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The Building Blocks of Earth

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Title: PowerPoint Presentation Author: Isotope Geochemistry Lab Last modified by: Gary S. Solar Created Date: 6/29/2000 6:06:59 PM Document presentation format – PowerPoint PPT presentation

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Title: The Building Blocks of Earth


1
The Building Blocks of Earth
Atoms, Elements and Compounds Introduction to
Minerals.
2
Minerals are Composed of Atoms
1. Atoms can be subdivided into numerous
subatomic particles, however we will be concerned
with protons, neutrons and electrons.
3
Minerals are Composed of Atoms
1. Atoms can be subdivided into numerous
subatomic particles, however we will be concerned
with protons, neutrons and electrons. 2.
Protons and neutrons are together in the nucleus
of an atom. Electrons are in motion in orbits
around the central nucleus.
4
Minerals are Composed of Atoms
1. Atoms can be subdivided into numerous
subatomic particles, however we will be concerned
with protons, neutrons and electrons. 2.
Protons and neutrons are together in the nucleus
of an atom. Electrons are in motion in orbits
around the central nucleus. 3. Protons carry a
positive electronic charge. Electrons carry a
negative charge. Neutrons carry no charge.
5
Minerals are Composed of Atoms
1. Atoms can be subdivided into numerous
subatomic particles, however we will be concerned
with protons, neutrons and electrons. 2.
Protons and neutrons are together in the nucleus
of an atom. Electrons are in motion in orbits
around the central nucleus. 3. Protons carry a
positive electronic charge. Electrons carry a
negative charge. Neutrons carry no charge. 4.
Most atoms have no total charge (they are
electrically neutral).
6
The Periodic Table
The periodic table is read from top to bottom,
left to right, as atomic number increases 1H,
2He, 3Li, 4Be, 5B, 6C, and so on.
7
Electronic and Nuclear Properties of Atoms
Properties of atoms reflect some combination of
features related to electrons or to the nucleus.
- Atomic Number ? - Atomic Mass ? The
electronic properties are those related to how
atoms connect to one another bonding. The
nuclear properties include features
like radioactivity.
8
The Periodic Table
The periodic table is read from top to bottom,
left to right, as atomic number increases 1H,
2He, 3Li, 4Be, 5B, 6C, and so on.
9
Size of the Nucleus
The number of neutrons tends to closely follow
the number of protons.
10
The Spacious Atom
Microcosms of our solar system, atoms are
dominantly empty space
electron orbits
If an oxygen atom had a total radius of 100 km,
the nucleus would be a 1 m diameter sphere in
the middle.
11
Electrons in Orbit
In a simplistic model, electrons float around the
nucleus in orbits (sometimes called shells).
electron orbits
As the number of electrons increases, they start
to fill orbits farther out from the nucleus. In
most cases, electrons are lost or gained only
from the outermost orbits.
12
Charged Atoms Ions
- Left to their own devices, atoms are
electrically neutral. That means that they have
an equal number of protons and electrons. -
During the course of natural events, protons are
not gained or lost, but electrons may be. -
Atoms with more or fewer electrons than protons
are electrically charged. They are called
ions loss of electrons causes the atom to have
a charge (cation) gain of electrons
causes the atom to have a - charge (anion). -
Complex cations and anions can also occur NH41,
(SO4)-2
13
The Periodic Table
Elements in columns (groups) have similar
outer-electron configurations, and so tend to
behave similarly.
alkali earths
transition metals
halogens
alkalis
rare earths
noble gases
actinides
14
Oxidation State
halogens
Most atoms will form the same ions all the time.
For example, all the alkalis form 1 ions, and
the halogens always form -1 ions.
alkalis
15
The Periodic Table the Bulk Earth
A small number of elements make up gt99 of the
solid Earth.
16
The Periodic Table the Crust
The crust is a little more elementally
interesting (again, as a result of
differentiation), but it is still mainly made of
a small number of elements.
17
Isotopes
Carbon (atomic 6) has three natural isotopes
with atomic masses of 12, 13 and 14.
isotope p n C-12 6 6 C-13 6 7
C-14 6 8
Tin (Sn, atomic 50) has ten natural isotopes
with atomic masses of 112, 114, 115, 116, 117,
118, 119, 120, 122 and 124. How many protons and
neutrons do these isotopes have?
18
Chemical Bonds
  • Ionic Bonds
  • Atoms with near-full (halogens) and near-empty
    (alkalis/alkali
  • earths) outer electron orbits, as well as
    transition metals, may
  • form ionic bonds.
  • Covalent Bonds
  • Covalent bonds are where atoms share outer shell
    electrons.
  • The bulk of minerals are dominantly ionically
    bonded. However, many minerals have bonds with
    mixed covalent and ionic bonds between their
    atoms in their crystal structures.

19
Ionic Bonds
Atoms satisfy themselves by the give and take of
outer shell electrons. Transition metals tend to
sacrifice electrons from their inner orbits.
20
Covalent Bonds Electron Sharing
These carbon atoms are held together by
sharing outer-orbit electrons.
21
Alternative Bonds
metallic bonds (a form of covalent bonds) Van
der Waals force, essentially an ionic bond.
22
What is a Mineral?
23
What is a Mineral?
  • naturally occurring
  • inorganic compound
  • specific chemical formula
  • definite crystal structure

24
What is a Mineral?
  • naturally occurring consistent physical
    properties
  • inorganic compound
  • specific chemical formula
  • definite crystal structure
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