K cl o3decomp05
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This experiment studied the thermal decomposition of potassium chlorate (KClO3) in the absence of a catalyst. Three possible reactions were predicted to occur, producing either KCl, KClO2, or KClO. Oxygen gas produced was collected over water and its volume measured. The mass of the solid product was also measured and used to determine which reaction occurred. Analysis of the gas and solid products indicated that the decomposition reaction produced KClO2 in the absence of a catalyst, rather than KCl as occurs with a catalyst present.
K cl o3decomp05
- 1. The Decomposition of Potassium Chlorate Small quantities of molecular oxygen (O2) can be obtained from the thermal decomposition of certain oxides, peroxides, and salts of oxoacids. Some examples of these reactions are 2 Ag2O(s) 4 Ag(s) + O2(g) 2 BaO2(s) 2 BaO(s) + O2(g) MnO2 2 KClO3(s) 2 KCl(s) + 3 O2(g) The last reaction, the decomposition of potassium chlorate, includes manganese(IV) oxide (MnO2) as a catalyst. A catalyst is a substance that causes an increase in the rate of a chemical reaction without being used up in the reaction. It is this reaction that will be studied in this experiment. The thermal decomposition of KClO3 (potassium chlorate) in the absence of a catalyst will be studied. The identify of the solid that remains after the decomposition can be determined from the quantity of oxygen that is evolved. Identification can then be made by comparing the measured mass of the solid product with a calculated value based on the quantity of O2. The solid product that results from the thermal decomposition of KClO3 is KCl when the catalyst MnO2 is present. What will happen if the catalyst is not added? Will the loss of oxygen be less extensive? If so, the solid product could be either KClO2 (potassium chlorite) or KClO (potassium hypochlorite). This experiment will investigate these questions. The three reactions that could possibly occur can be written and balanced based on these predictions. A sample of KClO3 of known mass will be heated in the absence of a catalyst until the evolution of oxygen is complete. Oxygen will be collected in a flask by the displacement of water. The volume of water displaced equals the volume of O2 gas produced. In order to determine the correct stoichiometry of this reaction, you will need to obtain the number of moles of O2 that have been evolved. You can calculate this quantity from the rearranged form of the ideal gas law: RT PV n = where P refers to the partial pressure of oxygen in the collected gas mixture, V is the volume of water displaced, T is the Kelvin temperature of the gas mixture, and R is the constant. A commonly used value for R is 0.082056 L·atm/mol·K. If this value for R is used, then P must be expressed in atmospheres and V in liters. Since the oxygen is collected over water, water vapor will also be present in the gas. The experiment is designed so that the total pressure of the oxygen and water vapor will be equal to the atmospheric pressure:
- 2. OHOTotal 22 PPP += you can easily measure atmospheric pressure with a barometer. The partial pressure of oxygen in the flask can be calculated by subtracting the vapor pressure of water from the atmospheric pressure. Table I gives the vapor pressure of water at various temperatures. Figure I shows the apparatus for this experiment. The sample of KClO3 is placed in the test tube and the Erlenmeyer flask is filled with water. Some of the water is displaced by oxygen and is pushed into the beaker. The volume of water in the beaker will be identical to the volume of oxygen in the flask. Procedure 1. Record the atmospheric pressure from the laboratory barometer. This will equal the pressure of the (O2 + H2O) gas mixture that develops in your Erlenmeyer flask. 2. Caution: KClO3 is a very strong oxidizing agent. Make certain you place the lid back on the bottle containing the KClO3 after you obtain your sample. Do not let this substance contact paper or the rubber stopper in the test tube of the apparatus. 3. Record the weight of the beaker on a top-loading balance. Assemble the apparatus as shown in Figure I. 4. Fill the Erlenmeyer flask with distilled water, so that the level of the water is about 1 inch below the short glass tube. Open the pinch clamp. Remove the stopper from the test tube. Use a suction bulb to force air through the glass tube (test-tube end) until the rubber tube is filled with water. Allow a little water to enter the beaker to about 2 inches. Close the pinch clamp near the end of the tubing where the water will exit. 5. Make sure that the test tube is clean and dry. Take the test tube and a clean, empty, dry 400 mL beaker to the top-loading balances. Tare the empty beaker, add the test-tube and record its mass. Tare the beaker and test-tube. 6. Carefully add a small amount of KClO3 to the test tube. Continue to add KClO3 until you have about 1.0 g of KClO3 in the test tube. A sample in the range of 0.9 g to 1.1 g of KClO3 will work. Record the mass to 0.01 g. 7. Clamp the test-tube to the ringstand and stopper the test tube. 8. Open the pinch clamp. Lift the beaker with your hands until the water level in the beaker is equal to the water level in the Erlenmeyer flask. When the water levels are equal, have your partner close the pinch clamp. This equalizing process will ensure that the pressure acting on the water in the beaker (atmosphere) is equal to the pressure acting on the water in the flask.
- 3. 9. Empty the beaker but do not dry it. The volume of the water drops that remain in the beaker will be roughly equal to the volume that will remain after the displaced water is poured into a graduated cylinder for measurement. 10. Place the glass tube (connected to the hose) back into the beaker. MAKE CERTAIN THE PINCH CLAMP IS OPEN! Caution: If the clamp is not opened at this point, the build-up of gas during heating could cause an explosion, although it is more likely that a stopper would be forced to loosen. Also, make certain that the longer glass rod is not touching the bottom of the Erlenmeyer flask. This would also result in a closed system and an explosion could result. 11. Heat the test tube. The solid will melt, oxygen will be evolved, and water from the flask will be displaced into the beaker. Be cautious at first and brush the flame over the test tube. After a few minutes when the liquid solidifies, the test tube can be heated more strongly. One gram of KClO3 reactant should cause the displacement of between 250 and 300 mL of water. 12. Heat the solid thoroughly until no more gas is evolved. The contents of the test tube will solidify, since the melting point of the product is greater than that of KClO3. 13. Turn off the flame and allow the system to come back to room temperature. Allow five minutes for this process. 14. As in step 8, equalize the water levels (this may require lifting the Erlenmeyer flask) and close the clamp. 15. Remove the tube from the beaker. Record the mass of the beaker plus the water on a top- loading balance. Use Table I to determine the volume of water displaced. 16. Measure the temperature of the water to the nearest degree. Assume this is the temperature of the gas. Determine the appropriate vapor pressure of water from Table II. 17. Obtain the mass of the test-tube and its contents. Calculate and record the mass of the product. 18. If you have any reason to believe that your experiment did not work (e.g. you did not get ca. 300 mL of water transfer during the experiment), repeat steps 6-24 with a second sample of KClO3. If you believe that you were able to capture the complete volume of oxygen gas, a second trial is not necessary.
- 4. Figure I: A diagram of the laboratory setup used in this experiment. Table I Density (g/mL) of Water at Various Temperatures (o C) Temp. Density Temp. Density Temp. Density 17 0.9988 22 0.9978 27 0.9965 18 0.9986 23 0.9976 28 0.9962 19 0.9984 24 0.9973 29 0.9959 20 0.9982 25 0.9971 30 0.9956 21 0.9980 26 0.9968 31 0.9953 Table II Vapor Pressure of Water (torr) (data from the CRC Handbook of Chemistry and Physics, 49th edition, 1968.) Temp. Vapor Pressure Temp. Vapor Pressure Temp. Vapor Pressure 17 14.5 22 19.8 27 26.7 18 15.5 23 21.1 28 28.3 19 16.5 24 22.4 29 30.0 20 17.5 25 23.8 30 31.8 21 18.7 26 25.2 31 33.7
- 5. Questions 1. Write a balanced chemical equation for each of the three possible reactions that could occur when potassium chlorate, KClO3 is thermally decomposed. 2. Suppose the atmospheric pressure when you performed your experiment was 751 torr. The temperature of your water was found to be 23.0°C. What is the pressure of the oxygen gas, 2OP , that is produced? Data Treatment 1. Determine: a. moles of oxygen that were produced. b. moles KClO3 that were reacted. c. ratio of the number of moles of oxygen to the number of moles of KClO3. Write the chemical equation for the reaction that the data suggest occurred. 2. Using the mass of reactant KClO3 that you used in your most successful trial, calculate how many grams of each of the solid products of each possible reaction would theoretically be produced in the decomposition. Which decomposition reaction occurred, based on the mass of solid generated in the reaction? Write the chemical equation for the reaction that the data suggest occurred: 3. You determined which chemical reaction occurred by analyzing the amount of gas produced in the reaction, and the mass of solid product remaining after reaction. Which determination method do you believe is more reliable, the analysis of the mass of the solid product or the analysis of the gas produced? Explain your answer. 4. In the presence of a catalyst, KCl is produced in the thermal decomposition of KClO3. You did not use a catalyst. Did you get the same products for this reaction as you would have with a catalyst?