Minerals
Minerals
-
Different or same mineral (Figure: halite and calcite)
Minerals
-
Figure: breaking calcite with a hammer (small rhombs)
Minerals
-
Minerals: naturally-occurring inorganic crystalline solids with specific
chemical composition
-
What minerals are present on Earth will depend on:
-
abundance of elements
-
chemistry--valence and size of ion (see later discussion)
-
Abundance of Elements (Figure: pie diagrams of whole-Earth and Crust elements)

Basic Chemistry
-
Atomic structure
-
Fundamental unit of matter - atom
-
Atom composed of:
-
electron - negative charge of 1; revolves around nucleus
-
proton - positive charge of 1
-
neutron - no charge
-
element - basic component, no further chemical separation possible
-
atomic number Z - number of protons
Basic Chemistry
Atomic Structure (cont.)
-
atomic weight - average weight of an atom of an element (in amu)
-
mass number (A) - number of protons & neutrons
-
Example: general: AQ; for carbon-14: 14C
-
isotope - same # of protons, different # of neutrons
-
stable isotopes - 12C, 13C, 208Pb
-
unstable or radioactive isotopes - 14C, 40K, 238U
Basic Chemistry (cont.)
Atomic Structure (cont.)
-
bond - results from electrostatic attraction
-
compound - distinct substance formed by chemical bonding of two or more
atoms in definite proportion
-
molecule - smallest unit of compound with properties of that compound
Basic Chemistry (cont.)
Atomic Structure
-
Atomic structure
-
electrons travel in orbitals
-
orbitals organized into shells
-
chemically stable atom - outer shell is filled (p. 47)
-
Valence - number of electrons that an element tends to gain or lose
-
Periodic Table - elements organized by atomic number and chemical behavior
(p. 43)
Basic Chemistry (cont.)
Ions
-
ions - charged atoms or molecules
-
cations - positive ions (Na+ Ca2+, Fe3+)
-
anions - negative ions (Cl-, Br-)
-
complex ions - polyatomic ions (SO42-, HCO3-)
Basic Chemistry (cont.)
Types of Bonds
-
ionic - electrons not shared
-
large difference in ability to attract electrons
-
ex: NaCl, CaCl2
-
bond strength increases as charge increases
-
covalent - electrons shared
-
small difference in ability to attract electrons
-
metallic bond - metals; freely mobile electrons
-
van der Waals forces - weak bonds
-
more than one bond type common - Ex: CaCO3
-
Ca-CO3 bond ionic
-
C-O bonds covalent
Earth Minerals
Factors Determining Occurrence revisited
-
Factors
-
Abundance of elements
-
Valence
-
Size of ion
Earth Minerals
Factors Determining Occurrence (cont.)
-
Valence
-
in part determines which and how many atoms bond (see periodic table)
-
strive to achieve electrical neutrality
-
Examples
-
Na+ + Cl- = NaCl
-
Ca2+ + 2Cl = CaCl2
-
Si4+ and 2O-2 = SiO2
Earth Minerals
Factors Determining Occurrence (cont.)
-
Size of ion
-
Controls arrangement of atoms
-
Measured in terms of ionic radius
-
When atoms, ions, or molecules are arranged in a regular, repeating 3-D
pattern -> crystal.
Earth Minerals
Crystals and Minerals
-
Features of crystals:
-
smooth faces when space allows
-
same angle between faces
-
size depends on time
-
Minerals: naturally-occurring inorganic crystalline solids with specific
chemical composition
-
coordination number - number of anions directly bonded to a cation (or
vice-versa)
-
Coordination
number vs. ionic radius ratio
Earth Minerals
Substitution
-
one ion can substitute for another if
-
similar in size
-
similar in charge
-
Ex: Fe2+ for Mg2+ in Mg2SiO4
(type of olivine); sometimes written as (Mg, Fe)2SiO4
-
Anions can also substitute
Earth Minerals
Substitution (cont.)
-
substituting ion may make up <1% of composition ? trace element
-
coupled substitution - Na+, Si4+ for Ca2+,
Al3+ in anorthite (CaAl2Si2O8)
Earth Minerals
Solid Solution, Polymorphs
-
because of substitution, composition may for a continuum ? solid solution
-
def: single, homogenous crystal phase which may vary in composition without
the appearance of an additional phase
-
polymorph - same chemical composition, different structure
Copyright. Grossman, 1997