Lab 525 ONLINE LESSON If viewing this lesson in Powerpoint Use down or up arrows to navigate

Lab 525 ONLINE

LESSON

If viewing this lesson in Powerpoint

Use down or up arrows to navigate

Do take notes as we peruse through this

lesson…

Radiometric Dating

A question that is often asked…

How old is the earth?

And the answer is…

Pretty Old

Radiometric dating is the process of

measuring the age of rocks

By measuring the age of rocks, geologists can determine the age of a number of geologic events...

To include the age of the earth!!!

Radiometric dating is based on the concept of radioactivity…the disintegration (falling apart) of atoms

What is an atom?

An atom is the smallest particle in the universe

with a distinct set of chemical

characteristics…..

An atom is a structure…it is a package of particles

Everything in the universe is comprised of atoms…bicycles

Cellphones

Dumbasses

Everything

An atom is comprised of three basic components

ATOM

PPROTON (positively charged)

NNEUTRON (neutral)

e-ELECTRON (negatively charged)

e-

NUCLEUS

The electron orbits the nucleus which contains the protons and neutrons

RULE: The number of protons determines the chemical identity

of an element

For instance… -all Hydrogen contains 1 proton… -all Helium contains 2 protons… -all Uranium contains 92 protons…

Element = a substance that cannot be broken

down into other substances by chemical

means…

For instance… Hydrogen is an element Helium is an element Uranium is an element

CARBON

12C

Carbon-12 is a species of carbon…

CARBON

12C

It contains 6 protons and 6 neutrons…for a total of 12 particles in the nucleus

CARBON

14C

Carbon-14 is another species of carbon…

CARBON

14C

Carbon-14 contains 6 protons but 8 neutrons…for a total of 14 particles…

CARBON

14C

The neutron count may vary but the proton count remains the same…6 protons…

SO: The number of protons determines the chemical identity

of an element

Decay types are part of Radioactivity …

there are three types to be concerned

with…

DECAY TYPES

ALPHA

BETA

ELECTRON CAPTURE

e-

P P

P

P

N N

N

N

e-

DECAY TYPES

ALPHA P P

N N

2 protons and 2 neutrons are thrown out of the nucleus…this reduces the number of protons and thus changes the element…

DECAY TYPES

BETAe-

PN

A neutron turns into a proton

This will change the element

DECAY TYPES

ELECTRON CAPTURE

P N

e-

A proton turns into a neutron

This will change the element

With all 3 decay types…elements will

change their chemical identity because of the change in the

number of protons…

A common decay series is

238U/206Pb

URANIUM = PARENT

LEAD = DAUGHTER

A decay series is the progression of the disintegration of

elements…a start to finish process…

This beginning to end process is the essence of radiometric dating…

238U92

For instance… Uranium 238 is a parent element and it decays over time to to Lead 206…

238U92

The decay process starts out with 92 protons and 146 neutrons for a total of 238 particles in the nucleus…

238U92

And includes a series of steps before uranium turns into lead…

238U92

2 protons and 2 neutrons are ejected from the nucleus and changes the element… uranium to thorium

234Th90

A neutron is converted to a proton and changes thorium to paladium…

234Pa91

And so on and so on…

234U92

230Th90

226Ra88

222Rn86

218Po84

214Pb82

214Bi84

214Po84

210Pb82

210Po84

206Pb82

Through a series of steps…uranium is changed to lead…

So how does radiometric dating allow geologists to date rocks?

A rock is found in the field…an igneous rock…

It is formed as a result of melted material from the interior of the planet…

That eventually cooled…

The minerals inside the rock solidified with some radioactive material inside the crystals…

Radioactive elements started at 100% parent material (dark blue dots)…

Then over time…the parent material decayed to daughter material (light blue dots) one atom at a time…

Over time a reduction of parent material will occur as well as an increase of daughter material

Principally, this means that we can make a ratio between parent material and daughter material…

This ratio can be placed into an equation…

ln(n0/nt)(100000000)

T =0.0154

ln(n0/nt)(100000000)

T =

“nt” Original amount of parent material

“n0” Leftover amount of parent material (daughter amount subtracted from parent material)

0.0154

“T” Age of a rock

The bean counting exercise involves counting brown beans which represents parent material nt

The amount of parent material nt is determined by counting the total number of beans…brown and white…

The white beans represent daughter material… n0 is calculated by number of brown beans

ln(n0/nt)(100000000)

T =

Values are then placed into this

equation

0.0154

ln(n0/nt)(100000000)

T =

And the age of a rock can be calculated…

0.0154

ln(n0/nt)(100000000)

T =

This is referred to as absolute time…

0.0154

Absolute time is used in concert with a

Relative Time Scale…

Periods such as Cretaceous and Jurassic are relative time periods…

Meaning one period is older or younger than another period…

Cretaceous rocks are younger than Jurassic rocks…

Ordovician rocks are older than Triassic rocks…

A Relative Time scale is older at the bottom

And younger at the top…

The Relative Time scale was developed to show the relationship of sedimentary rocks…

Superimposed relative to each other…

The Relative Time scale was developed with no absolute time values…

However, with radiometric dating…real absolute time values can be assigned to each relative time period…

Geologic Time Scale…