NOTES: 25.2 – Nuclear Stability and Radioactive Decay

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Presentation transcript:

NOTES: 25.2 – Nuclear Stability and Radioactive Decay

Why does the nucleus stay together? STRONG NUCLEAR FORCE ● Short range, attractive force that acts among nuclear particles ● Nuclear particles attract one another ● Much stronger than electrical or gravitational force STABLE NUCLEUS ● A nucleus that does NOT spontaneously decay ● MOST ATOMS ARE STABLE!!

Nuclides ● Different atomic forms of all elements ● Most small nuclides have equal # of protons and neutrons ● Some nuclides have “magic #’s” of protons and neutrons and are especially stable

The neutron-to-proton ratio determines the STABILITY of the nucleus ● For low atomic #’s: Equal #’s of protons and neutrons ● Above atomic #20: More neutrons than protons

Nuclei whose neutron-to-proton ratio is unstable undergo radioactive decay by emitting 1 or more particles and/or electromagnetic rays:

When is a nucleus STABLE? ● for nuclei below atomic #20, the stable nuclei have roughly equal numbers of protons and neutrons ● EXAMPLES: carbon-12: 6 pro, 6 neu nitrogen-14: 7 pro, 7 neu oxygen-16: 8 pro, 8 neu

When is a nucleus STABLE? ● for nuclei above atomic #20, the stable nuclei have more neutrons than protons; ● the “stable” neutron : proton ratio is 1.5 ● EXAMPLE: lead-206: 82 protons, 124 neutrons (ratio = 124 / 82 ≈ 1.5)

When is a nucleus UNSTABLE? ● too many neutrons relative to protons ● decay by turning a neutron into a proton and emitting a beta particle (an electron) – this results in an increase in # of protons and a decrease in # of neutrons: ● EXAMPLE:

When is a nucleus UNSTABLE? ● too many neutrons AND too many protons to be stable ● all nuclei with atomic # greater than 83 are radioactive and are especially heavy ● most of them emit alpha particles as they decay ● EXAMPLE:

REVIEW: Radioactive Decay ● An unstable nucleus loses energy by emitting radiation ● Radiation = penetrating rays and particles emitted by a radioactive source ● Radioisotopes = unstable isotopes undergo change to become more stable

Nuclei whose neutron-to-proton ratio is unstable undergo radioactive decay by emitting 1 or more particles and/or electromagnetic rays: Type/ symbol Identity Mass (amu) Charge Penetration Alpha Beta Gamma Proton Neutron helium nucleus 2+ low 4.0026 electron 0.00055 1- low-med high energy radiation high proton, H nucleus 1+ 1.0073 low-med neutron 1.0087 very high

Comparing penetrating ability…

Half-Life: ● every radioactive isotope has a characteristic RATE of decay called the HALF-LIFE. ● HALF-LIFE = the amount of time required for ½ of the nuclei of a radioisotope sample to decay to its products ● Half-lives may be short (fraction of a second) or long (billions of years)

Half-Life

Daughter Parent

Uses of Radioactive Isotopes: ● if there is a long half-life: can be used to determine the age of ancient artifacts; ● if there is a short half-life: can be used in nuclear medicine (rapid decaying isotopes do not pose long-term radiation hazards to patient)

How is the decay rate of a radioactive substance expressed? Equation: A = Ao x (1/2)n A = amount remaining Ao = initial amount n = # of half-lives (**to find n, calculate t/T, where t = time, and T = half-life, in the same time units as t), so you can rewrite the above equation as: A = Ao x (1/2)t/T

½ Life Example #1: ● Nitrogen-13 emits beta radiation and decays to carbon-13 with t1/2 = 10 minutes. Assume a starting mass of 2.00 g of N-13. A) How long is three half-lives? B) How many grams of the isotope will still be present at the end of three half-lives?

½ Life Example #1: ● Nitrogen-13 emits beta radiation and decays to carbon-13 with t1/2 = 10 minutes. Assume a starting mass of 2.00 g of N-13. A) How long is three half-lives? (3 half-lives) x (10 min. / h.l.) = 30 minutes

½ Life Example #1: ● Nitrogen-13 emits beta radiation and decays to carbon-13 with t1/2 = 10 minutes. Assume a starting mass of 2.00 g of N-13. B) How many grams of the isotope will still be present at the end of three half-lives? 2.00 g x ½ x ½ x ½ = 0.25 g

½ Life Example #1: ● Nitrogen-13 emits beta radiation and decays to carbon-13 with t1/2 = 10 minutes. Assume a starting mass of 2.00 g of N-13. B) How many grams of the isotope will still be present at the end of three half-lives? A = Ao x (1/2)n A = (2.00 g) x (1/2)3 A = 0.25 g

½ Life Example #2: ● Mn-56 is a beta emitter with a half-life of 2.6 hr. What is the mass of Mn-56 in a 1.0 mg sample of the isotope at the end of 10.4 hr?

½ Life Example #2: ● Mn-56 is a beta emitter with a half-life of 2.6 hr. What is the mass of Mn-56 in a 1.0 mg sample of the isotope at the end of 10.4 hr? A = ? n = t / T = 10.4 hr / 2.6 hr A0 = 1.0 mg n = 4 half-lives A = (1.0 mg) x (1/2)4 = 0.0625 mg

½ Life Example #3: ● Strontium-90 is a beta emitter with a half-life of 29 years. What is the mass of strontium-90 in a 5.0 g sample of the isotope at the end of 87 years?

½ Life Example #3: ● Strontium-90 is a beta emitter with a half-life of 29 years. What is the mass of strontium-90 in a 5.0 g sample of the isotope at the end of 87 years? A = ? n = t / T = 87 yrs / 29 yrs A0 = 5.0 g n = 3 half-lives A = (5.0 g) x (1/2)3 A = 0.625 g