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International Research Journal of Engineering and Technology (IRJET) e-ISSN: 2395-0056
Volume: 07 Issue: 02 | Feb 2020 www.irjet.net p-ISSN: 2395-0072
© 2020, IRJET | Impact Factor value: 7.34 | ISO 9001:2008 Certified Journal | Page 1890
Variation of liquid limit and plastic limit of clayey soils on iron and
sulphur contamination
Aiswarya U S1, Rani V2
1Aiswarya U S, M.tech student, Civil Engineering Department, Marian Engineering College, Kerala, India
2Rani V, Associate Professor, Civil Engineering Department, Marian Engineering College, Kerala, India
----------------------------------------------------------------------***---------------------------------------------------------------------
Abstract –a study was conducted to determine the effect of
contaminants on different clayey soils. Thecontaminantsused
were iron and sulphur. The variation of geotechnical
properties of the clayey soils were studiedbyconductingliquid
limit and plastic limit test using different molarities of
contaminants. The variations at molarities 0.05M, 0.1M, 0.2M,
0.4M, 0.8M, 1M. Variations in liquid limit and plastic limits
were observed with increase in concentrationofcontaminants
Key Words: contamination, bentonite, kaolinite, iron,
sulphur
1. INTRODUCTION
Heavy metals are natural constituents of the earth
crust. A number of these elements are biologically
essential and are introduced into aquatic enrichments
by various anthropogenic activities. Heavy metals at
trace levels present in natural water, air, dusts, soils
and sediments play an important role in human life..
The chemical composition of soil, particularlyitsmetal
content is environmentally important, because toxic
metals concentration can reduce soil fertility, can
increase input to foodchain,whichleadstoaccumulate
toxic metals in food stuffs, andultimatelycanendanger
human health.
Iron is an essential element in human nutrition. It is of
great biologically significance. Lack of iron causes
anaemia andit is the commonest nutritionaldeficiency
in the world. Normal amounts of iron are essential, but
abnormally larger amountadverselyaffectsthehuman
health. Prolonged iron accumulation may cause
damage in tissues Sulphur deposition in soils causes
acidificationofsoilsmainlyclayeysoils.Adverseeffects
of sulphur contamination of soils are shown by the fall
in pH, an increase of phytotoxic aluminium
concentration and by lossesofcalciumandmagnesium
ions through leaching.
Rintu Molly Johnet al., (2017) studied the effect of iron
on the liquid limit, plastic limit and hydraulic
conductivities of two soils. The results show that iron
tended to reduce the permeability of the soils. The
liquid limit and plastic limit was found to increase for
CL clay whereas for CH clay both the limits initially
decreased and then showed an increasing trend.
Soorya S.R et al., (2015) deals with an attempt to study
the effect of lead and iron contamination on the liquid
limit, plastic limit, free swell and strengthpropertiesof
high plasticity clay. The experimental resultsindicated
that the properties of clays were significantly affected
by the lead contaminationthat may influences the clay
liner performances.
Both of these contaminants not only cause ill effectson
soil but alsoleadtovariationingeotechnicalproperties
of the soil and hence the variations of geotechnical
properties on such contaminants are to be studied. In
this study variation in liquid limit and plastic limit of
bentonite and kaolinite due to different contaminants
at different molarities are studied.
1.1 Objectives of the study
The main objectives of the study include:
 Study on the variationofliquidlimitandplastic
limit of bentonite and kaolinite on iron
contamination.
 Study on the variationofliquidlimitandplastic
limit of bentonite and kaolinite on sulphur
contamination.
2. MATERIALS AND METHODOLOGY
2.1. Soil
Two types of soils were used in the study. The first one
was high plastic clay (CH)i.e., sodium bentoniteandthe
second one was low plastic clay (CL) i.e., Kaolinite. The
image of the soil sample is given in fig 1 and fig 2
respectively. The index properties are also shown in
table 1 and table 2 respectively.
International Research Journal of Engineering and Technology (IRJET) e-ISSN: 2395-0056
Volume: 07 Issue: 02 | Feb 2020 www.irjet.net p-ISSN: 2395-0072
© 2020, IRJET | Impact Factor value: 7.34 | ISO 9001:2008 Certified Journal | Page 1891
Fig-1: Bentonite
Fig-2: Kaolinite
Table -1: Properties of bentonite
SOIL PROPERTIES VALUES
Specific gravity 2.59
Liquid limit (%) 336
Plastic limit (%) 47
Shrinkage limit (%) 12.4
Plasticity index (%) 289
IS classification CH
Percentage clay (%) 82
UCS (KPa) 45.9
OMC (%) 38
Dry density (KN/m3) 12.65
Coefficient Of Permeability(m/s) 3.2x10-10
Table -2: Properties of kaolinite
SOIL PROPERTIES VALUES
Specific gravity 2.6
Liquid limit (%) 34
Plastic limit (%) 23
Shrinkage limit (%) 14.1
IS classification CL
UCS (KPa) 63
OMC (%) 20
Dry density (g/cc) 1.357
Percentage of clay (%) 66
Percentage of silt (%) 23
Percentage of sand (%) 11
2.2. Contaminants used
In the present study the contaminants used were Iron
and Sulphur. For artificially contaminating the soil
samples anhydrous ferric chloride and
sodiumthiosulphate were used. Details of the
contaminants used are given in table 3.
Table -3: Details of contaminants used
Parameters
Constituent
salt used
Chemical
formula
Molecular
weight
(g/mol)
Iron
Ferric
chloride
FeCl3 162.2
Sulphur
Sodium
thiosulphate
Na 2S 2O3 158.11
International Research Journal of Engineering and Technology (IRJET) e-ISSN: 2395-0056
Volume: 07 Issue: 02 | Feb 2020 www.irjet.net p-ISSN: 2395-0072
© 2020, IRJET | Impact Factor value: 7.34 | ISO 9001:2008 Certified Journal | Page 1892
2.3. Test procedure
In this study the soil was contaminated using Ferric
chloride and Sodiumthiosulphate. The soils was
contaminated using different molarities of
contaminants i.e., 0.05M, 0.1M, 0.2M, 0.4M, 0.8M, 1M.
The liquid limit and plastic limit tests were carried out
as per IS 2720 PART 5.
3. RESULTS AND DISCUSSION
3.1. Variationofliquidlimitinbentoniteduetoiron
and sulphur contamination.
Variation of liquid limit in bentonite due to iron and
sulphur contamination is shown in chart 1. The
experimental results show that liquid limit showed
considerable decrease with the increase in the
concentration
Chart 1: Variation in liquid limit
of iron and sulphur contamination in bentonite. This
decrease in liquid limit may be due to the increase in
salt solution. The increase in salt solution may lead to
the reduction in the thickness of diffused double layer
(Gleason et al., 1997, Schmitz et al., 2004).
3.2. Variation of plastic limit in bentonite due to
iron and sulphur contamination.
Variation of plastic limit in bentonite due to iron and
sulphur contamination is shown in chart 2.
0
10
20
30
40
50
0 0.5 1 1.5
Plasticlimit(%)
Molarity (M)
Iron
Sulphur
Chart 2: Variation in plastic limit
Theexperimentalresultsshowthatplasticlimitshowed
considerable decrease with the increase in the
concentration of sulphur contamination in bentonite.
This decrease in liquid limit may be due to the increase
insalt solution.Theincreaseinsaltsolutionmayleadto
the reduction in the thickness of diffused double layer
(Gleason et al., 1997, Schmitz et al., 2004). The plastic
limit initially showed a reduction with increase in
concentration of iron and later increased with increase
in iron concentration.
3.3. Variation of liquid limit in kaolinite due to iron
and sulphur contamination.
Variation of liquid limit in kaolinite due to iron and
sulphur contamination is shown in chart 3.
Chart 3: Variation in liquid limit
From the experimental results it was observed that the
liquid limit decreased with increase inconcentrationof
sulphur. This decrease in the liquid limit may be due to
the decrease in the net negative charges. The reduction
in negative charges causes reduction in immobilized
water; this is because the water is attracted to the
surface of the clay by electric force of various kinds
includingelectrostaticattraction(Michaels1959).Thus
causes reduction in the thickness of diffused double
layer and causes reduction in liquid limit. Liquid limit
increaseswithincreaseinconcentrationofiron(Arasan
and Yetimoglu, 2007) and this is due to the dispersion
of clay particles and formation of new swelling
compounds.
3.4. Variation ofplasticlimitinkaoliniteduetoiron
and sulphur contamination.
Variation of plastic limit in kaolinite due to iron and
sulphur contamination is shown in chart 4. From the
experimental results it was observed that plastic limit
showed considerable decrease with increase in the
concentration of sulphur, this reduction is due to the
reduction in net negative charges (Shackelford et al.,
2015). The plastic limit showed considerable increase
with iron contamination and this was in agreement
with Arasan and Yentimoglu (2007).
International Research Journal of Engineering and Technology (IRJET) e-ISSN: 2395-0056
Volume: 07 Issue: 02 | Feb 2020 www.irjet.net p-ISSN: 2395-0072
© 2020, IRJET | Impact Factor value: 7.34 | ISO 9001:2008 Certified Journal | Page 1893
Chart 4: Variation in plastic limit
4. CONCLUSIONS
The study was conductedtoinvestigatethevariationof
geotechnical properties like liquid limit and plastic
limit in bentonite and kaolinite on iron and sulphur
contamination. The conclusions made from the study
include:
 In bentonite the liquid limit reduced to about
50.8% due to iron and 57.4% due to sulphur.
 Plastic limit reduced to about 11.42% due to
iron and 48% due to sulphur in bentonite.
 An increase of about 8.82% was observed due
to iron contamination and22.6%decreasewas
observed due to sulphur in liquid limit of
kaolinite.
 Plastic limit increased to about 27.8% due to
iron and 46% due to sulphur in kaolinite.
 The reduction in negative charge and also the
reductionin diffused double layerarethemain
reasons for the variation in the geotechnical
properties in bentonite and kaolinite.
REFERENCES
[1] Arasan, S. and Yetimoglu, T (2008), “Effect of inorganic
salt solution on the consistency limits of two clays”,
Turkish Journal of Engineering and Environmental
Science 32, 107-115.
[2] Musa Alhassan (2012), “Effect of Municipal solid waste
on geotechnical properties of soils”, International
journal of Environmental Science Management And
Engineering Research,1 (5), 204-210
[3] Singh, S., and Prasad, A., (2010). “Influence of ferric
chloride and humic acid on bentonite as clay liner”,
International Journal of Geotechnical Engineering, 4:1,
pp 45-53.
[4] Strezov.V and Chaudhary, C (2017),“Impactsofironand
steelmaking facilities on soil quality”, Journal of
Environmental Management, pp 1-5
[5] Sivapullaiah, P.V. and Manju, (2005) “Kaolinite alkali
interaction and effects on basic properties”,
Geotechnical and Geological Engineering, 23, 601-614
[6] Zhibin Liu, Xin Ma, Wenlong Dai, (2011) “Experimental
Research on Engineering Property of Heavy Metal-
contaminated Kaolinite”, Applied Mechanics and
Materials Vol 94-96 pp 1921-1929

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  • 1. International Research Journal of Engineering and Technology (IRJET) e-ISSN: 2395-0056 Volume: 07 Issue: 02 | Feb 2020 www.irjet.net p-ISSN: 2395-0072 © 2020, IRJET | Impact Factor value: 7.34 | ISO 9001:2008 Certified Journal | Page 1890 Variation of liquid limit and plastic limit of clayey soils on iron and sulphur contamination Aiswarya U S1, Rani V2 1Aiswarya U S, M.tech student, Civil Engineering Department, Marian Engineering College, Kerala, India 2Rani V, Associate Professor, Civil Engineering Department, Marian Engineering College, Kerala, India ----------------------------------------------------------------------***--------------------------------------------------------------------- Abstract –a study was conducted to determine the effect of contaminants on different clayey soils. Thecontaminantsused were iron and sulphur. The variation of geotechnical properties of the clayey soils were studiedbyconductingliquid limit and plastic limit test using different molarities of contaminants. The variations at molarities 0.05M, 0.1M, 0.2M, 0.4M, 0.8M, 1M. Variations in liquid limit and plastic limits were observed with increase in concentrationofcontaminants Key Words: contamination, bentonite, kaolinite, iron, sulphur 1. INTRODUCTION Heavy metals are natural constituents of the earth crust. A number of these elements are biologically essential and are introduced into aquatic enrichments by various anthropogenic activities. Heavy metals at trace levels present in natural water, air, dusts, soils and sediments play an important role in human life.. The chemical composition of soil, particularlyitsmetal content is environmentally important, because toxic metals concentration can reduce soil fertility, can increase input to foodchain,whichleadstoaccumulate toxic metals in food stuffs, andultimatelycanendanger human health. Iron is an essential element in human nutrition. It is of great biologically significance. Lack of iron causes anaemia andit is the commonest nutritionaldeficiency in the world. Normal amounts of iron are essential, but abnormally larger amountadverselyaffectsthehuman health. Prolonged iron accumulation may cause damage in tissues Sulphur deposition in soils causes acidificationofsoilsmainlyclayeysoils.Adverseeffects of sulphur contamination of soils are shown by the fall in pH, an increase of phytotoxic aluminium concentration and by lossesofcalciumandmagnesium ions through leaching. Rintu Molly Johnet al., (2017) studied the effect of iron on the liquid limit, plastic limit and hydraulic conductivities of two soils. The results show that iron tended to reduce the permeability of the soils. The liquid limit and plastic limit was found to increase for CL clay whereas for CH clay both the limits initially decreased and then showed an increasing trend. Soorya S.R et al., (2015) deals with an attempt to study the effect of lead and iron contamination on the liquid limit, plastic limit, free swell and strengthpropertiesof high plasticity clay. The experimental resultsindicated that the properties of clays were significantly affected by the lead contaminationthat may influences the clay liner performances. Both of these contaminants not only cause ill effectson soil but alsoleadtovariationingeotechnicalproperties of the soil and hence the variations of geotechnical properties on such contaminants are to be studied. In this study variation in liquid limit and plastic limit of bentonite and kaolinite due to different contaminants at different molarities are studied. 1.1 Objectives of the study The main objectives of the study include:  Study on the variationofliquidlimitandplastic limit of bentonite and kaolinite on iron contamination.  Study on the variationofliquidlimitandplastic limit of bentonite and kaolinite on sulphur contamination. 2. MATERIALS AND METHODOLOGY 2.1. Soil Two types of soils were used in the study. The first one was high plastic clay (CH)i.e., sodium bentoniteandthe second one was low plastic clay (CL) i.e., Kaolinite. The image of the soil sample is given in fig 1 and fig 2 respectively. The index properties are also shown in table 1 and table 2 respectively.
  • 2. International Research Journal of Engineering and Technology (IRJET) e-ISSN: 2395-0056 Volume: 07 Issue: 02 | Feb 2020 www.irjet.net p-ISSN: 2395-0072 © 2020, IRJET | Impact Factor value: 7.34 | ISO 9001:2008 Certified Journal | Page 1891 Fig-1: Bentonite Fig-2: Kaolinite Table -1: Properties of bentonite SOIL PROPERTIES VALUES Specific gravity 2.59 Liquid limit (%) 336 Plastic limit (%) 47 Shrinkage limit (%) 12.4 Plasticity index (%) 289 IS classification CH Percentage clay (%) 82 UCS (KPa) 45.9 OMC (%) 38 Dry density (KN/m3) 12.65 Coefficient Of Permeability(m/s) 3.2x10-10 Table -2: Properties of kaolinite SOIL PROPERTIES VALUES Specific gravity 2.6 Liquid limit (%) 34 Plastic limit (%) 23 Shrinkage limit (%) 14.1 IS classification CL UCS (KPa) 63 OMC (%) 20 Dry density (g/cc) 1.357 Percentage of clay (%) 66 Percentage of silt (%) 23 Percentage of sand (%) 11 2.2. Contaminants used In the present study the contaminants used were Iron and Sulphur. For artificially contaminating the soil samples anhydrous ferric chloride and sodiumthiosulphate were used. Details of the contaminants used are given in table 3. Table -3: Details of contaminants used Parameters Constituent salt used Chemical formula Molecular weight (g/mol) Iron Ferric chloride FeCl3 162.2 Sulphur Sodium thiosulphate Na 2S 2O3 158.11
  • 3. International Research Journal of Engineering and Technology (IRJET) e-ISSN: 2395-0056 Volume: 07 Issue: 02 | Feb 2020 www.irjet.net p-ISSN: 2395-0072 © 2020, IRJET | Impact Factor value: 7.34 | ISO 9001:2008 Certified Journal | Page 1892 2.3. Test procedure In this study the soil was contaminated using Ferric chloride and Sodiumthiosulphate. The soils was contaminated using different molarities of contaminants i.e., 0.05M, 0.1M, 0.2M, 0.4M, 0.8M, 1M. The liquid limit and plastic limit tests were carried out as per IS 2720 PART 5. 3. RESULTS AND DISCUSSION 3.1. Variationofliquidlimitinbentoniteduetoiron and sulphur contamination. Variation of liquid limit in bentonite due to iron and sulphur contamination is shown in chart 1. The experimental results show that liquid limit showed considerable decrease with the increase in the concentration Chart 1: Variation in liquid limit of iron and sulphur contamination in bentonite. This decrease in liquid limit may be due to the increase in salt solution. The increase in salt solution may lead to the reduction in the thickness of diffused double layer (Gleason et al., 1997, Schmitz et al., 2004). 3.2. Variation of plastic limit in bentonite due to iron and sulphur contamination. Variation of plastic limit in bentonite due to iron and sulphur contamination is shown in chart 2. 0 10 20 30 40 50 0 0.5 1 1.5 Plasticlimit(%) Molarity (M) Iron Sulphur Chart 2: Variation in plastic limit Theexperimentalresultsshowthatplasticlimitshowed considerable decrease with the increase in the concentration of sulphur contamination in bentonite. This decrease in liquid limit may be due to the increase insalt solution.Theincreaseinsaltsolutionmayleadto the reduction in the thickness of diffused double layer (Gleason et al., 1997, Schmitz et al., 2004). The plastic limit initially showed a reduction with increase in concentration of iron and later increased with increase in iron concentration. 3.3. Variation of liquid limit in kaolinite due to iron and sulphur contamination. Variation of liquid limit in kaolinite due to iron and sulphur contamination is shown in chart 3. Chart 3: Variation in liquid limit From the experimental results it was observed that the liquid limit decreased with increase inconcentrationof sulphur. This decrease in the liquid limit may be due to the decrease in the net negative charges. The reduction in negative charges causes reduction in immobilized water; this is because the water is attracted to the surface of the clay by electric force of various kinds includingelectrostaticattraction(Michaels1959).Thus causes reduction in the thickness of diffused double layer and causes reduction in liquid limit. Liquid limit increaseswithincreaseinconcentrationofiron(Arasan and Yetimoglu, 2007) and this is due to the dispersion of clay particles and formation of new swelling compounds. 3.4. Variation ofplasticlimitinkaoliniteduetoiron and sulphur contamination. Variation of plastic limit in kaolinite due to iron and sulphur contamination is shown in chart 4. From the experimental results it was observed that plastic limit showed considerable decrease with increase in the concentration of sulphur, this reduction is due to the reduction in net negative charges (Shackelford et al., 2015). The plastic limit showed considerable increase with iron contamination and this was in agreement with Arasan and Yentimoglu (2007).
  • 4. International Research Journal of Engineering and Technology (IRJET) e-ISSN: 2395-0056 Volume: 07 Issue: 02 | Feb 2020 www.irjet.net p-ISSN: 2395-0072 © 2020, IRJET | Impact Factor value: 7.34 | ISO 9001:2008 Certified Journal | Page 1893 Chart 4: Variation in plastic limit 4. CONCLUSIONS The study was conductedtoinvestigatethevariationof geotechnical properties like liquid limit and plastic limit in bentonite and kaolinite on iron and sulphur contamination. The conclusions made from the study include:  In bentonite the liquid limit reduced to about 50.8% due to iron and 57.4% due to sulphur.  Plastic limit reduced to about 11.42% due to iron and 48% due to sulphur in bentonite.  An increase of about 8.82% was observed due to iron contamination and22.6%decreasewas observed due to sulphur in liquid limit of kaolinite.  Plastic limit increased to about 27.8% due to iron and 46% due to sulphur in kaolinite.  The reduction in negative charge and also the reductionin diffused double layerarethemain reasons for the variation in the geotechnical properties in bentonite and kaolinite. REFERENCES [1] Arasan, S. and Yetimoglu, T (2008), “Effect of inorganic salt solution on the consistency limits of two clays”, Turkish Journal of Engineering and Environmental Science 32, 107-115. [2] Musa Alhassan (2012), “Effect of Municipal solid waste on geotechnical properties of soils”, International journal of Environmental Science Management And Engineering Research,1 (5), 204-210 [3] Singh, S., and Prasad, A., (2010). “Influence of ferric chloride and humic acid on bentonite as clay liner”, International Journal of Geotechnical Engineering, 4:1, pp 45-53. [4] Strezov.V and Chaudhary, C (2017),“Impactsofironand steelmaking facilities on soil quality”, Journal of Environmental Management, pp 1-5 [5] Sivapullaiah, P.V. and Manju, (2005) “Kaolinite alkali interaction and effects on basic properties”, Geotechnical and Geological Engineering, 23, 601-614 [6] Zhibin Liu, Xin Ma, Wenlong Dai, (2011) “Experimental Research on Engineering Property of Heavy Metal- contaminated Kaolinite”, Applied Mechanics and Materials Vol 94-96 pp 1921-1929