Depth and Pressure:
3-Hole Demonstration

Teaching Note:
How living things respond to the tremendous pressures that occur at the bottom of oceans fascinates students and teachers alike. The following activities facilitate student learning about the relationship between depth and pressure as well as the effects of those pressures on humans and animals. This activity can be done as a class presentation or as an individual or group challenge.

Materials:

Drawing of 2 Containers with Three Holes
	Punched in Them

  • 2 containers into which you can punch holes (plastic milk jugs, milk cartons, soup cans, one gallon cans, #10 food cans)
  • Something to punch holes in those containers (hammer and nails, pen or pencil)
  • 1 ruler
  • 1 sink or large bin in which to catch water
  • adhesive tape
  • water

Teaching Note:
Run the experiment in advance of class with another pair of containers. Determine an appropriate distance between holes, as well as how much water will be dispensed into the collection sink or bin. It is important to have appropriately sized holes as well. If the holes are too small, the water will dribble out, and if they're too big, the water will pour out too fast to allow accurate measures.

Suggested Lesson:

Ask, "Where is water pressure greater, at the top of the ocean or on the ocean floor?" Ask students to explain their responses. Record responses and the students' reasons for giving them.

For small group experimentation, give groups of students the following task, and then have them report back to the class:

    "Using the following materials (two containers, hole-punching tool, tape, ruler, water bin, water), design an experiment that demonstrates one of the following:

    1. As depth increases, pressure increases
    2. As depth increases, pressure stays the same
    3. As depth increases, pressure decreases

    Allow students time to discuss, experiment, and record results.

For whole class demonstration:

    Punch three holes into each container. In the first container, punch a vertical row of holes a couple of inches apart. In the second container, punch a horizontal row of holes a couple of inches apart. Place the containers in the sink or large bin and place one piece of tape across each row of holes. Fill the containers with water. Remove the tape from each container one at a time in a swift motion. Note the length of each stream as the water spews from the container.

    For a more scientific or accurate measure of stream length, turn each container so that the holes are pointed to the right of the audience (students). Place a piece of graph paper or a ruler behind each container. (Darken the lines with a marker so that they can be seen easily.) Have one student note the length of each stream of water. Point out that the graph paper/ruler acts as a stream meter or pressure guage against which the student is able to measure the relative strengths of the two streams.

Questions for Discussion or Written Reflection:

  1. Which container had varying stream lengths?

  2. Which hole projected the longest stream of water? Which had the shortest?

  3. Did the horizontal or vertical row of holes have the same stream lengths?

  4. Were our original predictions true?

  5. Which is proven:

    • As depth increases, pressure increases?

    • As depth increases, pressure stays the same?

    • As depth increases, pressure decreases?

  6. How does our knowledge of the depth/pressure relationship affect deep-sea research?

  7. How does depth/pressure affect the type of sea life we find as we travel towards the bottom of the ocean? How do animals and plants adapt to the intense pressure of deep ocean habitats?

  8. Pressure at sea level is 14.7 pounds per square inch. What is the progression of pressure increase as we move to one mile below the surface? Does salinity or temperature affect the amount of pressure or how fast it increases? If so, how might we measure their effects?

  9. What is the best shape for a deep sea instrument housing or submersible? "Best" refers to the strongest shape for the thickness of the material.

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