RADIOACTIVITY MATERIALS: PURPOSE: LEARNING OBJECTIVES: DISCUSSION:

Similar documents
EXPERIMENT FOUR - RADIOACTIVITY This experiment has been largely adapted from an experiment from the United States Naval Academy, Annapolis MD

A Study of Radioactivity and Determination of Half-Life

Radioactivity APPARATUS INTRODUCTION PROCEDURE

David A. Katz Department of Chemistry Pima Community College, 2202 W. Anklam Rd. Tucson, AZ 85709, USA

Lab 14. RADIOACTIVITY

NUCLEAR SPECTROMETRY

Lab NUC. Determination of Half-Life with a Geiger-Müller Counter

Radioactivity INTRODUCTION. Natural Radiation in the Background. Radioactive Decay

MASS ATTENUATION COEFFICIENT OF LEAD

Physics 1000 Half Life Lab

PHYSICS 176 UNIVERSITY PHYSICS LAB II. Experiment 13. Radioactivity, Radiation and Isotopes

Physics 248, Spring 2009 Lab 6: Radiation and its Interaction with Matter

Jazan University College of Science Physics Department. Lab Manual. Nuclear Physics (2) 462 Phys. 8 th Level. Academic Year: 1439/1440

Chem 100 Section Experiment 12 Name Partner s Name. Radioactivity

EXPERIMENT 11: NUCLEAR RADIATION

Introduction. Information on the Use of Radio Isotopes in the Physics Lab. Physics 1CL RADIOACTIVITY Winter 2010

PHYS 3650L - Modern Physics Laboratory

4 α or 4 2 He. Radioactivity. Exercise 9 Page 1. Illinois Central College CHEMISTRY 132 Laboratory Section:

Radioactivity. Introduction

What is Radiation? Historical Background

NUCLEAR SCALERS PURDUE UNIVERSITY INSTRUMENT VAN PROJECT HALF-LIFE OF A RADIOISOTOPE

Overview: In this experiment we will study the decay of a radioactive nucleus, Cesium. Figure 1: The Decay Modes of Cesium 137

Overview: In this experiment we study the decay of a radioactive nucleus, Cesium 137. Figure 1: The Decay Modes of Cesium 137

Absorption of Gamma Rays

Aluminum Half-Life Experiment

Radioactivity 1. How: We randomize and spill a large set of dice, remove those showing certain numbers, then repeat.

Name Date Class NUCLEAR RADIATION. alpha particle beta particle gamma ray

EQUIPMENT Beta spectrometer, vacuum pump, Cs-137 source, Geiger-Muller (G-M) tube, scalar

Name Date Class NUCLEAR CHEMISTRY. Standard Curriculum Core content Extension topics

CHEMISTRY 170. Radioisotopes

Ph 3504 Radioactive Decay

UNIT 18 RADIOACTIVITY. Objectives. to be able to use knowledge of electric and magnetic fields to explore the nature of radiation

Physics 23 Fall 1989 Lab 5 - The Interaction of Gamma Rays with Matter

Experiment: Nuclear Chemistry 1

I. Pre-Lab Introduction

Lab 12. Radioactivity

Chem 1A Chapter 5 and 21 Practice Test Grosser ( )

Radiation and Radioactivity. PHYS 0219 Radiation and Radioactivity

Unit 13: Nuclear Practice Packet Regents Chemistry: Practice Packet: Unit 13 Nuclear Chemistry

LABORATORY VIII NUCLEAR PHENOMENA

Chapter 21

CHEMISTRY 130 General Chemistry I. Radioisotopes

Strand J. Atomic Structure. Unit 2. Radioactivity. Text

INSTRUCTOR RESOURCES

Activity 11 Solutions: Ionizing Radiation II

RADIOACTIVITY IN THE AIR

PHYSICS A2 UNIT 2 SECTION 1: RADIOACTIVITY & NUCLEAR ENERGY

2) Estimate your annual radiation dose from background radiation.

11 Gamma Ray Energy and Absorption

Modern Physics Laboratory Beta Spectroscopy Experiment

Read Hewitt Chapter 33

Unit 3: Chemistry in Society Nuclear Chemistry Summary Notes

22.S902 IAP 2015 (DIY Geiger Counters), Lab 1

Science Teacher Workshop Meter Exercises - Greg's Answers. Hands on demonstration with Geiger Counters and experiments for the classroom.

Figure 1. Time in days. Use information from Figure 1 to calculate the half-life of the radioactive isotope.

Radioactivity. (b) Fig shows two samples of the same radioactive substance. The substance emits β-particles. Fig. 12.1

LAB 13 - RADIOACTIVITY, BETA, AND GAMMA RAYS

Name Date Class NUCLEAR CHEMISTRY

(a) (i) State the proton number and the nucleon number of X.

UNIQUE SCIENCE ACADEMY

Radioactive Half-life of Potassium-40

Absorption and Backscattering ofβrays

5 Atomic Physics. 1 of the isotope remains. 1 minute, 4. Atomic Physics. 1. Radioactivity 2. The nuclear atom

atomic number and mass number. Go over nuclear symbols, such as He-4 and He. Discuss

Radioactive Decay. Scientists have discovered that when atoms of one kind of element emit radiation, they can change into atoms of a NEW element.

Particle Physics. Question Paper 1. Save My Exams! The Home of Revision. International A Level. Exam Board Particle & Nuclear Physics

Atomic Notation (or Nuclear Symbol): Shorthand for keeping track of protons and neutrons in the nucleus

Safety: Do not eat the radioactive candium until it has decayed into a safer element.

Phys 243 Lab 7: Radioactive Half-life

Absorption and Backscattering of β-rays

Chapter 33: The Atomic Nucleus and Radioactivity Review questions pg. 658

Radioactivity Outcomes. Radioactivity Outcomes. Radiation

P7 Radioactivity. Student Book answers. P7.1 Atoms and radiation. Question Answer Marks Guidance

Problem statement, Standards, Data and Technology

THE COMPTON EFFECT Last Revised: January 5, 2007

UNIT 13: NUCLEAR CHEMISTRY

SCINTILLATION DETECTORS & GAMMA SPECTROSCOPY: AN INTRODUCTION

Chemistry 19 Prep Test - Nuclear Processes

Chapter 30 Nuclear Physics and Radioactivity

RADIOACTIVITY, BETA, AND GAMMA RAYS

Lifetime Measurement

hν' Φ e - Gamma spectroscopy - Prelab questions 1. What characteristics distinguish x-rays from gamma rays? Is either more intrinsically dangerous?

the properties of that element

IGCSE Physics 0625 notes: unit 5 Atomic Physics: Revised on 01 December

Determining the Efficiency of a Geiger Müller Tube

L 36 Modern Physics [3] The atom and the nucleus. Structure of the nucleus. The structure of the nucleus SYMBOL FOR A NUCLEUS FOR A CHEMICAL X

Computer 3. Lifetime Measurement

Radioactivity III: Measurement of Half Life.

Chapter 37. Nuclear Chemistry. Copyright (c) 2011 by Michael A. Janusa, PhD. All rights reserved.

Radioactive Dice Decay

Nuclear fission is used in nuclear power stations to generate electricity. Nuclear fusion happens naturally in stars.

Atomic Structure and Radioactivity

ABSORPTION OF BETA AND GAMMA RADIATION

2) Explain why the U-238 disintegration series shown in the graph ends with the nuclide Pb-206.

BETA-RAY SPECTROMETER

Shielding Alpha, Beta, and Gamma Radiation 11/08 Integrated Science 3

25.1. Nuclear Radiation

Chemistry Review Unit 1 Study Guide

Nuclear Reactions Homework Unit 13 - Topic 4

In order to get the G.C.S.E. grade you are capable of, you must make your own revision notes using your Physics notebook.

Transcription:

RADIOACTIVITY This laboratory experiment was largely adapted from an experiment from the United States Naval Academy Chemistry Department MATERIALS: (total amounts per lab) small bottle of KCl; isogenerator kit; eluting solution; cobalt-60 source; strontium-90 source; 1 Geiger counter; 2 Daedalon counters with probes; 2 white Geiger probe/absorber holders; 1 thin Al foil (#5); 2 Al plates; 2 Pb sheets; 4 Petri dishes; disposable gloves (for instructor) PURPOSE: To determine the half-life of potassium-40 and barium-137m, and to determine the relative penetrating abilities of gamma radiation and beta particles. LEARNING OBJECTIVES: By the end of this experiment, the student should be able to demonstrate the following proficiencies: 1. Show that radioactive decay is a first-order kinetic process. 2. Demonstrate the random nature of nuclear disintegrations. 3. Illustrate the fact that radioactivity is a natural phenomenon. 4. Show how to determine the half-life of a radioisotope with a very long half-life. 5. Show how to determine the half-life of a radioisotope with a short half-life. 6. Examine the shielding of radiation by different types of materials. DISCUSSION: Radioactivity is the spontaneous disintegration of unstable atomic nuclei with accompanying emission of radiation. It is known to be a random process at the atomic level, but the bulk (statistical) behavior of a sample of radioactive material is readily seen to obey first-order kinetics. The first-order differential rate law for radioactive species has the same form as the equation applied to chemical kinetic processes, but it is usually expressed in terms of the number of radioactive nuclei, N, rather than the concentration: where dn/dt is the change in the number of radioactive nuclei with respect to time, t, and k is the rate constant. As is characteristic of first-order decay processes, the rate constant is related to the half-life, t 1/2, by the equation The half-life is the time required for half of a substance to disappear. For a first-order decay process, it is independent of the initial number of particles decaying. The basic equipment used to measure radioactivity is the Geiger counter. It actually measures the rate, usually in units of counts per minute (cpm). Each "count" is the response of the detector to a single particle (typically particles, particles and rays) penetrates the detector tube and causes a discharge of a current pulse across the radius of the tube. Thus, each count represents one

radioactive nucleus undergoing decay. The counting rate detected by the instrument is called the Activity, A, which is directly proportional to the number of radioactive nuclei: A = kn (3) The integrated form of the radioactive decay rate law is also the same as that for first-order chemical kinetics: where N o is the initial number of radioactive nuclei. Since the activity is proportional to the number of radioactive nuclei, these equations are sometimes also written in terms of the activity, A = A o e kt. In linear form (y = mx + b), the equation becomes ln A = k t + ln Ao (5) where A 0 is the initial activity. Thus, a plot of ln A vs. t yields a straight line with a slope that is equal to k. The half-life, t 1/2, is obtained using Equation 2. The half-life is most accurately determined from a plot of ln(activity) vs. time. A. Half-Life of a Short-Lived Radioisotope Cesium-137 is a radioactive isotope with a half-life of 30.2 years. It undergoes decay to produce barium-137m, an unstable nuclear "isomer" that further decays to the stable barium-137 nucleus by emission: The half-life of 137m Ba is only 2.55 minutes. Because of their different chemical behavior, Cs and Ba can be readily separated and the half-life of the short-lived barium isotope can be followed directly. An isogenerator (an ion-exchange column) is used in this exercise to generate 137 Ba. It is loaded with 137 Cs, which continually decays to produce the Ba isotope. If a sample of an eluting solution is passed through the column, it will remove only the barium. The eluted solution can then be measured for activity with a Geiger counter at several points over a short (10-15 minutes) time span. A plot of ln(activity) vs. time yields a straight line, thus demonstrating first-order kinetic behavior. (See Equation 5.) (5)

B. Absorption of Radiation The absorption of radiation depends on the type of radiation (α, β, or γ), the energy of the radiation, and the nature of the absorber. Only β particles and γ rays will be considered in this exercise because the window on the Geiger tube is too thick to allow α particles to enter the tube. In general, γ rays interact with matter in an all-or-nothing way, just like other kinds of photons (e.g., red light). The more matter available per unit area, the greater the attenuation of the beam. The absorbed rays disappear and are exchanged for one or two particles (electrons or positrons). β particles, on the other hand, are not absorbed by matter but instead are "scattered". As they bounce through the material, they lose their energy a little at a time until they finally come to rest. Because we are using radiation with a very small range in energy, the results for both β and absorption will appear similar, but they would not be if a wider range of energy were available. C. Effects of Distance on Absorption of Radiation Generally,,, and radiation falls off as all electromagnetic radiation, as 1/(distance) 2 or the inverse squared law. This law merely states that the intensity of the radiation emitted from the sun varies with the squared distance from the source. As a result of this law, if the intensity of radiation at a given distance is one unit, at twice the distance the intensity will become only one-quarter. At three times the distance, the intensity will become only one-ninth of its original intensity at a distance of one unit, and so on. We will measure this effect with two radiation sources: and and see if this law is obeyed. PROCEDURE: Your lab section will be divided into 4 groups and will perform Parts A D in a round-robin fashion. Do not proceed to another part of the experiment until told to do so by your instructor. Do not touch any radioactive sample or piece of equipment until told to do so by your instructor. You will have approximately 20 minutes to complete each part, so you will need to be prepared for each lab portion. Part A. Half-Life of a Short-Lived Radioisotope 1. Do not touch the radioactive sample. Your instructor will prepare it and set it up for you. 2. Familiarize yourself with the Geiger counter. You will likely have to change scale during the course of this exercise. You will probably begin with the X100 scale and change to the X10 scale after the readings fall below 300 (on the X100 scale). 3. NOTE: Your sample will be placed under the Geiger tube by your TA. 4. Record the activity (in cpm) of the sample in 30 second intervals over a period of 10 minutes, and then for an additional 5 minutes at 1 minute intervals. Take your first reading as time zero (t = 0). REMEMBER TO RECORD BOTH THE METER READING AND THE SCALE to obtain the activity value. (Because the readings are not steady, you will probably have to do some averaging by eye. One easy way to even out the readings is to have two members of the group take readings, two serve as recorders, and one serve as the timer. At the end of the 15 minute period, all measurements at a given time can be averaged.)

5. Your instructor will discard the radioactive sample. Do not touch it. Part B. Absorption of Radiation 1. Place the orange cobalt-60 -source in the depression at the bottom of the white plastic Geiger tube stand. (Always place the source with the printed side facing the tube.) 2. Measure and record the activity of the (Co-60 source + background) without absorbers as follows. Switch the counter to ON and set the Rate/Continuous switch to CONTINUOUS. The counter will start clicking and the display will show the number of counts. Press and hold down the RESET button; the count will stop. Switch the Rate/Continuous switch to RATE. Release the RESET button. The counter will begin counting for one minute (but the display will not change). After one minute, the counter will update the display with the total counts in that time interval. 3. Locate the thin Al foil that is packaged in a cardboard slide mount. (THESE FOILS ARE QUITE FRAGILE; DO NOT TOUCH THE FOIL ITSELF, BUT HANDLE ONLY BY THE CARDBOARD MOUNT!) Place it in the slot closest to the Geiger tube. Set the Rate/Continuous switch to CONTINUOUS. The counter will start clicking and the display will show the number of counts. Press and hold down the RESET button; the count will stop. Switch the Rate/Continuous switch to RATE. Release the RESET button. The counter will begin counting for one minute (but the display will not change). After one minute, the counter will update the display with the total counts in that time interval. Record the activity measured with the thin Al foil absorber. 4. Remove the Al foil and replace it with one thick Al plate. Repeat the measurement and record the activity with the thick Al plate absorber. 5. Remove the Al plate and replace it with a thick lead sheet. DO NOT BEND THE Pb SHEET! Repeat the measurement. Add a second Pb sheet (in another slot) and repeat the measurement. 6. Remove all absorbers and replace the orange cobalt-60 -source with the green strontium-90 β-source. 7. Repeat steps 2 through 5, recording the original source activity, and the activities with the various absorbers as before. 8. Remove all absorbers. Move the sources at least two feet away from the Geiger tube. Repeat the measurement once to obtain a background count. Part C. Effect of Distance on Amount of Radiation Absorbed Effect of Distance on Amount of Radiation Absorbed 1. The measurements for the β - source will be measured at the following distances: 2.80, 2.45, 2.11, 1.84, 1.59, 1.34, and 1.08 inches. Please record these distances in your notebook. 2. Place the green strontium-90 β - source in the depression at the bottom of the white plastic Geiger tube stand. (Always place the source with the printed side facing away from the tube.) 3. Measure and record the activity of the green strontium-90 β - source without absorbers as follows. Switch the counter to ON and set the Rate/Continuous switch to CONTINUOUS. The counter will start clicking and the display will show the number of counts. Press and hold down the RESET button; the count will stop. Switch the Rate/Continuous switch to RATE. Release the RESET button. The counter will begin counting for one minute (but the display will not change). After one minute, the counter will update the display with the total counts in that time interval.

4. Using a thick Aluminum plate, place the Sr-90 source on the spot where the tape is located and move the plate into bottom slot on the stage and collect two single minute measurement. 5. Move the plate/sample to the next level and take 2 single minute measurements. Continue moving the plate closer to the probe for a total of 14 measurements. Part D. Radon Decay Pathway Using the computers in the lab, your team will need to search the internet and carefully outline the radioactive decay process for the decay of radon gas. Please note for each decay step, 1) the type of decay ( or ), 2) the name and mass of the new isotope formed, and 3) the halflife of the new isotope. Individually, answer the following questions: 1) What is the primary danger(s) associated with radon gas? 2) What is the organ system most often affected by radon? 3) Where would radon gas tend to accumulate in a house? 4) Why do radon gas levels tend to be higher in Missouri than in Florida? 5) What is the approximate total time (years) for the total radon 222 lead 206 decay?

DATA SECTION Part A. Half-Life of a Short-Lived Radioisotope Time (minutes) Activity (cpm) Time (minutes) Activity (cpm) Part B. Absorption of Radiation Cobalt-60 Gamma Source Strontium-90 Beta Source Absorber Activity (cpm) Absorber Activity (cpm) None None Al foil Al foil 2x Al foil 2x Al foil Al plate Al plate 2x Al plate Al plate 1 Pb sheet 1 Pb sheet 2x Pb sheets 2x Pb sheets Background cpm Part C. Effect of Distance on Amount of Radiation Absorbed Strontium-90 Beta Source Absorber Activity (cpm) 1. 2.80 2. 2.45 3. 2.11 4. 1.84 5. 1.59 6. 1.34 7. 1.09 Background cpm

DATA ANALYSIS - Part A. Half-Life of a Short-Lived Radioisotope 1. Create a spreadsheet that contains the following columns: time (min) activity (cpm) ln Activity Input your time and activity data, and use a formula to compute ln Activity. Make two graphs: (1) Plot Activity vs. time. (2) Plot ln Activity vs. time and perform a linear regression. Your plot should be properly labeled, and the linear regression equation and R 2 should be shown on the graph. Slope of line: y-intercept of line: R 2 : Submit your spreadsheet and the two graphs with your lab report. 2. From your linear regression equation, calculate the half-life of 137 Ba in units of minutes. t 1/2 of 137 Ba: min 3. The accepted half-life of 137 Ba is 2.55 min. Calculate the percent error of your measurement. percent error: 4. On your Activity vs. time plot, draw a smooth line through the data, then indicate, on the plot, the first 3 half-lives of 137m Ba. List the times of these successive half-lives: first half-life: min second half-life: min third half-life: min average half-life: min 5. The half-lives should be constant (all take the same amount of time), another feature characteristic only of first-order kinetic behavior. How does your average half-life, determined here, compare to that obtained from the first-order rate law (item 2)? percent difference:

Part B. Absorption of Radiation Perform the following calculations and write the results in the table below, or in a similar Excel spreadsheet. 1. A simple way to quantify the absorbers is with their "area density", which is the mass absorber per unit area. The area densities for the various absorber components are: thin Al foil: 21.5 mg/cm 2, thick Al plate: 40.9 mg/cm 2, single Pb sheet: 188.3 mg/cm 2, Calculate the total area density employed for each of the absorption measurements obtained. This is done by multiplying the appropriate value above by the number of plates/sheets used. 2. Determine values of the Corrected Activity by subtracting the Background from the Measured Activity. 3. The Corrected Activity for the Co-60 gamma source or Sr-90 beta source without absorbers represents 100% penetration. Calculate the percent penetration for each of the other Corrected Activities. Part C. Effect of Distance on Amount of Radiation Absorbed 1. Construct a graph using Excel to determine the effect of distance on absorption of radiation the Strontium-90 source. Don t forget to correct for background radiation.

Prelab QUESTIONS 1. Write balanced nuclear equations describing the decay of potassium-40 by the three primary modes of decay: decay, decay, and positron capture. Are the product nuclei stable? 2. In determining the half-life of barium-137m, it was not necessary to subtract out the background. Why not? 3. You used a strontium-90 source in Part C of this experiment. Write the balanced equation showing this decay. 4. In many instances in these experiments, you might have tried to make identical Measurements but obtained different values of the Activity. How can that be? (HINT- it is probably NOT operator error!)