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The Distance that Water Jets Travel from a Container

Cory Peters

 

Table of Contents

 

 

Background

Statement of Problem

Hypothesis

Materials

Diagram of Experiment

Procedure

Results

Remarks

Analysis

Potential Improvements

Conclusion

Bibliography

Relevant Links

Raw Data: Text .:. Excel

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Background:

            Pressure is a measure that defines the force an object exerts over an area. The SI unit of pressure is the Pascal, which is equivalent to 1 Newton per square meter of area. Pressure is present everywhere in the form of the atmospheric pressure, equivalent to around 101,325 Pascals of pressure, conveniently called 1 atmosphere of pressure. This is caused because there is around 100 km of atmosphere, which weighs down on the surface of the Earth. Pressure caused by a fluid which presses down on a surface is known as hydrostatic pressure. Hydrostatic pressure can also be observed in water, such as at the bottom of the Marianas Trench, where hydrostatic pressure creates pressures of around 110,000,000 Pascals.

            Another such example of hydrostatic pressure comes from leaks in containers of water. The hydrostatic pressure exerts a force to the water escaping from a container of water, causing it to spill out the sides at a horizontal velocity, rather than falling down the sides. This results in the spills going out some horizontal distance from the container due to the distance from the ground giving the water both time to fall and an initial horizontal velocity. One would expect that the ideal ideal distance that the water would travel would come from a leak somewhere in the middle of the container because a leak at the bottom would not give the water enough time to fall and gain distance, and a leak at the top would not provide enough pressure to gain enough distance. Therefore, one would suspect that a container with a leak in the middle would cause a leak with the greatest distance due to it equalizing the two opposing factors of the bottom giving enough force, but not enough time, and the top giving enough time, but not enough force. However, the leak would most likely be slightly more towards the top because atmospheric pressure would also result in the water gaining horizontal velocity, and is independent of the initial height, leading to a constant horizontal force that is independent of height, negating part of the reason why a leak at the top would be unideal. Additionally, Torricelli's Law states that the velocity of a jet of water out of a can has a velocity of where g is the acceleration due to gravity and h is the height from the top of the container. Combining this with the fact that the time it takes a projectile to fall from a height h is , the result is that the total distance traveled is , which has a maximum when h is exactly half of hmax.

 

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Statement of Problem:

            The purpose of this investigation is to measure the effect of changing the height of a hole in container of water has on the distance of the resulting jet.

 

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Hypothesis:

            The distance traveled by the water jets will be approximated by the equation where h is the height from the bottom of the container of the hole, which means a general curve which peaks at the point 10 cm in height and 20 cm in distance.

 

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Materials:

       Empty 2L bottle of soda - used as the container that water will be shot from.

       Drill - used to make uniform holes in the bottle

       Ruler - used to measure the appropriate heights of the holes

       Caliper - used to measure the distance of the water jets to a high degree of accuracy

       Ruler - used to measure the distance of the height of the water and the holes on the bottle

       Watering can - used to refill the bottle to the same water level between experiments

       Paper - placed beneath the bottle to have a spot to jot where the water strikes

       Marker - used to a) mark a fill line on the bottle to ensure consistent water levels between tests b) mark where the bottle is placed on the paper to measure the distance the jets travel c) make a hole in the paper where the water jets land from each trial

       Tape - used to cover the holes in the bottle when not in use

 

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Diagram of experiment:

 

 

 

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Procedure:

 

            To begin the experiment, a line 20 cm above the bottom of the bottle was drawn in with the marker using the ruler to measure the 20 cm distance. Then, holes were drilled into the bottle at regularly spaced intervals, using the ruler to ensure that they are the correct distance apart and the drill to create the holes into the bottle. Additionally, how high each of the holes were from the bottom of the bottle was measured and recorded for later use. Then, tape was placed over each of the holes to make sure water doesn’t spill from the bottle while filling up with water. In the next step, the bottle was filled up to the earlier demarcated 20cm fill line. In addition, a watering can was filled up to refill the 2 liter bottle with water in between experiments in order to guarantee that the amount of water was consistent between trials. A long piece of paper was placed beneath the bottle to give a surface to mark how far each water jet traveled. In addition to the piece of paper, a line was drawn from the start of the bottle on the paper to more easily measure the distance traveled by the water in later steps. For each hole, the piece of tape covering it was removed, the location where the water stream landed marked on the piece of paper with the marker, the tape reapplied, the bottle refilled to the 20 cm line using the watering can and then the bottle was shifted over and this process was repeated to create 5 data points per hole. After marking these 5 data points, the calipers were used to measure the distance between the line where the bottle started and the marked hole. The tape was then reapplied to the hole, a new sheet of paper was placed under the bottle, and the process of data collection was repeated using a different hole.

 

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Results:

 

Height of hole above bottom (cm)

Distance of Water (cm)

Expected Distance (cm)

Hole 1

0

5.33±.368

0

Hole 2

2.5±.05

15.82±.445

13.23±0.151

Hole 3

5.0±.05

17.76±.584

17.32±.115

Hole 4

7.5±.05

17.96±.445

19.36±.103

Hole 5

10.0±.05

16.70±.699

20.0±.100

Hole 6

12.5±.05

15.86±.203

19.36±.103

Hole 7

15.0±.05

15.36±.406

17.32±.115

Hole 8

17.5±.05

7.69±.165

13.23±0.151

 

Table of the results

 

                                              Raw Data: Text .:. Excel

 

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Remarks:

 

            With the exception of hole 2 and hole 3, all the observed data points traveled a shorter distance than the distance predicted by the model due to Torricelli’s law ( ) where hmax is 20 cm. There are a couple of factors that can be attributed to this, one is the drag caused by the air friction, making each water jet travel slightly less further than if this experiment were done in a vacuum, which is what the mathematical model assumes. Additionally, there was likely systematic error because the line drawn to mark the location of the bottle on the paper was drawn in by hand, adding the potential for error due to the inability of humans to draw proper straight lines and place lines correctly. Additionally, because the lines were drawn in with the bottle already placed down, the only way for the location to vary is to vary away from the bottle, creating error in the fact that all the measured distances will be slightly too small due to the systematic human error in drawing the line.

 

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Analysis:

 

            One of the things predicted by the mathematical model is that there will be a peak value at a height that is 10cm with a distance of 20cm. In the observed data, the peak value is located at 7.5 cm up the bottle with a distance of 17.96cm. The factors influencing the distance to be shorter than predicted were earlier discussed. In addition, the graph of the observed data appears to peak sooner than the mathematical formula. After the peak on the graph, all the data is decreasing, which happens at the 7.5cm mark instead of the 10cm mark. There are several potential reasons for this discrepancy such as the air resistance having more time to take effect at higher elevation holes, or the fact that higher heights are more greatly influenced by the specific level filled to because the velocity is proportional to the square root of the height above the hole, meaning that uncertainty in the fill level will cause a larger uncertainty in the velocity of a hole higher up than a lower hole. To more easily visualize this, a difference of 1 cm in water fill will have a much larger effect on a hole that is 1.5 cm from the top than one that is closer to the bottom.

 

Chart of the percent errors

 

 

Height of hole above bottom (cm)

Distance of Water (cm)

Expected Distance (cm)

Percent error (%)

Hole 1

0

5.33±.368

0

N/A

Hole 2

2.5±.05

15.82±.445

13.23±0.151

19.6

Hole 3

5.0±.05

17.76±.584

17.32±.115

2.56

Hole 4

7.5±.05

17.96±.445

19.36±.103

7.27

Hole 5

10.0±.05

16.70±.699

20.0±.100

16.5

Hole 6

12.5±.05

15.86±.203

19.36±.103

18.1

Hole 7

15.0±.05

15.36±.406

17.32±.115

11.3

Hole 8

17.5±.05

7.69±.165

13.23±0.151

41.9

 

There appears to be no blatant pattern to the percent errors - they are neither all going up nor going down nor remaining constant - which is indicative that the divergence between the expected and observed results was most likely not due to systematic error but rather random error or an invalid mathematical model. However, one piece that appears significant is that the lower holes are more conforming to the model than the higher holes. For instance, the two least percent errors present in the chart (2.56% and 7.27%) occur in the lower half of the holes and the greatest error comes from the very top hole (41.9%). This could represent that there were errors that were more pronounced from the higher holes. For instance, there could be more time for the air resistance to affect the higher holes, this slowing the water jets down and causing this greater discrepancy between the mathematical predictions and the observed data. In addition, some other potential sources of error are enumerated below.

 

       Human error - placing the mark where the 2 liter bottle is and marking where the water jets fall

       Non-consistent setup - the marker used to indicate the 20cm fill line was thick and therefore the amount of water placed into the bottle could be slightly different between trials due to difficulty seeing the exact 20cm fill mark.

       Errors due to equipment - the roundness of the hole also affected the distance that the water jet traveled. For instance, while doing this experiment, the original hole 3 was drilled improperly and could not properly create a water jet. What this demonstrated was that the more circular the hole the longer the jets would travel and the less circular the jets the less distance. Therefore, due to the difficulties in cutting into plastic 2 liter bottles, there could have been error due to not every hole being perfectly round.

 

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Potential improvements:

 

       Different material - using a different material would also holes to be properly drilled and thus avoiding any errors caused by non uniform holes in the bottle

       A more consistent fill line - either using a thinner marker or gathering all the water spilled between trials would allow for more consistent water level between trials. Another option would be to use an actual cylindrical container instead of one that tapers off at the end like a 2 liter bottle does so that the container can be filled to the brim between trials for a consistent fill line

 

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Conclusion:

 

            Despite the data not following the exact results predicted by the mathematical model, it still follows the general trend of increasing rapidly until it peaks in the middle at around 20cm and then slowly decreases, increasingly so towards the bottom. In addition, the peak obtained in the data is only one hole away from the hole ½ of the way up, which is one of the key predictions of the mathematical model, so the hypothesis that the distance traveled by the water jets is  where h is the height from the bottom of the container is supported by this experiment.

 

 

 

 

 

 


 

Bibliography

 

“About the Mariana Trench - DEEPSEA CHALLENGE Expedition.” DEEPSEA CHALLENGE, National Geographic, 1 July 2014, www.deepseachallenge.com/the-expedition/mariana-trench.

 

The Editors of Encyclopædia Britannica. “Atmospheric Pressure.” Encyclopædia Britannica, Encyclopædia Britannica, Inc., 12 Jan. 2018, www.britannica.com/science/atmospheric-pressure.

 

Pielke, Roger A. “Atmosphere.” Encyclopædia Britannica, Encyclopædia Britannica, Inc., 12 Jan. 2018, www.britannica.com/science/atmosphere.


 

 

 

 

 

 

Relevant Links

 

https://en.wikipedia.org/wiki/Torricelli%27s_law - Statement and derivation of Torricelli's theorem

https://en.wikipedia.org/wiki/Bernoulli%27s_principle - Principle from which Torricelli’s theorem is derived

https://en.wikipedia.org/wiki/Hydrostatic_test - Example of the considerations taken in the real world as a result of the effect described in this paper

http://adl.stanford.edu/aa222/Lecture_Notes_files/chapter2_singlevar.pdf - Description of process used to calculate the theoretical maximum of the distance of the jets

https://www.nottingham.ac.uk/nmp/sonet/rlos/bioproc/starlings/3.html - Description of the source of pressure in this experiment