Presentation is loading. Please wait.

Presentation is loading. Please wait.

Ch. 18: The Nucleus Review 21.1: Nuclear Stability and Radioactive Decay 21.2 Kinetics of Decay 21.3 Nuclear Transformations.

Similar presentations


Presentation on theme: "Ch. 18: The Nucleus Review 21.1: Nuclear Stability and Radioactive Decay 21.2 Kinetics of Decay 21.3 Nuclear Transformations."— Presentation transcript:

1 Ch. 18: The Nucleus Review 21.1: Nuclear Stability and Radioactive Decay 21.2 Kinetics of Decay 21.3 Nuclear Transformations

2 Review Nucleus contains protons and neutrons Atomic number (Z) - # p+
Mass number (A) - # p+ + # n0 Isotopes- differ in number of neutrons only Same Z but different A Nuclide- specific type of atom, member of a group of isotopes Nuclear symbol notation

3 Radioactivity and Stability
A nucleus that decomposes forming another nucleus and one or more particles All nuclides are unstable with 84 p+ or more Lightweight nuclides are stable with equal numbers of n0 and p+ Heavy nuclides should have ratio >1 to be stable

4 Radioactivity and Stability

5 Types of Decay- A changes
Alpha particle production α particle: helium nucleus Spontaneous fission Splitting of a heavy nucleus into 2 lighter nuclides that are about the same size

6 Types of Decay- A is Constant
Beta Particle Production β particle is an electron Can assume the mass is zero Net effect : changing a n0 into a p+

7 Types of Decay- A is Constant
Gamma Ray Production γ ray is collection of high energy photons Occurs with other types of decay Helps a nucleus release extra energy so it can relax to a lower energy state

8 Types of Decay- A is Constant
Positron Production Occurs for nuclides below the line of stability Positron is a positive particle with same mass of electron Also called antiparticle of electron Net effect: change p+ into n0

9 Types of Decay- A is Constant
Electron Capture One of the inner electrons in an atom is captured by nucleus Gamma rays always produced Decay Series When several types of decay occur until a stable nuclide is produced

10 Writing Equations 116C produces a positron
21483Bi produces a beta particle 23793Np produces an alpha particle

11 Writing Equations Beta particle (electron) Electron capture Positron
Positron production

12 Kinetics of Decay Rate of decay is directly proportional to number of nuclides available All are first order Constant half-life

13 Example If the half-life of a decay is 67.0 hours, how much of a mg sample will remain after 335 hours? 335 / 67 = 5 half-life’s 1.000 mg  mg  0.250 mg  mg  0.062 mg  mg

14 Nuclear Transformations
Change of one element into another Scientists have been able to use this to make the periodic table larger by creating new elements Since 1940, have been able to make transuranium elements (93-112)

15 18.4 Detection and Uses of Radioactivity 18.5 Thermodynamic Stability
18.6 Nuclear Fission and Fusion 18.7 Effects of Radiation

16 Carbon-14 Dating Used to date items made out of natural fibers
Created by Willard Libby in 1940s Based on the decay of naturally existing carbon-14 isotope by β-particle production It is also created

17 Carbon-14 Dating These happen at the same rate as long as the plant is alive but when it dies, the decay happens more rapidly than the creation Ratio of 14-C to 12-C decreases Most accurate for pieces older than 10,000 years

18 Medical Applications Radiotracers
Radioactive nuclides that can be traced in people by monitoring their radioactivity Thallium-201 For assessing heart damage from heart attacks Is taken up by healthy heart tissue only

19 Medical Applications Iodine-131 For diagnosing thyroid problems
Patients drink a solution of 131-I and the uptake is monitored

20 Thermodynamic Stability
Can be determined by calculating the change in potential energy if the nucleus is made from individual particles We can create energy changes by comparing the sum of the masses: mass defect Mass of 168O – mass of (8 10n n) Convert amu on periodic table to g (1amu=1.66x10-24 g) x10-23 – [8( x10-24) + 8( x10-24)] -2.269x10-25 g/nucleus = g/mol : lost when 1 mol of 16-O is formed

21 Thermodynamic Stability
Find energy (J) using E=mc2 E = (-1.366x10-4kg)(3.00x108m/s) = -1.23x1013J/mol Binding energy Energy required to decompose this nucleus into its particles Often in MeV / nucleon mass must be in kg!

22 Thermodynamic Stability

23 Nuclear Fission and Fusion
Splitting a heavy nucleus into 2 smaller nuclei with smaller mass numbers Can use neutrons to create instability Neutrons produced are used to cause more fission Produces a huge amount of energy

24 Nuclear Fission and Fusion

25 Nuclear Fission and Fusion
Combination of 2 light nuclei to form a heavier, more stable nucleus Stars produce their energy using this Requires very high temperatures Must be shot at each other to get close enough

26 Effects of Radiation Any sort of energy transferred to cells can break bonds and cause damage Radioactive species are sources of high energy particles so can be very harmful Types Somatic: cause illness, cancer, death Genetic: produce damage in offspring

27 Factors in Effects of Radiation
The more energy, the more damage How deep it goes into body γ rays > β particles (1 cm) > α particles (skin) How easily they attract electrons from biomolecules (ionization) γ rays cause less than α particles How long it stays inside body


Download ppt "Ch. 18: The Nucleus Review 21.1: Nuclear Stability and Radioactive Decay 21.2 Kinetics of Decay 21.3 Nuclear Transformations."

Similar presentations


Ads by Google