a physico-geometric approach to solid-state reactions by
TRANSCRIPT
Nobuyoshi KOGAGraduate School of Education
HIROSHIMA University
A Physico-geometric Approach to Solid-State Reactions by Thermal Analysis
OUTLINE
Theme:How to characterize the overall kinetics of the solid-state reactions from physico-geometric points of view?
Contents:(1) Physico-Geometry of Solid-State Reactions(2) Kinetic Model Functions(3) Kinetic Equations(4) Application of Thermoanalytical Method(5) Sample Controlled Thermal Analysis(6) Concluding Remarks
Surface Nucleation (1)ex. Thermal Decomposition of Solids
Reactant Surface one of the most reactive sites
Reaction initiates by nucleation and growthSurface defects and dislocationsCrystallographic directionReaction atmosphereOthers
Nonisothermal dehydration of α-NiSO4⋅6H2O to tetrahydrates under flowing N2.
Surface Nucleation (2)
□ Relation to Crystallographic Direction
plate-like single crystals with stacking layer structure
Edge surfaceThe most reactive sitesProduct nuclei appear parallel to the most developed surface (010)
Isothermal dehydration of zinc acetate dihydrate to anhydride under flowing N2.
Surface Nucleation (3)
□Influence of Reaction Atmosphere
At a reduced pressure of 1.5 hPa
Under flowing N2
Formation of trihyrate nuclei
Formation of monohydrate nuclei
Isothermal dehydration of copper(II) sulfate pentahydrate
Surface Nucleation (4)
□Structure of Product Nuclei
Isothermal dehydration of copper(II) sulfate pentahydrate to trihydrate.
Surface Nucleation (5)
Classification of Product NucleiClassification Characteristics Example
Fluid-flux Retention of a volatile product at interface condensed as liquid
Dehydration of alumKBr+Cl2→KCl+BrCl
FusionProduct melting facilitates reaction
Decomposition of ammonium dichromate and copper(II) malonate
FunctionalStrain and/or heterogeneous catalytic breakdown of intermediate at reaction interface
Decomposition of copper(II) formate, nickel formate, nickel aquarate and silver malonate
Flux-filigree Two-zone structure of reaction interface
Dehydration of Li2SO4·H2O
Reaction Interface (1)
A zone of locally enhanced reactivity located at reactant/product contactReaction Interface
Reaction proceeds by advancement of reaction interface towards the center of reactant crystal
Crystallographic directionShape of reaction frontStructure of reaction
interfaceIsothermal dehydration of copper(II) acetate monohydrate
Reaction Interface (2)Example (1)
Wavy frontSurface nuclei Growing hemisphericallyoverlap
Isothermal dehydration of lithium sulfate monohydrate to anhydride
Reaction Interface (3)Example (2)
Reaction front
A saw-like shape
Product layer
A repeated stacking of dense and coarse aggregates of the product crystallites
Isothermal dehydration of copper(II) sulfate pentahydrate to trihydrate
Reaction Interface (4)Example (3)
Reaction front Needle-like product crystallites
Penetration to reactant crystal
Surface nucleation at edge surface of plate-like crystal 2D-shrinkage
Isothermal dehydration of zinc acetate dihydrate
Reaction Interface (5)Example (4)
Reaction Interface An optically different layer of 20~50mm thickness
Isothermal dehydration of copper(II) acetate monohydrate
Reaction Interface (6)
A Model of Reaction Interface
What is taking place?
ex. Thermal dehydration• Water mobility within the
crystalline reactant.• Diffusive migration of water to
crystal edge or interface.• Water volatilization at the
crystal edge of interface.• Chemical reaction, if any.• Recrystallization of solid
reactant to product structure.• Water vapor adsorption/
desorption on product solid.• Intranuclear diffusive escape of
water and loss beyond crystal.
Kinetic Model Function(1)A hypothetical transfer from homogeneous to heterogeneous model
Kinetic Model Function(2)Typical kinetic model functions for solid-state reaction
Model Symbol
Nucleation & Growth Am (0.5≤m≤4)
Phase Boundary Controlled Rn (1≤n≤3)
D1 (one D)
D2 (two D)
D3 (three D)
D4 (three D)
Diffusion Controlled
( )tk
fdd1 α
α = ( ) ( ) ktf
g =∫=α
ααα 0
d
( ) ( )[ ]m m1 1 1 1− − − −α αln / ( )[ ]− −ln /1 1α m
( )n n1 1 1− −α / ( )1 1 1− −α / n
12α α2
( )−
−1
1ln α α + 1 −α( ) ln 1−α( )
( )( )
3 1 2 3
2 1 1 1 3−
− −⎡⎣⎢
⎤⎦⎥
α
α
/
/ ( )1 1 1 3 2− −⎡
⎣⎢⎤⎦⎥
α /
( )3
2 1 1 3 1− − −⎡⎣⎢
⎤⎦⎥
α / ( )1 23
1 2 3− − −α α /
Kinetic EquationGeneral Kinetic Equation
( )αα kft=
ddPhysico-geometric Kinetic
Model Function
Temperature Dependence of rate constant
Other functional dependence of reaction rate
⎟⎠⎞
⎜⎝⎛−=
RTEAk exp
( ),.....,,dd PTa
tαα
∝
( ) ( ),.....,,expdd PTaf
RTEA
tααα
⎟⎠⎞
⎜⎝⎛−=
( ) 1,.....,, =PTa αIdealized Kinetic Equation
( )αα fRTEA
t⎟⎠⎞
⎜⎝⎛−= exp
dd
Application of TA
Technique Measuring Property Kinetic Rate Data
DTA Temperature difference (Tp, αp)
TG Mass change (dα/dt, α, T, t)
DSC Heat flow rate (dα/dt, α, T, t)
EGA Evolved gas (dα/dt, α, T, t)
Isothermal Analysis(1)
(1) Measurement of Isothermal mass-loss data
0 50 100 150 200 250 3000
50
100
150
200
250
300
T
/ °C
-4
-3
-2
-1
0
DTG
TG
∆m
/ m
g
-0.03
-0.02
-0.01
0.00
0.01
0.02
0.03T
(d∆
m/d
t) / m
g m
in-1
Isothermal Analysis(2)(2) Determination of rate constant k
(b) Integral( )αα kf
t=
dd(a) Differential
( ) ktg =α
0 10 20 30 400.0
0.1
0.2
0.3
0.4
0.5
0.6
0.7
0.0
0.5
1.0
1.5
2.0
2.5
3.0
0.00 0.02 0.04 0.060
5
10
15
20
25
30
0.0
0.5
1.0
1.5
2.0
D3
R2 A1
D2
(b) Integral
g(α)
t / min-1
D3
D2
R2
f(α)
(dα/dt) / min-1
(a) differential
A1
Isothermal Analysis(3)
(3) Determination of E & A
3.02 3.04 3.06 3.08 3.10 3.12 3.14-10.0
-9.5
-9.0
-8.5
-8.0
-7.5
-7.0
D2:
Ea=106.5±5.4 kJ mol-1
A1: Ea=106.6±5.4 kJ mol-1
ln k
/ s-1
T-1 / kK-1
Arrhenius plot
RTEAk −= lnln
Nonisothermal Analysis(1)
(1) Measurement of Nonisothermal rate data
0 40 80 120 160 200 240100
150
200
250
300
350
400
T
T
/ °C
-4
-3
-2
-1
0
DTG
∆m /
mg
-0.08
-0.06
-0.04
-0.02
0.00
0.02
TG
(d∆
m/d
t) / m
g m
in-1
Nonisothermal Analysis(2)From single TA run2) Integral
1) Differential
At φ=const.φααφ
Tt
tTT
dd
dd
0
=
+=
( )αφα fRTEA
T ⎟⎠⎞
⎜⎝⎛−= exp
dd
( ) RTEA
fT−=⎥⎦
⎤⎢⎣
⎡⎟⎠⎞
⎜⎝⎛ ln
ddln
αφα
( )( )
( )xpR
AETRTEA
fg
T
T φφααα
α
=⎟⎠⎞
⎜⎝⎛−== ∫∫ dexpd
00
RTEx =with
( ) ( ) ( ) ( ) ( )xx
xx
xx
xxpx
π−≅
−−
−= ∫
∞ expexpexp
For example( )
xxxx /2−
=πCoats & Redfern method
1.68 1.72 1.76 1.80
-5
-4
-3
-2
-1
0
R3
A1
ln [(
dα/d
t)/f(a
)] /
min
-1
T-1 / kK-1
(a) Sharp & Wentworth
A2
------------------------f(α) Ea / kJ mol-1
------------------------ A1 234±1A2 122±1R3 184±3------------------------
( )RTE
ERT
RAE
Tg
−⎥⎦
⎤⎢⎣
⎡⎟⎠⎞
⎜⎝⎛ −=
21lnln2 φα
1.68 1.72 1.76 1.80
-16
-15
-14
-13
-12
R3
A2
A1
(b) Coats & Redfern
ln [g
(α)/T
2 ] / K
-2
T-1 / kK-1
Nonisothermal Analysis(3)From a series of TA runsIsoconversional method
( )αα fRTEA
t ⎟⎠⎞
⎜⎝⎛−= exp
dd 2) Integral
( )( )
( )xpR
AETRTEA
fg
T
T φφααα
α
=⎟⎠⎞
⎜⎝⎛−== ∫∫ dexpd
001) Differential
RTEx =withFriedman method
( )[ ]RTEAf
t−=⎟
⎠⎞
⎜⎝⎛ αα ln
ddln ( )
RTExp 4567.0315.2log −−=Ozawa method
2.20 2.24 2.28 2.32 2.36 2.40 2.44 2.48-3.5
-3.0
-2.5
-2.0
-1.5
-1.0
-0.5
0.0
T-1 / kK-1
α=0.2 α=0.4 α=0.6 α=0.8
ln (d
α/dt
) / m
in-1
(a) Friedman ( ) RTE
RgAE 4567.0315.2loglog −−=α
φ
2.20 2.24 2.28 2.32 2.36 2.40 2.44 2.48-0.2
0.0
0.2
0.4
0.6
0.8
1.0
1.2
log φ
/ K m
in-1
T-1 / kK-1
(b) Ozawa
From a series of TA runs Nonisothermal Analysis(4)Peak method Kissinger method
○ First order equation( )αα f
RTEA
t ⎟⎠⎞
⎜⎝⎛−= exp
dd
f’(α)=-1First derivative with respect to t
△ For other kinetic models( ) ( )
⎥⎦⎤
⎢⎣⎡ +⎟
⎠⎞
⎜⎝⎛−⎟
⎠⎞
⎜⎝⎛−= 22
2
expd
dexpdd
RTE
RTEAff
RTEA
tφ
αααα
At peak maximum
0 20 40 60 80 1000.50
0.55
0.60
0.65
0.70
0.75
0.80
0.85
A4
D2
D4
R2R3
A3
A2
α p
xp
A1
0dd
2
2
=⎟⎠
⎞⎜⎝
⎛
ptα
( )p
p
p RTE
EARf
T−⎥⎦
⎤⎢⎣
⎡=αφ '
lnln 2
( ) ( )ααα
dd' ff =with
Nonisothermal Analysis(5)Kinetic Master Plot
Isothermal NonisothermalIntroduction of generalized time θ
0.0 0.2 0.4 0.6 0.8 1.00.0
0.5
1.0
1.5
2.0
2.5
3.0
3.5
0.0 0.2 0.4 0.6 0.8 1.00.0
0.5
1.0
1.5
2.0
2.5
3.0
3.5
Fractional reaction α
D2
D3
D4
A4
A3
A2
A1
R3
R2f(α)/f
(0.5
)
(a) Differential (b) Integral
g(α
)/g(0
.5)
A4A3
A2
R2
R3
A1D2
D4
D3
( )( )
( )( ) 5.0dd
dd5.0 =
=αα
ααt
tff( )αα kf
t=
dd
( ) ktg =α( )( ) 5.05.0 =
=α
αt
tgg
∫ ⎟⎠⎞
⎜⎝⎛−=
ta t
RTE
0
dexpθ
( )αθα Af=
dd
( ) ( ) θθααα
θα
AAf
g === ∫∫00
dd
( )( )
( )( ) 5.0dd
dd5.0 =
=αθαθαα
ff
( )( ) 5.05.0 =
=αθθα
gg
1) Differential
2) Integral1) Differential
2) Integral
⎟⎠⎞
⎜⎝⎛=
RTE
taexp
dd
dd αθα
( )xpR
Ea
βθ =
Ambiguities of TA Kinetics(1)
Yes!!(1) For simulating the reaction process(2) For estimating life-time(3) Others
□Physico-chemical meaning of the kinetic parameters?
□Practical usefulness of the kinetic parameters?
Not answered as yet!!
Problems(1) Further detailed characterization of reaction mechanism(2) Missing functional dependence in the idealized kinetic equation(3) Reliability of the kinetic rate data measured by TA
1) Self-cooling or self-heating effects2) Self-generated reaction atmosphere3) Mass-transfer and heat-transfer phenomena4) Others
Ambiguities of TA Kinetics(2)Self-cooling effect
0 5 10 15 20 25300
350
400
450
500
550
-1.5
-1.0
-0.5
0.0
-0.4
-0.3
-0.2
-0.1
0.0
0.1
8
9
10
11
12
13
14
T
/ K
t / min
TG /
mg
TTG
β
DTA
/ µV
DTAE
ndo.
β / K
min
-1
Ambiguities of TA Kinetics(3)
Self-generated atmosphere
450 500 550 600 650 700-8
-6
-4
-2
0
2
4
6
8
-30
-20
-10
0
10
20
30
0.0
0.5
1.0
1.5
2.0
2.5
3.0
3.5
TG /
mg
T / K
CO2
Endo
.D
TA / µV
TG
DTA
H2O
Con
cent
ratio
n / g
m-3
Ambiguities of TA kinetics(4)Mass-transfere phenomena
Increase of Sample Mass
Balk or Pellet PowderDifficulty of gross diffusion of product gas through sample power matrix
Difficulty of internal diffusive escape of product gas through solid product layer
1.0
0.8
0.6
0.4
0.2
0.0
Frac
tiona
l rea
ctio
n α
6050403020100
Time / min
2.5 mg 5.0 mg 10.0 mg 20.0 mg
Li2SO4⋅H2O → Li2SO4 + H2O
CRTA(1)
Practical Usefulness of CRTA Techniques(1)Separation of overlapped reaction steps(2)Measurement of kinetic rate data(3)Process control and product control
CRTA(2)
Technique Feedback parameter
CRTG Rate of mass change
CRDL Rate of length change
CREGD Rate of total gas evolution
CREGA Rate of specific gas evolution
CREGD-TG(1)
Thermal Decomposition of Calcite
CaCO3→CaO + CO2( ) ⎟⎟
⎠
⎞⎜⎜⎝
⎛−⎟
⎠⎞
⎜⎝⎛−=
0
1expdd
PPf
RTEA
tαα
1.0
0.8
0.6
0.4
0.2
0.0
1-P/
P 0
140012001000800600
T / K
P=10-2
110
102
103
105 Pa
104
P0 in Pa = 1.87x1012exp(-19697/T)
Temperature Dependence of 1-P/P0
CREGD-TG(2)
CREGD-TG(3)
0 50 100 150 200 250 300 350
400
600
800
1000
(d∆W/dt)
∆W
T
T / K
Time / min
-2.5
-2.0
-1.5
-1.0
-0.5
0.0
Mas
s cha
nge ∆
W /
mg
-0.015
-0.010
-0.005
0.000
0.005
0.010
0.015
(d∆
W/d
t) / m
g m
in-1
Typical CREGD-TG Record
CREGD-TG(4)
0.0 0.2 0.4 0.6 0.8 1.0800
850
900
950
1000
1050
1100
0.65 mg 1.14 mg 2.01 mg 3.28 mg 5.43 mg 9.82 mg 15.31 mg 20.70 mg 42.65 mg
T /
K
Fractional reaction α
Effect of Sample MassHow to change decomposition rate for kinetic calculation?
(1)Control pressure
(2)Sample mass
(3)Basal pressure
CREGD-TG(5).1
0
constPP
≈⎟⎟⎠
⎞⎜⎜⎝
⎛− ( )[ ]
RTEAf
t−=⎟
⎠⎞
⎜⎝⎛ αα ln
ddln
1.04 1.08 1.12 1.16 1.20
-11
-10
-9
-8
-7
α=0.80.6 0.4
0.2
0.65 mg 1.14 mg 2.01 mg 3.28 mg 5.43 mg 9.82 mg 15.31 mg 20.70 mg 42.65 mg
ln (d
α/d
t) / s
-1
kK / T
Friedman Plot
CREGD-TG(6)
0 200 400 600 800300
400
500
600
700
800
900
1000
1100T
/ K
Time / min
-20
-16
-12
-8
-4
0
(d∆W/dt)
∆W
T
Mas
s cha
nge ∆W
/ m
g
-0.06
-0.04
-0.02
0.00
0.02
0.04
0.06
(d∆
W/d
t) / m
g m
in-1
Typical Rate-jump CREGD-TG Record
( )( )2
1
21
21
d/dd/dlntt
TTTTRE
αα
−=
CREGA-TG(1)
CREGA-TG(2)
300 400 500 600 700-4
-3
-2
-1
0
1
Mas
s cha
nge ∆
W /
mg
T / K
-6
-4
-2
0
2
4
6
∆T / µV
TG
DTA
DTG
-0.30
-0.25
-0.20
-0.15
-0.10
-0.05
0.00
0.05
(d∆W
/dt)
/ mg
min
-1
Thermal decomposition of synthetic
malachite TG-DTA
Smooth
Single Stepmass-lose process
E≈190 kJ mol-1
First Order Reaction
Kinetics
Cu2CO3(OH)2 → 2CuO + CO2↑ + H2O↑
CREGA-TG(3)
520 540 560 580 600 620
0.0
0.2
0.4
0.6
0.8
1.0
Static air 60 ml min-1 (N2) 90 ml min-1 (N2) 1.5 Pa
Frac
tiona
l rea
ctio
n α
T / K
0.00
0.02
0.04
0.06
0.08
0.10
0.12
(dα/
dt) /
min
-1
Influence of Reaction Atmosphere With increasing
the influence of self-generated atmospheric
condition
Reaction temperature shifts systematically to lower temperature region
CREGA-TG(4)
700
650
600
550
500
T / K
1.00.80.60.40.20.0Fractional Reaction α
flowing dry N2 flowing dry N2-CO2 flowing wet N2
Dry N2
Dry N2-CO2
Normal
Wet N2
Inverse
Influence of atmospheric CO2 and H2O
CREGA-TG(5)
400 500 600 700 800-10.0
-7.5
-5.0
-2.5
0.0
2.5
5.0
7.5
10.0
-40
-20
0
20
40
60
80
0
1000
2000
3000
4000
5000
0
1
2
3
4
∆T / µV
Mas
s cha
nge ∆W
/ m
g
T / K
∆T
∆W
CO2
H2O
CO
2 / pp
m
H2O
/ g
m-3
Sample mass: 20.08 mg
Carrier Gas: dry N2
Flow Rate: 200 ml min-1
H.R.: 10.0 K min-1
A Typical TG-DTA-EGA Curves
CREGA-TG(6)
0 50 100 150 200300
400
500
600
700
800
-8
-6
-4
-2
0
2
4
6
8
0
100
200
300
0
2
4
6
8
10
∆W
T
T / K
time / min
Mas
s cha
nge ∆W
/ m
g
CO2
H2O
CO2 /
ppm
H2O
/ g
m-3
Typical CREGA(CO2)-TG Curves
Sample mass: 20.55 mg
Carrier Gas: dry N2
Flow Rate: 200 ml min-1
H.R.: 2.0 K min-1
Controlled Gas: CO2 (100ppm)
CREGA-TG(7)
500
525
550
575
600
0 -1 -2 -3 -4 -5 -6
H2O= 1.08 g m-3
H2O= 8.16 g m-3
H2O=11.57 g m-3
Mass change ∆W / mg
T / K
Sample mass: 20.55 mgCarrier Gas: N2
with H2O: 1.98 g m-3
8.14 g m-3
11.57 g m-3
Flow Rate: 200 ml min-1
H.R.: 2.0 K min-1
Controlled Gas: CO2Controlled Value: 100ppm
Influence of Water Vapor
0.0 0.2 0.4 0.6 0.8 1.0475
500
525
550
575
600
625
0.0 0.2 0.4 0.6 0.8 1.0475
500
525
550
575
600
625(b) H2O = 8.2 g m-3(a) H2O = 1.1 g m-3
CO2= 0.1 g m-3
CO2= 0.3 g m-3
CO2= 0.55 g m-3
T / K
Fractional reaction α
CO2= 0.1 g m-3
CO2= 0.3 g m-3
CO2= 0.55 g m-3
CREGA-TG(8)
Influence of CO2
CREGA-TG(9)
How to change decomposition rate for kinetic calculation?
Parameter Problem
Control Value Change in the partial pressure of evolved gas
Sample Mass Change in the mass-transfer phenomena in the sample matrix
Flow Rate Change in the suction effect
CREGA-TG(10)
0 50 100 150 200 250 300300
400
500
600
700
-8
-6
-4
-2
0
2
4
6
8
0
50
100
150
200
0
1
2
3
4
5
T / K
time / min
Mas
s cha
nge ∆W
/ m
g CO2 /
ppm
H2O
/ g
m-3
Two Different CREGA(CO2)-TG Curves for Kinetic Calculation
Sample Mass: 20.22 mg
Ref. Mass:20.20 mg
Carrier Gas: dry N2
Flow Rate: 200 ml min-1
H.R.: 2.0 K min-1
Controlled Gas: CO2 (100ppm)
Conclusion(1)
Application of Dynamic Temperature Change in the Type of Feedback Control
Thermal Decomposition of Solids
Possibility of Quantitative Control of the Relationship between Reaction Kineticsand Self-generated Reaction Atmosphere
Near-equilibrium Far-equilibrium
Conclusion(2)
Logical Consideration on Kinetic Characteristics
Appropriate Control of Reaction Atmosphere and Reaction Rate
Practical Usefulness of CRTA Techniques(1)Separation of overlapped reaction steps(2)Measurement of kinetic rate data(3)Process control and product control
The End