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Developers:
Joanne
Beals
Saint Anselm School
Philadelphia, PA
Albert
Rieck
Rohm and Haas Company
Spring House, PA
Grade
Level:
5
through 8
Disciplines:
Earth
Science, Engineering, Mathematics
Goals:
Upon
completion of this lesson, the students will
- understand
that the sun in the driving force for the water cycle.
- understand
evaporation, condensation, and precipitation.
- identify,
test, and measure the solids in fresh and salt water.
- learn
how to desalinate water using a simple still.
- investigate
the different densities of salt and fresh water.
- recognize
the importance of El Ni�o and its affects on
ocean currents.
Summary:
This
unit on salt water is divided into three investigations
related to the water cycle.
- Evaporation
- Water is constantly evaporating from the oceans.
The salt, however, remains behind during this process.
The students will perform a simple windowsill evaporation
test on distilled, tap and salt water. They will examine
the solids and determine what percentage of each water
sample was solid.
- Condensation
- Using a still, students will simulate the evaporation
of ocean water, have it condense on the sides of a
container and allow it to precipitate back into the
container as fresh water, demonstrating how precipitation
is fresh water from the ocean.
- Precipitation
- El Nino and other weather patterns induced by ocean
currents will be simulated in an investigation in
the differing densities of fresh and salt water.
Investigation
1: How much salt is in distilled, fresh, and ocean water?
Objectives:
Upon
completion of this lesson, the students will
- measure
and weigh water samples and aluminum weigh pans.
- use
a scale correctly.
- determine
percentage of salt in the samples.
Materials:
Salty
water - 35 grams of salt per liter of water
Tap water
Distilled water
Pipettes
Balance - capable of measuring to 0.01 gram
Aluminum weigh pans
Oven for faster evaporation - 3000F for 20
minutes (optional)
Vocabulary:
Distilled
water
Procedure:
- Weigh
six numbered aluminum weigh pans. Record the weight
of each pan.
- Fill
two of the pans with a pipette of tap water, two with
distilled water, and two with simulated ocean water.
Weigh and record the weight of each pan. This is the
wet weight.
- Place
the pans on the windowsill and let the water evaporate.
In a few days, depending on the temperature, humidity,
and time of year, the pans will be dry. Weigh the
pans again. This is the dry weight.
- Calculate
the percentage of solid in each sample.
- wet
weight - pan weight = solution weight
- dry
weight - pan weight = solids weight
- solid
weight divided by solution weight times 100% = %
of solids in solution
Sample
Data Chart:
|
Pan Number
|
Pan Weight
|
Wet Weight
|
Dry Weight
|
Solution
Weight
|
Solids Weight
|
%
|
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Distilled
1
|
1.28
|
2.27
|
1.29
|
0.99
|
0.01
|
1.0%
|
|
Distilled
2
|
1.26
|
3.92
|
1.29
|
2.66
|
0.03
|
1.1%
|
|
Tap 1
|
1.26
|
2.39
|
1.28
|
1.13
|
0.02
|
1.8%
|
|
Tap 2
|
1.29
|
2.30
|
1.30
|
1.01
|
0.01
|
1.0%
|
|
Sea 1
|
1.28
|
2.41
|
1.33
|
1.13
|
0.04
|
3.5%
|
|
Sea 2
|
1.29
|
3.66
|
1.40
|
2.37
|
0.11
|
4.6%
|
Critical
Thinking Questions:
- Why
does seawater have the largest amount of solids?
- Why
does the distilled water have the least amount of
solids?
- Why
do we test two samples of each type of solution?
Investigation
2: Why is rainwater fresh if it evaporates from a salty
ocean?
Objectives:
Upon
completion of this lesson, the students will:
- build
a still from the materials provided.
- simulate
ocean water by mixing salt and tap water.
- test
condensed water for saltiness.
- understand
that only fresh water evaporates from the ocean.
Materials:
2
liter beaker tape
400 ml beaker plastic wrap
100 ml beaker straws
salty water - 18 grams of salt per 500 ml
Vocabulary:
Desalination,
distillation, purification
Procedure:
- Make
seawater by mixing 18 grams of salt in 500 ml of water.
- Measure
out 50 ml of salt water into a 100-ml beaker.
- Place
the 400-ml beaker upside down inside the 2-liter beaker.
- Place
the 100-ml beaker of salty water on top of the 400-ml
beaker.
- Build
a teepee of straws and tape them to the inside rim
of the 2-liter beaker.
- Place
plastic wrap around the straws and the outside edge
of the 2-liter beaker. Make sure that it is airtight.
- Place
the container in bright sunlight and check for condensation.
- After
considerable condensation has occurred, unwrap the
plastic and taste the water that has condensed on
the sides of the container.
Diagram:
Straws - Plastic wrap
2 L beaker
100
mL beaker
400 ml beaker
Discussion
Questions:
- Why
does the water condense on the plastic wrap?
- Why
does the container need to be placed in the sun?
- What
does the plastic wrap do?
- What
part of this experiment corresponds to precipitation?
- Where
are the salt particles if the condensed water is fresh
water?
Investigation
3: What type of water is denser - Fresh or Sea Water?
Objectives:
Upon
completion of this lesson, the students will:
- simulate
ocean water.
- demonstrate
that fresh water floats on top of salt water because
it is less dense.
- recognize
that wind helps create surface currents.
- understand
that deep cool ocean currents regulate surface temperature.
- see
that cold deep water currents can rise above warmer
currents because of wind action.
- learn
that El Nino is characterized by lack of winds on
the ocean's surface.
- see
that weather patterns are the result of ocean temperatures.
Materials:
Clear
Pyrex baking dish
ice
Red and blue food dye
beaker
Salty water - 145 grams of salt in 1 liter of water
Vocabulary:
density
Procedure:
- Fill
a glass baking dish half full with warm tap water
(20-250C).
- Add
a few drops of red food dye and mix.
- In
a separate beaker mix 145 grams of salt with 1 liter
of tap water and dye the water blue.
- Add
ice to the salt water until it is very cold (5-100C).
- Slowly
pour the icy salty water into the red warm water.
- Observe
the results.
- Blow
gently on the surface of the water and observe the
results.
Diagram:
Notes:
The
icy blue water will flow along the bottom of the pan.
It does not mix with the red surface water. The students
will expect to see purple. When they blow on the surface
they can see the icy water begin swirling to the surface.
When there is an El Nino the ocean winds do not blow,
so the surface water continues to heat up making it
more difficult for the cool deep water to surface because
it is denser that the warm surface water. During El
Nino, there is widespread ocean warming which has the
effect of changing weather patterns, such as those experienced
in 1998.
Discussion
Questions:
- Why
isn't the water purple from the side view?
- Why
are there two distinct layers?
- Why
did the blue water sink and flow along the bottom?
- Why
does the wind cause the cold water to rise to the
surface?
Data
Chart:
|
Sample
|
Pan Weight
|
Wet Weight
|
Dry Weight
|
Solution Weight
|
Solids Weight
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%
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Distilled
1
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| Distilled
2 |
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Tap
1
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Tap 2
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Sea 1
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Sea 2
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This experiment is courtesy of 
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