Survey of Reservoir Greenhouse gas Emissions	file:///P:/PDF_Harvest/ScienceInventory/ScienceInventoiyHarvest/OOS...

Survey of Reservoir Greenhouse gas
Emissions

Lake Minatare Water Quality Survey

Jake Beaulieu
25 July, 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 Minatare can be found under
SITEJD NLA17_NE-10007.

Afield sensor is used to measure chlorophyll a, dissolved oxygen, pH, specific conductivity, and water
temperature 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 Minatare. These data will be included in a formal
peer-reviewed publication to be submitted for publication in 2024.

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Northern Appalachians
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Southern Appalachians
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Temperate Plains
Upper Midwest
Western Mountains

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UPR-EGP, arid the GIS User Community

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

2. Lake Minatare Survey Design

The Lake Minatare survey design included 15 sampling sites that were sampled on 2021-06-14. Water chemistry
samples were collected from a 13.8m deep site nearby the dam (Figure 2). Click on any of the sites to see the site
id, water temperature, pH, and dissolved oxygen at the water surface.

pie sites

sites

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UPR-EGP, arid the GIS User Community 		

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Survey of Reservoir Greenhouse gas Emissions

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

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, an indicator of algae abundance, in the water column. Chlorophyll a concentration
was 2 ug/L during the sampling, indicating the lake was oligotrophic.

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)), chlorophyll a, and dissolved
oxygen (do). All lake disturbance values are least disturbed.

Chemical Condition Indicators Measured at Water Chemistry Site

Threshold Values	Observed Values

parameter

units

least disturbed

moderately disturbed

most disturbed

concentration

status

do

mg/l

>5

>3

it <5

<3

8

least disturbed

tp

ug/l

<34

>34 i

CO
LO

V

>56

14

least disturbed

tn

ug/l

<657

>657

A
CO
CO
CD

>830

592

least disturbed

chlorophyll a

ug/l

<6.85

>6.85 t

A
CO
CO

>13.8

1.6

least disturbed

4. Within-lake Spatial Patterns

Afield sensor was used to measure water temperature, pH, and dissolved oxygen 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.

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Water temperature, dissolved oxygen, and pH showed very little spatial variation across the reservoir's surface
waters.

water

sitelD	temp

1	23.4

2	22.94

3	22.7

4	22.9

5	22.98

16	22.7

17	22

18	23.7

19	23.5

20	23.3

21	22.8

22	22.8

23	22.2

24	22.3

25	22

sitelD	pH

1	8.41

2	8.33

3	8.45

4	8.46

5	8.42

16	8.45

17	8.27

18	8.51

19	8.47

20	8.48

21	8.43

22	8.39

23	8.56

24	8.54

25	8.55

DO

sitelD (mg/L)

1	7.27

2	7.15

3	7.78

4	7.64

Water
Temp.

(°C)

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Getmapping, Aerogrid, IGN, IGP, UPR-EGP, and the GIS User Community	

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21	7.77

22	7.58

23	7.81

24	7.63

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 Minatare was 13.8 m deep. The top 5m of the water column was relatively
warm, but temperature dropped rapidly below 5m, indicating strong thermal stratification. Dissolved oxygen was
also lower below 5 m.

Lake Minatare Depth Profiles

Temperature (°C)

10	15	20	25	30

_4

Dissolved Oxygen (mg L )

1. Jake Beaulieu, United States Environmental Protection Agency, Office of Research and Development,

Beaulieu.Jake@epa.gov (mailto:Beaulieu.Jake@epa.gov)^

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