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CONCEPTS
- Oxygen dissolved in water permits fish and other aquatic creatures
to breathe and live underwater.
- Less gas can remain dissolved in heated water.
- Driving the air out of water by excessive heating can kill fish through
oxygen depletion.
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MATERIALS
- Cooking pans or glass beakers
- Heating sources: Bunsen burners, or stove tops (gas or electric),
or hot plates
- Thermometers (optional)
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PREPARATION
- Teachers may wish to observe this effect first at home by putting
tap water, 2 - 4 cm (0.8 - 1.6 in) deep, in a cooking pan or large frying
pan. Use a low heat so that the water temperature rises about 10°C
(18°F) every minute. Very small dissolved air bubbles will begin
to form on the bottom at about 35°C (95°F), usually around the
edge of the pan. They will gradually expand and then rise to the surface
and pop. At about 90°C (194°F) water vapor bubbles will form
but collapse before reaching the surface. After the water starts to
boil, turn off the heat and let the water cool to room temperature.
Reheat the water and observe the lack of dissolved air.
- Try again the next day with the same water: no air bubbles should
appear. Cool the water and with the pan covered, vigorously shake the
water for about ten seconds. Reheat the water to see if air has been
dissolved. Different heat sources will produce different bubble patterns
depending on where the thermal energy is transferred.
- This activity can be done individually at home by the students, with
reports afterward, or in the classroom in small groups.
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PROCEDURE
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Engagement
- Question students if any are SCUBA divers. How do they breathe
underwater? How do fish breathe underwater? If there is an aquarium
in the classroom does it have a bubbler (aerator)? How does air
get into water in nature? How can we tell air really is dissolved
in water? This activity will give one method to answer the last
question.
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Activity
- Bring a cooking pan from home or use a school beaker.
- Pour tap water into your container to a depth of two to four
centimeters (0.8 - 1.6 in). (Alternative: Let two beakers of cold
water sit overnight or a couple of days. Put an aquatic plant
in one of the beakers. This plant's photosynthesis will add more
oxygen to alter the initial condition of this beaker.)
- Place your container over the heat source. (If using the alternative
method, remove plant from beaker. Note which beaker had the plant
in it. Heat both beakers side by side.)
- Activate your heat source at a low setting.
- Time the temperature change (if using a thermometer) to give
about 10°C (18°F) increases each minute.
- Observe the air bubbles formed on the container bottom, noting
size and distribution.
- Estimate the total number of bubbles formed (hundreds, thousands)
and their approximate diam-eters in mm.
- Just before boiling, about 90°C (194°F), notice the
different bubbles being formed on the bottom. Do they rise to
the surface as the air bubbles did?
- Continue heating the water until boiling occurs, then turn off
the heat source.
- Cool the water to room temperature by placing the pan in a sink
containing a few centimeters of water at room temperature or cooler.
- Reheat the water and look for air bubbles. How are your observations
similar to or different from your observations the first time
you heated the water. (If using the alternate method with two
beakers, put both side-by-side on a hot plate. Note any differences
between the beaker with and the beaker without the plant.)
- (Optional) If time permits, cool the water again to room temperature.
After it is cool, place a cover over the pan and vigorously shake
the water for about ten seconds. Reheat the water and again look
for air bubbles.
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Explanation
- Dissolved air in the water will expand on heating, forming bubbles
at the bottom surface. When the buoyant
force on a bubble overcomes surface tension, it will rise to the
surface and pop. With time, convection
currents in the water will cause all of the dissolved air to coalesce
and form bubbles near the warm bottom and side surfaces.
- The second set of bubbles that form near the boiling point are
water vapor bubbles. These rise to the surface once their internal
pressure exceeds atmospheric pressure. At higher elevations where
atmo-spheric pressure is lower, boiling occurs at lower temperatures.
- After the dissolved gas has been driven off through heating
and when the same water is reheated a short time later, you will
not observe bubbles until the water starts to boil. Shaking the
cool water, or using a bubbler such as those used in aquariums,
helps put oxygen and other gases back into the water.
- The amount of dissolved oxygen in freshwater and seawater is
important for life. Aquatic animals such as fish require oxygen
to live. They obtain it by processing dissolved oxygen in the
water.
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EXTENSION
- Investigate whether there is a connection between adding large amounts
of heat to rivers and the loss of fish due to oxygen depletion. What
type of natural or human-caused processes could add significant amount
of heat to rivers or seas? Are there rules and regulations that limit
the input of heat into rivers, streams, and oceans? Why or why not?
Should there be such limitations?
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VOCABULARY
- buoyant (buoyancy): 1) the tendency of an object to float or
rise when submerged in a fluid. 2) the power of a fluid to exert an
upward force on a body placed in it.
- convection: process by which, in a fluid being heated, the
warmer part of the mass will rise and the cooler portions will sink.
If the heat source is stationary, convection cells may develop as the
rising warm fluid cools and sinks in regions on either side of the axis
of rising.
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SOURCE
- "Visit to an Ocean Planet" educational CD-ROM, Copyright
Caltech and NASA/Jet Propulsion Laboratory
- Adapted from the San Juan Institute Activity Series, 1997.
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