Tests to Analyse and Classify the Plasticity, Particle Size and Engineering Properties of Soils

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Tests to Analyse and Classify the Plasticity, Particle Size and Engineering Properties of Soils CIVL2410 Soil Mechanics: Classification Lab Report SID: 510460929 1.1 Abstract This report describes the experiments regarding plasticity and particle size analysis, specifically through the experiments of Cone Penetrometer, Atterberg Tests, and Sieving and Hydrometer Tests. The aim of these experiments was to use experimental methods to classify and identify the engineering properties of given soils. Through the examination of the moisture contents present within the soil, and the examination of the particle sizes for another sample, the soils were classified through the Unified Soils Classification Systems (USCS). The liquid limit, plastic limit and plasticity index were identified for a set of sample soils, whereas the grading curve was determined for another sample of soil. By examining the grading curve, the soil sample which exhibited behaviours of sand, displayed the composition of the typical grading curve of C: Well graded with some clay. Examining the plasticity of another soil sample, which exhibited behaviour of clay, found that through the discovery of its plastic and liquid limits, it was determined that the soil was an inorganic clay with high plasticity. The liquid limit was on average 56.9 with an accompanying plastic limit of 19.8 with an average plasticity index of 37.1. This was used within the USCS to classify that the soil was an inorganic clay (CH).
2.1 Introduction Soil is a particulate material with engineering properties that are difficult to control. Classification is undertaken to understand the likely behaviours of specific soils. It is important that engineers understand these behaviours to determine the limitations of the soil which they must work with. Fine and coarse grained soils observe differences in the ability to resist plastic deformation, as well as differing in strength and stiffness. These differences in properties lead to different usability depending on a soils classification. By undertaking experiments following the Australian Standard AS1289 Section 3, in conjunction with Unified Soil Classification System (USCS), the plasticity and particle size of a given soil core sample can be determined. A sieve and hydrometer experiments were undertaken to determine the grading curve of the provided cohesionless soil. Atterberg tests alongside a cone penetrometer test were performed on cohesive soils to determine the plastic and liquid limits of the given soil. The aim of these experiments was to classify the provided soil to gain an understanding of the engineering properties and the practical usability of the soil.
3.1 Methodology 3.1.1 Plasticity: Liquid Limit - The “25 Blows” Method To begin the experiment, measure eight little trays which will hold the soil samples. These trays should be labelled and their weights should be recorded. For the plasticity experiment, use three samples of soils which have been premixed with nominal water which are close to the liquid limit. Choose one of the soil samples and place a little sample inside of the liquid limit apparatus and level it out so that the height of soil is level with the apparatus base. Using a standard grooving tool, create a groove within the soil by scraping to the bottom of the bowl. Once the groove has been created within the soil, rotate the handle of the apparatus twice per second, until the groove has closed up. During this process, count the blows of the apparatus until the groove has closed. Record the amount of blows and clean out the bowl. Repeat the same experiment with the same sample until the amount of blows between two consecutive tests is not greater than one. Use a small sample from the bowl and place it into a tray and weigh the tray with the soil. Repeat this for each different soil sample and record the amount of blows (Appendix 1.1). 3.1.2 Plasticity: Liquid Limit - The Cone Penetrometer Method Choose one of the soil samples and fill up a small container and level the top surface of the soil. Place the container within the penetrometer and lower the cone so that it just touches the surface of the soil. Set the dial gauge to zero, and release the cone for five seconds, and then lock it. Record the final penetration value (Appendix 1.2) and use one of the eight little trays and put in a small sample from the container. Reset the cone, and repeat the experiment with the different soil samples. 3.1.3 Plasticity: Plastic Limit - The “Make-a-Snake” Method Weigh a saucer which will be used for later calculations. Using a soil sample which has been dried to near the plastic limit, roll 10 of the soil into a “slug” with a diameter ?? 3 of approximately 5 mm. Continue rolling the “slug” until the diameter is 3 mm. If the soil doesn’t crumble, create a ball with the rolled “slug” and repeat the process again. Once the “slug” crumbles at 3 mm in diameter, flatten 1 of the soil and place it in the ?? 3 saucer and weigh the soil and saucer. Place the saucer inside an oven which has been set on medium heat and leave it in for thirty seconds and weigh the soil again. Change the temperature to medium-low and place the saucer in the oven for twenty seconds and weigh it and repeat the experiments until the weights on successive are at least (<1% difference). Record the values (Appendix 1.3).
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3.2.1 Particle Size Analysis: Sieving Using a tub of sandy soil, weigh the soil within the tub and record the mass. Using a set of clean sieves, measure the mass of each individual sieve within the set and record the values. (Sieve sizing in Appendix 1.5). Assemble the sieves in order, and pour the soil into the sieves and place the sieves into a shaking machine for three to four minutes. Disassemble the sieves and weigh each tray with its captured soil. Set aside the bottom sieve for the hydrometer test. 3.2.2 Particle Size Analysis: Hydrometer Before the experiment, measure the mass of a hydrometer. Pour the soil from the bottom of the sieve into a shaker and add approximately 150 ml of distilled water into the shaker. Turn on the shaker for 5 minutes, and after it is finished, place soil into a graduated cylinder. Make sure to clean out the shaker completely and pour as much of the soil into the cylinder. Add water into the cylinder until it is filled to the 1000 ml mark. Cover the top of the graduated cylinder and rotate it vertically to properly mix the soil with the water. As the cylinder is undergoing the mixing, get ready to use the timer. Place the cylinder down and immediately place the hydrometer and thermometer inside and start the timer. At time intervals of 15 seconds, 30 seconds, 1 minute, 2 minutes, 4 minutes and 8 minutes, observer and record the values (Appendix 1.6) for temperature and hydrometer readings on the meniscus. 𝑅'
4.1 Results The following results from the experiments are shown below. Number of Blows Moisture Content (%) Sample Preliminary Final 1 21 22 54.5 2 40 41 53.6 3 41 42 62 Fig. 1: “25 Blows” Experiment Results and Calculated Moisture Content Fig 1 demonstrates the results from the 25 blows experiment in which the highest moisture content came from sample 3, which saw a significantly higher moisture content as compared to sample 2 which had a similar number of blows. Cone Penetration (mm) Moisture Content (%) Sample Test 1 Test 2 Test 3 Average 1 24 23.3 22 23.1 64.4 2 18.6 17.5 18.7 18.3 56.3 3 17.5 16.6 17.4 17.2 53.7 Fig. 2: Cone Penetration Experiment Results and Calculated Moisture Content Fig 2 shows that the cone was able to penetrate deeper with samples with a higher moisture content, demonstrating the plasticity of the soil. Moisture Content (%) Test Microwave Method Standard Method 1 21.5 27.5
2 18.1 17.3 Average: 22.4 Fig. 3: Moisture Content of PL Snake Method Fig 3 shows the results obtained to find moisture content using the “Snake Method”. This would then be used to determine the Plastic Limit of the soil. In comparison to the other testing method, the moisture content is significantly lower. The average of the microwave method values would be taken as the plastic limit ( AS 1289.3.2.1) Sample Water (g) Dry Soil (g) Moisture Content (%) LL 25 Blows 1 3.78 6.93 54.5 LL 25 Blows 2 2.74 5.11 53.6 LL 25 Blows 3 4.65 7.5 62 LL Cone 1 4.98 7.73 64.4 LL Cone 2 5.11 9.08 56.3 LL Cone 3 5.89 10.96 53.7 PL Snake 1 0.11 0.4 27.5 PL Snake 2 0.13 0.75 17.3 Fig 4: Calculated Moisture Content of all Experiments Fig 4 highlights the moisture contents calculated for each experimental method. Cone Penetration test 1 exhibited the largest moisture content, whereas the “Snake” sample 2 exhibited the lowest, displaying the significance of the reduction in moisture content through friction. The moisture content of each experiment were calculated as shown in Appendix 1.4
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Fig 5: Liquid Limit Graphs of Cone Penetrometer and 25 Blows Method Using “25 Blows” Using Cone Penetrometer LL PL 𝐼 ? LL PL 𝐼 ? 59 19.8 39.2 54.8 19.8 35 Fig 6: Liquid Limit, Plastic Limit, and Plasticity Index of Experimental Methods Fig 5 represents the graph of moisture content vs. the according values for each experiment. For Cone Penetration, moisture content is plotted against cone penetration in mm, whereas the 25 Blows Method is plotted against the number of blows. The liquid limit values were calculated through the equation determined in Fig 5 (Appendix 1.7)
Using Appendix 1.11, this soil can be seen as an inorganic clay with high plasticity. This clay, through Appendix 1.12, is seen to exhibit high toughness near its plastic limit, as well as high to very high dry strength crushing characteristics. It also shows no dilatancy. The liquid limit is tabulated in Fig 6 along with the plastic limit and plasticity index. The plasticity index is calculated through . 𝐼 ? = ?? − 𝑃? Sieve Number Mesh Size ‘D’ K = % Passing Through 1 2.36 mm 100 2 1.18 mm 93.24 3 600 μm 81.99 4 425 μm 67.60 5 300 μm 49.37 6 150 μm 27.46 7 75 μm 13.38 Bottom pan <75 μm Fig 7: Percentage of Total Soil Mass Passing Each Sieve Elapsed Time t (min) Diameter ‘D’ (μm) K = ( ) * 100 ? ? /? ???𝑎? 0.25 (15 secs) 86.88 11.60 0.5 64.85 10.64 1 47.90 8.71 2 36.34 6.78 4 28.19 2.44
8 20.82 0.02 16 15.24 0.02 Fig 8: Percentage Finer in Hydrometer Assumptions regarding the calculation of K in Fig 8, are listed in appendix 1.5 Fig 9: Percentage Finer for Each Particle Size Fig 7 and Fig 8 highlight the % finer for each diameter of particles, which are plotted in Fig 9 to demonstrate the grading curve of the soil
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5.1 Discussion Initial observations regarding the plasticity experiment samples were that the soil exhibited characteristics of clay. The moisture content provided within the soil ranged between 53% to 65% which remained constant between the experimental methods of “25 Blows” and Cone Penetrometer. This is characteristic of clays which contain and retain water well due to its fine particles. This isn’t the case for the “Snake” Method, in which the soils experienced a reduction in moisture content through friction by the action of rolling. The plastic limit of this soil was determined through the microwave method. Since the soil samples used for the “Snake” Method were nearing its plastic limit, the moisture content derived from these experiments is used as the plastic limit. By plotting the moisture content vs. number of blows for the “25 Blows” test results, as well as plotting moisture content vs. cone penetration for the penetrometer test, the liquid limits can be derived. By adding a trendline to the graphs, the following equations in fig 5 are used to interpolate the liquid limits which are then used to calculate the plasticity index of the provided soils. Examining Fig 6, the liquid limits for clay with high plasticity range between 60-85, with plasticity index ranging within 35-55 (Wagner, J., 2013). Analysing the results found, the values corresponding to the “25 Blows” method fit closer within these ranges as opposed to the cone penetrometer results. By using the USCS, and examining the plasticity chart (Appendix 1.11), it can be deduced that the provided soil falls within the CH section of the graph. These soils are classified as inorganic clays of high plasticity, with characteristics of high toughness near the plastic limit, high to very high dry strength crushing characteristics and no existing dilatancy. Through particle size analysis, a grade curve for the soil was constructed within fig 9. This curve illustrates the composition of the different particle sizes present within the soil mass. It divides the soil into its different particle sizes and the total percentage of the total mass is of each particle size. This curve found is comparable to a curve graded as C: well graded with some clay. This shows that this soil is suitable for construction due to the large range of particle sizes present within the soil. Well graded soils undergo compaction easily while minimising the voids present within the mass. The classification of this soil is important due to the understanding of how these soils can be used in relation to foundations. This well graded soil can be regarded as sandy-silt as its predominant particle sizes are mostly less than 0.1 mm in particle size but greater than 0.01, which highlights the range of medium to coarse silt.
6.1 Conclusion The soils in this experiment have been classified and concluded to be inorganic clays with high plasticity, denoted with a group symbol of CH. This soil has a liquid limit of 59%, a plastic limit of 19.8% and a plasticity index of 39.2%. This clay experiences a high moisture content due to the characteristic of clay which has the ability to hold water well. The other soil examined had been classified as a sandy-silt through the construction of its grade curves. It has been deduced as a well-graded soil with clay which is suitable for construction purposes. With the knowledge of classification, engineers have to ability to deduce whether a soil present within a site is suitable for construction, thus avoiding any future occurrences through the examination and classification of the soils.
7.1 References Dhir, R.k. (2017). Sustainable Construction Materials: Copper Slag . United Kingdom:Elsevier. Wagner, J.-F. (2013). Developments in Clay Science (Vol. 9). Netherlands:Elsevier. Akbulut, S. (2011). Effect of particle size and shape on the grain-size distribution using image analysis. Turkey: INTERNATIONAL JOURNAL OF CIVIL AND STRUCTURAL ENGINEERING.
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8.1 Appendix Appendix 8.1.1 - Original Recorded Table Values Appendix 1.1 - 25 Blows Method Recorded Values Appendix 1.2 - Cone Penetration Test Recorded Values Appendix 1.3 - Snake Method Recorded Values The average of the microwave methods was taken to be the plastic limit of the soil, later used in appendix 1.7.
Appendix 1.4 - Calculation of Moisture Content Calculations were done through the steps highlighted within the column headings. Appendix 1.5 - Recorded Sieve Values
was assumed as and was determined using appendix 1.8, based on 𝐶 ? 2. 5 × 10 −4 𝐶 𝑇 the temperature of 18.7. F1, F2, and F3 values were all determined through appendix 1.8 to 1.10. Mass in suspension was calculated through the formula below: Factor a is taken as 0.98, due to soil particle density being taken as 2.75 Appendix 1.6 - Recorded Hydrometer Values Appendix 1.7 - Calculated Liquid Limit, Plastic Limit, and Plasticity Index for Experimental Methods The following equations were derived through fig 5 in which cone penetrometer test was 1.7757x + 23.449 and 25 blows had an equation of y = 0.1854x + 50.21. To calculate 𝑦 = the liquid limit for the 25 blows method, the value of 25 was to be substituted into its unique equation to determine the moisture content. The corresponding moisture content to 25 blows was taken as the liquid limit. For the cone penetrometer test, the liquid limit
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was found by using the equation with x taken as 20 mm, in which the corresponding y value would be taken as the liquid limit. Plasticity index was calculated through appendix 1.3, and thus plasticity index is calculated using Ip = LL - PL. Appendix 1.8 - values based on Temperature Readings 𝐶 𝑇
Appendix 1.9 - values depending on Rh1 values 𝐹 1
Appendix 1.10 - values based on density and temperature and time 𝐹 2 𝑎?? 𝐹 3
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Appendix 1.11 - Plasticity Chart Appendix 1.12 - Unified Soil Classification Chart