Chapter 4. and parts of Chapters 15, and 17

Radioactive materials and radiation     pgs. Ch 4     80-85
Radon: what it is and your home     pgs. Ch 17     476-480
Fission reactors and Nuclear Waste     pgs. Ch 15     443-450

  Continued and Related Issues

  Geological and Natural Processes and Connections


Continuation and Augmentation

Outline

Nuclear Processes
General Radioactive Decay
  Fission - used today and developed this century.
  Fusion - experimented with today and used in the future?
  Natural radioactive decay
  Natural products and origins

Two Focus Case Studies of related environmental problems chosen for this example

Radon
  Natural Fission of Uranium
  Geology and Radon's origin
  How we have only recently made it significant in our lives.
  1984 - the wake-up call

Nuclear Waste
  How we use Geology as the primary environmental barrier to isolation of nuclear waste

  WIPP (Waste Isolation Pilot Plant - Carlsbad NM)
    What it is
    How it works
    How it was built
    What geology it depends on
    Personal experience

Nuclear Change

Nuclear change is the third type of change
1. physical,
2. chemical,
3. nuclear

Three types of nuclear events:

  1. Natural radioactive decay
  2. Nuclear fission
  3. Nuclear fusion

In nuclear reactions, the total matter + energy is conserved.

Some nuclear matter is converted into energy and this is what we use as we react nuclear fuel.


"In a nuclear change, the total amount of matter and energy involved remains the same."


Natural Radioactivity

Uranium

Example of an environmental complex situation caused by radioactive decay

Radon (Rn) is one of the natural decay products of Uranium and Rn 222 has a half-life of 3.4 days (Rn 240, 54.5 sec. half-life)

Radon

  (alpha -particle)


Isotopes of hydrogen and uranium


Various particles emitted in radioactive processes

Three (common or primary) particles or energies emitted in nuclear reactions

    electromagnetic radiation very short l, high energy


    Helium nucleus (2 protons, 2 neutrons)


    conversion of neutron to proton in nucleus


Other particles or energies emitted in nuclear reactions

Positron

positive electron from the nucleus with p to n result -1 atomic #, same atomic weight


Electron Capture

inner orbital electron captured by nucleus p to n, same atomic weight, -1 atomic #.


Neutron decay

nucleus ejects a neutron atomic weight -1, atomic # same.


Table of examples of each type of decay. Figure (4-1) energy of radiation or particle


Examples:

How do you get an electron from the nucleus when there are no electrons in the nucleus (Beta particle)?

Note: Nuclear events transform sub-atomic particles and elements but the sum of the matter and energy remains constant.

Neutron is converted to a proton within the nucleus and an electron is emitted.


Positron is analogous to a positive electron.

A positron emission can be viewed as a result of a conversion of a proton to a neutron in the nucleus.


Penetration power and ionizing radiation


What is the energy of gamma ray frequency?



Compared to 200-500 J/mol for a covalent bond what kind of energy is this?


So What?

Is this ionizing radiation?

Like what other radiation?

What do all ionizing radiation's have in common?

Reference: Recall the bond energy of some molecules.

Molecule Bond Bond Energy in kJ/mol
Methane H-CH3 438.4 ± 1
CH3-C6H5 317.1 ± 6.3
CH3-CH2CCH3 308.4 ± 6.3
Ethyl alcohol H-OC2H5 436.0 ± 4.2
F-CF2Cl 490.0 ± 25


Naturally occurring radioactive elements

U-238, U-235, Th-232, C-14, K-40 others . . .

Uranium is highly concentrated in Seawater

U-238, 99.275% abundance with a 4.51 x 109 y half life (alpha and gamma decay)

U-235, 0.7% abundance with a 7.0 x 108 y half life (alpha and gamma decay)

Examples: Seawater

Thorium there is no stable isotopic form

Th-232 100% abundance with a 1.41 x1010 y half life (alpha and gamma decay)

Example: Thorium is used in lantern mantels

Biologically active K-40, C-14, Others

K-40 0.0117% abundance with a 1.28 x 109 y half life (beta and gamma decay)
If you are alive you have some in you

Example:
Essential for nerves in all mammals

Carbon -12 98.9% abundant stable
Carbon -13 1.1% abundant stable
Carbon -14 trace% 5730 year half life (Beta decay)
If you are alive you have some in you

Example:
This is how you can carbon date a mummy


Map of the Chesapeake Bay showing dissolved concentration of uranium in ng/mL


Nuclear Fission and Fusion

A chain reaction of large mass isotopes such as U-235 requires:

High purity of U-235
Critical mass

Example of Uranium fission:

Uranium

How much energy?

2 x 1013 J / mol
(20,000,000,000,000 J/mol; or 20 trillion)

Figure 3-11, 3-12, 3-13 demonstrate fission of U-235


Nuclear fission

Nuclear fission chain reaction

Nuclear fusion


Fusion:   "Sun power"


Scientific copy is:

(Unfortunately, we need a couple million degrees just to get it going)

Fusion is more efficient than Fission



Radon       (read pg. 573-74, Miller)

Attention to the presence of Radon gas in US homes was brought sharply to the front page news in 1984 - An engineer at the Limerock Nuclear power Plant in Pennsylvania repeatedly triggered the plant's radioactivity detectors. The source of the radiation was his home (Mr. Watrus). At the time EPAês budget for evaluating radon was $0.

Watrus Home in 1984 --> 2.7 x 103 pCi/L (equated to 455,000 chest x-rays/yr.)

EPA action level 4 pCi/L

Out door reference level approximately 0.2 pCi/L

Why?

Uranium ore - to - Radium - 226 to Radon - 219, 220, 222 U - 238

Radon - 219, 220 1/2 life ~ seconds

Radon - 222, 3.8 days 1/2 life

Radon - 222 to Polonium - 218 and Polonium - 214
  alpha- emitters 1/2 life 3.1 min. 2 x 10-4 s

Where is Radon found and why?

Associated with deposits of Uranium
  Granite
  Phosphate Rock
  Water that flows through granite or uranium deposits
  Collecting in low cavities in the earth, caves, mines, basements

Radon is continuously renewed by the constant decay of Uranium.

Why does it enter your basement?
Why does it not react with something in the ground first?
What is radon?

Data you may need to make reach a conclusion:

Atomic wt of Radon is 222 g/mole
Wt. of air is approximately 14.4 g/mole

Problem:

  Radon - inert   Po is a reactive positive ion and clings to lungs (bronchial tissue)

alpha- penetration approx. 70µm, approx 2x the cell membrane thickness of lung tissue thus access to DNA is the proposed cause of lung cancer.

Enough energy to break both sides of a DNA chain simultaneously.
  Why is this a problem?

Specific location of carcinoma in lung, yes (bronchial tissue)

5,000 to 20,000 deaths per year attributed to Radon.
Detection - Yes
Epidemiology - Yes (dose response of Uranium miners)
Engineered barriers - Yes (Radon pumps and sealing cracks)


Sources of indoor radon-222 gases


Energy Consumption

84% of commercial energy used in the US is wasted.

41% is wasted due to the second law of thermodynamics and inefficient transfer mechanisms. (resistance losses, waste heat loss, etc.)

43% is wasted unscientifically and could be recovered.

Examples: Figure (29) energy losses.

What is the number one (#1) anthropogenic source of air borne radiation?

Science is simply common sense at its best – that is, rigidly accurate in observation, and merciless to fallacy in logic.
– Thomas Huxley

Nuclear Waste Storage

Kinds of Nuclear Waste
  1. High Level - fuel rods, bomb fuel
  2. Transuranic "TRU" -

Nuclear Waste Isolation
  Dangerous for 10,000 years
  Isolate from human contact - How?

Geology and Time
  High level waste not finalized yet.
  TRU waste - WIPP facility in NM
    Geology is the key

  How is the facility constructed?   In a salt geological layer 2190 ft. below the surface of the earth

A picture is worth a thousand words.

WIPP site for disposal of TRU waste

What is it?

What is doing the protecting?

How long must it be there?

What guarantees the safety?

What is the most likely scenario of it getting out?

Why has it taken 25 years to get this far?

Some examples:

Some data:

  a. Unique geological site in a salt dome over 1500 feet thick

  b. Relatively stable geological formation

  c. 500 feet above sea level

  d. Location over 2,190 feet down

  e. Relatively dry and impervious to water

  f. Relatively little valuable geology for future interest

  g. Dry climate

h. No local rivers or water sources

Pictorial examples and diagrams of the site provide an appreciation for the scale and complexity this task.

Examples

Most likely scenario of WIPP release:

    Human intervention:

1. Drilling or mining in the distant future

2. Accidental damage to transport vehicle

3. Terrorist or sabotage to transport or site

Observations

Suggestions

"Science is built up with facts, as a house is with stones. But a collection of facts is no more a science than a heap of stones is a house".
        Jules Henri Poincare'

Matching energy use to quality of energy
  Example:   Space heating requires the lowest quality of energy
  Use of high quality energy to perform this task is wasteful

Figures (30), (31), (32) energy efficiency

"We cannot recycle waste heat, we can only conserve energy"

Discussion of energy use in the US

Figures (32-35)

Waste heat

Conservation of energy
Efficiency of devices

Why is solar heating (passive) so efficient?
Where does the energy come from?

In what form of energy, does the Sun deliver energy to Earth?

Why is a fluorescent light 22% efficient and an incandescent 5%?
What energy form is given off?
What energy form is wasted?
Why?




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created 11/6/98