CHEM 1112: Nuclear Chemistry

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48 Terms

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Nuclear Composition

  • nuclei contain two types of nucleons:

    • protons (+ charge)

    • neutrons (neutral charge)

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Proton, Neutron, and Electron charge/mass

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Atomic # vs. Mass #

  • Atomic #:

    • Z

    • number of protons in nucleus

  • Mass #:

    • A

    • number of protons + neutrons in nucleus

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Principal Isotropes of H

  • protium

    • most abundant

  • deuterium

  • tritium

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Nuclide

  • a particular nucleus

  • characterized by # of protons (Z) and neutrons (N) that they possess

    • chlorine-37 is a nuclide

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Isotopes

  • atoms of the same element whose nuclei contain different numbers of neutrons

    • chlorine-37 is an isotope of chlorine

  • some isotopes are unstable, and tend to rearrange or disintegrate

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Mass Deficit

  • ∆m

  • a nucleus has a lower mass than the sum of its parts

    • this is because so much energy is released upon the formation of a stable nucleus, that the nucleus actually loses mass

  • can be calculated by comparing the “sum of the parts” to the observed mass

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Nuclear Binding Energy

  • a positive mass defect (∆m) times the speed of light (s) to find a change in energy (∆E)

  • energy corresponding to the mass defecit

    • positive sign represents the energy required to disassemble the nucleus

  • nuclides with mass # around 56 are the most stable

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Relative Nuclear Stability

  • to compare which nucleus of two separate nuclides is more stable, we must compare binding energy per nucleon

  • ∆E/nucleon

    • higher binding energy per nucleon → more stable

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Unstable Nuclei

  • too many or too few neutrons (for the # of protons) which causes the nucleus to be unstable

    • unstable nuclei may become more stable by giving off this excess matter and/or energy, or by capturing a nearby electron

  • nuclei that are too large (too many protons in the small area of the nucleus) will be unstable

    • such nuclei may become more stable by giving off the excess matter or even splitting to form two new nuclei

  • all isotopes of elements with atomic numbers greater than 83 are unstable

  • Unstable nuclides decay to form more stable nuclides

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Belt of Stability

  • unstable nuclides in green

  • stable nuclides in blue

    • generally, most stable isotopes have n > Z

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Nuclear Stability

  • balance between attractive forces and repulsive forces

    • attractive forces only over very very short distances

  • elements with large atomic # (Z) need more neutrons

    • this increases the value of net nuclear binding force

    • this increases the distances between protons

    • this decreases repulsion

  • more stable nuclides have roughly equal numbers of neutrons and protons

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Nuclear Decay

  • decomposition of unstable nuclides into more stable ones, often accompanied by a change in mass

    • radioactive decay

  • decay MUST conserve mass # and charge !!!!!

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Radioactivity

  • spontaneous nuclear disintegration of atoms with emission of particles or electromagnetic radiation.

  • radiation that is emitted from a radioactive isotope may include:

    • alpha particles

    • beta particles

    • positrons

    • gamma rays

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Alpha Particle

  • ɑ

  • high energy helium nuclei consisting of two protons and two neutrons

    • mass # is 4

    • charge is 2+

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Beta Particle

  • β

  • high energy negatively charged particle (electron)

    • mass # is 0

    • charge is -1

  • will not exist long, usually will promptly collide with an electron

    • both will be annihilated with the release of energy (usually 2 gamma photons)

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Positron

  • composed of + charged particles (positrons)

    • mass # is 0

    • charge is +1

  • will not exist long, will promptly collide with an electron

    • both will be annihilated with the release of energy (usually 2 gamma photons)

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Gamma Photons

  • 𝛾

  • very high energy electromagnetic radiation

    • mass # is 0

    • charge is 0

  • a photon

  • very penetrating, and can pass through a human body

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Chemical Change

  • in chemical change, no material is created or destroyed

  • end up with the same number/types of atoms

  • net charge is conserved

  • energy may be absorbed or produced, but any mass change is not measurable

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Radioactive Decay

  • total mass number is conserved

  • total charge is conserved

  • types of atoms will usually change

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Nuclear vs. Chemical Reaction

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ɑ-emission

  • Z decreased by two units and A decreases by 4 units

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β-emission

  • Z increases by one unit and A does not change

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Positron Emission

  • Z does not change, and A is decreased by 1 unit

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Electron Capture

  • Z does not change, and A is decreased by 1 unit

  • an inner shell electron of the atom is a reactant

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Types of Nuclear Decay

  • Too big ?

    • ɑ-emission

  • Protons too large ?

    • β-emission

  • Protons too small ?

    • positron emission

    • electron capture

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Decay Sequences

  • series of radioactive decays that an unstable nucleus undergoes in order to become stable

  • may either be ɑ-decay or β-decay

  • all decays obey the 1st order rate law

    • Rate= k[A]

    • t1/2 = 0.693/k

    • ln[A]t / [A]o = -kt

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Unstable Nuclei

  • stable isotopes remain stable, whereas unstable isotopes continuously disintegrate

    • thus, every element should be composed of ONLY stable isotopes

  • unstable isotopes present either have half-lives longer than the age of the earth, or are products of the decay of these nuclides

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Nuclear Transmutation

  • transformation of one element into another

    • occurs during nuclear reactions

    • is not restricted to natural decay processes

    • can also occur through induced nuclear reactions

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Induced Nuclear Reaction

  • occurs when a nuclear projectile collides and reacts with another nucleus

  • classified according to the nature of the nuclear projectile

    • most common: neutron-capture

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Neutron Capture

  • always exothermic

  • product is a metastable, highly excited nuclide that usually decays by either proton or gamma emission

  • neutrons could come from the sun, or produced in a nuclear reactor

    • the earths atmosphere is constantly bombarded with solar neutrons

    • can be captured by the most abundant element in atmosphere 14N to form unstable 15mN, which will fragment into 12C + 3H

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Fission

  • when heavy nuclides fragment

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Fusion

  • when light nuclides combine

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Fission Chain Reaction

  • the fission of a large nucleus produces two or three neutrons, each of which is capable of causing fission of another nucleus by the reactions shown attached.

    • if this process continues, a nuclear chain reaction occurs

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Subcritical Mass

  • fissile material is too small and allows too many neutrons to escape the material, so a chain reaction does not occur

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Critical Mass

  • a large enough number of neutrons in the fissile material induce fission to create a chain reaction

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Advantages of Nuclear Fission (energy production)

  • generates a tremendous amount of electricity from a small amount of fuel

  • generates no air pollution, or greenhouse gases

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Problems with Nuclear Fission (energy production)

  • potential for nuclear accidents as the fission reaction can overheat

  • the disposal of products brings issues, as they may be radioactive and have long half-lives

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Advantages with Nuclear Fusion (energy production)

  • generates a tremendous amount of electricity from a small amount of fuel

  • generates no air pollution, or greenhouse gases

  • provides about 10x more energy per gram of fuel than fission

  • does not produce radioactive waste products

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Problems with Nuclear Fusion (energy production)

  • very high temperatures required for fusion to occur, and no existing material can withstand those temperatures for long

  • need to contain using magnetic fields

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Tokamak Fusion Reactor

  • uses a powerful magnetic field to confine plasma

    • able to reach temperatures around 100-150 million oC

  • difficult to attain conditions to allow the reaction to be self-sustaining and controlled

    • record is 22 minutes of maintained plasma reaction, reached a few months ago

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Applications of Radioactivity

  • radiocarbon dating

  • applications to human health

    • diagnosis of disease

    • treatment of disease

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Radiocarbon Dating

  • in the upper atmosphere 14C both forms and degrades at a constant rate, thus there is a relatively constant ratio of 14C:12C in the atmosphere

    • from this, scientists can work backwards to determine the length of time since an organism had ‘died’

  • can date organisms up to 50,000 years old with 5% accuracy

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Uranium/Lead Dating

  • can estimate age of older objects that were never alive, using other techniques

    • U-238 decays to Pb-206 with a half-life of 4.5×109 years

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Positron Emission Tomography

  • PET scan

  • detects gamma rays emitted during positron annihilation

  • used commonly to detect areas of high metabolic activity

    • active areas of brain

    • sites of tumours

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Warburg Effect

  • the rate of glycolysis is elevated in almost all tumours

  • useful for potential treatment strategies

  • useful for diagnosis of cancer

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Glycolysis

  • set of reactions that converts glucose to pyruvate or lactate

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Boron Neutron Capture Theory

  • novel approach where tumour cells are allowed to pick up compounds rich in boron-10.

    • the tissues are then bombarded with neutrons

    • boron-10 will capture the neutrons, forming radioactive boron-11

  • targets:

    • brain tumours

    • head and neck cancer

    • melanoma

    • liver cancer

    • lung cancer

    • mesothelial tumour

    • breast cancer

  • able to target tumour cells since target cells are actively producing proteins that contain tyrosine