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8.2 The Chemical Earth

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Title: 8.2 The Chemical Earth


1
8.2 The Chemical Earth
  • Focus 1
  • The living and non-living components of the Earth
    contain mixtures

2
Balancing Chemical Equations
  • Write the unbalanced equation.
  • Chemical formulas of reactants are listed on the
    left-hand side of the equation.
  • Products are listed on the right-hand side of the
    equation.
  • Reactants and products are separated by putting
    an arrow between them to show the direction of
    the reaction. Reactions at equilibrium will have
    arrows facing both directions.
  • Balance the equation.
  • Apply the Law of Conservation of Mass to get the
    same number of atoms of every element on each
    side of the equation. Tip Start by balancing an
    element that appears in only one reactant and
    product.
  • Once one element is balanced, proceed to balance
    another, and another, until all elements are
    balanced.
  • Balance chemical formulas by placing coefficients
    in front of them. Do not add subscripts, because
    this will change the formulas.
  • Indicate the states of matter of the reactants
    and products.
  • Use (g) for gaseous substances.
  • Use (s) for solids.
  • Use (l) for liquids.
  • Use (aq) for species in solution in water.
  • Write the state of matter immediately following
    the formula of the substance it describes.
  • Source http//chemistry.about.com

3
Balancing Chemical Equations
  • Try these examples
  • 1)Mg O2 ? MgO
  • 2)Zn HCl ? ZnCl2 H2
  • 3)CaCO3 ? CaO CO2

4
Balancing Chemical Equations
  • 1)2Mg O2 ? 2MgO Balanced
  • 2)Zn 2HCl ? ZnCl2 H2 Balanced
  • 3)CaCO3 ? CaO CO2 Balanced

5
Elements, Compounds and Mixtures
  • -Elements are made of one type of atom and cannot
    be broken down into simpler substances. Examples
    Iron(Fe), Oxygen(O2)
  • -Compounds are pure, homogeneous substances that
    can be broken down into simpler substances, are
    made of two or more elements and always have
    elements in the same ratio by mass. Examples
    table salt (NaCl), pure water (H2O)
  • -Mixtures contain two or more pure substances
    that are sometimes heterogeneous and can be
    separated by physical means such as filtering,
    boiling or the use of a magnet. Examples iron
    filings in sand, sugar dissolved in water

6
The Spheres of the Earth
  • The names of the four spheres are derived from
    the Greek words for stone (litho), air (atmo),
    water (hydro), and life (bio).
  • Lithosphere
  • The lithosphere is the solid, rocky crust
    covering entire planet. This crust is inorganic
    and is composed of minerals. It covers the entire
    surface of the earth from the top of Mount
    Everest to the bottom of the Mariana Trench.
  • Hydrosphere
  • The hydrosphere is composed of all of the water
    on or near the earth. This includes the oceans,
    rivers, lakes, and even the moisture in the air.
    Ninety-seven percent of the earth's water is in
    the oceans. The remaining three percent is fresh
    water three-quarters of the fresh water is solid
    and exists in ice sheets
  • Biosphere
  • The biosphere is composed of all living
    organisms. Plants, animals, and one-celled
    organisms are all part of the biosphere. Most of
    the planet's life is found from three meters
    below the ground to thirty meters above it and in
    the top 200 meters of the oceans and seas.
  • Atmosphere
  • The atmosphere is the body of air which surrounds
    our planet. Most of our atmosphere is located
    close to the earth's surface where it is most
    dense. The air of our planet is 79 nitrogen and
    just under 21 oxygen the small amount remaining
    is composed of carbon dioxide and other gasses.
  • Source http//geography.about.com/od/physicalgeog
    raphy/a/fourspheres.htm

7
The Spheres of the Earth
  • Mixtures in the Lithosphere
  • -Rocks-mixtures of silicates, metals and other
    minerals
  • -Sand-mixture of silicon dioxide and shells
  • -Soils-mixture of clays, metals, sand,
    decomposing matter
  • -Mineral ores-oxides, sulfides, carbonates,
    sulfates and chlorides of metals
  • -Coal, oil and natural gas-mixtures of carbon
    compounds
  • Mixtures in the Hydrosphere
  • -Sea water- mixture of water and various salts
    such as sodium, magnesium and calcium chlorides,
    and other halides and sulfates
  • -Ground water- mixture of water and dissolved
    chlorides and sulfates and suspended minerals
  • -Dissolved gases- nitrogen, oxygen and carbon
    dioxide

Mixtures in the Biosphere -Blood-mixture of
plasma, red and white cells -Animals, plants,
bacteria-contain mixtures of carbon compounds
(carbohydrates, proteins, fats and
vitamins) -Water with dissolved
minerals -Dissolved gases-oxygen, nitrogen, and
carbon dioxide
Mixtures in the Atmosphere -Mixture of gases-
elements of nitrogen, oxygen, argon and a small
amount of other gaseous compounds such as water,
carbon dioxide, carbon monoxide, sulfur dioxide
and nitrogen dioxide
8
Separation of Mixtures
  • Sieve
  • To separate solids of different sizes
  • Filtration
  • To separate solids and liquids/solutions

9
Separation of Mixtures
  • Evaporation (to dryness)
  • To separate dissolved solids in liquids
  • Distillation
  • To separate liquids from solutions (purification)

10
Separation of Mixtures
  • Separating Funnel
  • To separate two immiscible liquids and for
    solvent extraction. This technique makes use of a
    difference in densities
  • Separation by solubility
  • To separate mixtures of solids.
  • One solid is soluble in a solvent and the others
    are not
  • The insoluble components are removed by
    filtration
  • Evaporation is used to recover the pure dissolved
    substance (solute)

11
Separation of Mixtures
  • Liquification and fractional distillation
  • To separate mixtures of gases-gases are cooled to
    liquefy them, followed by fractional
    distillation. Fractional distillation allows for
    separation of substances with similar boiling
    points.
  • Other methods to separate gases would make use of
    differences in solubility in liquids such as
    water.

12
Separation of Mixtures
  • Chromatography
  • is the separation of mixtures by selective
    adsorption (absorbing onto the surface) onto a
    stationary phase. This technique is used to sort
    a mixture out into its separate components.
  • There are several types for various mixtures and
    they include
  • Column chromatography
  • Paper chromatography
  • Thin layer chromatography
  • Gas chromatography (GC)
  • All techniques make use of an inert substance
    such as alumina, silica or paper. The components
    of a mixture adhere to the inert substance with
    different strengths, which leads to separation.

13
Separation of Mixtures
  • Paper chromatography
  • This is the simplest form of chromatography.
  • The stationary phase is a special chromatography
    paper, but often filter paper is used in schools.
  • The mobile phase is a solvent mixture, e.g. water
    and ethanol.
  • The mixture under analysis is placed in a tiny,
    concentrated dot near the bottom of the paper.
  • The paper is hung with the bottom dipped in
    solvent, which rises up the paper to come in
    contact with the mixture.
  • As the solvent rises further up the paper, the
    components are separated as they are swept along.
  • The strip of paper is called a chromatogram.
  • Identification of the components is based on Rf
    values a ratio between the distance travelled
    by the component to the distance travelled by the
    solvent front.

Solvent Front
Starting line
14
Separation of Mixtures
  • Gas chromatography (GC) uses a stationary phase
    and a mobile phase. The mobile phase is a carrier
    gas and the stationary phase may be a liquid or a
    solid. GC is a very rapid, highly sensitive and
    reliable form of analysis, but is limited to
    compounds that can be vaporised without
    decomposing. Low-molecular-weight organic
    compounds are ideal for this sort of analysis.
    The diagram on the right shows a typical
    chromatogram.

15
Separation of Mixtures-summary of techniques
Separation Method Property used to achieve separation
Sieving Particle size
Filtration One substance is solid, the other is liquid or solution
Evaporation Liquid has a much lower boiling point than the solid
Distillation Large difference in boiling point
Fractional Distillation Smaller difference in boiling point
Separating Funnel Density (m/vol) of immiscible liquids
Adding a solvent then filtration One substance is soluble in a solvent and the others are not
Chromatography Different adsorption to a stationary phase
16
Separation of Mixtures-examples
Separation Method Example of use
Sieving To separate sand from gravel at a rock quarry
Filtration Drinking water purification processes
Evaporation Salt evaporation ponds for table salt
Distillation Obtaining pure water from sea water
Fractional Distillation Separation of crude oil components (petrol, diesel, kerosene, waxes, etc.)
Separating Funnel To remove oil from water, solvent extraction in analytical testing (e.g. pesticides)
Adding a solvent then filtration Removal of salt from sand with water
Chromatography Analytical testing (e.g. water contaminants)
17
Chemical Analysis
  • Two general types
  • Qualitative Analysis
  • to determine what substances are present in a
    sample
  • Quantitative Analysis
  • to determine how much of each substance there is
    in a sample

18
Percentage composition
  • Quantitative Analysis of a substance involves the
    determination of actual percentages present in a
    sample.
  • This involves either
  • Volumetric analysis-involves measuring
    percentages by volume.
  • Gravimetric analysis-involves measuring
    percentages by mass/weight.
  • In either case, the calculations will be similar

19
Gravimetric Analysis
  • There are a variety of reasons for determining
    the composition of a substance in a mixture
    including
  • Determining the amount of pollutants present in
    drinking water.
  • Determining the amount of a metal present in an
    ore sample.
  • Quality control in the production of a variety of
    consumer goods. (e.g. ensuring the correct
    quantities of N, P, and K in fertilisers)
  • Soil testing to determine suitability for
    plant/crop growth.

20
Gravimetric Analysis
  • Gravimetric analysis involves the use of a
    variety of separation techniques, followed by a
    simple calculation to determine the percentage
    composition of a substance.
  • For example
  • A sample of ore weighing 10.63g is found to
    contain 1.55g of nickel (Ni) and 0.76g of cobalt
    (Co). Calculate the composition of Ni and Co.
  • component mass of component in sample x 100
  • total mass of sample
  • Ni 1.55g/10.63g x 100 14.58
  • Co 0.76g/10.63g x 100 7.15

21
Class Assignment
  • Choose a mixture from one of the 4 spheres of the
    Earth and gather information about the following
  • Industrial separation processes to separate the
    mixture
  • The properties of the mixture that are used in
    these separation processes.
  • The products of separation and their uses
  • The issues associated with wastes generated from
    these processes.
  • Present your information in Report Style with
    supporting diagrams, and a source list.

22
8.2 The Chemical Earth
  • Focus 2
  • Although most elements are found in combinations
    on Earth, some elements are found uncombined

23
Properties of the Elements
  • Elements are classified into three categories
    based on their physical properties.
  • The 3 categories are
  • Metals
  • Non-metals
  • Semi-metals or metaloids
  • Some of the physical properties used in this
    classification
  • Density (mass/volume)
  • Boiling point/melting point
  • Electrical and Thermal conductivity
  • State at room temperature (solid, liquid or gas)
  • Appearance

24
The Periodic Table
http//library.tedankara.k12.tr/chemistry/vol1/ato
mstr/trans50.jpg
25
http//www.dayah.com/periodic/Images/periodic20ta
ble.png
26
Properties of the Elements
  • Metals (e.g. Fe, Cu, Mg, Al, Au)
  • solid at room temperature (except Hg) and usually
    dense/hard.
  • usually high melting/boiling points.
  • have a shiny (lustrous) appearance.
  • are malleable (able to be hammered into sheets).
  • are ductile (able to be drawn into wires).
  • are good conductors of heat and electricity.
  • Uses construction materials, utensils,
    electrical wiring, household appliances, drink
    cans, etc.

27
Properties of the Elements
  • Non-metals (e.g. C, S, He, Cl)
  • can be solid liquid or gas at room temperature.
  • usually have relatively low melting/boiling
    points.
  • are usually not lustrous.
  • are usually brittle, not malleable or ductile.
  • Are poor conductors of heat and electricity
    (except for C in the form of graphite).
  • Uses carbon used as an electrode in dry cells
    and is the lead in pencils, sulfur used in
    vulcanising rubber, neon is used in neon signs
    and chlorine is used in bleach and swimming pools
    as well as in the production of plastics such as
    PVC.

28
Properties of the Elements
  • Semi-metals (B, Si, Ge, As, Sb)
  • have properties that are a combination of metal
    and non-metal properties.
  • usually have high melting/boiling points.
  • have variable conductivities depending upon
    temperature, but are usually low.
  • have variable appearance.
  • Uses mixtures of silicon and germanium are used
    as semi-conductors in transistors and computer
    chips. They can be mixed with other elements
    (e.g. As and B) to increase their conductivities.

29
Reactivity of the Elements
  • The elements vary greatly in their reactivity.
    How reactive an element is directly related to
    how the electrons are arranged in the atom
    influencing what form it will take in nature.
  • Some elements are not very reactive and are
    therefore found uncombined in nature. These
    include the noble gases (He, Ne, Ar, Kr, Xe,
    Rn), and the metals Au, Ag, Pt and Cu
    (sometimes).
  • Some elements occur as molecules that contain
    only one type of atom. These are referred to as
    molecular elements. These are also found combined
    with other elements in compounds. These include
    O2, N2, H2, Cl2, I2, P4
  • Most of the elements are reactive and therefore
    occur as compounds in nature. These include
    NaCl, H2SO4, SiO2.

General rule The more reactive an element is,
the less of a chance it will be found uncombined
in nature.
30
8.2 The Chemical Earth
  • Focus 3
  • Elements in Earth materials are present mostly as
    compounds because of interactions at the atomic
    level

31
The particle nature of matter
  • Matter is often described as being made up of
    small particles that are continuously moving and
    interacting. In each of the three states of
    matter (solid, liquid, gas) the particles
    experience vibrational motion. Liquids and gases
    experience translational (movement) motion as
    well. Gases experience more translational motion
    than liquids as they have more energy.

32
The particle nature of matter
  • The primary "particle" in chemistry is the atom.
    Atoms are defined as the smallest particle of an
    element. However, you probably know that there is
    a substructure to an atom that it is made of
    protons, neutrons and electrons. You may also
    know that protons and neutrons are each made of
    three quarks.

33
The particle nature of matter
  • Each element has a distinctive atomic number and
    mass number.
  • The atomic number (Z) corresponds to the number
    of protons in the nucleus.
  • The mass number (A) corresponds to the total
    number of neutrons and protons in the nucleus.

Mathematically A Z number of neutrons
34
Structure of the Atom
  • The particles that make up the elements are
    called atoms. All atoms of one element are the
    same, but they are different from the atoms of
    all other elements. In other words, each element
    has a distinct type of atom with a specific
    number of protons, neutrons and electrons.
  • Protons have a ve charge
  • Electrons have a ve charge
  • Neutrons have no charge

35
Structure of the Atom
  • Protons (p) and neutrons (n) are found in the
    centre of the atom in the nucleus
  • Electrons (e) are found in the surrounding space
    around the nucleus moving randomly in what is
    known as an electron cloud.

Relative mass Relative charge
electron (e) 1/2000 -1
proton (p) 1 1
neutron (n) 1 0
36
Structure of the Atom
  • Isotopes
  • All atoms of the same element have the same
    number of protons in the nucleus, however they do
    not necessarily have the same mass. These atoms
    differ in the number of neutrons and therefore,
    the mass number and are known as isotopes. Some
    well-known isotopes are in the table to the
    right.

Name p n e
Hydrogen 1 0 1
Deuterium 1 1 1
Tritium 1 2 1
Carbon 12 6 6 6
Carbon 13 6 7 6
Carbon 14 6 8 6
Uranium 235 92 143 92
Uranium 238 92 146 92
37
Structure of the Atom
  • The Bohr Model
  • Bohrs model of the atom consists of electrons in
    distinct energy levels or shells. The shells
    closest to the nucleus are the lowest energy
    (n1) and fill first.
  • The maximum number of electrons in each shell can
    be calculated by 2n2.
  • Therefore,
  • n1 maximum of 2 e
  • n2 maximum of 8 e
  • n3 maximum of 18 e
  • and so on
  • The valence shell or outer shell can hold a
    maximum of 8.

38
Structure of the Atom
  • Orbitals
  • Schrödinger used quantum mechanics to describe
    the shape of the clouds within each energy
    level. These are called orbitals and each energy
    level contains an increasing number of orbitals
    to accommodate more electrons. All energy levels
    contain s orbitals, which are spherical (one
    lobe). All but the first energy level contain 3
    p orbitals, which are dumbbell shaped (two
    lobes). After the first two, each energy level
    contains 5 d orbitals, most of which have 4
    lobes. Higher energy levels contain 7 f
    orbitals. Each orbital can accommodate 2
    electrons. Therefore
  • s orbitals hold 2 electrons
  • p orbitals hold 6 electrons
  • d orbitals hold 10 electrons
  • f orbitals hold 14 electrons

Note For Interest Only! You are not required to
learn this information for the HSC
http//webfac1.enmu.edu/longro/www/orbitals/atorb.
htm
39
Structure of the Atom
  • Below is a representation of the relative energy
    levels of electron orbitals and how they appear
    around the nucleus.

Note For Interest Only! You are not required to
learn this information for the HSC
40
Ions loss or gain of e-
  • An atom that loses or gains electrons is called
    an ion.
  • There are two types
  • Cations () have lost electrons, making them
    positively charged (eg Mg2 loss of 2e-)
  • Anions (-) have gained electrons, making them
    negatively charged (eg O2- gain of 2e-)

41
Ions
  • The loss or gain of e- to form ions is directly
    related to the number of valence e- in an atom.
    All atoms have a driving force towards a noble
    gas e- configuration as this is the most stable
    configuration (i.e. 8 e- in the valence shell,
    unless we are talking about the 1st shell which
    only holds 2 e- as in He).
  • We can predict the ions that are formed by atoms
    by using the Periodic Table. The group number
    (column number) indicates the number of e- in the
    valence shell. Therefore
  • Group I has one valence e- and will tend to lose
    1e- forming a 1 ion and
  • Group VII has 7 valence e- and will tend to gain
    1e- forming a -1 ion, etc.
  • The transition metals are more difficult to
    predict as many of these elements have a variable
    e- configuration, however, these will all lose
    electrons to form positive ions.
  • In general
  • Metals tend to form cations () and non-metals
    tend to form anions (-)

42
Ionic bonding
  • Electrostatic attraction between oppositely
    charged particles
  • Ionic bonds are formed from the transfer of
    electrons from one atom to another. As previously
    stated, this is to obtain an overall noble gas
    configuration. The ratio of atoms results in an
    electrically neutral compound.
  • Because oppositely charged particles attract to
    form these bonds, ionic bonds tend to form
    between metals and non-metals.
  • Note ionic compounds do not form discreet
    molecules, rather they tend to form an array of
    anions and cations in a fixed ratio which is
    given in the empirical formula. (See next slide)

cation
anion
Example Mg2 Cl- ? MgCl2
43
Ionic bonding
  • No discreet molecules are formed in ionic bonding
    due to electrostatic forces holding the atoms
    together. More information about these and their
    properties in 8.2.5.

44
Covalent Bonding
  • Covalent bonds are formed between two atoms
    sharing electrons.
  • In covalent bonding, there is no electrostatic
    attraction as in ionic bonding. Atoms will
    share a pair (single bond) or pairs (double or
    triple bonds) of e- to gain a noble gas
    configuration. For example
  • Cl with and electron configuration of (2,8,7)
    will covalently bond with another Cl of (2,8,7)
    or with H of (1) to form Cl2 or HCl.
  • In the examples of Cl2 and HCl, all atoms have a
    full valence shell due to the sharing of
    electrons. Cl has 8 e- and H has 2 e-. These
    compounds then exist as individual particles or
    molecules and are known as covalent molecular
    substances to distinguish them from covalent
    lattices such as in silicon dioxide and diamond.
  • Other examples include water, ammonia and carbon
    dioxide.

45
Covalent Bonding
  • Covalent bonding leads to the formation of
    discreet molecules (i.e. single units that are
    often weakly bonded together by intermolecular
    forces). More about these and their properties in
    8.2.5.

Water
Chlorine
Hydrogen Chloride
46
Lewis Dot Structures
  • Lewis dot structures are a way of representing
    the valence e- configuration of an atom and show
    how valence e- are arranged in compounds.
  • Lewis dot structures can be used to show the
    formation of ions but are more commonly used to
    show covalent bonding.
  • The compounds formed to the right are methane,
    ammonia, water and hydrogen chloride
    (hydrochloric acid).

47
8.2 The Chemical Earth
  • Focus 4
  • Energy is required to extract elements from their
    naturally occurring sources

48
Physical vs. Chemical
  • Physical changes that are associated with
    physical properties which do not change the
    chemical composition of a substance.
  • E.g. hardness, density, malleability, ductility,
    electrical and thermal conductivities, melting
    point, boiling point, solubility
  • Chemical changes that occur when a substance
    breaks down or reacts with another substance in a
    chemical reaction
  • A new substance is always formed and has
    different properties than the original reactants.

49
Physical Changes - examples
  • Changing of state (melting iron, boiling water)
  • Changing the physical appearance (crushing ore in
    a ball mill, drawing copper into wires)
  • Dissolving a solid in a liquid (sugar into water)
  • Separation of mixtures (filtering sand from
    water, separating sea salt from water)
  • Physical changes no new substances!

50
Chemical Changes - indications
  • A gas is evolved (iron and HCl generate H2 gas)
  • A solid (precipitate) is formed when two
    solutions are added together (silver nitrate and
    sodium chloride solutions produce a white solid
    of silver chloride).
  • A change in colour (purple potassium permanganate
    (KMnO4) is added to hydrogen peroxide, the
    solution turns colourless).
  • Change of temperature (magnesium is burned in air
    and becomes very hot)
  • Chemical change at least one new substance!

51
Physical vs. Chemical -Water
  • Water- a physical change
  • Boiling water is an example of relatively weak
    intermolecular forces (Hydrogen bonds) breaking.
  • Energy required 44 kJ/mol
  • Water-a chemical change
  • Electrolysis of water involves the breaking of
    very strong covalent bonds between H and O atoms.
  • Energy required 286 kJ/mol

52
Physical vs. Chemical -Water
  • Electrolysis breaking covalent bonds
  • Boiling breaking H bonds



H bond
53
Physical vs. Chemical -summary
Chemical change (reaction) Physical change
At least one new substance is formed No new substances are formed
Difficult to reverse (e.g. unboiled egg?) Easily reversed (e.g. melt ice and freeze it again)
Generally requires a large amount of energy Generally, relatively small quantities of energy
54
Decomposition Reactions Energy absorbed
  • When a compound decomposes into two or more other
    pure substances, energy is normally absorbed in
    the form of heat, light or electricity.

Heat Light Electricity
AB ? A B
55
Decomposition Reactions-examples
  • Heat
  • Solid copper nitrate decomposes to solid copper
    oxide, nitrogen dioxide and oxygen gases.
  • Electricity
  • Molten lead bromide (4000C) forms bromine gas at
    the ve electrode and liquid lead at the ve
    electrode.
  • Light
  • Solid silver chloride decomposes to silver metal
    and chlorine gas. (decomposition of silver
    compounds is the basis of photography
    development).

56
Synthesis ReactionsEnergy released
  • A synthesis or combination reaction involves the
    combination of two or more pure substances. When
    a compound is formed from its elements, it is
    known as a direct combination reaction. These
    reactions normally release energy.

A B ? AB energy
57
Synthesis reactions - examples
  • Magnesium burns in air (oxygen) to produce
    magnesium oxide (light and heat energy released)
  • Hydrogen and oxygen combine in an explosive
    reaction to produce water (much energy released)
  • Copper metal combines with yellow sulphur when
    heated to produce copper (I) sulphide. (much heat
    energy is released)

58
Decomposition and SynthesisEveryday Applications
  • Decomposition
  • Air bags sodium azide (NaN3) decomposes to
    sodium and nitrogen gas by ignition with a
    detonating cap.
  • Limestone (primarily CaCO3) decomposes to
    calcium oxide and carbon dioxide by heating to
    make lime (CaO), cement and glass.
  • Aluminium - the industrial process of
    electrolysing aluminium oxide produces aluminium
    metal.
  • Synthesis
  • Rust iron and oxygen combine in the presence of
    water to form iron (III) oxide.
  • Burning coke (primarily carbon) is used as a fuel
    in smelting iron ore in a blast furnace during
    the steel making process.
  • Pollutants - NO (nitric oxide or nitrogen
    monoxide) and NO2 (nitrogen dioxide) are formed
    inside the combustion chambers of cars from
    nitrogen and oxygen gases.

59
8.2 The Chemical Earth
  • Focus 5
  • The properties of elements and compounds are
    determined by their bonding and structure

60
Properties of elements and their compounds are
very different
  • 8Fe(s) S8(s) heat ? 8FeS(s)

substance colour Melting point (0C) Boiling point (0C) Density (g/cm3) magnetic
Iron Grey 1535 2750 7.9 yes
Sulphur Yellow 113 445 2.1 no
Iron (II) sulphide Yellow-gold 1194 - 4.84 no
61
Properties of elements, compounds and mixtures
are very different
  • Aluminium
  • Physical properties
  • M.P. 6600C
  • Density 2.7 g/cm3
  • Conductivity 37.8 x106 Sm-1 (20 C)
  • Chemical properties
  • 4Al(s) 3O2(g) ? 2Al2O3(s)
  • 2Al(s) 6HCl(g) ? 2AlCl3(aq) 3H2(g)
  • Oxygen
  • Physical properties
  • M.P. -2190C
  • Density 0.0013 g/cm3
  • Conductivity non-conductor
  • Bauxite ore (Al2O3?xH2O)
  • Physical properties
  • M.P. 20450C
  • Density 3.5-4 g/cm3
  • Conductivity non-conductor
  • Chemical properties
  • Al2O3(s) 2NaOH 3H2O(l) ? 2NaAl(OH)4(aq)
    (Bayer process)
  • NB Bauxite is essentially an impure aluminium
    oxide. The major impurities include iron oxides,
    silicon dioxide and titanium dioxide. The
    impurities remain as solids and do not react with
    NaOH. This process removes these impurities.

62
Structure of metals
  • Metals can be described as three-dimensional
    lattices of positive ions in a sea of delocalised
    electrons.

63
Covalent Bonding
  • Covalent Molecular-strong bonds, weak
    intermolecular forces holding molecules together
  • Covalent Network-covalent bonding lattice that
    extends indefinitely throughout the crystal

64
Ionic bonding
  • No discreet molecules are formed in ionic bonding
    due to electrostatic forces holding the atoms
    together. They form a continuing 3D lattice.

65
Properties associated with bond typesMetallic
bonding
  • High melting points-due to strong attraction
    between positively charged metal ions and
    delocalized electrons. The higher the valency,
    the stronger the bond e.g. Ca2 is stronger than
    K.
  • Good conductors of heat and electricity-due to
    the high mobility of delocalized electrons.
    Electrons enter and leave a metal easily.
  • Malleable and ductile-due to delocalized
    electrons not belonging to any particular metal
    atom. Therefore, one layer of ions can slide
    over another without disrupting the bond between
    metal atoms. The electrons and metal ions simply
    rearrange.
  • Hardness- tend to be hard due to tightly packed
    atoms.

66
Properties associated with bond typesIonic
bonding
  • High melting points-due to strong electrostatic
    attraction between anions and cations.
  • Non-conductors of electricity in solid state-due
    to oppositely charged particles, which are in
    fixed positions.
  • Conductors in the liquid (molten) state-due to
    the ions being able to move freely through the
    liquid.
  • Hardness-due to strong electrostatic attraction
    between oppositely charged particles.
  • Brittle-due to the fixed location of oppositely
    charged particles. Displacement of ions moves
    them closer to ions of a similar charge, which
    increases the repulsive forces along the
    fracture.

67
Properties associated with bond typesCovalent
molecular bonding
  • Low melting points-due to generally weak
    attractive forces between molecules. There are
    exceptions to this rule (e.g. I2 melts at 1140C,
    but decomposes at 10000C).
  • Non-conductors-due to lack of mobile charged
    species or delocalized electrons.
  • Soft-due to weak forces existing between
    molecules.

68
Properties associated with bond typesCovalent
Network bonding
  • Very high melting points and boiling points-due
    to strong covalent bonding, which form rigid 3-D
    structures.
  • Non-conductors-due to lack of mobile charged
    species or delocalized electrons.
  • Extremely hard- due to strong covalent bonding,
    which form rigid 3-D structures.

69
The Chemical Earth
  • Compiled by Robert Slider (2006)
  • Please share this resource with others
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