Helen Scott Candidate Number: SL Chemistry internal Assessment Experiment to investigate the Chemical Composition of Minerals Objective In this experiment, you will react a variety of minerals with hydrochloric Acid to determine their chemical composition. Research Question How does a sample’s reaction with Hydrochloric acid depend on the the chemical composition of a mineral? Thesis If a mineral contains CO3 (is a carbonate) then it will react with HCl, forming CO2 gas. Materials Electric Balance Watch Glass 500 mL Beaker (±5 mL) 100 mL Graduated Cylinder (±5 mL) Gas Syringe 3 samples of Calcium Carbonate 3 samples of Dolomite 3 samples of Silicon Dioxide 6 M HCl Safety and Environmental Care 1 Avoid any skin contact with HCl Wear full coverage splash proof lab goggles to protect your eyes when working with acids Have adequate ventilation when working with hydrochloric acid\ Helen Scott Candidate Number: SL Chemistry internal Assessment Variables Independent: -Mineral used -Molarity of HCl Dependent: -Amount of CO2 released -Change in Mass Method 1. Make sure all lab materials have been well cleaned. 2. Weigh the sample of Calcium Carbonate on the electric balance. Record data in the table. 3. Measure 100 mL of HCl into a 300 mL beaker. 4. Place the Calcium Carbonate sample into the acid. 5. Quickly cover the beaker with the Gas syringe apparatus, measuring how much CO2 is released, record your findings in the data table. 5. Observe the reaction. Once it ends remove the mineral sample and once dry, weigh it again. Record data in the table. 6. Repeat the procedure twice using a new sample of Calcium Carbonate and then with Dolomite and Silicon Dioxide. Setting Up 2 Helen Scott Candidate Number: SL Chemistry internal Assessment Results Using the data collected from the mass of the acid, and the initial and final masses of the mineral sample, calculate the percent of sample lost to the reaction. Disposal Discard the mineral sample in the waste basket. Flush the acid down the sink with plenty of water. 3 Helen Scott Candidate Number: SL Chemistry internal Assessment Background Information Reaction with Acids is a property of minerals that can help identify carbonate minerals. Dilute hydrochloric acid will be used in this lab to react with a variety of minerals. The release of appreciable bubbles of carbon dioxide in a relatively short period of time indicate that the mineral being tested is a carbonate. A carbonate is a salt of carbonic acid, characterized by the presence of the carbonate ion, CO32. The mineral samples used are: Calcium Carbonate, CaCO3 (Limestone) Dolomite, (CaMg)(CO3)2 Silicon Dioxide, SiO2 (Quartz) The volume of gas formed can be calculated according to the equation: 𝛥𝑉 = 𝑉2 − 𝑉1 ΔV = Amount of gas formed V1=the initial value you started with V2=the amount left after the reaction 4 Helen Scott Candidate Number: SL Chemistry internal Assessment Raw Data Table 1.0 – Table to show raw data collected for all three food types Initial Mass Final Mass Initial Gas Final Gas (±0.01 g) (±0.01 g) Volume Volume (±0.05 mL) (±00.5 mL) Calcium Carbonate Trial 1 Trial 2 Trial 3 Dolomite Trial 1 Trial 2 Trial 3 Silicon Dioxide Trial 1 Trial 2 Trial 3 5 Helen Scott Candidate Number: Observations Calcium Carbonate Dolomite Silicon Dioxide 6 SL Chemistry internal Assessment Helen Scott Candidate Number: SL Chemistry internal Assessment Processed Data Table 2.0 – Table to show the amount of gas formed in each trial and the average change in mass for each type of mineral. Gas Formed Average Volume of Gas Formed (±0.05 mL) (±0.05 mL) Calcium Carbonate Trial 1 Trial 2 Trial 3 Dolomite Trial 1 Trial 2 Trial 3 Silicon Dioxide Trial 1 Trial 2 Trial 3 Figure 2.1 – Example calculation of the volume of gas formed in the first trial of Calcium Carbonate 𝛥𝑉 = 𝑉2 − 𝑉1 Uncertainty Calculation = The absolute uncertainties are added: = 7 Helen Scott Candidate Number: SL Chemistry internal Assessment Table 3.0- Table to show the change in mass in each trial and the average change in mass for each type of mineral. Change in Mass Average Change in Mass (±0.02 g) (±0.02 g) Calcium Carbonate Trial 1 Trial 2 Trial 3 Dolomite Trial 1 Trial 2 Trial 3 Silicon Dioxide Trial 1 Trial 2 Trial 3 Figure 3.1 – Example calculation of the change in mass of the first trial of Calcium Carbonate. ΔMass = Final Mass – Initial Mass = =- Uncertainty Calculation The absolute uncertainties are added: = = 8 Helen Scott Candidate Number: SL Chemistry internal Assessment Figure 3.2 – Example calculation of the average change in mass of Calcium Carbonate. MeanΔMass = ∑ 𝛥𝑀𝑎𝑠𝑠 Uncertainty Calculation 𝑛 When the average of a set of values is taken, the uncertainty remains the same: = = ±_ Table 4.0 – Table to show the correlation between volume of gas formed and change in mass Average Change in Mass Average Volume of Gas Formed Calcium Carbonate Dolomite Silicon DiOxide Figure 4.1- Graph to show the correlation between volume of gas formed and change in mass in the reaction with Calcium Carbonate 9 Helen Scott Candidate Number: SL Chemistry internal Assessment Figure 4.2 - Graph to show the correlation between volume of gas formed and change in mass in the reaction with Dolomite Figure 4.3 - Graph to show the correlation between volume of gas formed and change in mass in the reaction with Silicon Dioxide 10 Helen Scott Candidate Number: Conclusion 11 SL Chemistry internal Assessment Helen Scott Candidate Number: SL Chemistry internal Assessment Evaluation The effect of random errors would be reduced by the repetition of the trials for each mineral. Factor Gas lost to environment Effect on Experiment The measurement of gas formed can be inaccurate because of factors leading to the loss of gas to the environment. Human error, and an unsound piece of equipment could contribute to a slightly skewed result. Incomplete reaction between minerals and acid Since not the entire mineral is CO3 the rock would not completely dissolve, this would mean that it would be virtually impossible to accurately tell when all of the CO3 has been reacted with and dissolved. This would lead to an incomplete reaction and therefore slightly skewed results. Surface Area of Minerals The surface area of each sample was different and the Dolomite was powdered, this difference would contribute to results that were not wholly comparable based on the difference of surface area left to react, which would change the rate of reaction. 12 Improvement Helen Scott Candidate Number: Works Cited 13 SL Chemistry internal Assessment