Some Physical Properties Treatment of Expansive Soil Using Marble Waste Powder

DOI : 10.17577/IJERTV3IS10168

Download Full-Text PDF Cite this Publication

Text Only Version

Some Physical Properties Treatment of Expansive Soil Using Marble Waste Powder

1

Rozhan Sirwan Abdulla

1

2

Dr. Nadhmiah Najmaddin majeed

College of Science , Sulymania University

2

Geology Department , College of Science , Salahaddin University

Abstract

This research is an attempt to investigate the effect of marble waste powder on the stabilization of swelling soils. The two areas within the Erbil ,(Bastora and Erbil Airport ) , to investigate the swelling characteristics of soil samples and their treatment with marble waste powder taken from (Penjwen, Said Sadiq and Pirmam)areas. Index properties of the soils were determined according to unified soil classification system. The Bastora soil classified as CH group , whereas Airport soil classified as CL group.The evaluation involves the determination of the swelling potential of expansive soil in its natural state. The marble waste powders were added at percentages (10%, 20% and 30%) by weight of soil.The results show that the addition of marble dust decreases liquid limit, plasticity index and plastic limit. With increasing percentage of marble dust in expansive soils, swelling percentage decreases. Data of swelling index revealed that the swelling in Bastora soil is more than the Erbil Airport soil. While Penjwen marble waste powder is more effective to avoid the swelling problems. The Pirmam marble waste powder showed least effect. Further, the mineral composition of soil samples was studied by XRD analysis, which is also confirmed the presence of swelling minerals (Montmorillonite). The bulk mineralogy of the marble waste powder of Penjwen, Said Sadiq, and Pirmam areas include calcite, dolomite and quartz.

Keywords: Soil swelling, wastes ,XRD , plastic limit , marble dust.

1. Introduction

Swelling soils are soils that experience significant volume change associated with changes in water contents. These volume changes can either be in the

form of swell or in the form of shrinkage. Many soils that exhibit swelling and shrinking behavior contain expansive clay minerals, such as smectite (montmorilonite) that absorb water. The abundance of this mineral (smectite) in the soil led to increase its swell potential, because when it absorbs water its volume increases and swells [9,12] . In Erbil Governorate, some of the soils are essentially of the expansive variety, though these soils are considered only moderately expansive there have been different types of damages caused the structures founded on these soil. Soil stabilization is a well- known technique used to improve the physical properties of soil , the effects of mixing local sand with expansive soils on their swelling potentials also studied [5]. Numerous studies on evaluation the effectiveness of lime, cement, and combinations of lime and cement stabilization on swell potential of expansive soils[3,13,14, 8].

Mixtures of Kaolinite-Bentonite were mixed with waste marble dust for design of landfill liner explained by [15]. The potential of marble dust (by-productof marble industry) as stabilizing additive to expansive soil studied and evaluated [1] and the potential of limestone dust (LSD) and coal fly ash (CFA) to stabilize some soils problem in southeastern Pennsylvania studied[7].

2. Geology

At Bastora location good exposure of lower Bakhtiari (Mukdadiya) formation and upper Fars (Injana) formation is noticed. In addition of river terraces is occurred in Bastora valley, and good soil profile as a result of weathering of the underlying rocks characterizes the area. On the other hand Erbil Airport section belongs to Erbil plane ,during field survey no geologic formations are seen to crops out in this area. The area is covered with a thick (nearly 100-150m.) of

unconsolidated sediments, which is regarded to quaternary sediments, consisting of clay, fine silt with pebbly sands, and gravel of different grain sizes (Jassim and Goff, 2006).

3. Materials and Methods

In this study, three different types of marble waste were taken from Erbil marble factory that includes marble waste of (Penjwen, Said Sadiq, and Pirmam) which has been added to expansive soil samples was taken from two studied sections, these are Bastora area and Erbil Airport area, which were located around the Erbil city (fig 1 ) .

Figure 1. Satellite image from Google Earth of the Bastora and Erbil Airport areas

    1. Preparation of Samples

      The studied soil samples were divided into ten parts. The first part was left in its natural state, while the other nine parts were mixed with marble waste powder of (Penjwen, Said Sadiq, and Pirmam) at different percentages (10 % , 20 %, and 30%).

    2. Test Program

Grain size analysis, hydrometer tests, Atterberg limits, specific gravity and x-ray differaction analysis were carried out on each specimen in both studied areas for natural soils and soils mixed with three different types of marble waste powders with three different percentages (10%, 20%, and 30%).

The following laboratory tests have been carried out both on natural soil and stabilized soil with marble waste .

3-2-1-Particle Size Distribution

Particle size distribution of the investigated samples was determined by sieve analysis and hydrometer methods, this test is performed to determine the percentage of different grain sizes present in the soil

,accordance to American Society Test Method per standard ASTM D 422- 63.

3-2-2- Liquid Limit

The test procedures of liquid limit is performed by cone penetration method (BS 1377: 1990, test, No 2 A).

3-2-3- Plastic limit

The plastic limit procedure according to B.S 1377: 1990, test No.3

4. Results and Discussion

% Finer

The grain size analysis revealed that size of the particles in a certain soil represented in Fig ( 2 ) indicates the percentage of the particles in Bastora and Airport soil are the clay percent is about (27%,27%) whereas the silt percent is (68.58% ,69.76%) and sand percent is (4.42% , 3.24) respectively.

100

90

80

70

60

50

40

30

20

10

0

0.0001

0.001

0.01

Diam eter m m

0.1

1

% Finer

Figure ( 2 ): Grain size analysis of Bastora natural soil

100

90

80

70

60

50

40

30

20

10

0

0.0001

0.001

0.01

Diam eter m m

0.1

1

Figure 3.Grain size analysis of Airport natural soil

Figures 4 & 5 together with the expansive soil classification system , which was compiled from Holtz and Gibbs (1956), the present study show that the liquid limit of selected soil sample of Bastora natural soil is about 51.5, which classified as High potential of volume change, this indicates high swelling, while airport natural soil liquid limit is 44.4, which regarded as Medium potential of volume change, indicating medium swelling. By adding the (10%, 20%, 30%) marble waste powder of Penjwen , Said Sadiq, Pirmam to the Bastora and Airport natural soil, the liquid limit of Bastora and Airport areas decreases as the stabilizer percentage increases. The maximum reduction of liquid limit in Bastora soil is from 51.5 to 35.2 by adding 30% of the marble waste powder of penjwen and the maximum reduction of liquid limit in Airport soil is from 44.4 to 30.78 by adding 30% of the marble waste powder of penjwen. The liquid limit is more affected

Table 1. Liquid limit of Bastora natural and treated soils by addition three different percenages of different

marble waste powder

Position

Liquid Limit (LL)

Natural

Natural soil with adding

marble waste powder

Bastora natural

soil

51.5

10%

20%

30%

Penjwen

39.9

37.2

35.2

Said Sadiq

44

40.55

37.6

Pirmam

45.8

43.78

40

cone penetration (mm)

30

by addition of the marble waste powder with the soils, 25

as shown in (table 1 ). 20

natural soil

10% marble waste

20% marble waste

15 30% marble waste

) 30

m m

on( 25 10% marble waste

i t

a

r natural soil

t 20

ne

pe 15 20% marble waste

one 30% marble waste

c 10

30 35 40 45 50 55

moistuer content

cone penetration(mm)

30 10

18 28 38 48 58

10% marble waste

natural soil

20% marble waste

30% marble waste

25 moistuer content%

20 (a)

15

10

30 35 40 45 50 55

moistuer content

(a)

30

cone penetration (mm)

25 natural soil

20 10% marble waste

20% marble waste

30

25

15 30% marble waste

10

natural soil

cone penetration

25 30 35 40 45 50

10% marble waste

moistuer content %

20% marble waste

30% marble waste

20

(b)

15

10

30 35 40 45 50 55

moistuer content

(b)

natural soil

10% marble waste

20% marble waste

30% marble waste

cone penetration

30

25

20

15

10

35 40 45 50 55

moistuer content

(c)

Figure ( 4 ): Relation between moisture content% and cone penetration of Bastora soil with adding marble waste powder of

  1. Penjwen (b) Said Sadiq (c)Pirmam

    30

    natural soil

    10% marble waste

    20% marble waste

    30% marble waste

    cone penetration(mm)

    25

    20

    15

    10

    25 30 35 40 45 50

    moistuer content %

    (c)

    Figure 5. Relation between moisture content% and cone penetration of Airport soil with adding marble waste powder of

    1. Penjwen (b) Said Sadiq (c)Pirmam

Table 2. Liquid limit of Airport natural and treated soil by addition of three different percentages of different marble

waste powder

Position

Liquid Limit (LL)

Airport natural soil

Natural

Natural soil with adding

marble waste powder

44.2

10%

20%

30%

Penjwen

35

34.25

30.78

Said Sadiq

35.16

33.2

30.8

Pirmam

36.15

34.35

32.9

Addition of marble waste powder to the expansive soil, plastic limit of Bastora and Airport decreases as the stabilizer percentage increases. The maximum reduction of Plastic limit in Bastora soil is from 28.44 to 22.8 (table 3 ) by addition 30% of the marble waste powder of penjwen and the maximum reduction of plastic limit in Airport soil is from 24.20 to 17.25 (table 4 ) by addition 30% of the marble waste powder of Said Sadiq.

Table 3. Plastic limit of Bastora natural soil treated soil by addition of three different percentages % of marble

waste powder

Position

Plastic Limit (PL)

Bastora

natural soil

Natural

Natural soil with adding marble

waste powder

28.44

10%

20%

30%

Penjwen

25.23

23.58

22.8

Said

Sadiq

27.33

26.7

25.11

Pirmam

28.16

27.39

24.17

Table 4. Plastic limit of Airport natural soil treated soil by addition of three different percentages % of marble

waste powder

Position

Plastic Limit (PL)

Airport natural soil

Natural

Natural soil with adding

marble waste powder

24.2

10%

20%

30%

Penjwen

23.96

23.68

20.63

Said

Sadiq

19.33

18.7

17.25

Pirmam

20.86

20.51

19.97

Addition of marble waste powder to the expansive soil of Bastora and Airport areas, demonstrate that the plasticity index of both areas decreases as the stabilizer percentage increases

The maximum reduction of plasticity index in Bastora soil is from 23.06 to 12.40 (table 5 ) by addition 30% of the marble waste powder of penjwen and the maximum reduction of plasticity index in Airport soil is from 20 to10.15 (table 6 ) by addition 30% of the marble waste powder of penjwen. These indicate that the Plasticity index (PI) decreases when the stabilizer percentages increases.

Table 5. Plasticity index of Bastora natural and treated soil by addition of three different percentages% of marble

waste powder

Position

Plasticity Index (PI)

Bastora natural soil

Natural

Natural soil with adding

marble waste powder

23.06

10%

20%

30%

Penjwen

14.67

13.62

12.4

Said Sadiq

16.67

13.83

12.49

Pirmam

17.64

16.39

15.83

Table 6. Plasticity index of Airport natural and treated soil by addition of three different percentages% of marble

waste powder

Position

Plasticity Index (PI)

Airport natural soil

Natural

Natural soil with adding

marble waste powder

20

10%

20%

30%

Penjwen

11.04

10.57

10.15

Said Sadiq

15.83

14.5

13.55

Pirmam

15.29

13.84

12.93

According to unified soil classification system Al- Asho( 1991) the Bastora natural soil classified as (CH), and high plasticity clayey soil. Whereas Airport natural soil classified as (CL), low plasticity clayey soil .

The specific gravity in Bastora natural soil is about

2.72 gm/cm3, and for Airport natural soil is aout 2.70 gm/cm3 .

XRD analysis were done for Bastora ,Erbil Airport areas and marble waste powder of Penjwen, Said Sadiq, and Pirmam areas, to identify the clay mineralogy and bulk mineral components.The existing clay minerals in studied soil samples were identified according to first

reflection (001) and other reflections. XRD-analysis revealed the presence of (Montmorillonite, palygorskite, illite, kaolinite, and chlorite (clay minerals) Fig(6)associated with quartz, carbonate and feldspars minerals (non-clay minerals) Fig(7) and (Table 7). XRD analysis for bulk samples of waste marble powder for Penjwen area shows that the abundant non-clay mineral is calcite , dolomite and quartz figure (8).

Table 7. Mineralogical composition of the studied natural soils and Waste Marbles in Bastora and Erbil

Airports areas.

Soil types and Marbles

Arrangement of the Minerals

Clay Minerals

Non-Clay

Minerals

Bastora normal soil

Smectite, Chlorite, Palygorskite, Iillite,

Kaolinite

Quartz, Calcite, Feldspar

Erbil Airport normal soil

Smectite, Chlorite, Palygorskite, Iillite,

Kaolinite

Quartz, Calcite, Feldspar

Marble Waste

powder of Penjwen

Calcite, Dolomite, Quartz

Marble Waste powder of Said

Sadiq

Calcite, Quartz

Marble Waste powder of

Pirmam

Calcite, Dolomite, Quartz

5. Conclusion

The grain size analysis of Bastora and Erbil Airport natural soil, demonstrate that the clay percent is (27%),(27%) silt percent is (68.58%),(69.76%) and sand percent is (4.42%),(3.24%) respectively.

According to Unified Soil Classification System (USCS), the Bastora soil classified as CH group and the Erbil Airport soil as CL group .

Addition of 10 %, 20 % and 30 % of the marble waste powder of Penjwen, Said Sadiq and Pirmam areas to the (natural soil) of Bastora and Airport area led to decrease in the Liquid limits ,Plastic limits and Plasticity index .

XRD analysis for soil samples revealed that the presence of swelling mineral such as Smectite in both studied areas. Other present clay minerals include were , palygorskite, illite, kaolinite and chlorite. In addition to mixed layer, illite-palygorskite and smectite-chlorite. Non- Clay minerals include calcite, quartz and feldspars. The bulk mineralogy for Marble waste powder of Penjwen, Said Sadiq and Pirmam areas, include; calcite, dolomite, with few quartz minerals.

References

[1] Agrawal, V. and Gupta, M., 2011, Expansive soil stabilization using Marble dust ,international Journal of Earth Sciences and Engineering,Vo.4,No.6 SPL, pp 59-62. [2]Al-Asho, M.O., 1991, Principles of soil mechanics. Dar Al-Kutib. Mosul University (in Arabic). 574 p.

  1. Al-Rawas, A. A., Taha, R., Nelson, J.D., Al-Shab, T.B. and Al-Siyabi, H., 2002, A Comparative evaluation of various additives used in the stabilization of expansive soils. Geotechnical Testing Journal, Vol. 25, No. 2, pp. 199-209.

  2. ASTM D 422-63, 2007, Standard Test Method for Particle-Size Analysis of Soils.

  3. Basma, A. A., Al- Rawa, A.A., Al-Saadi, S.N. and Al- Zadjali, T.F., 1998, Stabilization of expansive clays in Oman. Environmental and Engineering Geosciences, Vol. IV, No.4. pp. 503-510.

  4. British Standard Institution, 1990, Method of test of soils for civil engineering purpose (BS 1377 part :2), London.

  5. Brooks, R., Udoeyo, F.F., and Takkalapelli, K.V., 2011, Geotechnical Properties of Problem Soils Stabilized with Fly Ash and Limestone Dust in Philadelphia. http://link.aip.org/link/doi/10.1061/(ASCE)MT.1943- 5533.0000214, 6 p.

  6. Chavva P.K., Vanapally, S.K., Puppala, A.J. and Hoyos, L., 2005, Evaluation of Strength, Resilient Moduli, Swell, and Shrinkage Characteristics of Four Chemically Treated Sulfate Soils, from North Texas, GSP 136, ASCE Special Publication, Geofrontiers, Austin

  7. Chen, F.H, 1988, Foundation on expansive soils, Elsevier, Amsterdam.

  8. Holtz, W. G. and Gibbs, H. J., 1956, Engineering Properties of Expansive Clays. Trans. ASCE, 121, pp. 641- 663.

  9. Jassim, S.Z. and Goff, J.C. 2006, Geology of Iraq. Dolin, Prague and Moravian Museum, Brno, Czech Republic. 341p.

  10. Nelson, J.D. and Miller, D.J., 1992, Expansive Soils, Problems and Practice in Foundation and Pavement Engineering, John Wiley and Sons Inc., New York.

  11. Parson, R.L. and Milburn J.P., 2003, Engineering behavior of stabilized soils ,Transportation research record, Journal of the Transportation Research Board,Washington, DC- 0361-1981, pp. 20-29.

  12. Winterkorn, H.F. and Pamukcu ,S., 1991, Soil stabilization and groutin. Foundation Engineering Hand book (2nd Edition), New York: Van Nostrand Rein hold, pp. 317-378.

  13. Zorluer, I. and Taspolat, L.T., 2009, Reuse of waste marble dust in the landfill layer. First International Symposium on Sustainable Development. Sarajevo, Bosnia and Herzegovina. pp. 301-305.

    I-P

    S+Ch K

    S+Ch: Smectite+Chlorite I-P: Illite-Palygorskite K: Kaolinite

    sity n te

    In

    Heated (550 °C) Ethylene Glycol

    Normal

    4 6 8 10 12 14 16 18

    2 °

    ( a )

    Ch

    I-P

    S K

    S: Smectite Ch: Chlorite

    1. P: Illite-palygorskite K: Kaolinite

      Intensity

      Heated (550 °C) Ethylene Glycol

      Normal

      4 6 8 10 12 14 16 18

      2 °

      ( b )

      Figure 6 XRD pattern of the clay fraction of natural soil of

      1. Bastora area (b) Erbil Airport area

Intensity

Smectite

Ilite-Palygorskite

Kaolinite

Quartz

Calcite

Quartz

Feldspar

Calcite

Quartz

Quartz

5 10 15 20 25

30

2

35 40 45

Quartz

Calcite

( a )

Intensity

Smectite

Ilite-Palygorskite

Kaolinite

Quartz

Calcite

Feldspar

Quartz

Quartz

5 10 15 20 25 30 35 40 45

2 (b)

Figure 7. XRD of the bulk natural soil of Erbil

  1. Bastora area (b) Airport area

    Intensity

    Calcite

    Calcite

    Dolomite

    Quartz

    Quartz

    5 10 15 20 25 30 35 40 45

    2

    Calcite

    (a)

    Intensity

    Calcite

    Quartz

    Quartz

    5 10 15 20 25 30 35 40 45

    2

Intensity

Calcite

Calcite

Dolomite

Quartz

Quartz

5 10 15 20

25

2

30 35 40 45

( c )

Figure 8. XRD of the bulk Mrable Waste Powder of

  1. Penjwen (b) Said Sadiq (c) Pirmam area

Leave a Reply