthropogenic input of nitrogen to a watershed increased, they could
not determine the fate of 70 to 85 percent of the nitrogen that entered
those watersheds. The investigators suggested that the nitrogen they could
not account for might have been removed by or stored in plants, soil, groundwater,
and riparian wetlands, and that some of the nitrogen might be residing in
groundwater that was slowly moving towards surface waters.
Why all the mystery about nitrogen in these
watersheds? Watersheds suffer from nonuniqueness, a mathematical modeling
term used to describe situations where a particular outcome can result from
a multitude of input scenarios. At a river mouth, the nitrogen in a single
gallon of water may originate from a variety of places and at different
times. The water may contain nitrogen that entered the watershed from human
or animal waste, precipitation, or fertilizer. The nitrogen pool may contain
atoms that have resided within the watershed for widely different time periods.
Some of the nitrogen may have entered the watershed as precipitation on
streets or sidewalks that drain directly into storm drains and then traveled
to a river mouth within hours or days. Other nitrogen may have entered the
water from septic system effluent and then traveled through the groundwater
for years before emerging as springflow that feeds streams and rivers.
The nonuniqueness of watersheds compels watershed
scientists to grapple with the cohesiveness of the land areas that they
study and manage. We work to define the major sources of specific materials,
we identify the flow paths of those materials (which might include infiltration
to the groundwater, overland runoff, or interaction with wetlands), and
we investigate the fate and transformations that occur as a specific constituent
moves from its source to its final outlet at the sea. In our watershed research,
we examine the role of landscape setting on nitrogen removal capacity of
riparian wetlands. Our research integrates several landscape attributes,
including geomorphology, hydrology, and soils. We conduct process-level
studies to examine how and why groundwater nitrate is altered within the
biologically-active, saturated soil in a riparian zone. We then couple our
process-level information with estimates of groundwater flow paths to evaluate
the role of riparian zones at the watershed scale. (See illustration at
left.) The challenge is to identify the mix of attributes that generate
effective nitrogen retention zones and incorporate them into management
support tools that have relevance beyond the specific watersheds that we
study.
When confronted with
the variability and uncertainty generated by the interactions of localized
phenomena, scientists often move to a coarser scale of evaluation to find
order and meaningful relationships. We find that nitrogen export to a coastal
estuary is related to human and animal population densities within a watershed.
However, stepping back to a coarser scale of resolution is no help to watershed
decision makers who demand finer scales of analyses. They target their activities
to specific locales or land-use types to maximize the effect on a given
watershed value or function. If the goal is to reduce nitrogen export to
coastal waters, how do we balance restoring riparian buffers with upgrading
septic systems and reducing atmospheric deposition? Can scientists identify
landscape characteristics that result in hot spots of nitrogen pollution?
Can we identify natural features that have great potential to remove nitrogen?
Can we manage certain vegetated ecosystems to store nitrogen for decades
or longer? Most importantly, can we create and test models that demonstrate
the linkages between source areas that contribute nitrate to the watershed
and sink areas that remove nitrogen from the watershed? And finally, how
can we get people to institute the solutions that scientists and land managers
develop?
Watershed science in 1999 is analogous to
smoking research in 1969. In 1969, researchers knew in a broad sense that
smoking was bad and that people shouldn't do it, just as we know today that
there are strong links between specific human activities and nitrogen delivery
to coastal waters. However, in 1969 we could not describe the specific mechanisms
that damaged human health, just as we cannot account for the specific fate
of nitrogen in watersheds today. And most importantly, we couldn't, and
still can't, figure out how to get people to stop smoking, just as we can't
get people to implement effective nitrogen controls. The same interplay
of scientific knowledge, values, economic interests, and behavior that make
smoking cigarettes a complex problem, are the same issues that complicate
watershed management. This complex interplay suggests that watershed science
will be exciting and challenging for several decades to come.
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