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White Paper on Oxygen
The Lake Merritt Institute
November, 2003
Background
In May of 1999 the US Environmental Protection Agency placed Lake Merritt on
the 303d
list, which means it is a body of water whose beneficial uses are impaired.
Lake Merritt
was listed due to high levels of trash, and low levels of dissolved oxygen.
In most cases,
placement of this list results in the establishment of Total Maximum Daily Loads
(TMDL's) which are regulatory limits on the causes of listing. However
in the case of Lake
Merritt, the Regional Water Quality Control Board chose to allow Oakland to
develop and
implement plans to solve the problem without establishment of a TMDL.
Scope of this Paper
This white paper provides information on:
- Sources of oxygen, how it is depleted and why it is important
- Oxygen levels in the Lake
- Known and suspected causes of low oxygen levels in the Lake
- What can be done to improve the situation.
General Information on Oxygen
Sources of Oxygen in the Lake: Oxygen is transferred to water
from the air and by
photosynthetic activity of plants during daylight. In Lake Merritt, it comes
from the vast
populations of plant life (plankton, algae and widgeon grass) and from contact
with the
air. At night, or in places where there is no light, photosynthesis does not
occur, and
oxygen is not produced. During darkness and especially when they are decomposing,
plants use up oxygen.
Variation: Oxygen levels in the Lake are continually changing
in response to daily and
seasonal cycles. Peak levels typically occur during mid day when photosynthetic
activity
is maximum. Minimum levels typically occur just before dawn. The amount of oxygen
in
the water is also influenced by seasonal factors such as rainfall, runoff, tidal
flows, day
length, light intensity and the amount of plant life. If water is stratified
into separate
layers (e.g. top and bottom) oxygen levels can be quite different in these layers.
What Causes Low Oxygen? Oxygen is used up by respiration (breathing)
and by chemical
reactions. In Lake Merritt oxygen is used up by the respiration of plants and
animals, and
especially by biological and chemical reactions in the mud at the bottom where
leaves and
other organic matter are decomposing. Because of this, and because light does
not always
reach the bottom, oxygen levels at the bottom of the lake are lower than at
the surface.
Why is Oxygen Important? Oxygen is necessary for almost all
forms of animal life. If
deprived of it for even short periods of time, animals will die. The presence
of oxygen also
means that decomposition will not create odors such as hydrogen sulfide.
How Much is Necessary? Because of its low solubility, oxygen
in occurs in water at only a
tiny fraction of the amount in air. Air is 20% oxygen, but when oxygen is dissolved
in
water, it typically exists at levels from 1 (extremely low) to 20 (very high)
milligrams per
liter, which is equal to 1 or 20 parts per million (ppm). Various forms of life
can endure
various levels of oxygen: Some, such as active fish need 5 ppm or more, while
others such
as clams and mussels can survive at 3 ppm. State water quality standards recommend
that
oxygen be at least 5 ppm in natural water bodies. But levels below 3 ppm create
stress on
the aquatic environment and at one to zero, odorous conditions can develop.
Oxygen Levels in the Lake
Most of Lake Merritt is not impaired by low oxygen during most of the time because
levels
are typically above 5 ppm. However, under certain conditions, some areas of
the Lake
become impaired.
Alameda County Annual Reports: From 1990 – 1995 the Alameda
County Flood Control
District published annual reports on water quality in Lake Merritt. Included
were the
results of weekly or monthly oxygen testing of surface and bottom waters. Briefly
summarized, these reports verified that:
- Surface waters contain medium to high
levels of oxygen. Typical readings at the
Lake center are between 7 and 13 ppm. At the ends of Lake arms, surface levels
are
typically above 5 ppm. Higher levels are sometimes recorded during plankton
blooms. Oxygen levels at the petro-barriers (the black and yellow floating
barriers)
occasionally drop below 4 ppm.
- Bottom waters are what have caused Lake
Merritt to be listed as impaired by EPA.
Typical readings at the Lake center are from 5 to 10 ppm (but fell below 3
ppm four
times in 1991, and once in 1992). At the ends of Lake arms, bottom levels
have typically
been below 5 ppm and fell below 3 ppm 14 times in 1991, 9 times in 1992 and
7 times in
1993. Seven incidents in a year may not seem like much, unless you are trying
to
survive during that incident.
- Plant life can create high levels of
oxygen in Lake Merritt during the day, but at
night, their respiration can significantly reduce oxygen levels. Also, when
plants
die off, oxygen is used up by decomposition, and very low levels can occur.
In
general, excess amounts of seaweed (which dominates in the spring and summer)
or plankton (which dominates in the rainy season) can create both high and
low oxygen levels.
- Conditions near major storm drain outfalls
(outfalls #6, 7, 8, 27, 51, 54, 56 and 60)
are the worst of any areas tested in the Lake. These outfalls bring in leaves
and
other organic materials which use up oxygen in the water as they decompose.
The
aeration fountains are located in these areas to transfer oxygen from the
air to the water.
Continuous Monitoring Probe Data – Lake Center: From
June of 2002 until July of 2003, probes measuring temperature, salinity and
oxygen were installed by the City of Oakland near the Lake center. They were
located about one foot from the surface and one foot from the bottom, and recorded
data every 15 minutes. Although this data has not been thoroughly analyzed,
the data do reveal that on a weekly basis between June, 2002 and May 2003:
- Mean oxygen levels at the surface were
typically above 5, but did drop below 5
four times.
- Mean oxygen levels at the bottom were
typically above 5 but did drop below 5
eleven times.
These mean values indicate that most of the time oxygen levels are satisfactory
but that
there are periods when they become too low. They do not however, represent the
stress
on animals that occurs when oxygen reaches minimum levels. Looking at weekly
minimum data, we find that:
- Oxygen levels at the surface dropped
below 3 at least twice
- Oxygen levels at the bottom dropped
below 3 at least 15 times
- Oxygen levels at the bottom dropped
below 2 at least 6 times
- Oxygen levels at the bottom dropped
below 1 at least twice.
Oakland High School Data: Since 1996, students from the Oakland
High Environmental Academy have been taking weekly oxygen samples during the
school year. There data is particularly valuable because they measure at four
stations, not just the Lake Center. In general, water quality in the arms of
the Lake is not as good as the Lake center because tidal circulation is not
as strong in the upper arms.
Although these data represent grab samples rather than continuous monitoring,
they do confirm that, on occasion, very low oxygen levels do occur in the Lake.
For example:
- On November 12, 2002, oxygen levels
at all four stations were between 1.5 and 3.5.
- On December 10th, 2002, oxygen at the
Estuary channel (near the inlet/outlet) and at
the Glen Echo station (near the creek inlet) were both measured at 2 at the
bottom.
- On December 17th, 2002 oxygen levels
at the bottom by the Estuary Channel were
2.5 and 1.5 near the bird islands.
Lighthouse Charter School Data: From June through early December of
2002, the Lighthouse Charter school measured oxygen levels at the surface of
the Lake. While most readings were above 5, they were consistently below 5 from
September 4th to through October 24th.
Known Causes of Low Oxygen in the Lake
Although more study of the data will provide details, it is known that three
factors contribute to low oxygen levels at the bottom of the Lake. These are
stratification, decomposition of plant material and restriction of tidal circulation.
Stratification: During and after rainfall, runoff from the
4.650 acre watershed brings fresh water to the Lake. Being less dense, this
surface water floats above a layer of tidal salt water at the bottom. When this
occurs, especially when the tide gates are closed during high tide for flood
control, the bottom layer becomes trapped and loses oxygen due to the decomposition
of organic matter carried in with the rain. Such conditions have been documented
in the Institute’s March, 2003 “Tidings” newsletter.
Plant Decomposition: Although algae growth in the Lake occurs
mainly in the spring, summer and early fall, widgeon grass growth follows a
cycle of growth in May and June, followed by die off and decomposition in August
and September. As the enormous volume of plant material decomposes, it uses
up oxygen. Some of the lowest levels of oxygen have been measured during this
period when the widgeon grass is rotting. Large blooms of plankton and algae
can also depress oxygen levels when they die off.
Restriction of Tidal Circulation: When the weather forecast
includes a 50% or more chance of rain, County personnel prevent high tides from
entering the Lake to restrict potential flooding. Surface water drains out during
low tides, but since the Lake bottom is 3 – 4 feet
below the outfall, the bottom layer of water does not drain well. Deprived of
mixing with estuary water during high tides, it becomes lower in oxygen. Such
conditions have been documented by the Oakland High Environmental Academy based
on 1998 – 1999 data
copy available upon request).
What Can Be Done to Improve the Situation?
An earlier report by the Water Quality Task Force listed several important actions
which can improve oxygen levels at Lake Merritt. These include:
- Further planning to eliminate sanitary
sewer overflows
- A review of the discharges from animal
stables at Children’s Fairyland and the police stables
- Modification of tide gate operations
(while maintaining flood control)
- Reduction of sediment transported to
creeks
- Construction of wetland habitats
- A reduction of leaf / organic matter
inflow
- Regular harvesting of widgeon grass
and algae
- Minimize pesticide and especially fertilizer
input into the Lake
- Reduce the level of bird waste around
the Lake and
- Conduct regular water quality testing.
Many of these suggestions cannot be funded by measure DD, which is limited to
capital improvements. Following are additional details on those concepts that
might be funded by DD:
Aeration Fountains: Currently, three aeration style fountains
are installed in Lake Merritt, and a fourth is scheduled to be added in November,
2003. They provide both oxygen and aesthetic benefits, but the increase in oxygen
is limited to the local area around the fountain. For example, oxygen levels
measured at bottom waters near the bandstand fountain contained above 4 ppm
oxygen at a time when levels 20 – 60 or more feet away
were at 2 ppm or less. They can provide islands of higher oxygen water when
conditions throughout the Lake are poor, and (except for the shallow water intake
unit) help to break up stratification of the top and bottom layers.
Aeration Bubblers: These devices have not yet been tried at
Lake Merritt. Operating on 110 volts (the fountains use 220) they provide a
more economical (but less aesthetic) means of adding oxygen directly to the
water. They are commonly used at residential lagoons and in Lakes to provide
oxygen and reduce stratification. Small compressors are installed in boxes along
the shoreline, and feed air to underwater dispersion devices near the bottom.
Capital costs are about half that of fountains and there are no intake screens
to clog, but the diffusers may be prone to encrustation by barnacles, mussels,
tube worms et cetera. Also, they are least effective in shallow waters. The
Institute is currently planning a test bubbler system in conjunction with the
fountain to be installed at 18th Street.
Minimize Tide Gate Closure: DD
funding of a new flood control station would allow incorporation of state of
the art tide gauges and computer modeling to minimize restriction of high tides
while maintaining flood control. If decisions on gate closure were made on a
12 hour basis, the gates could be kept open at each tidal cycle unless closure
was required for flood control. For more details on tidal flow restriction,
refer to the “White Paper on Water Level Control and Tidal Flows”
at the Institute website.
Install Bottom Outlet Drains: Currently,
water drains from Lake Merritt into tunnels that
are 3-4 feet higher than the Lake bottom. This restricts drainage of the lower
quality
bottom water. Installation of bottom drains as part of the 12th Street re-building
under DD
would allow removal of this water, which is sometimes very low in oxygen. These
drains
would empty into the channel on outgoing tides.
Install Storm Drain Filters: By removing organic matter from
urban runoff before it
reaches the Lake, storm drain filters can reduce the amount of materials that
use up
oxygen. Leaves, fecal material, paper et cetera are trapped in the filter, removed
during
maintenance and taken to the landfill.
As part of the Water Quality Task Force work, a demonstration storm drain filter
(screen) was installed at Lake Merritt 5 about two years ago. An informational
brochure describing it is available upon request. The unit has no moving parts,
works continuously, does not become clogged, and can be cleaned in about 25
– 30 minutes. Cleaning is required about 4 – 5 times per year and
the unit is designed prevent flooding. Oakland’s filter uses a continuous
deflection separation (cds) technology and the filter at outfall # 5 prevents
items smaller than about 1 x 9 mm. from escaping. It is installed on a drain
that is 18 inches in diameter and drains an area of 12 acres. It has worked
well since installation (an inspection can be arranged). This type of unit was
chosen by the Water Quality Task Force after a study of the various types of
stormwater treatment.
Current Plans: Planning is underway for three additional cds type filters;
at outfalls, 2, 4 and 45. These filters will be on drains of 24, 24 and 33 inches
in diameter and can probably be installed on city land within Lakeside Park.
Remaining Outfalls: With four filters installed, 56 will remain unfiltered,
including 7 that are more than 54 inches in diameter or greater. These large
storm drains carry more flow, and consequently more oxygen consuming organic
matter and trash. However, on these largest filters, tidal flows extend considerably
upstream and filters cannot be installed within the tidal zone. The Institute
has suggested upstream locations for about eight filters on these larger drains
(see memo of August 15, 2003).
Size Limits on Storm Drain Treatment Devices: With the exception of
cds type devices and
constructed wetlands, storm drain treatment technologies are limited in the
size of
watershed that they can treat. Subsurface vaults, oil/water separators, media
filters, drain
inlet devices, vegetated swales and infiltration systems are designed for areas
such as
shopping centers, parking lots and components of small subdivisions. Devices
with such
limited capacity are unable to handle the flows to Lake Merritt’s largest
storm drains.
Because large volumes of water can pass through the cds screen, it is likely
that these units
can be installed along branches of creeks that feed into our large storm drains.
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