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Science and engineering of glass and natural stone in construction
The vitreous stateF. Wittel
1
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The vitreous state
From melts to glasses:Thermodynamic aspectsMicro-structural aspects
Glass in natureIgneous, metamorphic and sedimentary glass
Synthetic glassThe discovery of glassChemical composition of glassRaw materials
Durability of glass
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Teaching goals:
You will
…learn about the nature of glass from different perspectives and will have a first look into glass formation.
… get to know natural glass
…hear the story of the invention of glass, learn about chemical compositions of the most important building glasses
… learn about raw materials and batch compositions
… combine what you learned to realize that durability of glass is just a consequence of everything.
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Understanding glasses: what is it?
Glass is …
… a transparent, shiny body obtained by smelting sand or grave with an alkali and salt, that is used in
diverse ways (practical) D.J.G. Krünitz, Oeconomische Encyclopedie 1779
… a solid, non-crystal material (structural)
… a super cooled liquid that solidifies without crystallization (Gustaf Tamman (1861-1938) , Der
Glaszustand)
… an amorphous mixture of basic and acidic oxides (chemical)
… and inorganic melting product that solidifies without crystallization (DIN 1259-1)
… a solid being constituted by a spatial, disordered network of building blocks with low coordination
number (structural) W.L. Zachariasen (1932), B.E. Warren (1933)
… all non-crystalline, solid material are in the glassy state
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Glass basics: The V-T-Diagramm
Network structureStrongly interconnected wide open
Heat expansion by asymmetric potentials+
expansion by changes of network structure
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Glass density depends on cooling rate
Small rate leads to higher density, higher rate to low density (up to 20%)
Reason: Molecule can not reach thermodynamically
preferred higher packing due to fast increase in viscosity
Glass temperature depends on cooling rates
Glass basics: Dependence on cooling rate
01 /th
ll
T
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Basics: Glass – a definitionNon-crystal solid with amorphous structure Glassy state
Crystalline StatePeriodic lattices
• All bond of identical strength/ energy• precise melting point
Vitreous state• Frozen, disordered structure
• Increased viscosity when cooled transformation regime
• Glass transition at the end of the transformation regime• Sudden change in heat expansion• Decrease of specific heat cp
Experiment: Glass vs. Tin
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Glass summaryglasses Crystalline materials
Transformation regime (TR) Precise melting point T_s
Dilatation in TR like liquid Discontinuity in volume at T_s
liquid liquid
Irregular network(irregular bonding angles and distances) no long range
order (like a liquid) isotropic , frozen super cooled liquid of extremely high viscosity (1019dPas RT)
Regelar, periodic arrangement, long range order anisotropic
Strong and weak bonds neighbour each otherSolidification regime
Bonds with similar strength Melting point
Silica Glass Silica Crystal (rock crystal)
meltingAnd cooling
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Can be taken by
quite a number of materials
The vitreous state
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The vitreous state: Micro-structural aspects
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Structure theories: Crystallite hypothesis by A. Lebedev
Glass as an assembly of minute crystalline ordered regions (~1.5nm), so called micro crystallites
Ordering is highest in the center of the micro crystallites, but decays towards the exteriors
Micro crystallites are bonded to each other by an amorphous intermediate layer.
Submicroscopic crystallites are so small, that they can not be called crystals any more.
No difference to network hypothesis
Historical value lies in the first hypothesis with focus on inhomogeneity in glasses.
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Structure theories: Network hypothesis by Zachariasen and Warren
Energy difference between vitreous and crystalline state more or less indistinguishable Identical chemical bonding and structural unit
If glass is a frozen super cooled liquid, then the structure of liquids is the one of the solid Molecules are disordered
Glasses with SiO2 as network former, silicate SiO-4-tetrahedra can be arranged in a regular or
an irregular 3D random statistical network.
Symmetry and periodicity is missing.
Differentiation between network formers and modifiers.
Crystalline quartz (2D/3D) Vitreous quartz (2D/3D)
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Cation-anion-packing: Sphere model
Coordination-number
3 4 6 8 12 20
rcat/ran2
3 13
31
2 2 1 3 1 1
2 2 ( 5 5 ) 1 12 3 (1 5 ) 1
Cations have to fill the cation gap entirely. If they are smaller, the structure collapses to the next lower coordination number.
Tetrahedral gap for cation-anion-radii rate of 0.225<rcat/ran<0.414.
Structures are not allowed to rattle when being vibrated.
Example: r(Si4+)=0.041nm; r(O2-)=0.14nm rcat/ran=0.293
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Network former silica glasses: atomic shellSi: 4 valence electron (like C)
Ground state 3s2p2 hybridized sp3 tetrahedral structure (109.5°)
[SiO4]4- Tetrahedron is short range order
Hybrid orbital has larger electron cloud than atom orbital large overlap volumes are possible
(additional gain of binding energy is the main reason for hybridization)
[SiO4] Tetraedron (nesosilicate)
109.47°Bonding angle
2-
4+
2-
2-
2-
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Excursion: Silicate formations
Polymerization of neso-silicated by ≡Si-O-Si ≡ -covalent bondings.
Oxygen is bridge forming oxygen.
Si-Si distances in SiO-structures
Zeolithe
Tectosilicates
Phyllosilicat
Inosilicates
Sorosilicate -quartz
Amorphous Silicate
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Rules for vitrificationNetwork former / modifier make the molecular skeleton of glass basically no other substances are needed
Coordination number of the cation has to be small (3 or 4). (Zachariasen)
Connection of tetrahedra only via joined vertices and not edges or surfaces (max. distance of cations)
Network former mainly acidic oxides with radii ratio cation/oxide anion 0.2-0.4.
Anion should not be bound to more than 2 cations.
Sum of electrons in the p-orbitals divided by the number of atoms has to be >2.
Example SiO2:
(1*2+2*4)/3=3.33>2
strong tendency for
vitrification
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Diezel’s filed strength
2 2
2 20 0
1,
4 4c a t a n a n c a t
c a t a n
D ie ze lsf ie lds tr e n g thF
z z e z e zf a r r
a a
Dietzel’s Field strength F
Ion radii and Diezel’s field strength
Estimates for the behavior of a certain element in a glass network
Element Valence
Z
Ionic
radius(forCN=6)
r in Å
Most
frequentcoordinationnumber CN
Ionic
distance foroxides a inÅ
Field strengthat distance ofO2 ions Z/a2
Function inglass
structure
K 1 1.33 8 2.77 0.13
Net
wor
km
odifi
er
Z/a
2 ~0.
1-0.
4
Na 1 0.98 6 2.3 0.19Li 1 0.78 6 2.1 0.23Ba 2 1.43 8 2.96 0.24Pb 2 1.32 8 2.74 0.27Sr 2 1.27 8 2.69 0.28Ca 2 1.06 8 2.48 0.33Mn 2 0.91 6 2.23 0.4Fe 2 0.83 6 2.15 0.43Mn 2 0.83 4 2.03 0.49
Inte
rmed
iate
Z/a
2~
0.5-
1
Mg 2 0.78 6 2.1 0.454 1.96 0.53
Zr 4 0.87 8 2.28 0.77Be 2 0.34 4 1.53 0.86Fe 3 0.67 6 1.99 0.76
4 1.88 0.85Al 3 0.57 6 1.89 0.84
4 1.77 0.96Ti 4 0.64 6 1.96 1.04B 3 0.2 4 1.5 1.34
Net
wor
kfo
rmer
Z/a
2~
1.5-
2
Ge 4 0.44 4 1.66 1.45Si 4 0.39 4 1.6 1.57P 5 0.34 4 1.55 2.1B 3 0.2 3 1.36 1.63After Diezel
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Natural glasses
Earth, moon, meteoroids.. Glasses are
abundant in the universe.
Glass formation…
… by amorphous solidification products of
volcanic melts (volcanic glass)
… by meteoroid impacts (impactites, tectites)
… by lightening strokes (fulgurites)
… by rockslides (frictionites)
… by shock waves (diaplectic glass)
… by biology (glass sponge)
||Institute for Building Materials lunar volcanic glasses, Apollo 15 mission
Apollo 17 pyroclastic orange
Apollo 15 pyroclastic green glass
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Natural igneous glass: Pyroclastic glass
Volcanic rock in amorphous state
No own rock type but a certain structural rock fabric
Originates from quenching of pyroclastic flows by water or ice
Pumice stone cellular, porous glass formed by explosive eruptions of gaseous magma.
Obsidian; volcanic glass with different names, depending on chemical composition. rhyolitic (silica rich), phonolitic, andesitic etc. obsidian. Water content < 1%.
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Natural metamorphic glass: Glass from Meteorite impacts
Impactite• Meltet material at the impact location• Melt quenches at the place of impact with inclusions from the impactor• Can be found in the surrounding of the crater• Examples: Libyan desert glass (LDG), Suevite
Tektite• Impact of big meteorides• Plasma is ejected into the atmosphere and cooled down without
inclusions• Can be found several hundred of km distant• Example: Moldavit, Indochinite
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Natural metamorphic glass: Formed by lightening strikes
Lightening strikes in sandy soils (Beach) T> 1800°C
Fulgurite (lat. fulgur=thunderbolt) «petrified lightening"
Natural hollow glass tubes with diameter up to several cm and length of several meters with branches
Penetration depth up to 15 meters below the surface
Color and composition depends on the soil type (black to white)
Very smooth interior with small blisters, rough outside with sand grains
Lightening strike in solid rock exogenic fulgurite
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Markus Kayser – Solar Sinter Project
Sand Babel Wolkenkratzer
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Natural glass: vitrification by shock metamorphis
Vitrification not by a super cooled melt, but by an external force by shock waves
lattice structure of crystals is destroyed without going through the liquid phase
Shock waves by meteorite impacts or nuclear weapon tests
In meteorites Maskelynite is found, that is a diaplectic glass with the composition of Plagioklas
Special type of impact glasses that originate from shock wave metamorphis.
Lunar sample 78235.
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DevitrificationGlass is as old as the universe. But why are there no volcanic glasses as old as the universe or even the Precambrian (>4.5Billion years)?
Glasses are in a metastable state Devitrification (crystallization) in geological time scales Thermodynamic stable crystal structure starting form crystal seeds. today entirely recrystallized.
Snowflake obsidian is in the state of Crystallization to SiO2 Cristobalit
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DevitrificationCrystallization below the transformation regime.
Aging by pressure and temperature.
Exsolution of crystalline silica and field spar crystals.
Loss of strength, increased hardness, anisotropy, increased opacity.
24-48 hours close to the melting point and slow cooling. Reaumur’s porcelain.
Quartz glass is strongly endangered.
Devitrification layer that grows into the material (ß-Cristobalit).
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Sodium Oxide
Stabilized SiO2 backbone
Stabi-lizer
Soluble glass
Soluble glassNetwork former
Network modifier
The discovery of synthetic glasses
Discovery about 5000B.C. by Phoenician traders in Lebanon (following Plinius the Elder «Historia naturalis» 23-79n.Chr.)
Fireplace in between nitrate blocks on the beech
Liquefaction of the blocks with the sand by the temperatures of the fire
Opaque, glassy substance
Stabilization:
≡Si-O-Na + Na-O-Si≡ + Ca-O ≡Si-O-Ca-O-Si ≡ + Na-O-Na
Reaction to form sodium silicate (Soluble glass)
≡Si-O-Si≡ + Na-O-Na ≡Si-O-Na + Na-O-Si ≡
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Network formerThe condition of electro neutrality leads to the rule that only stoichiometry has to be fulfilled.:
Quartz crystal
M2X3 MX2 M2X5 Electron sum
Silicon dioxide SiO2 x 3.33
Bor trioxide B2O3 x 2.8
Phosphor pentoxide P2O5 x 3.71
Germanium GeO2 x 3.3
Arsenic / Diarsenic trioxid As2O3 x 3.6
Antimony Sb2O5 x 3.71
Ion radii
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Network modifierSince glasses have no texture, the properties have to be influences via chemistry of bondings via foreign ions!Network modifiers split up the network and reduce the number of connections smaller glass temperature and viscosity.
Modifiers are normally alkaline oxides with large cations:Sodium oxide (Na2O) ↓ Lime (CaO) chemical resistance ↑Potassium oxide (K2O) glass is getting longer; Lithium oxide (Li2O) ↓↓ More rare: Barium oxide, Niobium oxide, Rubidium oxide, Strontium oxide, Cesium oxide (CsO), Tantalum(V)-oxide, Tellurium oxide
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Network modifiers
Manipulation of structure and hence mechanical and chemical properties of glasses
Production from inexpensive carbonates:
High corrosion resitance against acids and bases
High glass temperature
Decrease of viscosity
Increase of electrical conductivity
SiO2 content
high lower
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Network modifier for soda-lime glassOpening of the SiO network by calcium and sodium oxide
1. Formation of independent chain endings:
covalent bonding (BO) Ionic bond (NBO)
2. Closing of endings/ ionic bond with metal cation:
[SiO4] Tetrahedron
Soluble glass
O-
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Intermediates
Take position in between network formers and modifiers.
Can not form one component glass
Examples:Manganese(II)-oxide (MnO) glass gets longer
Alumina (Al2O3) glass gets longer, mech. strength ↑, chem. resistance ↑
Lead oxide (PbO) Tg ↓, diffraction number ↑, el. resistance ↑, absorption of X-rays ↑
Titanium dioxide (TiO2) diffraction number ↑, acidic resistance ↑
Zirconium(IV)-oxide(ZrO2) chemical resistance↑, opacifying agent for enamel
Zinc oxide ZnO hardness ↑, acts as flux, Tg ↓, devitrification ↓, degassing ↑;
Polonium oxide (PoO) Tin(II)-oxide (SnO) Cadmium-oxide (CdO) Beryllium oxide (BeO) Thorium-oxide (ThO2) Selenium(IV)-oxide(SeO2) Iron(II)-oxide (FeO) Iron(III)-oxide (Fe2O3) Nickel(II)-oxide (NiO) Cobalt(II)-oxide (CoO)
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Glass recipes - glasses become transparent
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Glass recipes – glasses become transparent
«Take 60 parts of sand, 180 parts of ash from marine plants, 5 parts of char – and you get glass» oldest glass recipe by the Assyrian king Assubanipal (7. B.C.)
Glass does not have a clearly defined chemical composition, it is a mixture of metallic oxides and other chemical elements and components.
Building blocks of glasses are oxides of Si, B, Al, Mg, Ca, Ba, Pb, Zk, Li, Na, K
Chemical analysis always refers to the element in form of its oxide.
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Composition of some important glasses
Glass type/ weight % SiO2 Al2O3 Na2O K2O MgO CaO B2O3 PbO TiO2 F As Se Ge Te
Quartz glass 100 – – – – – – – – – – – – –
Soda-lime glass* 72 2 14 - - 10 - - - - – – – –
Float glass 72 1,5 13,5 - 3,5 8,5 - - - - – – – –
Lead glass 60 8 2,5 12 - - - 17,5 - - – – – –
Boro-silicate glass 80 3 4 0,5 - - 12,5 - - - – – – –
E-glass 54 14 - - 4,5 17,5 10 - - - – – – –
Enamel 40 1,5 9 6 1 - 10 4 15 13 – – – –
Chalcogenide glass 1 – – – – – – – – – – 12 55 33 –
Chalkogenide glass 2 – – – – – – – – – – 13 32 30 25
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Overview glass types
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Classification of glasses 1
Hard glass Soft glass
High resistivity againt chemical attacs Low production costs
High cooling temperatures Easyer melting and forming
High thermal resistivity
Boro-silicate glasses Soda-lime glass; lead glass; non-silicate glasses
Oxydic glass Non-oxydic glass
Silicate glasses ; Soda-lime glass Nitrateglass, Fluorideglass
Mixtures of diverse glasses like boro-silicate glasses
Chalcogenide glass
Non-silicate glass like borate glass, phosphate glass
Metallic glass
Polymeric glasses like PS, PMMA …
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Oxidic glasses: silicate glass
Aluminosilicate glass Lead silicate glass
high contents of aluminum oxide Al2O3
(15-25%) along with low sodium oxides
high amounts of lead oxide (>10% up to 30%)
High electrical resistanceHigh chemical resistance
Increased light refractionLow electrical conductivityLow viscosity and melting temperatureIncreased absorption of X-rays
LCD flat panel displaysFiber-glass (E-glass)Fire protection glazingHalogen lightsCombustion pipes
Optical glassRadiation protection glazing
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Oxidic glasses: silicate glass
Quartz glass (Silica glass) Soda-Lime-Glass
SiO2 100% Silicon dioxide with network modifiers like Sodium oxide and limeSiO2 72%; Na2O 14.5%; CaO 8.5%Al2O3 1.5%; MgO 3.5%
Low heat expansion coefficientHigh UV- transmissivityExtremely good chemical resistivityTemperature resistant up to 1400°CHigh electric conductivity
Low softening temperatureLow chemical resistivityHigh heat expansion coefficient
Chemical glassware, glass fibers Window glass, mold glass, packaging glass
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Oxydic glasses: Glass mixtures
Boro-silicate glass (Duran)
Mixtures of silica and boro trioxide with additions: Na2O-B2O3-SiO2
Good fusabilityHigh chemical resistivityLow heat expansion coefficientHigh thermal resistivity
Lab glass
TechnicalBoro silicate glass:
in wt% Jenaer Geräteglas 20
Jenaer Duranglas
Jenaer Rasothermglass
Pyrex (USA)
SiO2 76 74 78 80.8
B2O3 7 14 12.5 12
Na2O 6.5 4.5 5.5 4.3
BaO 4.0 3.0 - -
Al2O3 4.5 3.5 3.0 2.2
Thermal expansion 10-7 [-/K] a10-100=46 a10-100=38 a10-100=33 a10-300=33
Tb [°C] 550 534 527 560
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Oxydic glasses: Non-silicate glasses
Borate glass Phosphate glass
B2O3 40%Al2O3 30%CaO 30%
P2O + Additions
High electrical resistanceAddition of PbOHigh light diffractionLow chemical resistivity
Addition of BaOHigh light diffractionLow chemical resistivity
Optical glasses Heat insulation glass, optical glass
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Adjustment of glass propertiesStatistical analysis based on glass-datenbancs like SciGlass or Interglas.
Large databanks for glass properties (SciGlass> 360.000 different glass compositions).Prediction of diverse compositions by regression analysis.Basically all physical and chemical properties of glasses and glass forming melts.• Different interpolation schemes for wide ranges of concentration.• Ternary phase diagrams for vitrification• Optical spectra.
Crystallization or phase changes are not allowed to happen within the scheme
01 1
n n
i i ik i ki k
G la s s p ro p e r ty b b C b C C
b variable coefficientn number of glass componentsC concentration of component
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Variations in density 2-6g/cm3; Density SiO2 as quartz 2.65/ glass 2-2.2g/cm3
Loosened structure, path dependent
Addition of alkali oxides increases glass density:
opening of the network vs. filling of voids
Due to higher atomic weight, the density increases.
Estimate:
BinaryAlkali-silicate glasses
1 0 0
/i ii
p
Oxide i (g/cm3) Oxide i (g/cm3)
SiO2 2.24 As2O5 3.33
Al2O3 2.75 CaO 4.3
B2O3 2.9 ZnO 5.94
Na2O 3.2 BaO 7.2
K2O 3.2 PbO 10.3
MgO 3.25
Adjustment of glass properties: Density
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Relation between thermal expansion and chemical composition of glass is rather linear.
Linear model can be used:
pn percentage of weight of each constituent
kn constants
High expansion factors of sodium oxide point at low thermal resistance of soda-lime glass.
3 n nk p
Oxide constant Oxide constant
SiO2 15 MgO 135
Al2O3 52 CaO 489
ZrO2 69 ZnO 21
Na2O 1296 BaO 520
K2O 1170
Adjustment of glass properties: Heat expansion
Values factored by 109 for clarity.
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Raw materials for glass
Glass products
facilities
Raw materials energy
primary, minerals (Sand, fieldspar, lime stone, Dolomite,….)Primary, synthetic (Soda, Sulfates, colorants)Secondary (cullet)
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Quality + Availability = price
• Chemical composition: Main components, impurity (e.g. Fe-content), moisture content, etc.
• Phases: main phase, critical phase
• Grain habitus• Grain size distribution• Uniformity of quality
• Local / global market• Local production vs. Import
dependence (Stability of exporting country)
• Natural vs. Industrially produced
• Glass industry main or secondary customer
• Transportation distance (needed storage)
Raw materials for glass
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Primary raw materialsElement Oxide Raw material
Si SiO2Sand cullet
Ti TiO2Illmenite, FeTiO3 TiO2
Zr ZrO2Zirconium, ZrSi04 ZrO2
Al Al2O3fieldspar(Ba,Ca,Na,K,NH4)(Al,B,Si)4O8
Nephelinite Metal furnaceslag
Phonolith Kaolinite
Al(OH)3 Al2O3
B B2O3Borax H3BO3 B2O3 Colemanite Tincal/Borax
Fe Fe2O3Red iron oxide FeS FeS2
Cr Cr2O3Cr2O3 K2Cr2O7
Na Na2O Trona Na2CO3 NaOH
K K2O Potash, K2CO3
Ca CaO Lime stone
Mn MnO MnO2 MnCO3
S SO3Na2So4 K2SO4 CaSo4 Gips BaSO4
Pb PbO PbO Pb3O4
Mg MgO Dolomite, CaMg(CO3) 2 MgCO3
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Quartz sand: grain size <1mm; almost pure SiO2; small contamination with Fe2O3 (green coloring); network former.
Soda: Soda; Na2CO3; NaO-carrier, lowering of melting point of SiO2; flux; network modifier. CO2 is released refining
Potash: Potassium carbonate K2CO3; brings Potassium oxide into the batch; network modifier and flux.
Field spar: NaAlSi3O8; Increase of hardness and stabilization
Lime: Network modifier; Increase of strength and resistance.
Dolomite: Carrier for CaO and MgO, acts like Lime.
Cullet: Significant decrease of energy use but bad color separation, foreign metals, ceramics and special glasses included not usable for window glass.
By careful selection of raw materials, the iron content can be significantly reduced clear glass.
Soda-lime glass: raw materials
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Raw materials: A glimpse into the past
Egypt1500. BC
Rome 100 AD
Europe 1300 AD
Syria 1400 AD
Today
SiO2 65 68 53 70 73
Soda, Na2O 20 16 3 12 16
Potash, K2O 2 0.5 17 2 0.5
Lime, CaO 4 8 12 10 5
Magnesium, MgO
4 0.5 7 3 3
Batch Plant ash, Quartz Soda, Sand Potash, Sand/Quartz
potash, Sand/Quartz
Syntheticcomponents
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New processes
Leblanc-Process
Solvay-process
I.
II.
III.
IV.
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New processes
Trona-processTrona (trisodium hydrogendicarbonate dihydrate); Na3(CO3)(HCO3)•2H2O
Largest deposits close to Green River Wyoming (dried-up, covered lakes)
Entirely replaces Solvay-Process in the USA.
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ETH Zürich, HIF E
Chemical attack by…1. Hydrofluoric acid2. Aqueous acids3. Alkali
Water & combined acid/base attack
Glass corrosion
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Chemical resistance of glass
Attack by hydrofluoric acid
Hydrofluoric acid dissolves the silicon dioxide backbone and forms SiF. In aqueous solution if further reacts to Fluorosilic acid:
SiO2 + HF SiF4 + H2O;
SiF4 + 2HF H2(SiF6)
Easily dissolvable silicon hexafluoride SiF6
Is formed.
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Attack by aqueous acids
Ion exchange reaction – Protons of the acid replace cations in the glass.
Reaction: -Si-O-Na + + H + -Si-OH + Na +
Due to the reaction the acid depletes with protons, the pH value increases.
A silicate layer, saturated with protons is formed, that acts as a diffusion barrier for further attack passivation
Chemical resistance of glass
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Attack by alkali
Entire dissolution of the silica backbone, attack on the bridging oxygen.
SiO2 molecule is dissolved and washed away.
Always new surfaces are formed no passivation
Severity of alkali attack decreases in the order:
NaOH KOHLiOHNH3
Chemical resistance of glass
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[SiO4] tetrahedron
Ionic end of chainHydroxide ion
Hydroxideion
Gla
s sk
inV
olu
me
stru
ctu
re
Chemical resistance of glass
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Case 1 passive layer Formationtd c
ted t
Case 2 competing reactionsDiffusion dissolution
c t c t
Case 3 constant dissolution d c ad t
d c a td t
Chemical resistance of glass: EvolutionType I: Formation of a passive surface layer, e.g. silica glass in neutral solution. The dissolution rate is dc/dt ∞ te-at .Type II: Protective layer by leaching of alkali, but network is unaltered. Example is and aqueous acid on silica glass.Type III: Leaching and surface reaction lead to two protective layers of different constitution, but network remains stable.Type IV: Leaching and dissolution take place simultaneously and leaching layer grows into the network. One example is alkali glass in water. Two competing reactions are diffusion c∞t1/2 and dissolution c∞t.Type V: Continuous dissolution of the network without leaching zone. Hydrofluoric acid on silica glass is one example, with a constant dissolution rate of dc/dt∞a.
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Chemical resistance of glass: Evolution
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Classes of chemical resistivity
DIN 12112 DIN 52322 DIN 12111
Acid class
solubility in acid
Half of the surface weight loss after 6h [mg/dm2]
Caustic class
solubility in base
Surface weight loss after 3h [mg/dm2]
Hydrolytic class
HCl usage
[ml]
Acid equivalent as Na2O
[mg/g]
1 none 0-0.7 1 Weakly 0-75 1 <0.1 <31
2 Weakly 0.7-1.5 2 moderate 75-175 2 0.1-0.2 31-62
3 Moderate 1.5-15 3 strongly >175 3 0.2-0.85 62-264
4 Strongly >15 4 0.85-2 264-620
5 >2 620-1085
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Teaching goals:
You will
…learn about the nature of glass from different perspectives and will have a first look into glass formation.
… get to know natural glass
…hear the story of the invention of glass, learn about chemical compositions of the most important building glasses
… learn about raw materials and batch compositions
… combine what you learned to realize that durability of glass is just a consequence of everything.
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Thank you for your attention.
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