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R.p Pathak.et al. Int. Journal of Engineering Research and Applications www.ijera.com
ISSN: 2248-9622, Vol. 6, Issue 4, (Part - 1) April 2016, pp.46-52
www.ijera.com 46|P a g e
Effect of Grain Size and Reaction Time in Characterisation of
Aggregates for Alkali Silica Reaction Using Chemical Method
R.P. Pathak1
, Pankaj Sharma2
, Kachhal Prabhaakar3
, Sameer Vyas4
, N.V. Mahure5
,
N Sivakumar 6
1-6
Central Soil and Materials Research Station, Hauz Khas, New Delhi-110016
ABSTRACT
Concrete can deteriorate as a result of alkali aggregate reaction, an interaction between alkalis present in
alkaline pore solution originating from the Portland cement and reactive minerals in certain types of aggregates.
Potential reactivity of aggregates with regard to alkalis present in concrete mix can be determined by Mortar Bar
method, Chemical Method and Petrographic analysis. Of these the chemical method though is quick and does
not require a large quantity of material for testing yet have its own inherent limitations. It does not ensure
completion of reaction as the observations are limited to 24hour only and also does not assess the effect of
varying the combination of coarse and fine aggregates. A study on chemical method by allowing the reaction for
a prolonged time up to 96 hours and also on different grain size ranged matrix was carried at Central Soil and
Materials Research Station, New Delhi. Simultaneously the test results of the modified method are compared to
the existing Mortar Bar method, Chemical Method and Petrographic analysis The outcome of the studies clearly
reflects that the grain size play an important role in the reaction, the reaction time has a demarked impact on
reactivity, in the cases having a high value of silica release the choice of reduction in alkalinity as an indicator
of degree of reaction is not reliable, instead measuring remaining Na2O concentration in Sodium hydroxide
solution after the reaction seems to be much more meaningful in justifying the silica release.
Keywords: Aggregate, Petrographic, Mortar Bar Expansion, Alkali, Silica,
I. INTRODUCTION
Alkali aggregate reaction (AAR) occurs
when there is interaction between the alkalis
present in the pore solution and silicious minerals
in some aggregates forming a calcium alkali
silicate gel(1)
. Potential reactivity of aggregates
with regard to alkalis present in concrete mix can
be determined by chemical method (CM)
developed by Milenz and co-workers of US Bureau
of Reclamation (USBR) in USA(2,3,4)
. For
determining potential reactivity of aggregates CM -
ASTM C 289 -81 and IS 2386 (Pt VII) (5, 6)
are
being followed. These methods cover the chemical
determination of the potential reactivity of an
aggregate with alkalis in a Portland cement
concrete as indicated by the amount of reaction
during 24 hours at 80o
C between 1N NaOH
solution and aggregate that has been crushed and
sieved to pass a 300µm sieve and retained on a
150µm sieve. This chemical method has had a
word wide success, because it is quick, easy to do
and does not require a large quantity of material.
However, it suffers from several defects like
Non Representative Grain Size of Sample
(150µm to 300µm)
The material passing the 150µm sieve is
discarded. The desired fraction is washed. The
reactive silica present in amorphous state in the
aggregates passes
with the fraction smaller than 150µm. Washing of
the desired fraction removes any traces of
amorphous silica.
Abnormality in Measurement of Reduction
in Alkalinity (Rc)
The Reduction in Alkalinity is the
measurement of remaining OH-
ions concentration
after the reaction. The choice of measuring OH ion
concentration is not correct as it is involved in two
reactions. Apart from OH-
ion the HCl titration
using phenolphthalein indicator, is also influenced
by some other anions such as carbonates, silicates,
chlorides and sulphates.
Inadequate Reaction Time
Strained quartz is a slow reacting material,
thus the reaction time of 24 hours is not adequate
to ensure release of total silica content.
Anomaly in Estimation of Nature of
Aggregate in Siliceous Limestone Samples
Siliceous limestone does not show
deleterious nature because of low silica content
compared to the very high CaCO3 level and a very
high Rc because of carbonates.
RESEARCH ARTICLE OPEN ACCESS
R.p Pathak.et al. Int. Journal of Engineering Research and Applications www.ijera.com
ISSN: 2248-9622, Vol. 6, Issue 4, (Part - 1) April 2016, pp.46-52
www.ijera.com 47|P a g e
Reappraisal of Chemical Method (Sorentino’s
Kinetic Test Method)
Sorrentino el al(7)
, reappraised the CM by
considering
 Grain size of materials (60% of 150µm to
300µm and 40% passing 150µm),
 Extension of reaction time upto 96 hrs. and
 Reduction in alkalinity
Considering these factors Sorentino’s
Kinetic Test Method (SKT)(8)
was developed and
a new qualification diagram (Fig. 1) for estimation
of nature of aggregate was defined.
Fig. 1 Interpretation Diagram of the Kinetic
Test
The experimental values of silica release
(Sc) and sodium concentration are expressed in the
form of their molar ratio (SiO2/Na2O) as a function
of time. In the new diagram three areas were
assigned for different type of reactivity. The
separation lines have been established on the basis
of field performance record of the materials and /
or on the results of the concentration expansion test
at 380
C for mortar bar test for fine aggregates,
concrete prisms tests for the coarse ones.
A New Approach
SKT with following modifications (NSKT) was
adopted for the present study for characterisation of
the aggregate.
 Tests were conducted on samples with
(i) Grain size of materials (150µm to 300µm), as
per CM
(ii) Grain size of materials (60% of 150µm to
300µm and 40% passing 150µm), as per
SKT
(iii) Grain size of materials (passing 150µm),
II. MATERIALS AND METHOD
Six Genesis rock type samples from 3
different hydroelectric projects (Fig. 2) were
selected as detailed in Table 1. These samples were
subjected to petrographic analysis (PA), Mortar Bar
Expansion test (MBE)(9)
and CM as per BIS code,
SKT and NSKT
Fig. 2 Sampling Location
Table 1: Details of collected Aggregate Samples
III. RESULTS AND DISCUSSION
Petrographic Examination
The result of PA is presented in Table-2.
Sample no. 1, 2, 3, 5 and 6 have more than 40% of
strained quartz(10,11)
and angle of Undulatory
Extinction greater than 30o(11).
Mortar Bar Expansion Test
The results of MBE are presented in Table
3. Sample no. 1, 4, 5 and 6 shows more than 0.06%
expansion in six months while sample no. 2 and 3
show expansion less than 0.05%.
Chemical Test
Chemical tests as per CM, SKT and
NSKT methods were performed on all the six
samples. Reduction Rc, Sc, remaining Na2O
concentration in millimoles/litre in 1 N NaOH
solution and ratio of SiO2/Na2O are observed for
each sample. The results are presented in Fig. 3a-
3f, 4a-4f and 5a-5f.
IV. INTERPRETATION OF RESULTS
In PA the potential alkali reactivity of
crystalline rocks is related to the percentage and
straining effects in quartz (Gogte, 1973)(9)
. Rock
aggregate containing 40% or more
strongly undulatory, fractured or highly granulated
quartz are highly reactive; those with 30 to 40%
strained quartz(12)
are moderately reactive while the
ones with predominantly unstrained or
recrystallized quartz are innocuous.
Sl.
No.
Name of Project Rock Type Sampl
e No.
1. Nathpa Jhakri
Power Corporation,
HP
Garnet Mica
Genesis
1
Biotite Genesis 2
2. Kirthai HE Project,
J&K
Quartz Mica
Genesis
3
Genesis
(mylonitised)
4
3. Hirakud Dam
Project, Orissa
Mylonitized
Feldspathic Genesis
5
Genesis
(Feldspathic)
6
R.p Pathak.et al. Int. Journal of Engineering Research and Applications www.ijera.com
ISSN: 2248-9622, Vol. 6, Issue 4, (Part - 1) April 2016, pp.46-52
www.ijera.com 48|P a g e
The aggregates showing mortar bar
expansion above 0.05% in six months are classified
as reactive, while those showing lesser expansion
in same period as innocuous (Gogte 1973).
Behaviour of the six aggregate samples as observed
through PA, MBE, CM, SKT and NSKT test
approaches is summarised in Table 4 .
It is noticed that both Rc and Sc values are
increasing with increase in reaction time. The
overall reactivity of different matrices is found to
be in the following order
Sample with grain size matrix
(100% <150 µ) > (60:40 Mixture of 300 - 150µ
& <150 µ ) > (100 % 300 - 150 µ)
V. CONCLUSIONS
Following conclusions can be drawn from
above test results.
1. The grain size play an important role in the
reaction. The fraction less than < 150µ has
shown greater reactivity than other two
fractions. The amorphous silica is generally
lost in the fraction size 300 - 150 µ, hence
showed lowest reactivity. The choice of
fraction containing a mixture of fraction 300 -
150 µ (60%) and fraction < 150µ ( 40% ) is
better to have a representative sample.
2. The reaction time has also impact on
reactivity. As we increase reaction time the
values of reduction in alkalinity and silica
release has generally increase. The aggregates
having good amount of strained quartz have
shown higher reaction values at higher
temperature.
3. Reduction in alkalinity to assess nature of the
aggregate where a high value of silica release
occurs is found to be ill illustrative where as
measuring remaining Na2O concentration in
Sodium hydroxide solution after the reaction
seems to be much more meaningful in
justifying the silica release.
R.p Pathak.et al. Int. Journal of Engineering Research and Applications www.ijera.com
ISSN: 2248-9622, Vol. 6, Issue 4, (Part - 1) April 2016, pp.46-52
www.ijera.com 49|P a g e
Table 2: Result of Petrographic Examination
Sample
No
Mineral Name Quantit
y %
Strained
Quartz %
Angle of Undulatory
Extinction
1 Quartz 30-40 85-90 26-32o
Feldspar 45-50
Biotite 5-7
Muscovite 7-9
Garnet 1-2
2 Quartz 40-45 70-75 26-28o
Feldspar 38-40
Biotite 10-12
Muscovite 4-6
3 Quartz 60-66 40-42 26-28o
Feldspar 18-20
Muscovite 8-10
Biotite 8-10
4 Quartz 52-58 8-10 44-46o
Feldspar 28-30
Muscovite 4-6
Biotite 8-10
5 Quartz 28-30 90-95 38-40o
Feldspar 46-48
Biotite 5-7
Pyroxene 3-4
Chlorite 2-3
Sericite 5-7
Sphene 1-2
Calcite 2-3
Epidote 1-2
6 Quartz 30-35 90-95 38-45o
Feldspar 46-48
Biotite 8-12
Chlorite 2-3
Magnetite 1-2
Sphene 1-2
Calcite 1-2
Table 3: Results of Mortar Bar Expansion Test
Sl.no. Sample No Expansion in % in 6 months
1 1 0.08
2 0.04
2 3 0.04
4 0.06
3 5 0.08
6 0.10
Table 4: Characterisation of Aggregate using Different Tests
I: Innocuous, ID: On border line of Innocuous to Deleterious, D: Deleterious
Sample
No.
PA MBE C
M
SKT NSKT
Time (Hrs) Grain Matrix
< 150 µ (1) 150 µ - 300 µ
(2)
40% of (1) &
60% of (2)
2
4
4
8
7
2
9
6
Time (Hrs.) Time (Hrs.) Time (Hrs.)
2
4
4
8
7
2
9
6
2
4
4
8
7
2
9
6
2
4
4
8
7
2
9
6
1 D D I I I I
D
D I D D D I D D D I I I
D
D
2 D I I I I I D I I
D
D D I D D D I I I D
3 D I I I I I I I I I I I I I I I I I I
4 I D I I I I I I I D D I I D D I I I I
5 D D I I I I
D
D I D D D I D D D I I I
D
D
6 D D I I I I
D
D I D D D I D D D I I I
D
D
R.p Pathak.et al. Int. Journal of Engineering Research and Applications www.ijera.com
ISSN: 2248-9622, Vol. 6, Issue 4, (Part - 1) April 2016, pp.46-52
www.ijera.com 50|P a g e
(a) Sample 1 (b) Sample 2 (c ) Sample 3
(d) Sample 4 (e) Sample 5 (f) Sample 6
Fig. 3 Charactrisation of Aggregate based on Rc
Test on different grain size matrix
R.p Pathak.et al. Int. Journal of Engineering Research and Applications www.ijera.com
ISSN: 2248-9622, Vol. 6, Issue 4, (Part - 1) April 2016, pp.46-52
www.ijera.com 51|P a g e
(a) Sample 1 (b) Sample 2 (c ) Sample 3
(d) Sample 4 (e) Sample 5 (f) Sample 6
Fig. 4 Charactrisation of Aggregate based on Rc
Test on fraction 150 – 300 µ
R.p Pathak.et al. Int. Journal of Engineering Research and Applications www.ijera.com
ISSN: 2248-9622, Vol. 6, Issue 4, (Part - 1) April 2016, pp.46-52
www.ijera.com 52|P a g e
(a) Sample 1 (b) Sample 2 (c ) Sample 3
(d) Sample 4 (e) Sample 5 (f) Sample 6
Fig. 5 Charactrisation of Aggregate based on Rc
Test on fraction 150 – 300 µas a function of
Time
ACKNOWLEDGEMENT
We extend our sincere thanks to Sh. Murari
Ratnam, former Director CSMRS for his guidance.
We extend our sincere gratitude to Sh. Sohan Singh
and Sh. Devender Singh of CSMRS for their
valuable timely help. Sincere gratitude are
extended to all the authors whose publications
provided us directional information from time to
time.
REFERENCES
[1]. ICOLD Bulletin no. 79, “Alkali Aggregate
Reaction in Concrete Dam”.
[2]. RC Millenz and LP Witte, “Tests Used by
the Bureau of Reclamation for Identifying
Reactive Concrete Aggregates, Proc.
ASTM Vol. 48, pp 1071-1103, 1948.
[3]. Millenz RC, “Petrographic Examination
of Concrete Aggregate to Determine
Potential Alkali Reactivity, Highway
Research Board Report 10-C, 29-35, 1950.
[4]. RcMillenz and EJ Beneton, “Evaluation of
the Quick Chemical Test for Alkali
Reactivity of Concrete Aggregate”,
Bulletin 171, Highway Research Board, p
1, 1958.
[5]. ASTM C-289-03, “ Standard Test Method
for Potential Alkali – Silica Reactivity of
Aggregates (Chemical Method).
[6]. IS 2386 (Pt VII)-1963, “Methods of Test
for Aggregates for Concrete Part VII
Alkali Aggregate Reactivity”.
[7]. D Sorrentino, S Sabio, D junique,
AttaqueAlcaline des Granulats: mise au
point d’un Test Clentique. Annales
ITBTP, No. 499, Dec. 1991.
[8]. D Sorrentino, JY Clement and S Sablo,
“Alkali Aggregate Reaction: Proposals
for A Kinetic Test on Aggregates”, 9th
International Congress on the Chemistry
of Cement”, pp254-260, 1992.
[9]. DS Gogte, “An Evaluation of Some
Common Indian Rocks with Special
reference to Alkali Ggregate Reaction,
Engineeing Geology, 1973
[10]. AK Mullik, “Evaluation of ASR Potential
of Concrete Aggregates Containing
Strained Quartz” NCB Quest. Vol. 1,
No.1, PP 35-46, August 1987.
[11]. C Sudhindra, SB suri and KN Nair,
“Strained Quartz – A Menance for
Durability of Concrete for Hydraulic
Structures, Proc. of International
Symposium on New Materials and
Techniques for Dam Construction, 5-7th
March 1987, Madras.
[12]. Building Research Establishment Digest
no. 332, 1988. Reaction, Materials and
Structures, Vol. 33, pp 88-33, March
2000.

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Effect of Grain Size and Reaction Time in Characterisation of Aggregates for Alkali Silica Reaction Using Chemical Method

  • 1. R.p Pathak.et al. Int. Journal of Engineering Research and Applications www.ijera.com ISSN: 2248-9622, Vol. 6, Issue 4, (Part - 1) April 2016, pp.46-52 www.ijera.com 46|P a g e Effect of Grain Size and Reaction Time in Characterisation of Aggregates for Alkali Silica Reaction Using Chemical Method R.P. Pathak1 , Pankaj Sharma2 , Kachhal Prabhaakar3 , Sameer Vyas4 , N.V. Mahure5 , N Sivakumar 6 1-6 Central Soil and Materials Research Station, Hauz Khas, New Delhi-110016 ABSTRACT Concrete can deteriorate as a result of alkali aggregate reaction, an interaction between alkalis present in alkaline pore solution originating from the Portland cement and reactive minerals in certain types of aggregates. Potential reactivity of aggregates with regard to alkalis present in concrete mix can be determined by Mortar Bar method, Chemical Method and Petrographic analysis. Of these the chemical method though is quick and does not require a large quantity of material for testing yet have its own inherent limitations. It does not ensure completion of reaction as the observations are limited to 24hour only and also does not assess the effect of varying the combination of coarse and fine aggregates. A study on chemical method by allowing the reaction for a prolonged time up to 96 hours and also on different grain size ranged matrix was carried at Central Soil and Materials Research Station, New Delhi. Simultaneously the test results of the modified method are compared to the existing Mortar Bar method, Chemical Method and Petrographic analysis The outcome of the studies clearly reflects that the grain size play an important role in the reaction, the reaction time has a demarked impact on reactivity, in the cases having a high value of silica release the choice of reduction in alkalinity as an indicator of degree of reaction is not reliable, instead measuring remaining Na2O concentration in Sodium hydroxide solution after the reaction seems to be much more meaningful in justifying the silica release. Keywords: Aggregate, Petrographic, Mortar Bar Expansion, Alkali, Silica, I. INTRODUCTION Alkali aggregate reaction (AAR) occurs when there is interaction between the alkalis present in the pore solution and silicious minerals in some aggregates forming a calcium alkali silicate gel(1) . Potential reactivity of aggregates with regard to alkalis present in concrete mix can be determined by chemical method (CM) developed by Milenz and co-workers of US Bureau of Reclamation (USBR) in USA(2,3,4) . For determining potential reactivity of aggregates CM - ASTM C 289 -81 and IS 2386 (Pt VII) (5, 6) are being followed. These methods cover the chemical determination of the potential reactivity of an aggregate with alkalis in a Portland cement concrete as indicated by the amount of reaction during 24 hours at 80o C between 1N NaOH solution and aggregate that has been crushed and sieved to pass a 300µm sieve and retained on a 150µm sieve. This chemical method has had a word wide success, because it is quick, easy to do and does not require a large quantity of material. However, it suffers from several defects like Non Representative Grain Size of Sample (150µm to 300µm) The material passing the 150µm sieve is discarded. The desired fraction is washed. The reactive silica present in amorphous state in the aggregates passes with the fraction smaller than 150µm. Washing of the desired fraction removes any traces of amorphous silica. Abnormality in Measurement of Reduction in Alkalinity (Rc) The Reduction in Alkalinity is the measurement of remaining OH- ions concentration after the reaction. The choice of measuring OH ion concentration is not correct as it is involved in two reactions. Apart from OH- ion the HCl titration using phenolphthalein indicator, is also influenced by some other anions such as carbonates, silicates, chlorides and sulphates. Inadequate Reaction Time Strained quartz is a slow reacting material, thus the reaction time of 24 hours is not adequate to ensure release of total silica content. Anomaly in Estimation of Nature of Aggregate in Siliceous Limestone Samples Siliceous limestone does not show deleterious nature because of low silica content compared to the very high CaCO3 level and a very high Rc because of carbonates. RESEARCH ARTICLE OPEN ACCESS
  • 2. R.p Pathak.et al. Int. Journal of Engineering Research and Applications www.ijera.com ISSN: 2248-9622, Vol. 6, Issue 4, (Part - 1) April 2016, pp.46-52 www.ijera.com 47|P a g e Reappraisal of Chemical Method (Sorentino’s Kinetic Test Method) Sorrentino el al(7) , reappraised the CM by considering  Grain size of materials (60% of 150µm to 300µm and 40% passing 150µm),  Extension of reaction time upto 96 hrs. and  Reduction in alkalinity Considering these factors Sorentino’s Kinetic Test Method (SKT)(8) was developed and a new qualification diagram (Fig. 1) for estimation of nature of aggregate was defined. Fig. 1 Interpretation Diagram of the Kinetic Test The experimental values of silica release (Sc) and sodium concentration are expressed in the form of their molar ratio (SiO2/Na2O) as a function of time. In the new diagram three areas were assigned for different type of reactivity. The separation lines have been established on the basis of field performance record of the materials and / or on the results of the concentration expansion test at 380 C for mortar bar test for fine aggregates, concrete prisms tests for the coarse ones. A New Approach SKT with following modifications (NSKT) was adopted for the present study for characterisation of the aggregate.  Tests were conducted on samples with (i) Grain size of materials (150µm to 300µm), as per CM (ii) Grain size of materials (60% of 150µm to 300µm and 40% passing 150µm), as per SKT (iii) Grain size of materials (passing 150µm), II. MATERIALS AND METHOD Six Genesis rock type samples from 3 different hydroelectric projects (Fig. 2) were selected as detailed in Table 1. These samples were subjected to petrographic analysis (PA), Mortar Bar Expansion test (MBE)(9) and CM as per BIS code, SKT and NSKT Fig. 2 Sampling Location Table 1: Details of collected Aggregate Samples III. RESULTS AND DISCUSSION Petrographic Examination The result of PA is presented in Table-2. Sample no. 1, 2, 3, 5 and 6 have more than 40% of strained quartz(10,11) and angle of Undulatory Extinction greater than 30o(11). Mortar Bar Expansion Test The results of MBE are presented in Table 3. Sample no. 1, 4, 5 and 6 shows more than 0.06% expansion in six months while sample no. 2 and 3 show expansion less than 0.05%. Chemical Test Chemical tests as per CM, SKT and NSKT methods were performed on all the six samples. Reduction Rc, Sc, remaining Na2O concentration in millimoles/litre in 1 N NaOH solution and ratio of SiO2/Na2O are observed for each sample. The results are presented in Fig. 3a- 3f, 4a-4f and 5a-5f. IV. INTERPRETATION OF RESULTS In PA the potential alkali reactivity of crystalline rocks is related to the percentage and straining effects in quartz (Gogte, 1973)(9) . Rock aggregate containing 40% or more strongly undulatory, fractured or highly granulated quartz are highly reactive; those with 30 to 40% strained quartz(12) are moderately reactive while the ones with predominantly unstrained or recrystallized quartz are innocuous. Sl. No. Name of Project Rock Type Sampl e No. 1. Nathpa Jhakri Power Corporation, HP Garnet Mica Genesis 1 Biotite Genesis 2 2. Kirthai HE Project, J&K Quartz Mica Genesis 3 Genesis (mylonitised) 4 3. Hirakud Dam Project, Orissa Mylonitized Feldspathic Genesis 5 Genesis (Feldspathic) 6
  • 3. R.p Pathak.et al. Int. Journal of Engineering Research and Applications www.ijera.com ISSN: 2248-9622, Vol. 6, Issue 4, (Part - 1) April 2016, pp.46-52 www.ijera.com 48|P a g e The aggregates showing mortar bar expansion above 0.05% in six months are classified as reactive, while those showing lesser expansion in same period as innocuous (Gogte 1973). Behaviour of the six aggregate samples as observed through PA, MBE, CM, SKT and NSKT test approaches is summarised in Table 4 . It is noticed that both Rc and Sc values are increasing with increase in reaction time. The overall reactivity of different matrices is found to be in the following order Sample with grain size matrix (100% <150 µ) > (60:40 Mixture of 300 - 150µ & <150 µ ) > (100 % 300 - 150 µ) V. CONCLUSIONS Following conclusions can be drawn from above test results. 1. The grain size play an important role in the reaction. The fraction less than < 150µ has shown greater reactivity than other two fractions. The amorphous silica is generally lost in the fraction size 300 - 150 µ, hence showed lowest reactivity. The choice of fraction containing a mixture of fraction 300 - 150 µ (60%) and fraction < 150µ ( 40% ) is better to have a representative sample. 2. The reaction time has also impact on reactivity. As we increase reaction time the values of reduction in alkalinity and silica release has generally increase. The aggregates having good amount of strained quartz have shown higher reaction values at higher temperature. 3. Reduction in alkalinity to assess nature of the aggregate where a high value of silica release occurs is found to be ill illustrative where as measuring remaining Na2O concentration in Sodium hydroxide solution after the reaction seems to be much more meaningful in justifying the silica release.
  • 4. R.p Pathak.et al. Int. Journal of Engineering Research and Applications www.ijera.com ISSN: 2248-9622, Vol. 6, Issue 4, (Part - 1) April 2016, pp.46-52 www.ijera.com 49|P a g e Table 2: Result of Petrographic Examination Sample No Mineral Name Quantit y % Strained Quartz % Angle of Undulatory Extinction 1 Quartz 30-40 85-90 26-32o Feldspar 45-50 Biotite 5-7 Muscovite 7-9 Garnet 1-2 2 Quartz 40-45 70-75 26-28o Feldspar 38-40 Biotite 10-12 Muscovite 4-6 3 Quartz 60-66 40-42 26-28o Feldspar 18-20 Muscovite 8-10 Biotite 8-10 4 Quartz 52-58 8-10 44-46o Feldspar 28-30 Muscovite 4-6 Biotite 8-10 5 Quartz 28-30 90-95 38-40o Feldspar 46-48 Biotite 5-7 Pyroxene 3-4 Chlorite 2-3 Sericite 5-7 Sphene 1-2 Calcite 2-3 Epidote 1-2 6 Quartz 30-35 90-95 38-45o Feldspar 46-48 Biotite 8-12 Chlorite 2-3 Magnetite 1-2 Sphene 1-2 Calcite 1-2 Table 3: Results of Mortar Bar Expansion Test Sl.no. Sample No Expansion in % in 6 months 1 1 0.08 2 0.04 2 3 0.04 4 0.06 3 5 0.08 6 0.10 Table 4: Characterisation of Aggregate using Different Tests I: Innocuous, ID: On border line of Innocuous to Deleterious, D: Deleterious Sample No. PA MBE C M SKT NSKT Time (Hrs) Grain Matrix < 150 µ (1) 150 µ - 300 µ (2) 40% of (1) & 60% of (2) 2 4 4 8 7 2 9 6 Time (Hrs.) Time (Hrs.) Time (Hrs.) 2 4 4 8 7 2 9 6 2 4 4 8 7 2 9 6 2 4 4 8 7 2 9 6 1 D D I I I I D D I D D D I D D D I I I D D 2 D I I I I I D I I D D D I D D D I I I D 3 D I I I I I I I I I I I I I I I I I I 4 I D I I I I I I I D D I I D D I I I I 5 D D I I I I D D I D D D I D D D I I I D D 6 D D I I I I D D I D D D I D D D I I I D D
  • 5. R.p Pathak.et al. Int. Journal of Engineering Research and Applications www.ijera.com ISSN: 2248-9622, Vol. 6, Issue 4, (Part - 1) April 2016, pp.46-52 www.ijera.com 50|P a g e (a) Sample 1 (b) Sample 2 (c ) Sample 3 (d) Sample 4 (e) Sample 5 (f) Sample 6 Fig. 3 Charactrisation of Aggregate based on Rc Test on different grain size matrix
  • 6. R.p Pathak.et al. Int. Journal of Engineering Research and Applications www.ijera.com ISSN: 2248-9622, Vol. 6, Issue 4, (Part - 1) April 2016, pp.46-52 www.ijera.com 51|P a g e (a) Sample 1 (b) Sample 2 (c ) Sample 3 (d) Sample 4 (e) Sample 5 (f) Sample 6 Fig. 4 Charactrisation of Aggregate based on Rc Test on fraction 150 – 300 µ
  • 7. R.p Pathak.et al. Int. Journal of Engineering Research and Applications www.ijera.com ISSN: 2248-9622, Vol. 6, Issue 4, (Part - 1) April 2016, pp.46-52 www.ijera.com 52|P a g e (a) Sample 1 (b) Sample 2 (c ) Sample 3 (d) Sample 4 (e) Sample 5 (f) Sample 6 Fig. 5 Charactrisation of Aggregate based on Rc Test on fraction 150 – 300 µas a function of Time ACKNOWLEDGEMENT We extend our sincere thanks to Sh. Murari Ratnam, former Director CSMRS for his guidance. We extend our sincere gratitude to Sh. Sohan Singh and Sh. Devender Singh of CSMRS for their valuable timely help. Sincere gratitude are extended to all the authors whose publications provided us directional information from time to time. REFERENCES [1]. ICOLD Bulletin no. 79, “Alkali Aggregate Reaction in Concrete Dam”. [2]. RC Millenz and LP Witte, “Tests Used by the Bureau of Reclamation for Identifying Reactive Concrete Aggregates, Proc. ASTM Vol. 48, pp 1071-1103, 1948. [3]. Millenz RC, “Petrographic Examination of Concrete Aggregate to Determine Potential Alkali Reactivity, Highway Research Board Report 10-C, 29-35, 1950. [4]. RcMillenz and EJ Beneton, “Evaluation of the Quick Chemical Test for Alkali Reactivity of Concrete Aggregate”, Bulletin 171, Highway Research Board, p 1, 1958. [5]. ASTM C-289-03, “ Standard Test Method for Potential Alkali – Silica Reactivity of Aggregates (Chemical Method). [6]. IS 2386 (Pt VII)-1963, “Methods of Test for Aggregates for Concrete Part VII Alkali Aggregate Reactivity”. [7]. D Sorrentino, S Sabio, D junique, AttaqueAlcaline des Granulats: mise au point d’un Test Clentique. Annales ITBTP, No. 499, Dec. 1991. [8]. D Sorrentino, JY Clement and S Sablo, “Alkali Aggregate Reaction: Proposals for A Kinetic Test on Aggregates”, 9th International Congress on the Chemistry of Cement”, pp254-260, 1992. [9]. DS Gogte, “An Evaluation of Some Common Indian Rocks with Special reference to Alkali Ggregate Reaction, Engineeing Geology, 1973 [10]. AK Mullik, “Evaluation of ASR Potential of Concrete Aggregates Containing Strained Quartz” NCB Quest. Vol. 1, No.1, PP 35-46, August 1987. [11]. C Sudhindra, SB suri and KN Nair, “Strained Quartz – A Menance for Durability of Concrete for Hydraulic Structures, Proc. of International Symposium on New Materials and Techniques for Dam Construction, 5-7th March 1987, Madras. [12]. Building Research Establishment Digest no. 332, 1988. Reaction, Materials and Structures, Vol. 33, pp 88-33, March 2000.