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
Use ice if you need to. Then, fill one beaker with 175 mL of water and the other with 350 mL. Warm the water in the 350mL beaker up to 55 degrees celsius and cool the water in the 175mL beaker to 15 degrees celsius, the same temperature as the pitcher because it will be your control group. Once the beaker that should be heated is at 55 degrees celsius, pour 175 mL of the water into a glove and pour the other 175 mL into a ziplock baggie. Pour the 15 degrees celsius, 175 mL of water into another ziplock baggie. Before you set these in water, have a stopwatch ready and make sure that the water in the baggies and glove is at the right temperature.
In site one there was a high proportion of very unspherical rocks. According to this the hypothesis is right, in site two there is a lot more smother rocks medium sized and in site 3 there are very small pebbles which are very smooth and spherical. The pebbles get smoother and rounder while it goes downstream. Due to us only taking about 10 rocks our result may have been not right as there were some pebbles which were largely over sized. Most of the other load is dissolved by solution such as limestone and chalk
Thereafter I used a pipette to meticulously drop in water up to the 250ml mark.
In the lab we filled the first beaker up with water. Then we took a pipet (filled with the liquid) and dropped water droplets onto the
The purpose of this particular lab was to experiment and identify the chemical and physical changes throughout the experiment.
The main objective of this experiment is to differentiate between a physical change and a chemical change.
Complete this week’s lab by filling in your responses to the questions from Geoscience Laboratory. Select answers are provided for you in red font to assist you with your lab work. Although you are only required to respond to the questions in this worksheet, you are encouraged to answer others from the text on your own.
Examine a piece of nichrome wire. On the data sheet, record the color and the luster of the metal. Use a forceps to hold the wire in the flame of your burner for about two minutes (recall where the hottest part of the flame is located). Describe the appearance of the wire while held in the hottest part of the flame. Allow the wire to cool and reexamine it. From your observations, determine if there was a physical or a chemical change. Give specific reasons for your conclusions. Save the nichrome wire for step #2.
Christopher and Kate noticed that after a rainstorm some of the rocks in their yard appear to shrink. They wondered how the mass of the rocks changed when dissolved in water. To
Fill a test tube about 1/3 full with cold tap water for use in step 34.
4.Measure 35mL of warm water and add them into each of the 4 test tubes at about roughly the same time. It is essential that the water is warm. Do not seal the test tube.
2. Fill a flask with pure water (0% sugar), another with 0.2M water, another flask with 0.4 M water, and another flask with 0.8M water.
XII. Take the 250 ml beaker to your lab bench. Set up a gravity filtration with a plastic funnel, folded wet filter paper, and an Erlenmeyer flask. Pour the content in the 250 ml beaker slowly through the filter paper. Wash the filter paper with deionized water. Dispose of the filtrate in the proper labeled waste container.
Chemical weathering is much more common in locations where there is a lot of water, because water is important to many of the chemical reactions that can take place. Club soda is a solution of water, acid and sodium bicarbonate and is one among different chemical substances that can be used to investigate the effect of chemical weathering in rocks.
This was the mechanical weathering lab that gives us the knowledge of how rocks break down. The sugarcubes represent the rock before and after the event of weathering. We used the sugarcubes because the they are a sedimentary rock, which means that they are very easy to break. What we thought was going to happen was that using gravity and a small container, putting the the cubes in the container and shaking it for three minutes would cause the sugarcubes to break down. The data does not make a perfect because every time you break down a rock you don’t always break off the same amount of rock for everyone.