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.

Slides:



Advertisements
Similar presentations
Absolute Dating Radioactive Dating. Radioactivity Almost all of the elements contain radioactive isotopes Isotopes are atoms of the same element with.
Advertisements

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.
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:
By: HULK And Bruce Banner
Detecting Radiation A Geiger counter is the most familiar tool for detecting radiation. A Geiger counter is the most familiar tool for detecting radiation.
HALF-LIFE Chapter 7.2 – BC Science 10.
 Hand in any work needed.  Get out a small piece of paper, PUT YOUR NAME ON IT.  When bell rings the quiz will start and you will have 1 minute per.
Half-Life and Radioisotope Dating
Radioactive Decay Radioactive elements are unstable. They decay, change, into different elements over time. Here are some facts to remember: The half-life.
Radioactive Decay Now, let’s see how we can use the half-life rate to
Absolute Dating of Rocks and Strata
Radioactivity Lab Prompt
Absolute Dating : A Measure of Time
Absolute Dating Chapter 7 Lesson 2.
Nuclear Chemistry Ch 18, Pg 666, # 1-8
Half-Life Nuclear Chemistry. What is Half-Life? The time it takes for half of a given amount of a radioactive isotope to undergo decay.
Absolute Dating Notes and Practice. Directions: Use the following presentation to complete the notes sheet.
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.
Detecting Radiation  A Geiger counter is the most familiar tool for detecting radiation.  The probe of this device contains argon gas. When radiation.
Chapter 4.1. Half-Life Original Sample One half-life Two half-lives Three half-lives Contains a certain One-half of the One-fourth of One-eight of the.
Copyright © 2014 All rights reserved, Government of Newfoundland and Labrador Earth Systems 3209 Unit: 2 Historical Geology Reference: Chapters 6, 8; Appendix.
CARBON DATING Determining the actual age of fossils.
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.
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.
Section 2: Determining Absolute Age
RADIOCARBON DATING Students will: understand the half-life of an isotope.
ABSOLUTE AGE Absolute Dating Radiometric Dating Half Life Isotope Radioactive decay Carbon 14.
Relative Dating and Fossils Relative dating Relative dating Law of Superposition Law of Superposition Index Fossils Index Fossils What are fossils? What.
Warm-up 1. How do scientists use ‘relative dating?’ 2. Which layer is the oldest? 3. Which layer is the youngest? 4. Which layers are older than the fault.
Chapter 8 Section 2 Handout
Detecting Radiation  A Geiger counter is the most familiar tool for detecting radiation.  The probe of this device contains argon gas. When radiation.
The fossil below is that of a Coelophysis and was found in upstate N.Y. Approximately how old is the rock?
Radioactive Dating Chapter 7 Section 3.
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.
The half-life of a radioactive isotope explains the amount of time that it takes half of the isotope in a sample to decay.
Table of Contents Titles: Age and Time Page #: 13 Date: 9/12/12.
Chapter 7.2 – Half life Science 10. Types of decay Alpha Alpha.
Half Life Calculation of Radioactive Decay Atomic Physics.
Warm-up How do scientists use ‘relative dating?’
4/27/2017 Isotopes and Half Life
Half life and its uses No of coins Start Throw 1 Throw 2 Throw 3 Throw 4 Throw 5 Throw 6 Throw 7 We are going to start with 2 coins each and throw them.
 What are the limitations of relative age dating?  What do you think Absolute age dating is?
How Do We Know the Age of the Earth? February 26 th, 2015.
Absolute Age Finding a rock’s birthday. Absolute Age? Give an example of an absolute age of a rock layer… That rock layer is 200 million years old. Remember,
The Rock Record Section 2 Section 2: Determining Absolute Age Preview Objectives Absolute Dating Methods Radiometric Dating Radioactive Decay and Half-Life.
Do First Actions: Turn in yesterday’s worksheet 1. List the layers from youngest to oldest.
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 Dating.
ABSOLUTE AGE DATING Absolute Age Dating is finding the numerical age of an object Artifacts (rocks or fossils) contain radioactive elements which are.
Science 7: Unit E: Planet Earth Topic 9 – Geologic Time.
By stating that rock unit A is older than rock unit B, we are
Radio-dating.
Absolute Dating.
Geologic Time and Earth History Part 2 – Absolute Age
Measuring the speed of radioactive decay
Absolute Dating.
NOTES: GEOLOGIC DATING
Half-Life Half-life is the time required for half of a sample of a radioactive substance to disintegrate by radioactive decay. Atoms with shorter half-lives.
NOTES: GEOLOGIC DATING
Measuring the speed of radioactive decay
Radio-dating.
Evolution – Radiometric Dating Evidence
7.2 Half-Life.
Presentation transcript:

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 by measuring the number of radioactive C-14 isotopes.

How it works  Radiation on this planet causes radioactive isotopes to form.  A known percentage of the carbon dioxide in the air contains the radioactive C-14 isotope.  This carbon dioxide is used to “build” all living things (plants use it for food, animals eat the plants etc.)

Finding an age  The amount of C-14 in an object can be measured.  This amount is compared to the amount assumed to be there when it died.  You count the half lives to determine its age.

Disputing Carbon Dating  Some people have stated the amount of radiation hitting the planet (causing the known percentage of C-14) has changed over time.  This would cause serious errors in these calculations.

Radiodating  Radiodating always require you to determine the amount of radioactive isotopes present in the past and compare it to what is present today.  C-14 works because the amount of C- 14 in living things hasn’t changed over time.  Other types today compare the amount of daughter isotope present to the amount of radioactive isotope to determine how old it is.

Potassium-40 dating  Rocks (never living) can also be dated if they have other certain isotopes.  K-40 decays into Ar-40.  When a rock is formed we can assume all gases would escape, so all argon in a rock should be the product of K-40 decay.  measure the K-40 and compare it to the Ar-40 and you can determine its age.

Uranium-238 dating  U-238 decays into Pb-206 which is extremely rare.  If you have a rock with U-238 and Pb- 206 present, you can assume the Pb- 206 came from the decay of U-238.  Scientists have come up with the 4.5 billion year age of the planet using these methods.

For example  If you measure 15 g of C-14 and you assume you started with 60 g, then the object is…  11,430 years old  60g30g15g (2 half lives)  5715 years x 2 = 11,430 years

Math  The equation is difficult to use, so instead we will read it off a graph.  Here is equation m f /m i = 1/ 2 hl  Percentage left is current mass/initial mass x100 % = m f /m i x 100  Multiply the number of half lives by the value of one half life to get an age.

Problems  If you have 32% of a material left, how many half lives have passed?  1.64 half lives  If you have 17% of Ra-223 left, how old is it?  2.55 half lives x 11 days =  28 days

Problems  If original sample had 78 g of K-40, and you now have 73 g left; how old is the sample?  93.5% left .095 half lives x 1.28x10 9 yrs  1.2 x10 8 years  A sample of Radon-222 is 9.4 days old. There are.27 g present, how much was originally present?  1.5 g

Problems  If you have 67 g of Tc-96, and you assume you started with 88 g, how old is the object?  If you have an 8.0 day old sample of Radon-222 and there are 25 g present, how much was there to start?