This document summarizes water quality monitoring results from stations along the Severn River from May to June 2012. Oxygen levels decreased with depth at all stations, showing hypoxic conditions near the bottom. The deepest stations experienced bottom anoxia by early July. Salinity was highest near the surface and decreased with depth. Oxygen levels below 1 mg/L stressed bottom-dwelling organisms.
Results of weekly water quality monitoring in Maryland's Severn River in the summer of 2013. Dissolved oxygen depth profiles are shown for 13 stations, with accompanying pycnocline intensity changes and results of hydrogen sulfide measurements. Our data show that two anoxic "dead zones" form at the bottom of the tidal Severn River during the summer, independent of the well known seasonal Chesapeake dead zone.
Results of the Severn Riverkeeper Water Quality Monitoring Program, showing oxygen depth profiles from 7 stations in Severn creeks and at the edge of Round Bay.
Most dissolved substances found in water are measured in parts per million (ppm) or even smaller amounts. This means that for every one million parts (units) of water there is a certain number of parts of the substance.
Results of weekly water quality monitoring in Maryland's Severn River in the summer of 2013. Dissolved oxygen depth profiles are shown for 13 stations, with accompanying pycnocline intensity changes and results of hydrogen sulfide measurements. Our data show that two anoxic "dead zones" form at the bottom of the tidal Severn River during the summer, independent of the well known seasonal Chesapeake dead zone.
Results of the Severn Riverkeeper Water Quality Monitoring Program, showing oxygen depth profiles from 7 stations in Severn creeks and at the edge of Round Bay.
Most dissolved substances found in water are measured in parts per million (ppm) or even smaller amounts. This means that for every one million parts (units) of water there is a certain number of parts of the substance.
A lacustrine environment is a type of aquatic environment that is characterized by a large body of standing water, such as a lake. Lacustrine environments are typically low-energy environments, meaning that the water is relatively calm and there is little wave action. This allows for the deposition of fine-grained sediments, such as silt and clay.
Lacustrine environments are home to a variety of plants and animals, including algae, fish, and amphibians. The types of plants and animals that live in a lacustrine environment will vary depending on the climate, the depth of the water, and the nutrient content of the water.
Lacustrine environments are important for a number of reasons. They provide a habitat for a variety of plants and animals. They also help to regulate the water cycle and to prevent flooding. Lacustrine environments can also be used for recreation, such as swimming, fishing, and boating.
Here are some of the characteristics of lacustrine environments:
Low-energy: Lacustrine environments are typically low-energy environments, meaning that the water is relatively calm and there is little wave action. This allows for the deposition of fine-grained sediments, such as silt and clay.
Variety of plants and animals: Lacustrine environments are home to a variety of plants and animals, including algae, fish, and amphibians. The types of plants and animals that live in a lacustrine environment will vary depending on the climate, the depth of the water, and the nutrient content of the water.
Important for water regulation: Lacustrine environments are important for a number of reasons. They provide a habitat for a variety of plants and animals. They also help to regulate the water cycle and to prevent flooding.
Used for recreation: Lacustrine environments can also be used for recreation, such as swimming, fishing, and boating.
Here are some examples of lacustrine environments:
Lakes: Lakes are the most common type of lacustrine environment. They are typically formed by glacial activity, volcanic activity, or tectonic activity.
Oxbow lakes: Oxbow lakes are formed when a river bends and then cuts off, leaving a crescent-shaped lake behind.
Crater lakes: Crater lakes are formed when a volcano erupts and collapses, leaving a depression that fills with water.
Lakes can be formed in a variety of ways, but the most common are:
Glacial activity: Glaciers are large masses of ice that slowly move across the land, carving out depressions as they go. When a glacier melts, the depression is filled with water, forming a lake.
Glacial activity lake formationOpens in a new window
www.pmfias.com
Glacial activity lake formation
Volcanic activity: When a volcano erupts, it can leave behind a crater that fills with water, forming a lake.
Volcanic activity lake formationOpens in a new window
www.nps.gov
Volcanic activity lake formation
Tectonic activity: Tectonic activity is the movement of the Earth's plates. When tectonic plates move, they can create cracks
Chemical Oceanography is fundamentally interdisciplinary. The chemistry of the ocean is closely tied to ocean circulation, climate, the plants and animals that live in the ocean, and the exchange of material with the atmosphere, cryosphere, continents, and mantle
Practice Problems -Due next class period Fully describe how nitrogen .pdftrishacolsyn25353
Practice Problems -Due next class period Fully describe how nitrogen (ammonia an dissolved
oxygen problems in surface waters? Describe the processes of lake stratifica diagram or drawing
that you have generated yourself. Identify a Nitrogen, Phosphorus, or Nutrient impaired water
using the EPATMDL database and discuss the following items d nitrate) and phosphorus
pollutants lead to tion and turnover in your own words, using at least 1 Provide a map of the
watershed or find a photo specific to the watershed that shows o eutrophication. o What specific
pollutant(s) drive eutrophication within the watershed? what point source and non-point source
polluters contribute to the problem? o How much Nitrogen and/or Phosphorus is allowed on a
water shed basis for the point source and non-point source polluters? As an avid outdoorsperson,
explain whether you would swim or fish in this water? o Environmental Engineering Class 14
Limnology
Solution
Answer 1: Poor water quality in lakes can have many unpleasant consequences. Rough fish –
such as carp and bullhead – populations increase at the expense of game fish populations. Severe
nuisance algal blooms yield unpleasant odor and appearance that reduce the aesthetic appeal of
lakes. This may result in declines in fishing and swimming and hurt tourism. As algae die and
decompose, the process consumes oxygen. Submerged plants without sunlight die, decompose
and consume more oxygen. Without enough dissolved oxygen in the water, fish and other
organisms suffer and die because they can\'t “breathe.” This can occur locally or much farther
downstream leading to degraded estuaries, lakes and reservoirs
Answer 2: Lake is stratified on the basis of temperature difference along the lake depth. Also
called as lake thermal stratification. Cold water is denser than warm water and the epilimnion
generally consists of water that is not as dense as the water in the hypolimnion.
There are 3 layers
Lake turnover is the process of a lake\'s water turning over from top (epilimnion) to bottom
(hypolimnion). During the summer, the epilimnion, or surface layer, is the warmest..
A lacustrine environment is a type of aquatic environment that is characterized by a large body of standing water, such as a lake. Lacustrine environments are typically low-energy environments, meaning that the water is relatively calm and there is little wave action. This allows for the deposition of fine-grained sediments, such as silt and clay.
Lacustrine environments are home to a variety of plants and animals, including algae, fish, and amphibians. The types of plants and animals that live in a lacustrine environment will vary depending on the climate, the depth of the water, and the nutrient content of the water.
Lacustrine environments are important for a number of reasons. They provide a habitat for a variety of plants and animals. They also help to regulate the water cycle and to prevent flooding. Lacustrine environments can also be used for recreation, such as swimming, fishing, and boating.
Here are some of the characteristics of lacustrine environments:
Low-energy: Lacustrine environments are typically low-energy environments, meaning that the water is relatively calm and there is little wave action. This allows for the deposition of fine-grained sediments, such as silt and clay.
Variety of plants and animals: Lacustrine environments are home to a variety of plants and animals, including algae, fish, and amphibians. The types of plants and animals that live in a lacustrine environment will vary depending on the climate, the depth of the water, and the nutrient content of the water.
Important for water regulation: Lacustrine environments are important for a number of reasons. They provide a habitat for a variety of plants and animals. They also help to regulate the water cycle and to prevent flooding.
Used for recreation: Lacustrine environments can also be used for recreation, such as swimming, fishing, and boating.
Here are some examples of lacustrine environments:
Lakes: Lakes are the most common type of lacustrine environment. They are typically formed by glacial activity, volcanic activity, or tectonic activity.
Oxbow lakes: Oxbow lakes are formed when a river bends and then cuts off, leaving a crescent-shaped lake behind.
Crater lakes: Crater lakes are formed when a volcano erupts and collapses, leaving a depression that fills with water.
Lakes can be formed in a variety of ways, but the most common are:
Glacial activity: Glaciers are large masses of ice that slowly move across the land, carving out depressions as they go. When a glacier melts, the depression is filled with water, forming a lake.
Glacial activity lake formationOpens in a new window
www.pmfias.com
Glacial activity lake formation
Volcanic activity: When a volcano erupts, it can leave behind a crater that fills with water, forming a lake.
Volcanic activity lake formationOpens in a new window
www.nps.gov
Volcanic activity lake formation
Tectonic activity: Tectonic activity is the movement of the Earth's plates. When tectonic plates move, they can create cracks
Chemical Oceanography is fundamentally interdisciplinary. The chemistry of the ocean is closely tied to ocean circulation, climate, the plants and animals that live in the ocean, and the exchange of material with the atmosphere, cryosphere, continents, and mantle
Practice Problems -Due next class period Fully describe how nitrogen .pdftrishacolsyn25353
Practice Problems -Due next class period Fully describe how nitrogen (ammonia an dissolved
oxygen problems in surface waters? Describe the processes of lake stratifica diagram or drawing
that you have generated yourself. Identify a Nitrogen, Phosphorus, or Nutrient impaired water
using the EPATMDL database and discuss the following items d nitrate) and phosphorus
pollutants lead to tion and turnover in your own words, using at least 1 Provide a map of the
watershed or find a photo specific to the watershed that shows o eutrophication. o What specific
pollutant(s) drive eutrophication within the watershed? what point source and non-point source
polluters contribute to the problem? o How much Nitrogen and/or Phosphorus is allowed on a
water shed basis for the point source and non-point source polluters? As an avid outdoorsperson,
explain whether you would swim or fish in this water? o Environmental Engineering Class 14
Limnology
Solution
Answer 1: Poor water quality in lakes can have many unpleasant consequences. Rough fish –
such as carp and bullhead – populations increase at the expense of game fish populations. Severe
nuisance algal blooms yield unpleasant odor and appearance that reduce the aesthetic appeal of
lakes. This may result in declines in fishing and swimming and hurt tourism. As algae die and
decompose, the process consumes oxygen. Submerged plants without sunlight die, decompose
and consume more oxygen. Without enough dissolved oxygen in the water, fish and other
organisms suffer and die because they can\'t “breathe.” This can occur locally or much farther
downstream leading to degraded estuaries, lakes and reservoirs
Answer 2: Lake is stratified on the basis of temperature difference along the lake depth. Also
called as lake thermal stratification. Cold water is denser than warm water and the epilimnion
generally consists of water that is not as dense as the water in the hypolimnion.
There are 3 layers
Lake turnover is the process of a lake\'s water turning over from top (epilimnion) to bottom
(hypolimnion). During the summer, the epilimnion, or surface layer, is the warmest..
1. Severn Riverkeeper Summer Water Quality Monitoring Program
2012 Weekly Dissolved Oxygen Results—Mainstem Stations
Pierre Henkart, PhD
2. Severn mainstem monitoring stations
SR7 – Our shallow
N SR6 – Our Severn Narrows station with a depth of 5 meters. We
generally notice fresher water near the surface, the influence of the
(~1.5m) upper
fresh Severn Run entering to the northeast. Summer bottom anoxia
station with
is pronounced here.
fresher water from
nearby Severn
Run, especially SR5 – Our mid Round Bay station with a depth of 7
after rains. meters. Bottom anoxia usually sets in by early July, and
Turbidity is high. in the absence of storms, persists until September.
RBN – Our “Round Bay North” SR3 – Our “Joyce” station in a deep hole
station, with a typical Severn depth south of Joyce Point, at a depth of 12-13
of ~ 7 meters. This is the heart of meters (~40 feet). There are a few other
the Severn summer dead zone. deep spots like this in the Severn.
RBS – Our “Round Bay South” SR1 – Our “USNA” station in
station, which is interesting because the mid-channel opposite College
bottom sometimes gets anoxic in the Creek, with a depth of 7 meters
summer. It has a typical Severn depth of ~
7 meters.
SR2 – Our “Rte 50 bridge” station with a depth of 7
meters. We get to watch the peregrine falcons that nest
on the bridge. We also get to compare our data with the The distance
monthly MD DNR monitoring data (their station WT7.1) Annapolis from SR0 to SR7:
on the “Eyes on the Bay” website.
18 km = 11 miles
SR0 – Our “near Chesapeake” station south of Greenbury
Point, in the channel, with a depth of 6 meters (a bit less than
20 ft). SR0 is near the NOAA “Annapolis” buoy providing
great continuous on-line water quality data at 1 meter depth.
3. Oxygen depth profiles show habitat stress and “hypoxic squeeze”
We show our water quality data as depth profile bar graphs. You can
think of yourself as a scuba diver entering the water from our monitoring
Dissolved boat and then heading straight for the bottom. As you go down oxygen
oxygen, levels will change. We’ve plotted the depth in a downward direction, so
0 mg/liter the longer the bar, the deeper the water. The oxygen levels are color
coded according to the oxygen concentrations needed by different
>5 marine organisms. The Severn’s large active fish need at least 5 mg/liter
1 oxygen, and levels greater than that are colored green. Since most
oxygen in the water comes from the air, the top of the water column has
3-5 higher oxygen. In most cases, water near the surface has more than 5
2
Depth, meters
mg/liter, so the tops of most bars are green. Smaller fish like white perch
are adapted to live with lower oxygen levels, but will avoid water with
3 less than three mg/liter dissolved oxygen. They will utilize both the
1-3 green and yellow portions of the water column. Benthic organisms that
live in or on the bottom (oysters, worms, etc) are adapted to yet lower
4 oxygen levels down to 1 mg/liter, and they will tolerate bottom water in
the orange 1-3 mg/liter oxygen range. Oxygen levels below 1 mg/liter
.2-1 (red) are stressful to tough benthic organisms, even for short durations.
5 Truly anoxic conditions exist below 0.2 mg/liter oxygen, where only
anaerobic bacteria can live. This anoxic water will suffocate even the
<.2 toughest multicellular organisms quickly.
6
The lower oxygen levels in deeper water will “squeeze” fish habitat
toward the surface. The extent of squeeze will depend on the oxygen
preference of the fish involved, but few fish will be found in waters with
less than 1 mg/liter dissolved oxygen.