HALF-LIFE Chapter 7.2 – BC Science 10.

Slides:



Advertisements
Similar presentations
Radioactive Isotopes and Half Life
Advertisements

Absolute Dating Radioactive Dating. Radioactivity Almost all of the elements contain radioactive isotopes Isotopes are atoms of the same element with.
8.3 Radioactive Dating.
Radiometric Dating Timothy G. Standish, Ph. D..
LOJ Feb 2004 Radioactivity 6 Half Life LOJ Feb 2004 Half Life The half-life of a radioactive substance: is the time it takes for the number of parent.
ABSOLUTE AGE IS EXPRESSED IN SPECIFIC UNITS, SUCH AS YEARS BEFORE PRESENT. ONE METHOD OF ABSOLUTE DATING IS COUNTING THE ANNUAL LAYERS OF GLACIAL LAKE.
7.2 Half-life.
UNIT 3 Geologic Time and Fossils
ABSOLUTE AGE Absolute dating- used to determine the age of a rock or fossil more exactly based on the properties of atoms An atom:
Methods of Dating Absolute and Relative.
Radioactive dating.
It can be difficult to determine the ages of objects by sight alone. e.g. It can be difficult to tell which students in a classroom are oldest. Radioactivity.
Radioactive dating.
By: HULK And Bruce Banner
ABSOLUT DATING Explanations collected from three online presentations.
Sci. 3-3 Absolute Dating: A measure of Time Pages
Detecting Radiation A Geiger counter is the most familiar tool for detecting radiation. A Geiger counter is the most familiar tool for detecting radiation.
Absolute Dating Chapter 3, Sec.3. Process to find the approximate age of rocks or fossils.
Absolute Dating.
Mass of individual atoms Lesson 1 – introduction to project and atomic structure.
Absolute Dating of Rocks and Strata
Radioactivity Lab Prompt
Relative and Absolute Dating Hill Science 6. Relative Dating Fossils can be dated relative to one another by noting their positions in strata. Fossils.
Absolute Dating : A Measure of Time
1 Radioactivity and Half-Life. 2 Radioactivity An unstable atomic nucleus emits a form of radiation (alpha, beta, or gamma) to become stable. In other.
7.2 Half-Life the time it takes for half of a radioactive sample to decay is a constant rate (always the same half life for each element) Example: Strontium-90.
7.2 Half-life.
Radioisotopes, and their use in “dating” rocks. Radioactive Decay Certain isotopes of some elements are not stable. They naturally change (decay) over.
(c) McGraw Hill Ryerson Half-life It can be difficult to determine the ages of objects by sight alone.  Radioactivity provides a method to determine.
History of Life: Origins of Life Chapter Age of Earth The earth is about 4.5 billion years old How did we measure that? Radiometric Dating = calculating.
(c) McGraw Hill Ryerson Half-life It can be difficult to determine the ages of objects by sight alone.  Radioactivity provides a method to determine.
Absolute Dating Throughout the centuries mankind has striven to try to determine the exact age of Earth. What these people were seeking was a numerical.
Carbon dating  Dates of very old materials are determined using carbon-14 or C- 14 dating.  It can only be used on things once alive.  This is done.
Tips on Dating. Why Date? Different methods of dating will help determine the actual age of a layer of rock or a fossil Scientists look at how much radioactive.
RADIOCARBON DATING Students will: understand the half-life of an isotope.
ABSOLUTE AGE Absolute Dating Radiometric Dating Half Life Isotope Radioactive decay Carbon 14.
A Fossil.  Any method of measuring the age of an event or object in years.
Carbon Dating The age of a formerly living thing can be determined by carbon dating As soon as a living organism dies, it stops taking in new carbon.
Chapter 7.2 – Half life Science 10. Types of decay Alpha Alpha.
Radiometric Dating Chapter 18 Geology. Absolute Dating Gives a numerical age Works best with igneous rocks difficult with sedimentary rocks Uses isotopes.
Warm-up How do scientists use ‘relative dating?’
4/27/2017 Isotopes and Half Life
Radioactive Dating. Amount of Parent Isotope Present Amount of Daughter Isotope Present Decay.
 Half-life – the time it takes for ½ of a radioactive sample to decay  Half-life for a radioactive element is a constant rate of decay  Half-life differs.
7.2: Using Radioactivity to Determine Age. How old is it? How do scientists guess how old things are? How do scientists guess how old things are? One.
ABSOLUTE AGE DATING Absolute Age Dating is finding the numerical age of an object Artifacts (rocks or fossils) contain radioactive elements which are.
The shorter the half-life, the faster the decay rate.
Ch.3, Sec.3 – Absolute Dating: A Measure of Time
By stating that rock unit A is older than rock unit B, we are
Measuring the speed of radioactive decay
It can be difficult to determine the ages of objects by sight alone.
7.2 Half-life.
Chemistry Do Now Directions: Take out your Do Now sheet and begin.  
AC Vocabulary Chapter 6 Section 3
Review: Types of decay 1. Alpha.
Radioactivity provides a method to determine the age of a material
Unit 1: Radio Activity Lesson 2: Half-Life
7.2 Half Life Half Life: the constant rate at which radioactive isotopes naturally decay. This rate refers to the time it takes for half of the nuclei.
Absolute Dating.
Rate of Radioactive Decay
7.2 What is Half Life? Half Life is the time required for half of the radioactive sample to decay. (c) McGraw Hill Ryerson 2007.
Measuring the speed of radioactive decay
Absolute Dating.
Absolute Dating.
Absolute Dating.
Absolute Age of Rocks Notes
Measuring the speed of radioactive decay
Rate of Radioactive Decay
Absolute Dating.
7.2 Half-Life.
Presentation transcript:

HALF-LIFE Chapter 7.2 – BC Science 10

Half - life The time required for half ½ the nuclei in a sample of a radioactive isotope to decay The half life for any radioactive isotope is a constant for any radioactive isotope. Each radioisotope decays at a unique rate

Time = 0 100% sample (8 pennies) are still radioactive

Time = 1 half life 50% of sample (4 pennies) are still radioactive

Time = 2 half lives 25% of sample (2 pennies) are still radioactive

Time = 3 half lives 12.5% of sample (1 penny) still radioactive

Time = 4 half lives No more pennies are radioactive. Think about a sample with millions of atoms…

7.2 Half-life It can be difficult to determine the ages of objects by sight alone. Radioactivity provides a method to determine age. Measure the relative quantities of remaining radioactive material stable products formed. See pages 302 - 304 (c) McGraw Hill Ryerson 2007

7.2 Half-life Carbon dating measures the ratio of carbon-12 and carbon-14. Stable carbon-12 and radioactive carbon-14 exist naturally in a constant ratio. When an organism dies, carbon-14 stops being created and slowly decays. Carbon dating only works for organisms less than 50 000 years old. . See pages 302 - 304 (c) McGraw Hill Ryerson 2007

Carbon Dating – carbon-14 Living things replace the carbon-12 and carbon-14 in their bodies when they are alive. However when living things die, they do not replace the carbon-14 as carbon-14 decays into nitrogen-14 Carbon-14 takes 5715 years to decay half of its nuclei into nitrogen- 14 Carbon-12 remains unchanged. Therefore something that has been alive within the past 50000 years contains enough nuclei of remaining carbon-14 to measure. The ratio of carbon-12 and carbon-14 can estimate the age of the sample

Carbon Dating

Carbon dating This picture shows a skeleton and a model for C-14 decay. The arrows represent the amount of C-14 giving off it's radiation as time passes. Notice the amount goes down by half for every half life.

Decay Curve All decay curves for any radioactive element look the same except for the length of the half life.

The Rate of Radioactive Decay Half-life measures the rate of radioactive decay. Half-life = time required for half of the radioactive sample to decay. Strontium-90 has a half-life of 29 years. If you have 10 g of strontium-90 today, there will be 5.0 g remaining in 29 years. See pages 305 - 306 (c) McGraw Hill Ryerson 2007

The Rate of Radioactive Decay Decay curves show the rate of decay for radioactive elements. The curve shows the relationship between half- life and percentage of the original substance remaining. The Rate of Radioactive Decay The decay curve for strontium-90

Common Isotope Pairs Parent isotope = the original, radioactive material Daughter isotope = the stable product of the radioactive decay The rate of decay remains constant, but some elements require one step to decay while others decay over many steps before reaching a stable daughter isotope. See page 307 (c) McGraw Hill Ryerson 2007

Common Isotope Pairs There are many radioisotopes that can be used for dating. Carbon-14 decays into nitrogen-14 in one step. Uranium-235 decays into lead-207 in 15 steps. Thorium-235 decays into lead-208 in 10 steps. See page 307 (c) McGraw Hill Ryerson 2007

The Potassium-40 Clock Radioisotopes with very long half-lives can help determine the age of very old things. The potassium-40/argon-40 clock has a half-life of 1.3 billion years. Argon-40 produced by the decay of potassium-40 becomes trapped in rock. Ratio of potassium-40 : argon-40 shows age of rock. See pages 307 - 308

The Potassium-40 Clock See pages 307 - 308

K-40 Clock

Half-Life Practice Problems

If there are 50 grams of U-238 on day zero of radioactive decay, how much will there be after 4.5 billion years (1 Half Life)? A) 0.0 grams B) 10 grams C) 25 grams D) 50 grams

Solution to problem #1

Based on the graph, 2 half-lives equals A) 4.5 billion years. B) 9 billion years. C) 12.5 billion years. D) 18 billion years.

Solution to problem #1

Use the chart to determine the half-life of Carbon-14. A) 5,000 years B) 5700 years C) 10,000 years D) 11,400 years

Practice Problems 1. How long will it take 200 grams of Plutonium 239 (half life 24,400 years) to decay to 25 grams?

Practice Problems 1. How long will it take 200 grams of Plutonium 239 (half life 24,400 years) to decay to 25 grams?

Practice Problems 2. How many grams of iodine 131 (half life 8 days) would be left after 24 days if you start with 25 grams?

Practice Problems 1. How many grams of iodine 131 (half life 8 days) would be left after 24 days if you start with 25 grams?

Summary A half-life is the length of time required for half the nuclei in a sample of a radioactive isotope to decay into its products.

Earth Day Activities List activities here

Getting the Word Out about Earth Day List ideas here

Earth Day Resources List resources here