This document describes various laboratory methods for determining soil properties, including liquid limit, plastic limit, and field density. The liquid limit can be found using a Casagrande apparatus or cone penetrometer, which measure the number of blows or penetration depth required for a soil sample to close a groove at different water contents. The plastic limit is the water content at which a soil thread crumbles. Field density is measured using a core cutter method or sand replacement method.
This document describes procedures to determine consistency limits of soils, including liquid limit, plastic limit, and shrinkage limit, according to IS codes. Key points:
1) The liquid limit is the water content at which a soil transitions from liquid to plastic state, defined as the water content required for a soil sample to flow together over 13mm after 25 blows.
2) The plastic limit is the water content at which a soil transitions from plastic to semi-solid state, defined as the minimum water content needed for a soil to be rolled into 3mm threads.
3) The shrinkage limit is the lowest water content at which a soil is fully saturated without changing volume during drying. Consistency limits are used
The document discusses three soil tests: the liquid limit test determines the moisture content needed for a soil pat to close a groove after 25 drops from 10 mm; the plastic limit test finds the moisture content where a 3 mm soil thread will crumble; and the shrinkage limit test measures the volume and mass of wet and dried soil in a dish to determine moisture loss.
This document summarizes the liquid limit and plastic limit tests conducted on a soil sample. The liquid limit was found to be 51.679% using two different methods that produced similar results. The plastic limit was 24.525%. Based on these Atterberg limits, the soil was classified as clay with high plasticity. The limits help characterize the soil's engineering properties and behavior when wet or dry. The experiment showed the soil behaves plastically when wet and becomes hard when dry, typical of clays.
Goetechnical lab tests, atterberg limits tests Kamal Bhagat
The document discusses various methods used to characterize soils, including Atterberg limits, Proctor compaction testing, and field density testing.
The Atterberg limits—liquid limit, plastic limit, and shrinkage limit—describe the critical water content ranges where a fine-grained soil transitions between solid, semi-solid, plastic, and liquid states.
Proctor compaction testing involves compacting soil samples at different moisture contents to determine the optimum moisture content and maximum dry density for compaction.
Field density testing uses core cutter and sand replacement methods to directly measure the dry density of compacted soils in construction projects like embankments, highways, and railways.
This presentation focuses on the significance of soil compaction (particularly the Proctor Test), how the test is performed, necessary equipment and helpful tips.
Determination of Liquid Limit of Soil : Civil EngineeringAbdullah Hayat Khan
This document describes the procedure to determine the liquid limit of soils according to the Casagrande cup method. It provides background on the concept of the Atterberg limits and defines the liquid limit. The objective is to establish the relationship between moisture content and blows to determine the liquid limit value. The apparatus and step-by-step procedure are outlined. An example calculation is shown. References for additional information are also provided.
This document describes various laboratory methods for determining soil properties, including liquid limit, plastic limit, and field density. The liquid limit can be found using a Casagrande apparatus or cone penetrometer, which measure the number of blows or penetration depth required for a soil sample to close a groove at different water contents. The plastic limit is the water content at which a soil thread crumbles. Field density is measured using a core cutter method or sand replacement method.
This document describes procedures to determine consistency limits of soils, including liquid limit, plastic limit, and shrinkage limit, according to IS codes. Key points:
1) The liquid limit is the water content at which a soil transitions from liquid to plastic state, defined as the water content required for a soil sample to flow together over 13mm after 25 blows.
2) The plastic limit is the water content at which a soil transitions from plastic to semi-solid state, defined as the minimum water content needed for a soil to be rolled into 3mm threads.
3) The shrinkage limit is the lowest water content at which a soil is fully saturated without changing volume during drying. Consistency limits are used
The document discusses three soil tests: the liquid limit test determines the moisture content needed for a soil pat to close a groove after 25 drops from 10 mm; the plastic limit test finds the moisture content where a 3 mm soil thread will crumble; and the shrinkage limit test measures the volume and mass of wet and dried soil in a dish to determine moisture loss.
This document summarizes the liquid limit and plastic limit tests conducted on a soil sample. The liquid limit was found to be 51.679% using two different methods that produced similar results. The plastic limit was 24.525%. Based on these Atterberg limits, the soil was classified as clay with high plasticity. The limits help characterize the soil's engineering properties and behavior when wet or dry. The experiment showed the soil behaves plastically when wet and becomes hard when dry, typical of clays.
Goetechnical lab tests, atterberg limits tests Kamal Bhagat
The document discusses various methods used to characterize soils, including Atterberg limits, Proctor compaction testing, and field density testing.
The Atterberg limits—liquid limit, plastic limit, and shrinkage limit—describe the critical water content ranges where a fine-grained soil transitions between solid, semi-solid, plastic, and liquid states.
Proctor compaction testing involves compacting soil samples at different moisture contents to determine the optimum moisture content and maximum dry density for compaction.
Field density testing uses core cutter and sand replacement methods to directly measure the dry density of compacted soils in construction projects like embankments, highways, and railways.
This presentation focuses on the significance of soil compaction (particularly the Proctor Test), how the test is performed, necessary equipment and helpful tips.
Determination of Liquid Limit of Soil : Civil EngineeringAbdullah Hayat Khan
This document describes the procedure to determine the liquid limit of soils according to the Casagrande cup method. It provides background on the concept of the Atterberg limits and defines the liquid limit. The objective is to establish the relationship between moisture content and blows to determine the liquid limit value. The apparatus and step-by-step procedure are outlined. An example calculation is shown. References for additional information are also provided.
This document presents information on determining the Atterberg limits of soils, which are important properties used to characterize soils in engineering. It discusses the purpose and procedures for determining the liquid limit and plastic limit through laboratory tests. The liquid limit is the moisture content where a soil changes from plastic to liquid state, while the plastic limit is where it changes from semi-solid to plastic. Factors like clay content and type, organic matter, and exchangeable cations can affect the Atterberg limits. The document describes the apparatus used and discusses the meaning and applications of these tests.
This document provides information about various soil testing methods and procedures used in geotechnical engineering, including:
- Common soil tests like Atterberg limits, sieve analysis, moisture content, unit weight, and California Bearing Ratio.
- Details on performing the liquid limit, plastic limit, and sieve analysis tests in the lab.
- Explanations of key concepts like the plasticity index and using Atterberg limits for soil classification.
- Information on other topics like compaction testing, grain size distribution, and sieve size designations.
Determination of water content-dry density relation using light compaction (Standard Proctor Test).
Soil Specimen (Compositions of Dhanauri Clay and Delhi Silt).
It is seen that as the proportion of clay is increased in the soil mix the Optimum Moisture Increases and the Maximum Dry Density Decreases.
This document describes procedures for determining the liquid limit of a soil sample using the cone penetration test method. The objective is to determine the moisture content at which the soil changes from a plastic to a liquid state. The test involves mixing soil with varying amounts of water and measuring penetration of a standardized cone into the sample. When the penetration reaches 20mm, the moisture content corresponds to the liquid limit. The document outlines the required equipment, procedures, data collection and analysis steps to calculate the liquid limit percentage. Analysis of the results helps characterize the soil sample and determine appropriate foundations and structures to build on that site.
Determination of Liquid Limit and Plastic Limit of given soil sample.
Soil Sample - A sample weighing about 60 g was taken from the thoroughly mixed portion of material (70% Bentonite: 30% Kaolinite) passing 425-micron IS Sieve [ IS: 460 (Part 1)-1978] obtained in accordance with IS: 2720 (Part 1)-1983.
The four combinations of Bentonite-Kaolinite mixture gave following trend. In general with decrease in bentonite content and increase in kaolinite content, the Liquid Limit, Plastic Limit and Plasticity Index starts decreasing.
Sieve analysis
Atterberg limit test (liquid limit & Plastic limit)
Compaction test (Standard and modified proctor test)
California bearing ratio test (CBR)
-Determination of water content of soil by oven drying method
-Determination of dry density of soil by sand replacement method
-Grain Analysis of Soil
-Determination of liquid limit and plastic limit of soil
-Liquid limit determination by cone penetrometer
-California Bearing Ratio (CBR) value test
- Direct shear test
-Standard penetration test
This document summarizes a standard Proctor compaction test conducted on a soil sample. The test involves compacting the soil at different moisture contents in layers using a standardized hammer and measuring the dry unit weight. The maximum dry unit weight of 1.74 g/cm3 was found at an optimum moisture content of 13.7% based on the graph, however one data point exceeded the theoretical zero-air void curve, invalidating the test. The test will need to be redone to get accurate and dependable results.
1) The Proctor compaction test is used to determine the optimal moisture content and maximum dry density of soil. It involves compacting soil in layers in a mold using controlled blows and measuring the dry density at different moisture contents.
2) The test procedure involves weighing equipment, sieving dry soil, compacting soil in layers using blows from a ram, weighing the compacted soil, determining moisture content, and repeating at different moisture contents.
3) A compaction curve is made by plotting dry density against moisture content. The peak of the curve indicates the optimum moisture content which produces the highest dry density.
The document describes the standard Proctor compaction test procedure. The test is used to determine the maximum dry density and optimum moisture content of soils. It involves compacting soil samples at incrementally increased moisture contents using a specified compaction method. A compaction curve is plotted showing the relationship between dry density and moisture content. The peak of the curve indicates the optimum moisture content and maximum dry density achieved for that soil. The test uses a cylindrical metal mold, rammer, balance, oven and other equipment to compact and analyze the soil samples according to steps that sieve, mix, compact and weigh the soil at different moistures.
The document describes the oedometer test procedure used to determine soil properties like compression coefficient, consolidation coefficient, permeability, and compressibility. The test involves placing a saturated soil sample in an oedometer apparatus and incrementally increasing the load over time while monitoring settlement. Properties are calculated from the settlement readings using methods like square root of time or log of time.
This report summarizes an experiment to determine the minimum and maximum dry density of a Badarpur sand soil specimen. Testing was conducted according to Indian Standards and involved compacting sand in a vibratory compactor and measuring the dry density. The average minimum dry density was found to be 1.469 g/cm3 and the average maximum was 1.679 g/cm3. These values were 11-15% higher than a Yamuna River sand sample. The Badarpur sand was also observed to be more angular in shape compared to the Yamuna River sand. The report discusses how dry density values can depend on testing methods and compaction energy applied.
Determination of in situ density of soilSumanHaldar8
This document describes methods to determine the unit weight of soil. There are five types of unit weight: bulk, saturated, dry, submerged, and solid. The core cutter and sand replacement methods are explained. The core cutter method involves extracting a soil sample with a cutter, weighing it, and calculating bulk and dry unit weights. The sand replacement method involves using a calibrated container, pouring sand into an excavated hole to displace the soil, then weighing and calculating the soil's unit weight. Precautions for each method are provided.
The document discusses compaction tests for soil. It defines compaction as packing soil particles more closely together through dynamic loading, reducing air voids without changing water content. Compaction improves soil engineering properties like strength and permeability. Laboratory tests establish relationships between dry density and moisture content under controlled conditions. The standard Proctor test uses a 2.6 kg hammer and the modified Proctor test uses a 4.89 kg hammer, transmitting more energy to achieve higher compaction. Both tests yield curves showing maximum dry density occurs at optimum moisture content.
The document discusses soil compaction testing. There are two main types of compaction tests - standard and modified proctor. The standard proctor test uses a 4 inch diameter mold compacted in 3 layers with 25 blows per layer. The modified proctor uses a 6 inch mold compacted in 5 layers with 25 blows per layer. The test determines the optimum moisture content for compaction by measuring dry unit weight at different moisture contents. Testing involves compacting soil samples, determining dry unit weights and moisture contents, and plotting a curve showing maximum dry unit weight corresponds to optimum moisture content.
Index properties of soil and Classification of soils(Geotechnical engineering)Manoj Kumar Kotagiri
This document provides an overview of index properties and classification of soils. It discusses various index properties such as moisture content, specific gravity, density, particle size distribution, and consistency limits. Methods for determining these properties, such as oven drying, pycnometer, core cutter, and sieve and sedimentation analysis are described. Index properties are important for identifying soils and determining their engineering behavior and properties like strength, compressibility, and permeability.
This document discusses soil compaction, including the standard Proctor test used to determine optimum moisture content and maximum dry unit weight of soils. The standard Proctor test involves compacting soil in 3 layers in a standardized mold using a hammer dropped from a specific height. Compaction curves relate dry unit weight to water content, with the peak indicating optimum conditions. Key factors that affect compaction are water content, compactive effort, soil type, and compaction method. Field tests verify compaction using methods such as nuclear gauges, which are faster than destructive sand cone and balloon tests.
The sand replacement test determines the in situ density of natural or compacted soils using sand pouring cylinders. The test involves excavating a soil sample, measuring its mass, and replacing the excavated volume with sand of a known density to find the sample volume. This allows calculating the dry density based on the sample mass and volume. The test establishes a relationship between dry density and moisture content. It is used to evaluate compaction levels in the field according to acceptance criteria for different depths.
The document provides instructions for conducting 12 geotechnical engineering experiments in the geotechnical engineering lab at B.V. Raju Institute of Technology. The experiments include determining Atterberg limits, field density via core cutter and sand replacement methods, grain size analysis, constant and variable head permeability tests, unconfined compression test, direct shear test, compaction tests, and CBR testing. Students must complete 8 of the 12 experiments listed. Instructions are provided for each experiment, including the aim, theory, apparatus required, and procedures to follow.
Atterberg limit test
soil mechanics
prepared by Rezhwan Hama Karim
University Of Halabja
Civil Engineering Department.3rd stage
Soil lap
University Of Halabja
Civil Engineering Department.3rd stage
Soil lap
Contents:
Introduction
Purpose of this experiment
Materials and equipment
Procedure
Data analysis
Discussion
Conclusion
Introduction
Atterberg limits tests establish the moisture contents at which fine-grained clay and silt soils transition between solid, semi-solid, plastic, and liquid states. Liquid limit determination from a plot of the number of drops of the standard cup required to close a standard groove in a soil pat against the water content of the soil. The liquid limit is the water content of the soil that would correspond to the standard groove closing in 25 drops of the cup. The plastic limit is the water content at which a soil-water paste changes from a semisolid to a plastic consistency as it is rolled into a 3.175-mm (1/8-inch) diameter thread in a standard test.
Purpose of this experiment
This lab is performed to determine the plastic and liquid limits of a fine-grained soil. The liquid limit (LL) is arbitrary defined as the water content, in percent, at which a pat of soil in a standard cup and cut by a groove of standard dimensions will flow together at base of the groove for a distance of 13mm (1/2in.) when subjected to 25 shocks from the cup being dropped 10mm in standard liquid limit apparatus operated at a rate of two shocks per second. The plastic limit (PL) is the water content, in percent, at which a soil can no longer be deformed by rolling into 3.2mm (1/8in.) diameter threads without crumbling.
Standard reference
ASTM D4318-standard test method for liquid limit, plastic limit, and plasticity index of soils.
Discussion:
In this test we found Liquid limit plastic limit for find plastic index and due this results we found type of our fine grained soil in this way:
Depending in USCS system we found that LL (35.33) <50% this mean our soil is low plasticity soil. And with this equation we find is our soil is silt or clay PI < (0.73(LL-20)) which PI (7.83) < (0.73(LL-20)) which PI<11.69 this mean our soil is silt so this explain to us that our soil is low plasticity silt ML (lean silt). Approximately we can say that we don’t have error in our test but for plastic limit test we repeated the trail for three times until the diameter of the soil same as diameter of the rod and produce crack however we can say there’s no error for our test.
Conclusion:
Attaberg limit is the test method which used for finding each of liquid limits due to our liquid limit curve which we draw it between water content and number of blows and we found plastic limit by taking water content average for each trail and by differencing LL and PL we found plastic index. And with this plastic index and liquid limit we classified our fine grain soil which is our result is low plasticity silt as we said in the discussion.
This document presents information on determining the Atterberg limits of soils, which are important properties used to characterize soils in engineering. It discusses the purpose and procedures for determining the liquid limit and plastic limit through laboratory tests. The liquid limit is the moisture content where a soil changes from plastic to liquid state, while the plastic limit is where it changes from semi-solid to plastic. Factors like clay content and type, organic matter, and exchangeable cations can affect the Atterberg limits. The document describes the apparatus used and discusses the meaning and applications of these tests.
This document provides information about various soil testing methods and procedures used in geotechnical engineering, including:
- Common soil tests like Atterberg limits, sieve analysis, moisture content, unit weight, and California Bearing Ratio.
- Details on performing the liquid limit, plastic limit, and sieve analysis tests in the lab.
- Explanations of key concepts like the plasticity index and using Atterberg limits for soil classification.
- Information on other topics like compaction testing, grain size distribution, and sieve size designations.
Determination of water content-dry density relation using light compaction (Standard Proctor Test).
Soil Specimen (Compositions of Dhanauri Clay and Delhi Silt).
It is seen that as the proportion of clay is increased in the soil mix the Optimum Moisture Increases and the Maximum Dry Density Decreases.
This document describes procedures for determining the liquid limit of a soil sample using the cone penetration test method. The objective is to determine the moisture content at which the soil changes from a plastic to a liquid state. The test involves mixing soil with varying amounts of water and measuring penetration of a standardized cone into the sample. When the penetration reaches 20mm, the moisture content corresponds to the liquid limit. The document outlines the required equipment, procedures, data collection and analysis steps to calculate the liquid limit percentage. Analysis of the results helps characterize the soil sample and determine appropriate foundations and structures to build on that site.
Determination of Liquid Limit and Plastic Limit of given soil sample.
Soil Sample - A sample weighing about 60 g was taken from the thoroughly mixed portion of material (70% Bentonite: 30% Kaolinite) passing 425-micron IS Sieve [ IS: 460 (Part 1)-1978] obtained in accordance with IS: 2720 (Part 1)-1983.
The four combinations of Bentonite-Kaolinite mixture gave following trend. In general with decrease in bentonite content and increase in kaolinite content, the Liquid Limit, Plastic Limit and Plasticity Index starts decreasing.
Sieve analysis
Atterberg limit test (liquid limit & Plastic limit)
Compaction test (Standard and modified proctor test)
California bearing ratio test (CBR)
-Determination of water content of soil by oven drying method
-Determination of dry density of soil by sand replacement method
-Grain Analysis of Soil
-Determination of liquid limit and plastic limit of soil
-Liquid limit determination by cone penetrometer
-California Bearing Ratio (CBR) value test
- Direct shear test
-Standard penetration test
This document summarizes a standard Proctor compaction test conducted on a soil sample. The test involves compacting the soil at different moisture contents in layers using a standardized hammer and measuring the dry unit weight. The maximum dry unit weight of 1.74 g/cm3 was found at an optimum moisture content of 13.7% based on the graph, however one data point exceeded the theoretical zero-air void curve, invalidating the test. The test will need to be redone to get accurate and dependable results.
1) The Proctor compaction test is used to determine the optimal moisture content and maximum dry density of soil. It involves compacting soil in layers in a mold using controlled blows and measuring the dry density at different moisture contents.
2) The test procedure involves weighing equipment, sieving dry soil, compacting soil in layers using blows from a ram, weighing the compacted soil, determining moisture content, and repeating at different moisture contents.
3) A compaction curve is made by plotting dry density against moisture content. The peak of the curve indicates the optimum moisture content which produces the highest dry density.
The document describes the standard Proctor compaction test procedure. The test is used to determine the maximum dry density and optimum moisture content of soils. It involves compacting soil samples at incrementally increased moisture contents using a specified compaction method. A compaction curve is plotted showing the relationship between dry density and moisture content. The peak of the curve indicates the optimum moisture content and maximum dry density achieved for that soil. The test uses a cylindrical metal mold, rammer, balance, oven and other equipment to compact and analyze the soil samples according to steps that sieve, mix, compact and weigh the soil at different moistures.
The document describes the oedometer test procedure used to determine soil properties like compression coefficient, consolidation coefficient, permeability, and compressibility. The test involves placing a saturated soil sample in an oedometer apparatus and incrementally increasing the load over time while monitoring settlement. Properties are calculated from the settlement readings using methods like square root of time or log of time.
This report summarizes an experiment to determine the minimum and maximum dry density of a Badarpur sand soil specimen. Testing was conducted according to Indian Standards and involved compacting sand in a vibratory compactor and measuring the dry density. The average minimum dry density was found to be 1.469 g/cm3 and the average maximum was 1.679 g/cm3. These values were 11-15% higher than a Yamuna River sand sample. The Badarpur sand was also observed to be more angular in shape compared to the Yamuna River sand. The report discusses how dry density values can depend on testing methods and compaction energy applied.
Determination of in situ density of soilSumanHaldar8
This document describes methods to determine the unit weight of soil. There are five types of unit weight: bulk, saturated, dry, submerged, and solid. The core cutter and sand replacement methods are explained. The core cutter method involves extracting a soil sample with a cutter, weighing it, and calculating bulk and dry unit weights. The sand replacement method involves using a calibrated container, pouring sand into an excavated hole to displace the soil, then weighing and calculating the soil's unit weight. Precautions for each method are provided.
The document discusses compaction tests for soil. It defines compaction as packing soil particles more closely together through dynamic loading, reducing air voids without changing water content. Compaction improves soil engineering properties like strength and permeability. Laboratory tests establish relationships between dry density and moisture content under controlled conditions. The standard Proctor test uses a 2.6 kg hammer and the modified Proctor test uses a 4.89 kg hammer, transmitting more energy to achieve higher compaction. Both tests yield curves showing maximum dry density occurs at optimum moisture content.
The document discusses soil compaction testing. There are two main types of compaction tests - standard and modified proctor. The standard proctor test uses a 4 inch diameter mold compacted in 3 layers with 25 blows per layer. The modified proctor uses a 6 inch mold compacted in 5 layers with 25 blows per layer. The test determines the optimum moisture content for compaction by measuring dry unit weight at different moisture contents. Testing involves compacting soil samples, determining dry unit weights and moisture contents, and plotting a curve showing maximum dry unit weight corresponds to optimum moisture content.
Index properties of soil and Classification of soils(Geotechnical engineering)Manoj Kumar Kotagiri
This document provides an overview of index properties and classification of soils. It discusses various index properties such as moisture content, specific gravity, density, particle size distribution, and consistency limits. Methods for determining these properties, such as oven drying, pycnometer, core cutter, and sieve and sedimentation analysis are described. Index properties are important for identifying soils and determining their engineering behavior and properties like strength, compressibility, and permeability.
This document discusses soil compaction, including the standard Proctor test used to determine optimum moisture content and maximum dry unit weight of soils. The standard Proctor test involves compacting soil in 3 layers in a standardized mold using a hammer dropped from a specific height. Compaction curves relate dry unit weight to water content, with the peak indicating optimum conditions. Key factors that affect compaction are water content, compactive effort, soil type, and compaction method. Field tests verify compaction using methods such as nuclear gauges, which are faster than destructive sand cone and balloon tests.
The sand replacement test determines the in situ density of natural or compacted soils using sand pouring cylinders. The test involves excavating a soil sample, measuring its mass, and replacing the excavated volume with sand of a known density to find the sample volume. This allows calculating the dry density based on the sample mass and volume. The test establishes a relationship between dry density and moisture content. It is used to evaluate compaction levels in the field according to acceptance criteria for different depths.
The document provides instructions for conducting 12 geotechnical engineering experiments in the geotechnical engineering lab at B.V. Raju Institute of Technology. The experiments include determining Atterberg limits, field density via core cutter and sand replacement methods, grain size analysis, constant and variable head permeability tests, unconfined compression test, direct shear test, compaction tests, and CBR testing. Students must complete 8 of the 12 experiments listed. Instructions are provided for each experiment, including the aim, theory, apparatus required, and procedures to follow.
Atterberg limit test
soil mechanics
prepared by Rezhwan Hama Karim
University Of Halabja
Civil Engineering Department.3rd stage
Soil lap
University Of Halabja
Civil Engineering Department.3rd stage
Soil lap
Contents:
Introduction
Purpose of this experiment
Materials and equipment
Procedure
Data analysis
Discussion
Conclusion
Introduction
Atterberg limits tests establish the moisture contents at which fine-grained clay and silt soils transition between solid, semi-solid, plastic, and liquid states. Liquid limit determination from a plot of the number of drops of the standard cup required to close a standard groove in a soil pat against the water content of the soil. The liquid limit is the water content of the soil that would correspond to the standard groove closing in 25 drops of the cup. The plastic limit is the water content at which a soil-water paste changes from a semisolid to a plastic consistency as it is rolled into a 3.175-mm (1/8-inch) diameter thread in a standard test.
Purpose of this experiment
This lab is performed to determine the plastic and liquid limits of a fine-grained soil. The liquid limit (LL) is arbitrary defined as the water content, in percent, at which a pat of soil in a standard cup and cut by a groove of standard dimensions will flow together at base of the groove for a distance of 13mm (1/2in.) when subjected to 25 shocks from the cup being dropped 10mm in standard liquid limit apparatus operated at a rate of two shocks per second. The plastic limit (PL) is the water content, in percent, at which a soil can no longer be deformed by rolling into 3.2mm (1/8in.) diameter threads without crumbling.
Standard reference
ASTM D4318-standard test method for liquid limit, plastic limit, and plasticity index of soils.
Discussion:
In this test we found Liquid limit plastic limit for find plastic index and due this results we found type of our fine grained soil in this way:
Depending in USCS system we found that LL (35.33) <50% this mean our soil is low plasticity soil. And with this equation we find is our soil is silt or clay PI < (0.73(LL-20)) which PI (7.83) < (0.73(LL-20)) which PI<11.69 this mean our soil is silt so this explain to us that our soil is low plasticity silt ML (lean silt). Approximately we can say that we don’t have error in our test but for plastic limit test we repeated the trail for three times until the diameter of the soil same as diameter of the rod and produce crack however we can say there’s no error for our test.
Conclusion:
Attaberg limit is the test method which used for finding each of liquid limits due to our liquid limit curve which we draw it between water content and number of blows and we found plastic limit by taking water content average for each trail and by differencing LL and PL we found plastic index. And with this plastic index and liquid limit we classified our fine grain soil which is our result is low plasticity silt as we said in the discussion.
This document discusses various index properties of soil and methods for determining them. It describes determining the specific gravity of soil through different methods like the pycnometer bottle method. It also discusses determining the in-situ dry density of soil using a core cutter and discusses particle size analysis through sieve analysis and sedimentation analysis. The document also describes determining the consistency limits of fine-grained soils, including the liquid limit and plastic limit tests. It defines the relative density of soils and provides categories of soil denseness based on relative density percentages.
1) The document discusses methods for classifying soils through sieve analysis, liquid limit tests, and plastic limit tests. Sieve analysis is used to determine the grain size distribution of coarser soil particles, while hydrometer testing identifies finer particles.
2) The tests are used to classify soils based on properties like plasticity index and grain size distribution curve. This allows soils to be designated under specific categories in the Unified Soil Classification System.
3) Key measurements identified include D10, D30, D60 grain sizes, Cu and Cc values for grading, and liquid limit and plastic limit water contents for defining soil types.
This document discusses procedures for determining the liquid limit and plastic limit of fine-grained soils through laboratory tests. The liquid limit is defined as the minimum water content at which a soil pat will flow together over a distance of 13mm under 25 blows. The plastic limit is the minimum water content at which a 3mm thread of soil will just start cracking. Test results for a sample soil show a liquid limit of 26%, plastic limit of 15%, and plasticity index of 11%, identifying it as a low compressibility silty clay soil.
index properties of soil, Those properties of soil which are used in the identification and classification of soil are known as INDEX PROPERTIES
Water content
Specific gravity
In-situ density
Particle size
Consistency
Relative Density
The standard Proctor test is conducted to determine the optimum water content and maximum dry density of soil for compaction. Soil samples are compacted in layers in a standardized metal mold at different water contents using a rammer. The bulk density of each compacted sample is calculated and a curve is plotted of dry density versus water content. The water content corresponding to the highest dry density is the optimum water content. A penetration resistance test is also conducted using a Proctor needle to obtain the relationship between penetration resistance and water content.
The document provides instructions for determining various properties of soil samples through laboratory tests, including:
- Moisture content using the oven-dried method in 3 samples from depths of 1', 2', and 3'.
- Liquid limit using a liquid limit device by taking samples at different moisture contents and counting drops to close a groove.
- Plastic limit by rolling soil into 3mm threads until they crumble.
- Procedures are described for apparatus, calculations, and reporting results for each test. Precautions are provided to ensure accurate measurements.
The document describes a laboratory experiment to determine the permeability of a soil sample using the constant head permeability test method. Three trials were conducted on the sample, which had an average dry unit weight of 1.58 g/cm3 and void ratio of 0.646. The average coefficient of permeability from the trials was determined to be 0.050733 cm/sec, classifying the sample as coarse sand according to ASTM standards. Factors that influence permeability and potential sources of error in the experiment are also discussed.
The document provides details on various tests conducted on highway materials and soils, including aggregate impact value testing, water content determination, consistency limits testing, rebound hammer testing, and sand replacement testing. It describes the objectives, apparatus, procedures, observations, and calculations for each test. The tests are used to evaluate the properties and suitability of aggregates, soils, and concrete for use in highway and road construction projects.
Geo technical properties of soil by sajid hussainsajid hussain
This document provides an overview of foundational principles of soil mechanics. It discusses key topics including grain size distribution, plasticity, soil classification, effective stress, consolidation, and shear strength. Sieve analysis and hydrometer testing are described for determining grain size distribution of coarse-grained and fine-grained soils. Index properties like liquid limit, plastic limit, and plasticity index are also summarized. The concepts of total stress, pore water pressure, and effective stress are introduced. Finally, the process of consolidation, whereby excess pore pressures dissipate over time under increased loading, is explained.
This document describes laboratory tests to determine the Atterberg limits of a fine-grained soil sample. The liquid limit is the moisture content at which a soil pat will flow together over a distance of 13 mm after 25 shocks. The plastic limit is the moisture content at which a soil thread cannot be rolled to 3.2 mm without crumbling. Laboratory tests are performed to determine the liquid limit and plastic limit of a soil sample. The results, including the plasticity index, are used to classify soils.
This document describes a laboratory test procedure to determine the Atterberg limits of a fine-grained soil, which are used to classify soils. The test involves measuring the moisture content at which the soil transitions from a plastic to liquid state (liquid limit), and from a semi-solid to plastic state (plastic limit). Samples are tested at different moisture contents and the number of blows to close a groove are recorded to find the liquid limit. The plastic limit is found by rolling threads of soil at different moisture contents. The liquid limit, plastic limit, and plasticity index are calculated and used to classify the soil.
The document describes the process for determining the Atterberg limits of a soil sample, which are important measures of a soil's plasticity properties. The liquid limit is the water content at which a soil transitions from a plastic to liquid state, while the plastic limit is the minimum water content for a soil to exhibit plastic behavior. The test involves determining the water contents at which a soil sample exhibits these behaviors using standardized laboratory procedures and equipment like a liquid limit device. The results are used to classify soils and understand their engineering properties.
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1. WELCOME TO OUR
PRESENTATION
SUBMITTED TO
DR. MD. ZAINAL ABEDIN
PROFESSOR
DEPT. OF FARM STRUCTURE &
ENVIRONMENTAL
ENGINEERING
SUBMITTED BY
1605085
1605087
1605088
1605090
1605100
3. A. DETERMINATION OF THE LIQUID LIMIT
OF SOIL BY CASAGRANDE METHOD
Objectives: To determine the liquid limit of soil.
Theory:
The liquid limit is the water content at which the soil will flow under its
own weight. In liquid limit the soil behaves practically like a liquid, but
has small shear strength. It flows to close the groove is just 25 blows in
Casagrande’s liquid limit device. As it is difficult to get exactly 25 blows
in a test, 3 to 5 tests are being conducted, and the number of blows (N)
required in each test is determined. A semi-log plot is drawn between
log(N) and the water content (w). The liquid limit is the water content
corresponding to N = 25 blows, as obtained from the plot.
4. Apparatus Required:
1. Casagrande apparatus, 2. Grooving tools of both standard and
ASTM types, 3. Oven, 4. Spatula, 5. Evaporating dish or glass sheet,
6. 425 µ IS sieve, 7. Balance and 8. Wash bottle etc.
5. Methodology
1) The drop of the cup of the liquid limit device was adjusted
by releasing the two screws at the top and by using the
handle of the grooving tool or a gauge. The drop should be
exactly 1 cm at the point of contact on the base. The screw
was tightened after adjustment.
2) About 120gm of the air-dried soil sample passing 425 µ is
sieve was taken.
3) The sample was mixed thoroughly with distilled water in an
evaporating dish or a glass plate to form a uniform paste.
Mixing should be continued for about 15 to 30 minutes, till a
uniform mix was obtained.
4) The mix was kept under humid conditions for obtaining
uniform moisture distribution for sufficient period. For
some fat clay this maturing time may be up to 24 hours.
6. Methodology(cont.)
5) A portion of the matured paste was taken and remixed it thoroughly. It
was placed in the cup and leveled it by a spatula to have a maximum
depth of the soil as 1 cm at the point of the maximum thickness.
6) A groove was cut in the sample. The grooving tool was drawn through
the paste in the cup along the symmetrical axis, along the diameter
through the center line of the cam. The tools were held perpendicular
to the cup.
7) The handle of the device was turned at a rate of 2 revolutions per
second. The number of blows was counted until the two halves the
soils specimen come in contact at the bottom of the groove along a
distance of 12 mm due to flow and not by sliding.
8) A representative specimen of the soil was collected by moving spatula
width-wise from one edge to the other edge of the soil cake, at right-
angles to the groove. The specimen was placed in a container for
moisture content determination. The water content was determined.
7. Methodology(cont.)
9) The retaining soil was removed from the cup. It was mixed
with the soil left in the evaporating dish.
10) The water content of the mix was changed in the
evaporating dish, either by adding more water if the water
content was to be increased, or by kneading the soil, if the
water content was to be decreased. In no case, the dry soil
should be added to reduce the water content.
11) Steps 4 to 10 were repeated and the number of blows (N)
and the water content were determined in each case.
12) The flow curve between log(N) and w was drawn, and the
liquid limit corresponding to N = 25 blows was determined.
8. Fig: Liquid limit of soil by casagrande
method
Fig: Casagrande apparatus
9. Sl.
No.
Observations and Calculations
Replications
1 2 3 4 5
Observations
1. No. of blows (N) 32 30 24 20 16
2. Can No. 𝑹 𝟏 𝑹 𝟐 𝑹 𝟑 𝑹 𝟒 𝑹 𝟓
3. Weight of the empty Can (W1) 21.3 21.3 21.3 21.3 21.3
4. Weight of Can + Wet soil (W2) 28.7 32.0 24.3 32.0 25.7
5. Weight of Can + Dry soil (W3) 27.7 30.0 23.7 29.1 24.1
Calculation
6. Water content, 𝒙 =
𝑾 𝟐−𝑾 𝟑
𝑾 𝟑−𝑾 𝟏
× 𝟏𝟎𝟎 15.6 22.0 25.0 37.2 57.0
Data sheet
Result: At liquid limit ,water content was 29%
10. B. Determination of the Plastic Limit of
soil by Casagrande Method
Objectives:
To determine the plastic limit of a soil specimen
Theory:
The plastic limit of a soil is the water content of the soil below
which it ceases to be plastic. It begins to crumble when rolled
into threads of 3 mm diameter.
12. Methodology:
1. 30 gm of air-dried soil was taken from a thoroughly
mixed sample of the soil passing 425 sieve.
2. The soil was mixed with distilled water in on a glass
plate to make it plastic enough to shape into a small
ball.
3. The plastic soil mass was left for some time for
maturing.
4. About 8 gm of the plastic soil was taken and it was rolled
with fingers on a glass plate. The rate of the rolling
should be about 80 to 90 strokes per minutes to form a
thread of 3 mm diameter, counting one stroke when the
hand moves forward and backward to the starting point.
13. Methodology(cont.):
5. If the diameter of the thread becomes less than 3mm
without cracks, it shows that the water content is
more than the plastic limit. The soil was kneaded to
reduce the water content and it was rolled again into
thread.
6. The process of alternate rolling and kneading was
repeated until the thread crumbled, and the soil could
no longer be rolled into thread. The pieces of the
crumble soil thread was collected in a moisture
content container.
7. The procedure was repeated at least twice more with
fresh sample of plastic soil each time
14. Data sheet:
Sl.
No. Observations and Calculations
Replications
1 2 3 4 5
Observations
1. Can No. 𝑹 𝟏 𝑹 𝟐 𝑹 𝟑 𝑹 𝟒 𝑹 𝟓
2. Weight of the empty can, W1
21.3 21.3 21.3 21.3 21.3
3. Weight of Can + wet soil, W2
28.7 32.0 24.3 32.0 25.7
4. Weight of can + dry soil, W3
27.7 30.0 23.7 29.1 24.1
Calculation
5. Water content, 𝑥 =
𝑊2−𝑊3
𝑊3−𝑊1
× 100 15.6 22.0 25.0 37.2 57.0
Result: Average water content is 31.36%
15. C. Determination of the plastic and liquid limits of
soil by cone-penetrometer method
Objective:
To determine the cone-penetrometer plastic limit and liquid limit of
soil
Theory:
Cone penetrometer consists of a stainless steel cone having an apex
angle of 300
± 10
and a length of 35 mm. The cone is fixed at the
lower end of a sliding rod which is fitted with a disc at its top. The
total mass of the cone, sliding rod and the disc is 80𝑔𝑚 ± 0.05𝑔𝑚 . The
prepared soil paste is placed in a cup of 50 mm internal diameter and
50 mm height. The cup is placed below the cone and is allowed to
penetrate the soil for 5 seconds. If the penetration vs moisture content
curve is drawn, the water content at 20 mm penetration is the liquid
limit and the water content at minimum penetration is the plastic
limit.
16. Since it is difficult to obtain the penetration of 20 mm exactly, liquid limit
is determined from the equation given below
𝒘𝒍 =
𝒘 𝒚
𝟎. 𝟔𝟓 + 𝟎. 𝟎𝟏𝟕𝟓𝒚
Where, 𝑤𝑙 =liquid limit
y=penetration when water content is 𝑤 𝑦
𝑤 𝑦=water content when penetration y
Apparatus required:
1. Cone-penetrometer, 2.A cup of 50 mm internal diameter and 50 mm
height, 3. M.C. Can, 4. Balance, 5. Oven and 6. Spatula etc.
17. Methodology :
1. 500 gm of dried soil was taken in a glass plate and water was
put for make the paste.
2. The paste was kept for 30 minutes for maturing.
3. The cup of 50 mm internal diameter and 50 mm height was
filled with this paste so that there was no entrapped air. The
excess soil was removed and the cup surface was leveled.
4. The cup was placed below the cone penetrometer and the
cone was lowered gradually so as to just touch the surface of
the soil in the cup.
5. The graduated scale was adjusted as zero when cone touch the
cup surface.
6. The cone was released and penetration of soil was allowed for
5 seconds.
18. Methodology(cont.)
7. When the cone penetrated 20 mm exactly then soil sample was
taken for water content determination.
8. It is very difficult to get exactly 20 mm penetration, so the
penetration y was measured near 20 mm for the water content
wy. The process was repeated 4 to 10 times.
9. The liquid limit was calculated by using the equations.
10. In order to determine both the liquid and the plastic limits a
penetration vs moisture curve is drawn, the water content at 20
mm penetration is the liquid limit and the water content at
minimum penetration is the plastic limit.
19. Fig: Plastic and liquid limits of soil by
cone-penetrometer method
Fig: A cone penetrometer
20. Data sheet:
Sl.
No.
Observations and Calculations
Replications
1 2 3 4 5
Observations
1. Penetration, y 22.0 16.0 18.5 25.6 31.0
2. Weight of the empty can, W1 21.3 21.3 21.3 21.3 21.3
3. Weight of Can + wet soil, W2 27.9 31.0 28.7 24.3 32.0
4. Weight of can + dry soil, W3 27.6 30.1 27.7 23.7 29.1
Calculation
5. Water content,𝑤 𝑦 =
𝑊2−𝑊3
𝑊3−𝑊1
× 100
when penetration y mm
4.8 10 15.6 25.0 37.2
6. Liquid Limit,𝑤𝑙 =
𝑤 𝑦
0.65+0.0175𝑦
0.048 0.10 0.156 0.25 0.372
Result: From graph, we got water content 18% at liquid limit and 10% at
plastic limit
21. Precautions:
a) We have to use instruments very carefully.
b) All the measurement should be taken carefully.
c) Before using any instrument, we should know how
to use it.
d) After using the instrument, we should clean it.