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Group IV a Complete

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    P-Block Elements

    Group IV A

    The Carbon Family

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    Elements of Group IV ACarbon C

    Silicon SiGermanium Ge

    Tin Sn

    Lead Pb

    The elements in this group range from a non-metal, carbon to themetals tin and lead, with the intervening element germaniumshowing semi metallic behavior.

    Germaniumwas a missing element in Mendeleevs periodic table.He named this element as ekasilicon and predicted its propertiesthat later matched with those of germanium.

    Siliconis the second most abundant element in the earths crust; toolsmade of flint (a form of SiO2) were used in the Stone Age.

    Tin and lead have also been known since ancient times All theelements have an outer electronic configuration of ns2 np2

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    Carbon

    Carbon is the base of all life and the element with the mostcomplex chemistry, which is called organic chemistry. Coal,

    which consists mostly of carbon, is known and used since

    prehistoric time. The massive combustion ofcoal and oil,

    which is carbon based, causes enormous harm to the life on

    our planet. This is because, amongst others, a lot of carbon

    dioxide, CO2, is emitted.

    Graphite, which is very soft, is the most common carbon

    allotrope. Another one is diamond, famous for its value and

    hardness. Fullerenes are further allotropes, which werediscovered in 1985. They could have many different

    applications in the future.

    Compounds of carbon and another, more electropositive

    element are called carbides, like silicon carbide and tungstencarbide.

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    Diamond

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    Silicon Carbide

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    Graphite

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    Carbon Nanotube

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    Silicon

    The metalloid silicon is a very abundant element. Much of the earth's crust is made out of

    silicates and silica (SiO2). The latter is the chief ingredient of quartz and sand and is used

    as raw material for glass since ages. Elemental silicon is an important industrial material,

    where it is used in huge amounts for semiconductors, computer chips, in electronics, for

    solar energy and photovoltaics.

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    Ultra pure Silicon

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    Germaniumis a shiny silvery metalloid and a semiconductor. The latter makes it an important

    material in electronics and solar technology. Germanium is corrosion-resistant, very brittle and

    slightly toxic, it doesn't have biological functions.

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    Tinis a very common metal. It is soft and has a low melting point, which makes it a verygood workable material, that is used since ancient times. Bronze is usually an alloy of

    copper and tin. The common -tin can transform into powdery -tin at low temperatures

    (below 13C, 56F). This is known as tin pest, which destroys the affected item.

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    Leadis known since ancient times and was widely used then. This often caused bigsanitary problems, because its compounds are quite toxic. 208Pb is the last stable isotope in

    the periodic table and the end of the thorium decay chain. Therefore lead is quite

    abundant for an element with such a high number. Lead is a grey, very heavy and soft

    metal with a low melting point. Amongst others, it is used for weights and for radiationprotection. Lead forms in air quickly a protecting oxide layer, which makes it dark.

    http://images-of-elements.com/thorium.phphttp://images-of-elements.com/thorium.php
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    A piece oflead, cut through, is silvery for a short time, before the surface oxidizes.

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    Carbon

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    Overview of Chemical properties of Group IV A

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    HCOOH + conc. H2SO4 CO + H2O

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    Organometallic compounds

    Organo silicon compounds

    Organo germanium

    Organo tin

    Organo lead

    GROUP ASIGNMENT

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    GENERAL INTRODUCTION

    BONDING SITUATION

    METHODS OF SYNTHESIS

    LITERATURE (from 2000-2013)

    NO PLAGIARISM

    ACS REFEREMCE WRITING STYLE

    TYPED AND PRINTED

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    Submitted within time

    1. Increased understanding and critical thinking

    2. Citation is from reliable resources

    3. Acceptable reference writing style

    4. Relevant references from peer reviewed journals (as directed by the course instructor)

    5. Plagiarism/Similarity index

    (as dictated by Turnitin Report)

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    silicones

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    Si

    O

    O

    Si

    Si

    O

    CH3CH3

    CH3

    CH3CH3

    CH3

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    repellents, i.e., not wetted by water.

    Stable towards heat and chemical reagents.

    Non toxic and inert and have medical applications.

    Non volatile on heating.

    Used for making water proof cloth

    Used as insulating materials for electrical appliances.

    Mixed in paint and enamels to make them water proof.

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    Structural Variety, key to modulating the process

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    Silicates

    Salts of silicic acids are called silicates

    Soluble silicates such as Na or K silicates are known as soluble glass

    Three stable silicic acids are known to exist:

    1. meta silicic acid H2SiO3 (SiO2.H2O)

    2. ortho silicic acid H4SiO4 (SiO2.2H2O)

    3. Pyrosilicic or disilicic acid H6Si2O7

    Salts of these acids are known

    Dehydration of these compounds leads to formation of SiO2 (silica)

    Silica with 5% water content is called silica gel, it has a spongy structure and is used as a

    dehydrating agent and can absorb water, reheating it can restore the original structure

    which can be used again.

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    Soluble Metal SilicatesString bases react very slowly with silica to form various soluble metal silictaes.

    SiO2 + 2NaOH Na2SiO3 + H2O

    SiO2 + 4NaOH Na4SiO4 + 2H2O

    2SiO2 + 6NaOH Na6Si2O7 + 3H2O

    Natural Silicates comprise a largevariety of compounds, structures of which

    are based on SiO4 tetrahedra with metal

    atoms occupying spaces in between the

    tetrahedra.

    The SiO4 tetrahedra are joined together in

    different manner to give different structures

    of silicates

    Silicates are extremely stable structures due

    to vacant d orbitals on Si which can accept

    electron density from oxygen

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    Structures of Silicates

    1. Orthosilicates

    SiO4 repeating units

    e.g., Mg2SiO4 Olivine a mineral

    ZrSiO4 Zircon

    Be2SiO4 phenacite

    Si

    O-

    O

    -

    O-

    O-

    4-

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    Pyrosilicates or Disilicates

    Two SiO4 units are joined together

    Repeating unit is Si2O76-

    e.g., Se2Si2O7

    PbSi2O7

    Zn4(OH)2Si2O7

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    Cyclosilictaes

    Discrete units made up of 3 or 6 tetrahedra in a ring.

    i.e., Si3O96-

    Si6O1812-

    Examples include:

    BaTiSi3O9

    Ca3Si3O9

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    Si

    O

    Si

    Si

    OO

    O

    O

    O

    O

    O

    Si

    OSi

    O

    OO

    O

    O

    O

    Si

    O

    O

    Si

    O

    O

    Si

    Si

    O

    OO

    O

    OO

    O

    Si3O96-

    Si6O1812-

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    Metasilicates Infinite Chain Atoms

    Silicates in which tetrahedra are linked together in long chains orstrings

    If single chained. They are called Pyroxenes

    Of double stranded then they are called Amphiboles

    Si

    O

    O

    Si

    O

    Si

    O

    Si

    O

    Si

    O

    Si

    O

    O

    O

    O

    O

    O O

    O

    O

    O

    O

    OO

    SiO32-

    Pyroxenes

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    O

    Si

    O

    Si

    O

    Si

    O

    Si

    O

    O

    O

    O

    O

    O

    O

    OO

    O

    Si

    O

    Si

    O

    Si

    O

    Si

    O

    Si

    O

    O

    O

    OO

    O

    OO

    Si

    O

    Si

    O

    Si

    O

    Si

    O

    O

    O

    O

    O

    O

    O

    OO

    Si

    O

    Si

    O

    Si

    OO

    O

    O O

    O

    n

    Ambhibolescontain (Si4O11-6)n anions and is and have double chains with cross

    linking

    Various asbestos minerals are of this type, their fibrous nature is a result of one

    dimensional anion structure and can be cleaved in direction parallel to the

    chains

    Phyllosilicates are silicates with anions as sheets (Si O )n2- Individual sheets are held

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    O

    Si

    O

    Si

    O

    Si

    O

    Si

    O

    O

    O

    O

    O

    O

    O

    OO

    O

    Si

    O

    Si

    O

    Si

    O

    Si

    O

    Si

    O

    O

    O

    OO

    O

    OO

    Si

    O

    Si

    O

    Si

    O

    Si

    O

    O

    O

    O

    O

    O

    O

    O

    O

    Si

    O

    Si

    O

    Si

    OO

    O

    O O

    O

    O

    Si

    O

    Si

    O

    Si

    O

    Si

    O

    O

    O O

    O

    OO

    O

    Si

    O

    Si

    O

    Si

    O

    Si

    O

    Si

    O

    O

    O

    OO

    O

    OO

    Si

    O

    Si

    O

    Si

    O

    Si

    O

    O

    OO

    O

    OO

    Si

    O

    Si

    O

    Si

    OO

    O

    O O

    O

    Phyllosilicates are silicates with anions as sheets, (Si2O5)n2-. Individual sheets are held

    together by metal cations which lie in between them. These are found in talc. Clays and

    mica

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    Phyllosilicate mineral, Chrysocolla

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    y , y

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    Olivine

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    Garnet

    Uvarovite

    Green Thorite from Zircon family a silicate mineral

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    Green Thorite, from Zircon family, a silicate mineral

    Structure of Zircon

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    Structure of Zircon

    Quartz SiO2

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    Kyanite - Al SiO

    http://en.wikipedia.org/wiki/Kyanitehttp://en.wikipedia.org/wiki/Kyanite
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    Kyanite - Al2SiO5

    http://en.wikipedia.org/wiki/Kyanitehttp://en.wikipedia.org/wiki/Kyanite
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    SiO2 based

    Mineral

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    Applications of silicates

    Used in glass industry

    Ceramic industry

    Cement industry

    Clays (used for making bricks etc.) and silica

    gel are examples of silicate structure

    Clays are classified as porcelain and china clay

    according to composition

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