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Chapter 4:
Structure of the Atom
4.1 Early theories and 4.2 Defining the atom
Historical Background:
Models of the Atom: -see reference chart (On Pg. 10 of your packet)
4.1 Early theories and 4.2 Defining the atom
Models of the Atom Date scientist discovery________________ 100 BC Democritus/Greeks concept of the atom 1770 Antoine Lavosier Law of conservation of mass 1800 Joseph Proust Law of definite proportions 1803 John Dalton Law of multiple proportions Atomic Model I 1880 William Crookes Cathode Rays (electrons) 1885 Goldstein Canal Rays (protons) 1900 J.J. Thomson Plum Pudding Model
Electron Atomic Model II
1909 Ernest Rutherford nucleus of atom Atomic Model III 1913 Niels Bohr Planetary Model Atomic Model IV 1920- Schroedinger/Planck/ Modern or Wave Model Present DeBroglie/Einstein/etc. Atomic Model V
4.1 Early theories and 4.2 Defining the atom 1. Atomists and Democritus
Greeks approx 2,500 years ago Matter was made up of atoms “atomos” or
“Indivisible” particles Seashell experiment—broken into smaller &
smaller pieces
4.1 Early theories and 4.2 Defining the atom 2. John Dalton
1766-1844; returned to theory of atoms Atoms are like billiard balls (solid spheres)
which cannot be broken down further 4 major postulates
1) All elements are composed of atoms 2) Atoms of the same element are identical 3) Atoms can physically mix or chemically combine
in simple whole number ratios 4) Reactions occur when atoms separate, join, or
rearrange
4.1 Early theories and 4.2 Defining the atom 3. William Crookes
developed Crookes tube (CRT) in 1870’s first evidence for existence of electrons
because you could “see” electrons flow and confirm their existence.
tube is precursor to today’s TV picture tubes
4.1 Early theories and 4.2 Defining the atom 4. J.J. Thomson
discovered electron in 1897 discovered positively charged particles
surrounded by electrons found the ratio of the charge of an electron to
its mass to be 1/1837
4.1 Early theories and 4.2 Defining the atom 4. J.J. Thomson
4.1 Early theories and 4.2 Defining the atom 4. J.J. Thomson
cathode ray tube experiments – advancement of Crookes tube
“plum-pudding model”
4.1 Early theories and 4.2 Defining the atom 5. Ernest Rutherford
Discovered nucleus (dense core of atom) in 1911
Gold foil experiments
Quote from E.R.’s Lab Notebook “It is about as incredible as if you had fired a
15-inch shell at a piece of tissue paper and it came back and hit you.” -ER
4.1 Early theories and 4.2 Defining the atom
Video Clip: Rutherford Gold Foil Experiment
4.1 Early theories and 4.2 Defining the atom 6. Robert Milliken
Oil drop experiment determined the charge and mass of an
electron
Video Clip: Milliken Oil Drop Experiment
4.1 Early theories and 4.2 Defining the atom 7. James Chadwick
discovered the neutron (no charge, but same mass as proton)
Neutrons help disperse the strong repulsion of positive charges
Relative Sizes Nucleus diameter = 10-5 nm Atom diameter = 10-1 nm Nucleus = basketball --> Atom = 6
miles wide!
4.1 Early theories and 4.2 Defining the atom 8. Niels Bohr
improved on Rutherford’s work “planetary model”- positive center is
surrounded by electrons in defined orbits circling the center
4.1 Early theories and 4.2 Defining the atom defined the following:
energy level – the location where an electron is found at a set distance from the nucleus dependent on the amount of energy it has
ground state – the typical energy level where an electron is found; lowest energy
excited state – an energy level higher than the ground state for an electron; temporary condition
4.1 Early theories and 4.2 Defining the atom 9. Quantum Mechanical Model
Erwin Schroedinger; Mathematical model Electron locations are based on probability Electrons are not particles, but waves!
http://phet.colorado.edu/en/simulation/hydrogen-atom
Defined: Orbital – region where an electron is likely to
be found 90% of the time
4.3 How atoms differ
Atoms – vocabulary and classifications
Atom – the smallest particle of matter that retains its properties.
can “see” individual atoms with a scanning tunneling microscope.
4.3 How atoms differ
Subatomic particles – the component parts of an atom: proton, neutron, and electron
4.3 How atoms differ
Ion- atom with the same number of protons but a different number of electrons. If the atom has a (+) charge it has fewer
electrons than protons, If the atom has a (-) charge it has more electrons than protons.
4.3 How atoms differSubatomic
ParticleMass and Abbreviation Charge Location Discoverer
Proton 1 amu, p+ +1 Nucleus None
Neutron 1 amu, n 0 Nucleus Chadwick in 1932
Electron Almost zero, e- -1 Electron cloud
Thomson
4.3 How atoms differ Calculations involving Subatomic
Particles:
atomic number = # of protons mass number = # of protons + # of neutrons (neutral atom): # of protons = # of electrons (charged ion): charge = #p+ - #e-
4.3 How atoms differ Isotopes and Calculations:
Isotope – atoms of the same element with different numbers of neutrons
Atomic mass – weighted average of the masses of all the isotopes of an element
4.3 How atoms differ Isotope (Isotopic Notation)
Mass #
Atomic #
Atomic Symbol
Z
AX
Example: Uranium-238
4.3 How atoms differ Isotope Problems:
Multiply the mass number of the isotope by the decimal value of the percent for that isotope
Add the relative masses of all of the isotopes to get the atomic mass of the element
4.3 How atoms differ Example:
If 90% of the Beryllium in the world has a mass number of 9 and only 10% has a mass number of 10, what is the atomic mass of Beryllium?
4.4 Unstable Nuclei and Radioactive Decay
Vocabulary
Radioactivity-the spontaneous emission of radiation from substances
Nuclear reactions- changes in an atom’s nucleus
Radiation-rays and/or particles emitted from radioactive material
4.4 Unstable Nuclei and Radioactive Decay
Types of Radiation
Alpha radiation -stream of high energy alpha particles
alpha particles consist of 2 protons and 2 neutrons and are identical to helium-4 nucleus.
symbol 4He 2+
2
not much penetrating power, travel a few centimeters, stopped by paper, no health hazard
4.4 Unstable Nuclei and Radioactive Decay
mass number decreases by 4 atomic number by 2
alpha decay: 226 Ra 222Ra + 4 He 88 86 2
Example: Uranium-238
4.4 Unstable Nuclei and Radioactive Decay
Beta radiation high speed electrons
To form beta radiation a neutron splits into a proton and an electron
The proton stays in nucleus and the electron propels out at high speed.
Symbol 0e- 0e- 0B
-1 -1 -1
100 times more penetrating then alpha, pass through clothing to damage skin
4.4 Unstable Nuclei and Radioactive Decay
Beta decay: 131I 131 Xe + 0B 53 54 -1
Example: Astatine-220
4.4 Unstable Nuclei and Radioactive Decay
Gamma radiation similar to X rays doesn’t consist of particles
symbol: 0 0
penetrates deeply into solid material, body tissue, stopped by Pb or concrete, dangerous
usually emitted with alpha and beta radiation no mass or electrical charge emission of gamma rays by themselves cannot
result in the formation of a new atom
4.4 Unstable Nuclei and Radioactive Decay
Practice:
What is the alpha decay of plutonium-250?
4.4 Unstable Nuclei and Radioactive Decay
2. What is the beta decay of Carbon-14?
4.1 Early theories and 4.2 Defining the atom
Models of the Atom Date scientist discovery________________ 100 BC Democritus/Greeks concept of the atom 1770 Antoine Lavosier Law of conservation of mass 1800 Joseph Proust Law of definite proportions 1803 John Dalton Law of multiple proportions Atomic Model I 1880 William Crookes Cathode Rays (electrons) 1885 Goldstein Canal Rays (protons) 1900 J.J. Thomson Plum Pudding Model
Electron Atomic Model II
1909 Ernest Rutherford nucleus of atom Atomic Model III 1913 Niels Bohr Planetary Model Atomic Model IV 1920- Schroedinger/Planck/ Modern or Wave Model Present DeBroglie/Einstein/etc. Atomic Model V
End of Chapter 4!