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Lab Report On Chemical Weathering

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Jesus Chavez

Chemical Weathering

Background Information:
First of all chemical weathering is when there is rainwater that is able to react with mineral grains in rocks to form new minerals and also soluble salts. This type of reaction would usually occur when the water is slightly acidic. For this reaction to occur it needs water and would occur more rapidly at higher temperatures for example damp and warm climates would be the best for this reaction to occur. Chemical weathering usually happens more often in the spring because this is when it is more humid and hot outside and that is what chemical weathering needs for it to occur and also when it is usually hot or humid there will also be water.

Purpose: The purpose of this lab is to simulate the effects of slightly acidic rainwater on rocks and minerals.

Hypothesis: If the level of acidity rises of the solution being placed on the rock or mineral then a greater amount of dissolving will happen because of more acidic solution will destroy more chemical bonds in the rock/mineral.

Procedure:
- Get a scale and record the initial mass of the limestone chips
- Get 5 50mL beakers and fill the first one with 30 mL of water
- Fill the second beaker with 30 mL of hydrochloric acid (strength:1 M)
- Fill the third beaker with 30 mL of hydrochloric acid (strength:2 M)
- Fill the fourth beaker with 30 mL of hydrochloric acid (strength:3 M)
- Fill the last beaker with 30 mL of hydrochloric acid (strength: 6 M)
- Then place

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