UNIVERSITY OF NAIROBI EFFECT OF QUARRY DUST ON THE PHYSICAL PROPERTIES OF LATERITIC GRAVEL AS SUBBASE MATERIAL BY: ALVIN HABWE WETANGULA, F16/21400/2007 A project submitted as a partial fulfillment for the requirement for the award of the degree of BACHELOR OF SCIENCE IN CIVIL ENGINEERING 2015 1 ACKNOWLEDGEMENT I would like to acknowledge Eng. Elvis Cheruiyot Kipkorir for inspiring me to take this step to becoming a competent materials Engineer, Prof. Sixtus Kinyua Mwea and Eng. Dionysius Maina Wanjau for the encouragement that got me this far, Eng. Evans Goro who supervised me and steered my project in the right direction, and finally to the Lord almighty for getting me through the Bachelor of science in civil engineering 2 DEDICATION I dedicate this project to my father and mother who have worked hard and sacrificed to ensure that I reach this far in life, and to my brothers and sisters who have given me support. Thank you very much. 3 TABLE OF CONTENTS ACKNOWLEDGEMENT DEDICATION TABLE OF CONTENTS LIST OF FIGURES LIST OF TABLES ABBRIVIATIONS USED ABSTRACT CHAPTER ONE 1.0 INTRODUCTION 1.1 SUMMARY 1.1.1 QUARRY DUST 1.1.2 ROAD CLASSIFICATION 1.1.3 EXISTING ROAD CLASSIFICATION 1.1.4 SUB-BASE 1.1.5 LATERITIC GRAVEL 1.2 PROBLEM STATEMENT 1.3 JUSTIFICATION 1.4 OBJECTIVES 1.5 SCOPE CHAPTER TWO 2.0 LITERATURE REVIEW 2.1 SOIL 2.2 SOIL STABILIZATION 2.2.1 SOIL STABILIZATION METHODS 2.2.1.1 STABILIZATION BY USE OF STABILIZING AGENTS 2.2.1.1.1 CEMENT STABILIZATION 2.2.1.1.2 LIME STABILIZATION 2.2.1.1.3 BITUMINOUS STABILIZATION 2.2.1.2 STABILIZATION BY COMPACTION 2.2.1.3 SOIL STABILIZATION TO CONTROL SHRINK SWELL 2.2.1.4 SOIL STABILIZATION TO REDUCE WATER CONTENT 2.3 QUARRY DUST 2.3.1 PROODUCTION 2.3.2 QUARRY DUST CHARACTERISTICS 2.3.3 EFFECTS OF QUARRY DUST 4 2.3.4 2.3.5 UTILIZATION APPPLICATIONS OBSTACLES TO UTILIZATION CHAPTER THREE 3.0 METHODOLOGY 3.1 PREPERATION OF MATERIALS 3.2 PRELIMINARY TESTS 3.2.1 COMPACTION 3.2.2 CALOFORNIA BEARING RATIO 3.2.3 PARTICLE SIZE ANALYSIS OF SOILS 3.2.4 ATTERBERGS LIMITS CHAPTER FOUR 4.0 RESULTS AND ANALYSIS 4.1 COMPACTION TEST 4.2 CBR TEST 4.3 ATTERBERGS LIMIT TEST 4.4 PARTICLE SIZE DISTRIBUTION TEST CHAPTER FIVE 5.0 DISCUSSION, CONCLUSION AND RECOMMENDATION 5.1 DISCUSSION 5.2 CONCLUSION 5.3 ECONOMIC JUSTIFICATION 5.4 RECOMMENDATIONS CHAPTER SIX 6.0 REFFERENCES LIST OF FIGURES Figure 1 the different layers of a road Figure 2 Typical cement stabilization of soil Figure 3 Typical lime stabilization of soil Figure 4 Typical bituminous stabilization of soil Figure 5 Typical Quarry Figure 6 Typical Quarry Dust Figure 7 Equipment for standard compaction test 5 Figure 8 CBR loading press Figure 9 Sieve analysis Figure 10 Equipment for Atterberg Limits test equipment CHAPTER ONE 1.0 INTRODUCTION 1.1 Summary This project comprises of detailed investigation of how quarry dust can be used as a suitable agent of stabilizing lateritic gravel. A cost evaluation has also been done so as to establish the cost effectiveness of stabilization with quarry dust. 1.1.1 Quarry Dust Quarry dust can be defined as residue, tailing or other non-voluble waste material after the extraction and processing of rocks to form fine particles less than 4.75 mm. It is a waste from stone crushing units and accounts for about 25% of the final product. Quarry dust which is released directly into environment can cause environmental pollution. To reduce the impact of the quarry dust on environment and human, this waste can be used to produce new products or can be used as admixture in concrete so that the natural resources are used efficiently and hence environmental waste can be reduced 1.1.2 Road Classification Road Infrastructure is a key driver to development of Nations. A road classification system has several purposes which are interrelated. Key among these are: 6 Planning. The application of a road classification provides a framework for policy formulation in road administration and management. Road classification assists planners in allocating resources for maintenance and development for the road network between different groups of roads and also for setting priorities. Design. A road classification system indicates an expected level of service for specific road classes and therefore provides guidance to design engineers in applying appropriate design standards. Administration. Road classification also clarifies responsibilities amongst road administrations and the assignment of road sub-networks. Usage. A well-defined and consistent road classification system influences road user expectations, behavior and performance in traffic which improves the effectiveness with which the road network carries traffic. Hence the road classification system should provide road users with some confidence in the level and continuity of service intended to be provided. 1.1.3 Existing Road Classification System CLASS DESCRIPTION A FUNCTION International Trunk Roads Link centers of international importance and cross international boundaries or terminate at international ports or airports B National Trunk Roads Link nationally important centers C Primary Roads Link provincially important centers to each other or to higher class roads D Secondary Roads Link locally important centers to each other, or to more important centers or to a higher class road 7 E Minor Roads Any link to a minor center SPR G Government Roads L Settlement Roads R Rural Access Roads S Sugar Roads T Tea Roads W Wheat Roads Unclassified All other public roads and streets U The required CBR of the sub-base varies in the different road classes depending on the loading requirements. 1.1.4 Sub-base The sub base layer is a critical layer in road construction. This layer acts as the foundation of the road. It comes between the sub grade and the base. Sub base should be properly designed since it is the main load bearing layer of a pavement. It is primarily designed to evenly spread the applied load of the top paving layers and the traffic to the sub grade below. Due to this, proper design of the sub base will prevent channelization and settlement of the pavement from occurring. The sub base also protects the base from adverse effects of the sub grade. There are several materials used in making the sub base; these include graded crushed stones (GCS) 0/30mm or 0/40 mm, stabilized red soil or gravel. The stabilization can either be mechanical or chemical. The mechanical stabilization involves addition of milled asphalt, hoggins, slag, scalping. The chemical stabilization involves addition of cement lime or pozzolanic ash 8 Figure 1 The different layers of a road Function of the layers of a road: Surface - To increase the skid resistance of the road surface Binder Course - It is designed to reduce rutting and withstand the highest stresses Asphalt base Course - Providing adequate durability since this layer is not exposed to the environment. Base - To redistribute the applied load from the surface course to the sub base Sub-base and subgrade - Consist of unbound materials, such as indigenous soil, crushed or uncrushed aggregate, or re-used secondary material and constitute the foundations of the road structure, and 1.1.5 LATERITIC GRAVEL 9 Lateritic gravel is widely used in road construction due to its high strength and low plasticity compared to other soils. However to improve the properties of the lateritic gravel, stabilization is done. This lowers the plasticity incase the lateritic gravel contains significant amounts of fines. Lateritic gravels and laterites are formed through intense leaching of well drained soils under tropical and sub-tropical climates. 1.2 PROBLEM STATEMENT The sub-base layer being a very important layer in road construction needs proper design and use of high quality material. Stabilization using cement and lime has proved to be effective over the years. However due to the high prices of this stabilizers other methods need to be in co-operated so as to reduce the cost of stabilization and hence reducing the cost of constructing the road. There are various cheap methods of stabilizing the soils which are currently used in road construction. 1.3 JUSTIFICATION Quarry dust is a waste from stone crushing units and is therefore readily available at an affordable price. Quarry dust contains non plastic sand particles and will therefore lower the plasticity index of the gravel. Quarry dust has a higher CBR value than gravel because it is obtained from crushing stones and would therefore increase the gravels bearing capacity. Quarry dust contains a lot of fine grained particles and will therefore be within the required grading curve envelope 1.4 OBJECTIVES 1. To determine the effect of quarry dust on plasticity and shrinkage of lateritic gravel as sub material 2. To determine the effect of quarry dust on bearing strength of lateritic gravel as sub base material. 3. To determine the effect of quarry dust on particle size distribution of lateritic gravel as sub base material. 1.5 SCOPE 10 The materials to be used will be locally available materials. The California Bearing Ratio (CBR), the Attebergs limits and the sieve analysis are the tests which will be conducted to determine the effect of addition of the quarry dust on physical properties of lateritic gravel. A study of the past works done by other people will also be used to make references. CHAPTER TWO 2.0 LITERATURE REVIEW 2.1 SOIL Soil is unconsolidated mineral and organic matter on the earths surface. Soil comprises of organic matter, solids and voids. The voids are filled with air and water. Soil can be organized into the following three basic groups: Cohesive soils-This are soils which contains silts and clay particles. The particles are dense and tightly bound together by molecular attraction. They are plastic when wet. Granular soils-This contains sand particles which ranges from size 0.03 – 0.08 and medium gravel which ranges from size 0.08 – 1.0.Granular soil is water draining and obtains maximum dry density (MDD) at either saturated or full dry state. Organic soils-This is not suitable for compaction and not applicable in engineering. 2.2 SOIL STABILIZATION Soil stabilization is the alteration of soil properties to improve the engineering performance of soils. The properties most often altered are density, water content, plasticity and strength. Soil stabilization is classified into: Chemical stabilization- this involves the addition of cement or lime Mechanical stabilization- this is the use of locally available materials such as milled asphalt, hoggins and slag to achieve the desired soil properties. Thermal stabilization- this involves heating the soil to be stabilized with some additives such as cryolite, borax, and glass. 11 2.2.1 STABILIZATION METHODS 2.2.1.1 STABILIZATION BY USE OF STABILIZING AGENTS The incorporation of stabilizing agents, usually in relative low amounts, alters both physical and chemical properties. Lime and cement as well as bitumen have a wide application. 2.2.1.1.1 CEMENT STABILIZATION Factors which have made use of Portland cement popular as a stabilizer in the world are: Almost any soil can be stabilized with Portland cement if enough cement is used in combination with the right amount of water and proper compaction and curing. More information is available on cement-treated soil mixtures than other types of soil Stabilization Cement is readily available in most countries as home product. Mechanism of cement stabilization Upon coming into contact with water, the major hydration products of cement are; calcium silicate hydrates, calcium aluminates hydrates and hydrated lime of which the first two constitute the major cementitious component while lime is deposited as a separate crystalline solid phase. When cement is present in granular soil, the cementation is probably very similar to that of concrete, except that the cement phase does not fill the voids between the soil particles. Cementation is by means of mechanical bonding of calcium silicate and aluminates hydrates to the rough mineral surfaces. When cement is used to stabilize fine grained soils, cementation is both mechanical and chemical bonding involving reaction between the cement and the surfaces of soil particles. As more cement is added quantity of silt and clay is reduced progressively and coarse material of lower water retention capacity and volume stability value is obtained: this is a cement modified soil. As more and more cement is added a quantity of coarse grained material is increased where all the soil grains remains a solid mass.(S. B. SEHGAL, 1984). Materials for soil-cement stabilization Soil, Portland cement, and water are the three basic materials needed to produce soil-cement. Low cost is achieved mainly by using inexpensive local materials. The soil that makes up the bulk of soil-cement is either in place or obtained nearby, and the water usually hauled over short distances. The quantities of Portland cement and water to be added and the density to which the mixture must be compacted are determined from tests. The water serves two purposes: It helps to obtain maximum compaction (density) by lubricating the soil grains and It is necessary for hydration of the cement that hardens and binds the soil into a solid mass. 12 Properly produced soil cement contains enough water for both purposes. The cement could be almost any type of Portland cement that complies with the requirements of the latest ASTM (American Safety for Testing and Materials) and AASHTO (American Association of State Highway and Transportation Officials) Types I (normal) and IA (air entrained) Portland cements are the most commonly used. The water used in soil-cement should be relatively clean and free from harmful amounts of alkalis, acid, or organic matter. Water fit to drink is satisfactory. Sometimes seawater has been used satisfactorily when fresh water has been unobtainable. Figure 2 Typical cement stabilization of soil 2.2.1.1.2 LIME STABILIZATION Expansive soils are normally very suitable for lime stabilization. This increases the bearing capacity and reduces the potential swelling in the top layer of the sub grade. The treated layer is more impermeable so moisture variations are reduced. When lime is added to plastic material, it first flocculates the clay and substantially reduces plasticity index. This reduction is time dependent during the initial weeks, and has the effect of increasing the optimum moisture content and decreasing the maximum dry density in compaction. The compaction characteristics are therefore constantly changing with time and delays in compaction causes reduction in density and consequently reduction in strength and durability. The workability of the soil also improves as the soil becomes more friable. Both the ion exchange reaction and the production of cementations materials increase the stability and reduce the volume change within the clay fraction. The swell may even be reduced from 7% or 8% to 0.1% by the addition of lime. The production of cementitious material can continue for some time but the materials and the environment will influence the strength developed. (ALAN EVERETT, 1981). The reaction between various types of lime can be represented by: CaCO3 + heat = CaO + CO2 13 This reaction is reversible and it does not occur much below 5000 C and is the basis for the manufacture of quick lime from chalk or limestone. CaO + H2O = Ca (OH)2 + heat Hydrated lime is produced as a result of the reaction of quick lime with water. Ca(OH)2 + CO2 = CaCO3 + H2O Hydrated lime will form calcium carbonate upon exposure to air where it reacts with carbon dioxide present in air. Figure 3 Typical lime stabilization of soil 2.2.1.1.3 BITUMINOUS STABILIZATION Bitumen is solid or viscous liquid, which occurs in natural asphalt or can be derived from petroleum. It has strong adhesive properties and consists essentially of hydrocarbons. In natural condition it is too viscous to be used for stabilization and has to be rendered more fluidic either as “cut-back” bitumen or a “bitumen emulsion”. Cut back bitumen is a solution of bitumen in kerosene or diesel; when solvent evaporates bitumen is deposited. Emulsions are suspensions of bitumen particles in water; when the emulsion breaks the bitumen is deposited on the material to be stabilized. Unlike cement and lime, which reacts chemically with material being stabilized, bitumen acts as a binding agent, which simply sticks particles together thus preventing water ingress. Bituminous stabilization is uncommon in areas with high rainfall due to the high level of moisture content in the soil and addition of further fluids in form of bituminous materials may cause loss of strength. This is a process where the grading is improved by the incorporation of another material, which affects only the physical properties of the soil. Unlike stabilization by the incorporation of stabilizing agents the proportion of material added usually exceeds 10% and may be as high as 14 50%.Mechanical stabilization has drawbacks particularly in those countries which have heavy rainfall or where frost is a problem. Although a mechanically stable material is highly desirable it cannot always be achieved and even when it can it is often necessary to add a stabilizing agent to bring about a further improvement in the properties of a material. Figure 4 Typical bituminous stabilization of soil 2.2.1.2 STABILIZATION BY COMPACTION This is the process whereby soil particles are constrained to pack more closely together through a reduction in the amount of air contained in the soil mass. By compacting under controlled conditions, air voids in well graded soils can almost be eliminated. Compaction is measured quantitatively in terms of the dry density of soil, which is the mass of solids per unit volume of soil in bulk. The moisture content of the soil is the mass of water it contains expressed as a percentage of the mass of the dry soil. The increase in the dry density of the soil produced by compaction depends mainly on the moisture content of the soil and the amount of compaction applied. (PHILIP SHERWOOD, 1993). 2.2.1.3 SOIL STABILIZATION TO CONTROL SHRINK SWELL Many clay soils (plastic soils) undergo extensive volumetric changes when subjected to fluctuating moisture contents. These volumetric changes if not controlled can lead to movements in structures and impose loads which can cause premature failure. The plasticity of soils has historically been quantified by the plasticity index, as determined by ASTM D 4318. Typically specifications limit the plasticity index of a soil to no more than 10-12 to ensure a stable material. In general terms, the higher the plasticity index, the higher the potential to shrink or swell as the soil undergoes moisture content fluctuations. Historically, plastic soils have been treated with quick lime (CaO) or hydrated lime [Ca(OH)2] to lower their plasticity. The lime 15 chemically reacts with the soil particles, effectively changing the soil grains from clay size (less than 0.002 mm) to silt size (0.05 to 0.002 mm). The determination of the plasticity index is geared towards measuring this chemical change in the soil. Therefore, the determination of the plasticity limits is inappropriate when evaluating the effect of quarry dust on the shrink-swell characteristics of a soil. 2.2.1.4 SOIL STABILIZATION TO REDUCE WATER CONTENT Soils must be compacted to their maximum practical density to provide a firm base for overlying structures. For soils to be compacted the moisture content must be controlled because of the relationship between and moisture content. If the soil to be compacted is either too wet or too dry, the moisture content must be adjusted to near optimum to achieve maximum density. If a soil is too dry, moisture is simply added. If a soil is too wet, the moisture content of the soil must be lowered of sub grade stability to expedite construction. 2.3 QUARRY DUST 2.3.1 PRODUCTION Quarry dust is produced from the full range of quarrying activities including: Extraction - overburden removal, drilling and blasting, loading and hauling Rock preparation - such as pre-screening and primary crushing and screening Further processing- secondary, screening and treatment Figure 5 Typical Quarry Quarry dust comprises material less than (about) 6 mm generated from any of these activities. They may be used as specific products (for example, as fine aggregate below 4 mm) or within 16 other aggregate products (for example, as part of the overall grading for a Type 1 sub base). Quarry dust (that is material less than 6 mm) are an essential part of many aggregate products and are intentionally produced by quarrying activities in order to provide the required product grindings. The amount of dust produced during blasting is estimated to be as high as 20% (The University of Leeds, 2007c) Figure 6 Typical Quarry Dust 2.3.2 QUARRY DUST CHARACTERISTICS Different quarries, or activities within the same quarry, may generate a range of quarry dust in relation to their particle size and composition. For instance, dusts produced from primary screening may have higher or lower clay content than those produced through tertiary crushing and screening. Quarry dust is composed of the same mineral substances as the soil and solid rock from which they are derived, even though changes to their physical and chemical characteristics may have occurred. Quarry dust by their nature, are usually inert or non-hazardous. Disaggregation, mixing and moving to different locations, exposure to atmospheric conditions and to surface or groundwater, as well as segregation and the increase of surface area due to particle size reduction, may cause physical and chemical transformations with detrimental effects to the environment (BGS, 2003). Quarry dust are considered more consistent materials in relation to their composition and particle size, also over time (temporal variability), they are commonly inert or non-hazardous which means that their impact to the environment and human health is very low, and they could provide some degree of security to the end user in terms of stable material supply. Commonly, the decision making criteria upon which the suitability of quarry dust is determined, are based on technical specifications and standards or on characterization procedures developed by end users, such as construction product manufacturers. Therefore, it is end users that define whether quarry dusts comprise a valuable material. Parameters such as rock type, extraction 17 technique and processing route, affect the generation of quarry dust as well as their end properties, (for example, composition, particle size and shape). 2.3.3 EFFECTS OF QUARRY DUST Environmental protection and social responsibility is of vital importance to the quarrying sector to reduce any adverse consequences (for example, in health and safety) and costs associated with the production of quarry dust (for example, storage, dealing with arising transport, and handling). The generation of quarry fines may cause adverse impacts on the environment (such as the local air, land, water, flora and fauna) and human health, and the mitigation of potential impacts is mandatory. Commonly, various dust control practices (conventional or alternative) are employed to minimize the impact of dust generated by quarry activities (Petavratzi et al, 2005; Petavratzi, 2006; EIPPCB, 2006). Health issues and the protection of fauna and flora are addressed through the management and protection of air quality.The utilization of quarry dust is seen as a way to minimize the accumulation of unwanted material and at the same time to maximize resource use and efficiency. 2.3.4 UTILIZATION APPLICATIONS Various utilization prospects exist for quarry fines, which can broadly be classified into unbound and bound applications. Both categories of end use may require some degree of processing of the quarry fines to be undertaken in order to comply with technical specifications. End applications may be of high or low value, or may require a small or a large volume of quarry fines. These uses include: Soil mineralization, compost, artificial soils and remediation. Site restoration and landscaping. Road pavements Embankment construction. Landfill capping. Manufactured sand (sand replacement in concrete) 2.3.5 OBSTACLES TO UTILIZATION Quarry dusts can be suitable materials for a variety of end applications; however, currently their utilization is not widespread to the level it would have been expected mainly due to reasons related to the geographical position of quarries. Very often quarries operate in remote location from potential end users and the cost of material to them includes high transport costs, which discourages their use. There are occasions where producers of aggregates are not aware of 18 potential utilization routes for their quarry fines in the local area, and these materials remain unused. Another major obstacle to utilization is the limited knowledge of exact quantities of quarry fines. It is recommended that figures on quantities of fines produced, marketed and stockpiled should be calculated in order to properly evaluate the quantities of quarry fines currently available, and information that present the geographical distribution of quarry fines, should be compiled to enable the identification of potential end markets. Some of the barriers to utilization are related to the location of quarry fines, the limited awareness of potential markets by aggregate producers, the limited knowledge about quarry dusts arising and their characteristics, and the absence of fully developed fit for use specifications for a wide range of end products. Often quarry fines require some degree of processing before they can be used, which may increase their cost and at the same time requires suitable infrastructure and equipment to become readily available. CHAPTER THREE 3.0METHODOLOGY 3.1 PREPARATION OF MATERIALS The quarry dust was sampled from Kitengela. The parent rock of the dust was established to be granite rock. The lateritic gravel was also sourced from Kitengela. This was obtained at a depth of two meters below the ground surface. The sample was a disturbed sample. Ordinary Portland cement class 32.5 was also used as a stabilizer for comparison purposes. The materials were blended in the following ratios as tabulated. STABILIZED MATERIAL LATERITIC GRAVEL LATERITIC GRAVEL LATERITIC GRAVEL LATERITIC GRAVEL LATERITIC GRAVEL STABILIZER PERCENTAGE OF STABILIZER NONE QUARRY DUST QUARRY DUST QUARRY DUST QUARRY DUST 0 5 10 15 20 LATERITIC GRAVEL LATERITIC GRAVEL CEMENT CEMENT 0.5 2.5 19 The tests described below were all conducted for the tabulated materials. 3.2 PRELIMINARY TESTS 3.2.1 COMPACTION SIGNIFICANCE OF THE TEST The compaction test is used to aid in guiding the field compaction of soil so as to develop the best engineering properties of material. This test is primarily used to determine the MDD and OMC values of the material. High densities improve the shear strength, elastic modulus and the permeability of the material decreases. To achieve the high densities ,the material is compacted at OMC. The standard moisture test ASTM D 698; AASHTO T99 as conducted in the laboratory uses a constant compactive effort. This is used to simulate the compaction in the field. Greater compaction effort will result to an increase in density. However exessive compaction will result to rigid layer which would start to crack. Also the material would become more plastic with excessive compaction hence it would start to shear. Basing on this ,the compaction test would show the best field compaction required which should range from 93% to 105% of the MDD depending on the layer. APPARATUS A metal mould with a detachable base plate and removable collar. A metal hammer weighing 4.5kg with sleeve to control the specified drop of 30.5cm. A 19mm BS sieve and metal trays. A balance, hand tools and straight edge A sample container Oven 20 Moisture content dishes Measuring cylinder and water. PROCEDURE As per AASHTO T180 and BS 1924: Part 2:1990 Figure 7 Equipment for standard compaction test 3.2.2 CALIFORNIA BEARING RATIO. SPECIMEN PREPARATION 21 The lateritic gravel was air dried and the specified percentage of dosage was added to it. The amount of dosage to be added was calculated in terms of percentage of the dry weight of the gravel. The specified sample was crushed after the required duration of curing and soaking elapsed. The crushed sample was then air dried, crushed and sampled for the atterbergs limit test and particle size distribution. SIGNIFICANCE OF THE TEST The CBR value is used to classify sub grade materials into different categories i.e. S1 up to S6.The classes increases as the CBR value increases. This is used in determining the thickness of the sub base and the base layers hence the CBR value is very vital in the design of pavements. Material with high CBR value is desirable. The CBR test is also used to establish how suitable a material is to be used in construction of base or sub base layers. Since the CBR value gives the load bearing capacity of a material, it is hence used to indicate the suitability of the material in layers construction. APPARATUS CBR machine A cylindrical metal mould with detachable base plate, top plate and collar. Spacer Rammer Surcharge weights Gauges PROCEDURE As per ASTM designation, D, 1883 specifications. 22 Figure 8 CBR loading press 3.2.3 PARTICLE SIZE ANALYSIS OF SOILS Sieve analysis (wet sieving followed by dry sieving) SIGNIFICANCE OF TEST The mechanics of the analysis of soil is the determination of percent of individual grain sizes present in the sample. The results of the tests are of the most value when used for classification purposes. Quite often it will be found that the lager the grain size the better the engineering properties. In addition the detrimental capillarity and frost damage are not a problem with course 23 materials, whereas they can be very dangerous with the fine grained silts and clay. Highway specifications for sub-base and base materials also use the grain size analysis for quality measurements. The results of the gradation tests are used to determine the size, percent of course or fines that are needed for a dense impermeable material. This will hence be achieved by mechanical stabilization. On occasion, the degree of permeability is estimated on the basis of grain size. The layered grained soils will readily permit the flow of water than fined grained soils. APPARATUS Wet/dry sieving Set of sieves A balance accurate to 0.1 grams Trays Oven PROCEDURE As per BS 1377 specifications. 24 Figure 9 Sieve analysis 3.2.4 ATTERBERGS LIMITS Liquid limit: AASHTO designation: T89 Plastic limit: AASHTO designation; T90 Plasticity index: AASHTO designation: T90 Shrinkage limit: AASHTO Plasticity modulus : Plasticity index x percentage passing sieve number 36 SIGNIFICANCE OF THE TEST The atterbergs limits test consists of liquid limit plastic limit and a value frequently used in conjunction with these limits is the plasticity index. The engineering properties of soil vary with the amount of water present. The results of the atterbergs tests are used to differentiate between 25 various states of the soil at different moisture contents. The liquid limit is the moisture at which the soil changes from plastic state to liquid. The plastic limit is the border between plastic and semi-solid. The plastic index is the arithmetic difference between the liquid limit and plastic limits. This can also be obtained by multiplying linear shrinkage and a constant value of 2.13 Low plasticity index indicates a granular soil with little or no cohesion. The atterbergs limits in the construction of pavements are very vital in that it indicates the shrinkage of the material. A material having high plasticity index is not suitable in pavement construction since it will suffer excessive shrinkage in dry conditions and excessive expansion in wet conditions. The effect of constructing on such material would be cracks on the pavement, settlement of the pavement and ratting of the road surface. Another important parameter to consider is the plasticity modulus. This is a product of the plasticity index and the of fines passing sieve number 36 or 425micr meters.A lower plasticity modulus is desirable since it indicates that the material has got lower amount of plastic fines and lower plasticity index. APPARATUS Flat glass plate Cone penetrometer Two spatulas Cone cap A wash bottle Moisture content dishes PROCEDURE. Various methods are used in the determination of the atterbergs limits but in this experiment the Cone penetrometer approach was used. 26 Figure 10 Equipment for Atterberg Limits test equipment 27 CHAPTER FOUR 4.0 RESULTS AND ANALYSIS 4.1 COMPACTION TEST 28 Dry Density / Optimum Moisture Content Relationship BS 1377: part 4: 1990 SOURCE KITENGELA Description: NEAT GRAVEL Date Tested: Method of Compaction: T180 7/1/2015 Date Sampled: 5/1/2015 Sample No: PR001 Total mass of sample kg 4.0 Moisture Addition (cc) 500 600 700 800 900 Tin No. Wgt of Wet Soil + Tin (g) Wgt of Dry Soil + Tin (g) Wgt of Water (g) Wgt of Tin (g) Wgt of Dry Soil (g) Moisture Content (%) Average moisture content (%) 181 129.7 119.3 10.4 76.2 43.1 24.0 24.0 53 148.5 135.6 12.9 86.4 49.2 26.2 26.2 100 141.9 126.9 15.0 75.1 51.8 28.9 28.9 65 167.0 144.5 22.5 72.4 72.1 31.2 31.2 65 156.9 136.3 20.6 75.7 60.6 34.0 34.0 Mass of Mould/ Base/ Soil (g) Mass of Mould + Base (g) A Mass of Compacted Soil (g) Volume of Mould (m 3) Bulk Density (Kg/m3) Moisture Content (%) Dry Density (kg/m 3) 5535 4115 1420 0.001 1485 24.0 1198 5700 4115 1585 0.001 1658 26.2 1314 5825 4115 1710 0.001 1789 28.9 1387 5860 4115 1745 0.001 1825 31.2 1391 5845 4115 1730 0.001 1810 34.0 1351 M ax Dry Density = 1390 kg/m3 Optimum Moisture % = pmc 0.0 30.4 1450 Dry Density (g / cm 3) 1400 1350 1300 1250 1200 1150 1100 20.0 25.0 30.0 Moisture Content (%) 35.0 29 Dry Density / Optimum Moisture Content Relationship BS 1377: part 4: 1990 SOURCE KITENGELA Description: 0.5% CEMENT STABILIZED GRAVEL Date Tested: Method of Compaction: T180 10/1/2015 Date Sampled: 5/1/2015 Sample No: PR002 Total mass of sample kg 4.0 Moisture Addition (cc) 500 600 700 800 Tin No. Wgt of Wet Soil + Tin (g) Wgt of Dry Soil + Tin (g) Wgt of Water (g) Wgt of Tin (g) Wgt of Dry Soil (g) Moisture Content (%) Average moisture content (%) 126 289.3 245.0 44.3 101.9 143.1 31.0 31.0 123 287.5 241.5 46.0 106.8 134.7 34.1 34.1 145 278.6 230.3 48.3 101.2 129.1 37.4 37.4 68 252.9 205.8 47.1 88.4 117.4 40.1 40.1 Mass of Mould/ Base/ Soil (g) Mass of Mould + Base (g) A Mass of Compacted Soil (g) Volume of Mould (m 3) Bulk Density (Kg/m3) Moisture Content (%) Dry Density (kg/m 3) 5725 4115 1610 0.001 1684 31.0 1286 5865 4115 1750 0.001 1831 34.1 1365 5880 4115 1765 0.001 1846 37.4 1344 5820 4115 1705 0.001 1783 40.1 1273 M ax Dry Density = 1367 kg/m3 pmc 0.0 Optimum Moisture % = 35.0 1400 Dry Density (g / cm 3) 1375 1350 1325 1300 1275 1250 1225 1200 25.0 27.0 29.0 31.0 33.0 35.0 37.0 39.0 Moisture Content (%) 41.0 43.0 45.0 30 Dry Density / Optimum Moisture Content Relationship BS 1377: part 4: 1990 SOURCE KITENGELA Description: 5% QUARRY DUST STABILIZED GRAVEL Date Tested: Method of Compaction: T180 10/1/2015 Date Sampled: 5/1/2015 Sample No: PR004 Total mass of sample kg 4.0 Moisture Addition (cc) 500 600 700 800 900 Tin No. Wgt of Wet Soil + Tin (g) Wgt of Dry Soil + Tin (g) Wgt of Water (g) Wgt of Tin (g) Wgt of Dry Soil (g) Moisture Content (%) Average moisture content (%) 50 237.1 208.0 29.1 88.6 119.4 24.4 24.4 201 197.6 170.9 26.7 74.8 96.1 27.8 27.8 95 233.7 201.3 32.4 98.3 103.0 31.5 31.5 227 200.5 169.1 31.4 76.0 93.1 33.7 33.7 216 210.3 174.4 35.9 75.6 98.8 36.3 36.3 Mass of Mould/ Base/ Soil (g) Mass of Mould + Base (g) A Mass of Compacted Soil (g) Volume of Mould (m 3) Bulk Density (Kg/m3) Moisture Content (%) Dry Density (kg/m 3) 5700 4115 1585 0.001 1658 24.4 1333 5800 4115 1685 0.001 1763 27.8 1379 5895 4115 1780 0.001 1862 31.5 1416 5855 4115 1740 0.001 1820 33.7 1361 5810 4115 1695 0.001 1773 36.3 1300 M ax Dry Density = 1420 kg/m3 Optimum Moisture % = pmc 0.0 30.6 1450 Dry Density (g / cm 3) 1425 1400 1375 1350 1325 1300 1275 1250 1225 1200 20.0 22.0 24.0 26.0 28.0 30.0 32.0 34.0 Moisture Content (%) 36.0 38.0 40.0 31 Dry Density / Optimum Moisture Content Relationship BS 1377: part 4: 1990 Date Sampled: 5/1/2015 SOURCE KITENGELA Sample No: PR005 Description: 10% QUARRY DUST STABILIZED GRAVEL Layer: Date Tested: Method of Compaction: T180 10/1/2015 Total mass of sample kg 4.0 Moisture Addition (cc) 500 600 700 800 Tin No. Wgt of Wet Soil + Tin (g) Wgt of Dry Soil + Tin (g) Wgt of Water (g) Wgt of Tin (g) Wgt of Dry Soil (g) Moisture Content (%) Average moisture content (%) 58 258.4 222.8 35.6 89.6 133.2 26.7 26.7 62 239.6 205.7 33.9 90.4 115.3 29.4 29.4 51 205.6 176.4 29.2 90.4 86.0 34.0 34.0 198 241.3 199.2 42.1 81.2 118.0 35.7 35.7 Mass of Mould/ Base/ Soil (g) Mass of Mould + Base (g) A Mass of Compacted Soil (g) Volume of Mould (m 3) Bulk Density (Kg/m3) Moisture Content (%) Dry Density (kg/m 3) 5800 4115 1685 0.001 1763 26.7 1391 5915 4115 1800 0.001 1883 29.4 1455 5900 4115 1785 0.001 1867 34.0 1394 5850 4115 1735 0.001 1815 35.7 1338 M ax Dry Density = 1455 kg/m3 Optimum Moisture % = pmc 0.0 30.0 1500 1475 Dry Density (g / cm 3) 1450 1425 1400 1375 1350 1325 1300 1275 1250 1225 1200 25.0 30.0 35.0 Moisture Content (%) 40.0 32 Dry Density / Optimum Moisture Content Relationship BS 1377: part 4: 1990 SOURCE KITENGELA Description: 15% QUARRY DUST STABILIZED GRAVEL Date Tested: Method of Compaction: T180 10/1/2015 Date Sampled: 5/1/2015 Sample No: PR006 Total mass of sample kg 4.0 Moisture Addition (cc) 500 600 700 800 Tin No. Wgt of Wet Soil + Tin (g) Wgt of Dry Soil + Tin (g) Wgt of Water (g) Wgt of Tin (g) Wgt of Dry Soil (g) Moisture Content (%) Average moisture content (%) 106 249.6 224.2 25.4 106.4 117.8 21.6 21.6 222 227.3 196.6 30.7 75.6 121.0 25.4 25.4 195 213.8 183.6 30.2 75.0 108.6 27.8 27.8 184 205.2 173.3 31.9 75.3 98.0 32.6 32.6 Mass of Mould/ Base/ Soil (g) Mass of Mould + Base (g) A Mass of Compacted Soil (g) Volume of Mould (m 3) Bulk Density (Kg/m3) Moisture Content (%) Dry Density (kg/m 3) 5800 4115 1685 0.001 1763 21.6 1450 5905 4115 1790 0.001 1872 25.4 1493 5950 4115 1835 0.001 1919 27.8 1502 5870 4115 1755 0.001 1836 32.6 1385 M ax Dry Density = 1502 kg/m3 Optimum Moisture % = pmc 0.0 27.4 1550 Dry Density (g / cm 3) 1525 1500 1475 1450 1425 1400 1375 1350 1325 1300 20.0 25.0 30.0 Moisture Content (%) 35.0 33 Dry Density / Optimum Moisture Content Relationship BS 1377: part 4: 1990 SOURCE KITENGELA Description: 20% QUARRY DUST STABILIZED GRAVEL Date Tested: Method of Compaction: T180 10/1/2015 Date Sampled: 5/1/2015 Sample No: PR007 Total mass of sample kg 4.0 Moisture Addition (cc) 500 600 700 800 Tin No. Wgt of Wet Soil + Tin (g) Wgt of Dry Soil + Tin (g) Wgt of Water (g) Wgt of Tin (g) Wgt of Dry Soil (g) Moisture Content (%) Average moisture content (%) 181 225.8 199.0 26.8 76.2 122.8 21.8 21.8 53 284.4 244.9 39.5 87.8 157.1 25.1 25.1 100 232.3 206.0 26.3 108.3 97.7 26.9 26.9 65 251.6 212.6 39.0 86.3 126.3 30.9 30.9 Mass of Mould/ Base/ Soil (g) Mass of Mould + Base (g) A Mass of Compacted Soil (g) Volume of Mould (m 3) Bulk Density (Kg/m3) Moisture Content (%) Dry Density (kg/m 3) 5875 4115 1760 0.001 1841 21.8 1511 5960 4115 1845 0.001 1930 25.1 1542 5975 4115 1860 0.001 1946 26.9 1533 5920 4115 1805 0.001 1888 30.9 1443 M ax Dry Density = 1542 kg/m3 Optimum Moisture % = pmc 0.0 25.1 1550 Dry Density (g / cm 3) 1525 1500 1475 1450 1425 1400 20.0 25.0 30.0 Moisture Content (%) 35.0 34 MDD AND OMC SUMMARY SAMPLE NUMBER PR 001 PR 002 PR 003 PR 004 PR 005 PR 006 PR 007 MDD Kg/m3 DESCRIPTION NEAT GRAVEL 0.5% CEMENT STABILIZED GRAVEL 2.5% CEMENT STABILIZED GRAVEL 5% QUARRY DUST STABILIZED GRAVEL 10% QUARRY DUST STABILIZED GRAVEL 15% QUARRY DUST STABILIZED GRAVEL 20% QUARRY DUST STABILIZED GRAVEL 1390 1367 1360 1420 1455 1502 1542 OMC % 30.4 35.0 36.2 30.6 30.0 27.4 25.1 MDD COMPARISON 1600 1542 1550 1502 MDD Kg/m3 1500 1455 1450 1400 1420 1390 1367 1360 1350 1300 1250 NEAT GRAVEL 0.5% 2.5% 5% QUARRY 10% 15% 20% CEMENT CEMENT DUST QUARRY QUARRY QUARRY STABILIZED STABILIZED STABILIZED DUST DUST DUST GRAVEL GRAVEL GRAVEL STABILIZED STABILIZED STABILIZED GRAVEL GRAVEL GRAVEL MATERIAL DESCRIPTION 35 OMC COMPARISON 40 36.2 35 30 35.0 30.4 30.6 30.0 27.4 25.1 OMC % 25 20 15 10 5 0 NEAT GRAVEL 0.5% CEMENT 2.5% CEMENT 5% QUARRY 10% QUARRY 15% QUARRY 20% QUARRY STABILIZED STABILIZED DUST DUST DUST DUST GRAVEL GRAVEL STABILIZED STABILIZED STABILIZED STABILIZED GRAVEL GRAVEL GRAVEL GRAVEL MATERIAL DESCRIPTION 36 4.2 CBR TEST 37 CARLIFORNIA BEARING RATIO TEST BSC CIVIL ENGINEEING FIFTH YEAR PROJECT MATERIAL DESCRIPTION: NEAT GRAVEL SAMPLE NUMBER DATE SAMPLED PEN PR001 10/2/2015 TOP 0 50 100 150 200 250 300 350 400 450 500 DATE TESTED BOT 0 60 100 130 170 205 230 265 300 335 351 PEN x FCT 0 61 104 152 210 260 300 325 345 355 358 14-2-2015 TOP LOAD BOT LOAD 0.0 0.6 1.3 1.9 2.5 3.2 3.8 4.4 5.1 5.7 6.4 0.0 0.8 1.4 2.0 2.8 3.4 4.0 4.3 4.5 4.7 4.7 0.0 0.8 1.3 1.7 2.2 2.7 3.0 3.5 4.0 4.4 4.6 5.0 4.5 4.0 3.5 LOAD 3.0 2.5 2.0 TOP BOTTOM Log. (BOTTOM) 1.5 1.0 0.5 0.0 0.0 1.0 2.0 3.0 4.0 5.0 6.0 7.0 PENETRATION PEN 2.5 5.0 TOP READING BOT READING 2.2 3.9 2.8 4.5 TOP CBR BOT CBR CBR VALUE 16.62 29.46 21.15 33.99 34% 38 CARLIFORNIA BEARING RATIO TEST BSC CIVIL ENGINEEING FIFTH YEAR PROJECT MATERIAL DESCRIPTION: 0.5% CEMENT STABILIZED GRAVEL SAMPLE NUMBER DATE SAMPLED PEN PR002 10/2/2015 TOP 0 50 100 150 200 250 300 350 400 450 500 DATE TESTED BOT 0 55 83 115 142 165 198 232 250 266 282 PEN x FCT 0 85 188 266 302 350 372 382 385 24-2-2015 TOP LOAD BOT LOAD 0.0 0.6 1.3 1.9 2.5 3.2 3.8 4.4 5.1 5.7 6.4 0.0 1.1 2.5 3.5 4.0 4.6 4.9 5.0 5.1 0.0 0.7 1.1 1.5 1.9 2.2 2.6 3.1 3.3 3.5 3.7 6.0 5.0 LOAD 4.0 3.0 TOP BOTTOM Log. (BOTTOM) 2.0 1.0 0.0 0.0 1.0 2.0 3.0 4.0 5.0 6.0 7.0 PENETRATION PEN 2.5 5.0 TOP READING BOT READING 1.8 3.3 3.8 5.1 TOP CBR BOT CBR CBR VALUE 13.60 24.92 28.70 38.52 38.5% 39 CARLIFORNIA BEARING RATIO TEST BSC CIVIL ENGINEEING FIFTH YEAR PROJECT MATERIAL DESCRIPTION: 2.5% CEMENT STABILIZED GRAVEL SAMPLE NUMBER DATE SAMPLED PEN PR003 10/2/2015 TOP 0 50 100 150 200 250 300 350 400 450 500 DATE TESTED BOT 0 64 89 140 205 260 316 384 462 532 537 PEN x FCT 0 105 252 380 490 592 655 730 785 840 870 24-2-2015 TOP LOAD BOT LOAD 0.0 0.6 1.3 1.9 2.5 3.2 3.8 4.4 5.1 5.7 6.4 0.0 1.4 3.3 5.0 6.5 7.8 8.6 9.6 10.3 11.1 11.5 0.0 0.8 1.2 1.8 2.7 3.4 4.2 5.1 6.1 7.0 7.1 14.0 12.0 10.0 LOAD 8.0 6.0 TOP BOTTOM Log. (BOTTOM) 4.0 2.0 0.0 0.0 1.0 2.0 3.0 4.0 5.0 6.0 7.0 PENETRATION PEN 2.5 5.0 TOP READING BOT READING 2.6 6.0 6.6 10.2 TOP CBR BOT CBR CBR VALUE 19.64 45.32 49.85 77.04 77.0% 40 CARLIFORNIA BEARING RATIO TEST BSC CIVIL ENGINEEING FIFTH YEAR PROJECT MATERIAL DESCRIPTION: 5% QUARRY DUST STABILIZED GRAVEL SAMPLE NUMBER DATE SAMPLED PEN PR004 10/2/2015 TOP 0 50 100 150 200 250 300 350 400 450 500 DATE TESTED BOT 0 90 206 310 400 473 510 PEN x FCT 0 115 231 340 412 520 590 610 14-2-2015 TOP LOAD BOT LOAD 0.0 0.6 1.3 1.9 2.5 3.2 3.8 4.4 0.0 1.2 2.7 4.1 5.3 6.2 6.7 0.0 1.5 3.0 4.5 5.4 6.9 7.8 8.0 9.0 8.0 7.0 6.0 LOAD 5.0 4.0 TOP BOTTOM Log. (BOTTOM) 3.0 2.0 1.0 0.0 0.0 1.0 2.0 3.0 4.0 5.0 PENETRATION PEN 2.5 5.0 TOP READING BOT READING 5.2 5.4 TOP CBR BOT CBR 39.27 40.79 CBR VALUE 41% 41 CARLIFORNIA BEARING RATIO TEST BSC CIVIL ENGINEEING FIFTH YEAR PROJECT MATERIAL DESCRIPTION: 10% QUARRY DUST STABILIZED GRAVEL SAMPLE NUMBER DATE SAMPLED PEN PR005 10/2/2015 TOP 0 50 100 150 200 250 300 350 400 450 500 DATE TESTED BOT 0 90 155 210 260 300 340 383 402 430 440 PEN x FCT 0 80 203 292 345 390 420 440 452 462 465 24-2-2015 TOP LOAD BOT LOAD 0.0 0.6 1.3 1.9 2.5 3.2 3.8 4.4 5.1 5.7 6.4 0.0 1.1 2.7 3.8 4.5 5.1 5.5 5.8 6.0 6.1 6.1 0.0 1.2 2.0 2.8 3.4 4.0 4.5 5.0 5.3 5.7 5.8 7.0 6.0 5.0 LOAD 4.0 3.0 TOP BOTTOM Log. (BOTTOM) 2.0 1.0 0.0 0.0 1.0 2.0 3.0 4.0 5.0 6.0 7.0 PENETRATION PEN 2.5 5.0 TOP READING BOT READING 3.6 5.2 4.5 5.9 TOP CBR BOT CBR CBR VALUE 27.19 39.27 33.99 44.56 44.6% 42 CARLIFORNIA BEARING RATIO TEST BSC CIVIL ENGINEEING FIFTH YEAR PROJECT MATERIAL DESCRIPTION: 15% QUARRY DUST STABILIZED GRAVEL SAMPLE NUMBER DATE SAMPLED PEN PR006 10/2/2015 TOP 0 50 100 150 200 250 300 350 400 450 500 DATE TESTED BOT 0 130 210 275 340 372 404 452 490 530 562 PEN x FCT 0 132 350 445 550 622 650 24-2-2015 TOP LOAD BOT LOAD 0.0 0.6 1.3 1.9 2.5 3.2 3.8 4.4 5.1 5.7 6.4 0.0 1.7 4.6 5.9 7.2 8.2 8.6 0.0 1.7 2.8 3.6 4.5 4.9 5.3 6.0 6.5 7.0 7.4 9.0 8.0 7.0 6.0 LOAD 5.0 4.0 TOP BOTTOM Log. (BOTTOM) 3.0 2.0 1.0 0.0 0.0 1.0 2.0 3.0 4.0 5.0 6.0 7.0 PENETRATION PEN 2.5 5.0 TOP READING BOT READING 4.4 6.4 7.2 TOP CBR BOT CBR CBR VALUE 33.23 48.34 54.38 0.00 54.4% 43 CARLIFORNIA BEARING RATIO TEST BSC CIVIL ENGINEEING FIFTH YEAR PROJECT MATERIAL DESCRIPTION: 20% QUARRY DUST STABILIZED GRAVEL SAMPLE NUMBER DATE SAMPLED PEN PR007 10/2/2015 TOP 0 50 100 150 200 250 300 350 400 450 500 DATE TESTED BOT 0 68 190 380 435 515 580 655 695 745 750 PEN x FCT 0 64 122 210 330 440 555 640 690 730 747 24-2-2015 TOP LOAD BOT LOAD 0.0 0.6 1.3 1.9 2.5 3.2 3.8 4.4 5.1 5.7 6.4 0.0 0.8 1.6 2.8 4.3 5.8 7.3 8.4 9.1 9.6 9.8 0.0 0.9 2.5 5.0 5.7 6.8 7.6 8.6 9.2 9.8 9.9 12.0 10.0 LOAD 8.0 6.0 TOP BOTTOM Log. (BOTTOM) 4.0 2.0 0.0 0.0 1.0 2.0 3.0 4.0 5.0 6.0 7.0 PENETRATION PEN 2.5 5.0 TOP READING BOT READING 5.6 9.0 4.4 9.0 TOP CBR BOT CBR CBR VALUE 42.30 67.98 33.23 67.98 68.0% 44 CBR SUMMARY SAMPLE NUMBER PR 001 PR 002 PR 003 PR 004 PR 005 PR 006 PR 007 DESCRIPTION CBR % NEAT GRAVEL 0.5% CEMENT STABILIZED GRAVEL 2.5% CEMENT STABILIZED GRAVEL 5% QUARRY DUST STABILIZED GRAVEL 10% QUARRY DUST STABILIZED GRAVEL 15% QUARRY DUST STABILIZED GRAVEL 20% QUARRY DUST STABILIZED GRAVEL 34.0 38.5 77.0 41.0 44.6 54.4 68.0 CBR COMPARISON 90.0 77.0 80.0 68.0 70.0 CBR % 60.0 54.4 50.0 40.0 38.5 41.0 44.6 34.0 30.0 20.0 10.0 0.0 NEAT GRAVEL 0.5% 2.5% 5% QUARRY 10% 15% 20% CEMENT CEMENT DUST QUARRY QUARRY QUARRY STABILIZED STABILIZED STABILIZED DUST DUST DUST GRAVEL GRAVEL GRAVEL STABILIZED STABILIZED STABILIZED GRAVEL GRAVEL GRAVEL MATERIAL DESCRIPTION 45 ANALYSIS OF CBR FOR THE MATERIAL The CBR test measures the bearing strength of a material. The materials tested gave the results as tabulated in the summary for CBR. The CBR of neat gravel gave a CBR value of 34.0%. This is lower than the minimum required CBR for material to be used for Sub base and base layers of 35% and 60% respectively. However this material is good enough for sub grade layer. It can be classified as class S6 for subgrade material. These are materials with CBR of mean greater than 30%. This material is suitable enough to be used as subgrade layers in Class A roads, airport runways and railways due to its ability to withstand high imposed loads at the subgrade level. Stabilization with 0.5 % cement, 5% quarry dust,10% quarry dust and 15% quarry dust improves the CBR values. However with these percentages of stabilizers, the material does not still qualify to be used as sub base layer or base layer material since the minimum required CBR for stabilized sub base and base material is 60% and 100% respectively. Higher CBR values are achieved when stabilization is done using quarry dust as compared to cement stabilization. The highest values of CBR are achieved when stabilization is done using 20% quarry dust and 2.5 % cement. The CBR values achieved are 68% and 77 % respectively. With this amount of stabilizer the material is sufficient enough to be used as sub base material since the CBR value is more than 60%, which is the minimum required CBR for stabilized sub base material. The stabilization of this material to a value of 100% CBR would require high dosage of stabilizer. It is hence not recommended for use in base construction since it would be uneconomical to stabilize this material to base quality. 46 4.3 ATTERBERG LIMIT TEST 47 FIFTH YEAR PROJECT ATTERBERG LIMITS USING CONE PENETROMETER Lab Ref: Description: NEAT GRAVEL Date Tested: 28/2/2015 Stabilizer content %: Date Sampled: 26/2/2015 Sample No: Material Type: PR001 Source: NEAT GRAVEL KITENGELA (NEAT) Liquid limit Test No. Plastic limit 1 2 3 4 5 6 1 2 15.4 17.0 20.1 22.1 21 46 7 12 JJ 7F Mass of container and wet soil 61.0 67.1 74.9 82.3 15.4 15.4 Mass of container and dry soil 48.8 52.6 56.6 60.5 13.6 13.6 Mass of container 28.4 28.8 28.2 28.0 8.5 8.5 Mass of moisture 12.2 14.5 18.3 21.8 1.8 1.8 Mass of dry soil 20.4 23.8 28.4 32.5 5.1 5.1 Moisture content 59.8 60.9 64.4 67.1 35.3 35.3 Initial dial reading Final dial reading Cone penetration Container No. Average 68.0 LINEAR SHRINKAGE (J) 66.0 Moisture Content (%) 35.3 Length of Oven dry sample 127 mm Initial Length of sample 140 mm 13 mm % LS ═ 9.3 % PI = LS x 2.13 ═ 27.7 64.0 LS = 62.0 60.0 % Ret on 425µm sieve 58.0 15.0 20.0 Penetration y = 1.0979x +(mm) 42.585 25.0 LIQUID LIMIT % 64.4 PLASTIC LIMIT % 35.3 PLASTICITY INDEX 29.1 48 FIFTH YEAR PROJECT ATTERBERG LIMITS USING CONE PENETROMETER Lab Ref: Date Sampled: Description: 2/3/2015 Sample No: 0.5% CEMENT STABILIZED GRAVEL Date Tested: 2/3/2015 Stabilizer content %: 0.5% CEMENT Material Type: PR002 Source: STABILIZED GRAVEL Liquid limit Test No. KITENGELA Plastic limit 1 2 3 4 5 6 1 2 15.1 17.4 20.3 22.4 27 18 38 32 4R W Mass of container and wet soil 54.8 64.8 72.9 78.9 15.9 15.9 Mass of container and dry soil 45.6 52.0 55.9 59.1 14.0 13.9 Mass of container 27.3 28.7 27.6 28.6 8.0 7.9 Mass of moisture 9.2 12.8 17.0 19.8 1.9 2.0 Mass of dry soil 18.3 23.3 28.3 30.5 6.0 6.0 Moisture content 50.3 54.9 60.1 64.9 31.7 33.3 Initial dial reading Final dial reading Cone penetration Container No. Moisture Content (%) Average 68.0 66.0 64.0 62.0 60.0 58.0 56.0 54.0 52.0 50.0 48.0 46.0 44.0 42.0 40.0 15.0 32.5 LINEAR SHRINKAGE (J) Length of Oven dry sample 128.5 mm 140 mm 11.4 mm % LS ═ 8.1 % PI = LS x 2.13 ═ 24.3 Initial Length of sample LS = % Ret on 425µm sieve 20.0 Penetration (mm) y = 1.9731x + 20.455 25.0 LIQUID LIMIT % 60.0 PLASTIC LIMIT % 31.8 PLASTICITY INDEX 28.2 49 FIFTH YEAR PROJECT ATTERBERG LIMITS USING CONE PENETROMETER Lab Ref: Date Sampled: Description: 26/2/2015 Sample No: 5% QUARRY DUST STABILIZED GRAVEL Material Type: Date Tested: 28/2/2015 Stabilizer content %: 5% QUARRY DUST PR004 Source: STABILIZED GRAVEL Liquid limit Test No. KITENGELA Plastic limit 1 2 3 4 5 6 1 2 15.6 17.6 20.3 22.3 2 24 38 1 MA O Mass of container and wet soil 52.4 58.6 67.5 76.9 17.0 17.0 Mass of container and dry soil 43.6 47.2 52.2 58.1 14.8 14.8 Mass of container 28.2 27.8 27.5 29.1 8.6 8.7 Mass of moisture 8.8 11.4 15.3 18.8 2.2 2.2 Mass of dry soil 15.4 19.4 24.7 29.0 6.2 6.1 Moisture content 57.1 58.8 61.9 64.8 35.5 36.1 Initial dial reading Final dial reading Cone penetration Container No. Average 66.0 LINEAR SHRINKAGE (J) Length of Oven dry sample 64.0 Moisture Content (%) 35.8 128.5 mm 140 mm 11.5 mm % LS ═ 8.2 % PI = LS x 2.13 ═ 24.5 Initial Length of sample 62.0 LS = 60.0 58.0 % Ret on 425µm sieve 56.0 15.0 20.0 Penetration (mm) 25.0 LIQUID LIMIT % 62.0 PLASTIC LIMIT % 35.8 PLASTICITY INDEX 26.2 y = 1.1513x + 38.852 50 FIFTH YEAR PROJECT ATTERBERG LIMITS USING CONE PENETROMETER Lab Ref: Date Sampled: Description: 26/2/2015 Sample No: 10% QUARRY DUST STABILIZED GRAVEL Material Type: Date Tested: 28/2/2015 Stabilizer content %: 10% QUARRY DUST PR005 Source: STABILIZED GRAVEL Liquid limit Test No. KITENGELA Plastic limit 1 2 3 4 5 6 1 2 15.3 17.3 20.0 22.2 32 13 11 41 4R W Mass of container and wet soil 65.8 72.4 79.9 86.3 16.2 16.3 Mass of container and dry soil 52.5 56.7 60.6 64.4 14.4 14.3 Mass of container 28.6 29.1 28.5 28.8 8.8 8.8 Mass of moisture 13.3 15.7 19.3 21.9 1.8 2.0 Mass of dry soil 23.9 27.6 32.1 35.6 5.6 5.5 Moisture content 55.6 56.9 60.1 61.5 32.1 36.4 Initial dial reading Final dial reading Cone penetration Container No. Average 62.0 LINEAR SHRINKAGE (J) Length of Oven dry sample Moisture Content (%) 34.3 128.5 mm 60.0 140 mm 11.2 mm % LS ═ 8.0 % PI = LS x 2.13 ═ 23.9 Initial Length of sample LS = 58.0 56.0 % Ret on 425µm sieve 54.0 15.0 20.0 y = 0.8969x + 41.772 Penetration (mm) 25.0 LIQUID LIMIT % 59.6 PLASTIC LIMIT % 34.3 PLASTICITY INDEX 25.3 51 FIFTH YEAR PROJECT ATTERBERG LIMITS USING CONE PENETROMETER Lab Ref: Date Sampled: Description: 28/2/2015 Sample No: 15% QUARRY DUST STABILIZED GRAVEL Material Type: Date Tested: 28/2/2015 Stabilizer content %: 15% QUARRY DUST PR006 Source: STABILIZED GRAVEL Liquid limit Test No. KITENGELA Plastic limit 1 2 3 4 5 6 1 2 15.5 17.3 20.0 22.5 26 27 6 35 AK BX Mass of container and wet soil 59.4 67.7 73.2 84.3 13.6 13.5 Mass of container and dry soil 49.2 53.6 57.6 63.8 12.2 12.2 Mass of container 29.3 27.3 29.3 29.3 8.0 7.9 Mass of moisture 10.2 14.1 15.6 20.5 1.4 1.3 Mass of dry soil 19.9 26.3 28.3 34.5 4.2 4.3 Moisture content 51.3 53.6 55.1 59.4 33.3 30.2 Initial dial reading Final dial reading Cone penetration Container No. Average 61.0 LINEAR SHRINKAGE (J) 59.0 Moisture Content (%) 31.8 Length of Oven dry sample 128.5 mm 57.0 140 mm 11.4 mm % LS ═ 8.1 % PI = LS x 2.13 ═ 24.3 Initial Length of sample 55.0 LS = 53.0 51.0 49.0 47.0 45.0 15.0 % Ret on 425µm sieve 20.0 Penetration (mm) y = 1.095x + 34.239 25.0 LIQUID LIMIT % 56.0 PLASTIC LIMIT % 31.8 PLASTICITY INDEX 24.2 52 FIFTH YEAR PROJECT ATTERBERG LIMITS USING CONE PENETROMETER Lab Ref: Date Sampled: Description: 28/2/2015 Sample No: 20% QUARRY DUST STABILIZED GRAVEL Material Type: Date Tested: 28/2/2015 Stabilizer content %: 20% QUARRY DUST PR007 Source: STABILIZED GRAVEL Liquid limit Test No. KITENGELA Plastic limit 1 2 3 4 5 6 1 2 15.5 17.6 20.2 22.8 31 48 30 10 A1 Q Mass of container and wet soil 56.3 63.9 74.6 81.2 16.5 16.6 Mass of container and dry soil 48.0 52.2 57.8 61.3 14.6 14.7 Mass of container 28.7 28.8 28.1 28.7 8.9 8.8 Mass of moisture 8.3 11.7 16.8 19.9 1.9 1.9 Mass of dry soil 19.3 23.4 29.7 32.6 5.7 5.9 Moisture content 43.0 50.0 56.6 61.0 33.3 32.2 Initial dial reading Final dial reading Cone penetration Container No. Average 64.0 32.8 LINEAR SHRINKAGE (J) 62.0 Moisture Content (%) 60.0 Length of Oven dry sample 128.5 mm 58.0 140 mm 11.2 mm % LS ═ 8.0 % PI = LS x 2.13 ═ 23.9 Initial Length of sample 56.0 54.0 LS = 52.0 50.0 48.0 46.0 44.0 % Ret on 425µm sieve 42.0 40.0 15.0 20.0 y = 2.4614x + 5.8246 Penetration (mm) 25.0 LIQUID LIMIT % 55.0 PLASTIC LIMIT % 32.8 PLASTICITY INDEX 22.2 53 4.4 PARTICLE SIZE DISTRIBUTION (GRADING) TEST 54 PARTICLE SIZE DISTRIBUTION-GRADING FIFTH YEAR PROJECT DATE SAMPLED 3/3/15 DATE TESTED 3/3/15 MATERIAL DISCRIPTION SAMPLE NUMBER WEIGHT BEFORE WASH WEIGHT AFTER WASH NEAT GRAVEL PR001 SIEVE SIZE UPPER LIMIT LOWER LIMIT 50 37.5 28 20 10 5 2 1 0.425 0.075 100 100 100 100 90 75 50 40 33 20 100 95 80 60 35 20 12 10 7 4 SOURCE KITENGELA SIEVE SIZE 50 28 20 10 5 2.36 1.18 0.6 0.425 0.3 0.15 0.075 less 0.075 wt retained 0 0 0 0 8.1 18.1 16.8 16.2 9.1 7.1 13.9 8 99.4 wt passing 100.6 100.6 100.6 100.6 92.5 74.4 57.6 41.4 32.3 25.2 11.3 3.3 200 100.6 % passing 100.00 100.00 100.00 100.00 91.95 73.96 57.26 41.15 32.11 25.05 11.23 3.28 GRADING ENVELOPE UPPER LIMIT 120 100 % PASSING 80 LOWER LIMIT 60 40 GRADING CURVE 20 0 0 10 20 30 40 50 60 SIEVE SIZE 55 PARTICLE SIZE DISTRIBUTION-GRADING FIFTH YEAR PROJECT DATE SAMPLED 3/3/15 DATE TESTED 3/3/15 MATERIAL DISCRIPTION SAMPLE NUMBER WEIGHT BEFORE WASH WEIGHT AFTER WASH 0.5% CEMENT STABILIZED GRAVEL PR002 SOURCE KITENGELA SIEVE SIZE 50 28 20 10 5 2.36 1.18 0.6 0.425 0.3 0.15 0.075 less 0.075 SIEVE SIZE UPPER LIMIT LOWER LIMIT 50 37.5 28 20 10 5 2 1 0.425 0.075 100 100 100 100 90 75 50 40 33 20 100 95 80 60 35 20 12 10 7 4 wt retained 0 0 0 15.3 11.5 13.7 12 10.7 5.8 5.9 10.8 4 109.3 wt passing 90.7 90.7 90.7 75.4 63.9 50.2 38.2 27.5 21.7 15.8 5 1 200 90.7 % passing 100.00 100.00 100.00 83.13 70.45 55.35 42.12 30.32 23.93 17.42 5.51 1.10 GRADING ENVELOPE UPPER LIMIT 120 100 % PASSING 80 LOWER LIMIT 60 40 GRADING CURVE 20 0 0 10 20 30 40 50 60 SIEVE SIZE 56 PARTICLE SIZE DISTRIBUTION-GRADING FIFTH YEAR PROJECT DATE SAMPLED 3/3/15 DATE TESTED 3/3/15 MATERIAL DISCRIPTION SAMPLE NUMBER WEIGHT BEFORE WASH WEIGHT AFTER WASH 2.5% CEMENT STABILIZED GRAVEL PR003 SOURCE KITENGELA SIEVE SIZE 50 28 20 10 5 2.36 1.18 0.6 0.425 0.3 0.15 0.075 less 0.075 SIEVE SIZE UPPER LIMIT LOWER LIMIT 50 37.5 28 20 10 5 2 1 0.425 0.075 100 100 100 100 90 75 50 40 33 20 100 95 80 60 35 20 12 10 7 4 wt retained 0 0 0 26 11 17.5 19.7 17.9 8.3 7.4 12.6 8.1 71.3 wt passing 128.7 128.7 128.7 102.7 91.7 74.2 54.5 36.6 28.3 20.9 8.3 0.2 200 128.7 % passing 100.00 100.00 100.00 79.80 71.25 57.65 42.35 28.44 21.99 16.24 6.45 0.16 GRADING ENVELOPE UPPER LIMIT 120 100 % PASSING 80 LOWER LIMIT 60 40 GRADING CURVE 20 0 0 10 20 30 40 50 60 SIEVE SIZE 57 PARTICLE SIZE DISTRIBUTION-GRADING FIFTH YEAR PROJECT DATE SAMPLED 3/3/15 DATE TESTED 3/3/15 MATERIAL DISCRIPTION SAMPLE NUMBER WEIGHT BEFORE WASH WEIGHT AFTER WASH 5% QUARY DUST STABILIZED GRAVEL PR004 SOURCE KITENGELA SIEVE SIZE 50 28 20 10 5 2.36 1.18 0.6 0.425 0.3 0.15 0.075 less 0.075 SIEVE SIZE UPPER LIMIT LOWER LIMIT 50 37.5 28 20 10 5 2 1 0.425 0.075 100 100 100 100 90 75 50 40 33 20 100 95 80 60 35 20 12 10 7 4 wt retained 0 0 0 10.1 6.6 14.6 14.9 14.8 7.8 7.3 13.7 7.8 102 wt passing 98 98 98 87.9 81.3 66.7 51.8 37 29.2 21.9 8.2 0.4 200 98 % passing 100.00 100.00 100.00 89.69 82.96 68.06 52.86 37.76 29.80 22.35 8.37 0.41 GRADING ENVELOPE UPPER LIMIT 120 100 % PASSING 80 LOWER LIMIT 60 40 GRADING CURVE 20 0 0 10 20 30 40 50 60 SIEVE SIZE 58 PARTICLE SIZE DISTRIBUTION-GRADING FIFTH YEAR PROJECT DATE SAMPLED 3/3/15 DATE TESTED 3/3/15 MATERIAL DISCRIPTION SAMPLE NUMBER WEIGHT BEFORE WASH WEIGHT AFTER WASH 10% QUARY DUST STABILIZED GRAVEL PR005 SOURCE KITENGELA SIEVE SIZE 50 28 20 10 5 2.36 1.18 0.6 0.425 0.3 0.15 0.075 less 0.075 SIEVE SIZE UPPER LIMIT LOWER LIMIT 50 37.5 28 20 10 5 2 1 0.425 0.075 100 100 100 100 90 75 50 40 33 20 100 95 80 60 35 20 12 10 7 4 wt retained 0 0 0 24.9 5.7 11.3 14.8 15.2 8.1 7.6 12.8 7.8 92.2 wt passing 107.8 107.8 107.8 82.9 77.2 65.9 51.1 35.9 27.8 20.2 7.4 -0.4 200 107.8 % passing 100.00 100.00 100.00 76.90 71.61 61.13 47.40 33.30 25.79 18.74 6.86 -0.37 GRADING ENVELOPE UPPER LIMIT 120 100 80 % PASSING LOWER LIMIT 60 40 GRADING CURVE 20 0 0 -20 10 20 30 40 50 60 SIEVE SIZE 59 PARTICLE SIZE DISTRIBUTION-GRADING FIFTH YEAR PROJECT DATE SAMPLED 3/3/15 DATE TESTED 3/3/15 MATERIAL DISCRIPTION SAMPLE NUMBER WEIGHT BEFORE WASH WEIGHT AFTER WASH 15% QUARY DUST STABILIZED GRAVEL PR006 SOURCE KITENGELA SIEVE SIZE 50 28 20 10 5 2.36 1.18 0.6 0.425 0.3 0.15 0.075 less 0.075 SIEVE SIZE UPPER LIMIT LOWER LIMIT 50 37.5 28 20 10 5 2 1 0.425 0.075 100 100 100 100 90 75 50 40 33 20 100 95 80 60 35 20 12 10 7 4 wt retained 0 0 0 15.7 7.2 15.4 17.6 15.8 8.1 6.7 13.5 8.9 91.5 wt passing 108.5 108.5 108.5 92.8 85.6 70.2 52.6 36.8 28.7 22 8.5 -0.4 200 108.5 % passing 100.00 100.00 100.00 85.53 78.89 64.70 48.48 33.92 26.45 20.28 7.83 -0.37 GRADING ENVELOPE UPPER LIMIT 120 100 80 % PASSING LOWER LIMIT 60 40 GRADING CURVE 20 0 0 -20 10 20 30 40 50 60 SIEVE SIZE 60 PARTICLE SIZE DISTRIBUTION-GRADING FIFTH YEAR PROJECT DATE SAMPLED 3/3/15 DATE TESTED 3/3/15 MATERIAL DISCRIPTION SAMPLE NUMBER WEIGHT BEFORE WASH WEIGHT AFTER WASH 20% QUARY DUST STABILIZED GRAVEL PR007 SOURCE KITENGELA SIEVE SIZE 50 28 20 10 5 2.36 1.18 0.6 0.425 0.3 0.15 0.075 less 0.075 SIEVE SIZE UPPER LIMIT LOWER LIMIT 50 37.5 28 20 10 5 2 1 0.425 0.075 100 100 100 100 90 75 50 40 33 20 100 95 80 60 35 20 12 10 7 4 wt retained 0 0 0 10.5 6.2 20.3 17.6 13.7 6.8 6.4 11.8 8.5 98.5 wt passing 101.5 101.5 101.5 91 84.8 64.5 46.9 33.2 26.4 20 8.2 -0.3 200 101.5 % passing 100.00 100.00 100.00 89.66 83.55 63.55 46.21 32.71 26.01 19.70 8.08 -0.30 GRADING ENVELOPE UPPER LIMIT 120 100 80 % PASSING LOWER LIMIT 60 40 GRADING CURVE 20 0 0 -20 10 20 30 40 50 60 SIEVE SIZE 61 FIFTH YEAR PROJECT MATERIAL SUMARY FOR GRADING AND ATTERBERGS LIMITS RESULTS SAMPLE NO MATERIAL DESCRIPTION % PASSING SIEVE 0.425 PI PM PR001 NEAT GRAVEL 29.1 32.11 934.40 PR002 0.5% CEMENT STABILIZED GRAVEL 28.2 23.93 674.83 PR003 2.5% CEMENT STABILIZED GRAVEL 0 21.99 0.00 PR004 5% QUAEY DUST STABILIZRD GRAVEL 26.2 29.8 780.76 PR005 10% QUAEY DUST STABILIZRD GRAVEL 25.3 25.79 652.49 PR006 15% QUAEY DUST STABILIZRD GRAVEL 24.3 26.45 642.74 PR007 20% QUAEY DUST STABILIZRD GRAVEL 22.2 26.01 577.42 0 1000.00 1 2 3 4 5 CURVE6 PLASTICITY MODULUS 7 8 1000.00 934.40 900.00 900.00 780.76 PLASTICITY MODULUS 800.00 700.00 800.00 674.83 652.49 700.00 642.74 577.42 600.00 600.00 500.00 500.00 400.00 400.00 300.00 300.00 200.00 200.00 100.00 100.00 0.00 0.00 0.00 PM CURVE PM GRAPH MATERIAL TYPE 62 0 1 2 3PLASTICITY 4 5 CURVE6 INDEX 35 30 7 8 35 29.1 28.2 30 26.2 25.3 24.3 25 PI VALUES 22.2 25 20 20 15 15 10 10 5 5 0 NEAT GRAVEL 0 0 0.5% 2.5% 5% QUAEY 10% QUAEY 15% QUAEY 20% QUAEY CEMENT CEMENT DUST DUST DUST DUST STABILIZED STABILIZED STABILIZRD STABILIZRD STABILIZRD STABILIZRD GRAVEL GRAVEL GRAVEL GRAVEL GRAVEL GRAVEL MATERIAL DESCRIPTION PI GRAPH PI CURVE 63 ANALYSIS OF ATTERBERGS LIMITS AND GRADING TEST The significance of atterbergs limits test is to show the behavior of the material with changes of water. This is a key parameter since variation of weather leads to changes in the material. The change of rainy to sunny seasons leads to expansion and shrinkage of the granular material. The atterbergs limits test shows clearly how the tested material would behave with these changes. The neat gravel had a PI of 29.1.Addition of cement led to a decrease in the PI from 29.1 to 28.2 with 0.5 % cement and the material became non plastic with 2.5% cement. This is as a result of chemical reaction with cement and the clay or plastic particles which in turn reduces the plasticity. From the Ministry of Transport and Communication Standard Spec For Road and bridge construction clause 1203a, the maximum required PI limit for sub base gravel material should be 15%.Thus the neat gravel and 0.5 % stabilization does not meet the requirement. Use of this material would result to excessive expansion with ingress of water and excessive shrinkage during dry season. This would result to fatigue and failure of the pavement. Stabilization using 2.5% cement makes the material non plastic. This is undesirable in pavement construction since the material would not be easily workable and have less cohesiveness. As a result of this, the material would not bond perfectly and would tend to shear off while being compacted. Stabilization using quarry dust led to decrease in the PI with increase in the quantity of the quarry dust. This is as a result of addition of quarry dust which is non-plastic hence lowering the PI of the material. The lowest PI with quarry dust stabilization was achieved with 20% quarry dust. At this point, a PI value of 22.2 % was obtained. This is also higher than the minimum required PI value for sub base granular material. From the same specification, the maximum allowed Plasticity Modulus (PM) is 250.All the stabilization dosages had PM values more than 250%.This indicated that the material had a lot of fine plastic particles passing sieve 0.425.Both mechanical and chemical stabilization lowered the amount of the particles passing sieve 0.425.Stabilization with cement reacted by bonding the fines particles hence a reduce in the fines while stabilization with quarry dust added more course material hence lowering the fines quantity. The neat gravel passed outside the grading envelope for base material as per the roads and bridge construction hence showing that the material is not good enough to be used as base material. The grading curve moved outside the upper limit showing lack of sufficient course material. The curve for the suitable material should move smoothly inside the envelope. Stabilization with both cement and quarry dust made the material more course. However all the materials lacked 64 material retained at sieve 20 to 37.5.This shows the material is not suitable to be used in base layer basing on the grading results, since any addition of quarry dust would not improve the lack of material in sieve 20 to 37.5 and cement stabilization would also not add any significant material in the same sieve. 65 CHAPTER FIVE 5.0DISCUSSIONS, CONCLUSIONS AND RECOMMENDATIONS 5.1 DISCUSSIONS 66