Radiometric Dating “clocks in rocks”. Absolute Dating Gives a numerical age Gives a numerical age Works best with igneous rocks & fossils Works best with.

Slides:



Advertisements
Similar presentations
Sci. 3-3 Absolute Dating: A measure of Time Pages
Advertisements

Mass of individual atoms Lesson 1 – introduction to project and atomic structure.
Absolute Dating of Rocks and Strata
1.Will not take any after next Tuesday 1/13 1.Define each of these terms: You may use your notes and they do not need to be in complete sentences  Energy.
Radioactive Decay.
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
Section 1: What is Radioactivity?
INTRODUCTION TO ABSOLUTE (RADIOMETRIC) DATING
Preview Key Ideas Bellringer Nuclear Radiation Nuclear Decay Math Skills Radioactive Decay Rates SECTION 1: WHAT IS RADIOACTIVITY?
Geologic History: Absolute Dating Unit 6 Absolute Age.
Unit 2 Lesson 3 Absolute Dating
What is it to be Radioactive? Radioactive decay is the process in which an unstable atomic nucleus loses energy by emitting radiation in the form of particles.
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.
Radioactive Decay. What do you know about Radioactivity? 1.All atoms are made up of __________. 2.What are some radioactive isotopes? 3.Why do some isotopes/atoms.
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.
List the order of events that took place: earthquake deposit D deposit B deposit G intrusive lava rocky deposit R river cuts through deposit E deposit.
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.
Review. What type of decay will happen if the nucleus contains too many neutrons? Beta Decay.
Atoms and Study of the Past I. What is an atom? An atom (element) is the basic unit of matter. The Periodic Table displays the 115 known atoms.
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.
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.
Radioactive Half-life
Chapter 8 Section 2 Handout
The fossil below is that of a Coelophysis and was found in upstate N.Y. Approximately how old is the rock?
Dating Rocks and Remains Radioactive Decay: Vocabulary Half-Life: The amount of time it takes for half of a radioactive isotope to decay. Radioactive.
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.
Absolute Dating. Absolute dating provides a numerical age for the material tested, while relative dating can only provide a sequence of age. Absolute.
Absolute Dating.
Chapter 7.2 – Half life Science 10. Types of decay Alpha Alpha.
Radioactive Decay.
Early Pioneers in Radioactivity Roentgen: Discoverer of X-rays 1895 Becquerel: Discoverer of Radioactivity 1896 The Curies: Discoverers of Radium and Polonium.
Radiometric Dating Chapter 18 Geology. Absolute Dating Gives a numerical age Works best with igneous rocks difficult with sedimentary rocks Uses isotopes.
Section 1: What is Radioactivity?
4/27/2017 Isotopes and Half Life
Thursday, October 15 th, 2015 The ABG's (or Alpha, Beta, Gamma) of Radioactivity.
Nuclear Decay. Radioactivity The emission of high-energy radiation or particles from the nucleus of a radioactive atom.
 What are the limitations of relative age dating?  What do you think Absolute age dating is?
Nuclear Decay You will be learning: 1.What is alpha, beta, and gamma radiation. 2.Know the half-life of a radioactive material. 3.How to describe the process.
The Rock Record Section 2 Section 2: Determining Absolute Age Preview Objectives Absolute Dating Methods Radiometric Dating Radioactive Decay and Half-Life.
Radioactive Decay. Types of Radioactive Decay Alpha Decay: nucleus eject an alpha particle (made of 2 protons and 2 neutrons – a helium nucleus)
CALCULATING HALF-LIFE Aim: How can we measure how much of a radioactive element decayed? DO NOW: If we start with 4.5 grams of Radon- 222 and over a period.
Do First Actions: Turn in yesterday’s worksheet 1. List the layers from youngest to oldest.
Absolute Dating: A Measure of Time January 27,2015.
Absolute Dating.
Nuclear Stability and Decay 1500 different nuclei are known. Only 264 are stable and do not decay. The stability of a nucleus depends on its neutron-to-
ABSOLUTE AGE DATING Absolute Age Dating is finding the numerical age of an object Artifacts (rocks or fossils) contain radioactive elements which are.
The ABG's (or Alpha, Beta, Gamma) of Radioactivity
Ch.3, Sec.3 – Absolute Dating: A Measure of Time
By stating that rock unit A is older than rock unit B, we are
I. Absolute Dating A. The process of establishing the age of an object (fossil or rock layer) by determining how long it existed.
An unstable nucleus releases energy to become more stable
Chemistry Do Now Directions: Take out your Do Now sheet and begin.  
AC Vocabulary Chapter 6 Section 3
Review: Types of decay 1. Alpha.
Absolute Dating.
Geologic Time and Earth History Part 2 – Absolute Age
Radioactivity.
Radiometric Dating “clocks in rocks”
Absolute Dating.
Absolute Dating.
Absolute Dating.
Absolute Age of Rocks Notes
Radioactive Decay.
Absolute Dating.
Presentation transcript:

Radiometric Dating “clocks in rocks”

Absolute Dating Gives a numerical age Gives a numerical age Works best with igneous rocks & fossils Works best with igneous rocks & fossils Uses isotopes Uses isotopes

Isotopes- different number of neutrons Carbon 14 ( 14 C) Carbon 14 ( 14 C) –2 “extra” neutrons –radioactive

Common dating isotopes ParentDaughter Half life Potassium 40 Argon by Rubidium 87 Strontium by Uranium 235 Lead by Carbon 14 Nitrogen 14 6,000 years Sodium 22 Aluminum hours

radioactivity Nuclei break apart Nuclei break apart Emit particles or waves (radiation) Emit particles or waves (radiation)

Ionizing Radiation Radiation Alpha Particle Neutron Particle Beta Particle Radioactive Atom Gamma Ray (X Ray)

Average Annual Dose Cosmic 28 mrem Terrestrial 28 mrem Internal 40 mrem Medical X-Rays 40 mrem Nuclear Medicine 14 mrem Consumer Products 10 mrem Other 3 mrem Radon 200 mrem Natural Sources Man-Made Sources

Comparison of Radiation Dose Doses shown in bar graph are in units of mrem

Half-Life New1 Half- Life 2 Half- Lives 3 Half- Lives 4 Half- Lives Activity The time required for the amount of radioactive material to decrease by one-half

Half-lives ParentDaughter Half life Potassium 40 Argon by Rubidium 87 Strontium by Uranium 235 Lead by Carbon 14 Nitrogen 14 6,000 years Sodium 22 Aluminum hours

Half life problem If you begin with 80 grams of 14 C after a time, 20 grams are left. How old is the sample? If you begin with 80 grams of 14 C after a time, 20 grams are left. How old is the sample?

14 Carbon Only accurate for ages less than 100,000 years Only accurate for ages less than 100,000 years Parent gets too small to accurately measure Parent gets too small to accurately measure

Mass spectrometer measures D/P ratio

Preparing a rock for mass spectrometer

Using daughter/parent ratio 1) D/P ratio 1) D/P ratio 2) figure out number of half-lives 2) figure out number of half-lives –Use graph 3) multiply number of half-lives by the time of one half-live 3) multiply number of half-lives by the time of one half-live Example: 240 g 14 N ; 8 g 14 C Example: 240 g 14 N ; 8 g 14 C

Another half-life problem 1,000 grams of radioactive element is in a rock when it is formed. The element’s half-life is 2 million years. After a time, 125 grams of the original element remain. How old is the rock? 1,000 grams of radioactive element is in a rock when it is formed. The element’s half-life is 2 million years. After a time, 125 grams of the original element remain. How old is the rock?