Download EffectofTemponSolubilityofSaltGCCEGLX

Survey
yes no Was this document useful for you?
   Thank you for your participation!

* Your assessment is very important for improving the workof artificial intelligence, which forms the content of this project

Document related concepts

Physical oceanography wikipedia , lookup

Effects of global warming on oceans wikipedia , lookup

Ocean wikipedia , lookup

Global Energy and Water Cycle Experiment wikipedia , lookup

Transcript
1. 2 Effect of Temperature on Solubility of a Salt
GLX Version
Note: This is a Vernier lab that has been modified by ASIM for use with the GLX.
Introduction
Fluctuations in temperature cause changes to ocean salinity. Warmer surface waters dissolve more salts
creating a dense solution that begins to sink. Colder, less dense water rushes up to replace the sinking
denser water, creating convection currents in our oceans. Ocean currents bring warmth from the
equator toward the poles of the Earth. As global temperatures continue to rise, the increase in ocean
salinity or dissolved salts will disrupt ocean currents. Without the movement of warmer waters from
the equator, the end result could be the next ice age.
In this experiment, you will study the effect of changing temperature on the amount of solute that will
dissolve in a given amount of water. Water solubility is an important physical property in chemistry, and
is often expressed as the mass of solute that dissolves in 100 g of water at a certain temperature. In this
experiment, you will completely dissolve different quantities of potassium nitrate, KNO3, in the same
volume of water at a high temperature. As each solution cools, you will monitor temperature using a
Temperature Probe and observe the precise instant that solid crystals start to form. At this moment, the
solution is saturated and contains the maximum amount of solute at that temperature. Thus each data
pair consists of a solubility value (g of solute per 100 g H2O) and a corresponding temperature. A graph
of the temperature-solubility data, known as a solubility curve, will be plotted using the GLX.
Materials
GLX
Temperature Probe
Hot plate
Support rod for hot plate or
Ring stand
four 20 X 150 mm test tubes
Test tube rack
400 mL beaker
10 mL graduated cylinder
250 mL beaker
ring stand
2 utility clamps
stirring rod
potassium nitrate, KNO3
Procedure
1. Obtain and wear goggles.
NASA and Auburn University Global Climate Change Education
Chemistry Module
Page 12
2. Label four test tubes 1–4. Into each of these test tubes, measure out the amounts of solid shown in
the second column below (amount per 5 mL). Note: The third column (amount per 100 g of H2O) is
proportional to your measured quantity, and is the amount you will enter for your graph in Step 8.
Test tube
number
Amount of KNO3
used per 5 mL H2O
(weigh in Step 2)
Amount of KNO3
used per 100 g H2O
(use in Step 8)
1
2
3
4
2.0
4.0
6.0
8.0
40
80
120
160
3. Add precisely 5.0 mL of distilled water to each test tube (assume 1.0 g/mL for water).
4. Plug in and turn on the GLX. Connect the Temperature Probe to port 1 located on the left side of the
GLX. A temperature vs. time graph should be displayed.
5. Fill a 400 mL beaker three-fourths full of tap water. Place it on a hot plate situated on (or next to)
the base of a ring stand. Heat the water bath to about 90°C and adjust the heat to maintain the
water at this temperature. Place the Temperature Probe in the water bath to monitor the
temperature and to warm the probe. Press
to start and stop the temperature probe reading.
CAUTION: To keep from damaging the Temperature Probe wire, hang it over another utility clamp
pointing away from the hot plate, as shown in Figure 1.
Figure 1
6. Use a utility clamp to fasten one of the test tubes to the ring stand. Lower the test tube into the
water as shown in Figure 1. Note: In order to dissolve all of the KNO3, test tubes 3 and 4 need to be
heated to a higher temperature than test tubes 1 and 2. Use your clean stirring rod to stir the
NASA and Auburn University Global Climate Change Education
Chemistry Module
Page 13
mixture until the KNO3 is completely dissolved. Do not leave the test tube in the water bath any
longer than is necessary to dissolve the solid.
7. You are now ready to collect temperature-solubility data.
a. When the KNO3 is completely dissolved, press
to start collecting data.
b. Remove the Temperature Probe from the water bath, wipe it dry, and place it into the solution in
the test tube.
c. Unfasten the utility clamp and test tube from the ring stand. Use the clamp to hold the test tube
up to the light to look for the first sign of crystal formation. At the same time, stir the solution
with a slight up and down motion of the Temperature Probe.
d. At the moment crystallization starts to occur, press to stop
data collection. Record this
temperature in the data table beside the appropriate mass of KNO3.
e. After you have saved the temperature-mass data pair, return the test tube to the hot water bath
for just long enough to redissolve the crystals.
f. Place the Temperature Probe in the water bath for the next trial and return the test tube to the
test tube rack.
g. To clear the memory for the next data collection, select the Home key
check mark
Delete
and then use the
to select Data Files. The current, and probably only, file is highlighted. Select
and then OK
. Press the Home key
again and then Graph
.
8. Repeat Steps 7 and 8a – 8g for each of the other three test tubes. Here are some suggestions to save
time.
 One lab partner can be stirring the next KNO3-water mixture until it dissolves while the other
partner watches for crystallization and records data pairs.
 Test tubes 1 and 2 may be cooled to lower temperatures using cool tap water in the 250 mL
beaker. This drops the temperature much faster than air. If the crystals form too quickly, briefly
warm the test tube in the hot-water bath and redissolve the solid. Then repeat the cooling and
collect the data pair.
9. When you have collected the fourth and last data pair and have cleared the memory, disconnect the
temperature probe. Discard the four solutions as directed by your instructor.
10. Graph the four data points.
NASA and Auburn University Global Climate Change Education
Chemistry Module
Page 14
a. From the Home screen
Column, press
, select Table
. Select Edit
and then New
Data
to select. Repeat for a second data column.
b. To label a data column, press
the desired title, and press
Properties…, and press
to highlight the titles, sse the arrow keys
to select it. Use the arrow keys
to scroll to
to scroll to Data
to select it. Measurement Name is highlighted. Press
it, and type in solubility. Press
to make the change. Use the arrow keys
Measurement Unit, and press
to select it. Type in g solid/100g water. Press
the change. Select OK
to select
to scroll to
to make
when done. Repeat the process to name the second column
temperature with degree c as the unit.
c. Use the arrow keys
to scroll to the first cell in the first data column. Select Edit Cell
and type in the first solubility value. Press
are entered in the first column. Press
to enter it. Continue until all four values
and use the arrow keys
to scroll to the first cell
in the second data column. Repeat the process to enter the temperature data.
d. From the Home screen
, select Graph
. Make sure that solubility is on the x-axis
and temperature is on the y-axis. To change a title press
arrow keys
to scroll through the titles. Press
to scroll to the desired title, and press
e. Press Auto Scale
to highlight the titles and use the
to select the title, use the arrow keys
to make the change.
.
11. Print a copy of the graph of solubility vs. temperature. Draw a best-fit curve for the data points on
your printed graph if needed. Label both axes and show correct units. Give your graph an
appropriate title. Label tick marks with the numerical values they represent. Note: If you did not
print a graph, manually plot a graph of solubility of KNO3 vs. temperature using your data.
NASA and Auburn University Global Climate Change Education
Chemistry Module
Page 15
Name _____________________________
Name _____________________________
Period ____________ Date ____________
Data Table
Trial
Solubility
(g / 100 g H2O)
1
40.0
2
80.0
3
120.0
4
160.0
Temp
(°C)
1. According to your data, how is solubility of KNO3 affected by an increase in temperature of the
solvent?
2. Using your printed graph, tell if each of these solutions would be saturated or unsaturated:
a. 110 g of KNO3 in 100 g of water at 40°C _____________________________
b. 60 g of KNO3 in 100 g of water at 70°C _____________________________
c. 140 g of KNO3 in 200 g of water at 60°C _____________________________
3. According to your graph, will 50 g of KNO3 completely dissolve in 100 g of water at 50°C? Explain.
4. According to your graph, will 80 g of KNO3 completely dissolve in 100 g of water at 30°C? Explain.
5. At 30°C, approximately how many grams of KNO3 would dissolve in 100 g of water?
NASA and Auburn University Global Climate Change Education
Chemistry Module
Page 16
EXTEND
1.
Visit
NASA’s
website
http://nasascience.nasa.gov/earth-science/oceanography/physicalocean/salinity. Answer the following questions:
 Where are the highest salinity and the lowest salinity of oceans found?
 Why higher seawater salinity is found in the middle of oceans near the equator?
 Why lower seawater salinity is found near the Arctic and Antarctic areas?
 Describe two techniques used for measuring ocean water salinity. Which method can provide a
complete global data with relatively short periods (a few days) of time?
EVALUATION
1.
2.
What do you think about the effect of temperature on the solubility of a salt on our oceans?
What do you think will happen if the earth’s average temperature continues to rise?
NASA and Auburn University Global Climate Change Education
Chemistry Module
Page 17