8.1. What is meant by the shear strength of soils? Solution 8.1 Shear strength of a soil is its internal resistance to shearing stresses.

Size: px
Start display at page:

Download "8.1. What is meant by the shear strength of soils? Solution 8.1 Shear strength of a soil is its internal resistance to shearing stresses."

Transcription

1 8.1. What is meant by the shear strength of soils? Solution 8.1 Shear strength of a soil is its internal resistance to shearing stresses.

2 8.2. Some soils show a peak shear strength. Why and what type(s) of soil do so? Solution 8.2 Peak shear strength results from the tendency of some soils to dilate (expand). These soils are generally dense (e.g. dense sands and overconsolidated clays) and the confining stresses are not large enough to suppress dilation.

3 8.3. What is critical state for soils? Solution 8.3 Critical state is a condition reached when a soil attains a constant shear stress to normal effective stress ratio at a constant volume when sheared at large strains.

4 8.4. Which friction angle, peak or critical state, is more reliable? Why? Solution 8.4 Critical state is more reliable. It is unaffected by the normal effective stress and the dilation capacity of the soil.

5 8.5. Which failure criterion is used to interpret the results from a direct shear test? Why? Solution 8.5 Coulomb s criterion. The soil is sheared along a pre-determined failure plane.

6 8.6. Can you draw a Mohr s circle using the data from a direct shear test? Explain your answer. Solution 8.6 No. The stresses on the vertical planes are unknown.

7 8.7. Which failure criterion is used to interpret triaxial test results for long term loading condition? What is basis for this criterion? Solution 8.7 Mohr-Coulomb failure criterion. The basis of this criterion is that a soil will fail when the maximum stress obliquity is attained.

8 8.8. Which failure criterion is used to interpret triaxial test results for short term loading condition? What is basis for this criterion? Is this criterion used for clays or sand or both? Justify your answer. Solution 8.8 Tresca s failure criterion. The basis of this criterion is that the soil will fail at one-half the maximum principal stress difference. This criterion is used for clays under undrained condition.

9 8.9. What is soil cohesion and is it the same as the undrained shear strength? Explain your answer. Solution 8.9 No. Cohesion in the a measure of the intermolecular forces. The undrained shear strength is a measure of the shearing strength of soils (essentially fine-grained soils) when drainage of porewater is prevented.

10 8.10. Why does a sample need to be saturated to interpret the results from triaxial undrained tests? Solution 8.10 Because air in the voids can collapse or move within the soil resulting in a change in soil volume. In the undrained test, the soil volume is intended to be constant.

11 8.11. The confining pressure on a loose saturated sand under groundwater is 100 kpa. The sand is shaken by a seismic event. What is the value of the maximum excess porewater pressure that can develop in the sand? What is the corresponding effective stress? Solution 8.11 Maximum excess porewater pressure = 100 kpa The effective stress = 0. The sand mass will fluidize (be like a viscous liquid).

12 8.12. The confining pressure on a dense (relative density = 85%) saturated sand under groundwater is 100 kpa. Shearing stresses are applied to this sand. Would the excess porewater pressure increase or decrease as a result of the shearing? What is the minimum porewater pressure that can develop in this sand? Justify your answer. Solution 8.12 The excess porewater pressure is expected to increase initially and then decrease as the peak shear stress is attained. The assumption is that the effective confining pressure is not large enough to suppress the dilation tendency of the dense sand. The minimum porewater pressure is the vapour pressure of water (-99 kpa).

13 8.13. The normal and shear stresses at critical state on a horizontal sliding (failure) plane for a sand is 100 kpa and 57.7 kpa respectively. (a) Which failure criterion is best used to determine the friction angle of this sand? Justify your answer. (b) Determine the friction angle. Solution 8.13 (a) Coulomb s failure criterion. This criterion applies to soils that fail on a predermined failure plane, which in this case is the horizontal plane. (b) From equation (8.1) tan f cs = t cs = ( s n ) = f f cs = tan -1 (0.577) = 30 o

14 8.14 The following results were obtained from three direct shear (shear box) tests on a sample of sandy clay. The cross section of the shear box is 50 mm 50 mm Normal force (N) Shearing force (N) Which failure criterion is appropriate to interpret this data set? Justify your answer. (b) Plot a graph of normal force versus shear force for the data given. (c) Determine the critical state friction angle. (d) Is the soil dilatant? (e) Determine the friction angle at a normal force of 100 lb. Is this a peak or critical state friction angle? If this angle is a peak friction angle, what is the value of the dilation angle? Solution 8.14 (a) Coulomb s failure criterion. This criterion applies to soils that fail on a predermined failure plane, which in the direct shear test is the horizontal plane. (b) (c) The critical state friction angle (see graph) is From equation (8.1) P 580 cs tan tan 23.5 P x cs 1 0 z f (d) The soil is dilatant because all the consecutive points do not line on an approximate straight line through the origin. The first two data points lie way off from this line. (e) The friction angle at a normal force of 446 N is a peak friction angle. P 1 x p p tan tan 31.8 P 446 p at 446N z f o o o

15 8.15 The results of a direct shear test on a dense sand using a vertical force is 200 N are shown in the table below. Determine, and. The sample area is 65 mm x 65 mm and the sample height is 20 mm. In the P cs p table, x, z, and P x are the horizontal and vertical displacements and horizontal (shear) force, respectively. Solution Peak Critical state Horizontal load (N) Horizontal displacement (mm) Figure P8.15a

16 p Figure P8.15b The peak shear force is about 178 N and occurs when the horizontal displacement is about 6.6 mm. The vertical displacement just after the peak shear force is achieved remains approximately constant. The critical shear force is about 159 N (Note: At this shear force the soil volume remains approximately constant.). You can use force instead of stress in the equations below because the area is the same for shear and normal forces. 178 p 200 p at 45 lb 1 p 1 o tan tan 41.7 n 159 cs cs 1 o tan tan 38.5 n f f o o o Using the horizontal displacement versus the vertical displacement graph, the average slope for which the soil is dilating is a approximately tan -1 [(0 {-0.26})/(6 2)] = 3.7 o which is 0.5 o (about 16%) greater than the calculated value. This difference is reasonable in comparing experimental and theoretical derived values for this test.

17 8.16 An unconfined, undrained compression test was conducted on a compacted clayey sand classified as SC. The sample size was 38 mm in diameter 76 mmlong. The peak axial force recorded was 230 N, and the sample shortened by 2 mm. (a) Which failure criterion is appropriate to interpret the test data? (b) Determine the undrained shear strength. Solution 8.16 (a) The Tresca s failure criterion. (b) Diameter D m; length H 0.076m; axial displacement = ΔH o = m o r o 2 A m H o 1 1 H s u p o Pz 0.23 p 98.7kPa 2A o 2 2

18 8.17 CU triaxial tests were carried out according to ASTM standards on a sample of a clay classified as CH. The sample was isotropically consolidated using a cell pressure of 400 kpa before the axial displacements were incrementally applied. The results at peak and critical states are shown in the table below. (a) Which failure criterion is appropriate to interpret this data set? Justify your answer. (b) Draw Mohr s circles (total and effective stresses) for the test. (c) Calculate the peak and critical state friction angles and show these angles on the Mohr-circles. (d) Calculate the undrained shear strengths at peak and at critical state and show them on the Mohr-circles. (e) Determine the inclination of angle of the failure plane to the plane on which the major principal effective stress acts at peak shear stress. Solution 8.17 (a) For effective stress conditions, the friction angle is determined using the Mohr-Coulomb s failure criterion. For the total stress condition, the Tresca s failure criterion is used to determine the undrained shear strength. (b) See Table below for values to plot Mohr-circles. Peak effective stress Critical state effective stress Peak total stress Critical state total stress (c) (d) su = 1-3 )/2 kpa Peak 193 Critical state 162

19 p 29.4 (e) p= o o o

20 8.18 A CU test on a stiff, overconsolidated clay was carried out according to ASTM standards at a constant cell pressure of 90 kpa. The peak deviatoric stress recorded was 294 kpa. The corresponding excess porewater pressure was kpa. (a) Calculate the friction angle. Is this the critical state friction angle? Explain your answer. (b) Calculate the undrained shear strength. SOLUTION 8.18 (a) Peak The peak deviatoric stress was reported. Thus, the friction angle is not the critical state friction angle. (b) (su)p = 1-3 )/2 kpa Peak 147

21 8.19 CU tests were conducted on three samples of a compacted clay. Each sample was saturated before shearing. The results, when no further change in excess porewater pressure or deviatoric stress occurred, are shown in the table below. Calculate (a) the friction angle and indicate if this is for peak or critical state, (b) the undrained shear strength for each test, and (c) draw Mohr s circle of total and effective stress for each test and compare your results to those calculated in (a) and (b). Solution 8.19 (a) The average friction angle = 25.7 o (critical state ) (b) See table above (c) Mohr s circles of total and effective stress Total stress is shown by the light line and effective stress by the dark line. Because the porewater pressure is small the total and effective stresses are approximately equal. 26 o

22 8.19 A CU triaxial test was carried out on a silty clay that was isotropically consolidated using a cell pressure of 90 kpa. The following data were obtained. (a) Plot the deviatoric (axial) stress against axial strain and excess porewater pressure against axial strain. (b) Determine the undrained shear strength and the friction angle. Are these critical state or peak values? Justify your answer. Solution 8.20 (a) (b) These are critical state values as the axial stress and excess porewater pressures are approximately constant.

23 8.21 The results of an ASTM standard UU test on a sample of a stiff clay classified as CL is (σ 1 - σ 3) p = 70 kpa. The initial size of the sample was 38 mm x 76 mm long and it compressed by 2 mm. Determine s u. Solution 8.21 su = 1-3 )/2 = 70/2 = 35 kpa

24 8.22 Plot the corrected N value (N 1,60), the bulk unit weight and friction angle with depth for the data given in Figure Solution 8.22 The answers to this question depend on your interpretation of the test data and the empirical constants used. However, your answers should be about +-20% of the results given below.

25

26 8.23 Plot the undrained shear strength with depth for the CPT results shown in Figure Solution 8.23 The answers to this question depend on your interpretation of the test data and the empirical constants used. However, your answers should be about +-20% of the results given below. Make a composite diagram identifying soil layers. Use the empirical equation in Table 8.9 to make estimated of the undrained shear strength. Since no data was given regarding the physical parameters (e.g. plasticity index) of the soils, a conservative value of N k = 19 (Table 8.9) is used. A unit weight of 18 kn/m 3 is assumed as the average unit weight of the soil. The tables below show the estimated results.

27

28 8.24 You are in charge of designing a retaining wall. What laboratory tests would you specify for the backfill soil? Give reasons. Solution 8.24 The backfill for retaining walls are generally coarse-grained soils. The following tests are required. 1. Grain size to classify the soil. 2. Standard Proctor Compaction test to obtain maximum dry unit weight and optimum water content for specifications during construction. 3. Direct simple shear (DSS) test on the soil compacted to maximum dry unit weight and optimum water content to obtain the friction angle because the stress condition in the backfill of a long retaining wall is plane strain. If DSS apparatus is not available then substitute direct shear test. The soil should be sheared until the critical state is obtained. A simple angle of repose test can be done to compare with the critical state friction angle obtained from the test. The two results should be similar.

29 8.25 Solution 8.25 (a) 26.7 o Critical state is a reasonable assumption since the shears strains are large, the deviatoric stress and the porewater pressure are approximately constant. (b) See table above From the test s u s u cs ic zo cs ic s u 3sin ' cs Ro zo 3 sin ' cs 2 cs ic 3 max 140 where R o 4 35 Table cs ic 3 o 0.8 o s u 3sin ' cs Ro 3sin o 3 sin ' cs 2 3 sin s u 3 The test ratio, reasonable. (c ) Recommended strength values. cs ic, is about 12% less than the theoretical estimated value. The test results appear o o Long term loading: ' 26.7 ( Use 26 ) Short term: s u = 27.5 kpa (Use 27 kpa) cs

30

31 Solution 8.26 (a) (b) The shear strength parameters are the friction angles and the undrained shear strengths. These values are tabulated using a spreadsheet. You can get the same results by finding the angles subtended by the tangents and the x-axis (friction angles) of the Mohr circles shown above. The undrained shear strength for each Mohr circle is the maximum value of. (c) and (d)the confining effective stress in the field is higher than the maximum cell (effective) pressure applied to the test samples. The peak friction angle is expected to decrease if a cell (effective) pressure of 300 kpa were to be used on a test sample. For a preliminary assessment, a friction angle less than 26.6 degrees will be recommended for long term loading. However, an actual value is speculative. Consequently, the shear strength parameters for design cannot be recommended with confidence. (e) Yes. Re-testing should be done. The soil should be incrementally consolidated to a cell pressure at least to 300 kpa (= current effective confining pressure) x OCR (= overconsolidation ratio) and then unloaded incrementally to 300 kpa. The shearing phase of the CU test should then be conducted to large shear strains (> 15%) or until a constant deviatoric stress and constant porewater pressure is

32 achieved. The porewater pressure must be measured continuously.

SHEAR STRENGTH OF SOIL

SHEAR STRENGTH OF SOIL Soil Failure Criteria SHEAR STRENGTH OF SOIL Knowledge about the shear strength of soil important for the analysis of: Bearing capacity of foundations, Slope stability, Lateral pressure on retaining structures,

More information

Chapter 5 Shear Strength of Soil

Chapter 5 Shear Strength of Soil Page 5 Chapter 5 Shear Strength of Soil. The internal resistance per unit area that the soil mass can offer to resist failure and sliding along any plane inside it is called (a) strength (b) shear strength

More information

D1. A normally consolidated clay has the following void ratio e versus effective stress σ relationship obtained in an oedometer test.

D1. A normally consolidated clay has the following void ratio e versus effective stress σ relationship obtained in an oedometer test. (d) COMPRESSIBILITY AND CONSOLIDATION D1. A normally consolidated clay has the following void ratio e versus effective stress σ relationship obtained in an oedometer test. (a) Plot the e - σ curve. (b)

More information

Soil strength. the strength depends on the applied stress. water pressures are required

Soil strength. the strength depends on the applied stress. water pressures are required Soil Strength Soil strength u Soils are essentially frictional materials the strength depends on the applied stress u Strength is controlled by effective stresses water pressures are required u Soil strength

More information

Shear Strength of Soils

Shear Strength of Soils Shear Strength of Soils STRESSES IN A SOIL ELEMENT t s v Analyze Effective Stresses (s ) Load carried by Soil t Where: s H t t s H s = t f = s v = s H = t = s v Stresses in a Soil Element after Figure

More information

Chapter (12) Instructor : Dr. Jehad Hamad

Chapter (12) Instructor : Dr. Jehad Hamad Chapter (12) Instructor : Dr. Jehad Hamad 2017-2016 Chapter Outlines Shear strength in soils Direct shear test Unconfined Compression Test Tri-axial Test Shear Strength The strength of a material is the

More information

SOIL SHEAR STRENGTH. Prepared by: Dr. Hetty Muhammad Azril Fauziah Kassim Norafida

SOIL SHEAR STRENGTH. Prepared by: Dr. Hetty Muhammad Azril Fauziah Kassim Norafida SOIL SHEAR STRENGTH Prepared by: Dr. Hetty Muhammad Azril Fauziah Kassim Norafida What is shear strength Shear strength of a soil is the maximum internal resistance to applied shearing forces Why it is

More information

SHEAR STRENGTH OF SOIL

SHEAR STRENGTH OF SOIL SHEAR STRENGTH OF SOIL Necessity of studying Shear Strength of soils : Soil failure usually occurs in the form of shearing along internal surface within the soil. Shear Strength: Thus, structural strength

More information

Theory of Shear Strength

Theory of Shear Strength MAJ 1013 ADVANCED SOIL MECHANICS Theory of Shear Strength Prepared by, Dr. Hetty 1 Strength of different materials Steel Concrete Soil Tensile strength Compressive strength Shear strength Complex behavior

More information

Following are the results of four drained direct shear tests on an overconsolidated clay: Diameter of specimen 50 mm Height of specimen 25 mm

Following are the results of four drained direct shear tests on an overconsolidated clay: Diameter of specimen 50 mm Height of specimen 25 mm 444 Chapter : Shear Strength of Soil Example. Following are the results of four drained direct shear tests on an overconsolidated clay: Diameter of specimen 50 mm Height of specimen 5 mm Normal Shear force

More information

Triaxial Shear Test. o The most reliable method now available for determination of shear strength parameters.

Triaxial Shear Test. o The most reliable method now available for determination of shear strength parameters. TOPICS Introduction Components of Shear Strength of Soils Normal and Shear Stresses on a Plane Mohr-Coulomb Failure Criterion Laboratory Shear Strength Testing Direct Shear Test Triaxial Compression Test

More information

Theory of Shear Strength

Theory of Shear Strength SKAA 1713 SOIL MECHANICS Theory of Shear Strength Prepared by, Dr. Hetty 1 SOIL STRENGTH DEFINITION Shear strength of a soil is the maximum internal resistance to applied shearing forces The maximum or

More information

Laboratory Testing Total & Effective Stress Analysis

Laboratory Testing Total & Effective Stress Analysis SKAA 1713 SOIL MECHANICS Laboratory Testing Total & Effective Stress Analysis Prepared by: Dr. Hetty Mohr Coulomb failure criterion with Mohr circle of stress 2 ' 2 ' ' ' 3 ' 1 ' 3 ' 1 Cot Sin c ' ' 2

More information

Shear strength. Common cases of shearing In practice, the state of stress in the ground will be complex. Common cases of shearing Strength

Shear strength. Common cases of shearing In practice, the state of stress in the ground will be complex. Common cases of shearing Strength Shear strength Common cases of shearing Strength Near any geotechnical construction (e.g. slopes, excavations, tunnels and foundations) there will be both mean and normal stresses and shear stresses. The

More information

Ch 4a Stress, Strain and Shearing

Ch 4a Stress, Strain and Shearing Ch. 4a - Stress, Strain, Shearing Page 1 Ch 4a Stress, Strain and Shearing Reading Assignment Ch. 4a Lecture Notes Sections 4.1-4.3 (Salgado) Other Materials Handout 4 Homework Assignment 3 Problems 4-13,

More information

1.8 Unconfined Compression Test

1.8 Unconfined Compression Test 1-49 1.8 Unconfined Compression Test - It gives a quick and simple measurement of the undrained strength of cohesive, undisturbed soil specimens. 1) Testing method i) Trimming a sample. Length-diameter

More information

Welcome back. So, in the last lecture we were seeing or we were discussing about the CU test. (Refer Slide Time: 00:22)

Welcome back. So, in the last lecture we were seeing or we were discussing about the CU test. (Refer Slide Time: 00:22) Geology and Soil Mechanics Prof. P. Ghosh Department of Civil Engineering Indian Institute of Technology Kanpur Lecture - 43 Shear Strength of Soils Keywords: Triaxial shear test, unconsolidated undrained

More information

Prof. B V S Viswanadham, Department of Civil Engineering, IIT Bombay

Prof. B V S Viswanadham, Department of Civil Engineering, IIT Bombay 56 Module 4: Lecture 7 on Stress-strain relationship and Shear strength of soils Contents Stress state, Mohr s circle analysis and Pole, Principal stressspace, Stress pathsin p-q space; Mohr-Coulomb failure

More information

(Refer Slide Time: 02:18)

(Refer Slide Time: 02:18) Geology and Soil Mechanics Prof. P. Ghosh Department of Civil Engineering Indian Institute of Technology Kanpur Lecture 40 Shear Strength of Soil - C Keywords: Shear strength of soil, direct shear test,

More information

Stress and Strains in Soil and Rock. Hsin-yu Shan Dept. of Civil Engineering National Chiao Tung University

Stress and Strains in Soil and Rock. Hsin-yu Shan Dept. of Civil Engineering National Chiao Tung University Stress and Strains in Soil and Rock Hsin-yu Shan Dept. of Civil Engineering National Chiao Tung University Stress and Strain ε 1 1 2 ε 2 ε Dimension 1 2 0 ε ε ε 0 1 2 ε 1 1 2 ε 2 ε Plane Strain = 0 1 2

More information

1.5 STRESS-PATH METHOD OF SETTLEMENT CALCULATION 1.5 STRESS-PATH METHOD OF SETTLEMENT CALCULATION

1.5 STRESS-PATH METHOD OF SETTLEMENT CALCULATION 1.5 STRESS-PATH METHOD OF SETTLEMENT CALCULATION Module 6 Lecture 40 Evaluation of Soil Settlement - 6 Topics 1.5 STRESS-PATH METHOD OF SETTLEMENT CALCULATION 1.5.1 Definition of Stress Path 1.5. Stress and Strain Path for Consolidated Undrained Undrained

More information

Shear Strength of Soil

Shear Strength of Soil 8 Shear Strength of Soil 8 1 INTRODUCTION As a structural member, a piece of steel is capable of resisting compression, tension, and shear. Soil, however, like concrete and rock, is not capable of resisting

More information

SHEAR STRENGTH OF SOIL UNCONFINED COMPRESSION TEST

SHEAR STRENGTH OF SOIL UNCONFINED COMPRESSION TEST SHEAR STRENGTH OF SOIL DEFINITION The shear strength of the soil mass is the internal resistance per unit area that the soil mass can offer to resist failure and sliding along any plane inside it. INTRODUCTION

More information

Modified Cam-clay triaxial test simulations

Modified Cam-clay triaxial test simulations 1 Introduction Modified Cam-clay triaxial test simulations This example simulates a series of triaxial tests which can be used to verify that Modified Cam-Clay constitutive model is functioning properly.

More information

SHEAR STRENGTH I YULVI ZAIKA

SHEAR STRENGTH I YULVI ZAIKA SHEAR STRENGTH I YULVI ZAIKA MATERI Keruntuhan mohr coulomb, stress paths, kuat geser tanah non kohesif dan kohesif, evaluasi kuat geser di lapangan, tegangan normal dan tegangan geser pada sebuah bidang

More information

Foundation Analysis LATERAL EARTH PRESSURE

Foundation Analysis LATERAL EARTH PRESSURE Foundation Analysis LATERAL EARTH PRESSURE INTRODUCTION Vertical or near-vertical slopes of soil are supported by retaining walls, cantilever sheet-pile walls, sheet-pile bulkheads, braced cuts, and other

More information

Class Principles of Foundation Engineering CEE430/530

Class Principles of Foundation Engineering CEE430/530 Class Principles of Foundation Engineering CEE430/530 1-1 General Information Lecturer: Scott A. Barnhill, P.E. Lecture Time: Thursday, 7:10 pm to 9:50 pm Classroom: Kaufmann, Room 224 Office Hour: I have

More information

Compression and swelling. Mechanisms of compression. Mechanisms Common cases Isotropic One-dimensional Wet and dry states

Compression and swelling. Mechanisms of compression. Mechanisms Common cases Isotropic One-dimensional Wet and dry states Compression and swelling Mechanisms Common cases Isotropic One-dimensional Wet and dry states The relationship between volume change and effective stress is called compression and swelling. (Consolidation

More information

INTERPRETATION OF UNDRAINED SHEAR STRENGTH OF UNSATURATED SOILS IN TERMS OF STRESS STATE VARIABLES

INTERPRETATION OF UNDRAINED SHEAR STRENGTH OF UNSATURATED SOILS IN TERMS OF STRESS STATE VARIABLES INTERPRETATION OF UNDRAINED SHEAR STRENGTH OF UNSATURATED SOILS IN TERMS OF STRESS STATE VARIABLES S. K. Vanapalli and D.G. Fredlund Department of Civil Engineering University of Saskatchewan, Saskatoon

More information

Shear Strength of Soils

Shear Strength of Soils Shear Strength of Soils Soil strength Most of problems in soil engineering (foundations, slopes, etc.) soil withstands shear stresses. Shear strength of a soil is defined as the capacity to resist shear

More information

FOUNDATION ENGINEERING UNIT V

FOUNDATION ENGINEERING UNIT V FOUNDATION ENGINEERING UNIT V RETAINING WALLS Plastic equilibrium in soils active and passive states Rankine s theory cohesion less and cohesive soil - Coloumb s wedge theory condition for critical failure

More information

pcf REQUIRED: Determine the shear strength parameters for use in a preliminary shallow foundation design. SOLUTION:

pcf REQUIRED: Determine the shear strength parameters for use in a preliminary shallow foundation design. SOLUTION: 14.330 SOIL MECHANICS Assignment #8: Shear Strength Solution. PROBLEM #1: GIVEN: A regional residential building contractor is planning on building a custom 4,100 ft² home on Martha s Vineyard, MA. The

More information

Page 1 of 10. PROFESSIONAL ENGINEERS ONTARIO NATIONAL EXAMINATIONS Mav CIV-A4 GEOTECHNICAL MATERIALS AND ANALYSIS 3 HOURS DURATION

Page 1 of 10. PROFESSIONAL ENGINEERS ONTARIO NATIONAL EXAMINATIONS Mav CIV-A4 GEOTECHNICAL MATERIALS AND ANALYSIS 3 HOURS DURATION Page 1 of 10 PROFESSIONAL ENGINEERS ONTARIO NATIONAL EXAMINATIONS Mav 2015 3 HOURS DURATION NOTES: 1. This is a closed book examination. 2. Read all questions carefully before you answer 3. Should you

More information

Reinforced Soil Structures Reinforced Soil Walls. Prof K. Rajagopal Department of Civil Engineering IIT Madras, Chennai

Reinforced Soil Structures Reinforced Soil Walls. Prof K. Rajagopal Department of Civil Engineering IIT Madras, Chennai Geosynthetics and Reinforced Soil Structures Reinforced Soil Walls continued Prof K. Rajagopal Department of Civil Engineering IIT Madras, Chennai e-mail: gopalkr@iitm.ac.inac in Outline of the Lecture

More information

Chapter (11) Pile Foundations

Chapter (11) Pile Foundations Chapter (11) Introduction Piles are structural members that are made of steel, concrete, or timber. They are used to build pile foundations (classified as deep foundations) which cost more than shallow

More information

Table of Contents Chapter 1 Introduction to Geotechnical Engineering 1.1 Geotechnical Engineering 1.2 The Unique Nature of Soil and Rock Materials

Table of Contents Chapter 1 Introduction to Geotechnical Engineering 1.1 Geotechnical Engineering 1.2 The Unique Nature of Soil and Rock Materials Table of Contents Chapter 1 Introduction to Geotechnical Engineering 1.1 Geotechnical Engineering 1.2 The Unique Nature of Soil and Rock Materials 1.3 Scope of This Book 1.4 Historical Development of Geotechnical

More information

Lateral Earth Pressure

Lateral Earth Pressure 1 of 11 6/2/2012 4:28 AM Lateral Earth Pressure The magnitude of lateral earth pressure depends on: 1. Shear strength characteristics of soil 2. Lateral strain condition 3. Pore water pressure 4. State

More information

QUESTION BANK DEPARTMENT: CIVIL SUBJECT CODE / Name: CE 2251 / SOIL MECHANICS SEMESTER: IV UNIT 1- INTRODUCTION PART - A (2 marks) 1. Distinguish between Residual and Transported soil. (AUC May/June 2012)

More information

Geotechnical Properties of Soil

Geotechnical Properties of Soil Geotechnical Properties of Soil 1 Soil Texture Particle size, shape and size distribution Coarse-textured (Gravel, Sand) Fine-textured (Silt, Clay) Visibility by the naked eye (0.05 mm is the approximate

More information

2017 Soil Mechanics II and Exercises Final Exam. 2017/7/26 (Wed) 10:00-12:00 Kyotsu 4 Lecture room

2017 Soil Mechanics II and Exercises Final Exam. 2017/7/26 (Wed) 10:00-12:00 Kyotsu 4 Lecture room 2017 Soil Mechanics II and Exercises Final Exam 2017/7/26 (Wed) 10:00-12:00 Kyotsu 4 Lecture room Attention: The exam consists of five questions for which you are provided with five answer sheets. Write

More information

Prof. B V S Viswanadham, Department of Civil Engineering, IIT Bombay

Prof. B V S Viswanadham, Department of Civil Engineering, IIT Bombay 51 Module 4: Lecture 2 on Stress-strain relationship and Shear strength of soils Contents Stress state, Mohr s circle analysis and Pole, Principal stressspace, Stress pathsin p-q space; Mohr-coulomb failure

More information

SOIL MECHANICS Assignment #7: Shear Strength Solution.

SOIL MECHANICS Assignment #7: Shear Strength Solution. 14.330 SOIL MECHANICS Assignment #7: Shear Strength Solution. PROBLEM #1: GIVEN: Direct Shear test results from a SP soil shown in Figure A (from 14.330_2012_Assignment_#8_P1.csv on the course website).

More information

Recent Research on EPS Geofoam Seismic Buffers. Richard J. Bathurst and Saman Zarnani GeoEngineering Centre at Queen s-rmc Canada

Recent Research on EPS Geofoam Seismic Buffers. Richard J. Bathurst and Saman Zarnani GeoEngineering Centre at Queen s-rmc Canada Recent Research on EPS Geofoam Seismic Buffers Richard J. Bathurst and Saman Zarnani GeoEngineering Centre at Queen s-rmc Canada What is a wall (SEISMIC) buffer? A compressible inclusion placed between

More information

Advanced model for soft soils. Modified Cam-Clay (MCC)

Advanced model for soft soils. Modified Cam-Clay (MCC) Advanced model for soft soils. Modified Cam-Clay (MCC) c ZACE Services Ltd August 2011 1 / 62 2 / 62 MCC: Yield surface F (σ,p c ) = q 2 + M 2 c r 2 (θ) p (p p c ) = 0 Compression meridian Θ = +π/6 -σ

More information

YOUR HW MUST BE STAPLED YOU MUST USE A PENCIL (no pens)

YOUR HW MUST BE STAPLED YOU MUST USE A PENCIL (no pens) Spring 2008 CIVE 462 HOMEWORK #1 1. Print out the syllabus. Read it. Write the grade percentages in the first page of your notes. 2. Go back to your 301 notes, internet, etc. and find the engineering definition

More information

Appendix A Results of Triaxial and Consolidation Tests

Appendix A Results of Triaxial and Consolidation Tests Appendix A Results of Triaxial and Consolidation Tests Triaxial and consolidation tests were performed on specimens of the soils used for interface testing. The objectives of these tests were as follows:

More information

SHEAR STRENGTH OF SOIL. Chapter 10: Sections Chapter 12: All sections except

SHEAR STRENGTH OF SOIL. Chapter 10: Sections Chapter 12: All sections except SHEAR STRENGTH OF SOIL Chapter 10: Sections 10. 10.3 Chapter 1: All sections ecept 1.13 1.14 1.15 1.17 1.18 TOPICS Introduction Components of Shear Strength of Soils Normal and Shear Stresses on a Plane

More information

both an analytical approach and the pole method, determine: (a) the direction of the

both an analytical approach and the pole method, determine: (a) the direction of the Quantitative Problems Problem 4-3 Figure 4-45 shows the state of stress at a point within a soil deposit. Using both an analytical approach and the pole method, determine: (a) the direction of the principal

More information

16 Rainfall on a Slope

16 Rainfall on a Slope Rainfall on a Slope 16-1 16 Rainfall on a Slope 16.1 Problem Statement In this example, the stability of a generic slope is analyzed for two successive rainfall events of increasing intensity and decreasing

More information

Shear Strength of Soils

Shear Strength of Soils ENVIRONMENTAL GEOTECHNICS Shear Strength of Soils Prof. Ing. Marco Favaretti University of Padova Department of Civil, Environmental and Architectural Engineering Via Ognissanti, 39 Padova (Italy) phone:

More information

Soil and Rock Strength. Chapter 8 Shear Strength. Steel Strength. Concrete Strength. Dr. Talat Bader May Steel. Concrete.

Soil and Rock Strength. Chapter 8 Shear Strength. Steel Strength. Concrete Strength. Dr. Talat Bader May Steel. Concrete. Chapter 8 Shear Strength Dr. Talat Bader May 2006 Soil and Rock Strength Unconfined compressive strength (MPa) Steel Concrete 20 100 250 750 0.001 0.01 Soil 0.1 1.0 10 Rock 100 250 F y = 250 to 750 MPa

More information

SOME OBSERVATIONS RELATED TO LIQUEFACTION SUSCEPTIBILITY OF SILTY SOILS

SOME OBSERVATIONS RELATED TO LIQUEFACTION SUSCEPTIBILITY OF SILTY SOILS SOME OBSERVATIONS RELATED TO LIQUEFACTION SUSCEPTIBILITY OF SILTY SOILS Upul ATUKORALA 1, Dharma WIJEWICKREME 2 And Norman MCCAMMON 3 SUMMARY The liquefaction susceptibility of silty soils has not received

More information

Earth Pressure Theory

Earth Pressure Theory Lateral Earth Pressure Page 1 Earth Pressure Theory Examples of Retaining Walls Lateral Earth Pressure Page 2 At-Rest, Active and Passive Earth Pressure Wednesday, August 17, 2011 12:45 PM At-rest condition

More information

INTERNATIONAL JOURNAL OF CIVIL AND STRUCTURAL ENGINEERING Volume 1, No 4, 2011

INTERNATIONAL JOURNAL OF CIVIL AND STRUCTURAL ENGINEERING Volume 1, No 4, 2011 Undrained response of mining sand with fines contents Thian S. Y, Lee C.Y Associate Professor, Department of Civil Engineering, Universiti Tenaga Nasional, Malaysia siawyin_thian@yahoo.com ABSTRACT This

More information

Verification of the Hyperbolic Soil Model by Triaxial Test Simulations

Verification of the Hyperbolic Soil Model by Triaxial Test Simulations 1 Introduction Verification of the Hyperbolic Soil Model by Triaxial Test Simulations This example simulates a series of triaxial tests that can be used to verify that the Hyperbolic constitutive model

More information

Ch 5 Strength and Stiffness of Sands

Ch 5 Strength and Stiffness of Sands Ch. 5 - Strength and Stiffness of Sand Page 1 Ch 5 Strength and Stiffness of Sands Reading Assignment Ch. 5 Lecture Notes Sections 5.1-5.7 (Salgado) Other Materials Homework Assignment Problems 5-9, 5-12,

More information

7. STRESS ANALYSIS AND STRESS PATHS

7. STRESS ANALYSIS AND STRESS PATHS 7-1 7. STRESS ANALYSIS AND STRESS PATHS 7.1 THE MOHR CIRCLE The discussions in Chapters and 5 were largely concerned with vertical stresses. A more detailed examination of soil behaviour requires a knowledge

More information

Table 3. Empirical Coefficients for BS 8002 equation. A (degrees) Rounded Sub-angular. 2 Angular. B (degrees) Uniform Moderate grading.

Table 3. Empirical Coefficients for BS 8002 equation. A (degrees) Rounded Sub-angular. 2 Angular. B (degrees) Uniform Moderate grading. Hatanaka and Uchida (1996); ' 20N 20 12N 20 ' 45 A lower bound for the above equation is given as; 12N 15 ' 45 Table 3. Empirical Coefficients for BS 8002 equation A Angularity 1) A (degrees) Rounded 0

More information

LATERAL EARTH PRESSURE

LATERAL EARTH PRESSURE . INTRODUCTION Retaining structures commonly used in foundation engineering, such as retaining walls, basement walls and bulkheads to support almost vertical slopes of earth masses. Proper design and construction

More information

VALLIAMMAI ENGINEERING COLLEGE

VALLIAMMAI ENGINEERING COLLEGE VALLIAMMAI ENGINEERING COLLEGE DEPARTMENT OF CIVIL ENGINEERING SUBJECT CODE : CE6405 YEAR : II SUBJECT NAME : SOIL MECHANICS SEM : IV QUESTION BANK (As per Anna University 2013 regulation) UNIT 1- SOIL

More information

Soil Mechanics Prof. B.V.S. Viswanathan Department of Civil Engineering Indian Institute of Technology, Bombay Lecture 51 Earth Pressure Theories II

Soil Mechanics Prof. B.V.S. Viswanathan Department of Civil Engineering Indian Institute of Technology, Bombay Lecture 51 Earth Pressure Theories II Soil Mechanics Prof. B.V.S. Viswanathan Department of Civil Engineering Indian Institute of Technology, Bombay Lecture 51 Earth Pressure Theories II Welcome to lecture number two on earth pressure theories.

More information

Principles of Foundation Engineering 8th Edition Das SOLUTIONS MANUAL

Principles of Foundation Engineering 8th Edition Das SOLUTIONS MANUAL Principles of Foundation Engineering 8th Edition SOLUTIONS MANUAL Full clear download (no formatting errors) at: https://testbankreal.com/download/principles-foundation-engineering- 8th-edition-das-solutions-manual/

More information

Compute the lateral force per linear foot with sloping backfill and inclined wall. Use Equation No. 51, page 93. Press ENTER.

Compute the lateral force per linear foot with sloping backfill and inclined wall. Use Equation No. 51, page 93. Press ENTER. Sample Problems Problem 5.1 A gravity retaining wall is supporting a cohesionless soil. The active lateral force per linear foot of the retaining wall is most nearly (A) 5,000 lb/ft (B) 6,000 lb/ft (C)

More information

file:///d /suhasini/suha/office/html2pdf/ _editable/slides/module%202/lecture%206/6.1/1.html[3/9/2012 4:09:25 PM]

file:///d /suhasini/suha/office/html2pdf/ _editable/slides/module%202/lecture%206/6.1/1.html[3/9/2012 4:09:25 PM] Objectives_template Objectives In this section you will learn the following Introduction Different Theories of Earth Pressure Lateral Earth Pressure For At Rest Condition Movement of the Wall Different

More information

Reciprocal of the initial shear stiffness of the interface K si under initial loading; reciprocal of the initial tangent modulus E i of the soil

Reciprocal of the initial shear stiffness of the interface K si under initial loading; reciprocal of the initial tangent modulus E i of the soil Appendix F Notation a b B C c C k C N C s C u C wt C θ D r D 1 D 2 D 10 D 30 Reciprocal of the initial shear stiffness of the interface K si under initial loading; reciprocal of the initial tangent modulus

More information

2.7 Shear Strength of Unsaturated Soils

2.7 Shear Strength of Unsaturated Soils 2.7 Shear Strength of Unsaturated Soils D. G. FREDLUND, University of Saskatchewan, Saskatoon, Saskatchewan, Canada S. K. VANAPALLI, Lakehead University, Thunder Bay, Ontario, Canada 2.7.1 Introduction

More information

SOIL MODELS: SAFETY FACTORS AND SETTLEMENTS

SOIL MODELS: SAFETY FACTORS AND SETTLEMENTS PERIODICA POLYTECHNICA SER. CIV. ENG. VOL. 48, NO. 1 2, PP. 53 63 (2004) SOIL MODELS: SAFETY FACTORS AND SETTLEMENTS Gabriella VARGA and Zoltán CZAP Geotechnical Department Budapest University of Technology

More information

Module 5: Failure Criteria of Rock and Rock masses. Contents Hydrostatic compression Deviatoric compression

Module 5: Failure Criteria of Rock and Rock masses. Contents Hydrostatic compression Deviatoric compression FAILURE CRITERIA OF ROCK AND ROCK MASSES Contents 5.1 Failure in rocks 5.1.1 Hydrostatic compression 5.1.2 Deviatoric compression 5.1.3 Effect of confining pressure 5.2 Failure modes in rocks 5.3 Complete

More information

Drained Against Undrained Behaviour of Sand

Drained Against Undrained Behaviour of Sand Archives of Hydro-Engineering and Environmental Mechanics Vol. 54 (2007), No. 3, pp. 207 222 IBW PAN, ISSN 1231 3726 Drained Against Undrained Behaviour of Sand Andrzej Sawicki, Waldemar Świdziński Institute

More information

GEO E1050 Finite Element Method Mohr-Coulomb and other constitutive models. Wojciech Sołowski

GEO E1050 Finite Element Method Mohr-Coulomb and other constitutive models. Wojciech Sołowski GEO E050 Finite Element Method Mohr-Coulomb and other constitutive models Wojciech Sołowski To learn today. Reminder elasticity 2. Elastic perfectly plastic theory: concept 3. Specific elastic-perfectly

More information

Liquefaction Potential Variations Influenced by Building Constructions

Liquefaction Potential Variations Influenced by Building Constructions Earth Science Research; Vol. 1, No. 2; 2012 ISSN 1927-0542 E-ISSN 1927-0550 Published by Canadian Center of Science and Education Liquefaction Potential Variations Influenced by Building Constructions

More information

Introduction to Soil Mechanics

Introduction to Soil Mechanics Introduction to Soil Mechanics Sela Sode and Colin Jones WILEY Blackwell Contents Preface Dedication and Acknowledgments List of Symbols Soil Structure 1.1 Volume relationships 1.1.1 Voids ratio (e) 1.1.2

More information

Prof. B V S Viswanadham, Department of Civil Engineering, IIT Bombay

Prof. B V S Viswanadham, Department of Civil Engineering, IIT Bombay 50 Module 4: Lecture 1 on Stress-strain relationship and Shear strength of soils Contents Stress state, Mohr s circle analysis and Pole, Principal stressspace, Stress pathsin p-q space; Mohr-Coulomb failure

More information

CPT Data Interpretation Theory Manual

CPT Data Interpretation Theory Manual CPT Data Interpretation Theory Manual 2016 Rocscience Inc. Table of Contents 1 Introduction... 3 2 Soil Parameter Interpretation... 5 3 Soil Profiling... 11 3.1 Non-Normalized SBT Charts... 11 3.2 Normalized

More information

(Refer Slide Time: 01:15)

(Refer Slide Time: 01:15) Soil Mechanics Prof. B.V.S. Viswanathan Department of Civil Engineering Indian Institute of Technology, Bombay Lecture 56 Stability analysis of slopes II Welcome to lecture two on stability analysis of

More information

Landslide FE Stability Analysis

Landslide FE Stability Analysis Landslide FE Stability Analysis L. Kellezi Dept. of Geotechnical Engineering, GEO-Danish Geotechnical Institute, Denmark S. Allkja Altea & Geostudio 2000, Albania P. B. Hansen Dept. of Geotechnical Engineering,

More information

Cyclic Triaxial Behavior of an Unsaturated Silty Soil Subjected to Suction Changes

Cyclic Triaxial Behavior of an Unsaturated Silty Soil Subjected to Suction Changes 6 th International Conference on Earthquake Geotechnical Engineering 1-4 November 215 Christchurch, New Zealand Cyclic Triaxial Behavior of an Unsaturated Silty Soil Subjected to Suction Changes T. Nishimura

More information

(C) Global Journal of Engineering Science and Research Management

(C) Global Journal of Engineering Science and Research Management GEOTECHNCIAL ASSESSMENT OF PART OF PORT HARCOURT, NIGER DELTA FOR STRUCTURAL ANALYSIS Warmate Tamunonengiyeofori Geostrat International Services Limited, www.geostratinternational.com. *Correspondence

More information

FUNDAMENTALS SOIL MECHANICS. Isao Ishibashi Hemanta Hazarika. >C\ CRC Press J Taylor & Francis Group. Taylor & Francis Group, an Informa business

FUNDAMENTALS SOIL MECHANICS. Isao Ishibashi Hemanta Hazarika. >C\ CRC Press J Taylor & Francis Group. Taylor & Francis Group, an Informa business SOIL MECHANICS FUNDAMENTALS Isao Ishibashi Hemanta Hazarika >C\ CRC Press J Taylor & Francis Group Boca Raton London New York CRC Press is an imprint of the Taylor & Francis Group, an Informa business

More information

Chapter 2. 53% v. 2.2 a. From Eqs. (2.11) and (2.12), it can be seen that, 2.67

Chapter 2. 53% v. 2.2 a. From Eqs. (2.11) and (2.12), it can be seen that, 2.67 Chapter 2 2.1 d. (87.5)(9.81) (1000)(0.05) 3 17.17 kn/m c. d 1 w 17.17 1 0.15 3 14.93 kn/m G a. Eq. (2.12): s w (2.68)(9.81). 14.93 ; e 0.76 1 e 1 e e 0.76 b. Eq. (2.6): n 0.43 1 e 1 0.76 Vw wgs (0.15)(2.68)

More information

3-BEARING CAPACITY OF SOILS

3-BEARING CAPACITY OF SOILS 3-BEARING CAPACITY OF SOILS INTRODUCTION The soil must be capable of carrying the loads from any engineered structure placed upon it without a shear failure and with the resulting settlements being tolerable

More information

Geology 229 Engineering Geology. Lecture 5. Engineering Properties of Rocks (West, Ch. 6)

Geology 229 Engineering Geology. Lecture 5. Engineering Properties of Rocks (West, Ch. 6) Geology 229 Engineering Geology Lecture 5 Engineering Properties of Rocks (West, Ch. 6) Common mechanic properties: Density; Elastic properties: - elastic modulii Outline of this Lecture 1. Uniaxial rock

More information

Philadelphia University Faculty of Engineering

Philadelphia University Faculty of Engineering Final Exam, Second Semester: 2015/2016 Civil Engineering Department Course Title: SOIL MECHANICS Date: 9/6/2016 Course No: 0670331 Time: 2 hours Lecturer: Dr. Mohammed Mustafa Al-Iessa No. of pages: 9

More information

EARTHQUAKE-INDUCED SETTLEMENT AS A RESULT OF DENSIFICATION, MEASURED IN LABORATORY TESTS

EARTHQUAKE-INDUCED SETTLEMENT AS A RESULT OF DENSIFICATION, MEASURED IN LABORATORY TESTS 13 th World Conference on Earthquake Engineering Vancouver, B.C., Canada August 1-6, 2004 Paper No. 3291 EARTHQUAKE-INDUCED SETTLEMENT AS A RESULT OF DENSIFICATION, MEASURED IN LABORATORY TESTS Constantine

More information

Compressibility & Consolidation

Compressibility & Consolidation CHAPTER Compressibility & Consolidation Settlement If a structure is placed on soil surface, then the soil will undergo an elastic and plastic deformation. In engineering practice, the deformation or reduction

More information

Seismic Stability of Tailings Dams, an Overview

Seismic Stability of Tailings Dams, an Overview Seismic Stability of Tailings Dams, an Overview BY Gonzalo Castro, Ph.D., P.E. Principal International Workshop on Seismic Stability of Tailings Dams Case Western Reserve University, November 2003 Small

More information

Geotechnical Parameters for Retaining Wall Design

Geotechnical Parameters for Retaining Wall Design 11 th October 2012 Geotechnical Parameters for Retaining Wall Design Tanya Kouzmin 1 Most geotechnical failures are of retaining walls Are failure caused by WRONG calculations? Not usually calculation

More information

TIME-DEPENDENT BEHAVIOR OF PILE UNDER LATERAL LOAD USING THE BOUNDING SURFACE MODEL

TIME-DEPENDENT BEHAVIOR OF PILE UNDER LATERAL LOAD USING THE BOUNDING SURFACE MODEL TIME-DEPENDENT BEHAVIOR OF PILE UNDER LATERAL LOAD USING THE BOUNDING SURFACE MODEL Qassun S. Mohammed Shafiqu and Maarib M. Ahmed Al-Sammaraey Department of Civil Engineering, Nahrain University, Iraq

More information

Numerical model comparison on deformation behavior of a TSF embankment subjected to earthquake loading

Numerical model comparison on deformation behavior of a TSF embankment subjected to earthquake loading Numerical model comparison on deformation behavior of a TSF embankment subjected to earthquake loading Jorge Castillo, Yong-Beom Lee Ausenco, USA Aurelian C. Trandafir Fugro GeoConsulting Inc., USA ABSTRACT

More information

Intro to Soil Mechanics: the what, why & how. José E. Andrade, Caltech

Intro to Soil Mechanics: the what, why & how. José E. Andrade, Caltech Intro to Soil Mechanics: the what, why & how José E. Andrade, Caltech The What? What is Soil Mechanics? erdbaumechanik The application of the laws of mechanics (physics) to soils as engineering materials

More information

APPENDIX F CORRELATION EQUATIONS. F 1 In-Situ Tests

APPENDIX F CORRELATION EQUATIONS. F 1 In-Situ Tests APPENDIX F 1 APPENDIX F CORRELATION EQUATIONS F 1 In-Situ Tests 1. SPT (1) Sand (Hatanaka and Uchida, 1996), = effective vertical stress = effective friction angle = atmosphere pressure (Shmertmann, 1975)

More information

EN Eurocode 7. Section 3 Geotechnical Data Section 6 Spread Foundations. Trevor L.L. Orr Trinity College Dublin Ireland.

EN Eurocode 7. Section 3 Geotechnical Data Section 6 Spread Foundations. Trevor L.L. Orr Trinity College Dublin Ireland. EN 1997 1: Sections 3 and 6 Your logo Brussels, 18-20 February 2008 Dissemination of information workshop 1 EN 1997-1 Eurocode 7 Section 3 Geotechnical Data Section 6 Spread Foundations Trevor L.L. Orr

More information

Chapter 12: Lateral Earth Pressure

Chapter 12: Lateral Earth Pressure Part 4: Lateral Earth Pressure and Earth-Retaining Structures Chapter 12: Lateral Earth Pressure Introduction Vertical or near-vertical slopes of soil are supported by retaining walls, cantilever sheetpile

More information

EARTH PRESSURES ON RETAINING STRUCTURES

EARTH PRESSURES ON RETAINING STRUCTURES 12-1 12. EARTH PRESSURES ON RETAINING STRUCTURES 12.1 Active Pressure and Passive Pressure When a sudden change in level of the ground surface is to be provided for some purpose a retaining structure is

More information

LATERAL EARTH PRESSURE AND RETAINING STRUCTURES

LATERAL EARTH PRESSURE AND RETAINING STRUCTURES Topic Outline LATERAL EARTH PRESSURE AND RETAINING STRUCTURES Types of retaining structures Lateral earth pressure Earth pressure at rest Rankine s Theory Coulomb s Theory Cullman s graphic solution Braced

More information

CPT: Geopractica Contracting (Pty) Ltd Total depth: m, Date:

CPT: Geopractica Contracting (Pty) Ltd Total depth: m, Date: The plot below presents the cross correlation coeficient between the raw qc and fs values (as measured on the field). X axes presents the lag distance (one lag is the distance between two sucessive CPT

More information

Cone Penetration Testing in Geotechnical Practice

Cone Penetration Testing in Geotechnical Practice Cone Penetration Testing in Geotechnical Practice Table Of Contents: LIST OF CONTENTS v (4) PREFACE ix (2) ACKNOWLEDGEMENTS xi (1) SYMBOL LIST xii (4) CONVERSION FACTORS xvi (6) GLOSSARY xxii 1. INTRODUCTION

More information

Effect of Frozen-thawed Procedures on Shear Strength and Shear Wave Velocity of Sands

Effect of Frozen-thawed Procedures on Shear Strength and Shear Wave Velocity of Sands Effect of Frozen-thawed Procedures on Shear Strength and Shear Wave Velocity of Sands JongChan Kim 1), *Sang Yeob Kim 1), Shinhyun Jeong 2), Changho Lee 3) and Jong-Sub Lee 4) 1), 4) School of Civil, Environmental

More information

Module 3. DYNAMIC SOIL PROPERTIES (Lectures 10 to 16)

Module 3. DYNAMIC SOIL PROPERTIES (Lectures 10 to 16) Module 3 DYNAMIC SOIL PROPERTIES (Lectures 10 to 16) Lecture 15 Topics 3.6 STRESS-STRAIN BEHAVIOR OF CYCLICALLY LOADED SOILS 3.7 SOME BASIC ASPECTS OF PARTICULATE MATTER BEHAVIOR 3.8 EQUIVALENT LINEAR

More information

PRINCIPLES OF GEOTECHNICAL ENGINEERING

PRINCIPLES OF GEOTECHNICAL ENGINEERING PRINCIPLES OF GEOTECHNICAL ENGINEERING Fourth Edition BRAJA M. DAS California State University, Sacramento I(T)P Boston Albany Bonn Cincinnati London Madrid Melbourne Mexico City New York Paris San Francisco

More information