Exploration: A Logarithmic Look at Half-Life and the Decay Rates The Geiger Applet is designed to help students understands the process of radioactive decay, specifically the determination and uses of its half-life and decay rate. Prerequisites: Students must be familiar with logarithms and natural logarithms to answer many of these questions Students should be able to work with graphs. Students should be comfortable with converting the mass of a substance to the number of atoms the substance contains. Learning Outcomes: By the end of this lesson, students should understand that radioactive decay's rate can be calculated from observing it slightly and that there are many applications for the decay rate and half-life. If you have not already done so, open up the Geiger Counter Applet. You will need it to answer some of the following questions. Finding the Decay Rate and Half Life From the list of isotopes, select Radon-222. Run the Geiger Counter. 1. a. In the graph as seen in the applet, what are the units of your dependent and independent variables? dependent units: independent units: b. What are the units of the area of your graph? If the x units are converted to days, what are the units of the area of your graph? c. How many counts have been detected by the Geiger counter after 11 days? 2. Consider three graphs: N (t ) N 0 2 t / h , C (t ) C0 2 t / h , D(t ) D0 2t / h and where t is time and h is the half life (equal for all 3 formulae), and where D0 N 0 g and C0 N0 f (f and g are constants). a. Prove these three graphs are all of the same format and that their slopes are all the same (hint: consider how D(t) and C(t) relate to N(t)). b. Suppose that, out of the total activity, the Geiger counter only recieves 5 percent. Rewrite your N(t) formula to be a graph for the total activity. c. Activity can be measured as the current number of counts multiplied by the decay constant (k). Use your formulae from (a) and (b) to write a decay formula for the total number of counts, and another formula for the number of counts that reach the Geiger counter. 3. Consider a graph of "Counts that Reach the Geiger Counter versus Time" where time is in years. a. Use the slope tool to find the slope of your graph at 11 days. What are the units of the slope? How would you convert this to counts/day? Counts/s? What does the slope tell you about the sample? b. When tracking how the counts decay over time, what does the decay constant represent? c. Use the converted slope from your Geiger graph to calculate the decay constant at 4 different points which seem to be the most consistent with an exponential curve. Find the average. Time (days) Counts Slope Converted Slope (counts/day) Average: Decay Constant 4. The equation used for this curve can be either N (t ) N 0 2t / h A as seen in the applet or N (t ) N 0 e kt A , which is more common, where h is the half life and k is the decay constant. a. Prove that the half-life can be calculated as h ln(2) k . b. Calculate the half life of Radon-222. Round your answer to the nearest hundredth of a day if necessary. c. Use the "Create a Curve Fit" to create the curve with your calculated half-life. Is it close to the Geiger counter data? d. Copy the data of the Geiger graph into Excel and graph it. Add an exponential trend line. What is the k value? What is the half-life value? Compare your values with Excel's. What are some possible sources of error? Summary: It is important to realize that, while the graph's y units are the same as those for activity, that does not mean that it is an activity-time graph. The activity is the total number of disintegrations the sample experiences over a period of time; the graph only shows the disintegrations which reach the Geiger counter during that period of time. While the values on this graph are proportional to an activity-time graph, they are not the same. The other important thing to realize is that proportional exponential graphs will have the same slope. Because of this, we can use the slope of the Geiger counter's graph as if it was a graph of Counts vs. Time or Activity vs. Time. Working with Half-Lives From the list of isotopes, choose 5 you wish to work with for the remainder of the lesson. 5. Using the method described above, calculate the decay constant and halflife of each isotope. Record them in the table below. Also, convert the mass to kilograms and record it for each isotope (1 u = 1.6604E-27kg). Isotope Mass (u) Mass (kg) Decay Constant Half-Life 6. Suppose that you have 50 grams of each isotope. a. How many atoms do you have? b. Which isotope has the most activity? Explain. c. After 20 years, which isotope has the greatest activity? What is its activity? 7. Using Excel, find the approximate half-lives of Astatine-210 and Protactinium-234. a. Suppose each isotope begins with 10,000 atoms. After 3 hours, which isotope has greater activity? Calculate the activities. b. Which has more atoms after 10 days? Which as more mass? After how long would the masses be equal? 8. Suppose you discover under your front step a 2 kg mass of Radium-223 (half life of 11.43 days). You decide to vacate your home until there is only 1 billionth of the Radium left, just to be safe. a. How long will you have to wait before coming back to your home? Give your answer to the nearest week. b. While you are away, you learn that the Radium had been under your door step for the past 9 months. How much of radium was there to begin with? Round your answer to the nearest kilogram. Summary: Scientists have used their knowledge of half-lives and radiation for many purposes. Through their knowledge of Carbon-14's half life, they have been able to date many ancient artifacts by comparing the level of Carbon-14 in the artifact to the level in a still-living object. The also have been able to use it to determine how long after a nuclear power station has been shut down or a nuclear test has been conducted it is safe to occupy the area. With half-lives they can find the current amount or past amount of an isotope or determine how long it has existed or will exist in significant amounts.