PURPOSE: To observe the neutralization of acid snow by different minerals.
MATERIALS:
INTRODUCTION: Precipitation has a natural pH of approximately 5.6 which is slightly acidic. However, recent studies have measured precipitation with pH values as low as 3 in some areas. Oxides of sulfur (SO2 and SO3) and nitrogen (NO and NO2) are emitted from power plants, factories, and cars. Corrosive sulfuric and nitric acid are formed when these oxides combine with water vapor in the clouds.
Acid precipitation in the form of acid snow is especially hazardous. In spring, "acid shock" may result when melting snow runs into lakes and streams. This surge of acid may be lethal to organisms. Even though the pH may slowly rise during the summer, the damage has been done.
The bedrock in the drainage basin of a lake can reduce the effects of acid on organisms. The minerals in some bedrock neutralize the acid. Lakes with this type of bedrock may receive a great deal of acid with little long term change in pH. In other lakes, neutralization cannot occur because of different soils and bedrock.
In this activity you will test the ability of different minerals to neutralize the acid in snow. Granite (feldspar and quartz, SiO2) and limestone (calcium carbonate, CaCO3), two common types of bedrock, will be used.
PREDICTION:
1. Which rock will best neutralize the acid in snow?
PROCEDURE
A. Line the bottom of one container with a layer of granite and the bottom of a second container with limestone.
B. To simulate a lake, add distilled water to a depth of 5 cm above the stones. Record the pH of the water in both containers.
C.
D. Add half of each bucket of snow to each container. The same amount of snow should be added to each. Record the pH of the water in both containers.
E.
F. The following day, record the pH of the water in each container.
DATA TABLE:
Snow pH: __________
|
"Bedrock" of Simulated Lake |
Original pH |
pH After Adding Snow |
Final pH |
|
Limestone |
|
|
|
|
Granite |
|
|
|
CONCLUSIONS:
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DISCUSSION:
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