Survey of Reservoir Greenhouse gas Emissions

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Survey of Reservoir Greenhouse gas Emissions

Lake Moritclair Water Quality Survey

Jake Beaulieu1
02 June, 2022

1. Background

Between 2020 and 2023 the US Environmental Protection Agency (USEPA) will survey water quality and greenhouse gas (GHG) emissions from
108 reservoirs distributed across the United States (Figure 1). The objective of the research is to estimate the magnitude of GHG emissions from
US reservoirs.

All reservoirs included in this study were previously sampled by the USEPA during the 2017 National Lakes Assessment (2017 NLA). Data from
the 2017 NLA can be found at the EPA website (https://www.epa.gov/national-aquatic-resource-surveys/data-national-aquatic-resource-surveys).
Data for Lake Montclair can be found under SITEJD NLA17_VA-10010.

A field sensor is used to measure chlorophyll a, dissolved oxygen, pH, specific conductivity water temperature, and turbidity near the water surface
at a minimum of 15 locations within each reservoir. Water samples are collected from the deepest site for analysis of nutrients and chlorophyll a.

This preliminary report presents water quality results for Lake Montclair. These data will be included in a formal peer-reviewed publication to be
submitted for publication in 2024.



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Figure 1. Location of the 108 Reservoirs Included in Study.

2. Lake Montclair Survey Design

The Lake Montclair survey design included 15 sampling sites. Water chemistry samples were collected from a 14.5, 4.7m deep site nearby the
dam (Figure 2). Click on any of the sites to see the site id, water temperature, pH, turbidity, and dissolved oxygen at the water surface.

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Figure 2. Location of the 15 sampling sites in Lake Montciair.

3. Lake Disturbance and Trophic Status

Lakes are often classified according to their trophic state. There are four trophic state categories that reflect nutrient availability and plant growth
within a lake. A eutrophic lake has high nutrients and high algal and/or macrophyte plant growth. An oligotrophic lake has low nutrient
concentrations and low plant growth. Mesotrophic lakes fall somewhere in between eutrophic and oligotrophic lakes and hypereutrophic lakes have
very high nutrients and plant growth. Lake trophic state is typically determined by a wide variety of natural factors that control nutrient supply
climate, and basin morphometry. A metric commonly used for defining trophic state is the concentration of chlorophyll a (chla), an indicator of algae
abundance, in the water column. Chlorophyll a concentration was 36 ug/L during the sampling, indicating the lake was hypereutrophic.

Trophic State Classification

Analyte

Oligotrophic

Mesotrophic

Eutrophic

Hypereutrophic

chlorophyll a (ug/L)

<=2

>2 and <=7

>7 and <=30

>30

In addition to classifying lakes by trophic status, lakes can be classified by degree of disturbance relative to undisturbed lakes (i.e. reference lakes)
within the ecoregion. Degree of disturbance can be based on a wide variety of metrics, but here we use nutrients (total phosphorus (tp), total
nitrogen (tn)), suspended sediment (turbidity), chlorophyll a, and dissolved oxygen (do). Lake disturbance values range from least to most
disturbed.

Chemical Condition Indicators

Threshold Values	Observed Values

parameter	units	least disturbed	moderately disturbed	most disturbed	concentration	status

do	mg/l	>5	>3 & <5	<3	9	least disturbed

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Threshold Values

Observed Values

parameter

units

least disturbed

moderately disturbed

most disturbed

concentration

status

turbidity

NTU

<3.32

>3.32 I

x <4.67

>4.67

6.87

most disturbed

tp

ug/l

<34

>34 (

CD
LO

V

>56

24

least disturbed

tn

ug/l

<657

>657 f

X"

A
OO
CO
O

>830

670

moderately disturbed

chlorophyll a

ug/l

<6.85

>6.85 (

xw
A
CO
oo

>13.8

36.1

most disturbed

4. Within-lake Spatial Patterns

A field sensor was used to measure water temperature, pH, dissolved oxygen, and turbidity near the water surface at all sampling sites. Data are
reported in figures and tables below. Hover the curser over any point in the figures to reveal the sitelD corresponding to the adjacent data table.
Alternatively, click on any row in the data table to reveal the location of the sampling site on the map.

Turbidity was highest at the northwest end of the lake and decreased toward the dam, likely reflecting a pattern of suspended sediment dropping
out of the water column as water velocity decreased. The spatial pattern of water temperature reflects the time of sampling, with cooler
temperatures reflective of samples collected in the morning and warmer temperatures reflective of afternoon sampling. Dissolved oxygen and pH
tended to be highest toward the dam, likely reflecting high rates of algal metabolism in the relatively warm and clear water on that end of the lake

sitelD

water
temp

¦ ¦ ¦ ,
\ '

xti* mp.

1

28.5

2

29.2

3

28.6

4

29.8

5

28.5

6

28.9

7

28.6

8

29.9

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300 m
1000 ft



water

sitelD

temp

9

28.7

10

29.2

11

29.6

12

30.4

13

28.9

14

28.7

sitelD

pH (J

1

8.7

2

8.9

3

7.4

4

9.1

5

8.7

6

8.7

7

7.7

8

9.3

9

8.6

10

9

11

9.3

12

9.1

13

8.7

14

8.4

15

8.9

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sitelD

Turbidity
(NTU)

1

2

3

4

5

6

7

8

9

10

11

12

13

14

15

9.5
9

12.9
9.3
9.9
9.8
11.9

9.3
9.7

8.4

8.6
8.6
10

12.4

8.5

sitelD

DO
(mg/L)

1

7.9

2

12.7

3

10.4

4

12.9

5

8.4

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Survey of Reservoir Greenhouse gas Emissions

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10	12

11	13.1

12	12.3

13	12.6

14	11.2

15	12.6

5. Depth Profiles

Dissolved oxygen is one of the most important environmental factors affecting aquatic life. The biological demand for oxygen is often greatest near
the sediment where the decomposition of organic matter consumes oxygen through aerobic respiration. Near the surface of lakes, photosynthesis
by phytoplankton produces oxygen, often leading to a general pattern of decreasing oxygen availability with increasing depth. This pattern can be
exacerbated by thermal stratification. Thermal stratification occurs when lake surface waters are warmed by the sun, causing the water to become
less dense and float on top of the deeper, cooler lake water. Since the deeper layer of water cannot exchange gases with the atmosphere, the
dissolved oxygen content of the deep water cannot be replenished from the atmosphere. As a result, the deep water can become progressively
depleted of oxygen as it is consumed by biological activity, sometimes causing dissolved oxygen to become sufficiently scarce to stress oxygen
sensitive organisms including some fish and insects.

The deepest sampling location in Lake Montclair was 14.5, 4.7 m deep. In shallow lakes, wind induced mixing of the water column is often
sufficient to prevent thermal stratification. Lake Montclair was highly thermally stratified, with much colder water in the bottom half of the column.
Dissolved oxygen was nearly depleted near the lake bottom, indicating strong biological oxygen demand in lake sediment.

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Lake Montclair Depth Profiles

Temperature (°C)

10	15	20	25	30

Dissolved Oxygen (mg L 1)

1. Jake Beaulieu, United States Environmental Protection Agency, Office of Research and Development, Beaulieu.Jake@epa.gov
(mailto:Beaulieu.Jake@epa.gov)«J

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