2007
Norway
Lakes Water
Quality Report
The Lakes
Association of Norway, with support from the Town of
Norway ,
continued to monitor the health of the four
Norway
Lakes in
2007. Water quality monitoring was a combined effort of volunteers and
lake professionals. Monitoring of the lakes takes place from early May
through September, during the time of year when lakes and ponds are the
most biologically productive, and water quality problems are most likely
to occur. In addition to monitoring lake water quality, LAON also
conducted a screening survey for invasive aquatic plants on the four
lakes.
The weather that occurs during and preceding lake
monitoring can have a strong influence on indicators of lake water
quality, and is likely responsible for some of the variability that is
measured within individual seasons and from one year to the next. The
2007 monitoring season was characterized by heavy rain and stormwater
runoff in the spring and early summer, followed by moderating conditions
from July through September.
Pennesseewassee
Lake:
2007 was
an average year for
Pennesseewassee
Lake , when
compared to historical conditions. Water clarity averaged 5.7 meters
(about 18.5 feet) over the five month monitoring period, compared to
above average conditions in 2006 (6.56 meters), 5.9 meters in 2005, and
the historical average for the lake of 5.8 meters. While 2007 was one of
the clearest years on record for the lake (extending back to 1976) the
conditions in 2007 were about average for the thirty year water quality
data history for the lake.
The concentration of phosphorus
(the nutrient that is responsible for the growth of algae in lakes)
averaged 9 parts per billion (ppb) in 2007, compared to 7 ppb in 2006, 8
ppb in 2005, and the historical average of 9 ppb. It is likely that
heavy precipitation and runoff from the watershed resulted in higher
phosphorus levels and lower water clarity in 2007.
Chlorophyll-a (CHL) is a
pigment that is measured to determine the concentration of algae in lake
water. The 2006 average concentration measured 4.3 ppb, compared to 4.4
ppb in 2006, and the 2005 average of 4.1 ppb The 2007 average was very
slightly lower than the historical average of 4.4 ppb.
The three primary indicators of lake health were
consistently about average for Pennesseewassee in 2007.
Late
August and September dissolved oxygen levels were very low in the
deepest region of the lake, as has been the case for a number of years.
In August, the deepest six meters of water, measured at the deepest
point in the lake, were completely devoid of dissolved oxygen. By
September, conditions had improved somewhat, but oxygen levels remained
at, or near zero near the bottom of the lake. Low concentrations of late
summer dissolved oxygen serve as a warning that the lake is sensitive
and vulnerable to a decline in water quality, regardless of conditions
near the surface, where wind and wave action keep oxygen levels high
throughout the summer.
Natural water color levels were average in 2007, as
were pH and total alkalinity. All were within the normal range of values
for the lake.
No invasive aquatic plants were found in the
screening survey of Pennesseewassee
Lake .
A native species of Milfoil is known to occur in this lake. However,
this plant is
not invasive.
A species of non-native,
invasive snail, referred to as the “Chinese Mystery Snail” has been
documented in the lake. This snail has now been observed in all four of
the Norway
lakes, as well as in a number of area waterbodies, including Thompson,
the Range Ponds, and others. The ecological significance of this invader
has not been determined. However, from a nuisance perspective, the
large, dark green snails are offensive to the nose when they wash up on
the shoreline, and there has been at least one report of oxygen
depletion in a pond when a large number of the snails died over a short
period of time.
Gleotrichia is a colonial
blue-green algae that occurs naturally in many
Maine
lakes. Looking down into the water, “Gleo” has the appearance of tiny
off-white dots, often likened to tapioca. In recent years, this algae
has become problematic on some
Maine
lakes and ponds, and it may be on the increase throughout
Maine .
We will continue to carefully monitor the concentration of this algae in
Pennesseewassee.
Hobbs
Pond (Little Penn):
Hobbs Pond (Little Penn) was
very clear again in 2007, averaging 6.1 meters, which was also the 2006
average (nearly 20 feet). The historical water clarity average for Hobbs
Pond is 5.2 meters. In 2005, the average was 5.6 meters, and 5.9 meters
in 2004. On average, Hobbs
was nearly 3 feet clearer in 2007 than it has been historically!
Hobbs
drains directly into Pennesseewassee.
Phosphorus levels were very low in 2007, averaging 8 ppb for the five
month period. This was substantially lower than the historical average
of 11 ppb, and the 2006 average of 10 ppb!
In
addition, the average concentration of chlorophyll-a (algal
concentration in the pond) was even lower in 2007 (4.3 ppb) than the
relatively low average in 2006 (4.5 ppb) and notably lower than the
historical average of 4.9 ppb, and the 2005 average of 5.1 ppb.
During the past decade, the water quality of Hobbs
Pond has improved quite notably. Back in the late 1970’s and early 80’s,
the annual water clarity was nearly always in the mid 4 meter range
(about 15 feet). At times, individual water clarity readings were as low
as 2.0 meters (about 6 feet). LAON took the initiative to work with
landowners in the watershed to implement conservation practices, which
resulted in a nearly immediate turnaround in water quality.
However, the same words of
caution apply with Hobbs
as with Penn and Sand: Late summer oxygen levels near the bottom of the
pond were very low, and phosphorus samples taken near the bottom of the
lake were moderately high (19 ppb) compared to surface concentrations.
This means that, despite the fact that things look good near the
surface, this pond is sensitive and vulnerable, and water quality could
easily decline if continued efforts are not taken to protect the very
good water quality that has been documented in recent years.
Other water quality indicators
that are measured to help support the primary data (color, pH, and total
alkalinity) were within the normal range of readings for
Hobbs
in 2007.
No invasive aquatic plants were detected in Hobbs
Pond in the 200 screening survey, however, as indicated above, the
Chinese Mystery Snail was documented in the pond.
Sand
Pond:
Sand Pond
experienced a slightly below average year, especially when compared to
2006 and the spectacular conditions in 2005. Water clarity averaged 7.0
meters (~23 feet), compared to 7.7 meters in 2006, 8.5 meters in 2005,
and the historical average of 7.4 meters. Sand Pond is the clearest of
the four Norway
Lakes , and in general, the
water quality of this small pond is above average, compared to other
Maine lakes.
The average total phosphorus concentration in Sand
Pond last summer was 6 ppb, compared to 6 ppb in both 2006 and 2005, and
the historical average of 7 ppb. Chlorophyll-a averaged 3.0 ppb,
compared to 2.7 ppb in 2006, 2.5 ppb in 2005 and the historical average
of 2.6 ppb. It is interesting that while water clarity was lower in 2007
(but still very good, compared to many area lakes), the phosphorus level
has been relatively steady for three years running.
Late summer dissolved oxygen
levels were actually improved in 2007, at least compared to conditions
in late August, 2006. However, by September 21, there was virtually no
oxygen in the water below 10 meters depth. The maximum depth of Sand
Pond is approximately 17 meters (56 feet). Phosphorus samples taken near
the bottom of the deepest area of the pond in late summer were four
times as high as samples from the surface. This suggests that the pond
is in a very sensitive state, and that water quality could change if
conservation measures are not employed for both existing and new
development in the watershed.
All additional support indicators of water quality
were within normal ranges in Sand Pond during the 2006 monitoring
season.
No invasive aquatic plants were detected in the 2006
screening survey of Sand Pond. However, the Chinese Mystery Snail was
documented for the first time in this pond, and Gleotrichia (discussed
above) was observed in the water in September. We will continue to
closely monitor the pond for the presence of these two potentially
troublesome species.
North
Pond:
North Pond is relatively shallow, having a maximum
depth of less than 15 feet. The shallow depth can limit the value of
water clarity readings that are taken with a Secchi disk, because often
the disk reaches the bottom of the pond before it disappears from view.
In the 1970’s and 1980’s, the Seechi disk was nearly always visible on
the bottom of North Pond. However, when the pond started to experience
algal blooms, the situation changed. Often the disk would disappear in
the algae-laden water before it reached the bottom at only 12-13 feet.
In 2007,
the Secchi disk was visible on the bottom of North Pond in May, June,
July and September, but not in August. In 2006, the disk was visible on
the bottom throughout the five month monitoring period. The average
phosphorus concentration for the year was 15 ppb, compared to the low
average of 13 ppb in 2006 and16 ppb in 2005. The historical average for
North Pond is 18 ppb, so 2007 levels were definitely lower (better) than
average. The concentration of algae in the water, as indicated by
chlorophyll-a levels, was higher than it has been for the past two
years, averaging 5.2 ppb, compared to 3.8 ppb in 2006, and
4.1
ppb in 2005. However, it was still lower (better) than the historical
average of 6.6 ppb.
North
Pond experienced a mixed year in 2007, but overall good, especially when
compared to the historical average for the pond. But it was not as good
as in 2006, which was the best in more than two decades for the pond.
This may have been, in part,
the
result of nearly constant flushing of the pond from heavy rains
throughout the summer. The weather can certainly have a very strong
influence on variations in lake and pond water quality from one year to
the next. But the improvement
in
North Pond in recent years may also be attributed in part to
conservation practices that have been implemented in the watershed
through the efforts of LAON. North Pond drains into
Pennesseewassee
Lake .
No invasive aquatic plants were detected in the 2006
screening survey of North Pond, which included the extensive attached
wetland areas that drain to Pennesseewassee. The Chinese Mystery Snail
has existed in North Pond for more than a decade. The snail popula
Summary:
2007 was
an average year for the
Norway
Lakes , except
for Hobbs Pond (Little Penn), which was very clear. Weather conditions
during the early summer were similar to those in 2006, but lake systems
are complex, and it is possible that the declines observed in 2007 were
the result of cumulative conditions from two wet summers.
Each lake and pond responds in a unique way to the
influences of weather, changes in land use in the watershed, and other
forces upon the ecosystem. This is because of the wide range of
physical, chemical and biological characteristics of each lake basin and
its watershed.
The
following is a summary of findings for Pennesseewassee
Lake , and
Hobbs
(Little Penn), Sand and North Ponds.
|
LAKE
|
Water Clarity in Meters
|
Core Total Phosphorus (ppb)
|
Core Chlorophyll-a (ppb)
|
Color (SPU)
|
pH
|
Total Alkalinity
|
|
Pennesseewassee
|
5.7
|
9
|
4.3
|
12
|
6.8
|
14
|
|
Hobbs
(Little Penn)
|
6.1
|
8
|
4.3
|
12
|
6.8
|
10.7
|
|
Sand
|
7.0
|
6
|
3.0
|
6
|
6.6
|
6.3
|
|
North
|
3.1 (Bottom)
|
15
|
5.2
|
15
|
6.8
|
9.0
|
Special thanks are due to certified volunteer lake
monitors Patti Ann Douglas on Sand Pond, and Warren Bryant on
Pennesseewassee, who contributed additional Secchi disk transparency
(water clarity) data in 2007. Their efforts substantially improve our
confidence in the monitoring results on the two bodies of water last
summer.
TO BE ADDED: Statewide
perspective on Maine
lakes in 2007.
Prepared
by Scott Williams, Aquatic Biologist
|