Purpose:
The purpose
of the lab was to further understand the transfer of heat through the
observation of sand and water.
Hypothesis:
I predict
that the water will heat faster than the sand. I also predict that the water
will cool down quicker.
Materials:
·
2
thermometers
·
2
beakers, 400 mL
·
Water,
300 mL
·
Metric
ruler
·
String
·
Ring
stand and two ring clamps
·
Sand,
300 mL
·
Lamp
with 150-W bulb
·
Clock
or stopwatch
·
Graph
paper
Procedure:
1. Fill one beaker with 300 mL of dry
sand
2. Fill the second beaker with 300 mL of
water at room temperature
3. Arrange the beakers side by side
beneath the ring stand
4. Place one thermometer in each beaker
5. Suspend the thermometers from the
ring stand with string
6. Position the lamp so that it is about
20 cm above the sand and water. There should be no more than 8 cm between the
beakers.
7. Record the temperature of the sand
and water in the data table
8. Turn on the lamp. Read the
temperature of the sand and water every minute for 15 minutes. Record the
temperatures in the Light On column in the data table.
9. Turn the light off. Read the
temperature of the sand and water every minute for another 15 minute. Record
the temperatures in the Light Off column.
Results:
·
The
water heated up within the first 8 minutes.
·
The
temperature of the sand did not appear to rise.
·
Once
the lamp had been shut off, the temperature of the water rose at the 20 minute
mark.
·
Once
again, the temperature of the sand did not change.
Conclusion:
The purpose
of this lab was to observe the transfer of heat by comparing the heating and
cooling of sand and water. My hypothesis was that the water would heat and cool
faster than the sand. The results showed that the water heated and cooled while
the sand’s temperature remained the same. Although the results supported the
hypothesis, the information gathered stated otherwise. Sand is supposed to heat
up faster than water. This is because in general the land surface, being less reflective and more
absorbent, will absorb a great deal of solar radiation, and will
have a significant increase in temperature on a bright sunny day. The ocean, at
the same time, will reflect a greater portion of the radiation, causing it to
take longer to absorb the heat. The results most likely ended up like this
because a lamp was used instead of radiation from the sun. The data collected
showed that the temperature of the sand remained at 25°C and the temperature of
the water rose from 23°C to 24°C. The temperature then decreased back to 23°C. This
lab helped me understand why the sand at the beach is normally hot while the
water is typically cold. . Knowledge like this is good to have when you are at
the beach so you can somewhat predict how cold or warm the water will be based
on how warm the sand is.