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Technical Mineralogy Department of Geosciences
Technische Mineralogie ETHZ IMP 2010
Technical Mineralogy Department of Geosciences
Technische Mineralogie ETHZ IMP 2010
Alite
Ca3SiO5 = C3S
Polymorphic transformations: T1 T2 T3 M1 M2 M3 R T: triclinic M: monoclinic R: rhombohedral
620°C 920°C 980°C 990°C 1060°C 1070°C
Max. concentration of impurities: 1.0 wt% Al2O3, 1.2% Fe2O3, 1.5 % MgO impurities stabilize the M1 and or M3 in klinkers, rarely T2 is found
orthosilicate 0.71nm!
R- C3S projected along the c-axis
SiO4
Ca
O
Klinker production
Technical Mineralogy Department of Geosciences
Technical Mineralogy Department of Geosciences
Technische Mineralogie ETHZ IMP 2010
Belite
Ca2SiO4 = C2S
Polymorphic transformations: O1(g) M1(b) M2(aL ’) O2(aH’) H1(a) O: orthorhombic M: monoclinic H: hexagonal
<500°C 630°C 1160°C 1425°
Max. concentration of impurities: 4.0-6.0wt% Al2O3+ Fe2O3 impurities stabilize the b-phase
orthosilicate
0.55nm!a - C2S proj. down c-axis
Klinker production
Technical Mineralogy Department of Geosciences
Technical Mineralogy Department of Geosciences
Technische Mineralogie ETHZ IMP 2010
Aluminates and ferrites
Ca3Al2O6 = C3A (cubic) impurities: up to 4wt% NaO up to 16% Fe2O3+ SiO2 imputirities stabilize an orthorhombic polymorph
Ca2AlxFe1-xO10 = C4AF xclinker: around 1.0
impurities: up to 10 wt% MgO +TiO2 + SiO2
Klinker production
Technical Mineralogy Department of Geosciences
Technical Mineralogy Department of Geosciences
Technische Mineralogie ETHZ IMP 2010
Polymorphs and composition of phases present in clinker
C3A polymorphs is coupled with substitution. Clinker aluminate phases are cubic (fine grained) or orthorhombic (lath shapedand twinned) 13% to 20% of substituting elements: Mg, Al, Fe, Si
C3S early crystallized small crystals rich in substitutes: M3 late crystallized large crystals: M2 (single twins), rarely T1 (polysynthetic twins) 3-4% of substituting elements, mainly Mg, Al and Fe!
C2S usually only in the M1(b) polymorph with parallel twin lamellae. M2(aL ’) has typical crossed twin lamellae. The transformation M2(b) !M(g) should be avoided, because the accompanying drastic volume increase leads to excessive dusting. 4-6% of substituing elements, mainly Al and Fe
C3AF Main exchange vector Fe-2 SiMg !
Klinker production
Technical Mineralogy Department of Geosciences
Technical Mineralogy Department of Geosciences
Technische Mineralogie ETHZ IMP 2010
Microstructures
Alite crystals with both single and polysynthetic twins !
Klinker production
Belite crystals with complex twin lamellae (M2(aL ’) polymorph)
Belite crystals with paralllel twin lamellae (M(b) polymorph)
Belite crystals with crack formation along lamellae boundaries (M(b) !(M(b) transf.)
Technical Mineralogy Department of Geosciences
Technical Mineralogy Department of Geosciences
Technische Mineralogie ETHZ IMP 2010
Rotary kiln Without preheater/precalciner the kiln aspect ratio is about 30
Klinker production
Technical Mineralogy Department of Geosciences
Technical Mineralogy Department of Geosciences
Technische Mineralogie ETHZ IMP 2010
Rotary kiln with precalciner unit
Klinker production
Technical Mineralogy Department of Geosciences
Technical Mineralogy Department of Geosciences
Technische Mineralogie ETHZ IMP 2010
énergie
Technical Mineralogy Department of Geosciences
Technische Mineralogie ETHZ IMP 2010
Klinker reactions below 1300°C
Decomposition of calcite (calcining): 500 - 900°C free lime (CaO)
Decomposition of phyllosilicates: 300 - 900°C dehydroxilated, amorphous material
Temp. range products
Formation of first clinker phases: > 800°C belite, aluminates (different phases), ferrites
Formation of first melt phases: > 1000°C
Drying 100°C free water evaporates 100 - 300°C release of adsorbed and crystal water
Klinker production
Technical Mineralogy Department of Geosciences
Technical Mineralogy Department of Geosciences
Technische Mineralogie ETHZ IMP 2010
Decomposition of carbonate phases I
Decomposition reaction: CaCO3 = CaO + CO2
K =CaO[ ] CO2[ ]CaCO3[ ]
= pCO2
Equilibrium constant
Rate of decarbonation is influenced by:
- gas temperature (heat transfer)
- material temperature (=> K)!
- external partial pressure of CO2
- size and purity of the calcite particles
Klinker production
Calcite decomposition temperature as function of CO2 partial pressure
0.0
0.25
0.5
0.75
1.0
750 800 850 900
890!C
T(!C)
P(CO2)
Technical Mineralogy Department of Geosciences
Technical Mineralogy Department of Geosciences
Technische Mineralogie ETHZ IMP 2010
Belite formation
1. Formation of belite through solid state reaction
quartz amorphous material
belite
2. Transformation of the belite shells to belite crystal clusters
lime
Klinker production
Technical Mineralogy Department of Geosciences
Technical Mineralogy Department of Geosciences
Technische Mineralogie ETHZ IMP 2010
Klinker reactions between 1300°C and 1450°C
1. Melting reactions - Melting of primary aluminates and ferrites phases - Melting of part of the early formed belite
2. Formation of new phases Reaction of melt, free lime, unreacted silica and remaining belite to alite
3. Polymorphic transformation of belite
4. Recrystallization of alite and belite
5. Nodulization (clinkering)
Klinker production
Technical Mineralogy Department of Geosciences
Technical Mineralogy Department of Geosciences
Technische Mineralogie ETHZ IMP 2010
Appearance of first melt
1. Alkali and sulfate melts
Klinker production
Technical Mineralogy Department of Geosciences
2. C-S-A for cement compositionmelts: lowest eutecticum 1455°
Technical Mineralogy Department of Geosciences
Technische Mineralogie ETHZ IMP 2010
P: typical bulk composition of Portland cement klinkers First melt appearance: 1455°C
Phase diagram
Klinker production
Technical Mineralogy Department of Geosciences
see excercise 2
Technical Mineralogy Department of Geosciences
Technische Mineralogie ETHZ IMP 2010
Klinker production
Technical Mineralogy Department of Geosciences
CaO - SiO2 - Al2O3 phase diagram: section at 1500°C
A typical Portland cement composition at 1500° C (section shown on the right) is in a three phase field i.e. with alite, belite and an aluminium rich melt. The grey shaded areas are two phase fields
Technical Mineralogy Department of Geosciences
Technische Mineralogie ETHZ IMP 2010
Amount of melt and the silica module
At 1450°C and above the liquid content depends on the silica modulus
Klinker production
15
20
25
30
35
1.5 2.0 2.5 3.0 SM
Liqu
id p
hase
(wt
%)
3.5
Technical Mineralogy Department of Geosciences
Technical Mineralogy Department of Geosciences
Technische Mineralogie ETHZ IMP 2010
Formation and recrystallization of alite
amorphous material
lime
belite
alite
1. Formation of melt around lime crystals
2. Crystallization of alite walls at the contacts between belite cluster and lime
3. Recrystallized and new formed alite replaces lime crystals
Klinker production
Technical Mineralogy Department of Geosciences
Technical Mineralogy Department of Geosciences
Technische Mineralogie ETHZ IMP 2010
Klinker production
Technical Mineralogy Department of Geosciences
Technical Mineralogy Department of Geosciences
Technische Mineralogie ETHZ IMP 2010
Microtextures I (all pictures FL Smidth review 25)
0.05mm!
Alite wall separating CaO and a belite cluster
alite melt phase (aluminates,ferrites) belite lime
Belite clusters replacing previous quartz grains.
0.1mm!
Klinker production
Technical Mineralogy Department of Geosciences
Technical Mineralogy Department of Geosciences
Technische Mineralogie ETHZ IMP 2010
Alite crystallizing at the expense of lime and belite
0.3mm!
Microtextures II
lime belite
alite
Well crystallized, homogeneous clinker. The raw mix contained few quartz grains and a well controlled carbonate grain size.
pores
0.2mm!
Klinker production
Technical Mineralogy Department of Geosciences
Technical Mineralogy Department of Geosciences
Technische Mineralogie ETHZ IMP 2010
Klinker reactions during cooling
1. Crystallization of the restitic melt. Products: aluminates (C3A) and ferrites (C4AF)
2. Polymorphic transformations of alite and belite
3. Backreaction of alite to belite + lime
4. Recrystallization aluminates and ferrites
If cooling is too slow
Klinker production
Technical Mineralogy Department of Geosciences
Technical Mineralogy Department of Geosciences
Technische Mineralogie ETHZ IMP 2010
Microtextures III
Backreaction of alite rims to belite plus lime in a belite poor clinker (fast cooling).
0.04mm!
belite rims
Klinker production
Technical Mineralogy Department of Geosciences
Fast cooled clinker with euhedral alite and rounded belite crystals.
0.05mm!
Technical Mineralogy Department of Geosciences
Technische Mineralogie ETHZ IMP 2010
CU500898 0305.raw:1
6564636261605958575655545352515049484746454443424140393837363534333231302928272625242322212019181716151413121110
1'600
1'500
1'400
1'300
1'200
1'1001'000
900
800
700
600
500
400
300200
100
0
-100
-200
-300
-400
-500
C2S beta (MUMME) 22.64 %C3S monoclinic (NISHI) 55.50 %C4AF 4.13 %Periclase 3.76 %Lime 0.54 %C3A cubic 12.59 %Arcanite K2SO4 0.84 %
Klinker production
Technical Mineralogy Department of Geosciences
Quantitative determination of the klinker mineralogy
X-ray powder diffraction patterns are used for the quantitative determination of the klinker mineralogy. The technique, which allows to extract the quantity of each phase present is called Rietveld refinement.
Technical Mineralogy Department of Geosciences
Technische Mineralogie ETHZ IMP 2010
Normative mineralogy of clinker
Klinker production
Technical Mineralogy Department of Geosciences
Technical Mineralogy Department of Geosciences
Technische Mineralogie ETHZ IMP 2010
Energy balance in clinker production
Temp range 20-450°C wet 100°C ca. 450°C 450-900°C ca. 900°C ca. 900°C 900-1400°C 900-1400°C ca. 1300°C 1400-20°C 900-20°C 450-20°C !
Process Heating of the material Evaporation of free H2O Removal of H2O from clay heating of the material Dissociation of calcite Crystallisation of dehydrated clay Heating of the decarbonated material Heat of formation of clinker minerals Melting of liquid phases Cooling of clinker Cooling of CO2 Cooling of H2O Total
Heat exchange kJ/kg clinker 710 (1800) 170 820 2000 -40 525
-420 100
-1510 -500
-85 4325 -2555 !
Klinker production
Technical Mineralogy Department of Geosciences
Technische Mineralogie ETHZ IMP 2010
Energy costs of cement production
Process Quarry Crushers Prehomoginizing and transport Raw mill Raw meal silo Kiln feeder Kiln and cooler Coal mill Cement mill Packing plant Other total
Fuel Electricity Cost($/day) kcal/kg cement kwh/ton cement
0 0 2.5 600
1.5 360 0-100 27.0 9813 1.5 360 1.5 360 700 23.0 28853
2.5 600 30.0 7200
1.0 240 4.5 1080 700-800 95.0 49467 !
Klinker production
Dry process cement plant 5000t/day