NOTES: 25.2 Nuclear Stability and Radioactive Decay
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1 NOTES: 25.2 Nuclear Stability and Radioactive Decay
2 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!!
3 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
4 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
5 Nuclei whose neutron-to-proton ratio is unstable undergo radioactive decay by emitting 1 or more particles and/or electromagnetic rays:
6 When is a nucleus STABLE? for nuclei below atomic #20, the stable nuclei have roughly equal numbers of protons and neutrons EXAMPLES: carbon-12: nitrogen-14: oxygen-16: 6 pro, 6 neu 7 pro, 7 neu 8 pro, 8 neu
7 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 / )
8 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: B C e
9 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: Ra Rn He
10 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
11 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 or 4 2He or 0-1e p or 1 1 H helium nucleus electron high energy radiation proton, H nucleus low low-med high low-med Neutron 1 0n neutron very high
12 Comparing penetrating ability
13 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)
14 Half-Life Half Life Amount Time
15 250 Daughter Time Parent Amount
16 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)
17 How is the decay rate of a radioactive substance expressed? Equation: A = amount remaining A o = initial amount n = # of half-lives A = A o x (1/2) n (**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 = A o x (1/2) t/t
18 ½ Life Example #1: Nitrogen-13 emits beta radiation and decays to carbon-13 with t 1/2 = 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?
19 ½ Life Example #1: Nitrogen-13 emits beta radiation and decays to carbon-13 with t 1/2 = 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
20 ½ Life Example #1: Nitrogen-13 emits beta radiation and decays to carbon-13 with t 1/2 = 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
21 ½ Life Example #1: Nitrogen-13 emits beta radiation and decays to carbon-13 with t 1/2 = 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 = A o x (1/2) n A = (2.00 g) x (1/2) 3 A = 0.25 g
22 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?
23 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 =? A 0 = 1.0 mg n = t / T = 10.4 hr / 2.6 hr n = 4 half-lives A = (1.0 mg) x (1/2) 4 = mg
24 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?
25 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 =? A 0 = 5.0 g A = (5.0 g) x (1/2) 3 A = g n = t / T = 87 yrs / 29 yrs n = 3 half-lives
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