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Notes – Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

Notes – Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

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Notes – Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure. Earth’s composition. Atmosphere : Gaseous part of earth. Provides nitrogen, oxygen, neon, argon, water vapor, and carbon dioxide. Earth’s composition. - PowerPoint PPT Presentation

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Page 1: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

Notes – Unit 2 Section B /

Chapter 5Earth’s Mineral

Resources / Electron structure

Page 2: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

Earth’s composition

1) Atmosphere: Gaseous part of earth. Provides nitrogen, oxygen, neon, argon, water vapor, and carbon dioxide

Page 3: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

Earth’s composition

1) Atmosphere: Gaseous part of earth. Provides nitrogen, oxygen, neon, argon, water vapor, and carbon dioxide

2) Hydrosphere: Liquid portion composed of water and dissolved minerals and salts.

Page 4: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

Earth’s composition

1) Atmosphere: Gaseous part of earth. Provides nitrogen, oxygen, neon, argon, water vapor, and carbon dioxide

2) Hydrosphere: Liquid portion composed of water and dissolved minerals and salts.

Page 5: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

Earth’s composition1) Atmosphere: Gaseous part of

earth. Provides nitrogen, oxygen, neon, argon, water vapor, and carbon dioxide

2) Hydrosphere: Liquid portion composed of water and dissolved minerals and salts.

3) Lithosphere: solid part of earth. Greatest variety of chemical resources. Includes petroleum and metal-bearing ores.

Page 6: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

Earth’s composition

3) Lithosphere: solid part of earth. Greatest variety of chemical resources. Includes petroleum and metal-bearing ores.

Page 7: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

Earth’s composition

3) Lithosphere: solid part of earth. Greatest variety of chemical resources. Includes petroleum and metal-bearing ores.

Ore – Naturally occurring rock or mineral that can be mined

Page 8: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

Earth’s composition

3) Lithosphere: Includes petroleum and metal-bearing ores.

Ore – Naturally occurring rock or mineral that can be mined.

Minerals -

Page 9: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

Earth’s composition

3) Lithosphere: Includes petroleum and metal-bearing ores.

Ore – Naturally occurring rock or mineral that can be mined.

Minerals – Naturally occurring solid compounds containing elements or groups of elements

Page 10: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

Earth’s composition

3) Lithosphere: Includes petroleum and metal-bearing ores.

Ore – Naturally occurring rock or mineral that can be mined.

Minerals – Naturally occurring solid compounds containing elements or groups of elements

Granite – Rock (Ore)

Quartz - mineral

Page 11: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure
Page 12: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

Metals, Nonmetals and reactivity

• Metals are not generally found in their pure state.

• They react and combine with other elements to form ionic and covalent compounds.

• Their reactivity depends on their chemical families and properties

Page 13: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

Types of Atomic particles

• Atoms - The building blocks of matter.

• Particles –Electrons (-) e-

Protons (+) p+

Neutrons (no charge) no• Nucleus Protons and neutrons

Page 14: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure
Page 15: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure
Page 16: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

Atomic Particles

• Sodium =Atomic Mass =

Mass

# = - #(rounded) mass =

p+ =e- =no =

• Chlorine =Atomic Mass =

Mass

# = - #(rounded) mass =

p+ =e- =no =

Page 17: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

Atomic Particles

• Sodium = Na Atomic Mass = 22.99

Mass 23

# = 11 - # 11(rounded) mass = 23

p+ = 11e- = 11no = 12

• Chlorine =Atomic Mass =

Mass

# = - #(rounded) mass =

p+ =e- =no =

Page 18: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure
Page 19: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

Atomic Particles

• Sodium = Na Atomic Mass = 22.99

Mass 23

# = 11 - # 11(rounded) mass = 23

p+ = 11+e- = 11-no = 120

• Chlorine = ClAtomic Mass = 35 .453

Mass 35

# = 17 - # 17(rounded) mass = 35

p+ = 17+e- = 17-no = 180

Page 20: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

Electrons

Electrons – Negatively charged particles orbiting the nucleusPeriods – Show the number of electron shells or orbitals. Horizontal columns.Families – Vertical columns. Show the number of outside electrons.

Page 21: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

Electrons

Electrons – Negatively charged particles orbiting the nucleusPeriods – Show the number of electron shells or orbitals. Horizontal columns.Families – Vertical columns. Show the number of outside electrons.

Page 22: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure
Page 23: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

1

23 4 5 6 7

8

1

2

3

4

5

6

7

Valence electrons

Periods

Page 24: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

Electrons

Valence Electrons – The electrons found in the outside energy levelThe number of valence electrons determines many properties of that elementThe number of valence electrons make up families

Valence electrons

Page 25: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

Electrons

Valence Electrons – The electrons found in the outside energy levelThe number of valence electrons determines many properties of that elementThe number of valence electrons make up families

Valence electrons

Page 26: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

Honors ChemChapter 5

Electrons in Atoms

Page 27: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

Atomic models• Dalton – 1st Atom – no internal

structures

• Thomson – Plum pudding, electrons in sphere of positive

• Rutherford - small dense positive nucleus with electrons around nucleus

• Bohr – electrons in circular orbitals with fixed distances from nucleus. Lowest energy inside highest energy furthest from nucleus

Page 28: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

Atomic models

• Schrodinger – mathematical equation for location. Electron cloud model

• Quantum Mechanical model – modern description from Schrodinger’s mathematical equations

Page 29: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

Atomic models

• Schrodinger – mathematical equation for location. Electron cloud model

• Quantum Mechanical model – modern description from Schrodinger’s mathematical equations

Page 30: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

Electron configuration

• Quantum – the amount of energy required to move an electron from its present energy level to the next higher one

• Energy levels – region in space around nucleus where an electron is likely moving

Page 31: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

Electron configuration• Quantum – the amount of

energy required to move an electron from its present energy level to the next higher one

• Energy levels – region in space around nucleus where an electron is likely moving

• Energy levels are labeled by principle quantum numbers (n).

• n = 1,2,3,4, etc

Electron configuration

Page 32: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

Electron configuration• Quantum – the amount of

energy required to move an electron from its present energy level to the next higher one

• Energy levels – region in space around nucleus where an electron is likely moving

• Energy levels are labeled by principle quantum numbers (n).

• n = 1,2,3,4, etc• The higher the energy level

occupied by an electron, the more energetic it is

Page 33: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

Electron configuration

• Energy levels are labeled by principle quantum numbers (n).

• n = 1,2,3,4, etc• The quantum # equals the

number of sublevels for each principle energy level

• The formula 2n2 equals the maximum number of electrons allowed in a principle energy level

• Shell n 2n2

• K 1 2(1)2=• L 2 2(2)2=• M 3 2(3)2=• N 4 2(4)2=

Page 34: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

Energy levels

• Energy levels are labeled by principle quantum numbers (n).

• n = 1,2,3,4, etc• The quantum # equals the

number of sublevels for each principle energy level

• The formula 2n2 equals the maximum number of electrons allowed in a principle energy level

• Shell n 2n2

• K 1 2(1)2=• L 2 2(2)2=• M 3 2(3)2=• N 4 2(4)2=

Page 35: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

Electrons

• Electrons are found in orbitals or shells

• The electrons with the highest energy are on the outside shell.

• The electrons with the lowest energy are on the inside

Page 36: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

Electrons

• Each shell can only hold a certain amount of electrons

• The electrons with the highest energy are on the outside shell.

• The electrons with the lowest energy are on the inside

Page 37: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure
Page 38: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

# of electrons in orbitals

ShellK

LMN

n 2n2

1234

Page 39: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

# of electrons in orbitals

ShellK

LMN

n 2n2

1 2234

Page 40: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

# of electrons in orbitals

ShellK

LMN

n 2n2

1 22 834

Page 41: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

# of electrons in orbitals

ShellK

LMN

n 2n2

1 22 83 184

Page 42: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

# of electrons in orbitals

ShellK

LMN

n 2n2

1 22 83 184 32

Page 43: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

# of electrons in orbitals

ShellK

LMN

n 2n2

1 22 83 18 (8)4 32 (8)

Page 44: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

Electron shells

• Electrons fill from the inside out

• The first shell has 2, the second shell has 8, the third shell has 18(8)

• Octet rule – The maximum number of electrons in the outside shell is 8. The exception is shell # 1 with 2.

Page 45: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

Electron shells

• The atomic number of an element tells the number of protons and electrons

• Electrons are drawn in shells in pairs from inside out.

• The outside are valence electrons

Page 46: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure
Page 47: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

Valence electrons

Page 48: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure
Page 49: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

1

23 4 5 6 7

8

Page 50: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure
Page 51: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

Electron shells

• The atomic number of an element tells the number of protons and electrons

• Electrons are drawn in shells in pairs from inside out.

• The outside are valence electrons

N

Atomic # = 7 1st = 2Period = 2 2nd = 8

3rd = 8

Page 52: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

Electron shells

• The atomic number of an element tells the number of protons and electrons

• Electrons are drawn in shells in pairs from inside out.

• The outside are valence electrons

S

Atomic # = 16 1st = 2Period = 3 2nd = 8

3rd = 8

Page 53: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

1

23 4 5 6 7

8

Page 54: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

Electron dot diagram

• Shows each element with its valence electrons only

• Outside electrons are placed in pairs

• Dots show outside electrons

S

Page 55: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

Electron dot diagram

• Shows each element with its valence electrons only

• Outside electrons are placed in pairs

• Dots show outside electrons

• Elements will lose or gain e- to become stable and reach the octet (8 or 0)

Page 56: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

Electron dot diagram• Shows each element with its valence

electrons only• Outside electrons are placed in pairs• Dots show outside electrons

• Elements will lose or gain e- to become stable and reach the octet (8 or 0)

Elements that lose e- become positive , those that gain e-

become negative

Li =

C =

O =

Page 57: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

1

23 4 5 6 7

8

Page 58: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

Electron dot diagram• Shows each element with its valence

electrons only• Outside electrons are placed in pairs• Dots show outside electrons• Elements will lose or gain e- to become

stable and reach the octet (8 or 0)

Elements that lose e- become positive charged , those that

gain e- become negative charged

• Dots are placed R-L-T-B and then repeat pattern in pairs

Al =

N =

Cl =

Ar =

Page 59: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

Electron dot diagram• Shows each element with its valence

electrons only• Outside electrons are placed in pairs• Dots show outside electrons• Elements will lose or gain e- to become

stable and reach the octet (8 or 0)

Elements that lose e- become positive charged , those that

gain e- become negative charged

• Dots are placed R-L-T-B and then repeat pattern in pairs

Al = lose/gain _____ charge = ___

N = lose/gain _____ charge = ___

Cl = lose/gain _____ charge = ___

Ar = lose/gain _____ charge = ___

Page 60: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

Electron dot diagram

• Shows each element with its valence electrons only

• Outside electrons are placed in pairs

• Dots show outside electrons

S

Page 61: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

Electrons and Periodic Table

• Valence electrons in atoms show reactivity

• Atoms will lose or gain electrons to reach the octet (8) rule level.

• Inert (Noble) Gases have 8 valence electrons (2 for He) and are stable

Page 62: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

Electrons and Periodic Table

• Inert (Noble) Gases have 8 valence electrons (2 for He) and are stable

• Nonmetals –Groups 5a to 7a will gain electrons to become stable

• Metals – Groups 1a to 3a will lose electrons to become stable

Page 63: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

Electrons and Periodic Table

• Inert (Noble) Gases have 8 valence electrons (2 for He) and are stable

• Nonmetals –Groups 5a to 7a will gain electrons to become stable

• Metals – Groups 1a to 3a will lose electrons to become stable

Page 64: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

Orbitals

• Atomic orbitals – regions around the nucleus within which the electrons have the highest probability of being found

• Orbitals are sublevels which correspond to different shapes.

• s are spherical, p are dumbell shaped, etc

Page 65: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

• Sublevel orbitals can contain differing numbers of orbitals.

• s = 1 orbital• p = 3 orbitals• d = 5 orbitals• f = 7 orbitals

Page 66: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

Electron Arrangements in Atoms

Electron configuration – The ways in which electrons are arranged around the nuclei of atoms3 Rules:•1) Aufbau principle – electrons enter orbitals of the lowest energy first•2) Pauli exclusion principle

Page 67: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

Electron Arrangements in Atoms

Electron configuration – The ways in which electrons are arranged around the nuclei of atoms3 Rules:•1) Aufbau principle – electrons enter orbitals of the lowest energy first•2) Pauli exclusion principle

Page 68: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

Electron Arrangements in Atoms3 Rules:•2) Pauli exclusion principle – atomic orbitals can hold no more than two electrons•3) Hund’s rule – When electrons occupy orbitals of equal energy, one electron enters each orbital until all the orbitals contain one electron with parallel spins.

Page 69: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

Calculating Electron Configurations

• The shorthand method for writing electron configurations of an atom involves writing the energy level and symbol for every sublevel occupied by an electron and indicating the number of electrons in each sublevel with a subscript

Page 70: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

Calculating Electron Configurations

• The shorthand method for writing electron configurations of an atom involves writing the energy level and symbol for every sublevel occupied by an electron and indicating the number of electrons in each sublevel with a subscript.

Page 71: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

Calculating Electron Configurations• The shorthand method for

writing electron configurations of an atom involves writing the energy level and symbol for every sublevel occupied by an electron and indicating the number of electrons in each sublevel with a subscript.

• Nitrogen – Atomic # 7• Shorthand = 1s22s22p3

Page 72: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

• Write the electron configuration for Phosphorus,

• atomic # 15

Calculating Electron Configurations

Page 73: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

Write the electron configuration for Phosphorus, atomic # 1515 e-

Calculating Electron Configurations

Page 74: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

Write the electron configuration for Phosphorus, atomic # 1515 e-

Calculating Electron ConfigurationsConfiguration = 1s22s22p63s23p3 = 15 electrons

Page 75: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

• Write the electron configuration for Carbon, Argon, and Nickel

Calculating Electron Configurations

Page 76: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

• Write the electron configuration for Carbon (6), Argon (18), and Nickel(28)

Calculating Electron Configurations

Page 77: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

Write the electron configuration for Carbon, atomic # 66e-

Calculating Electron Configurations

Page 78: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

Write the electron configuration for Argon, atomic # 1818e-

Calculating Electron Configurations

Page 79: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

Write the electron configuration for Nickel, atomic # 2828e-

Calculating Electron Configurations

Page 80: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

Physics and the Quantum Mechanical Model

• Quantum mechanical model grew out of the study of Light

• Light consists of waves and particles

• Wave principles:• Amplitude = wave

height• Wavelength ( ) =

distance between crests

Page 81: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

Physics and the Quantum Mechanical Model

• Quantum mechanical model grew out of the study of Light

• Light consists of waves and particles

• Wave principles:• Amplitude = wave

height• Wavelength ( ) =

distance between crests

Page 82: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

Physics and the Quantum Mechanical Model

• Wave principles:• Amplitude = wave height• Wavelength ( ) = distance

between crests• Frequency ( ) = wave

cycles past a given point per unit time– Cycles/second = hertz (Hz) s-1

• Speed of light constant

Page 83: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

Physics and the Quantum Mechanical Model

• Wave principles:• Amplitude = wave height• Wavelength ( ) = distance

between crests

• Frequency ( ) = wave cycles past a given point per unit time– Cycles/second =

hertz (Hz) s-1

• Speed of light constant

Page 84: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

Physics and the Quantum Mechanical Model

• Frequency ( ) = wave cycles past a given point per unit time– Cycles/second = hertz

(Hz) s-1

• Speed of light constant

Page 85: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

Physics and the Quantum Mechanical Model

• Speed of light constant

C = 2.988 x 108 meters/second• (186,000 miles/second)

Page 86: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

Physics and the Quantum Mechanical Model

• Speed of light constant

C = 2.988 x 108 meters/second• (186,000 miles/second)• Wavelength and frequency are

inversely proportional

– High = Low– Low = High

• All electromagnetic waves travel at same speed = 3.0 x 108 m/s

Page 87: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

Physics and the Quantum Mechanical Model

• Wavelength and frequency are inversely proportional

– High = Low– Low = High

• All electromagnetic waves travel at same speed = 3.0 x 108 m/s

• Light = Quanta of energy calledPhotons

• Atomic Spectra – When atoms absorb energy, electrons move into higher energy levels. These electrons than lose energy by emitting light.

High

High Low

Low

Page 88: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

Physics and the Quantum Mechanical Model

• Wavelength and frequency are inversely proportional

– High = Low– Low = High

• All electromagnetic waves travel at same speed = 3.0 x 108 m/s

• Light = Quanta of energy calledPhotons

• Atomic Spectra – When atoms absorb energy, electrons move into higher energy levels. These electrons than lose energy by emitting light.

Page 89: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

Physics and the Quantum Mechanical Model

• Wavelength and frequency are inversely proportional

– High = Low– Low = High

• All electromagnetic waves travel at same speed = 3.0 x 108 m/s

• Light = Quanta of energy calledPhotons

• Atomic Spectra – When atoms absorb energy, electrons move into higher energy levels. These electrons than lose energy by emitting light.

Page 90: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

Physics and the Quantum Mechanical Model

• Wavelength and frequency are inversely proportional

– High = Low– Low = High

• All electromagnetic waves travel at same speed = 3.0 x 108 m/s

• Light = Quanta of energy calledPhotons

• Atomic Spectra – When atoms absorb energy, electrons move into higher energy levels. These electrons than lose energy by emitting light.

Page 91: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

Physics and the Quantum Mechanical Model

• Wavelength and frequency are inversely proportional

– High = Low– Low = High

• All electromagnetic waves travel at same speed = 3.0 x 108 m/s

• Light = Quanta of energy calledPhotons

• Atomic Spectra – When atoms absorb energy, electrons move into higher energy levels. These electrons than lose energy by emitting light.

Page 92: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

Chemical Bonds – Chemical forces which hold atoms together and form complete

electrons shellsIon – is an atom or group of

atoms that have an electric charge.Atoms become charged when they lose or gain electrons to become stableAtoms which lose electrons become positive (+) Atoms which gain electrons become negative (-)

Page 93: Notes –  Unit 2 Section B / Chapter 5 Earth’s Mineral Resources / Electron structure

Chemical Bonds – Chemical forces which hold atoms together and form complete

electrons shells• Ionic Bond – Positive (+) and

negative (-) ions attract – formed by the transfer of valence electrons.Na 11p+ 11p+

11e- 10e- = +1 Na

Cl 17p+ 17p+17e- 18e- = -1 Cl

Na +1 + Cl-1 = NaCl o