/
Lecture 6  Radioactive Isotopes Lecture 6  Radioactive Isotopes

Lecture 6 Radioactive Isotopes - PowerPoint Presentation

luanne-stotts
luanne-stotts . @luanne-stotts
Follow
488 views
Uploaded On 2017-04-06

Lecture 6 Radioactive Isotopes - PPT Presentation

Definitions and types of decay Derivation of decay e quations Half l ives and mean lives Secular Equilibrium Useful radiotracers in oceanography E amp H Chpt 5 The chart of the nuclides decay ID: 534389

parent decay activity daughter decay parent daughter activity polonium 210 life time atoms radioactive body present dose alpha ocean

Share:

Link:

Embed:

Download Presentation from below link

Download Presentation The PPT/PDF document "Lecture 6 Radioactive Isotopes" is the property of its rightful owner. Permission is granted to download and print the materials on this web site for personal, non-commercial use only, and to display it on your personal computer provided you do not modify the materials and that you retain all copyright notices contained in the materials. By downloading content from our website, you accept the terms of this agreement.


Presentation Transcript

Slide1

Lecture 6 Radioactive Isotopes

Definitions and types of decayDerivation of decay equationsHalf lives and mean livesSecular EquilibriumUseful radiotracers in oceanography

E & H

Chpt

5Slide2

The chart of the nuclides - decay

Q. 230Th90 How many protons / neutrons? Slide3

Full Chart of the Nuclides

1:1 lineValley of StabilityFor

230

Th N/P = 1.55Slide4

Radioisotopes and decay

Definitions and UnitsParent – Original radioactive atomDaughter – The product of decayDecay Chain – A series of sequential decays from one initial parentDecay is independent of chemistry and T and P.Decay is only a property of the nucleus (see Chart of Nuclides)

Types of Decay

D

P

D

N

D

Atomic

Wt.

Alpha

a

He2+ -2 -2 -4Beta b e- + 1 -1 0 (n → P+ + e-)Gamma g “packets of excess energy”

MeasurementsSlide5

The chart of the nuclides

– decay pathwaysX

b

decay

X

a

decaySlide6

Mathematical Formulation of Decay

Decay Activity (A) = decays per time (e.g. minutes (dpm) or second (dps))A = l

N

l

= decay constant (t

-1

)

N = # of atoms or concentration (atoms l

-1

)

Remember 1 mol = 6.02 x 10

23

atomsUnits:Becquerel (Bq) = 1 dps (the official SI unit)Curie (Ci) = 3.7 x 1010 Bq = Activity of 1 gram of 226RaNamed after Pierre CurieSee this link for the history:

http://www.orau.org/ptp/articlesstories/

thecurie.htmSlide7

Decay

Equations (essential math lessons)Decay is proportional to the # of atoms present (first order)dN/dt = - N = ANwhereN = the number of atoms of the radioactive substance present at time t = the first order decay constant (time-1)

The number of parent atoms at any time t can be calculated as follows.

The decay equation can be rearranged and integrated over a time interval.

where

N

o

is the number of parent atoms present at time zero. Integration leads to

or

orSlide8

Decay Curve

Both N and A decrease exponentiallySlide9

Half Life

The half life is defined as the time required for half of the atoms initially present to decay. After one half life: From the decay equation =  t1/2 ln (2) =  t1/2 0.693 =  t1/2so

Math note:

-ln(1/2) = - (ln 1 – ln 2)

= - ( 0 – ln 2)

= + ln2 = 0.693Slide10

Mean Life = Average Life of an Atom

t

= 1 /

l

= (1/0.693)

t

1/2

t

= 1.44

t

1/2

Q. Why is the mean life longer than the half life?Slide11

Isotopes used

in Oceanographysteady state transient

U-Th series are shown on the next

page. These tracers have a range

of chemistries and half lives.

Very useful for applications in

oceanography.Slide12

Two forms of Helium3He2 from beta decay of 3H

1 (called tritium) and primordial from the mantle3H1 = 3He2 + b4He2 the product of alpha decay from many elements (especially in U-Th series)How would you expect their distributions to vary in the ocean?Slide13

Example distributions of 3He

from mid-ocean ridge crestJohn Lupton (NOAA) et al (various)Slide14

Q.

Why is the inside of the earth hot?Q. What is the age of the earth? 6000 years or 4.5 x 109 yearsSlide15

238

U decay products in the oceanQ. What controls the concentration of 238U in SW?109 y24 d105

y

10

4

y

1600 y

3 d

22 y

U – conservative

Th

– particle reactive

Ra – intermediate (like Ca)

Rn = conservativePb – particle reactiveSlide16

Parent-Daughter Relationships

Radioactive Parent (A)Stable Daughter (B)A → B e.g. 14C → 15N (stable)Production of Daughter = Decay of Parent

A

B

l

A

2-box model

Example:

14

C →

15

N (stable)

t

1

/2

= 5730

years

l

= 0.693 / t

1/2Slide17

Radioactive Parent (A)

Radioactive Daughter (B)A → B → lA

l

B

source

sink

A

B

l

A

l

B

solution after assuming N

B

= 0 at t = 0

2-box model

mass balance for B

solution:Slide18

Three Limiting Cases

1) t1/2(A) > t1/2(B) or lA < lB one important example:2) t

1/2

(A) =

t

1/2

(B) or

l

A

=

l

B

e.g. 226Ra → 222Rn3) t1/2(A) < t1/2(B) or lA > lB 1600yrs 3.8 days

Case #1: long half life of parent = small decay constant of parent

SECULAR EQUILIBRIUM

Activity of daughter

equals activity of

parent!

Are concentrations also equal???Slide19

Q.

Are concentrations also equal???

Example:

226

Ra and

222

RnSlide20

Secular

equilibrium (hypothetical)t1/2 daughter = 0.8 hrt1/2 parent = time (hr)

Activity

(log scale)

daughter

t

1/2

Parent

d

oesn’t change

!

Daughter grows

in with half life of

the daughter!

Total

Activity

(

parent+daughter

)

Activity

of parent

and daughter

equal at

secular equilibriumSlide21

Grow in of

222Rnfrom 226RaExample:

After 5 half lives

activity of daughter =

95% of activity of parent

Another way to plotSlide22

Example: Rate of grow in

Assume we have a really big wind storm over the ocean so that all the inert gas 222Rn is stripped out of the surface ocean by gas exchange. The activity of the parent of 222Rn, 226Ra, is not affected by the wind. Then the wind stops and 222Rn starts to increase (grows in) due to decay.Q. How many half lives will it take for the activity of 222Rn to equal 50% (and then 95%)of the 226Ra present?Answer: Use the following equation to calculate the activity A at time tSlide23

Radon is a health hazzard!Radon source strength from rocksWhy are some zones high (red)?Slide24

There is considerable exposure due to artificially produced sources!

Possibly largest contributor is tobacco which contains radioactive

210

Po which emits 5.3 MeV

a

particles with an half life of T

1/2

=138.4days.Slide25

Was Litvinenko (a former Russian spy) killed by

210Po?? A case study of 210PoToxicity of Polonium 210Weight-for-weight, polonium's toxicity is around 106 times greater than hydrogen cyanide (50 ng for Po-210 vs 50 mg for hydrogen cyanide). The main hazard is its intense radioactivity (as an alpha emitter), which makes it very difficult to handle safely - one gram of Po will self-heat to a temperature of around 500°C. It is also chemically toxic (with poisoning effects analogous with tellurium). Even in microgram amounts, handling 210Po is extremely dangerous, requiring specialized equipment and strict handling procedures. Alpha particles emitted by polonium will damage organic tissue easily if polonium is ingested, inhaled, or absorbed (though they do not penetrate the epidermis and hence are not hazardous if the polonium is outside the body).Acute effectsThe lethal dose (LD50) for acute radiation exposure is generally about 4.5 Sv. (Sv = Sievertwhich is a unit of dose equivalent). The committed effective dose equivalent

210

Po

is 0.51 µSv/Bq if ingested, and 2.5 µSv/Bq if inhaled. Since

210

Po has an activity of

166 TBq per gram (1 gram produces 166×10

12

decays per second),

a fatal 4-Sv dose can be caused by ingesting 8.8 MBq (238 microcurie),

about 50 nanograms (ng), or inhaling 1.8 MBq (48 microcurie), about 10 ng.

One gram of

210Po could thus in theory poison 100 million people of which 50 million would die (LD50).Slide26

Body burden limit

The maximum allowable body burden for ingested polonium is only 1,100 Bq (0.03 microcurie), which is equivalent to a particle weighing only 6.8 picograms. The maximum permissible concentration for airborne soluble polonium compounds is about 10 Bq/m3 (2.7 × 10-10 µCi/cm3). The biological half-life of polonium in humans is 30 to 50 days. The target organs for polonium in humans are the spleen and liver. As the spleen (150 g) and the liver (1.3 to 3 kg) are much smaller than the rest of the body, if the polonium is concentrated in these vital organs, it is a greater threat to life than the dose which would be suffered (on average) by the whole body if it were spread evenly throughout the body, in the same way as cesium or tritium.Notably, the murder of Alexander Litvinenko in 2006 was announced as due to 210Po poisoning. Generally, 210Po is most lethal when it is ingested. Litvinenko was probably the first person ever to die of the acute α-radiation effects of 210Po , although Irene Joliot-Curie was actually the first person ever to die from the radiation effects of polonium (due to a single intake) in the late 1950s. It is reasonable to assume that many people have died as a result of lung cancer caused by the alpha emission of polonium present in their lungs, either as a radon daughter or from tobacco smoke.