definition - w/c, w/swater to cement / solid ratio by mass - pastecement-water mix allowing setting...
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Definition
- w/c, w/s water to cement / solid ratio by mass
- paste cement-water mix allowing setting and hardening to occur w/c: 0.3-0.6
- setting stiffening without significant increase in strength
- hardening development of strength
- curing storage under conditions allowing hydration: under water forthe first 24h, than under 100% humidity or air
Hydration of cement
Institut de Minéralogie et PétrographieUniversité de Fribourg
Technische MineralogieETHZ IMP 2008
Heat evolution during Portland cement hydration
I
II
III
time (hours)
heat
evolu
tion r
ate
W/k
g
Induction (dormant) period
0 10 20 30
Hydration of cement
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preinduction period
acceleration period
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Hydration reaction of the silicates
All clinker minerals undergo hydration reactions:
AliteC3S + (y+z)H2O = CxS Hy + zCH x+z = 3 x,y,z are not integers
CxS Hy : poorly crystallized phase, structurally similar to tobermorite C/S ratio of C-S-H 1.7 - 1.8, max range 1.2 - 2.1CH: portlanditeΔH=-500J/g
Belite
Reaction stoichiometry similar to alite, but the hydration is much slower and produces less portlandite than the hydraton of alite C/S ratio of the C-S-H phase vary between 1.6 and 2.0. ΔH=-250J/g
Hydration of cement
Institut de Minéralogie et PétrographieUniversité de Fribourg
Technische MineralogieETHZ IMP 2008
Hydration reaction of the aluminates
Aluminate react rapidly to aluminate hydrates
2C3A + 21H = C4AH13 + C2AH8 above 30°C both hydrate convert to a hydrogarnet C3AH6
In the presence of sulfate the reaction product is ettringite
2C3A + 3CSH2 + 6H = C3A• 3CSH32
when a surplus in C3A is present (almost always the case) ettringite reacts to monosulfate:
C3A• 3CSH32 + 2C3A + 4H = 3C3A• CSH12
Hydration of cement
Institut de Minéralogie et PétrographieUniversité de Fribourg
Technische MineralogieETHZ IMP 2008
Hydrated aluminate and ferrite phases are classified according to their stoichometry into AFm and AFt phases:
C3(A,F)CXn yH = AFm for Al2O3 and,or Fe2O3 plus mono CXn
C3(A,F)(CXn)3 yH = AFt for Al2O3 and,or Fe2O3 plus tri CXn
C4AH13 = C3(A)CH2 11H AFm phase C3A• 3CSH32= C3A• 3CS•32H32= C3(A)(CS)3 •32H AFt phase
Hydration of cement
Institut de Minéralogie et PétrographieUniversité de Fribourg
AFm and AFt phases
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Temporal evolution of the hydration of clinker phases (Copeland + Kantro, 1964)
Hydration of cement
Institut de Minéralogie et PétrographieUniversité de Fribourg
Temporal evolution of the reactants
Technische MineralogieETHZ IMP 2008
Hydration of cement
Institut de Minéralogie et PétrographieUniversité de Fribourg
Temporal evolution of the products
Temporal evolution of the hydration hydration products (Kurtis, )
Technische MineralogieETHZ IMP 2008
Heat evolution and hydration reactions I
Hydration of cement
Institut de Minéralogie et PétrographieUniversité de Fribourg
C3A hydrationFormation of ettringite
Ettringite coating retards further aluminate hydration
Ettringite to monosulfate transformation and further aluminate hydration
Relationship between reactions and heat evolution
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• Stage 1: Initial hydrolysis characterized by dissolution of ions– Coatings form on cement particles that slow dissolution
• Stage 2: Dormant period characterized by continued dissolution of ions with nucleation control– Determines initial set
• Stage 3: Acceleration is characterized by the accelerated formation of hydration products. CH forms in solution and C-S-H forms around calcium silicate particles. – Determines final set and rate of initial hardening.– Ettringite converts to monosulfate when sulfates in solution are
used up (peak is slightly after C3S peak)• Stage 4: Deceleration is characterized by continued formation of
hydration products with diffusion control – Determines rate of early strength gain
• Stage 5: Steady state is characterized by the slow formation of hydration products – Determines rate of later strength gain
Stages of Portland cement hydration
Hydration of cement
Institut de Minéralogie et PétrographieUniversité de Fribourg
Technische MineralogieETHZ IMP 2008
Heat evolution as function of grain size
Heat evolution rateduring hydration of alite as function of grain sizee.g. specific surface area.
Hydration of cement
Institut de Minéralogie et PétrographieUniversité de Fribourg
Technische MineralogieETHZ IMP 2008
Heat evolution during the hydration of an aluminate paste as functionof gypsum concentration. In the presence of sulfate, the aluminates transform to ettringite, which coat the grains and block further hydration.
Heat evolution during the hydration of aluminates
Hydration of cement
Institut de Minéralogie et PétrographieUniversité de Fribourg
Technische MineralogieETHZ IMP 2008
Composition of the solution
Hydration of cement
Institut de Minéralogie et PétrographieUniversité de Fribourg
Temporal evolution of the Ca2+, SiOx, pH and C/S of products
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Theories for the dormant period
Hydration of cement
Institut de Minéralogie et PétrographieUniversité de Fribourg
Alite hydration
Alite
The initial C-S-H pro-duct form a surface layer, which slows down the transport of water to the reactant and thus the hydration rate. The acceleration is due to a breaking of the layer due to morphological changes in the C-S-H layer
Supersaturation of the liquid in Ca(OH)2 due to the poisoning of the portlandite nuclei by silica ions slows down the dissolution of alite. With time the silica concentration decreases due to formation of first CSH and the calciumhydrox-ide becomes high enough to overcome the poisoning = end of the dormant period.
Ca2+
Ca2+
Ca2+
Ca2+Ca2+
Ca2+
poisoned port-landite nuclei The formation of the
first C-S-H I product is slowed down by the su-persaturation in Ca(OH)2. Nucleation of a second C-S-H II phase becomes possible after thermo-dynamic barriers of nucleation are overcome.
C-S-H
C-S-H I
C-S-H II
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SEM micrographs of fractured C3S pastes (w/c = 0.4) in pure water at (A) 7 days, (B) 13 days, (C) 1 month of hydration
Hydration products II
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Technische MineralogieETHZ IMP 2008
Hydration products III
Early Porous C-S-H gel (Eternite shingle, 2100x)Late dense C-S-H gel (Eternite shingle, 800x)
Hydration of cement
Institut de Minéralogie et PétrographieUniversité de Fribourg
Technische MineralogieETHZ IMP 2008
Hydration products IV
Lathshaped AFm (sulfatefree) crystals (3900x) Ettringite (sulfatefree) crystals (1500x)
Hydrogarnets (1500x)
All images are from fiber concretesamples.
Hydration of cement
Institut de Minéralogie et PétrographieUniversité de Fribourg
Technische MineralogieETHZ IMP 2008
Polymerisation degree of silicate anions during the hydration cement
Structure of C-S-H gel I
Hydration of cement
Institut de Minéralogie et PétrographieUniversité de Fribourg
Technische MineralogieETHZ IMP 2008
Structure of 1.4 nm tobermorite, a sheet like silicate composed ofoctahedral layers and silicate chains. The silica tetrahedra can be replaced by hydroxil ions. If part the bridging tetrahedra (B) are replaced only paired groups remain explaining the dimer signal in NMR studies.
Structure of C-S-H gel II
Hydration of cement
Institut de Minéralogie et PétrographieUniversité de Fribourg
Technische MineralogieETHZ IMP 2008
Structure of C-S-H gel III
Hydration of cement
Institut de Minéralogie et PétrographieUniversité de Fribourg
x
c
Structural waterAdsorbed waterCapillary poreC-S-H layerC-S-H particleC-S-H gel models
Technische MineralogieETHZ IMP 2008
• Concrete strength, durability, and volume stability is greatly influenced by voids in the hydrated cement paste
• Two types of voids are formed in hydrated cement paste– interlayer hydration space (gel pores)– capillary voids
• Concrete also commonly contains entrained air and entrapped air• Interlayer Hydration Space
– Space between layers in C-S-H with thickness between 0.5 and 2.5 nm
– Can contribute 28% of paste porosity– Little impact on strength, permeability, or shrinkage
• Capillary Voids– Depend on initial separation of cement particles, which is
controlled by the ratio of water to cement (w/c) – On the order of 10 to 50 nm, although larger for higher w/c – Larger voids effect strength and permeability, whereas smaller
voids impact shrinkage
Hydration of cement
Institut de Minéralogie et PétrographieUniversité de Fribourg
Voids in Hydrated Cement
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w/c is 0.5 for (a)
is 1.0 for (b)
Hydration of cement
Institut de Minéralogie et PétrographieUniversité de Fribourg
Volume relationships
Technische MineralogieETHZ IMP 2008
Hydration mechanisms in Portland cement I
Hydration of cement
Institut de Minéralogie et PétrographieUniversité de Fribourg
Technische MineralogieETHZ IMP 2008
Hydration of cement
Institut de Minéralogie et PétrographieUniversité de Fribourg
Hydration mechanisms in Portland cement II
Technische MineralogieETHZ IMP 2008
Hydration of cement
Institut de Minéralogie et PétrographieUniversité de Fribourg
Hydration products I
X-ray microscopy images of C3S in a solution saturated with portlandite and gypsum after 14 min (left) and 31 min (right). The fibrous phase is C-S-H that forms at the surface (scale bar 1micron).
Technische MineralogieETHZ IMP 2008