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Learning Experience 3


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Exercise on radiometric dating. The objective of the activity is to use both the head and tail sides of pennies to simulate the decay of a radioactive element. We will use our data to try and describe radioactive decay using a mathematical formula.  This learning experience emphasizes mathematical techniques in science.

Time Frame - About 1 hour

Materials

  • Worksheet (provided), a pencil and 16 pennies.

Advance Preparation/Background

Remind participants/students that when we write “2 to the 3rd power,” the number 2 is called the base and the number 3 is called the exponent. When a number is written with an exponent it is said to be in exponential form. For example, we may write the number 8 in exponential form as a power of 2.

23

base = 2

exponent = 3

23 = 2 x 2 x 2 =8

Procedure

For this exercise we will start with each of the 16 pennies heads up. Therefore, we will call our radioactive element “heads.” This element, “heads” will decay to the element called “tails.” The decay rate will be constant. Specifically, every 100 years one-half of the “heads” present will decay to “tails.” We refer to this amount of time for one-half of the original material present to decay as the half-life. The half-life of “heads” is 100 years.

You will now complete several half-life simulations using the 16 pennies. Starting with all 16 pennies in a heads-up position, turn pennies over to tails to indicate decay of the element. Enter your observational data in the chart below as you go. You will make 4 entries on each of 4 half-life intervals.

Start with the first line at the passage of 100 years, i.e., the total time passed = 100 years. Enter the total time passed, number of half-lives, number of heads and number of tails at this interval of the simulation.

The second line of data should be at 2 half-lives. Again enter all 4 observations as you did for the first line. The third line of data should be at 300 years and the fourth line should be at 400 years. Complete the chart in similar fashion as outlined in the instructions above.

Total time passed Number of half-lives Number of heads Number of tails
       
       
       
       
       
       
       
       

 

Extension of data to a mathematical formula

Now complete this second chart using data from the first chart and your knowledge of fractions and exponents.  For example, the first line would be after 1 half-life, there is 1/2 of heads remaining and the denominator of the fraction is 2. Remember, when you write the fraction of heads remaining using exponent form, you will be writing a fraction and expressing the denominator in exponential form as a power of 2.

Number of half-lives Fraction of heads remaining Denominator of this fraction Denominator expressed as a power of 2 Exponent used Fraction of heads remaining using exponent form
           
           
           
           
           
           
           
           

 

At the start of the exercise, the presenter/teacher will ask the following questions?

  • Can we write a mathematical formula for the fraction of original radioactive material left after a certain amount of time (a certain number of half-lives)? We may find it convenient to use exponential form in this exercise. In the first two columns below transfer your data from the previous table starting with the 1st half-life.
  • What relationship do you see between the normal number of half-lives which have passed and the normal exponent used to express the fraction of heads remaining using exponential form?
  • If I asked you what fraction of an element would be left after 5 half-lives could you come up with the answer using the information you have gathered above?  What would the answer be?
  • The following equation represents the fraction of original radioactive element remaining in an object. What does the letter “x” stand for in this equation (think about your answer to number 1 above)?

Formative Assessment - B

Purpose: To demonstrate how using the half-lives of isotopes can use radiometric dating to find the age of a rock.

The decay of radioactive isotopes is like a clock ticking away, keeping track of the time that has passed since the rock has formed.  As time passes, the concentration of parent material in a rock decreases as the concentration of daughter product increases. A geologist can calculate the absolute age of the rock in a process called radiometric dating by measuring the amount of parent and daughter materials in a rock and by knowing the half-life of the parent material.

Carbon-14 is a parent material, which decays to its daughter material, nitrogen-14. The half-life of an isotope is the time it takes for half of the atoms in the isotope to decay.   The half-life of carbon-14 is 5730 years; therefore, it will take 5730 years for half of the carbon-14 atoms to decay to nitrogen-14.   Only half of the atoms of carbon-14 remaining after the first 5430 years will decay during the second 5730 years.  Therefore, after two half-lives, one-fourth of the original carbon-14 atoms still remains.  Half of these carbon-14 atoms will decay during the next 5730 years; therefore after three half-lives, one-eighth of the original carbon-14 atoms still remains.

Carbon-14 is useful for dating fossils up to 50,000 years old.  Organisms take in carbon from the environment to build tissues.  When the organism dies, some of the carbon-14 decays and escapes as nitrogen-14 gas.  By measuring the amount of carbon-14 remaining, the age of the fossil can be determined.

Follow the steps listed below to illustrate the radioactive decay of carbon-14; then answer the questions:

  1. Cut a strip of paper 8 cm long and 2 cm wide.  This strip of paper represents all of the carbon-14 in an organism when it died.
  2. Cut the strip of paper in half.
  3. Discard one half of the paper which represents the decayed parent material.  Record this cut by placing an X in the chart below under 1 (for the first cut).
  4. Continue by cutting the second half of the paper in half.  Record the cut with an X in the chart below under the 2 (for the second cut).
  5. Continue cutting the paper until it is so small that you can’t make another cut.  Record each cut in the chart below.
Cuts 1 2 3 4 5 6 7 8 9 10 11
X                      
Answer: X X X X X X X X X X?  
Q.
How many times were you able to cut the paper in half until it was so small that it was practically impossible to cut it again?
A.
Most participants will be able to make nine or ten cuts.
Q.
Each cut represents the half-life of carbon-14.  What length of time is represented by each cut?
A.
5730 years
Q.
Multiply the number of cuts by the half-life of carbon-14. What is the total amount of time represented by the cuts?
A.
time in years = number of cuts X 5790
Q.
Could you use the half-life of carbon-14 to determine when a dinosaur died?  Explain your answer.
A.
No, dinosaurs died more than 65 million years ago so no carbon-14 would remain in the fossil.
ISOTOPE HALF-LIFE
Plutonium-238 86 years
Americium-241 433 years
Curium-242 163 days
Berkelium-249 314 days
Californium 360 days
Einsteinium-253 20 days
Nobelium-259 1-˝ hours
Lawrencium-260 180 seconds
Element 103-262 40 seconds
Q.
If you had a 100-gram sample of plutonium, how much would remain after 43 years?
 
A.
75 grams
Q.
If you had a 5-gram sample of Lawrencium, how much would still remain after 30 minutes?
A.
none
Q.
If you had a 100-gram sample of Einsteinium, how much would remain after 40 days?
A.
25 grams
Q.
A rock sample contains 7.5 grams of Californium-249 and 52.5 grams of the product into which the Californium has changed.  How old is this rock?
A.
1080 days

Extensions

  1. A tutorial on the 40Ar/39Ar Step-Heating dating technique (http://caldera.wr.usgs.gov/40Ar.html)
  2. Radioactive Isotopes - the “Clocks in Rocks” (http://vcourseware3.calstatela.edu/GeoLabs/index.html)
  3. Geologic Time Scale Analogy (http://jrscience.wcp.muohio.edu/lab/GeoTime.html)


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