Looking
into Earth's eye:
A watershed view of clear lakes by John A. Downing
In the mid-1800s,
Henry David Thoreau moved away from urban New England and spent
two years immersed in the daily observation of nature. He felt
that Walden Pond was the focus of the landscape, reflecting the
qualities of the surrounding terrain. When I returned to my native
Iowa in 1995, Thoreau's observations assumed new meaning.
In the years since Thoreau retreated to nature, Iowa's landscapes
were transformed from prairies and savanna with woodland-fringed
watercourses to some of the most agriculturally productive and
disturbed landscapes on the planet (read more about major
changes in the Iowa landscape).
Today, Iowa struggles with poor water quality, official labels
of impaired waters and the stigma of contributing to water quality
problems as far away as the Gulf of Mexico. Thoreau's perceived
connection between landscapes and lakes is underscored by modern
data-and our own eyes. The changes in Iowa's landscape are reflected
in Iowa's waters.
Watersheds
and Water quality
A watershed is all the land that drains into a river, lake or
other water body-so every lake is downhill from 100% of its watershed.
The watersheds of Iowa lakes average about 35 times the size of
the lake. Some lakes-such as Cold Spring, Little Wall and the
Iowa Great Lakes-have small watersheds relative to their areas,
while others have watersheds more than 100 times the lake area.
In other words, one acre of lake can receive run-off and nutrients
from a land area between 1 and 200 acres. Because of land disturbance,
fertilizer run-off, and soil loss in agricultural and urban environments,
lakes with high ratios of watershed area to lake area have the
poorest water quality.
For every ten gallons of rain that falls on the land, about three
gallons run off and head directly to the lake. The bigger the
rainfall, the higher the concentration of contaminants in run-off.
The faster this water moves, the more nutrient, soil and other
materials leave with it-and the water moves fastest when there
are no wetlands or other storage reservoirs to slow it down.
Even water that sinks into the soil often ends up in the lake.
Although soil can filter impurities from water, Bill Simpkins
of Iowa State University's Geology department has found that the
groundwater around Clear Lake now has much more nutrient than
normal-a pattern we'd expect to find in other Iowa watersheds
as well.
The linkages between watersheds and water quality are so tight
that measurements of water quality correctly predict the kinds
of land use in watersheds. The most important indicators of water
quality revolve around nutrient concentrations, particularly nitrogen
(N) and phosphorus (P). Kelly Poole of the Iowa Department of
Transportation has found that measuring the ratios of N and P
that end up in lakes allows one to predict the amount of animal
versus row-crop agriculture in watersheds. Livestock manures are
generally rich in P, while row crop fertilizers can be pure N.
Urban watersheds can have even tighter linkage because hard surfaces
lead to greater runoff.
The good news is that most water quality problems occurring in
lakes appear to originate in very small parts of watersheds. For
example, near Rock Creek Lake, we found that between 60-80% of
the nutrients and erosion came from 5-7% of the watershed. This
means that "surgical remediation," performed on the
most run-off prone lands, can solve some water quality problems
without major changes in overall land use. Likewise, because strings
of adjacent, erodible parcels of land can allow nutrient-laden
water to move quickly across watersheds, re-engineering watersheds
to slow water flow may also reduce water quality problems.
Human
values, nature's values
When I ask students how they sense good water quality, they are
about evenly divided between appearance and odor. Most people
like clear, blue water; a fresh scent; and a clean, healthy-looking
shore. Few like bright green or brown turbid water with a fishy
odor. More formal surveys show people want lakes that are (in
order) free from dangerous bacteria and toxins, clear, odor-free,
diverse in wildlife habitat and good for fishing.
A Clear Lake middle schooler summed it up well when asked what
changes we should make in Iowa lakes. "Get rid of the ugly
algae! It feels gross when it gets under your suit." She
was right. Cyanobacteria (the misnamed "bluegreen algae"
that plagues Iowa's most nutrient-laden lakes) can contain skin
and nerve toxins.
People value good water quality so much that some of Iowa's most
valuable "land" is water. Lakes like Clear Lake generate
revenues of tens of thousands of dollars per acre each year. Cathy
Kling and Joe Herriges of ISU's Economics Department have found
that both residents and visitors are willing to invest much more
for water quality improvement. Lake-use typically doubles with
improved water quality, making lake and watershed restoration
a very cost-effective investment. When Lake Ahquabi and its watershed
were restored, the Iowa Department of Natural Resources (DNR)
saw recreational use rebound to unprecedented levels.
So how should we make that investment? As noted above, attempting
to improve water quality without landscape change is a wasted
gesture. Don Bonneau of the Iowa DNR says that there is little
point in fixing a lake until you fix the watershed. Everything
we learn about Iowa lakes shows this to be true.
Restoring watersheds for
water quality: a Clear Lake example
The remediation project undertaken by the Clear Lake community
is a good model for many other Iowa lakes. Once funding is in
place, this will be the largest lake and watershed restoration
undertaken in the state.
Clear Lake's water quality has declined over the last century
(read about major changes) due to
increased phosphorus and nutrient loads from the watershed. Decreased
water clarity has reduced the diversity and abundance of aquatic
vegetation while allowing carp to exacerbate water quality problems
by digging up sediment and destroying wetland habitat.
The key in this and other Iowa watersheds is to target the parts
of the watersheds that will make the greatest difference to water
quality-then take specific steps to decrease nutrient concentrations
on the land, slow water transport across watersheds and alleviate
erosion.
Reduce nutrient load: Unchecked erosion, improper sewage disposal
(animal or human), overzealous fertilizer applications and other
poor watershed practices can overload lakes with nutrients. Excessive
nutrients cause eutrophication, an overproduction of plant life.
Eutrophication can give lakes uncontrolled algae blooms; rotten-egg,
fishy or ammonia smells; and silty bottoms-while decreasing their
water clarity, biological stability, fish habitat and production
of high quality sportfish.
Reduce phosphorus applications: Antonio Mallarino of ISU's Agronomy
department has found that soils frequently have more phosphorus
than plants need, so farmers and homeowners can save money and
the environment by avoiding over-applying phosphorus fertilizer.
As other research has shown, proper fertilization reduces phosphorus
runoff, which reduces eutrophication.
Make water walk, not run: Restoring and constructing wetlands
along key tributaries can slow water long enough for nutrients
to be absorbed. Any unneeded tile lines can be converted back
to slower streams and wetlands, which can slow water transport
and decrease watershed nutrient losses.
Reduce erosion: Planting permanent vegetation on the most erodible
parcels, maintaining drainage-ways and grass waterways, installing
buffer strips and protecting waterways from human and livestock
damage can all reduce erosion-and that reduces sediment. When
sediments are stopped, we also stop harmful nutrients.
Don't forget urban watersheds: Check and reroute storm drains,
septic systems and sewers. Keep streets clean and protect watersheds
from construction erosion.
Improve ecosystem balance: Carp in the Ventura Marsh, a protective
tributary of Clear Lake, became too abundant, stirring up sediments,
destroying wetland vegetation and allowing nutrients to get into
the lake. Within weeks of carp reduction, the wetland began to
hold much of the sediment and phosphorus it received, developing
a healthy wetland plant community and improving the lake water
quality.
In Clear Lake, the improvement in water quality from relatively
inexpensive watershed restoration projects will be substantial
and disproportionate to their cost. Thanks to hard work by dedicated
citizens, some improvements have already occurred-though more
remains to be done.
Toward
cleaner lakes
Cleaning up the lake itself makes sense only after watershed restoration
has been successful. Attempts to decrease the impact of accumulated
problems will not succeed until the problems cease to accumulate.
After the watershed has been restored, the lake manager's toolbox
offers many means of deepening, restoring and improving the function
of lake ecosystems.
Once Iowans make appropriate watershed corrections, we can expect
to see some improvement in water quality in three to five years-though
the full effect of restoration may not be seen for decades. Unfortunately,
it has taken us over a century of landscape change to bring our
lakes to their current quality and it may take us decades to get
back-but all the more reason to get started now!
As Thoreau looked into his Walden Pond and contemplated the depth
of his own nature, we can look to our lakes to gauge our own commitment
to water quality. Instead of being daunted by the average water
clarity of Iowa lakes (now only 2.6 feet), we can look to improved
watersheds that are reflected in the lakes they sustain.
Major
changes in the Iowa landscape
The black lines show how the landscape of Iowa has been altered
by human activities over the past 150 years-particularly by three
major transitions: 
1) conversion of
more than 90% of the land to farmland (1850-1930),
2) drainage and tiling of more than 90% of the wetlands (1900-1960),
and
3) four-fold intensification of agricultural yields through fertilization,
increased mechanization and pesticide use (1940 to present).
Increased soil erosion,
more volatile hydrology, and increased non-point pollution are
a legacy of these watershed changes.
The red line shows
the steady decline in the clarity of Clear Lake that has been
correlated with changes in the Iowa landscape. Clarity in the
late 1800s allowed aquatic plants to grow to depths of 18 feet.
Today, water clarity is 1-3 feet, depending on the weather and
season.
Back to article
Released
10/24/03
For more information,
e-mail Cathy Engstrom,
director of communications, or call (515) 288-1846.
© Copyright 2008 Iowa Natural Heritage Foundation
Comments? Suggestions? Email INHF Webmaster
|