Chemical Weathering

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Jared Dorfman November 9, 2017 Period 1
Chemical Weathering
Background:
Chemical weathering is occurred by rainwater reaction to the mineral grains and it is new new rocks that form and become sobule. This reaction happen when the water is slightly acidic with the minerals and rainwater. Chemical weathering needs water, and when the temperature is warm the climate will grow. Words to understand when learning chemical weathering is mineral grains. (Mineral grains is found in very small rocks, and it is very hard to see them.) Chemical weathering takes place in almost all types of rocks. Smaller rocks are found in chemical weathering however, because they …show more content…

Sometimes carbon dioxide from the air and soil combine with the water. That produces a weak acid called carbonic acid that can dissolve rocks. Chemical weathering is made up of rocks and soil. And Carbon Dioxide is form from the air or the soil that is combined with the water. When it is all produced it will be called carbonic acid That will be able to dissolve rocks. Carbonic acid is dissolved into limestone. Carbonic can go underground into the limestone, and it can open up caves. Also, chemical weathering works with iron. They become rust and it becomes a process called oxidation. A word that people should understand more is limestone. (Limestone is a hard sedimentary rocks, and they are composed.) The Purpose: The purpose of this experiment is to demonstrate how chemical weathering affects the different types of rocks.

Hypothesis: If different rocks is put into acid then the limestone will add mass because it is a sedimentary rock is formed by sediment and often formed when weathering and erosion break down a …show more content…

Our hypothesis for this lab was that the limestone will add mass because it is a sedimentary rock, and weathering and erosion break down a rock. Our data refute our hypothesis because we said it will gain mass when the limestone lost mass. The limestones Initial mass was 3.67, and after we put it in the oven the mass went down too 2.81. The mass went down by 0.86. Also, the graph above shows our data. The red line of the graph was the change in mass after we put it in the oven, and the blue line is the Initial mass. The red line doesn't move that much. After we put the rocks in the oven only one changed in mass. The Limestone changed 0.86 in mass, Quartzite changed 0.00 in mass, and Obsidian changed 0.00 in mass. By that data the oven did not really change the difference in mass. The blue line is our initial mass. Limestone was 3.87, Quartzite was 67.51, and Obsidian was 10.63. In the graph it shows the blue line going up. Our initial mass goes up, but our final mass stayed the same besides the limestone changed by 0.86. In the graph there were two trends. One goes up, and the other one basically stayed the same. The initial mass had a bigger impact because we used 3 rocks, and they were different masses. For the final mass the trend wasn’t that good because two of the final masses stay the same at zero, and the one that changed in mass was only a 0.86

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