Name ____________________________________________ Date ____________________ Blk___ NB#______ Nuclear Chemistry: Half-Lives and Radioactive Dating Scientists look at half-life decay rates of radioactive isotopes to estimate when a particular atom might decay. A useful application of half-lives is radioactive dating. This has to do with figuring out the age of ancient things. 1. Why is radioactive dating useful? __________________________________________________________________________________________ If you could watch a single atom of a radioactive isotope, U-238, for example, you wouldn’t be able to predict when that particular atom might decay. It might take a millisecond, or it might take a century. There’s simply no way to tell. But if you have a large enough sample, a pattern begins to emerge. It takes a certain amount of time for half the atoms in a sample to decay. It then takes the same amount of time for half the remaining radioactive atoms to decay, and the same amount of time for half of those remaining radioactive atoms to decay, and so on. This process is shown in the following table. 2. What two factors are necessary to determine the radioactive decay process? _______________________ _______________________ Half-Life Decay of a Radioactive Isotope Half-Life Percent of Radioactive The amount of time it takes for one-half of a sample to decay is called the half-life of the isotope. Isotope Remaining 3. What is the amount of time it takes to for a radioactive sample to decay called? 0 100.00 _________________________________________________ 1 50.00 2 25.00 3 12.50 4 6.25 5 3.12 6 1.56 7 0.78 8 0.39 9 0.19 10 0.09 It’s important to realize that the half-life decay of radioactive isotopes is not linear. For example, you can’t find the remaining amount of an isotope as 7.5 half-lives by finding the midpoint between 7 and 8 half-lives. This decay is an example of an exponential decay. 4. What term is used to describe the rate of decay for a radioactive isotope? __________________________________________________________________________________________ Safe handling of radioactive material Knowing about half-lives is important because it enables you to determine when a sample of radioactive material is safe to handle. The rule is that a sample is safe when its radioactivity has dropped below detection limits. And that occurs at 10 half-lives. So, if radioactive iodine-131 (which has a half-life of 8 days) is injected into the body to treat thyroid cancer, it’ll be “gone” in 10 half-lives, or 80 days. 5. Flourine-18 has a half-life of about 110 minutes. How many minutes would it be before it was considered “gone”? hours? Show Work!! __________________________________________________________________________________________ Radioactive dating Radioactive dating is helpful for figuring out the age of ancient things. Carbon-14 (C-14), a radioactive isotope of carbon, is produced in the upper atmosphere by cosmic radiation. The primary carbon-containing compound in the atmosphere is carbon dioxide, and a very small amount of carbon dioxide contains C-14. Plants absorb C-14 during photosynthesis, so C-14 is incorporated into the cellular structure of plants. Plants are then eaten by animals, making C-14 a part of the cellular structure of all living things. As long as an organism is alive, the amount of C-14 in its cellular structure remains constant. But when the organism dies, the amount of C-14 begins to decrease. Scientists know the half-life of C-14 (5,730 years), so they can figure out how long ago the organism died. Carbon-14 dating can only be used to determine the age of something that was once alive. It can’t be used to determine the age of a moon rock or a meteorite. For nonliving Substance substances, scientists use other isotopes, such as potassium-40. Half lives Remaining 0 703 6. The half-life of plutonium 100 351.5 n bone is about 100 years. If 200 175.75 a bone specimen has 703 300 87.875 grams of plutonium in it, 400 43.9375 how much will remain after 500 21.96875 700 years? 600 10.984375 ___________________ 700 5.4921875 7. Why would ALL radiometric graphs have the same basic shape? ________________________________________________ ________________________________________________ Parent Daughter Half Life (years) Dating Range (years) Minerals/materials 238U Uranium-238 206Pb Lead-206 4.5 billion 10 million 4.6 billion Minerals include zircon, uraninite. Igneous or metamorphic rocks. 40K Potassium-40 40Ar Argon-40 1.3 billion 0.05 million 4.6 billion Minerals include muscovite, biotite, Kfeldspar. Volcanic rocks. 87Rb Rubidium-87 87Sr Strontium-87 47 billion 10 million 4.6 billion Minerals include muscovite, biotite, Kfeldspar. Igneous or metamorphic rocks. 100 - 70,000 years Not used for dating rocks, except carbonates from earth's surface such as recent coral reefs. Used for young organic materials, or surface-water samples: Wood, charcoal, peat, bone, tissue, carbonate minerals from surficial environments, water containing dissolved carbon. 14C Carbon-14 14N Nitrogen-14 5,730 years 8. The above chart shows some of the materials that can be used for radiometric dating. What does is mean by “parent” material and “daughter” material? _____________________________________________________________ _____________________________________________________________ _____________________________________________________________ 9. In the figure to the right, what is the status of the Potassium-40? And the Argon-40? Potassium-40 is _______________________________________________ Argon-40 is ___________________________________________________ 10. How long does it take Potassium-40 to decay into Argon-40? ___________________________________________________________ 11. The half-life of Zn-71 is 2.4 minutes. If one had 100.0 g at the beginning, how many grams would be left after 7.2 minutes has elapsed? How to find Solution: 7.2 / 2.4 = 3 half-lives Find 3 half-lives on chart – 12.5 Convert percentage to decimal 12.5% = 0.125 100.0 g x 0.125 = 12.5 g remaining Number of Half Lives 0 1 2 3 4 5 6 Percentage of Parent Material 100 50 25 12.5 6.25 3.125 1.5625 Percentage of Daughter Material 0 50 75 87.5 93.75 96.875 98.4375 12. Os-182 has a half-life of 21.5 hours. If one had 200.0 g at the beginning, how many grams would be left after 86 hours has elapsed? 13. How long will it take for a 40.0 gram sample of I-131 (half-life = 8.040 days) to decay to 3.125% its original mass? 14. At time zero, there are 10.0 grams of W-187. If the half-life is 24 hours, how much will be present at the end of one day? Two days? Seven days? 15. 100.0 grams of an isotope with a half-life of 36.0 hours is present at time zero. How much time will have elapsed when 3.125 grams remains?