There is a place just outside of
Colfax, WI, off of highway 40, where a person can put on some waders, step into
a stream, and imagine that they are a pioneer exploring their way through new
territory. I have been to this place where the silt grabbed at my feet and the
water flirted dangerously close to the tops of my waders. Eighteen Mile Creek
is beautiful. It looks pristine as it rustles softly over the rocks at its
bottom, but this creek has a secret that it shares with many other streams and
rivers in the Red Cedar Watershed. It is absolutely full of P.
P is the symbol for the element
phosphorus which is a widely used additive to agricultural fields because it is
an essential nutrient for plant
growth. It is only present in the earth as nonrenewable mineral deposits which must be mined and manufactured
into fertilizers. Once P is applied to the field approximately 80 to 85% of it is immobilized by a
reaction with Ca, Fe, or Al ions present in the soil making that P unavailable
to plants.
After application P can be mobilized through surface flow, which
is one of the main ways P moves from agricultural systems to surface water. A
major source of surface flow is row
crops due to the large amount of bare
soil that is exposed for a majority of the year. Insoluble P is bound to
eroded soil particles. When rain falls on bare soil it detaches soil particles
and causes additional erosion via runoff. Both runoff water and soil are unavailable to plants. While not readily
available to most organisms, insoluble P can become a long-term source of soluble P once it has entered aquatic systems.
Unlike many other nutrients
essential to plant life that have an atmospheric pathway as part of their
biogeochemical cycle, the phosphorus
cycle is strictly geologic in nature. Once P has found its way into a
system it is very hard for the system to balance it out. In aquatic
environments the element phosphorus is often a limiting factor to plant growth.
However, in the Red Cedar Watershed P
has become abundant. This has led to ongoing water quality issues like
algal and cyanobacterial blooms that pose hazards to both human health and
ecosystem integrity.
The LAKES REU biology team analyzed
stream sediment from Wilson and Eighteen Mile Creeks to determine its
composition and viability for different reclamation measures focusing on
phosphorus as well as potassium, soluble salts, and regulated heavy metal
content. We found that the levels of heavy metals were well below the ceiling
limits set by the EPA. This indicates that sediment collected from the Red
Cedar Watershed could be safely applied to land as a soil additive. Monitoring
of all the heavy metals found within the sediment would have to be done each
time it is pulled from the stream for the purpose of a nutrient additive,
including mercury which was not done in our study. The sediment in both streams
was found to have sufficient amounts of soluble P for corn growth. This
indicates that the stream sediments could be used as a fertilizer and replace
traditional sources of P.
Halfway down the stream I wanted to
stop wading. It was too deep. The mud was too sticky. The bottom of the stream
was so stirred up I did not know where I was putting my feet. My next step
could lead to slipping, sticking, or topping my waders. I watched my teammates
forging ahead, one fearless and the other one slow and deliberate. Did they
make mistakes? Yes. A number of times I watched them slip, backtrack, get stuck
in the mud, and even top their waders. They kept going and so did I. In the end
we got all of our samples. Taking sediment from the streams is a mitigation
strategy. It would allow us to stop inputting new phosphorus into our
waterways. It would help prevent the problem from getting worse. It has been
done in other watersheds just like fish exclusions, common carp fishing,
constructed wetlands, floating islands, sediment traps, and dredging. What
other watersheds have done are paths we could follow.
We have a choice. We can either
stand uncertain and stuck in the mud or we can begin wading forward. We know
what waits for us if we stand still. The deceptively clear water of our streams
turns green and smelly when it flows into our lakes every summer. If we begin
wading forward, trying out different mitigation strategies, we might get wet or
even stuck in the mud but at the end of our stream we might find a clear lake,
shimmering in the sun. Wouldn’t that be worth a muddy, water logged pair of
waders?
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