EES 119/219
Lecture 4
Discussion of ore
deposits
Abundant metals
Fe ΰ Banded Iron Formation
Al ΰ Bauxite Deposits
Fe Characteristics
Crustal
abundance of Fe: 5.6 %; second most abundant metal in the crust (most
abundant element in the earth)
ΰ
Major
element, present in many rock forming minerals (e.g. Spinel)
Fe is a major or
minor constituent in all mineral classes
Chemical behavior of
Fe
Chemical
behavior: occurs in two main valence states: Fe+2 and Fe+3
Fe+2
ferrous iron ΰ FeO
Fe+3
ferric iron ΰ Fe2O3
The two types
indicate different ways to react with oxygen
Iron in the crustal
environment
Ferric
oxide may oxidize organic matter and thus become reduced to ferrous Fe
Ferrous
solutions may in turn be re-oxidized by atmospheric oxygen
ΰ
Iron acts as catalyst in the cycles of carbon and oxygen in crustal
compartments
Iron in the biosphere
Fe acts to
transfer oxygen from air or water to body tissues.
In green plants,
Fe is necessary for the formation of chlorophyll.
Some bacteria
possess an enzyme that transfers electrons from ferrous Fe to O2,
freeing them from the dependence on organic matter as an energy source
Iron ore deposits
Because of the
high abundance of Fe in the crust, Fe deposits are formed by many different
processes
Important for
ore formation: ferric Fe has low solubility in water, ferrous Fe has high
solubility
Grades: 30 ΰ 60% Fe
Fe in Fe3O4
72% (Fe = 56; O = 16)
Fe in Fe2O3
70%
ΰ
Grades are determined
for the extracted ore, typically accounting for the presence of gangue
minerals, but not host rock
Total production of steel
in 2006: ~ 1.2x109 tons/yr (Fig.
1)
Fe as metal
Iron is the most important metal for current
civilization
Fe is not present as native metal in the
crust
Hematite Fe2O3 ferric
iron
Magnetite Fe3O4 (FeO . Fe2O3)
ferrous + ferric
Limonite Fe2O3xnH2O
(rust)
Siderite FeCO3
Pyrite FeS2 and similar Fe
occurrences are not considered ore minerals
Types of Fe deposits
Magmatic
deposits: late segregation of magma ΰ Kiruna type deposit
Exposure
to weathering ΰ oxidation to ferric Fe ΰ other, more soluble materials are removed ΰ lateritic deposits (similar to bauxite
deposits)
Banded Iron Formation (BIF): Most important
type of Fe deposit BIF contain between 1012 and 1015
tons of Fe (Production 109 tons/yr)
Example:
Characteristics of BIF
Banded structure: alternation between Fe (Fe2O3)
and Si (SiO2) rich layers
Small, uniform grains (absence of large
pebbles etc.)
Large deposits
Age distribution
Precambrian (1.8 Ga or older)
Peak deposition ~ 2.0 Ga
Systematics of weathering
·
Chemical Weathering (H2O, pH)ΰ
transport in solution
ΰfine
grain deposits; continuous layers: limestone
·
Physical Weathering (H2O, wind, freezing)ΰ
mechanical transport
ΰVariable grain size:
conglomerates; sandstone
·
Temperature and pressure are within narrow
limits:
-30oC
< T< +60oC p~1 atm
Increase in O2
concentrations in the atmosphere: Fig. 4
Summary for BIF
Formation
reflect change in mobility between ferrous and ferric Fe
Change
in oxygen content of atmosphere
Seasonal
upwelling in coastal basins
Large
scale release of Fe from MOR and from erosion; transport possible only under low-oxygen
conditions
Formation
of BIF reflects significant changes in the oxygen content of the atmosphere due
to the occurrence of land plants
From Iron ore to
steel
Mining:
large scale, typically surface mining
Separation
of ore and transport to smelter
Production
of pig iron
Blast
Furnace
Production
of Steel
Steelmaking
is the second step in producing steel from iron ore. In this stage, impurities
such as sulfur, phosphorus, and excess carbon are removed from the raw iron,
and alloying elements such as manganese, nickel, chromium and vanadium are
added to produce the exact steel required
basic
oxygen furnace, also known as an LD converter
An electric
arc furnace is a system that heats charged material by means of an electric arc
Definitions:
Pig Iron: Fe compound after the initial separation from oxygen
ΰ contains relatively high amounts of C, not
used directly, but starting material for the production of steel (cast iron
is form of pig iron)
Steel: Fe metal containing between 0.5 and 1.5 % of C; often fortified with
other Fe-allow metals (Cr; Mo; W etc.) to give it specific characteristics
(toughness; hardness; elasticity etc.)