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Lesson 14 Radiotracers

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Lesson 14. Radiotracers. Introduction. Basic principle: All isotopes of a given element will behave identically in most physical, environmental and biological environments. Ea sier to detect radioactive atoms than stable atoms. Simple Cheap - PowerPoint PPT Presentation

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Page 1: Lesson 14

Lesson 14

Radiotracers

Page 2: Lesson 14

Introduction• Basic principle: All isotopes of a given

element will behave identically in most physical, environmental and biological environments.

• Easier to detect radioactive atoms than stable atoms.

• Simple• Cheap• Amazing breadth of applications. Now

part of the standard arsenal of analytical techniques

Page 3: Lesson 14

Designing a Radiotracer Experiment• Radioactive isotopes of a given

element behave the same as stable isotopes.

• Isotope Effect--Most concern for H, 15% effect for 12C vs 14C.

• Nonisotopic tracers

Page 4: Lesson 14

Intermolecular vs Intramolecular Effects

• Intramolecular--decarboxylation of malonic acid (HOO14C-12CH2-12COOH)

• Intermolecular--decarboxylation of benzoic acid-7-14C (C6H5-14COOH vs C6H5-12COOH)

Page 5: Lesson 14

Basic Principle #2• Radioactivity does not change

the chemical and physical properties of the system.

• Tracer activities, bond strengths, energy of emitted radiation

• 3H problem• “Daughter atom problems”

Page 6: Lesson 14

Basic Principle #3• No deviation from normal

physiological state.• Injecting stable as well as

radioactive material

Page 7: Lesson 14

Basic Principle #4• Chemical and physical form of the

labeled material is the same as the un-labeled material.

• Aqueous chemistry• Adsorption, carriers, carrier-tracer

exchange• Radiochemical purity• Position of the label

Page 8: Lesson 14

Basic Principle #5• Label stays intact

Page 9: Lesson 14

Practical Considerations

• Availability of tracer• t1/2• Labeling, position of the label• Ease of detection• Health and safety aspects• Waste disposal

Page 10: Lesson 14

Calculation of the amount of tracer

needed• No excuse for turning a tracer experiment into a detection problem.

• Statistics (> 104 cts)• Counting efficiency, detector type,

geometry factors, chemical yields• Safety factor

Page 11: Lesson 14

Hazard evaluation• Dose rates, RBEs• Effects on physiology• Waste problems• Green chemistry

Page 12: Lesson 14

Radiotracer Preparation

Commonly Used Tracers3H(T) R 12.33 yr

- 0.01814C R 5730 yr

- 0.15622Na C 2.60 yr

+, 1.27424Na R 15.0 hr

1.36932P R 14.3 d

- 1.71

•n-rich vs p-rich•PET nuclides

Page 13: Lesson 14

Labeling• Position: acetic-1-14C acid =

CH314COOH, acetic-2-14C acid =

14CH3COOH• Terms; Specifically labeled, U,

N G

Page 14: Lesson 14

Methods of labeling• Chemical synthesis,best except

for chirality• Biological synthesis, tedious• Tritium• Commercial supplier problems

Page 15: Lesson 14

Physical tracers• Wear, corrosion• Mixing• Fluid motion• Pollutant tracing• Measuring unknown volume

V = V1(A1

A2

−1)

Page 16: Lesson 14

Chemical Applications• Test separation procedures• Ksp measurements• Exchange reactions• Chemical reaction mechanisms

Page 17: Lesson 14

Example• Cyclization of -

phenoxyacetophenone to 2-phenylbenzofuran

Page 18: Lesson 14
Page 19: Lesson 14

Physical Isotope Effects• Gaseous diffusion• Distillation

Page 20: Lesson 14

Chemical Isotope Effects

AX + BX* ⇔AX* + BX

Table 4-2 Typical Equilibrium Isotope Effects Reacting System K

H2H(g) + H2O(l)⇔H2() + 2HOH(l) 3.2

14CO2()+12COCl2()⇔ 14COCl2()+12CO2() 1.0884

[Co(NH3)412CO3]++14CO32-⇔ 12CO3

2-+[Co(NH3)414CO3]+ 0.8933

Page 21: Lesson 14

Kinetic Isotope EffectsA + B → AB → products

d[B]dt

= k[A]a[B]b

d[B*]dt

= k * [A]a[B*][B]b−1

d[B]d[B*]

= k[B]k * [B*]

log10(Sγ

S0

) = ( k *k

−1)log10(1− γ )

Page 22: Lesson 14
Page 23: Lesson 14

Biological applications

Autoradiography

Page 24: Lesson 14

DNA Analysis

Page 25: Lesson 14

Radioimmunoassay

Page 26: Lesson 14

Figure 19. The radioimmunoassay technique to measure hormone levels in the body involves mixing natural hormones (from a blood sample) and radioactively prepared hormones together, and adding that mixture to a solution containing artificially produced antibodies. The two hormones compete for binding sites on the antibodies. The hormones attach to the antibodies in amounts that ore proportional to their concentration.

Page 27: Lesson 14

Environmental Applications of Radiotracers• Used in tracing pollutant motion in

atmosphere, hydrosphere, lithosphereAdvantages of radiotracers• Not influenced by state of system• Highly penetrating• Good detection sensitivity• If t1/2 short, will disappear after expt.• CheapBIG PROBLEM--HP

Page 28: Lesson 14

Typical Environmental Radiotracers

• 41Ar• 24Na• 82Br• 140La

Page 29: Lesson 14

Industrial Uses of Radiotracers

Nuclide Application

3H Self-luminous aircraft and exit signsLuminous dials, gauges, wrist

watchesLuminous paint

24Na Location of pipeline leaksOil well studies

46Sc Oil exploration tracer

55Fe Analysis of electroplating solutionsDefense power source

60Co Surgical instrument and medicine sterilization

Safety and reliability of oil burners

63Ni Detection of explosivesVoltage regulators and current surge

protectorsHeat power source

Page 30: Lesson 14

Nuclear Medicine• Therapy and diagnosis• Most important radionuclides

are 99Tcm and the I isotopes. Over 90% of procedures involve these nuclei

Page 31: Lesson 14

99Tcm

• 143 keV gamma rays• 6 hr t1/2

• Use of generators

Page 32: Lesson 14

99Mo β −

⏐ → ⏐ 99Tc m IT (142.7keVγ ) ⏐ → ⏐ ⏐ ⏐ ⏐ 99Tc

Page 33: Lesson 14
Page 34: Lesson 14

PET, Positron Emission Tomography

Page 35: Lesson 14
Page 36: Lesson 14
Page 37: Lesson 14

Isotope Dilution Analysis• Direct IDA

• In direct IDA, we are faced with the problem of determining the amount of some inactive material A in a system. Let us define this unknown amount as x grams. To the system containing x grams of inactive A, we add y grams of active material A* of known activity D. Thus we know the specific activity of the added active material, S1.

S1 = Dy

After thoroughly mixing the active material A* with the inactive A in the system, one isolates, not necessarily quantitatively, and purifies a sample of the mixture of A and A* and measures its specific activity, S2.

S2 =D

x + y

S2 =D

x + DS1

x =DS2

−DS1

=DS1

(S1

S2

−1) = y(S1

S2

−1)