(Get a) Half Life. Date Per. mathematical. But it can also be modeled for us to see with simple materials.

Similar documents
Scientific Inquiry. Standards B 1.2 & B 1.9

Lab [30 pts] Name A Simulation of Radioactive Decay

Phys 243 Lab 7: Radioactive Half-life

Experiment: Nuclear Chemistry 1

Radioactive Dice Decay

[2]

Activity Title: It s Either Very Hot or Very Cold Up There!

Fossils and Carbon Dating Created for SPICE by Rachel Naumann and Melissa Henkel May 2008 Lesson 1: Fossil Detectives

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

Plant Indicators for Acids and Bases

Substances and Mixtures:Separating a Mixture into Its Components

An 80 milligram sample of a radioactive isotope decays to 5 milligrams in 32 days. What is the half-life of this element?

38 Which statement explains the meaning of the half-life of a radioactive substance? 10 mm of aluminium

2.8-1 SCIENCE EXPERIMENTS ON FILE Revised Edition. Dew Formation

Radioactive Dating. April 15, 2014

Ionizing Radiation Awareness (Non-User)

Accuracy and Precision of Laboratory Glassware: Determining the Density of Water

Flame Tests: Identifying Metals

Half Life Practice Problems #3

COC Biotechnology Program

Exploring Habitats. Study Habitat Drawings to Identify Living Things & Nonliving Conditions. Safety Precautions

A Study of Radioactivity and Determination of Half-Life

USING COINS TO MODEL RADIOACTIVE DECAY

Lab 1: Precision and accuracy in glassware, and the determination of density

PART I: MEASURING MASS

(2) (1) Describe how beta radiation is produced by a radioactive isotope (1) (Total 4 marks)

Absolute Dating. Using half-lives to study past-lives. Notes #26

Notes: Part 1 - Nuclear Chemistry

Mahopac Central School District Curriculum Introduction to Science 8

Ch Radioactivity. Henry Becquerel, using U-238, discovered the radioactive nature of elements in 1896.

RADIATION SAFETY GUIDELINES FOR NON-USERS

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

The effects of sodium chloride on the Boiling Point of Dihydrogen Monoxide

Radioactivity. Introduction

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

LESSON 8: Power Pellets! Nuclear Energy in the United States

Floating Disks: An Investigation of Photosynthesis Student Materials. Introduction Lab Protocol Data Collection Worksheet...

Moles, Mass, and Volume

Rock of Ages, or Ages of Rocks

Station 1: measuring & graphing short lengths

EQ: How do we use the metric system in science?

Half Lives and Measuring Ages (read before coming to the Lab session)

Name: Period: Air Masses Notes 7 Minutes Page 2 Watch the air masses video. Make sure you follow along.

To measure ph s in a variety of solutions and mixtures and to account for the results obtained.

Atomic Structure and Radioactivity

Notepack 19. AIM: How can we tell the age of rocks? Do Now: Regents Question: Put the layers of rock in order from oldest to youngest.

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

#2: THE FLOATING PAPER CLIP

What type of radiation is emitted when a uranium-238 atom decays? From which part of a uranium-238 atom is the radiation emitted?

Newton s Second Law of Motion

6 Acid Base Titration

What happens during nuclear decay? During nuclear decay, atoms of one element can change into atoms of a different element altogether.

Measurement: Length, Area and Volume Part I

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

Chem 100 Section Experiment 12 Name Partner s Name. Radioactivity

Ch 22 Radioactivity Nuclear Chemistry

Name: Class: Date: SHORT ANSWER Answer the following questions in the space provided.

The detector and counter are used in an experiment to show that a radioactive source gives out alpha and beta radiation only.

Radioactive Half-life of Potassium-40

Chapter 10. Table of Contents. Section 1 What Is Radioactivity? Section 2 Nuclear Fission and Fusion. Section 3 Nuclear Radiation Today

Effective January 2008 All indicators in Standard / 11

Unit 4 Practice Exam. 1. Given the equation representing a nuclear reaction in which X represents a nuclide:

The Electromagnetic Spectrum. 7.1 Atomic Theory and Radioactive Decay. Isotopes. 19K, 19K, 19K Representing Isotopes

Working with Solutions. (and why that s not always ideal)

2) Estimate your annual radiation dose from background radiation.

Radiometric Dating (tap anywhere)

CHAPTER 1 RADIATION AND RADIOACTIVITY

GENERAL INSTRUCTIONS

Chapter: Inside the Atom. Section 2: The Nucleus

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

NUCLEAR SPECTROMETRY

Section 3. What Drives the Plates? What Do You See? Think About It. Investigate. Learning Outcomes

The Case of Melting Ice

Chapter 10. Section 10.1 What is Radioactivity?

Chemistry Lab: Introduction to Measurement

Chemical Reactions: Titrations

Key Question: What role did the study of radioactivity play in learning more about atoms?

Bay Area Scientists in Schools Presentation Plan

Chapter 28: Nuclear Chemistry Part 1: Notes The Basics of Nuclear Radiation and Nuclear Decay

Bellevue College CHEM& 121 Experiment: Stoichiometric Analysis of an Antacid 1

Read Hewitt Chapter 33

Chem 2115 Experiment #7. Volumetric Analysis & Consumer Chemistry Standardization of an unknown solution, analysis of vinegar & antacid tablets

Unit 1 Introduction to Chemistry & Data Analysis Chapters 1 2 of your book.

Norwood Science Center. Geology Grade 4

Matter and Its Changes

Chemical Energy Conversions. Vanderbilt Student Volunteers for Science VINSE/VSVS Rural

HHPS WHMIS. Rules MSDS Hazard Codes Systems. Biology based. Chemistry based. Safety Symbols. Safety in the Lab. Lab Equipment

Chapter 3 - Measurements

Can Tylenol Kill You?

Unit 3: Chemistry in Society Nuclear Chemistry Summary Notes

Nonrenewable Energy: Nuclear. Energy Part 2

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

10.1 RADIOACTIVE DECAY

Opening. Monster Guard. Grades 1-3. Teacher s Guide

Ocean Acidification in a Cup Materials

Titration with an Acid and a Base

My Fossil s Older Than Your Fossil

KEY 1 = PAN 2 = RIDERS 3 = BEAMS 4 = POINTER ~ Metric Measurement Scientist

The sources include Am-241 which emits alpha radiation, Sr-90 which emits beta radiation and Co-60 which emits gamma radiation.

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

Transcription:

Unit 5 (Get a) Half Life Name The theory of how half life break-down works is very Date Per. mathematical. But it can also be modeled for us to see with simple materials. As you do this lab, try to ask yourself, How is what I m doing like the decay of a radioactive nuclide? Part I: What is radioactive decay? Materials: Tap Water & Colored Water Calculator 500 ml Beakers 100 ml Graduated Cylinder Tape or labels to mark the beakers Graph Paper CAUTION: Please work neatly. Do not spill water. If you do, clean it up or tell the teacher. Water spills onto the floor or near electrical outlets can be a serious hazard. Procedure : 1. Obtain two large beakers for your lab group from your teacher. One will contain colored water, and the second just a little dry powder. 2. Label the beaker of water, Radionuclide. (Use neat, big letters.) Label the beaker with the dry powder, Decay Product. 3. Ask your teacher for the half life of your nuclide. Record it here: 4. Record the water volumes in your two beakers in the table below. (500 ml and 0 ml. Don t forget the units!) 5. Pour out exactly half of the colored water into your Decay Product beaker. What you just did represents one half life of your radionuclide. 6. Record the new volumes of your two beakers below. 7. Repeat this disintegration (Steps 5 & 6) 5 more times and record your data Number of Half Lives that have passed 0 1 Volume of Original Radionuclide Water Volume of Decay Product Water 400 ml 0 ml (Get a) Half Life Page 1 Sun, Apr 1, 2001

8, Graph your data. Choose appropriate intervals for the vertical and horizontal axes and be sure you label the appropriate units of measure. Discussion: A. How is this procedure like real radioactive decay? B. How is this procedure unlike real radioactive decay? (Give more than one answer if you can.) Part II: What happens if you use a radionuclide with too long a half life? Scientists use a number of different radionuclides to determine the ages of different rocks and fossils. (Rubidium-87, Uranium-238, Carbon-14, etc.) How can they decide which radionuclide is the best for each job? Procedure: 1. Obtain a second beaker of the same colored water. 2. Describe its color exactly, so if it change you will know. 3. Take out 10 ml of colored water and replace it with 10 ml of pure tap water. Did the color change? (It MUST have, because you took out some of the coloring and added fresh water.!) Can you SEE it s a different color? Why can t you see the color change? Part III: What happens if you use a radionuclide with too short a half life? Procedure: 1. You now need a third beaker with the same color of water. Describe it s color as exactly as you can. 2. Pour out half (200 ml) of the colored water into a sink or waste water receptacle. 3. Now add the same volume (200 ml) of fresh colorless water to bring the sample back up to 400 ml. 4. How did the color change? 5. Repeat the procedure, pouring out half of the new colored water and adding 200 ml of fresh water. Do this a total of 10 times. (Again, take care not to spill water.) 6. Can you still see the color? (Get a) Half Life Page 2 Sun, Apr 1, 2001

Would you be able to see the color if you did this 100 times? 7. What is the problem with using a real radionuclide with too short a half life? Wrap-Up: _ C. What happens to a radionuclide through time? D. What is a half life? E. Find a reference that lists several radionuclides. Name one radionuclide with a relatively short half life: What is it s half life? F. Name one radionuclide with a long half life: What is it s half life? G. The half life of Barium-137m is about 2.6 minutes. ( m means metastable; not really stable.) How long are three half lives of Barium-137m? If you started with 10 grams of Ba-137m, how much would be left after 2.6 minutes? If you started with 10 grams of Ba-137m, how much would be left after 5.2 minutes? How much of that 10 g would still be Ba-137m after 10.4 minutes? H. The half life of Rubidium-87 is 4.9 x 10 10 years. Would Rubidium-87 be a good substance to use to find the age of the campfires of early humans? Explain your answer. I. The half life of Carbon-14 is 5700 years. Would you use Carbon-14 to find the age of the first living things on Earth? What s the problem with using C-14 to measure this? (Get a) Half Life Page 3 Sun, Apr 1, 2001

Unit 5 Key to: (Get a) Half Life In Part I the amount of radionuclide will decrease, fast ar first, and then more slowly through time. The decay product will increase, fast ar first, and then more slowly through time. A. Like radioactive decay, half of the original substance is lost each X minutes. B. Unlike radioactive decay, we can see this water change. Also, this procedure is not expensive or as potentially dangerous. In Part II it will be impossible to see any change in color because the half life is too long. In Part III, representing a short half life, after a while, so little color is left that it s impossible to see. C. Through time, the original radionuclide decays, or becomes less and less. D. Half life is the amount of time it takes for half the radionuclide to decay, or change. E. (Answers will depend on the reference and the choice of which nuclides to use.) F.Students will probably chose Rb-87 (4.9 x 10 10 years) or U-238. (4.5 x 10 9 years) G. 2.6 minutes x 3 = 7.8 minutes. 5 grams. 1.25 grams. (Barium-137m is a real radionuclide that is often used in lab applications.) H. No. So little Rb-87 would have changed to Strontium-87 that we could not measure the decay product. Rubidium-87 has too long a half life. I. No. In such a long time, there would be too little Carbon-14 remaining to measure. Carbon-14 has too short a half life. (Get a) Half Life Page 4 Sun, Apr 1, 2001

Unit 5 (Get a) Half Life Tips Difficulty: Content: Easy to do. Not so easy to understand. Important Preparations: Have ready for each lab group three 500 ml beakers with 400 ml of colored water,and a second dry beaker with some drink mix powder that will become another color when it is wet. (Complimentary colors are suggested.) You may want to use a different sets of colors to represent different radionuclides and decay products. So all the students who get the same two colors (water and dry powder) have the same half life. If you do this, you can list the colors and half lives on the blackboard: Blue :30 (30 seconds) Yellow 1:00 (1 minute) Green 1:30 (One and a half minutes) (Times written :30 and 1:00 are listed as they are used in the earthquake epicenter labs in Unit 3.) Materials: As listed on the lab plus... Food Coloring Box (Small - About 3-5 colors) Colored drink powder such as colored Kool Aid (Several colors) (A different color than the food coloring) Pails for used water if students work away from sinks. Time: 30-40 minutes Suggestions for the Teacher: 1. Make half lives roughly a minute or two. 2. Use just one (1) drop of food coloring for each 400 ml sample of colored water. (continued) (Get a) Half Life Page 5 Sun, Apr 1, 2001

3. If you don t want the students working at sinks, provide some receptacle (a pail?) for each group. 4. Some sources call atoms like Carbon-14 and Uranium-138 radioisotopes. But isotopes differ only in the number of neutrons. These two substances differ in both neutrons and protons. Nuclide is a better term than isotope because we can correctly talk about different elements as different nuclides. They are not different isotopes because they differ in both neutrons and protons. I suggest NOT making a big point of this with young students. Half life is tough enough without needing to learn the definition of a nuclide. You have more important things to teach in this lab! 5. If you want to be able to detect and measure ionizing (dangerous) radiation, you may be able to obtain an old, yellow Geiger counter (free) from your Civil Defense unit in your county government. Tell them it s for use in a school. Be sure to get one that works Student Intro: 1. Please work neatly. Water spills can be messy and even dangerous. Some one could slip on a wet floor or even get a bad electrical shock. 2. This lab shows us how half life works. You can t show this with a real radioactive substance because of the cost of the equipment and, for strongly radioactive substances, great danger. 3. Although you can see, hear or feel radiation, even in dangerous amounts, it can be measured with instruments like a Geiger counter. (A-I) Post-Lab: It is suggested that you discuss these questions and answers. Extensions: The American Nuclear Society has people who train teachers about nuclear radiation and they may be able to give you a booklet of nuclear labs and demonstrations you (or a bright student) can do in your classroom. If you bring in real radioactive substances, be sure to clear it with your department head and/or administration. While they can be used safely, you will want to take care with nuclear issues and parent/community members. Don t make yourself vulnerable. Source: In memory of the Navajo Code Talkers and the Diné from Keyenta. (Get a) Half Life Page 6 Sun, Apr 1, 2001