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UNIT 1: ATOMIC STRUCTURE & NUCLEAR CHEMISTRY HONORS Chemistry Grafton High School UNIT OBJECTIVES: • SWBAT: Key Questions • How did the concept of the atom change and develop from the • • • • • • • • • • time of Democritus to the time of John Dalton? What is the structure of the nuclear atom? What are the three kinds of subatomic particles? What makes one element different from another? How do isotopes of an element differ? How do you calculate the atomic mass of an element? How do nuclear reactions differ from chemical reactions? What are the three types of nuclear radiation? How much of a radioactive sample remains after each half life? What are three devices used to detect radiation? What are some practical uses of radioisotopes? The ATOM • An atom is the smallest particle of an element that retains its identity in a chemical reaction. • Although early philosophers and scientists could not observe individual atoms, they were still able to propose ideas about the structure of atoms. HELIUM ATOM Helium Atom Shell proton + - N N + electron What do these particles consist of? - neutron Subatomic Particles Particle Charge Mass proton + ve charge 1 neutron No charge 1 electron -ve charge nil Numbers on the Periodic Table He 2 4 Atomic number the number of protons in an atom Mass Number the number of protons and neutrons in an atom number of electrons = number of protons Energy Levels (shells) Electrons are arranged in Energy Levels or Shells around the nucleus of an atom. • first shell a maximum of 2 electrons • second shell a maximum of 8 electrons • third shell a maximum of 8 electrons Electron Configuration With electronic configuration elements are represented numerically by the number of electrons in their shells and number of shells. For example; Nitrogen 2 in 1st shell 5 in 2nd shell configuration = 2 , 5 2 + 5 = 7 N 7 14 Electron Configuration ~ Bohr Model • Each orbital can hold a certain number of electrons. Orbitals (shells) fill from the inside (nearest nucleus) out. Electron Configurations EXAMPLES of electronic configuration for the following elements: a) Ca 20 b) Na 40 2,8,8,2 d) Cl 17 35 2,8,7 11 23 c) 2,8,1 e) Si 14 28 2,8,4 O 8 16 2,6 f) B 5 11 2,3 Bohr Diagrams With Bohr diagrams, elements and compounds are represented by Dots or Crosses to show electrons, and circles to show the shells. For example: X Nitrogen X X N XX X X N 7 14 Examples of Bohr Diagrams Draw the Dot & Cross diagrams for the following elements; X 8 X a) O b) Cl17 X 35 16 X X X X X X X X X Cl X X X X X O X X X X X X X X X Isotopes ~ varying # of neutrons • Atoms of a certain element all have the same number of protons • Number of neutrons may vary • The different variations in # of neutrons for a certain element are called ISOTOPES • Atomic Mass (decimal)= number of protons + average number of neutrons from all isotopes Isotopes of Carbon Looking at isotopes • The different numbers of neutrons in isotopes gives them different masses • Isotopes of an element do not occur in equal amounts: • Example: Isotopic Abundance • Isotopic Abundance = Percentage of an element’s atoms that exist as each isotope • Each isotope has its own mass that is different from other isotopes of that element. Isotopic mass is the average mass of the atoms of a specific isotope of an element. • Determines the isotope number Relative Atomic Mass • WATCH: https://goo.gl/4y80yz • What does the atomic mass on the periodic table measure? • The relative atomic mass shown as a decimal on the periodic table is the amount of protons plus the weighted average number of isotopes for that element: Atomic Number Chemical Symbol Relative Atomic Mass Calculating Relative Atomic Mass • NOTE: Use the percent abundance of the isotopes as a DECIMAL Relative Atomic Mass (Average Weighted Mass): Relative Atomic Mass = (% Isotope A as decimal x Isotopic Mass Isotope A) + (% Isotope B as decimal x Isotopic Mass Isotope B) + (% Isotope C as decimal x Isotopic Mass Isotope C) EXAMPLE: • Calculation of Relative Atomic Mass for Carbon: Atomic Mass Unit (AMU) • The unit of measurement for an atom is an AMU • AMU = Atomic Mass Unit • ONE (1) AMU = mass of ONE (1) proton • Why NOT grams? Atomic Mass Unit (AMU) • There are 6 X 1023 or 600,000,000,000,000,0 00,000,000 amus in one gram • (Remember that electrons are 2000 times smaller than one amu/one proton) Radioactivity • One of the pieces of evidence for the fact that atoms are made of smaller particles came from the work of ________ (1876-1934). • She discovered ________, the spontaneous disintegration of some elements into smaller pieces. • WATCH: https://goo.gl/IyuRj4 Nuclear Reactions vs. Normal Chemical Changes • Radioisotopes are isotopes with unstable nuclei and undergo radioactive decay • Nuclear reactions involve the nucleus • The nucleus opens, and protons and neutrons are rearranged • The opening of the nucleus releases a tremendous amount of energy that holds the nucleus together – called binding energy • “Normal” Chemical Reactions involve electrons, not protons and neutrons Mass Defect • Nuclear reactions involve energy changes many times the magnitude of chemical changes • Chemical reactions – Energy is conserved • Nuclear reactions – Small loss of matter (mass defect) releases tremendous energy (some of the mass can be converted into energy • Shown by a very famous equation! 2 E=mc Energy Mass Speed of light Types of Radiation Alpha (ά) – a positively charged helium isotope • we usually ignore the charge because it involves electrons, not protons and neutrons e 0 1 •Beta (β) – an electron 4 2 He 0 1 e •Gamma (γ) – pure energy; 0 0 called a ray rather than a particle Other Nuclear Particles • Neutron • Positron – a positive electron •Proton – usually referred to as hydrogen-1 •Any other elemental isotope 1 0 n 0 1 e 1 1 H Penetrating Ability Balancing Nuclear Reactions •In the reactants (starting materials – on the left side of an equation) and products (final products – on the right side of an equation) Atomic numbers must balance and Mass numbers must balance •Use a particle or isotope to fill in the missing protons and neutrons Alpha, Beta, and Gamma Particles • Atoms are not all stable. • Excess energy in an unstable atom is released in a basic particle or wave • Greek alphabet is used to name particles (in order of their discovery) REMEMBER! • The nuclear structure changes with radioactive decay, but radioisotopes are NOT chemically different! Alpha Particles • Heaviest particle • Rays, NOT waves –made of high-energy particles that are expelled from unstable nuclei • Alpha particle is a helium ion • Not very penetrating; easily absorbed • SPEED: 16,000km/sec (1/10th speed of light!) Nuclear Reactions • Alpha emission Note that mass number (A) goes down by 4 and atomic number (Z) goes down by 2. Nucleons (nuclear particles… protons and neutrons) are rearranged but conserved Beta Particles • LIGHTER energy particles • Energetic electron given off • • • • by unstable nuclei to restore energy balance Stopped by aluminum (few mm thick) or 3 meters of air 8,000 times smaller than alpha particle SPEED: 270,000 km/sec Can cause cellular damage Nuclear Reactions • Beta emission • Note that mass number (A) is unchanged and atomic number (Z) goes up by 1. • This is because it is caused by a neutron that breaks apart into a proton and electron (electron is emitted). Other Types of Nuclear Reactions Positron (0+1b): a positive electron 207 Electron capture: the capture of an electron 207 Gamma Ray • HIGH-ENERGY photon (light wave) • Same family as X-rays and light • MORE energetic and harmful • Damaging to living cells • Slows down energy by transferring it to cell components Artificial Nuclear Reactions New elements or new isotopes of known elements are produced by bombarding an atom with a subatomic particle such as a proton or neutron -- or even a much heavier particle such as 4He and 11B. Reactions using neutrons are called reactions because a ray is usually emitted. Radioisotopes used in medicine are often made by reactions. Artificial Nuclear Reactions Example of a reaction is production of radioactive 31P for use in studies of P uptake in the body. 31 P 15 + 1 n 0 ---> 32 P 15 + Transuranium Elements Elements beyond 92 (transuranium) made starting with an reaction 238 U 92 + 239 U 92 239 Np 93 1 n 0 ---> 239 U 92 + ---> 239 Np 93 + 0-1b ---> 239 Pu 94 + 0 b -1 Nuclear Fission Nuclear Fission • Fission is the splitting of atoms • Controlled reaction • These are usually very large, so that they are not as stable • Nuclear Power stations use heat released by nuclear reaction (nuclear fission) to boil water to make steam Fission Process - MODEL Nuclear Fission & POWER • Currently about 103 nuclear power plants in the U.S. and about 435 worldwide. • 17% of the world’s energy comes from nuclear. Diagram of a nuclear power plant Nuclear Explosion • Explosion occurs when reaction is allowed to run out of control • Large amounts of ENERGY released QUICKLY • WATCH: • Nuclear reactor controls rate of energy release • Uranium oxide held in fuel rods • Rods lowered into reactor core • Coolant (CO2) circulated to remove heat • Control rods in core absorb neutrons and control rate of chain reaction • Raised to speed up; lowered to slow down Nuclear Fusion Fusion small nuclei combine 2H 1 + 3H 1 4He 2 + 1n + 0 Occurs in the sun and other stars Energy Nuclear Fusion Fusion • Excessive heat can not be contained • Attempts at “cold” fusion have FAILED. • “Hot” fusion is difficult to contain Half-Life • HALF-LIFE is the time that it takes for 1/2 a sample to decompose. • The rate of a nuclear transformation depends only on the “reactant” concentration. Half-Life Decay of 20.0 mg of 15O. What remains after 3 halflives? After 5 half-lives? Kinetics of Radioactive Decay For each duration (half-life), one half of the substance decomposes. For example: Ra-234 has a half-life of 3.6 days If you start with 50 grams of Ra-234 After 3.6 days > 25 grams After 7.2 days > 12.5 grams After 10.8 days > 6.25 grams Learning Check! The half life of I-123 is 13 hr. How much of a 64 mg sample of I-123 is left after 39 hours? Effects of Radiation Geiger Counter • Used to detect radioactive substances Radiocarbon Dating Radioactive C-14 is formed in the upper atmosphere by nuclear reactions initiated by neutrons in cosmic radiation 14N + 1 n ---> 14C + 1H o The C-14 is oxidized to CO2, which circulates through the biosphere. When a plant dies, the C-14 is not replenished. But the C-14 continues to decay with t1/2 = 5730 years. Activity of a sample can be used to date the sample. Nuclear Medicine: Imaging Thyroid imaging using Tc-99m Food Irradiation •Food can be irradiated with rays from 60Co or 137Cs. •Irradiated milk has a shelf life of 3 mo. without refrigeration. •USDA has approved irradiation of meats and eggs.