How Does Water Speed Affect Turbidity in a River
Picture of the student researcher
Researched by Aaron R.
2001-02





PURPOSE

The purpose of this experiment was to determine river speed, to how much turbidity is collected in the water

I became interested in this idea when I herd that every year California grew smaller and smaller by the erosion of the Pacific Ocean. 

The information gained from this experiment will help wild life biologists and scientists in the field of water quality. 




HYPOTHESIS

My hypothesis is the faster the river the more turbidity there will be in the water. 

I base my hypothesis on the World Book Encyclopedia, that states the faster the river the more turbidity in the water. 

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EXPERIMENT DESIGN

The constants in this study were: 

  • The dept that the water samples were taken
  • How far out in the river they were taken.
  • The same units of measurements.
  • The river the samples are taken from. 
  • The time of year. 
The manipulated variable is the speed of the river. 

The responding variable was the amount of Turbidity collected in the water. 

To measure the responding variable I measured the flow with a flow meter and the amount of turbidity in the water with a turbidity meter.

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MATERIALS
 
QUANTITY  ITEM DESCRIPTION
One  Dell Latitude lap top computer for recording the data immediately after taking the samples. 
One  Vernier Lab Pro to hook the turbidity sensor and flow rate Sensor to thecomputer. 
Two  Meter stick to measure dept and distance the samples are taken
Three One hundered ml. viles.
One  Flow rate sensor, measure the speed of water.
One  Turbidity sensor to measure the amount of turbidity collected in the river. 

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PROCEDURES

1. Rinse equipment in the water the samples are taken from. 
2. Measure speed of water with flow meter. 
3. Measure depth of water.
4. Measure how far out in the river the samples are taken. 
5. Slowly emerge sample vials in current a meter from bank, and thirty
centimeters in depth. 
6. Then lift vial out of water at the same speed. 
7. Repeat steps 1-6 six more times, in three more locations taking two 
samples at each test site.  Each site on the river needs to be different speeds. 
8. Label test vials. 
9. Test samples with turbidity meter.
10. Graph results. 
11. Repeat steps 8-9 six more times.

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RESULTS

The original purpose of this experiment was to determine river speed, to how much turbidity is collected in the water

The results of the experiment were the faster the flow the more turbidity in the water 

See data and graph.



CONCLUSION

My hypothesis was  the faster the river the more turbidity collected in the water.

The results indicate that this hypothesis should be accepted. 

Because of the results of this experiment, I wonder if I had taken more trials the results would differ? 

If I were to conduct this project again I would take more samples.  I also would organize my experimental design better.  If I could I would redo the whole thing over from top to bottom.

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RESEARCH REPORT

INTRODUCTION

Water is requirement for life, and critical for the survival of all plants and animals on the earth.  Water gives life to every living thing. It also gives us recreation, and transportation possibilities.
Erosion, the wearing away of soil and rock, also affects us.  It changes the shape of the earth, which can change our way of life.

WATER

Water molecules are made up of two hydrogen atoms, and one oxygen atom.  Water is the only substance on earth that at normal temperature can take three forms; liquid, solid (ice and snow), or gas (water vapor).  Water is the most common substance on earth, which covers about 70% of the earth’s surface. There are about 326 million square miles of water on the earth’s surface.  For every square mile of the 326 million, there are over a billion gallons of water. 
Only 3% of earth’s water is fresh water, more than 2% is trapped in polar-icecaps, and 1% is below the earth’s surface.  Lakes and rivers hold only 1/15 of the earth’s surface water. The atmosphere holds .001 of the earth’s water. Water has the largest heat capacity, of any other substance besides ammonia, and can dissolve almost anything.  The ocean is too salty for drinking, agriculture, and industry. The single largest use of water is industry.   For example it takes about eighty gallons of water to make the Sunday newspaper.  For every pound of steel produced, it takes twenty gallons of water. 
One birch tree gives off seventy gallons of water vapor a day. An acre of corn gives off 4,000 gallons of water vapor per day. 

WATER CYCLE

The water cycle plays a huge part in our lives.  The heat from the sun causes evaporation, the vapor cools, forms clouds, rains and the cycle starts all over again.  About 75% of all precipitation lands back in the ocean.  Some evaporates again immediately. In the process of evaporation, the salt in the ocean is left behind.

WEATHER

Weather plays big part in erosion.  The wind picks up sediment and moves it from one place to another.  Rain and snow also cause erosion.  Earth is not the only planet in the solar system that has weather.  Mercury and possibly Pluto are the only planets that don’t have weather.  Weather takes place in the troposphere, which is the closest layer of atmosphere to earth.  Some tools that meteorologists use to predict weather are weather balloons, airplanes, ships, and satellites.  They also use Doppler radars to predict weather.  It uses color codes to indicate the speed and direction of storm clouds.  They provide warning for severe storms such as hurricanes.

EROSION

Erosion is the wearing away and removal of soil and rock on the surface of the earth.  Streams and rivers are the main component to erosion, so are wind, weather, and glacial movement.  Vegetation slows down the process of erosion.  Ice is the main cause of rock erosion.  When water gets in a crack of a rock, freezes, expanses, and breaks the rock apart, and then is carried to the ocean by streams, or the weather.

GLACIERS

Glaciers are a huge mass of ice that forms in areas with cold weather, a wet climate, and where snow from winter doesn’t melt in the summer.  The bottom layer turns to ice.  It also forms where there is shelter from the wind and the sun, manly in gullies and valleys.  There are two types of glaciers, a cold glacier and a warm glacier.  Cold glaciers require a temperature of ? 40°C.  Warm glaciers move faster down hills.  Glaciers have four zones. The sub-glacial zone is the bottom, the englacial zone is the ice.  Superglacial is on the surface, and extraglacial is at the edge.  When the glacier is large enough, gravity pulls it down hill.  As the ice mass slides down hill it picks up rocks.   Then the rocks act as blades, which push more rock.  High altitude regions are called "Accumulation zones."  Areas that loose ice during the summer months are called "Abulationzones."  Glaciers cover 10% of earth’s surface, and hold 75% of earth’s fresh water.  They cover over 15,000,000 square kilometers, U.S. glaciers cover 75,000 square kilometers, most being in Alaska.  If all this ice melted the sea level would rise seventy meters all over.  In Washington State alone glaciers provide 470 billion gallons of water each summer. Glacial movement is caused by, sliding of bottom layer ice, and rock sediment.  The pull of gravity is what causes glaciers to move down hill.  Glaciers only move less then a foot per day. 

GLACIER EROSION

Glaciers are a big part of erosion.  They have made many lakes and harbors, such as the Great Lakes, and Puget Sound.  Glacier erosion takes place in the subglacial zone. When a glacier moves across the land they pick up, and push rocks out of the way. When rocks are collected in the glacier they wear away more rock.  This process is called "abrasion." 

FRICTION

Friction is the resisting force overcome when two masses rub together which either slows down, or stops the object.  Rough surfaces catch on each other as they slide past.  All surfaces are rough at the microscopic level even though they may seem smooth to the eye. 
 There are many types of friction.  Some are static friction, which occurs with stationary objects.  Static friction is what stops objects from moving across a surface.  It is what keeps a book from sliding off a tilted desk.  Sliding friction occurs between moving objects.  Rolling friction occurs when a ball or log rolls on a surface. Fluid friction is the resistance the walls of a pipe or container provide against a moving liquid or gas.

RIVERS AND STREAMS

Rivers are large bodies of water that flow down hill in a channel like form.  All rivers sooner or later end up in the ocean or a lake.  The longest river is the Nile River in Africa, which is 4,145 miles long.  The next longest is the Amazon in South America, which is 4,000 miles long.  Even though it isn’t as long as the Nile, it holds more water than the Nile, and Mississippi Rivers. 
Rivers and streams come from snow melt and rain fall.  When the snowmelt collects, it forms small streams called gullies.  When gullies meet with many other gullies it forms a river. 
Rivers have been part of are lives from before the Egyptian Faeroes to present day.  Rivers give us electricity, transportation, trade, and a source of irrigation.  River systems consist of the river it self, and the surrounding streams that supply the river with water. 

SUMMARY

       Erosion, the wearing away of soil and rock, is both good and bad towards humans. Erosion is bad because it can threaten our homes and crops.   Erosion is good towards humans because it changes the shape of the earth.  Water is a requirement to human and animal life.  Water is the main component to erosion. That is the conclusion to my research report.
 

 


BIBLIOGRAPHY
 

"Erosion" http;//www.irim.com/ssm/ssm0052.htm

"Erosion" http//www.bartlyby.com/65/er/erosin.html

"Friction" http://www.reconstuctionist.com/friction.htm

"Glaciers" http://www.-nside.colorado.edu/glaciers/quick facts.htm

"Glaciers" http://www.digistar.mb.ca/minsci/geology/gfad.htm

Lofmen, John M. "Erosion,"  World Book Encyclopedia, 2000.

Morgan, Joseph M. "Weather" World Book Encyclopedia, 1998

"Rivers and Streams" http://geopgraphy.about.com/library/weekly/aa031897.htm 

Walker, Sally M.  Water Up Water Down. Colorado: Colorado Books inc.  pp. 1-10

Wycoff, Jerome  "Erosion" Encyclopedia Americana 1999 E-F 556-557 

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Acknowledgements 

I would like to thank the following people, with out them my project would not be possible.
* My mom, for helping me choose my topic, and helping me with my experiment.
* My dad for driving me to the river to conduct my experiment.  Also for helping me with the supplies and equipment.
* My friends Kyle and Landin for helping me with my display board. 
* My Friends Nick, Ethan, and Cody for listening to my presintation.
* Mrs. Helms for helping me and answering my questions.
* Last but not least Mr. Newkirk for helping me with my project.  With out him I would not have come this far. 


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