Parameter Trend Analysis

Dissolved Oxygen (DO)
Fecal Bacteria
Water Clarity
Chlorophyll a / Nutrients
Submerged Aquatic Vegetation
Stormwater Runoff Volume
River Section Map

Dissolved Oxygen

Click on charts for full size

The amount of dissolved oxygen (DO) has been steadily improving in all three sections of the river except in very recent years. The sharp drop in 2013 seems to be because of weather patterns (See Precipitation Pattern for more information) that was not favorable to DO. The weather pattern in 2014 was even worse but the %Score bounced back a little. There were many intense rainfall events that regularly caused Combined Sewer Overflow events in downstream DC in both 2013 and 2014. The CSO events dump raw sewage mixed with rainwater into the river when it rains heavily. The discharge includes organic matter which will later be decomposed by bacteria. The decomposition consumes oxygen in the water. See the example graph below that shows how DO changes in an intense rainfall.

Because the CSO discharge is churned up, the discharge itself has high DO values. As the time passes by, decomposition will proceed and it consumes oxygen in the water resulting in prolonged low DO values.

Because the MD Anacostia (Section 1) receives oxygen-rich water from two large tributaries -- the Northwest and the Northeast Branches -- DO tends to be higher than in the DC portion (Section 2&3).

DC Water (formerly DC WASA) broke ground in October 2011 on the $2.6 billion Clean Rivers Project (CSO Long Term Control Plan) to control sewer overflows. The Anacostia River will see benefits from the project starting in 2018. The project will reduce combined sewer overflows by 98 percent at completion in 2022. Both DC sections will then see significant improvement in DO levels. However, by improving existing infrastructure and maintaining it better, DC Water already reduced 40% of CSO by 2009 and 60% of it by 2011.

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Fecal Bacteria

Many Anacostia watershed residents know of the Combined Sewer Overflow problems in DC. The sewer system in DC is designed to overflow into the river when a rain event exceeds approximately a half inch. However, contrary to public perception, downstream DC water is cleaner than the upstream MD water in the Anacostia in terms of fecal bacteria. There are two possible reasons that might account for this: (1) the tidal action washes the mouth of the Anacostia with much cleaner Potomac River water twice a day, and (2) there is large amount of fecal matter input from Maryland. Washington Suburban Sanitary Commission (WSSC) in Maryland and DC Water are working to repair sewer leaks and implement remediation projects to reduce sewer overflows. However, there is quite a large uncontrolled portion of fecal matter from wildlife.

According to a study conducted by AWS and Charles Hagedorn of Virginia Tech University, funded in part by Chesapeake Bay Trust (CBT), approximately 70 percent of fecal bacteria from Maryland is attributed to wildlife. Approximately 7-8 % of fecal bacteria is from canine. Feces excreted on impervious surfaces by birds, squirrels, raccoons, deer, mice, rats, etc. is washed away by rainfall and is carried into streams. Though the largest source of fecal bacteria may be wildlife, its transport to the river is caused by the impervious surfaces we have created. In natural settings, wildlife feces tend to decompose on site and most rainwater infiltrates into the ground and will not cause fecal bacteria pollution in streams.

All river sections show steady improvement over the years with the District portions improving faster. Even though there were many intense rainfall events in 2014, the %Score for Fecal Bacteria is on track for improvement. However, the Maryland portion of the river (Section 1) seems to be leveling out or even declining in recent years. We need to see if Section 1 is really improving or not. This is especially important because we see a similar trend in Chlorophyll a ­ leveled out or declining in recent years in Section 1.

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Water Clarity (Secchi Disk Depth)

Water clarity indicators (Secchi Disk Depth tests) have been low for all sections in all years for which data is available. In almost all cases, the score was below 50 percent. In the graph above, the trend line (not the scatter plots) is the average value of scores for the past five years. This method clearly illustrates the trend.

From 2001 until 2009 water clarity in Maryland and Upper DC (Sections 1 and 2) had been declining. The best average score for these sections was in 2001. Since then, the average has been declining until recently. In the Lower DC Anacostia (Section 3) the best average score was in 1995. Since then the average was declining until about 2006. However, there seems to be improvement in the past several years in all sections. Responding to the recent water clarity improvement, submerged aquatic vegetation (SAV) re­appeared in 2013 after being absent from the Anacostia River for ten years. (See the trend analysis for SAV below for details.)

In order to accelerate resolving this grave issue, stringent regulations on stormwater runoff should be implemented because the increased peak stream flows resulting from flashy stormwater runoff from increased impervious surfaces have been eroding the streambanks and scouring streambeds, making the water cloudy. According to a study conducted for the Total Maximum Daily Loads (TMDL) for sediment, about 73% of sediment is coming from streambank erosion. The study was conducted for suspended sediment particles in the water. When heavier particles of sediment are taken into consideration, it is safe to say that more than 73% of sediment is coming from streambank erosion.

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%Scores for Chlorophyll a are improving. However, the overall better score in Maryland (Section 1) does not mean that there are no excessive nutrients coming from Maryland. Because Chlorophyll a is a green pigment in plants, algae, and cyanobacteria, it does not accurately reflect the nutrient amounts in water. There is a lag time between discharge of nutrients and their uptake by plants, etc.

In the free-flowing tributaries of the Anacostia, discharged nutrients travel to the tidal Anacostia. Because the tidal river moves slowly, there is plenty of time for microalgae to take up nutrients. Thanks also to the ample sunlight for photosynthesis in the tidal Anacostia, the DC portions of the river (Section 2 and Section 3) tend to have higher Chlorophyll a values, resulting in lower scores. Both upstream and downstream communities need to stop nutrients from entering runoff (fertilizer, for example) from properties.

It is very interesting to see the DC sections (Sections 2 and 3) have been better than the MD section (Section 1) in the past 2 years. DC Anacostia is improving faster than MD Anacostia with the MD section potentially becoming static or even declining in recent years. Chlorophyll is the green pigments of plants that converts sunlight into organic compounds.

Chlorophyll is the green pigment of plants that converts sunlight into organic compounds during photosynthesis. There are seven known types of chlorophyll; Chlorophyll a and Chlorophyll b are the two most common forms. Chlorophyll a is used as a measure of microalgae biomass, which is controlled by factors such as water temperature, light, and nutrient availability. Too much algae leads to large algal blooms that can reduce water clarity. Also, once an algae bloom dies, it depletes water of oxygen when it is decomposed.

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Submerged Aquatic Vegetation

SAV data source:

Submerged Aquatic Vegetation (SAV) are plants that cannot withstand excessive drying and therefore live with their leaves at or below the water surface. Such vegetation constitutes an important habitat for young fish and other aquatic organisms.

AWS's goal for restoring SAV in the Anacostia is 20 acres, a goal identified in the Anacostia Watershed Restoration Indicators and Targets for Period 2001-­2010 by scientists at Metropolitan Washington Council of Governments (COG).

In the graph as soon as the degradation of water clarity in the Lower DC Anacostia (Section 3) was observed in 1995, the acreage of SAV started to decline. No SAV had been observed in the Anacostia since 2003 until 2012, the score for the time duration had been zero (0) for over a decade. While there was no SAV in the tidal Anacostia, it is known that there is SAV in non­tidal tributaries to the Anacostia River.

However, in 2013, 0.9 acres of SAV (thus, the %Score is approximately 5% ­­ 0.9/20x100) was identified in Washington Channel and we learned that SAV is coming back to the Anacostia River!

AWS is not certain why SAV was present in the past --particularly in the 1980s and 1990s when the water clarity seemed worse than or equal to the current clarity. However, we have several hypotheses:

·   The nature of the cloudiness of the water was different. There are many factors that make the water cloudy. Recent cloudiness may be complex combination of sediment particles due to erosion, decaying organic matter from sewage, algae bloom, etc. while past cloudiness may have mainly come from sediment particles.

·   The river was monitored less often in the 1980s and 1990s. The water quality data may then be less reliable during the time period.

·   The SAV may have suffered in the 1980s and 1990s, but may still have been reducing pollution.

·   The overall nature of pollution may have changed. In more recent years, numerous types of pollutants including chemicals such as pharmaceuticals, pesticides, herbicides, and heavy metals on top of water cloudiness may have helped eliminate the plants.

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Stormwater Runoff Volume

Northwest Branch

Northeast Branch

%Scores for Stormwater runoff have been steadily decreasing as long as stream discharge (flow) data is available. AWS is expecting that this trend will change and start to show improvement, though it will take time due to the vast areas of impervious surfaces that must be retrofitted with water-infiltrating green infrastructure to measurably reduce runoff.

It will be instructive to monitor differences in rates of runoff reductions in the Anacostia’s Northeast and Northwest Branches where different standards and practices exist. The Northeast Branch is mainly in Prince George's County while the Northwest Branch flows largely through Montgomery County.

While new development throughout Maryland is required to treat runoff from a 1-year/24-hour storm (approx. 2.7 inches), the key to reduce stormwater runoff and restore the Anacostia is to treat runoff reduction for existing development. Montgomery County regulations now require that redevelopment projects treat 2.6" of rain. However, Prince George's County only requires treating 0.5 inches until 2016 and just 0.75 inches beyond that. Because of the difference in regulation over redevelopment, it is expected that the Northwest Branch will have better reduction about peak stream discharges.

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Anacostia River Section Map

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