fabric and strength of clays stabilized with lime …7.1 scanning electron micrograph of lime 41...
TRANSCRIPT
FABRIC AND STRENGTH OF CLAYS
STABILIZED WITH LIME
by
MEHDI ARABI
Thesis submitted in partial fulfilment of the requirements for the degree of Doctor of Philosophy of the Council for National Academic Awards, London.
VOLUME II
Department of Civil Engineering and Building,
The Polytechnic of Wales, Pontypridd, Mid Glamorgan, U.K.
Collaborating Establishment:
Wimpey Laboratories Limited, Hayes, Middlesex, U.K.
October, 1987
CONTENTS - VOLUME II
LIST OF FIGURES
Page No.
CHAPTER TWO
2.1 Principal particle size scales and a chart 1 showing percent clay, silt and sand in soil, after Yong and Warkentin [3]
2.2 Crystal chemistry of silicates, after 2,3 Mitchell [5].
2.3 Diagrammatic sketch of the kaolinite structure 4 and its charge distribution, after Mitchell [5].
2.4 Diagrammatic sketch of the montmorillonite 5 structure and its charge distribution, after Mitchell [5].
2.5 Diagrammatic sketch of the structure of 6 muscovite and its charge distribution after Mitchell [5],
2.6 Diagrammatic sketch of the structure of 7 chlorite, after Grim [6].
CHAPTER THREE
3.1 Effect of addition of lime on the plastic 8 limit of soils, after Hilt and Davidson [22].
3.2 Recommended amounts of lime for stabilization 9 of subgrades and bases, after McDowell [35].
3.3 Compressive^strength of lime treated clays, 10 cured at 61 " Grim [49].cured at 60°C for 72 hours, after Eades and
3.4 Comparison of continuous and cyclic freezing 11 for silty clay soil, after Croney and Jacobs [80].
3.5 Schematic illustration of upward flow of soil 12 moisture towards ice crystal, after Gillott [4],
3.6 Relation between temperature below freezing 13 point and suction, after Croney and Jacobs [80].
3.7 Temperature distribution beneath concrete road, 14 Jan 1963 and effect on soil suction, after Croney and Jacobs [80].
CHAPTER FOUR
4.1 Schematic illustration of states of colloidal IS dispersions and settled volumes (stable dispersion, coagulation, heterocoagulation and flocculation), after Ottewill [95].
4.2 Solubility diagrams for alumina, quartz and 16 calcium hydroxide, after Ottewill [95],
4.3 Crystal structure of calcium hydroxide, after 17 Grudemo [109],
4.4 Structure of C-S-H gel, after Grudemo [109]. 18
4.5 Structure of C-S-H gel, after Taylor [131], 19
4.6 Suggested structure for C-S-H gel, after 20 Taylor and Roy [108].
4.7 Suggested C-S-H gel structure, illustrating 21 bonds between and along sheets and polymerization of silicate chains, after Ramachandran et al. [140].
4.8 Three mechanisms of expansion of tobermorite 22 gel, after Brunauer [107].
4.9 Simplified pore model for C-S-H gel, after 23 Daimon et al. [130].
4.10 TG of synthetic C-S-H (I), after James 24 and Subba Rao [148].
4.11 TG curves for various C-S-H specimens, after 25 El-Hemaly et al. [128].
4.12 The loss of water from hydrated calcium 26 aluminates on ignition, after Lea [163].
CHAPTER FIVE
5.1 Particle-size distribution curve of the 27 Red Marl.
CHAPTER SIX
6.1 Relation between dry density and moisture 28 content for Red-Marl without lime additions.
6.2 Schematic representation of the self-level cap 29 used for measurement of the unconfined compressive strength.
6.3 Mercury penetration under pressure, after 30 Carlo Erba, Sci. Inst-[175).
6.4 Typical mercury porosimetric graph for a 31 soil-6 wt% lime specimen, cured for 24 weeks in a moist environment at 75 C.
6.5 Schematic representation of the apparatus used 32 for measurement of the permeability of the cured soil-lime specimens.
6.6 Relationship between dynamic viscosity of 33 water and temperature, after Head [177],
6.7 Schematic representation of the apparatus used 34 for the investigation of frost heave on the cured soil-lime specimens.
6.8 Schematic representation of the specimen 35 position in the freezing cabinet.
6.9 Plot of water absorption against time for 36 soil-lime cylinders of various compositions cured for 12 weeks at 50°C.
6.10 Geometrical conditions for X-ray diffraction 37 according to Bragg's Law, after Mitchell [5].
6.11 Interaction of electron beam with crystalline 38 sample and a schematic electron distribution in a bulk sample and a thin foil, after Lorimer and Cliff [180].
6.12 Schematic representation of the path of the 39 electron rays in a two stage electron microscope for bright field, dark field and diffraction image, after Beutelspacher and Van der Marel [181].
6.13 EDAX analysis of tanzanite and okenite using 40 TEM.
CHAPTER SEVEN
7.1 Scanning electron micrograph of lime 41 [Ca(OH) 2 ].
7.2 Thermogravimetric results for Ca(OH) 2 and 42 CaCO3 .
7.3 Thermogravimetric results for Red-Marl. 43
7.4 Dehydration curves for some clay micas and 44 related minerals, after Mackenzie [182].
7.5 Scanning electron micrographs of the Red-Marl. 45
7.6 EDAX results from TEM studies of soil particles 46 showing illite and chlorite compositions.
in
7.7 EDAX results from TEM studies of soil particles 47 showing albite and glauconite compositions.
7.8 Scanning electron micrograph of kaolinite. 48
7.9 TEM micrograph, electron diffraction pattern 49 and EDAX analysis of untreated kaolinite.
7.10 Thermogravimetric result for kaolinite. 50
7.11 Scanning electron micrograph of montmorillonite. 51
7.12 Thermogravimetric result for montmorillonite. 52
7.13 Scanning electron micrographs of illite. 53
7.14 Thermogravimetric result for illite. 54
7.15 Relation between liquid limit and lime content. 55
7.16 Relation between plastic limit and lime content. 56
7.17 Relation between plasticity index and lime 57 content.
7.18 Plasticity chart showing changes in plasticity 58 of lime treated Red-Marl.
7.19 Plasticity chart indicating the influence of 59 lime content, curing period and curing temperature on plasticity.
7.20 Plot of unconfined compressive strength against 60 curing time for soil-lime cylinders of various compositions cured in a moist environment at 25 C.
7.21 Plot of unconfined compressive strength against 61 curing time for soil-lime cylinders of various compositions cured in a moist environment at 50 C.
7.22 Plot of unconfined compressive strength against 62 curing time for soil-lime cylinders of various compositions cured in a moist environment at 75 C.
7.23 Variation in compressive strength with lime 63 content for 24 week moist-cured soil-lime cylinders at different temperatures.
7.24 Plot of unconfined compressive strength against 64 lime content for soil-lime cylinders cured for 12 weeks in a moist environment at 50 C.
7.25 Relationship between pH values and lime content 65 for slurries of Red-Marl after 1 hour at room temperature.
IV
7.26 Plot of unconfined compressive strength against 66 curing time for soil-lime cylinders of various compositions cured in an unsealed environment at room temperature (~20 C).
7.27 Plot of unconfined compressive strength against 67 curing time for soil-lime cylinders of various compositions cured in an unsealed environment at 25°C.
7.28 Plot of unconfined compressive strength against 68 curing time for soil-lime cylinders of various compositions cured in an unsealed environment at 50°C.
7.29 Plot of unconfined compressive strength against 69 curing time for soil-lime cylinders of various compositions cured in an unsealed environemnt at 75°C.
7.30 Variation in moisture content with curing time 70 for the specimens cured at different temperatures in unsealed environments.
7.31 Plot of unconfined compressive strength against 71 moisture content for untreated Red-Marl cylinders.
7.32 Plot of unconfined compressive strength against 72 curing time for soil-lime cylinders of various compositions cured in a nitrogen environment at room temperature (~20°C).
7.33 Plot of unconfined compressive strength against 73 curing time for soil-lime cylinders of various compositions cured in a carbon dioxide environment at room temperature (~20 C).
7.34 Variation in moisture content with curing period 74 for soil-14 wt% lime specimens cured in nitrogen and carbon dioxide environments.
7.35 Variation in weight during curing period for 75 specimens of various compositions cured in a carbon dioxide environment.
7.36 Effect of delay between mixing and compacting on 76 the unconfined compressive strength of soil-6 wt% lime cylinders cured for 12 weeks in a moist environment at 25, 50 and 75 C.
7.37 Effect of soil particle size on the unconfined 77 compressive strength for soil-6 wt% lime cylinders cured for 12 weeks in a moist environment at 50 C.
7.38 Plot of unconfined compressive strength against 78 curing time for soil-lime-1 wt% sodium chloride cylinders cured in a moist environment at 25 C.
7.39 Plot of unconfined compressive strength against 79 curing time for soil-lime-1 wt% sodium chloride cylinders cured in a moist environment at 50°C.
7.40 Plot of unconfined compressive strength against 80 curing time for soil-lime-1 wt% sodium chloride cylinders cured in a moist environment at 75°C.
7.41 Cumulative pore volume against pore radius for 81 soil-10 wt% lime specimens cured at 25°C for 1 and 24 weeks.
7.42 Cumulative pore volume against pore radius for 82 soil-2 wt% lime specimens cured at 75°C for 1 and 24 weeks.
7.43 Cumulative pore volume against pore radius for 83 soil-6 wt% lime specimens cured at 75°C for 1 and 24 weeks.
7.44 Cumulative pore volume against pore radius for 84 soil-10 wt% lime specimens cured at 75°C for 1 and 24 weeks.
7.45 Cumulative pore volume against pore radius for 85 soil-10 wt% lime specimens cured for 24 weeks at 25 and 75°C.
7.46 Cumulative pore volume against pore radius for 86 soil-2 wt% lime, soil-6 wt% lime and soil-10 wt% lime specimens cured for 24 weeks at 75°C.
7.47 Total pore volume against lime content for 87 specimens cured at 75 C for 1 and 24 weeks.
7.48 Permeability against lime content for specimens 88 cured at 25 C for 1 and 24 weeks.
7.49 Permeability against lime content for specimens 89 cured at 50 C for 1 and 24 weeks.
7.50 Permeability against lime content for specimens 90 cured at 75 C for 1 and 24 weeks.
7.51 Permeability against curing temperature for 91 specimens of various compositions cured for 24 weeks.
VI
7.52 Permeability against the percentage porosity 92 contributed by pores of radius greater than 40nm.
7.53 Frost heave against curing time for soil-lime 93 cylinders of various compositions cured at 25°C.
7.54 Frost heave against curing time for soil-lime 94 cylinders of various compositions cured at 50°C.
7.55 Frost heave against curing time for soil-lime 95 cylinders of various compositions cured at 75°C.
7.56 Frost heave against lime content for soil-lime 96 cylinders cured for 1 and 24 weeks at 25°C.
7.57 Frost heave against lime content for soil-lime 97 cylinders cured for 1 and 12 weeks at 50 C.
7.58 Photographs illustrating the frost heave and 98 formation of ice lenses in soil-lime cylinders of various compositions cured at different temperatures.
7.59 Thermogravimetric results for soil and cured 99 soil-lime samples, cured for 24 weeks at 50°C.
7.60 Plot of the wt% "consumed lime" against the wt% 100 loss of "gel water" in the temperature region 100-250°C.
7.61 Plot of unconfined compressive strength against 101 wt% "consumed lime" for soil-lime specimens cured at 50°C for various times.
7.62 Scanning electron micrograph of the fracture 102 surface of a 24 week (50°C) cured soil-14 wt% lime sample.
7.63 Part of the X-ray diffractometer of soil-10 wt% 103 lime sample cured for 1.5 years at 75 C.
7.64 Scanning electron micrographs of the fracture 104 surface of a 1 day (75°C) cured soil-10 wt% lime sample.
7.65 Scanning electron micrographs of the fracture 105 surface of a 3 weeks (75°C) cured soil-10 wt% lime sample.
7.66 Scanning electron micrographs of the fracture 106 surface of a 6 weeks (75°C) cured soil-10 wt% lime sample.
7.67 Scanning electron micrographs of the fracture 107 surface of a 6 week (75 C) cured soil-10 wt% lime sample and a 4 week cured Portland cement.
vii
7.68 SEN and EDAX results of the platelet particles 108 formed in a soil-10 wt% lime sample cured for 6 weeks at 75°C.
7.69 Scanning electron micrographs of the fracture 109 surface of 12 week (75 C) cured soil-10 wt% lime sample.
7.70 Scanning electron micrographs of the fracture 110 surface of 6 month (75 C) cured soil-10 wt% lime sample
7.71 Scanning electron micrographs of the fracture 111 surface of 1 year (75°C) cured soil-10 wt% lime sample.
7.72 Scanning electron micrographs of the fracture 112 surface of 18 month (75 C) cured soil-10 wt% lime sample.
7.73 Scanning electron micrographs of the fracture 113 surface of 2 year (75°C) cured soil-10 wt% lime sample.
7.74 Typical transmission electron micrographs 114 showing gel morphology after one year at 75 C for a soil-10 wt% lime sample.
7.75 Transmission electron micrograph and EDAX 115 analysis of gel formed in soil-10 wt% lime composite cured in a moist environment at 75 C for one year.
7.76 Transmission electron micrograph of typical 116 gel particle together with its electron diffraction pattern.
7.77 TEM micrograph and EDAX analysis of gel formed 117 in a soil-10 wt% lime composite cured in a moist environment at 75 C for 1 year.
7.78 TEM micrograph and EDAX analysis of gel formed 118 in soil-10 wt% lime comgosite cured in a moist environment at 75 C for 1 year.
7.79 TEM micrograph and EDAX analysis of gel formed 119 in a soil-10 wt% lime composite cured in a moist environment at 75 C for six weeks.
7.80 TEM micrograph and EDAX analyses of gel formed 120 on the borders of a quartz particle inQa soil-10 wt% lime composite cured at 75 C for 1 year.
viii
7.81 Scanning electron micrographs of the fracture 121 surface of a 12 week (75°C) cured refined Marl-20 wt% lime sample.
7.82 DTG traces for refined Marl-20 wt% lime samples 122 cured for 1 day to 24 weeks at 75 C.
7.83 TG traces for refined Marl-20 wt% lime samples 123 cured for 1 day to 24 weeks at 75°C.
7.84 Plot of reacted lime against curing time for 124 refined Marl-20 wt% lime samples cured at 75°C.
7.85 TEM micrograph, electron diffraction pattern 125 and EDAX analysis of gel formed in a refined Marl-20 wt% lime composite cured for 6 weeks at 75°C.
7.86 TEM micrograph, electron diffraction pattern 126 and EDAX analysis of gel formed in a refined Marl-20 wt% lime composite cured for 24 weeks at 75°C.
7.87 Part of the X-ray diffractometer of 127 montmorillonite-20 wt% lime sample cured for 12 weeks at 75 C.
7.88 Thermogravimetric results for 128 montmorillonite-20 wt% lime sample, cured for 12 weeks at 75°C.
7.89 TEM micrograph, electron diffraction pattern 129 and EDAX analysis of gel formed in a montmorillonite-20 wt% lime composite cured for 12 weeks at 75°C.
7.90 TEM micrograph and EDAX analysis of gel formed 130 in a montmorillonite-20 wt% lime composite cured for 12 weeks at 75 C.
7.91 Parts of the X-ray diffractometer of 131 kaolinite-20 wt% lime sample, cured for 12 weeks at 75°C.
7.92 Thermogravimetric results for untreated 132 kaolinite and kaolinite-20 wt% lime sample cured for 12 weeks at 75 C.
7.93 TEM micrograph, electron diffraction pattern 133 and EDAX analysis of gel formed in a kaolinite-20 wt% lime composite cured for 12 weeks at 75°C.
7.94 TEM micrograph and EDAX analysis of gel formed 134 in a kaolinite-20 wt% lime composite cured for 12 weeks at 75°C.
ix
7.95 TEN micrograph and EDAX analysis of gel formed 135 in a kaolinite-20 wt% lime composite cured for 12 weeks at 75°C.
7.96 Part of the X-ray diffractometer of 136 illite-20 wt% lime sample cured at 75°C for 12 weeks.
7.97 Thermogravimetric results for illite-20 wt% 137 lime sample cured at 75°C for 12 weeks.
7.98 Scanning electron micrographs of the fracture 138 surface of illite-20 wt% lime sample cured for 12 weeks at 75°C.
7.99 Typical TEM-EDAX analysis of gel formed in 139 illitep;20 wt% lime sample cured for 12 weeks at 75OC"
CHAPTER EIGHT
8.1 Crystal structure of Ca(OH) 2 , 140 after Taylor [131]
8.2 Representation of an idealized Si^O^ sheet 141 and the idealized dioctahedral sheet.
8.3 SEM micrographs of a 24 week cured soil-10 wt% 142 lime sample at 75°C showing exfoliation and breakdown of the clay layers.
8.4 SEM-EDAX analysis at point "X" in 143 Figure 8.3(a).
8.5 Representation of illite structure. 144
8.6 Phase development in the system CaO-Si02-H20 145 showing the course of cement-pozzolana-water reactions, after Glasser and Marr [192].
CHAPTER TWO
i—mil mi i i mini iiiiniii iiniiiii iiiniin i i numOOOCI 0001 001 01 X) 100
OorrwKr (1090'i'tmc tea*!, m"
Grovel
US Dwortmem rf Jkpiullurt
005 01 025 05 I 2
ftmODO? OOO6 002 005 01 02 Oi I 2 i 6 JO
I Sona —— T,. u 5 Publ.c Hoods I Fun I CCQIM I 6"'t "T *dininiilrot«n
F.nt | I Mrd'j0002 0006 002 OOfc 0? 06
(a)
inv c( Tc-. B B ,,, isri s , nn<)0 ,,_
100A°
60 40 Per Cent Sond
100
Figure 2.1
(a) Principal particle size scales
(b) Chart showing percent clay, silt and sand in soil,
after Yong and Warkentin [3]
Combinationof
TetrahedraDiagrammatic Representation ol Structure
Si-OGroup and
Negative Charge
Oxygen to SiliconHdtIO
E xdmple
Island Independent
(Si0 4 )«- 4 : 1 Ohvmes (Mg. Fe) 2 Si0 4
Double (S, 2 0,l 6 - 7 2 Amermanlte
Rings
><ISi 6 0, 8 >'-
3 1
Beniroite 8aT,Si,O,
Beryl 3e.,AI 2 S. 6 0, B
Chains 3 1 Pyroxenes
Bands11 4 Amphibotes
Figure 2.2
Crystal chemistry of silicates, after Mitchell [5!
Combinationol
TetrahedraDiagrammatic Representation of Structure
Si-0Group and
Negative Charge
Oxygen toSilicon Ratio
Example
Sheets
A A AX V V ___A /
V v v
5 2
Frameworks 2 1Quartz SiO,
Also feldspars, 'or example, orthoclase. KAISi 3 08
Figure 2.2
(continued)
(a)
6 (OH)
tetrahedron
Net Charge +28-28
(b)
Figure 2.3
(a) Diagrammatic sketch of the kaolinite structure
(b) Charge distribution in kaolinite, after Mitchell [5]
Exchangeable Cations
O*vg«ns y Hydroxyls Aluminum. Iron, Magnesium
O and 0 Silicon, Occasionally Aluminum \ O j
Net Charge +44 - 44 = 0
Figure 2.4
(a) Diagrammatic sketch of the montmorillonite structure
(b) Charge distribution in pyrophyllite
(type structure for montmorillonite, after Mitchell [5])
f } Oxygent. toy Hydroxyls, ^B Aluminum, ( ) Potassium
O and Silicons (One Fourth Replaced by Aluminums) ( 3 )
Net Charge + 44-44 = 0 OP
Figure 2.5
(a) Diagrammatic sketch of the structure of muscovite
(b) Charge distribution in muscovite, after Mitchell [5]
Figure 2.6
Diagrammatic sketch of the structure of chlorite,
after Grim [6]
CHAPTER THREE
PL
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r | j 3 \ i 1 } : i i 3 f : c t 1 . i i * \ 'r • 5 i i • L I | I 1 I : _ * i £ * J i/ i i 3 " 1 g f \ t 1 « i * * i * ** i l i i I I
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—— O WHITE MMNM IKMITIKMILLOftfTt—— • KCKOCCM «IO«T«O«ILLOIIITt——d •TOKIII* tiOWTMOKILUWITI——-A nTHIMI ILLITC
•KUKOITf
2 4 6 8 K> 12 LIME ADDED
Figure 3.3
Compressive strength of lime treated clays, cured
at 60°C for 72 hours, after Eades and Grim [49]
10
Soil
Brickearth (1) Harmondswofth
Index tests
LL[p*r wot )
25
PLtp«r c*nt )
17
PIIptrant!
8
Particle siiePassing
200 sieve(per c»nl )
79
Clay contentIptr cent }
2t
Sample compact «mDry
density
111 116
Moisture content(per ctnt 1
13 13
15
o mX
05
^ 111tb/ft3
Measured heavecontinuous freezi
116lb/ft 3 _
Heave deduced from cyclic freezing
_L50 100 150 200
Hours of freezing
(a) CYCLIC AND CONTINUOUS FREEZING
250 300
15
10 -
600
(b) HEAVE FOR CYCLIC FREEZING
Figure 3.4
Comparison of continuous and cyclic freezing
for silty clay soil, after Croney and Jacobs [80]
11
Soil
Ice cryslil
MoUlurc lilm (Hulll
\ *diorptint lorcts
r
\Joil pirlicit
Figure 3.5
Schematic illustration of upward flow of soil
tooisture towards ice crystal, after Gillott [4]
12
oI£
0
tt
3 2g
3 35 4 45Suction ot unfrozen moisture (pF)
Figure 3.6
Relation between temperature below freezing point
and suction, after Croney and Jacobs [80]
13
Temperature (degC)
-2 0
25
_ 10c
a.«* O 15
20
25
Sueti'on ( P F)
2 3
CONCRETE
Equilibriumsuction(unfrozen)
Suction for"temperature distribution of (a)
(a) TEMPERATURE DISTRIBUTION (M SOIL SUCTION
Figure 3.7
Temperature distribution beneath concrete road, Jan 1963, and
effect on soil suction, after Croney and Jacobs [80]
14
CHAPTER FOUR
o.o
(a) fc) Id}
Figure 4.1
States of colloidal dispersions (upper sketch)
and settled volumes (lower sketch):
(a) stable dispersion (b) coagulation,
(c) heterocoagulation, (d) flocculation,
after Ottewill [95]
15
-104 6 8 10
pH13
i E•o•o
S -2
c c u
Ca(OH)' \
10 12
CalOH),
14
Figure 4.2
Solubility diagrams for alumina, quartz and
calcium hydroxide, after Ottewill [95]
16
Layer lattice element with Ca ions
(cubes) in octahedral positions
between OH ions, situated 0.147nm
above and below the Ca plane. More
exact cell size 0.3593nm. Next
layer stacked directly on top, at a
distance of 0.4909nm.
CH structure
Figure 4.3
Crystal Structure of calcium hydroxide,
after Grudemo [109]
17
C-S-H gel structure
(a) C-S-H gel layer, based on the CH cell Cubes - Ca. tetrahcdra - Si, circles - 0 or OH
(b) Mosaic of CH-type cells in C-S-H layer. C/S • 1.68
Figure 4.4
Structure of C-S-H gel, after Grudemo [109]
18
A chain of CaO. octahedra sharing O-O edges with each other, and individual oxygen atoms with {a) S>>:Oi groups: (b) Si»Oi» groups and (c) longer Si-O chains
Figure 4.5
Structure of C-S-H gel, after Taylor [131]
19
50 n m
^Ca-0 sheets with attached anions including Si 207
• Typical spaces containing Ca H20 and anions including
compact polysilicate anions.
Figure 4.6
Suggested structure for C-S-H, after Taylor and Roy [108]
20
H H°'M M ~° CO
X M M /• Co** M0-Co_
H H M
POSSIBLE BONDS
BRIDGING BETWEEN SHEETS
5.
6' riI 'TO.U.-J
V.M
ALONG SHEETS
1.
Co
H H'o
Figure 4.7
Suggested C-S-H gel structure, illustrating bonds between
and along sheets and polymerization of silicate chains,
after Ramachandran et al. [140]
21
©
Figure 4.8
Three mechanisms of expansion of tobermorite gel,
after Brunauer [107]
22
OtfpwtcM
x : Intracrystallite pore,
o : Intercrystallite pore
• : Mono layer water
Figure 4.9
Simplified pore model for C-S-H gel,
after Daimon et al. [130]
23
WE
IGH
T
LO
SS
(W%
)
o> oM
O
nf o
•^
M)
C-i
CO
(0 00
<-r H-
O CO re
n (D
H m £ n
m a c
a m
20
10O 2OO 3OO 4OO 5OO «OO 70O 1OO 20O 3OO 4OO SCO 6OO 70OTEMPERATURE *C TEMPERATURE »C
Figure 4.11
TG curves for various C-S-H specimens,
after El-Hemaly et al. [128]
25
200 400 TLMPC.KATUKE Of ICN/JVON.'C
Figure 4.12
The loss of water from hydrated calcium
aluminates on ignition, after Lea [163]
26
CHAPTER FIVE
«m
s s
v> n
c«l U
O ®S I-IW
90
80
70
6O
50
40
30
20
10
O 0.0
-
!
1
001 C
i
-M •"" — —
—
**•'•* t
t
(01
--— 9O
•--60
- —70
•-60
• -50
• -40
^}P
,'-20
— to
f'
yy
i^
/
OOl
i•— \-
i>T~
/I» i
j111••— 1-
••— h-
-h-• — t-
J~
i
ff
.r
x >
Ctl
f p —-f-90
- 1
- --70
- --60
... 50
- --40
- +30
- --20
- -i ,0. .1 __ .
I.OParticle size (mm)
CLAY FINE (MEDIUM [COARSESILT
FINE j MEDIUM COARSESAND
Figure 5.1
Particle-size distribution curve of the Red Marl
27
CHAPTER SIX
MOISTURE CONTENT
Figure 6.1
Relation between dry density and moisture
content for Red Marl without lime additions
28
LOADING
^^^^^^n
SPECIMEN
Figure 6.2
Schematic representation of the self-level cap used
for measurement of the unconfined compressive strength
29
V
ri I
P' <
u> rj 3
C p» <
V rj
^ rj
' pi
Figure 6.3
Mercury penetration under pressure,
after Carlo Erba, Sci. Inst. [175]
30
\XV^A\\\NSSA\\X\\X\V^\ \\ \\ \ \ V v^ ^-^
Figure 6.4
Typical mercury porosimetric graph for a soil-6 wt% lime
specimen cured for 24 weeks in a moist environment at 75 C
BURETTE
AIR VALVE
RUBBER "O"RING
WATER
TO CONSTANT ,, HEAD
I U 148 I i 8 I s S
LOWER CAP
UPPER CAP TERRAM
-RUBBER MEMBRANE
SPECIMEN
Figure 6.5
Schematic representation of the apparatus used for measurement
of the permeability of the cured soil-lime specimens
32
V5
ratio
VO
0-5
XXX"
X
1O 2Otemperature T °C
30 4O
Figure 6.6
Relationship between dynamic viscosity
of water and temperature, after Head [177]
33
GLASS WOOL
SPECIMEN
SPECIMEN HOLDER
POLYSTYRENE
COPPER TRAYWATER BATH
rr -~
nitit njiijli---
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__ _ __ — _-
-3 -----
.-3 — - —
Figure 6.7
Schematic representation of the apparatus used for the investigations
of frost action on the cured soil-lime specimens
34
GLASS WOOL
SPECIMEN HOLDER
~ " ." ~ WATER BATH
Figure 6.8
Schematic representation of the specimen
position in the freezing cabinet
35
10 15 20
HOURS
30
Figure 6.9
Plot of water absorption against time for soil-lime cylinders
of various compositions cured for 12 weeks at 50°C
36
Incident Ray Diffracted RaY
Atomic Planes
Figure 6.10
Geometrical conditions for X-ray diffraction
according to Bragg's law, after Mitchell [5]
37
(a)
(b)
Figure 6.11
(a) Interaction of electron beam with crystalline sample
(b) Schematic electron distribution in a bulk sample and
a thin foil, after Lorimer and Cliff [180]
38
BDIM CT ION ClCCIHO" liri (Y TILTINC ILIUM III At ION STSTCM
_ _ Controst aperture _ _
_ _ Intermediate image
_ _ Projector lens _ _
Specimen _ _ _
Objective lens __
Selected oreo aperture _ __^
Diffraction lens - -
Intermediate diagram
Projector lens _ _
Fluorescent screen Photographic plate
Bright field Dork field
Final diagram
_____1_____
Diffraction pattern
Figure 6.12
Schematic representation on the path of the electron rays
in a two stage electron microscope for bright field (A)
dark field (B) and diffraction image (C),
after Beutelspacher and Van der Marel [181]
39
Tanzanite
Ca Al Si1.88 2.93 3.19
O kenite
Ca Si2.96 6.02
Figure 6.13
EDAX analysis of tanzanite and okenite using TEM
(a) tanzanite (b) okenite
40
CHAPTER SEVEN
Figure 7.1
Scanning electron micrograph of lime [Ca(OH)-1x2000
41
toto O
0
10
20
30 Ca(OH),
DTG
TG
(a)
01
O
0
10
20
30
40 CaCO,
DTG
TG
2OO 400 60O
TEMPERATURE
800 1000 C
(b)
Figure 7.2
Thermogravimetric results for
(a) Ca(OH) 2 and (b) CaC03
42
0
2VJ
O 4_jI- 6
— 8 iu^ 10
12
TG
200 400 600 800 1000 C
TEMPERATURE
Figure 7.3
Thermogravimetric results for Red-Marl
43
200 400 600 800 Temperature °C
1000
Figure 7.4
Dehydration curves for some clay micas and related minerals A-talc, B-muscovite, C-sericite,D-pyrophyllite, E-muscovite F-glauconite, G-fine-ground muscovite, H-illite, l-illite, Fithian,Illinois, U.S.A., j-illite, South Wales, K-muscovite, Goshen Massachusetts, U.S.A., after Mackenzie 1182]
44
(a)
Figure 7.5
Scanning electron micrographs of the Red-Marl
(a) X2000, (b) X5000
45
Figure 7.6
EDAX results from TEM studies of soil particles
showing illite and chlorite compositions
46
Illite
K Ca (Al Fe ) (Al Si )0.6 0.1 2 1.76 0.17' V 0.63 3.37
Chlorite
K Ca (Al Fe M9 J(AI Si )0.24 0.14 2.2 !.57 1.88 0.69 3.31
Illite
K Ca (Al Fe ) (Al Si )0.71 0.27 1.79 0.1, 0.98 3.02
Chlorite
(Al M9 Fe ) (Al Si )2.63 2.48 0.89 7 0.02 3.9 8
Albite
Na Al Si0,75 1.16 2.94
a
Glauconite
rMAS KC 9 I i a
Figure 7.7
EDAX results from TEM studies of soil particles
showing albite and glauconite compositions
(a) albite (b) glauconite
47
Figure 7.8
Scanning electron micrograph of kaolinite XlOOOO
48
0.15 AI m
I" 2 I" 4^0.98 Si 1.00
(b)
(c)
Figure 7.9
(a) TEM micrograph of untreated kaolinite
(b) electron diffraction pattern
(c) EDAX analysis
49
(0
O
8
12
16
TG
200 400 600
TEMPERATURE
800 1000 C
Figure 7.10
Thermogravimetric result for kaolinite
50
Figure 7.11
Scanning electron micrograph of
montmorillonite X5000
51
montmorjllomt*
CO COo
0
4
8
I 12ui£ 16
20
200 400 600
TEMPERATURE
800 1000 C
Figure 7.12
Thermogravimetric result for montmorillonite
52
(a)
(b)
Figure 7.13
Scanning electron micrographs of illite
(a) X2000, (b) X5000
53
* 4COCOO 8
X 12 O
I «
20
TO
200 400 600
TEMPERATURE
800 1000 C
Figure 7.14
Thermogravimetric result for illite
54
44
42
40
38
+• TESTED IMMEDIATELY A 1WEEK CUBED AT 1(*CO « WEEKS CURED AT tf*C
©14 WEEKS CUBED AT*S*C
V 1 WEEK CUNCD AT»0*C
36
34
32
30
A
O ©
A
or
©
©
6 10
LIME CONTENT^
14
Figure 7.15
Relation between liquid limit and lime content
55
O
32
30
28
26
24
-f- TESTED IMMEDIATELY
A 1WEEK CURED AT J»°C
O * WEEKS CURED AT»B*C
® 14WEEKS CUKEO AT IRC
^ 1 WEEK CUMED AT SO*CAT
-r-O®
TO
22
20
UNTREATED SOIL
6 10
LIME CONTENT^
14
Figure 7.16
Relation between plastic limit and lime content
56
LU0
>-H-
5
16
14
12
10
8
6
) UNTREATED SOIL
A
O
o®T
+ TESTED IMMEDIATELY
A 1WEEK CURED AT 16 C
O 4WEEKS CURED AT2S°C
© 24WEEKS CURED AT I5°C
W 1 WEEK CURED AT BO°C
AO AD
6 10
LIME CONTENT
14
Figure 7.17
Relation between plasticity index and lime content
57
tn
oo
x Ul o o
15-
-f-
TES
TED
IM
ME
DIA
TE
LY
A
tWE
EK
C
UR
ED
A
T »»
C
O
4WE
EK
S
CU
RE
D
AT J
S°C
©
24W
EE
KS
C
UR
ED
A
T 1S
C
1 W
EE
K
CU
RE
D
AT
*0°C
10
2025
UN
TR
EA
TE
D
SO
IL /
A''
30
35
LIQ
UID
L
IMIT
%
+
*
40
Figu
re 7
.18
Plas
tici
ty c
hart s
howing c
hanges i
n pl
asti
city
of
lime
tre
ated
Red
-Mar
l
20
O
10a.
L:LIME CONTENT
C:CURING PERIOD
TlCURING TEMPERATURE
20
UNTREATED SOIL
30 40
LIQUID LIMIT %
50
Figure 7.19
Plasticity chart indicating the influence of lime content,
curing period and curing temperature on plasticity
59
"E
E
IXI- ozUltr
UJ
CO(/) 111 ccQ.2 O O
14% LIME
8 12
AGE-WEEKS
24
Figure 7.20
Plot of unconfined compressive strength against curing time
for soil-lime cylinders of various compositions cured in a
moist environment at 25°C
60
1 2 3 8 12
AGE-WEEKS
Figure 7.21
Plot of unconfined compressive strength against curing time
for soil-lime cylinders of various compositions cured in a
moist environment at 50 C
61
1 2 8 12
AGE-WEEKS
24
Figure 7.22
Plot of unconfined compressive strength against curing time
for soil-lime cylinders of various compositions cured in a
moist environment at 75°C
62
216UJcc
12
111
UJcca 2 O O
10% LIME
14
Figure 7.23
Variation in compressive strength with lime content for 24 week
moist-cured soil-lime cylinders at different temperatures
63
"EE
IX h- OzUJoc
UJ
UJccCL2 O O
12
8
0 2 6 10 20 30 40
LIME CONTENT^
50
Figure 7.24
Plot of unconfirmed compressive strength against lime
content for soil-lime cylinders cured for 12 weeks in
a moist environment at 50°C
64
12.30 -
1225-
1220 -
12.15
12.10567
LIME CONTENT %
Figure 7.25
Relationship between pH values and lime content for
slurries of Red-Marl after 1 hour at room temperature
65
EEXzI
oUJcc
UJ
UJcc0.2 Oo
1 2 8 12
AGE-WEEKS
14% LIME
24
Figure 7.26
Plot of unconfined compressive strength against curing time
for soil-lime cylinders of various compositions cured in an
unsealed environment at room temperature (~20°C)
66
E E
oUl CCH-
UJ CC.Q.2 O U
O 1 2 8 12
AGE- WEEKS
24
Figure 7.27
Plot of unconfined compressive strength against curing time
for soil-lime cylinders of various compositions cured in an
unsealed environment at 25°C
67
VE STRENGTH-N/mm
COMPRESSI
7
6
5
4
3
2
ill • I
14%LIME
. I 10%
If- 6%
IT. . " 2%
L... :O 1 2 8 12 24
AGE-WEEKS
Figure 7.28
Plot of unconfined compressive strength against curing time
for soil-lime cylinders of various compositions cured in an
unsealed environment at 50 C
68
COMPRESSIVE STRENGTH-N/mmN> A 0> 00
14%LIME' I O/ •L . . 10%fc: • • «.II
m • • m • i
0124 8 12
AGE-WEEKS
24
Figure 7.29
Plot of unconfined compressive strength against curing time
for soil-lime cylinders of various compositions cured in an
unsealed environment at 75 C
69
ROOM TEMR (~20C)
0 1 2 8 12
AGE-WEEKS
o 25C
50*C
24
Figure 7.30
Variation in moisture content with curing time for the
specimens cured at different temperatures in unsealed
envi ronments
70
LU CC
LU
UJ CC Q.SOo
8 10 12 14
MOISTURE CONTENTS
Figure 7.31
Plot of unconfined conpressive strength against
moisture content for untreated Red-Marl cylinders
71
'6E
oUJcc
Ul>
CO</>UJcc0.2 O O
AGE-WEEKS
Figure 7.32
Plot of unconfined compressive strength against curing time
for soil-lime cylinders of various compositions cured in a
nitrogen environment at room temperature (~20°C)
EE
OzLJ QC
LU
tuDC Q.2 O O
0 1 2 8 12
AGE-WEEKS
24
Figure 7.33
Plot of unconfined conqpressive strength against curing time
for soil-lime cylinders of various compositions cured in a
carbon dioxide environment at room temperature (~20°C)
73
12
10
8
UJI- z o oUJ DC
COO 4
\
0 1 2 4
14 X LIME
NITROGEN
CARBON DIOXIDE
8 12
AGE-WEEKS
24
Figure 7.34
Variation in moisture content with curing period for soil-14 wt%
lime specimens cured in nitrogen and carbon dioxide environments
74
WEIGHT INCREASE(Qr) _ -A -k N O 01 O Cfl C• 14%LIME
[ , 'I ' « 'VV 2%Df^ —— i ——————————— • —————— 1 ————————— ,rt t ———— • ——— •124 12 24
DEGREE OF CARBONATION
97 \
«1 %
eo %
AGE-WEEKS
Figure 7.35
Variation in weight during curing period for specimens of
various compositions cured in a carbon dioxide environment
75
12
E 10
OzLU QC H CO
Ul>CO CO HIocQ.2 O O
8*
\
75°C
25°C
14
COMPACTION DELAY (DAYS)
28
Figure 7.36
Effect of delay between mixing and compacting on the unconfined
compressive strength of soil - 6 wt% lime cylinders cured for
12 weeks in a moist environment at 25, 50 and 75°C
76
12
I 10
Z UJcc
UJ
UJDC CL
8
O 2
63 150
PARTICLE SIZE
425 600(MICRON)
Figure 7.37
Effect of soil particle size on the unconfined
compressive strength for soil-6 wt% lime cylinders
cured for 12 weeks in a moist environment at 50 C
77
"E
II
OzUJcc
UJ>CO CO UJccO.
10 % LIME
8 12
AGE-WEEKS
24
Figure 7.38
Plot of unconfined compressive strength against curing time
for soil-lime - 1 wt% sodium chloride cylinders cured in a
moist environment at 25 C
78
EEZ IX »- O Z UJ<r
u>
UJcc o.2 O O
16
12
8
T ? r
10 % LIME
0 1 2 3 8 12
AGE-WEEKS
24
Figure 7.39
Plot of unconfined compressive strength against curing time
for soil-lime - 1 wt% sodium chloride cylinders cured in a
moist environment at 50°C
79
AGE-WEEKS
Figure 7.40
Plot of unconfirmed compressive strength against curing time
for soil-lime-1 wt% sodium chloride cylinders cured in a
moist environment at 75 C
80
O >
100 90 80 70 60 50
cc
O
Q.
40 30 20 10 0
B
10%
LIM
E
1 W
EE
K
CU
RED
AT
25°
C
J 10
% L
IME
I24
WE
EK
S
CU
RE
D
AT
25~C
i i
i i
11i
i i
i i
i r
4 6
8 10
14
8 8
10*
2 4
68
10
s"
2 4
6 8
10
* 2
4 8
8 10*
PORE
R
AD
IUS
nmFigure 7
.41
Cumulative p
ore
volume a
gainst p
ore
radius f
or s
oil
- 10 w
t% l
ime
specimens
cured
at 2
5°C
for
1 and
24 w
eeks
PORE VOLUME %
CO "8o
w
1-1 a~j • £*to
Q» rr
g * (ft »•«a <T>i-h <O O n h--^ i <ji (&0̂,s
H, «S 5'
01
NJ
at
"8i-i ID
0) CL (--
cot-h O
COoH-
Ito
%<M>
O 30m3J>Q
CO
33
PORE VOLUME %
10%
LIM
E
' 1
WE
EK
C
UR
ED
A
T 75
°C
, 10
% L
IME
^
24W
EE
K8
CU
RE
D
AT
75° C '
i i
t i ii
46
8 1Q
44
6 8
1Q4
6 8
1Q2
2 4
6 8
1Q3
2
PORE
R
AD
IUS
nm
4 6
8 10
Figu
re 7
.44
Cumulative p
ore
volu
me a
gain
st p
ore
radius
for
soi
l -
10 wt%
lim
e specimens
cured
at 7
5°C
for
1 an
d 24
weeks
00 (Jl
in 5 O >
100 90
80
70
60
50-
ui oc O a. 40
h
30 20 10 0
24 W
EE
KS
C
UR
ED
AT
75*
C
10%
LIM
EB1
b<!
24 W
EE
KS
C
UR
ED
AT 2
5 C
i t
114
6
8 10
*i
i i
i i
i 11
4
6
8 10*
4 6
8 10
POR
E R
AD
IUS
nmFigure 7
.45
Cumulative p
ore
volume a
gainst p
ore
radius f
or s
oil
- 10
wt% l
ime
specimens
cured
for
24 w
eeks a
t 25
and 7
5°C
CD
ONO >
100-
90-
80-
70
60
50K
O
0.
4
0 30 20 10
B1 B2
B3
T——
! I
I I
f t»
——
——
—I—
——
I——
i I
I |
| II—
——
——
I——
—I—
—I
I I
I I
I I—
——
——
I——
—I—
—I
I I
I I
I I—
——
——
I——
—I—
—i
i i
i •
"
10%
LIM
E
24 W
EE
KS
C
UR
ED
AT
75°C
6% L
I ME
24 W
EE
KS
C
UR
ED
AT
75°C
2%
LIM
E
24 W
EE
KS
C
UR
ED
A
T 75
C
I I
I I
I I
II
I I
I I
I I
I I
I I
I
4 6
8 1Q
1 2
4 8
8 10
* 2
4 0
8 1Q
3 2
4 ft
8 1
0*
2 4
6 8
10
PORE
R
AD
IUS
nmFi
gure
7.46
Cumulative p
ore
volume a
gainst p
ore
radius f
or s
oil
- 2 wt%
lime
,soil -
6 w
t% l
ime
and
soil 1
0Wt% l
ime
spec
imen
s cured
for
24 w
eeks
at
75°C
CURED AT 75 C
O.14
LIME CONTENT %
Figure 7.47
Total pore volume against lime content for
specimens cured at 75°C for 1 and 24 weeks
87
-s 10
^ 8 O
0) ®
E u-~ 4
CURING TEMPERATURE :25 C
ffi< UJ2 cc
-610
8
6 10
LIME CONTENT %
14
Figure 7.48
Permeability against lime content for
specimens cured at 25°C for 1 and 24 weeks.
88
O
I
-510
8
6
CURING TEMPERATURE : 50 C
4I
CD < UJ5 cc
-610
8
6 10
LIME CONTENT %
14
Figure 7.49
Penneability against lime content for
specimens cured at 50 C for 1 and 24 weeks,
89
10r
8O«) (A
E o
CD< UJ5 ocUJo.
CURING TEMPERATURE : 75 C
B
6 10
LIME CONTENT %
14
Figure 7.50
Penneability against lime content for
specimens cured at 75°C for 1 and 24 weeks
90
- 5
108
s 6EJd 4
m<LU2 ccUJ -•o- 10
8
CURING TIME : 24WEEKS
UNTREATED SOIL
25" 50'
CURING TEMPERATURE
75°C
Figure 7.51
Permeability against curing temperature for soil-lime
specimens of various compositions cured for 24 weeks
91
o 0 (f)
E o
00< LU2 ccUJo.
1010 15 20 25 30
POROSITY %(PORES>40nm)
Figure 7.52
Permeability against the percentage porosity
contributed by pores of radius greater than 40 nm
92
140i
120
100
CURING TEMPERATURE : 25 C°
2% lime
E EUJ
UJx
80
60
40
20
INTREATED SOI L
12
CURING TIME (WEEK)
24
Figure 7.53
Frost heave against curing time for soil-lime cylinders
of various compositions cured at 25°C
93
EUJ
UJx
140
12O
100
80
60
40
20
CURING TEMPERATURE: 50 C°
2 % I i m e
UNTREATED SOIL
10%
12
CURING TIME (WEEK)
24
Figure 7.54
Frost heave against curing time for soil-lime cylinders
of various compositions cured at 50°C
94
E EUJ
UJ
140
120
100
80
60
40
20
CURING TEMPERATURE ! 75C
UNTREATED SOIL
•—— _6_%
10%
2% lime
12
CURING TIME (WEEK)
24
Figure 7.55
Frost heave against curing time for soil-lime cylinders
of various compositions cured at 75 C
95
120
100
E E
UJ
UJ
CURING TEMPERATURE: 25 c
20-
0-
2 6
LIME CONTENT %
Figure 7.56
Frost heave against lime content for soil-lime
cylinders cured for 1 and 24 weeks at 25 C
96
UJ
UJX
140
120
100
CURING TEMPERATURE: soc
I 80
I
60
40
20
LIME CONTENT %
10
Figure 7.57
Frost heave against lime content for soil-lime
cylinders cured for 1 and 12 weeks at 50°C
97
Figure 7.58
Frost heave and formation of ice lenses in soil-lime cylinders
(a) soil-2 wt% lime cured for 1 week at 75°C
(b) soil-6 wt% lime cured for 6 weeks at 25°C
(c) soil-10 wt% lime cured for 6 weeks at 50°C
98
DTG
20O 400 600
TEMPERATURE
800 1000 C
Figure 7.59
Thermogravimetric results for soil and cured soil-lime
samples, cured for 24 weeks at 50°C, (A) soil, (B) soil
and 6 wt% lime, (C) soil and 10 wt% lime and (D) soil and
14 wt% lime
99
o
o
rr n> n sH
- ff (V ff Q»
ri- >-«
<D 0) O O O to Ul
o
0°
I (D
•J
CO
NS
UM
ED
LI
ME
(w%
)
ro
^
o>
oo
oro
m
-°
iH
roO 1
O
H
S
O
.0(/>
O)
! e
o ^
?•
'O10
ro o>
I 14
oUJ QC
UJ
12
10
8
6
ui 4 oc
2 4 6 8 10
CONSUMED LIME(w%)
12
Figure 7.61
Plot of unconfined compressive strength against wt% "consumed
lime" for soil-lime specimens cured at 50 C for various times
101
Figure 7.62
Scanning electron micrograph of the fracture surface
of a 24 week (50°C) cured soil-14 wt% lime sample, X5000
102
o
o 1 A=10
"0*
|
nm
A CO CO CO CO CO
in
T ?CO CO
CM CO ? 7
20 (CO.K«)
Figure 7.63
Part of the X-ray diffractometer of soil-10 wt%
lime sample cured for 1.5 years at 75°C
103
Figure 7.64
Scanning electron micrographs of the fracture surface of
a 1 day (75°C) cured soil-10 wt% lime sample
(a) X2000, (b) X5000
104
Figure 7.65
Scanning electron micrographs of the fracture surface of
a 3 week (75°C) cured soil-10 wt% lime sample
(a) X2000, (b) X5000
105
Figure 7.66
Scanning electron micrographs of the fracture surface of
a 6 week (75°C) cured soil-10 wt% lime sample
(a) X2000, (b) X5000
106
Figure 7.67
(a) fracture surface of a 6 week (75°C) cured
soil - 10 wt% lime sample, X2000
(b) 4 week cured Portland cement, X5000
107
Figure 7.68
SEM and EDiAX results of the platelets particles formed
in a soil - 10 wt% lime sample, cured for 6 weeks at 75 C
108
(a)
Figure 7.69
Scanning electron micrographs of the fracture surface
of 12 week (75°C) cured soil-10 wt% lime sample
(a) X5000, (b) XlOOOO
109
Figure 7.70
Scanning electron micrographs of the fracture surface
of 6 month (75°C) cured soil-10 wt% lime sample
(a) X5000, (b) X10000
110
Figure 7.71
Scanning electron micrographs of the fracture surface
of 1 year (75°C) cured soil-10 wt% lime sample
(a) X10000, (b) X20000
111
(a)
Figure 7.72
Scanning electron micrographs of the fracture surface
of 18 month (75°C) cured soil-10 wt% lime sample
(a) X10000, (b) X10000
112
Figure 7.73
Scanning electron micrographs of the fracture surface
of 2 year (75°C) cured soil-10 wt% lime sample
(a) X5000, (b) X10000
113
0.38|um
Figure 7.74
Typical transmission electron micrographs showing gel morphology
after one year at 75°C for a soil-10 wt% lime sample
114
C —S—H gel from cured soil-lime
0.3 8/" m
a
Ca Al Si285 0.98 6.17
Figure 7.75
(a)Transmission electron micrograph of gel formed in soil
10 wt% lime composite cured in a moist environment at 75°C
for one year, (b) EDAX analysis of gel
115
0.2 wm
diffraction ring from ge|
d = 0.293 ±0.01 nm
Figure 7.76
Transmission electron micrograph of typical gel particle
together with its electron diffraction pattern
116
CaCO,
im
J80 (02 J04 {86
Ca1.00 Sl1.00 ^0.20
(b)
Figure 7.77
(a) TEM micrograph of gel formed in soil-10 wt% lime
composite cured in a moist environment at 75 C for 1 year
(b) EDAX analysis of gel at point X
117
0.6 p m (a)
{02 |64 (96
Ca0.62 Si 1.00 M0.71 Mg0.12 K0.09 Fe0.11
Figure 7.78
(a) TEM micrograph of gel formed in soil-10 wt% lime
composite cured in a moist environment at 75 C for 1 year
(b) EDAX analysis of gel at point X
118
? 5 ,' ? 5 S J
038 [Um
eCa0.75 Si1.00
(a)
JB4 |9$
Fe0.45 K0.07
(b)
Figure 7.79
(a) TEM micrograph of gel formed in a soil-10 wt% lime
composite cured in a moist environment at 75°C for six weeks
(b) EDAX analysis of gel at point X
119
im
182
^0.07 Si1.00 K0.04 Ca0.06
(04Ca '0.90 Si2.00 M0.
(80 (02 [64Ca1.08 Si2.00 ^0.42
I
Figure 7.80
(a) TEM micrograph of gel formed on the borders of
a quartz particle in a soil-10 wt% lime composite
cured at 75°C for 1 year
(b) EDAX analysis at point "A"
(c) EDAX analysis at point "B"
(d) EDAX analysis at point "C"
120
Figure 7.81
Scanning electron micrographs of the fracture surface
of a 12 week (75°C) cured refined Marl-20 wt% lime sample
(a) X5000, (b) X10000
121
200 400 600
TEMPERATURE
800 1000 C
Figure 7.82
KG traces for refined Marl - 20 wt% lime samples
cured for 1 day to 24 weeks at 75°C
122
CO CO O
H X OUJ
day cured
1 week
200 4OO 600 8OO 1000 C
TEMPERATURE
Figure 7.83
TG traces for refined Marl-20 wt% lime samples
cured for 1 day to 24 weeks at 75°C
123
100
CURING TIME (WEEKS)
Figure 7.84
Plot of reacted lime against curing time for
refined Marl - 20 wt% lime samples cured at 75 C
124
d « 0.280 + 0.01 nm
fee to2 104 tesSi1.00 Ca0.34 K0.10 Fe0.15
Figure 7.85
(a) TEM micrograph of gel formed in a refined Marl - 20 wt% lime
composite, cured for 6 weeks at 75°C
(b) Electron diffraction at Point X, (c) EDAX analysis at point X
125
im
d = 0.287 + 0.01 nm (b)
Figure 7.86
(a) TEM micrograph of gel formed in a
refined Marl - 20 wt% lime composite,
cured for 24 weeks at 75°C
(b) Electron diffraction at point "A"
(c) EDAX analysis at point "A"
(d) EDAX analysis at point "B"
(e) EDAX analysis at point "C"
|02^0.36 Si1.00 0.03
1AS KC I i la
(08 [92Ca0.65 Si 1.00
(C)
[34 |e 60.03
"0.89 Si1.00
(e)
126
§
to
8 a § 10 01 01 fll ft 01 n°
(V n ft (D a H- l-h 0)
O
ft
O ff
it B H- rt
(D
| 0)
CO
ro O
3 o 3
** 3 o o 3 r+ 9
— 3
3>
0
O 3 3
montmorillonlte
CO (A0
2UJ
16
20
untreated
lime treated
200 400 600
TEMPERATURE
800 1000 C
Figure 7.88
Thermogravimetric results for montmorillonite - 20 wt%
lime sample, cured at 75°C for 12 weeks
128
d - 0.287 + 0.01 nm (b) |B2 |04 (06
Ca0.67 Si1.00 M0.33 Na0.12 Mg0.09 Fe0.05
4-
Figure 7.89
(a) TEM micrograph of gel formed in a montmorillonite - 20 wt%
lime composite cured for 12 weeks at 75°C
(b) Electron diffraction at point X (c) EDAX analysis at point X
129
0.05
Figure 7.90
(a) TEM micrograph of gel formed in a montmorillonite - 20 wt%
lime composite cured for 12 weeks at 75°C
(b) EDAX analysis at point X
130
kaolinite
29<Co.k<*)
k = lo n m
Figure 7.91
Parts of the X-ray diffractoroeter of kaolinite - 20 wt%
lime sample, cured for 12 weeks at 75 C
131
CO
SX O
8
12
16
TG
untreated
lime treated
200 4OO 60O 80O 1000 C
TEMPERATURE
Figure 7.92
Thennograviraetric results for untreated kaolinite and kaolinite-20 wt% lime sample, cured for 12 weeks at 75 C
132
d - 0.287 + 0.01 nm 06 |02 J84Ca0.20 S11.00 M0.83
Figure 7.93
(a) TEM micrograph of gel formed in a kaolinite - 20 wt% lime
composite cured for 12 weeks at 75°C (b) Electron diffraction
at point X (c) EDAX analysis at point X
133
M |B2 (64Ca0.40 Si1.00 ^0.86
Figure 7.94
(a) TEM micrograph of gel formed in a kaolinite-20 wt% lime
composite cured for 12 weeks at 75°C
(b) EDAX analysis at point X
134
M l« )B6Ca0.86 Si 1.00 ^0.85
Figure 7.95
(a) TEM micrograph of gel formed in a kaolinite - 20 wt%
lime composite cured for 12 weeks at 75°C
(b) EDAX analysis at point X
135
illite
e<
1 A=10 nm
Figure 7.96
Part of the X-ray diffractometer of illite - 20 wt%
lime sample cured at 75°C for 12 weeks
136
0
a* 4CO COO 8
12O
i20
untreated
lime treated
200 400 600
TEMPERATURE
800 1000C
Figure 7.97
Thermogravimetric results for illite - 20 wt%
lime sample cured at 75°C for 12 weeks
137
Figure 7.98
Scanning electron micrographs of the fracture surface of
illite - 20 wt% lime sample cured for 12 weeks at 75°C
(a) X 5000, (b) X 10000
138
Figure 7.99
Typical TEM-EDAX analysis of gel fonned in
illite - 20 wt% lime sample cured for 12 weeks at 75°C
(major composition : Ca^ ^g Si^ QQ Alg ^)
139
CHAPTER EIGHT
U-0.3593
Crystal structure of Ca(OH),: arrangement of linked Ca(OH)6 octahedra within a single layer. Parts of three rows of octahedra are shown. The lightly dotted faces of the octahedra are lying flat, with their points away from the observer. Each octahedron has a Ca*+ ion at it* centre and OH~ ions at each of its six apices; each OH~ ion is shared between three
octahedra.
Plan
Elevation
Crystal structure of a single layer of calcium hydroxide, full circles represent calcium atoms, and large circles, represent oxygen atoms; hydrogen atoms are not shown
Figure 8.1
Crystal structure of Ca(OH) 2 /
after Taylor [131]
140
Ideal 2 —dimensional
Si O net 2 5• Si o o
For Si—O= 0.16 nm
b= 0.905 nm
\
Ideal 2—dimensional
dioctahedral sheet
For « = AI , AI-O = 0.189nm
b= 0.801 nm
For • =AI (in Gibbsite)
b = 0-864n m
Figure 8.2
Representation of an idealized Si^Oc
sheet and the idealized dioctahedral sheet
(b)
Figure 8.3
SEM micrographs of a 24 week cured
soil-10 wt% lime sample at 75°C showing
exfoliation and breakdown of the clay layers
(a) X 5000, (b) X 10000
142
Figure 8.4
SEM-EDAX analysis at point "X"
in Figure 8.3(a)
143
H.O
2-2 —dimensional [si O]sheet
interlayer potassium »water
dioctahedral sheet of cations
SiO4 tetrahedron• om« llumlnium • utntllullon
(oy\ octahedron
<OH)~O mainly• Si4*
•!•<> Fe2 +
K(Fe.Mg,AI)2 (Al ,Si ^O
octahedral: tetrahe dral = 0.5
Figure 8.5
Representation of illite structure
144
CaO
H 2 0
C-S-H CH *CH;H
CH . .. -C-S-H/3
/ C-S-WATER-DEFICIENT REGION
cs Si 02
Figure 8.6
Phase development in the system CaO-SiO^-H-O
showing the course of cement-pozzolana-water reactions,
after Glasser and Marr [192]
145