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Does Flow Rate Affect Water Quality Parameters?
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Researched by Breeana S.
2000-01 |
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PURPOSE
The purpose of this experiment was to determine if different flow rates
affect the dissolved oxygen, pH, turbidity, and temperature in a stream.
I became interested in this idea while looking through a book about
water quality and seeing all of the things that affect the quality of water
on a daily basis.
The information gained from this experiment will determine what speed
of flow rate affects dissolved oxygen, pH, turbidity, and temperature the
most.
HYPOTHESIS
My hypothesis was that at a flow rate of 5cfs the dissolved oxygen level,
pH level, turbidity, and temperature would be different than a flow rate
of 4cfs.
I base my hypothesis on a pamphlet called, Naturemapping for Fish and
Streams and a biologist, Julie Larson, who said that low flow rates can
cause fatally high water temperatures which affects the level of dissolved
oxygen, turbidity, and pH levels.
EXPERIMENT DESIGN
The constants in this study were:
Same area for testing
Same amount of water tested
Same method of measuring
Same width from shoreline
Same equipment used
The manipulated variable was the speed of the water.
The responding variable was the level of dissolved oxygen, pH level,
temperature, and turbidity.
To measure the responding variable I used a dissolved oxygen probe,
pH strip, thermometer, and a turbidity meter.
MATERIALS
QUANTITY |
ITEM DESCRIPTION |
| 1 |
turbidity meter |
| 1 |
dissolved oxygen probe |
| 1 |
pH strip |
| 2 |
glass vials |
| 1 |
liter DI water |
| 3 |
plastic vials |
| 1 |
thermometer |
PROCEDURES
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Go to sample site #1 upstream of Wenas Creek on Longmire and Fink
Rd.
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Rinse equipment with water from sample site.
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Put the sample collection bottle and slowly descend bottle into stream
current and lift it back up at the same rate of motion filling the bottle
to 15% of its capacity.
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Repeat this step going across the width of the stream until the bottle
is filled 90 %.
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Release bottle from sample equipment and close it with a lid.
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Repeat steps 1-5 2 more times.
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Take glass vile and rinse with DI water or pure water.
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Wipe surface of the vile with clothe to prevent smudges.
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Put three drops of Oil glass on the vile and wipe with cloth.
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Hold lid of vile and shake it 4 times as to prevent air bubbles,
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Place vile in turbidity meter and wait for reading.
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Take 5 readings and average them and take their deviant.
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Take Multi Parameter Meter and test for dissolved Oxygen and saturation
level of stream.
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Read temperature of stream by using Multi Parameter Meter thermometer.
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Take a pH strip and dip in one of the sample bottles.
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Leave pH strip out for 5 minutes and then compare to the shade guide.
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Measure flow of stream in cubic feet per second.
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Take the width multiplied by the velocity.
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Measure width of stream and measure velocity by setting up a rope
from a specific point to another. (Should be ten feet long.)
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Drop an orange at starting point and time it till it reaches the end point.
Record data and comment on weather and habitat or area.
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Go to Urban site at Adobe way road and North Wenas.
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Repeat steps 1-21.
RESULTS
The original purpose of this experiment was to determine if different
flow rates would affect the dissolved oxygen level, pH, turbidity, and
temperature.
The results of the experiment were that at a flow rate of 5 cfs the
dissolved oxygen, pH, temperature, and turbidity were different than at
a flow rate of 4 cfs. The average turbidity was 3.09 NTU at 5 cfs and was
2.11NTU at 4 cfs. The temperature was 3.2° C. at 5 cfs and was 1.3°
C. at 4 cfs. At 5 cfs the dissolved oxygen level was 12.2, but 13.5
at 4 cfs. The pH level at 5 cfs was 8, but 7 at 4 cfs.
See the table and graph
CONCLUSION
My hypothesis was that at a flow rate of 5cfs the pH level, dissolved
oxygen level, turbidity, and temperature level would be different than
at a flow rate of 4cfs.
The results indicate that this hypothesis should be accepted because
at a flow rate of 5cfs the pH level, dissolved oxygen level, turbidity,
and temperature level was different than at a flow rate of 4cfs.
Because of the results of this experiment, I wonder if the weather or
season would affect my results. I also wonder if the surrounding land use
would effect my results.
If I were to conduct this project again I would test in a variety of
places, I would do more than one trial for each variable, and I would also
test for a wider range of flow rates and more of them.
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RESEARCH REPORT
Introduction
Water Quality is very important to aquatic life. There are so many things
that affect aquatic life. For example, dissolved oxygen allows fish to
breath and temperature affects the level of dissolved oxygen because the
warmer the water the less oxygen can stay dissolved in it. There are also
nutrients and turbidity that can affect fish and other aquatic life.
Dissolved Oxygen
Dissolved oxygen analysis measures the amount of gaseous oxygen dissolved
in an aqueous solution. Oxygen gets into water by diffusion from the surrounding
air, by rapid movement in the water, and as a waste product of photosynthesis.
Things can reduce dissolved oxygen levels like water temperatures, water
flow, and organic waste.
Dissolved oxygen depends on rainfall, saltiness, amount of decomposition,
amount of plant life, types of rocks in the riverbed, water temperature,
time of day, and water velocity.
Dissolved oxygen in water should not exceed 110 percent of the concentration
of oxygen in the air. If it does it could be harmful to aquatic life. The
lower the concentration, the greater the stress for aquatic life.
pH
pH is a measure of the acidic or basic nature of a solution. The concentration
of hydrogen ion activity in a solution determines the pH. It is worked
out mathematically: pH = -log [H+].
pH stands for potential hydrogen. The levels of pH are formed into
groups. These groups are Acidic, basic, and neutral. Acidic is from a range
of 1-7, basic is from a range of 7-14, and neutral is equal to 7.
A pH range of 6.0 to 9.0 appears to provide protection for the life
of freshwater fish and bottom dwelling invertebrates. Runoff from agricultural,
domestic, and industrial areas may contain iron, aluminum, ammonia, mercury
or other elements. The pH of the water will determine the toxic effects,
if any, of these substances.
Turbidity
Turbidity is a measure of how clear water is. The lower the turbidity,
the clearer the water is. The higher the turbidity, the cloudier the water
is. Turbidity is caused by the amount of suspended solids: clay, silt,
and algae. High turbidity indicates that enough suspended matter exists
to block sunlight from reaching the bottom of the water. High turbidity
may result from soil erosion, waste discharge, urban runoff, frequent disturbance
of sediment, excess nutrients resulting in algal blooms. It
may also color the water.
Temperature
Temperature determines the conditions in which living matter can exist.
Small temperature changes in the water can drive fish away from that area
and bring in other living things in their place. Temperature changes can
come from trees that are removed which then give the stream more sun. Factories
and power plants take water in to use as a coolant and then discharge it
back into the stream but warmer that it came in. Temperature affects other
things like dissolved oxygen, and pH levels.
Summary
Aquatic life has many elements that have to be at a certain level for aquatic
life to have a healthy life. Dissolved Oxygen allows aquatic life to breathe.
Turbidity is the measure of how clear water is. The pH level affects aquatic
life. Temperature affects dissolved oxygen, pH, turbidity, and determines
whether a living creature can exist. |
BIBLIOGRAPHY
Andrews, Frank C. "Oxygen," The World Book Encyclopedia. 1999. Vol.
14. Pp. 889-890
Asimov, Isaac. "Oxygen", New Age Encyclopedia.1995.vol.13.pp.533-534
Greenfield, David W. "Salmon", World Book Encyclopedia. 1998. Vol.17.
Pp. 69-71
Kentucky Water Watch, "Dissolved Oxygen." [Online] Available http://www.state.ky.us/nrepc/water/wcpdo.htm
Kentucky Water Watch, "pH." [Online] Available http://www/state.ky.us/nrepc/water/wcpph.htm
Laitinen, Herbert A. "pH", New Age Encyclopedia. 1995.vol.14.pp.333
"pH", World book Encyclopedia. 1999.vol.15.99.15
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ACKNOWLEDGEMENTS
I would like to thank the following people for there
help in making my science project posible and successful.
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I would like to thank Janey Peterson for the rides to
and from my test sites and to and from the rides to interviews.
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I would like to thank Bill Rice for getting all the equipment
that made my project possible and I would also like to thank him for coming
out to the field with me and showing me how all the equipment works.
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I would like to thank Ryan Anderson for coming out into
the field with me and for contacting Bill Rice to get all the equipment
I needed.
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I would like to thank Julie Larson for getting me started
with my project and giving me some names that I could use to get further
information.
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I would like to thank John Easterbrook for getting me
data that showed me what the numbers would be like and what I would be
doing.
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I would like to thank my advanced science teacher, Mr.
Newkirk for helping me find an interest that I would be interested in and
for correcting my project journal.
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I would like to thank Mrs. Pasckvale for helping me choose
my colors for my board and for helping me but my board together.
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