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Frontiers of Earth Science

ISSN 2095-0195

ISSN 2095-0209(Online)

CN 11-5982/P

Postal Subscription Code 80-963

2018 Impact Factor: 1.205

Front Earth Sci    2011, Vol. 5 Issue (2) : 162-169    https://doi.org/10.1007/s11707-011-0166-1
RESEARCH ARTICLE
Influence of natural pozzolana and lime additives on the temporal variation of soil compaction and shear strength
Khelifa HARICHANE1(), Mohamed GHRICI1, Hanifi MISSOUM2
1. Civil Engineering Department, Chlef University, Chlef 02000, Algeria; 2. Civil Engineering Department, Mostaganem University, Mostaganem 27000, Algeria
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Abstract

Soil stabilization has been practiced for quite some time by adding mixtures, such as cement, lime and fly ash. The additives of lime (L), natural pozzolana (NP) or a combination of both were investigated here on the impact on the temporal variation of geotechnical characteristics of two cohesive soils. Lime and natural pozzolana were added at the content of 0–8% and 0–20%, respectively. The soil specimens were cured for 1, 7, 28 and 90 days and then tested for shear strength. Our data show that a combination of lime with natural pozzolana causes the increase in the maximum dry density but the decrease in the optimum moisture content in the gray soil, and vice verse in the red soil. The shear stress of both cohesive soils stabilized with lime or with the combination of lime and natural pozzolana was found to increase with time. The cohesion and the internal friction angle in lime-added samples were demonstrated to increase with time. The combination of lime with natural pozzolana exhibits a significant effect on the enhancement of the cohesion and the internal friction angle at later stages. The lime-natural pozzolana combination appears to produce higher shear parameters than lime or natural pozzolana used alone.

Keywords cohesive soil      lime (L)      natural pozzolana (NP)      compaction      shear strength     
Corresponding Author(s): HARICHANE Khelifa,Email:kharichane@yahoo.fr   
Issue Date: 05 June 2011
 Cite this article:   
Mohamed GHRICI,Hanifi MISSOUM,Khelifa HARICHANE. Influence of natural pozzolana and lime additives on the temporal variation of soil compaction and shear strength[J]. Front Earth Sci, 2011, 5(2): 162-169.
 URL:  
https://academic.hep.com.cn/fesci/EN/10.1007/s11707-011-0166-1
https://academic.hep.com.cn/fesci/EN/Y2011/V5/I2/162
Basic characteristicsSoil 1Soil 2
ColorGrayRed
Depth/m4 m5 m
Natural water content/%32.8713.77
Specific gravity2.712.84
Passing 80 μm sieve/%8597.5
Liquid limit/%84.847.79
Plastic limit/%32.7823.23
Plasticity index/%52.0224.56
Classification (USCS)CHCL
Optimum water content/%28.315.3
Maximum dry density/(kN·m-3)13.816.9
Unconfined compressive strength/kPa55.6222.5
Tab.1  Physical characteristics of the soils
Chemical compositionNatural pozzolana/%
SiO246.4
Al2O317.5
Fe2O39.69
CaO9.90
MgO2.42
CaO free
SO30.83
Na2O3.30
K2O1.51
TiO22.10
P2O30.80
Loss of ignition5.34
Tab.2  Chemical composition of natural pozzolana
Chemical nameL
Physical appearanceDry white powder
CaO>83.3
MgO<0.5
Fe2O3<2
Al2O3<1.5
SiO2<2.5
SO3<0.5
Na2O0.4-0.5
CO2<5
CaCO3<10
Specific gravity2
Over 90 μm/%<10
Over 630 μm/%0
Insoluble material/%<1
Bulk density/(g·L–1)600-900
Tab.3  Physical and chemical properties of lime used here
DesignationSample mixture/%
SoilNPL
P0L010000
P0L49604
P0L89208
P10L090100
P20L080200
P10L486104
P20L476204
P10L882108
P20L872208
Tab.4  Stabilizer combination scheme for stabilized soils
Fig.1  Compaction characteristics of the gray soil under the different combinations of additives
Fig.2  Compaction characteristics of the red soil under the different combinations of additives
Fig.3  Maximum dry density (MDD) versus optimum moisture content (OMC) for soils tested
Fig.4  Shear stress produced under normal stress of gray soil in different curing time. (a) 1 day; (b) 7 days; (c) 28 days; (d) 90 days
Fig.5  Shear stress produced under normal stress of red soil in different curing time. (a) 1 day; (b) 7 days; (c) 28 days; (d) 90 days
Fig.6  Temporal variation of shear strength characteristics in the gray soil. (a) Cohesion; (b) friction angle
Fig.7  Temporal variation of shear strength characteristics in the red soil. (a) Cohesion; (b) friction angle
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