Keywords

1 Introduction

The study area comprising part of Godavari delta extends over Andhra coast from Rajahmundry to Narsapur. Geographically, the area lies between, 81.8040° E to 81.6966° E Long. and 16.4330° N to 17.0005° N Lat. and is covered by Survey of India topographical map Nos. 65 D & Hand 66 A & E. The north-western boundary touches the Madras- Calcutta grand trunk road passing through Vijayawada, Eluru and Rajahmundry. Administratively, the area falls in the jurisdiction of East and West Godavari districts of Andhra Pradesh. The delta is nearly flat and highly irrigated. The geological succession of the area comprises alluvial deposits (Recent period), Deccan trap (Eocene), Gondawana (Carboniferous), Cuddapah-Kurnool and Dharwars (Cambrian) and granite-gneisses (Archaean). The area receives rainfall both in south-west and north-east monsoon periods. The actual rain fall in the East Godavari District is 449.7 mm and the actual rain fall in the West Godavari district is 442.0 mm. The main soil groups are Black cotton soils with the subgroup Typical Pellusterts and Chromusterts with the essential clay mineral as fine montmorillonitic. The area under study has many tile factories where in untreated effluent comprising sludge made up of grounded tiles and water is left into the cultivable land rendering them nearly useless.

Vitrified Tiles are the latest and largest growing industry alternate for many tiling requirements across the globe with far superior properties compared to natural stones and other manmade tiles. India and China are the largest regions to contribute to the 6900 million square meters of production every year. With an annual growth rate of 20% worldwide and 25% in India, Vitrified tile is the fastest growing segment in the tile industry. Vitrified tiles own 12% share of the overall tile production across the world. With the increase in production of vitrified tiles in India, there is growing concern about the huge generation of tile polishing dust.

The raw material composition of Vitrified tiles is:

  • Quartz of 99% Silica,

  • Potash Feldspar of 12% to 14% Alkalis,

  • Soda Feldspar of 12% to 14% Alkalis,

  • Strengthening agent, China clay, body stains for producing in various colors.

VTS is collected from a tile factory situated at Narayanapuram Village, Ungutur Mandal, West Godavari, Tadepalligudem - 534407, Andhra Pradesh, India. The physical properties of Vitrified Tile Sludge (VTS) are given in the Tables 1 and 2 below.

Table 1. Chemical properties of Vitrified Tile Sludge (VTS)
Table 2. Engineering properties of pure vitrified tile sludge

The current experimental study is concerned with the selection of approximate type of soil to achieve a very high degree of compaction and to expose the compaction properties of clay. The results of the study can provide thoughts for applying clay soil in various applications of soil stabilization process.

1.1 Objectives of the Study

The following are the main objectives for the present study:

  1. (a)

    Evaluate the limiting VTS content to reduce the plasticity i.e., Atterberg limits viz., Liquid limit by 20% and Plastic limit by 10% off the native clayey soil

  2. (b)

    To increase the sub grade soil stiffness of the soil by at least 25%.

2 Literature Review

Al-Rawasa et al. (2005) has tried to stabilize expansive soil with lime, cement, combinations of lime and cement, sarooj (Artificial pozzolana), heat treatment and have found that with the addition of 6% lime, both the swell percent and swell pressure reduced to zero and heat treatment reduced swelling potential to zero. Al-Rawas et al. (2002) investigated the effectiveness of using cement by-pass dust, copper slag, granulated blast furnace slag, and slag-cement in reducing the swelling potential and plasticity of expansive soils. Bell (1989) through his experiments on Clayey soil showed that addition of a small percentage of lime enhanced many of the engineering properties of the soil. Boardman et al. (2001) with the help of two clay minerals assessed to assess the time-dependent effects of mineral structural chemistry on the lime–clay reaction. Briptive (2004) emphasized the need of a quick or simple test to show the amount of lime required to react chemically with a soil to bring about these physical changes to an optimum degree. Buhler and Cerato (2007) and Modak et al. (2012) mixed highly expansive soil with lime and class C fly ash to study the plasticity reduction in highly expansive natural clays from Idabel, Oklahoma. Çokça (2001) has used, high-calcium and low-calcium class C fly ashes from the Soma and Tuncbilek thermal power plants, respectively, in Turkey, for stabilization of an expansive soil. An evaluation of the expansive soil-lime, expansive soil-cement, and expansive soil-fly ash systems is presented. Cristelo et al. (2013) have studied the effects of sodium-based alkaline activators and class F fly ash on soil stabilization. Eades and Grim (1966) tried to show through simple test, the amount of lime required to react chemically with a soil to bring about these physical changes to an optimum degree. Edil et al. (2006) have evaluated the effectiveness of self-cementing fly ashes derived from combustion of sub-bituminous coal for stabilization of soft fine-grained soils. Addition of fly ash resulted in appreciable increases in the California bearing ratio (CBR). Ferguson (1993) had reported that Ash treatment can effectively reduce the swell potential of fat clay soils and increases the sub grade support capacity of pavement sub grades. Greeves (1996) used expansive black cotton soil to assess the influence of ambient temperature in the progress of lime-soil reactions. Higgins (2005) reported the incorporation of ground granulated blast furnace slag to combat the soil expansion. Hunter (1988) studied the expansive reactions between lime and sulfate‐bearing clay soils and reported that the long‐term pozzolanic chemistry of normal lime‐soil reactions found to be disrupted while Cation exchange, agglomeration, and carbonation are unaffected. Jones and Holtz (1973) studied the relationship between the mineralogical composition and water chemistry and their relationship to geotechnical properties and engineering structures failures. Kamon and Nontananandh (1991) prepared a product by burning industrial wastes along with lime to produce a by‐product having cementing characteristics and showed that the resulting by‐product is of promise for use in stabilizing a loam soil. Khattab et al. (2007) have evaluated the long-term stability characteristics of lime-treated expansive soils to improve the properties of expansive soils. Matsuo and Kamon (1981) have investigated a new stabilization method of soft clay soils using multivalent cations, trivalent cations, e.g. Fe3+ and A13+. The beneficial effects of this treatment are clarified not only for engineering properties but also for microscopic mechanisms (ionization process and aggregating phenomenon). McCarthy et al. (2014), investigated the engineering and durability properties of lime-stabilized soils treated with low-lime fly ash to limit swelling (heave) due to sulphate, associated with the ground improvement process. Turkoz et al. (2014) have evaluated the effect of magnesium chloride (MgCl2) solution on the engineering properties of clay soils. The results show that dispersive and expansive clay soils can be effectively improved using an additive MgCl2 solution. Puppala (2003) investigated with class F fly ash, sulphate-resistant cement, ground granulated blast furnace slag (GGBFS) and lime mixed with fibers as potential stabilizers in enhancing the strength and volume change properties of soft, expansive and sulphate-rich soils. Petry and Armstrong (1989) had developed performance-based testing of chemical stabilizers that simulate field conditions. The situations included a physical erosion test to determine dispersion of clays that have been treated, two swell test preparation sequences simulating injection of chemicals into clays, a wet-dry test sample preparation using field gradation specifications, and a three-dimensional swell test for stability of treated clays when subjected to wetting. Petry (1997) used Chemical stabilizing agents to improve the behavior of earth materials. Rao and Subba Rao (1994) have discussed the cause of ground heave of an inherently non-swelling, kaolinite-rich red soil (from Bangalore, India) due to prolonged spillage of concentrated (40%, weight/weight solution) caustic soda (sodium hydroxide) solution into the sub-soil through cracked drains in an industrial establishment. Treatment of the contaminated ground with 5% ferric chloride solution and simultaneously measures to minimize caustic soda solution spillage mitigate the soil against heave from caustic soda attack. Reddy et al. (2015) have employed three types of additives viz., (a) Cementitious: lime and fly ash (b) Non-cementitious: stone dust, and (c) Chemical additives: CaCl2 and Na2SiO3 to evaluate the performance of stabilized expansive soils. They investigated the influence of valence of cations (viz., monovalent, divalent and trivalent) and mean particle diameter of additive(s) on percentage reduction of swelling characteristics. Their results revealed that chemical additives exhibit superior performance over cementitious and non-cementitious additives in reducing the swelling characteristics. Brooks (2009) studied the suitability of expansive soil as a construction material using rice husk ash (RHA) and flyash. Saha and Saha (1991) have upgraded expansive soil as a construction material using rice husk ash (RHA) and flyash, a cost comparison was made for the preparation of the sub-base of a highway project with and without the admixture stabilizations. When the RHA content of 12% and a flyash content of 25%, Unconfined Compressive Stress increased by 97% while CBR improved by 47%. Sivanna (1976) had studied the problem of damage to structures in expansive soils world wide and have proposed that sodium carbonate and calcium carbonate is stabilizing a black cotton soil. Sivapullaiah studied the effect of electrolytes on the shear strength of clayey soils. Abood et al. (2007) had investigated the effect of adding different chloride compounds including (NaCl, MgCl2, CaCl2) on the engineering properties of silty clay soil. The increase in the percentage of each of the chloride compounds increased the maximum dry unit weight and decreases the optimum moisture content. While the liquid limit, plastic limit and plasticity index decreased with the increase in salt content, the unconfined compressive strength increased with the increase in salt content. Nalbantoglu (2001) has shown that Fly ash treatment has tremendous potential as an economical method for the stabilization of the soil. Significant reduction in the swell potential and an increase in the hydraulic conductivity values were reported.

3 Need for Study

From the literature review it is observed that: Almost all of the researchers have studied the effect of (1) Industrial Byproducts (Fly ash, Rice Husk Ash), (2) Chemical additives (Lime, Caustic Soda, Calcium Carbonate, Sodium Carbonate, Magnesium Chloride, Mono-valence, Divalent and trivalent compounds).

Effect of treatment on soil properties like specific gravity, liquid limit, plastic limit, plasticity index, grain size analysis, shear strength of soil and bearing resistance have been studied. Long-term behavior of soil like consolidation properties, hydraulic conductivity and resilient modulus has not been studied by most researchers.

  • There are many methods of laboratory experimentation to inhibit soil expansion but very few field methods to forecast soil expansion are available.

  • Stress – strain behavior of the modified soil needs to be studied.

  • Very minimal or no research has been conducted on industrial waste sludge despite the fact that they constitute environmental hazards and could have their usefulness in soil stabilization.

4 Experimental Studies

The methods adopted for the present study of investigation are presented below: Natural moisture content of the soil samples is determined as per IS: 2720 (Part II) “Methods of Test for Soils” (Water Content), BIS, New Delhi. The specific Gravity of the soil is determined as per 38. IS 2720 Part-III/Section 2 (1997), “Methods of Tests for soils” (Specific Gravity), BIS, New Delhi. The grain size analysis is conducted as per IS 2720 Part-IV (1995), “Methods of Tests for soils” (Grain Size Analysis), BIS, New Delhi.

The liquid, plastic limit (Atterberg’s limits) are determined as per IS 2720 Part-V (1995), “Methods of Tests for soils” (Atterberg Limits), BIS, New Delhi. THE maximum unit weight and optimum moisture content for a given effort of compaction are obtained as per IS 2720 Part-VIII (1997), “Methods of Tests for soils” (Proctor’s Compaction Test), BIS, New Delhi. The bearing resistance of the soil in soaked and un-soaked conditions is determined as per IS: 2720 (Part-16) (1979), “Methods of Tests for soils” (California Bearing Ratio), BIS, New Delhi. In CBR (Fig. 1) testing the rate of penetration of the plunger was kept at 1.25 mm/min and Proving ring capacity is 10 KN. Soaked CBR values at 2.5 mm and 5 mm penetration were calculated for all the samples.

Fig. 1.
figure 1

Liquid limit of clayey soil admixed with different proportions of VTS

While the Unconfined Compressive strength of the soil is determined as per IS 2720 (Part-10) (1991), “Methods of Test for Soils”, (Unconfined Compressive Strength), BIS, New Delhi. UCS testing is based on the fact that the minor principal stress is zero and the angle of internal friction of the soil is assumed to be zero. Strain controlled testing was followed and a strain rate of 1% per minute is used. At the time of testing loading is continued until the load on the specimen begins to decrease or until at least 20% of strain has been reached. In this case for the sample of 76 mm height 20% strain amounts to 0.2 × 76 = 15.2 mm.

Specimens for CBR and UCS testing are prepared at predetermined water content and unit weight. The free swell Index is determined as per IS: 2720 Part XL (1977), “Methods of Test for Soils”, Determination of Free Swell Index of Soils, BIS, New Delhi.

5 Results and Discussion on Results

The native clayey soil is admixed with VTS by varying its proportion and the optimum content of the VTS is determined (Table 3). The admixed proportions of VTS considered in this study are 0%, 10%, 20%, 30% and 40%.

Table 3. Summary of the laboratory test results

The following paragraphs describe the laboratory results (Table 4).

Table 4. Summary of the test results obtained with different proportions of the VTS with Clayey soil

The above values are plotted against the different proportions of VTS admixed with the Clayey soil. The following are the observations found from these tests:

  1. (a)

    As the admixed proportion of VTS increases from 10% to 40%, the liquid limit of the clayey soil is decreasing gradually (Fig. 1). The curve observed as falling trend. The similar trend is also observed in case of plastic limit of the soil (Fig. 2).

    Fig. 2.
    figure 2

    Plastic limit of the soil obtained with different proportions with VTS

  2. (b)

    In contrast, the dry unit weight of the soil is gradually increasing with slight reduction with OMC (Fig. 3).

    Fig. 3.
    figure 3

    Dry unit weight of the soil obtained with different proportions with VTS

  3. (c)

    The soaked CBR values are gradually increased from 2.34% to 5.04% with 0% and 20% replacement and there onwards the CBR values are found to be decreasing with further increasing of the VTS content (Fig. 4).

    Fig. 4.
    figure 4

    Soaked CBR values of soil obtained with different proportions of VTS

  4. (d)

    The UCS values are gradually increased from 6.68% to 8.5% with 0% and 20% replacement and thereafter, the UCS values are found to be decreasing with further increasing of the VTS content (Fig. 5).

    Fig. 5.
    figure 5

    UCS values of soil obtained with different proportions of VTS

6 Conclusions

The following are the conclusions drawn from the present study:

  1. (a)

    Addition of varied Vitrified Tile Sludge (VTS) content has improved the properties of the clay sample.

  2. (b)

    Replacement of Vitrified Tile Sludge by 20% is found to be optimum.

  3. (c)

    The flow characteristics, plasticity characteristics and shrinkage characteristics of the soil sample are gradually decreasing with increase in the percentage of VTS in the clay sample.

  4. (d)

    At the optimum VTS content of 20% replacement, the maximum dry density, soaked CBR value and UCS values are obtained as 1.635 gm/cc, 5.2% and 85, respectively.

Hence, it is concluded that the VTS as a waste product can also be used for soil stabilization purpose and the obtained results are based on this single study, further investigation is required to confirm the findings.