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Gravity-Driven Fluid Flow
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Objective: · To study gravity-driven fluid flow that is caused by differences in solution density. Science Standards: Science as Inquiry |
- abilities of technological design Science Process Skills: |
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Activity Management MATERIALS AND TOOLS
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If using this as an activity, provide each student group with a set of materials. Salt canisters, food coloring dispensers, and measuring cups can be shared among groups. The materials list calls for glass beakers or tall drinking glasses. Other containers can be substituted such as mason jars or plastic jars like those in which peanut butter is sold.
The vials are available from school science supply catalogs for a few dollars per dozen. Choose glass vials with screw tops and a capacity of 3 to 4 ml. Small cologne sample bottles can be substituted for the vials. It is important that the vials or bottles are not too large because the process of lowering large containers into the beakers can stir up the water too much. It is recommended you tie the string around the neck of the vial yourself to make sure there is no slippage.
The student instructions ask the students to conduct three different experiments. In the first, the effects of saltwater and freshwater are investigated. In the second, the effects of warm and cold water are investigated. The third experiment is an opportunity for students to select their own materials. They might try mixing oil and vinegar, sugar and saltwater, or oil and water. It may be necessary for the third experiment to be conducted on another day while the new materials are collected.
Give each student group at least one set of instructions and two data sheets. Save the student reader for use after the experiment.
Assessment:
Discuss the experiment results to determine whether the students understand
the concepts of buoyancy and sedimentation. Collect the student pages
for assessment of the activity.
Extensions:
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Gravity is an important force at work in the movement of fluids. Fluids can be liquids or gases. The important thing about fluids is they can flow from place to place and can take the shape of the container they are in. When you pour a liquid from one container into another, gravity is the driving force that accomplishes the transfer. Gravity also affects fluids "at rest" in a container. Add a small amount of heat to the bottom of the container and the fluid at the bottom begins to rise. The heated fluid expands slightly and becomes less dense. In other words, the fluid becomes buoyant. Cooler fluid near the top of the container is more dense and falls or sinks to the bottom. Many crystals grow in solutions of different compounds. For example, crystals of salt grow in concentrated solutions of salt dissolved in water. In the crystal growth process, the ions that make up the salt come out of solution and are deposited on the crystal to make it larger. When this happens, the solution that held the molecule becomes a little less salty than it was a moment ago. Consequently, the density of the solution is a little bit less than it was. This, in turn, causes a fluid flow in the solution. The slightly less salty solution is buoyant and rises to the top of the container while saltier, or more dense, solution moves in to take its place. |
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Scientists are interested in gravity-driven fluid flows because they have learned that these flows, when occurring during the growth of crystals, can create subtle changes in the finished crystals. Flaws, called defects, are produced that can alter the way those crystals perform in various applications. Crystals are used in many electronic applications, such as in computers and lasers.
To learn how to grow improved crystals on Earth, scientists have been growing crystals in the microgravity environment of Earth orbit. Microgravity virtually eliminates gravity-driven fluid flows and often produces crystals of superior quality to those grown on Earth. One of the major areas of materials science research on the International Space Station will involve crystal growth.
Gravity-Driven Fluid Flow
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Procedure
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Second Experiment Procedure:
Original Experiment:
