DETERMINATION OF UNCONFINED COMPRESSIVE STRENGTH OF SOIL in Foundation Engineering
INTRODUCTION
TERMINOLOGY
APPARATUS
SOIL SPECIMEN & ITS TYPES
THEORY
RELEVANCE OF THE EXPERIMENT
PROCEDURE
VIDEO
OBSERVATION
DISCUSSION
REMARKS
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.
This document describes the vane shear test procedure used to determine the undrained shear strength of soft clays. Key details include:
- The test involves inserting vanes into an undisturbed clay specimen and rotating them at a uniform rate until failure to measure the undrained shear strength.
- Calculations are done to determine the shear strength from the torque measurement, using the vane diameter and height.
- The test can also measure soil sensitivity by remolding the soil after the initial test and measuring the reduction in strength.
For full course visit our website
https://www.machenlink.com/course/soil-mehcanics/
Description
Determine the unit weight of natural soil in place.
Stages
Determination of sand filling the cone
Determination bulk unit weight of sand
Determination bulk unit weight of natural soil
Procedure
Determining the weight of sand filling the cone
Sand passing through a 600µ sieve and retained over 300µ sieve is used.
Pouring cylinder attached over pouring cone is placed over level ground and completely filled with sand and weighed
The weight of sand + cylinder before pouring =푤_1
Now place the cylinder on the glass plate and open the shutter allow the sand to run out. Weigh the sand collected on the glass plate. This is the weight of sand filling pouring cone.
The weight of sand in pouring cone =푤_푐표푛푒
The weight of sand + cylinder after pouring on the glass =푤_2
The weight of sand in pouring cone =푤_푐표푛푒=푤_1−푤_2
Determination of bulk unit weight of sand
Determine the volume of the calibrated container (V)
Filled the pouring cylinder with weight 푤_1 again. Now placed over calibrating container and open the shutter, permit the sand to run into calibrating cylinder. When no further movement of sand is seen, close the shutter. Remove the pouring cylinder and weigh it.
The weight of sand + cylinder after pouring into calibrated cylinder =푤_3
The weight of sand filling calibrated cylinder (푤_푐푐 )=푤_1−(푤_푐표푛푒+푤_3 ")"
Determination of bulk unit weight of natural soil
Exposed about 45 cm square area of the soil and trim it down to a level surface.
Keep the metal tray on the level surface and excavate a circular hole of 10 cm diameter and 15 cm depth.
The weight of excavated soil =푤^′
Remove the tray, and placed the sand pouring cylinder over the hole, the cylinder should have sand of weight 푤_1.
Open the shutter and permit the sand to run into the hole. Close the shutter when no movement of the sand seen.
Remove the cylinder and weigh the sand pouring cylinder.
The weight of sand +cylinder after pouring into hole =푤_4
The weight of sand in the hole 〖(푤〗_ℎ표푙푒)=푤_1−(푤_4+푤_푐표푛푒)
For full course visit our website :
https://www.machenlink.com/course/foundation-engineering/
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Class 6 Shear Strength - Direct Shear Test ( Geotechnical Engineering )Hossam Shafiq I
This document describes the direct shear test procedure used in a geotechnical engineering laboratory class to determine the shear strength parameters of soils. It discusses how the direct shear test is conducted by applying a normal stress and increasing shear stress to a soil sample until failure. Key steps of the test procedure are outlined, and the document explains how shear strength parameters like cohesion (C') and the internal friction angle (f) can be calculated from the test results and plotted on a Mohr-Coulomb failure envelope graph.
1. Plate load tests are conducted to determine the ultimate bearing capacity of soil and settlement under a given load by applying loads to circular or square steel plates embedded in an excavated pit.
2. The test setup involves excavating a pit below the depth of the proposed foundation, placing the test plate with a central hole at the bottom, and applying load using a hydraulic jack while measuring settlement.
3. The results provide the subgrade modulus, ultimate bearing capacity divided by a safety factor to determine the safe bearing capacity, and insight into foundation behavior and allowable settlement for design.
The document summarizes a laboratory vane shear test conducted to determine the undrained shear strength of a cohesive soil sample composed of 70% bentonite and 30% kaolinite. Two soil specimens were tested to obtain the undrained shear strength in both the undisturbed and remolded conditions. The vane shear apparatus and testing procedures are described. Test results including moisture content, bulk density, dry density, degree of saturation, and undrained shear strength are presented in a data table. The assumptions and applications of the vane shear test are discussed.
This slide will help you to determine the immediate settlement for flexible foundation i.e. isolate footing and rigid foundation i.e. matt or raft foundation. To be more clear about the topic a numerical problem with the solution is given.
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.
This document describes the vane shear test procedure used to determine the undrained shear strength of soft clays. Key details include:
- The test involves inserting vanes into an undisturbed clay specimen and rotating them at a uniform rate until failure to measure the undrained shear strength.
- Calculations are done to determine the shear strength from the torque measurement, using the vane diameter and height.
- The test can also measure soil sensitivity by remolding the soil after the initial test and measuring the reduction in strength.
For full course visit our website
https://www.machenlink.com/course/soil-mehcanics/
Description
Determine the unit weight of natural soil in place.
Stages
Determination of sand filling the cone
Determination bulk unit weight of sand
Determination bulk unit weight of natural soil
Procedure
Determining the weight of sand filling the cone
Sand passing through a 600µ sieve and retained over 300µ sieve is used.
Pouring cylinder attached over pouring cone is placed over level ground and completely filled with sand and weighed
The weight of sand + cylinder before pouring =푤_1
Now place the cylinder on the glass plate and open the shutter allow the sand to run out. Weigh the sand collected on the glass plate. This is the weight of sand filling pouring cone.
The weight of sand in pouring cone =푤_푐표푛푒
The weight of sand + cylinder after pouring on the glass =푤_2
The weight of sand in pouring cone =푤_푐표푛푒=푤_1−푤_2
Determination of bulk unit weight of sand
Determine the volume of the calibrated container (V)
Filled the pouring cylinder with weight 푤_1 again. Now placed over calibrating container and open the shutter, permit the sand to run into calibrating cylinder. When no further movement of sand is seen, close the shutter. Remove the pouring cylinder and weigh it.
The weight of sand + cylinder after pouring into calibrated cylinder =푤_3
The weight of sand filling calibrated cylinder (푤_푐푐 )=푤_1−(푤_푐표푛푒+푤_3 ")"
Determination of bulk unit weight of natural soil
Exposed about 45 cm square area of the soil and trim it down to a level surface.
Keep the metal tray on the level surface and excavate a circular hole of 10 cm diameter and 15 cm depth.
The weight of excavated soil =푤^′
Remove the tray, and placed the sand pouring cylinder over the hole, the cylinder should have sand of weight 푤_1.
Open the shutter and permit the sand to run into the hole. Close the shutter when no movement of the sand seen.
Remove the cylinder and weigh the sand pouring cylinder.
The weight of sand +cylinder after pouring into hole =푤_4
The weight of sand in the hole 〖(푤〗_ℎ표푙푒)=푤_1−(푤_4+푤_푐표푛푒)
For full course visit our website :
https://www.machenlink.com/course/foundation-engineering/
Follow #MachenLink
Facebook: https://www.facebook.com/machenLink/
Linkedin: https://www.linkedin.com/company/machenlink/
Twitter: https://twitter.com/MachenLink
Class 6 Shear Strength - Direct Shear Test ( Geotechnical Engineering )Hossam Shafiq I
This document describes the direct shear test procedure used in a geotechnical engineering laboratory class to determine the shear strength parameters of soils. It discusses how the direct shear test is conducted by applying a normal stress and increasing shear stress to a soil sample until failure. Key steps of the test procedure are outlined, and the document explains how shear strength parameters like cohesion (C') and the internal friction angle (f) can be calculated from the test results and plotted on a Mohr-Coulomb failure envelope graph.
1. Plate load tests are conducted to determine the ultimate bearing capacity of soil and settlement under a given load by applying loads to circular or square steel plates embedded in an excavated pit.
2. The test setup involves excavating a pit below the depth of the proposed foundation, placing the test plate with a central hole at the bottom, and applying load using a hydraulic jack while measuring settlement.
3. The results provide the subgrade modulus, ultimate bearing capacity divided by a safety factor to determine the safe bearing capacity, and insight into foundation behavior and allowable settlement for design.
The document summarizes a laboratory vane shear test conducted to determine the undrained shear strength of a cohesive soil sample composed of 70% bentonite and 30% kaolinite. Two soil specimens were tested to obtain the undrained shear strength in both the undisturbed and remolded conditions. The vane shear apparatus and testing procedures are described. Test results including moisture content, bulk density, dry density, degree of saturation, and undrained shear strength are presented in a data table. The assumptions and applications of the vane shear test are discussed.
This slide will help you to determine the immediate settlement for flexible foundation i.e. isolate footing and rigid foundation i.e. matt or raft foundation. To be more clear about the topic a numerical problem with the solution is given.
The document provides information about shear strength of soil. It defines shear strength and its components of cohesion and internal friction. It discusses Mohr's circle of stress and Mohr-Coulomb theory for shear strength. The types of soil are classified based on drainage conditions during shear testing. Common shear strength tests like direct shear test, triaxial test, unconfined compression test and vane shear test are also explained. Sample calculations for shear strength determination from test results are presented.
1. The document discusses consolidation in soils, including terminology, oedometer tests, preconsolidation pressure, and Terzaghi's theory of one-dimensional consolidation.
2. Key points include that consolidation is the decrease in soil volume due to increased loading, and includes primary consolidation through pore water expulsion and secondary consolidation via soil molecule rearrangement.
3. Oedometer tests are used to determine soil compressibility and preconsolidation pressure, the maximum past effective stress.
4. Terzaghi's theory assumes consolidation is one-dimensional, and that excess pore pressures dissipate over time according to a consolidation equation.
Class notes of Geotechnical Engineering course I used to teach at UET Lahore. Feel free to download the slide show.
Anyone looking to modify these files and use them for their own teaching purposes can contact me directly to get hold of editable version.
This document provides information on the standard penetration test (SPT), including the instruments, procedures, corrections, and applications. It describes that the SPT is commonly used to evaluate the in-situ properties of cohesionless soils. The key instruments are a split spoon sampler, drive-weight assembly with a 63.5 kg hammer, and cathead. The procedure involves drilling a borehole, driving the sampler with the hammer, and recording the number of blows to penetrate each 15 cm interval. Corrections are made to account for overburden pressure, dilatancy effects, and hammer energy efficiency. The SPT provides useful correlations to estimate properties like relative density, friction angle, and strength.
Consolidation is the process where water drains from saturated soil pores, transferring the load from water to soil particles and causing volume change. There are three types of consolidation: immediate, primary, and secondary. One-dimensional consolidation assumes vertical drainage, making the process primarily vertical. Terzaghi's theory of one-dimensional consolidation models this using parameters like permeability, compressibility, and effective stress. The coefficient of consolidation describes the rate of compression, while compression and swelling indices characterize the void ratio-effective stress relationship. The oedometer test experimentally determines consolidation properties from soil specimen compression under incremental loads.
The document describes the California Bearing Ratio (CBR) test procedure used to evaluate the strength of subgrade soils and base courses for pavement design. The CBR test involves compacting a soil sample and measuring the penetration resistance under a constant load over time. Higher CBR values indicate stronger soils that require less thick pavement sections. The document provides details on the test apparatus, sample preparation, soaking, loading and penetration measurements, and CBR calculations according to relevant Indian standards.
CNS layer (usefulsearch.org) (useful search) Make Mannan
A cohesive non-swelling (CNS) soil layer can be used to control swelling in expansive soils below structures. CNS soils are cohesive with low plasticity and contain non-swelling clay minerals. They exhibit little to no swelling when moisture changes and provide an environment that inhibits swelling in underlying expansive soils. Guidelines provided specify acceptable ranges for gradation, swelling pressure (≤10kN/m^2), cohesion (≥10kN/m^2), and consistency limits (LL 30-50%, PI 15-30%) for soils to qualify as CNS materials. Thickness of the CNS layer depends on the swelling pressure of the underlying soil.
1. Load-settlement curves for footings on dense sand or stiff clay show a pronounced peak and failure occurs at very small strains, with sudden sinking or tilting and surface heaving of adjoining soil.
2. For medium sand or clay, failure starts at a localized spot and migrates outward gradually, with large vertical strains and small lateral strains. Failure planes are not clearly defined.
3. Failure zones for footings on slopes do not extend above the horizontal plane through the base, and failure occurs when downward and upward pressures are equal.
Bearing capacity of shallow foundations by abhishek sharma ABHISHEK SHARMA
elements you should know about bearing capacity of shallow foundations are included in it. various indian standards are also used. Bearing capacity theories by various researchers are also included. numericals from GATE CE and ESE CE are also included.
This document discusses the consolidation of soil. It defines important terms like compression, compressibility, and consolidation. It outlines the differences between compaction and consolidation. The importance of consolidation theory is that it provides information on total settlement, time for settlement, and types of settlement. Terzaghi's spring analogy is described to explain the consolidation process. A one-dimensional consolidation test procedure is outlined. Important definitions related to consolidation like compression index, swelling index, and coefficients are provided. The document also discusses normally, under, and over consolidated soils and how to determine preconsolidation pressure. Terzaghi's one-dimensional consolidation theory and solution are presented. Methods to determine degree of consolidation and coefficient of consolidation from laboratory test data are
The California Bearing Ratio (CBR) test measures the bearing capacity of a soil by determining the ratio of the force required to penetrate a soil mass with a standard plunger to that of a standard material. It is used to classify and evaluate soils for flexible pavement subgrades and bases. The procedure involves compacting a soil sample, soaking it for 4 days, and then applying a load through a plunger at a rate of 1.25 mm/min while measuring penetration. Load readings are recorded and used to calculate the CBR value based on standard pressures at 2.5 and 5.0 mm penetrations.
Determination of Field Density Using Sand Cone Method | Jameel AcademyJameel Academy
The document describes a soil mechanics lab report on determining field density using the sand cone method. The test procedure involves digging a hole, placing the excavated soil in an airtight bag, then using a sand cone apparatus to pour sand into the hole to determine the hole's volume. Calculations are shown to find the field dry unit weight, water content, and relative density compared to the maximum dry unit weight from a lab compaction test. The results found a field dry unit weight of 1.4149 g/cm3 and relative density of 72%, indicating the field compaction was not adequate for the project.
- Soils fail primarily in shear when the shear stress along a failure plane reaches the soil's shear strength.
- The shear strength of soils is governed by the Mohr-Coulomb failure criterion, which consists of cohesive and frictional components that depend on effective stresses.
- Laboratory tests like direct shear and triaxial tests are used to measure the shear strength parameters (c, φ) of soils by simulating the in-situ stress conditions.
The document summarizes the standard penetration test (SPT), a common in situ geotechnical testing method. It describes the basic procedure, which involves driving a split spoon sampler into subsurface soils using a hammer, and recording the number of blows required for each increment of penetration. Corrections are made to SPT values to account for overburden pressure and dilatancy. Empirical correlations are presented relating SPT values to properties like density, shear strength, and consistency of cohesionless and cohesive soils. Both advantages like being inexpensive and quick, and limitations like lack of precision are discussed.
The standard penetration test (SPT) involves driving a split spoon sampler into the ground using a 140 lb hammer dropped 30 inches. The number of blows required to penetrate each 6 inch interval is recorded, and the penetration resistance value N is the sum of the blows over the second and third intervals. This test is commonly used to obtain bearing capacity and estimate soil properties like density and shear strength. It is performed whenever the soil stratum changes and at intervals of no more than 1.5 meters.
This document describes the procedure for conducting a direct shear test to determine the shear strength parameters (cohesion and angle of internal friction) of a soil sample. In a direct shear test, a soil sample in a shear box is subjected to increasing normal stresses and shear stresses are applied until failure. Shear stress and displacement measurements are recorded to calculate shear strength. The test is conducted under both consolidated and unconsolidated conditions. Shear strength parameters obtained from multiple tests at different normal stresses are used to calculate cohesion and angle of internal friction from a shear strength graph.
FIELD TEST FOR BEARING CAPACITY-revised for BC.pptxsbarai0802
This document discusses various field tests used to determine bearing capacity of soils, including the standard penetration test (SPT), plate load test, cone penetration test (CPT), and pressure meter test. The SPT involves driving a split spoon sampler into the ground using a hammer and measuring the blow counts, while corrections are applied to the observed value. The plate load test applies incremental loads to a steel plate in a pit until a maximum settlement is reached to determine ultimate bearing capacity. The CPT provides continuous measurements of cone resistance with depth to assess soil properties. The pressure meter test measures volume changes in a probe under increasing gas pressure to identify elastic and plastic soil behavior.
The document provides information about shear strength of soil. It defines shear strength and its components of cohesion and internal friction. It discusses Mohr's circle of stress and Mohr-Coulomb theory for shear strength. The types of soil are classified based on drainage conditions during shear testing. Common shear strength tests like direct shear test, triaxial test, unconfined compression test and vane shear test are also explained. Sample calculations for shear strength determination from test results are presented.
1. The document discusses consolidation in soils, including terminology, oedometer tests, preconsolidation pressure, and Terzaghi's theory of one-dimensional consolidation.
2. Key points include that consolidation is the decrease in soil volume due to increased loading, and includes primary consolidation through pore water expulsion and secondary consolidation via soil molecule rearrangement.
3. Oedometer tests are used to determine soil compressibility and preconsolidation pressure, the maximum past effective stress.
4. Terzaghi's theory assumes consolidation is one-dimensional, and that excess pore pressures dissipate over time according to a consolidation equation.
Class notes of Geotechnical Engineering course I used to teach at UET Lahore. Feel free to download the slide show.
Anyone looking to modify these files and use them for their own teaching purposes can contact me directly to get hold of editable version.
This document provides information on the standard penetration test (SPT), including the instruments, procedures, corrections, and applications. It describes that the SPT is commonly used to evaluate the in-situ properties of cohesionless soils. The key instruments are a split spoon sampler, drive-weight assembly with a 63.5 kg hammer, and cathead. The procedure involves drilling a borehole, driving the sampler with the hammer, and recording the number of blows to penetrate each 15 cm interval. Corrections are made to account for overburden pressure, dilatancy effects, and hammer energy efficiency. The SPT provides useful correlations to estimate properties like relative density, friction angle, and strength.
Consolidation is the process where water drains from saturated soil pores, transferring the load from water to soil particles and causing volume change. There are three types of consolidation: immediate, primary, and secondary. One-dimensional consolidation assumes vertical drainage, making the process primarily vertical. Terzaghi's theory of one-dimensional consolidation models this using parameters like permeability, compressibility, and effective stress. The coefficient of consolidation describes the rate of compression, while compression and swelling indices characterize the void ratio-effective stress relationship. The oedometer test experimentally determines consolidation properties from soil specimen compression under incremental loads.
The document describes the California Bearing Ratio (CBR) test procedure used to evaluate the strength of subgrade soils and base courses for pavement design. The CBR test involves compacting a soil sample and measuring the penetration resistance under a constant load over time. Higher CBR values indicate stronger soils that require less thick pavement sections. The document provides details on the test apparatus, sample preparation, soaking, loading and penetration measurements, and CBR calculations according to relevant Indian standards.
CNS layer (usefulsearch.org) (useful search) Make Mannan
A cohesive non-swelling (CNS) soil layer can be used to control swelling in expansive soils below structures. CNS soils are cohesive with low plasticity and contain non-swelling clay minerals. They exhibit little to no swelling when moisture changes and provide an environment that inhibits swelling in underlying expansive soils. Guidelines provided specify acceptable ranges for gradation, swelling pressure (≤10kN/m^2), cohesion (≥10kN/m^2), and consistency limits (LL 30-50%, PI 15-30%) for soils to qualify as CNS materials. Thickness of the CNS layer depends on the swelling pressure of the underlying soil.
1. Load-settlement curves for footings on dense sand or stiff clay show a pronounced peak and failure occurs at very small strains, with sudden sinking or tilting and surface heaving of adjoining soil.
2. For medium sand or clay, failure starts at a localized spot and migrates outward gradually, with large vertical strains and small lateral strains. Failure planes are not clearly defined.
3. Failure zones for footings on slopes do not extend above the horizontal plane through the base, and failure occurs when downward and upward pressures are equal.
Bearing capacity of shallow foundations by abhishek sharma ABHISHEK SHARMA
elements you should know about bearing capacity of shallow foundations are included in it. various indian standards are also used. Bearing capacity theories by various researchers are also included. numericals from GATE CE and ESE CE are also included.
This document discusses the consolidation of soil. It defines important terms like compression, compressibility, and consolidation. It outlines the differences between compaction and consolidation. The importance of consolidation theory is that it provides information on total settlement, time for settlement, and types of settlement. Terzaghi's spring analogy is described to explain the consolidation process. A one-dimensional consolidation test procedure is outlined. Important definitions related to consolidation like compression index, swelling index, and coefficients are provided. The document also discusses normally, under, and over consolidated soils and how to determine preconsolidation pressure. Terzaghi's one-dimensional consolidation theory and solution are presented. Methods to determine degree of consolidation and coefficient of consolidation from laboratory test data are
The California Bearing Ratio (CBR) test measures the bearing capacity of a soil by determining the ratio of the force required to penetrate a soil mass with a standard plunger to that of a standard material. It is used to classify and evaluate soils for flexible pavement subgrades and bases. The procedure involves compacting a soil sample, soaking it for 4 days, and then applying a load through a plunger at a rate of 1.25 mm/min while measuring penetration. Load readings are recorded and used to calculate the CBR value based on standard pressures at 2.5 and 5.0 mm penetrations.
Determination of Field Density Using Sand Cone Method | Jameel AcademyJameel Academy
The document describes a soil mechanics lab report on determining field density using the sand cone method. The test procedure involves digging a hole, placing the excavated soil in an airtight bag, then using a sand cone apparatus to pour sand into the hole to determine the hole's volume. Calculations are shown to find the field dry unit weight, water content, and relative density compared to the maximum dry unit weight from a lab compaction test. The results found a field dry unit weight of 1.4149 g/cm3 and relative density of 72%, indicating the field compaction was not adequate for the project.
- Soils fail primarily in shear when the shear stress along a failure plane reaches the soil's shear strength.
- The shear strength of soils is governed by the Mohr-Coulomb failure criterion, which consists of cohesive and frictional components that depend on effective stresses.
- Laboratory tests like direct shear and triaxial tests are used to measure the shear strength parameters (c, φ) of soils by simulating the in-situ stress conditions.
The document summarizes the standard penetration test (SPT), a common in situ geotechnical testing method. It describes the basic procedure, which involves driving a split spoon sampler into subsurface soils using a hammer, and recording the number of blows required for each increment of penetration. Corrections are made to SPT values to account for overburden pressure and dilatancy. Empirical correlations are presented relating SPT values to properties like density, shear strength, and consistency of cohesionless and cohesive soils. Both advantages like being inexpensive and quick, and limitations like lack of precision are discussed.
The standard penetration test (SPT) involves driving a split spoon sampler into the ground using a 140 lb hammer dropped 30 inches. The number of blows required to penetrate each 6 inch interval is recorded, and the penetration resistance value N is the sum of the blows over the second and third intervals. This test is commonly used to obtain bearing capacity and estimate soil properties like density and shear strength. It is performed whenever the soil stratum changes and at intervals of no more than 1.5 meters.
This document describes the procedure for conducting a direct shear test to determine the shear strength parameters (cohesion and angle of internal friction) of a soil sample. In a direct shear test, a soil sample in a shear box is subjected to increasing normal stresses and shear stresses are applied until failure. Shear stress and displacement measurements are recorded to calculate shear strength. The test is conducted under both consolidated and unconsolidated conditions. Shear strength parameters obtained from multiple tests at different normal stresses are used to calculate cohesion and angle of internal friction from a shear strength graph.
FIELD TEST FOR BEARING CAPACITY-revised for BC.pptxsbarai0802
This document discusses various field tests used to determine bearing capacity of soils, including the standard penetration test (SPT), plate load test, cone penetration test (CPT), and pressure meter test. The SPT involves driving a split spoon sampler into the ground using a hammer and measuring the blow counts, while corrections are applied to the observed value. The plate load test applies incremental loads to a steel plate in a pit until a maximum settlement is reached to determine ultimate bearing capacity. The CPT provides continuous measurements of cone resistance with depth to assess soil properties. The pressure meter test measures volume changes in a probe under increasing gas pressure to identify elastic and plastic soil behavior.
This experiment aims to determine the undrained shear strength of remolded cohesive soil using a vane shear test. The vane shear test involves pushing a four-bladed vane into a soil sample and rotating it until shear failure occurs along a cylindrical surface. The torque required to cause failure is measured and converted to a unit shear resistance. This test is suitable for soft soils where other shear tests may not work accurately, and it can be used to find both the undisturbed and remolded shear strengths to estimate soil sensitivity. The procedure involves filling a container with soil at a set density and water content, inserting the vane, and rotating it until failure while recording the applied torque and calculated shear strength.
This document summarizes in-situ methods for determining soil properties, specifically the vane shear test and pressure meter tests.
The vane shear test directly measures the undrained shear strength of soft clays in the field by inserting a rotating vane and measuring the torque. Pressure meter tests measure the soil's stress-strain response by expanding a membrane probe against the soil and recording the resulting pressures and strains. Self-boring pressure meters can test undisturbed soil by drilling into the ground, while displacement pressure meters push into pre-drilled boreholes. Both provide fundamental soil properties with minimal empirical corrections needed.
The document provides details on laboratory tests performed on cement and aggregates to determine their quality parameters. It describes procedures for determining the compressive strength, fineness, and setting time of cement. It also outlines tests to find the water absorption, impact value, abrasion value, flakiness index, and elongation index of aggregates used in construction. The tests are conducted according to Indian standards and provide important information about the strength and properties of materials used.
The Standard Penetration Test (SPT) involves driving a thick-walled sampler into the ground using blows from a hammer. The number of blows required for each 150mm of penetration is recorded. Higher blow counts indicate denser soil. SPT results provide an indication of soil strength properties and relative density, especially in granular soils where undisturbed samples are difficult to obtain. However, SPT results have limitations as the test can disturb soils and the blow count data has low resolution. Correlations are used to interpret SPT results but depend on soil type.
Bearing ratio capacity of compacted soilameresmail92
This document describes the standard test method for determining the California Bearing Ratio (CBR) of laboratory-compacted soils. The CBR test measures the bearing capacity of a soil by penetrating a piston into a compacted soil sample and measuring the resistance. There are two main compaction methods - static and dynamic - and the document outlines the detailed procedures for compacting soil samples using each method and then soaking and testing the samples to determine the CBR value. The CBR test is used to evaluate the strength of materials like subgrade, subbase and base course materials for roads and airfields.
This document provides information on preparing rock samples for laboratory testing. It discusses collecting core samples from the field and storing them properly to avoid contamination. It describes equipment for cutting, grinding, and polishing samples in the laboratory. Standard sizes for core drill bits and criteria for sample straightness, flatness, perpendicularity, and length to diameter ratios are presented. Proper preparation of representative rock samples is important for obtaining accurate test results on rock properties like strength and deformability.
This document outlines procedures for performing an unconfined compression test to determine the shear strength of cohesive soils. It describes the objectives of the test as measuring the shearing resistance and shear strength parameters (c and φ) of undisturbed or remolded cohesive soil specimens. The theory section explains that the unconfined compressive strength is the load per unit area at which a soil cylinder fails in compression and is used to calculate the soil's undrained shear strength as one half the unconfined compressive strength. The document provides details on required equipment, procedures for specimen preparation and testing, methods for data analysis and calculation of stress and strain, and conclusions regarding determination of unconfined compressive strength and undrained
The document summarizes various methods used to analyze soil properties for highway construction projects. It describes procedures for sieve analysis, liquid limit testing, plastic limit testing, and other methods to determine characteristics like density, bearing capacity, and moisture content that are used in designing roadway foundations and pavements. Preliminary soil surveys are also outlined to identify soil types and conditions along proposed routes to inform design and construction decisions.
This document provides details on performing a one-dimensional consolidation test to determine the consolidation properties of a saturated soil specimen. It describes the apparatus needed, including a consolidation ring, porous plates, loading device, and compression gauge. The procedure involves preparing an undisturbed soil specimen between the porous plates, incrementally increasing the load and recording compression vs the square root of time to generate consolidation curves. The test is run through multiple loading stages to pressures above expected in-situ stresses to determine the soil's coefficient of consolidation and pre-consolidation pressure.
1) The experiment determines the unconfined compressive strength (qu) of soil, which is the maximum load per unit area at which an unconfined cylindrical soil specimen fails during compression testing.
2) A cylindrical soil specimen is prepared at optimum moisture content and maximum dry density, and compressed axially between loading plates at a controlled strain rate while measuring load and deformation.
3) The stress-strain curve is plotted, and qu is taken as either the peak stress or stress at 20% axial strain. Shear strength S of the soil is then calculated as qu/2, assuming the soil's angle of shearing resistance φ is 0.
This document outlines the procedure for determining the California Bearing Ratio (CBR) of soils in a laboratory. The CBR is a measure of how much load a soil can support before failing. The procedure involves compacting soil specimens using static or dynamic methods, soaking them for 96 hours, and then penetrating the specimens with a piston at a rate of 1.25mm/min while measuring the load. The CBR is calculated based on the load-penetration curve and indicates the soil's strength and ability to support pavement structures.
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DETERMINATION OF UNCONFINED COMPRESSIVE STRENGTH OF SOIL
1. DETERMINATION OF
UNCONFINED COMPRESSIVE
STRENGTH OF SOIL
ASHISH NAYYAR(CO18212)
JAPTYESH SINGH(CO18229)
JOBANPREET SINGH(CO18232)
NISCHAY SINGH(CO18237)
RATTANBIR SINGH(CO18243)
SARTHAK PUNJ(CO18248)
in FOUNDATION ENGINEERING
Submitted to:
MOHAMMAD SAKIB PERWEZ KHAN SIR
2. INDEX
INTRODUCTION
TERMINOLOGY
APPARATUS
SOIL SPECIMEN & ITS TYPES
THEORY
RELEVANCE OF THE EXPERIMENT
PROCEDURE
VIDEO
OBSERVATION
DISCUSSION
REMARKS
3. INTRODUCTION
[as per IS code 2720(Part X) ]
The maximum load that can be transmitted to the subsoil by a foundation
depends upon the resistance of underlying soil to the shearing deformation
and compressibility. An axial load is applied at a constant rate of strain
without any lateral support to the soil specimen and is increased until failure
occurs.
The compressive load per unit area required to fail the soil specimen under
such conditions is called the unconfined compressive strength of the soil.
This test is applicable for determining strength of cohesive soils.
In this presentation we shall demonstrate the unconfined compressive test as
per IS code 2720 Part 10.
4. TERMINOLOGY
For the purpose of this standard, the following definitions shall
apply: -
Unconfined Compressive Strength, qu, it is the load per unit area at which
an unconfined cylindrical specimen of soil will fail in the. axial compression
test.
If the axial compression force per unit area has not reached a maximum
value even at 20 % axial strain, qu shall be taken as the value obtained at
20% axial strain.
6. APPARATUS USED
1. Unconfined Compression apparatus,
a) to apply compressive load at constant rate of strain
Can be any of the following: (provided All these loading devices shall have sufficient capacity and strain
control.)
Platform weighing scale equipped with a screw-jack activated yoke
Hydraulic loading device;
Screw jack with a proving ring; and
Any other loading device.
b) loading frame.
c) Also includes gear for different loading.
2. proving ring type
a) with Proving capacity 1 KN
For relatively weak soil with qu less than 100 KPa (1 kg/cm2) load shall be measurable to 1 KPa (0.1 kg/cm2).
For soils with qu equal to or greater than 100 KPa (1 kg/cm2) load shall be measurable to the nearest 5 KPa
(0.05 kg/cm2). The calibration of the proving ring shall be checked frequently, at least once a year.
7. 3. Dial gauge
Axial deformation of the sample shall be measured with a dial gauge having a least count of 0.01 mm
and travel to permit not less than 20 percent axial strain.
4 Bearing plates
Instrumented by clutch with help of electric motor
5. Weighing balance
Suitable for weighing soil specimens specially. Specimens of less than 100 g shall be weighed to the nearest
0.01 g whereas specimens of 100 g or larger shall be weighed to the nearest 0.1 g.
6. Oven
Thermostatically controlled, with interior of noncorroding material capable of maintaining the temperature at
110°C + - 5°C
7. Stopwatch
Timing device to indicate the elapsed testing time to the nearest second may be used for establishing the rate
of strain.
8. 8. Split mould (38 mm diameter, 76 mm long)
9. Vernier Calliper
•Suitable to measure physical dimensions of the test specimen to the nearest O-1 mm.
10. Sampling Equipment
•Sampling Tube
•Sample extractor
11. Miscellaneous Equipment
•Specimen trimming and carving tools,
•remoulding apparatus,
•Large mould
•Knife
•water content cans,
•data sheets, etc, as required.
•Grease or oil
9. SOIL SPECIMEN
The soil specimen to be used for test shall be
depend on the purpose for which it is tested and
may be compacted, moulded or undisturbed.
10. SPECIMEN SIZE
The specimen for test shall have a minimum
diameter of 38 mm and the largest particle
contained within.
The test specimen shall be smaller than 1/8 th of
the specimen diameter.
If after completion of test on undisturbed sample,
it is found that larger particles than permitted for
the particular specimen size tested are present.
The height to diameter ratio shall be within 2 to
2.5.
• Measurements of height and diameter shall
be made with Vernier callipers or any other
suitable measuring device to the nearest 0.1
mm.
12. UNDISTURBED SPECIMEN
Undisturbed specimens shall be prepared from large undisturbed
samples.
Undisturbed sample shall be prepared from the drive sampling tube.
The ejecting device shall be capable of ejecting the soil core from
the sampling tube within the same direction of travel during which
the sample entered the tube and with negligible disturbance of the
sample. Conditions at the time of removal of the sample may dictate
the direction of removal but the principle concern should be to stay
the degree disturbance negligible.
NOTES:
Three specimens obtained by trimming and carving from
undisturbed soil samples shall be tested.
When the sample is ejected horizontally, a curved plate
may be provided to butt against the sampling tube such
that the ejected specimen slips over it freely, This will avoid
bending of the specimen and facilitate bringing specimen
to vertical position in many cases.
13. The specimen shall be handled carefully to stop disturbance, change in cross section or loss of
water. If any type of disturbance is likely to be caused by the ejection device the sample tube shall
be split lengthwise or be cut off in small sections, to facilitate removal of the specimen without
disturbance.
The specimen shall be of uniform circular cross-section with ends perpendicular to the axis of the
specimen.
Specimen of required size could also be carved from large undisturbed specimens.
Tube specimen may be tested without trimming except for squaring of ends
Where the prevention of the possible development of applicable capillary forces is required the
specimens shall be sealed with rubber membranes, thin plastic coatings or with coating of grease
or sprayed plastic immediately after plastic immediately after preparation and through the whole
testing cycle.
Representative sample cuttings taken from the tested specimen shall be used for determination
of water content.
14. REMOULDED SPECIMEN
The specimen could also be prepared either from a failed undisturbed specimen or from a
disturbed soil sample. Just in case of failed undisturbed specimen, the fabric shall be wrapped
during a thin rubber membrane and thoroughly worked with the fingers to assume complete
remoulding. Care shall be taken to avoid entrapped air, to get uniform density, to remould to
an equivalent void ratio as that of undisturbed specimen and to preserve the natural water
content of the soil.
15. COMPACTED SPECIMEN
When compacting disturbed material, it shall be
done employing a mould of circular cross
section. Compacted specimen could also be
prepared at any predetermined water content
and density.
After the specimen is made, the ends shall be
trimmed perpendicular to the long axis and
faraway from the mould. Representative sample
cuttings shall be obtained or the whole specimen
shall be used for the determination of water
content after the test.
16. THEORY
The load per unit
area at which a
cylindrical specimen
of a cohesive soil fails
fails in compression
is called UCS (qu).
qu = P/A
where P = axial load
at failure
A = Corrected area
= A0/ (1-Ε),
where A0 is the initial
cross-sectional area
of the specimen,
Ε = axial strain =
(Change in length)/
(Original Length)
The undrained shear
strength (Su) of the
soil is equal to one
half of the UCS i.e.
Su = qu / 2.
17. RELEVANCE OF THE EXPERIMENT
To determine the shear strength of a soil triaxial shear test is
conducted. Also, it’s quick and straightforward to perform.
The consistency of clay is often determined using the worth
of unconfined compressive strength of soil.
This should be evaluated as unconfined compression test is
inappropriate for dry sands or crumble clays because the
materials would disintegrate without some land of lateral
confinement.
Shear strength of a soil the foremost important engineering
property. To settle on the simplest material for the
embankment, one has got to conduct strength tests on the
samples selected.
If it’s not evaluated then it’ll be needed to conduct the
bearing capacity test within the field which isn’t always
possible.
Sl
No.
Consistency of
Clay
Unconfined Compressive Strength (KN/m2)
1 Very Soft < = 25
2 Soft 25 – 50
3 Medium 50 – 100
4 Stiff 100 – 200
5 Very Stiff 200 – 400
6 Hard > = 400
18. PROCEDURE
The soil specimen is prepared at the desired water
content and density in the large mould.
The sampling tube into the large mould is pushed
and the sampling tube which is filled with the soil is
removed.
The soil sample in the sampling tube is saturated.
The split mould is lightly coated with a thin layer of
grease.
The sample is extracted out of the sampling tube
by a suitable method into the split mould, using
the sample extractor and the knife.
The two ends of the specimen are trimmed off in
the split mould.
The mould with the specimen is weighed.
The specimen is removed from the split mould by
splitting the mould into two parts.
19. PROCEDURE
The length and diameter of the specimen is
measured with Vernier callipers.
The specimen is placed on the bottom plate of the
compression machine.
The upper plate is adjusted to make contact with the
specimen.
The dial gauge and the proving ring gauge is
adjusted to zero.
The compression load is applied to cause an axial
strain at the rate of ½ to 2% per minute.
The dial gauge reading is recorded and the proving
ring after every 60 seconds for a strain between 6%
to 12% after every 2 minutes or so beyond 12%.
The test is continued until failure surfaces have
clearly developed or until an axial strain of 20% is
reached.
The angle between the failure surface and the
horizontal is measured if possible.
23. DISCUSSION
A graph is drawn between compressive stress and strain. The maximum
stress from the curve gives the value of unconfined compressive strength,
qu. If no maximum value of stress is out there, the strain at 20% strain is
taken as unconfined compressive strength. This test provides an immediate
value of the compressive strength of soil in the remoulded condition, it is
carried out within a short time to ensure that no drainage of water is
permitted into or out of the specimen.
In very plastic soils the axial stress does not readily reach a maximum value.
24. REMARKS
The type of soil in this test depends on the purpose for which it is tested and
may be compacted, remoulded or undisturbed. The specimen has minimum
diameter of 38 mm. Compacted specimen could also be prepared at any
predetermined water content and density.
Due to lack of stopwatch the readings taken may include some error.
Moreover, the specimen was already prepared so nothing can be said much
about the type of soil specimen.
Both the ends of the sample are shaped so that it should sit properly on the
bottom plate of loading frame. Rate of loading of the sample should be
constant. Readings should be taken with proper attention so as to have
accurate results. Reading should be taken perpendicularly so as to remove
parallax.
Unconfined Compressive Strength Test is a special type of Unconsolidated
Undrained (UU) test that is commonly used for clay specimen. It is special in
case of triaxial compression test.
25. REPORT
Unconfined compressive strength (UCS) test was carried out on the
undisturbed soil sample collected from the site in tube sampler. The soil
sample obtained had a diameter of 38 mm and the height of the sample
was trimmed to 76 mm to attain height to diameter ratio of 2 in accordance
with IS 2720 part 10. The value of unconfined compressive strength (q) of the
soil sample was determined in a conventional compression testing
machine at a constant strain rate of 0.6 mm/min in accordance with IS 2720
part 10. The sample was tested upto the breaking/failure load or 20% axial
deformation of the sample, whichever occurred earlier.
UCONFINED COMPRESSION TEST CARRIED OUT AT STATE
INFORMATION COMMISSION (SECTOR-3 PANCHKULA)
26. CALCULATION
Sample Calculation for sample collected from BH-1 (depth 12 m)
A = initial area of the sample = 11.3 cm²
Ac= Corrected area of the sample
=A (1-{change in length of specimen during testing/original
length of specimen})
Original length of specimen 76 mm
Final length of specimen = 60.8 mm
Strain in sample at failure = (76-60.8)/76 =20%
Ac=14.1 cm²
Load = 36.1 kg
q=Load/ Ac =2.56 kg/cm²
Undrained Shear strength (Cs) = q /2 = 1.28 kg/cm²