chapter 3.4 & 24.1 nuclear chemistry radioactivityradioactivity

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CHAPTER 3.4 & 24.1 Nuclear Chemistry Radioactivity

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Page 1: CHAPTER 3.4 & 24.1 Nuclear Chemistry RadioactivityRadioactivity

CHAPTER 3.4 & 24.1

Nuclear Chemistry

Radioactivity

Page 2: CHAPTER 3.4 & 24.1 Nuclear Chemistry RadioactivityRadioactivity

Radiation

Radiation: The process of emitting energy in the form of waves or particles.

Where does radiation come from?Radiation is generally produced when particles interact or decay.

A large contribution of the radiationon earth is from the sun (solar) or from radioactive isotopes of the elements (terrestrial).

Radiation is going through you atthis very moment!

http://www.atral.com/U238.html

Page 3: CHAPTER 3.4 & 24.1 Nuclear Chemistry RadioactivityRadioactivity

Man-made radiation sources that people can be exposed to include tobacco, television, medical x-rays, smoke detectors, lantern mantles, nuclear medicine,

and building materials.

Adding it all up, the average American is exposed to a total of about 360 millirems a year from natural and man-made radiation.

Page 4: CHAPTER 3.4 & 24.1 Nuclear Chemistry RadioactivityRadioactivity

IsotopesWhat’s an isotope?

Two or more varieties of an element having the same number of protons but different number of neutrons. Certain isotopes are “unstable” and decay to lighter isotopes or elements.

Deuterium and tritium are isotopes of hydrogen. In addition to the 1 proton, they have 1 and 2 additional neutrons in the nucleus respectively*.

Another prime example is Uranium 238, or just 238U.

Page 5: CHAPTER 3.4 & 24.1 Nuclear Chemistry RadioactivityRadioactivity

Definitions

• Radioactivity– emission of high-energy radiation from the nucleus of an

atom

• Nuclide– nucleus of an isotope

Page 6: CHAPTER 3.4 & 24.1 Nuclear Chemistry RadioactivityRadioactivity

Nuclear Decay• Why nuclides decay…

– to obtain a stable ratio of neutrons to protons

K

K4019

3919

Stable

Unstable(radioactive)

Page 7: CHAPTER 3.4 & 24.1 Nuclear Chemistry RadioactivityRadioactivity
Page 8: CHAPTER 3.4 & 24.1 Nuclear Chemistry RadioactivityRadioactivity

He42

Types of Radiation

• Alpha ()– helium nucleus paper2+

Beta-minus () electron e0

-11- lead

Gamma () high-energy photon 0 concrete

Page 9: CHAPTER 3.4 & 24.1 Nuclear Chemistry RadioactivityRadioactivity

Where do these particles come from ?

These particles generally come from the nuclei of atomic isotopes which are not stable.

The decay chain of Uranium produces all three of these formsof radiation.

Let’s look at them in more detail…

Page 10: CHAPTER 3.4 & 24.1 Nuclear Chemistry RadioactivityRadioactivity

Alpha Particles (a)

Radium

R226

88 protons138 neutrons

Radon

Rn222

Note: This is theatomic weight, whichis the number ofprotons plus neutrons

86 protons136 neutrons

+ nnp

p

a (4He)

2 protons2 neutrons

The alpha-particle ( )a is a Helium nucleus.

It’s the same as the element Helium, with the electrons stripped off !

Page 11: CHAPTER 3.4 & 24.1 Nuclear Chemistry RadioactivityRadioactivity

Beta Particles (b)

CarbonC14

6 protons8 neutrons

NitrogenN14

7 protons7 neutrons

+ e-

electron(beta-particle)

We see that one of the neutrons from the C14 nucleus “converted” into a proton, and an electron was ejected. The remaining nucleus contains 7p and 7n, which is a nitrogen nucleus. In symbolic notation, the following process occurred:

n p + e ( + )n And a neutrino is produced too.

Page 12: CHAPTER 3.4 & 24.1 Nuclear Chemistry RadioactivityRadioactivity

Gamma particles (g)In much the same way that electrons in atoms can be in an excited state, so can a nucleus.

NeonNe20

10 protons10 neutrons

(in excited state)

10 protons10 neutrons

(lowest energy state)

+

gamma

NeonNe20

A gamma is a high energy light particle.

It is NOT visible by your naked eye because it is not in the visible part of the EM spectrum.

Page 13: CHAPTER 3.4 & 24.1 Nuclear Chemistry RadioactivityRadioactivity

Gamma Rays

NeonNe20 +

The gamma from nuclear decayis in the X-ray/ Gamma ray

part of the EM spectrum(very energetic!)

NeonNe20

Page 14: CHAPTER 3.4 & 24.1 Nuclear Chemistry RadioactivityRadioactivity

Nuclear Decay…the ones we care about

• Alpha Emission

He Th U 42

23490

23892

Beta Emission

e Xe I 0-1

13154

13153

TRANSMUTATION

Page 15: CHAPTER 3.4 & 24.1 Nuclear Chemistry RadioactivityRadioactivity

Half-life

• Half-life (t½)– time it takes for half of the nuclides in a sample to

decayNuclear Decay

0

2

4

6

8

10

12

14

16

18

20

0 2 4 6 8 10

# of Half-Lives

Ma

ss

of

Iso

top

es

(g

)

Example Half-lives

polonium-194 0.7 seconds

lead-212 10.6 hours

iodine-131 8.04 days

carbon-14 5,370 years

uranium-238 4.5 billion years

Page 16: CHAPTER 3.4 & 24.1 Nuclear Chemistry RadioactivityRadioactivity

Half-life Problem How much of a 20-g sample of sodium-24 would

remain after decaying for 30 hours? Sodium-24 has a half-life of 15 hours.

GIVEN:

total time = 30 hours

t1/2 = 15 hours

original mass = 20 g

WORK:

number of half-lives = 2

20 g ÷ 2 = 10 g (1 half-life)

10 g ÷ 2 = 5 g (2 half-lives)

5 g of 24Na would remain.

Page 17: CHAPTER 3.4 & 24.1 Nuclear Chemistry RadioactivityRadioactivity

F ission

• splitting a nucleus into two or more smaller nuclei

• some mass is converted to large amounts of energy

n3 Kr Ba U n 10

9236

14156

23592

10

Page 18: CHAPTER 3.4 & 24.1 Nuclear Chemistry RadioactivityRadioactivity

F ission

• chain reaction - self-feeding reaction

Page 19: CHAPTER 3.4 & 24.1 Nuclear Chemistry RadioactivityRadioactivity

Nuclear Weapons

Page 20: CHAPTER 3.4 & 24.1 Nuclear Chemistry RadioactivityRadioactivity

Nuclear Power

• Fission Reactors Cooling Tower

Page 21: CHAPTER 3.4 & 24.1 Nuclear Chemistry RadioactivityRadioactivity

Nuclear Power

• Fission Reactors

Page 22: CHAPTER 3.4 & 24.1 Nuclear Chemistry RadioactivityRadioactivity

Nuclear Power

• Chernobyl

Page 23: CHAPTER 3.4 & 24.1 Nuclear Chemistry RadioactivityRadioactivity

Nuclear power

• Three mile Island

Page 24: CHAPTER 3.4 & 24.1 Nuclear Chemistry RadioactivityRadioactivity

Fusion

• combining of two nuclei to form one nucleus of larger mass• produces even more

energy than fission• occurs naturally in

stars

Page 25: CHAPTER 3.4 & 24.1 Nuclear Chemistry RadioactivityRadioactivity

Nuclear Power

• Fusion Reactors (not yet sustainable)

Page 26: CHAPTER 3.4 & 24.1 Nuclear Chemistry RadioactivityRadioactivity

Nuclear Power

• Fusion Reactors (not yet sustainable)

Tokamak Fusion Test Reactor

Princeton University

National Spherical Torus Experiment

Page 27: CHAPTER 3.4 & 24.1 Nuclear Chemistry RadioactivityRadioactivity

Nuclear Power

• 235U is limited• danger of meltdown• toxic waste• thermal pollution

• Hydrogen is abundant• no danger of meltdown• no toxic waste• not yet sustainable

FISSION

FUSION

vs.

Page 28: CHAPTER 3.4 & 24.1 Nuclear Chemistry RadioactivityRadioactivity

Cold Fusion?

Page 29: CHAPTER 3.4 & 24.1 Nuclear Chemistry RadioactivityRadioactivity

OthersIrradiated FoodRadioactive DatingNuclear MedicineNuclear Weapons