Possible effects on water quality

What is phosphorus and why is it a concern?

“Total phosphorus,” also referred to as “phosphorus,” is the measure of the phosphorus available for plant and algae growth. “Phosphate” is one form of phosphorus.

While phosphorus is a nutrient that is essential for life, too much phosphorus can result in excessive plant growth and algal blooms. Lakes with high levels of phosphorus are considered “eutrophic.”

Phosphorus is naturally occurring in soil, so erosion of shorelines contributes phosphorus to the lake. Since fertilizers and some herbicides contain phosphorus, phosphorus often enters lakes in run-off from lawns and farms. Leaking septic tanks also contribute phosphorus.

Lake Score Cards

Lake Bomoseen currently has good water quality, especially compared to many other lakes in Vermont. The DEC’s Vermont Lakes and Ponds Management and Protection Program (VLPP) publishes “Lake Score Cards” for 851 lakes and ponds in Vermont. Lake Bomoseen’s score card is shown below; the full version is available from the DEC here. To see the complete list of lakes and ponds with score cards, click here.

  • The Lake Score cards show the annual mean values for spring phosphorus, summer phosphorus, summer Secchi, and summer chlorophyll-a. Where there are enough sample points, a trendline is used to show the overall direction that the values have been trending over the years available.

  • The background color behind the points indicates the trophic state that the values correspond to—hypereutrophic, eutrophic, mesotrophic, or oligotropic.

  • According to the VLPP, “Total phosphorus (TP) concentrations at spring turnover represent the potential available phosphorus that will feed primary producers like aquatic plants and planktonic algae during the following summer.” These values have been collected by scientists in the VLPP’s Spring Phosphorus program.

    • Bomoseen’s values have been trending downward since 1980; the average value is 13.7 ug/L (micrograms per liter). This corresponds to the mesotrophic state.

    • For comparison, Lake St. Catherine’s average value is slightly higher at 14.6 ug/L (stable trend), and Lake Iroquois’s average value is 27.9 ug/L. Many of Lake Iroquois’s annual mean spring phosphorus values correspond to the eutrophic state.

  • Summer phosphorus (and Secchi disk and summer chlorophyll-a values) are recorded as part of the Vermont Lay Monitoring Program, in which volunteers take measurements throughout the summer.

    • The trend for summer phosphorus in Lake Bomoseen is in an upward direction, which warrants further investigation. It’s important to note that there are no values since 2019. What have the summer phosphorus levels been most recently?

    • Lake Bomoseen’s average summer phosphorus value is 13.3 ug/L, well below the eutrophic threshold of 30 ug/L.

    • For comparison, Lake St. Catherine’s average summer phosphorus value is 15.1 ug/L and Lake Iroquois’s is 24.8 ug/L.

  • A Secchi disk is an 8” metal disk with black and white quadrants. It is lowered into the water, and the depth at which it disappears from human sight is recorded. Secchi disk values are measures of water clarity or transparency. Values are affected by suspended solids in the water and the presence of planktonic algae. (The word “turbidity”—cloudiness caused by suspended solids—is often used in association with Secchi disk measurements.) In general, higher values, which indicate more transparency—are more desirable.

    • Lake Bomoseen’s Secchi disk values have been trending toward higher values (desirable) since 1990. The average summer Secchi disk reading is 7.4 m, which is well in the oligotrophic state.

    • For comparison, Lake St. Catherine’s Secchi disk readings have been decreasing over the years. Its average summer Secchi disk reading is 5 m, with most of its readings corresponding to the mesotrophic state. Lake Iroquois’s readings have been stable, but the average summer Secchi disk reading is only 3.9 m.

    • Note that the Lake Score Cards display the Secchi disk values with 0 at the the top of the plot, as if you were looking through the water column. The values for Lake Bomoseen are Highly Significantly Increasing, but the trendline points in a downward direction on the plot.

  • Chlorophyll-a is a photosynthetic pigment found in plants and phytoplankton (including cyanobacteria). The amount of chlorophyll-a in the water column serves as a good approximation of the amount of algae present. High values and increasing trends are cause for concern.

    • Lake Bomoseen’s average chlorophyll-a value is 2.0 ug/L, corresponding to the oligotrophic state, indicating that Lake Bomoseen does not have high levels of planktonic algae (including cyanobacteria). The trend has been stable.

    • For comparison, Lake St. Catherine’s average chlorophyll-a value is 4.2 ug/L (mesotrophic), and Lake Iroquois’s is 10.6 ug/L (eutrophic).

All of Lake Bomoseen’s recorded values fall into the mesotrophic or oligotrophic states. This suggests that Bomoseen is NOT a eutrophic lake, nor is it trending overall toward being a eutrophic lake.

We do not know what effect application of ProcellaCOR EC will have on these water quality parameters in Lake Bomoseen.

For more information on the VLPP’s scoring methodology, please read their document “The New Vermont Inland Score Card.”

The Lake Bomoseen score card shown above is a screenshot from the Vermont Department of Environmental Conservation’s Lake Score Card page. Accessed September 4, 2022.

Note 1: Above each of the graphs there is a p-value. A p-value is a measurement that is determined through statistics based on the data set. When the p-value is calculated to be 0.05 or more, the trend in the data is considered “stable.” When the p-value is calculated to be less than 0.05, the trend is “significantly increasing” or “significantly decreasing.” In this case, “significant” refers to the statistical meaning of the word.

Note 2: For phosphorus and chlorophyll-a, trends that are stable or decreasing are desirable for lake health. Too much phosphorus and chlorophyll-a can be problematic for the reasons explained above. For Secchi disk transparency, values refer to depth. Larger values mean that light can penetrate deeper due to less suspended solids. Larger values and increasing trends are thus more desirable for lake health.

Harmful Algal Blooms

One of the major water quality concerns is Harmful Algal Blooms (HABs). HABs are excessive growth of naturally-occurring cyanobacteria (blue green algae). The cyanobacteria can form surface scums or thick mats, which are unpleasant and can smell bad. Certain species of cyanobacteria produce cyanotoxins—natural poisons that can cause serious health problems in people or kill pets who play in or drink the water. HABs can deplete the oxygen in the surrounding water, causing fish kills, and can result in beach closures and water use and fishing restrictions. The Vermont Department of Health and the DEC monitor cyanobacteria levels and maintain a Cyanobacteria Tracker, which shows areas of the state with current HABs.

As shown in the lake score card, Lake Bomoseen has low levels of chlorophyll-a, suggesting low levels of planktonic algae and cyanobacteria. Lake Bomoseen does not currently have a HAB, nor does it have a history of problems with HABs.

At the time of writing (early September 2022), Lake St. Catherine was experiencing a Low Alert HAB. Lake Morey was experiencing two Low Alert and two High Alert HABs.

Does herbicide use contribute to HABs? While it’s hard to prove cause-effect, a lot of research has been done which shows that disrupting the ecosystem and the water chemistry can lead to major changes in a lake, including an increase in HABs. We do not know the effect that ProcellaCOR EC will have on chlorophyll-a levels and HAB occurrences.

Alternative stable states

Alternative Stable States is an ecological theory from the 1960s that predicts that ecosystems can exist with several stable states. An ecosystem will stay in a particular state until perturbations are large enough to push the ecosystem into another stable state. The shift to another state can result in catastrophic changes to the ecosystem. Ecologists apply this concept to lakes.

The Chautauqua Lake Association in western New York contracted Racine-Johnson Aquatic Ecologists to survey, analyze, and report on the health of Chautauqua Lake. In their report “2019 Status of Chautauqua Lake’s Aquatic Macrophyte Community Determined by a Late Summer/Early Fall Survey and Estimates of the Associated Invertebrate Community,” the ecologists explain this alternative stable states concept succinctly (page 8):

“The accepted scientific theory of alternative stable states predicts that shallow lakes with high nutrient concentrations can likely switch from a clear state where rooted aquatic plants dominate to a turbid state controlled by phytoplankton, often today concentrated with HABs.

The ecologists state that “The lake [Chautauqua] is eutrophic (very nutrient rich) and shallow eutrophic lakes generally fall into a macrophyte (clear state) or algae dominated (turbid state) waterbody. Today, an algae dominated lake would likely have higher populations of harmful algae or cyanobacteria. The lake requires a macrophyte dominated littoral zone that competes against an overabundance of cyanobacteria (HABs) to remain a healthy ecosystem with good water clarity, an excellent warm water fishery and provide a multiuse ecosystem for the stakeholders.”

Lake Bomoseen is NOT currently a eutrophic lake, however, the alternative stable state concept may still apply. (Researchers have found that the alternative stable state concept applies across a range of nutrient levels.) Lake Bomoseen is currently macrophyte (large aquatic plant) dominated and has minimal cyanobacteria. What will happen if a significant number of macrophytes are killed off with ProcellaCOR EC? Will this trigger a shift to an algae-dominated lake? We have no way of knowing.

Regardless of the trophic state of a lake, macrophytes and planktonic algae (including cyanobacteria) compete with each other for nutrients and light. There is no evidence to suggest that allowing Eurasian watermilfoil to continue growing will lead to growth of cyanobacteria or other planktonic algae.

Milfoil and algae

In addition to competing with planktonic algae for light and nutrients, Eurasian watermilfoil has been found to secrete anti-algal compounds.

  • In the late 1990s, researchers in Japan found that Myriophyllum spicatum (Eurasian watermilfoil) secretes anti-algal compounds that inhibit the cyanobacteria Microcystis aeruginosa. Abstract available here (1996) and here (1999).

  • In 1996, researchers in Germany found that extracts of Myriophyllum spicatum “exhibit a strong inhibitory action against various coccoid and filamentous cyanobacteria.” Full text available here.

We don’t know the extent to which the milfoil in Lake Bomoseen may be inhibiting cyanobacteria. Killing large amounts of milfoil could have an unwanted effect on cyanobacteria populations.

Milfoil and phosphorus

Milfoil takes up phosphorous as it grows. In previous years, milfoil has been removed from Lake Bomoseen through harvesting. According to the LBA, 1,400 cubic yards of milfoil were removed in 2021 through harvesting. Additional milfoil was removed through DASH.

What will happen to the phosphorus levels in Lake Bomoseen if large swaths of milfoil are killed (and left to breakdown or decompose in the lake) rather than being removed through harvesting?