DISTRIBUTION OF EXPANSIVE SOILS
|
|
- Florence Lyons
- 6 years ago
- Views:
Transcription
1 HOW TO DESIGN?
2 DISTRIBUTION OF EXPANSIVE SOILS
3 WIDE VARIETY OF CLIMATE
4 SAME SOIL -- DIFFERENT CLIMATE
5 RESIDENCE COMPLICATIONS
6 DESIGN NEEDS ENVELOPES
7 EDGE LIFT
8 EDGE DRYING
9 DESIGN AIDS SOIL MOVEMENT SOIL MOVEMENT TABLES SLAB DEFLECTION AND STRESSES SOIL VOLUME CHANGE SOIL MOISTURE VARIATION DISTANCE VERTICAL BARRIERS
10 SOIL SUCTION
11 EXAMPLE: VOLFLO-2 GIVEN VALUES: U WET U DRY Z m U EQUIL. U O n = 2.50 pf = 4.56 pf = ft = 3.31 pf = 1.03 pf = 1 cycle/year
12 SOIL MOVEMENT
13 SOIL MOVEMENT
14 SOIL MOVEMENT
15 SOIL MOVEMENT
16 SOIL MOVEMENT
17 SOIL MOVEMENT TABLES Design Differential Soil Movement, y m, Guide Number for Slab Design Measured Suction pf at Depth, z m, y m Guide Numbers Controlling Surface Suction, pf m Note: The positive sign indicates heave and the negative sign indicates shrinkage.
18 SOIL MOVEMENT TABLES Design Differential Soil Movement, y m, Guide Number for Slab Design: Lawn Irrigation Measured Suction pf at Depth, z m, m y m Guide Numbers Controlling Surface Suction Due to Lawn Watering pf units With 4 ft. Deep Moisture Barrier pf -- units
19 SOIL MOVEMENT TABLES Design Differential Soil Movement, y m, Guide Number for Slab Design: Flower Bed Case (4 ft Deep Flower Bed Moisture) Measured Suction pf at Depth, z m, m y m Guide Numbers Controlling Surface Suction Due to Flower Bed Watering pf units With 4 ft. Deep Moisture Barrier pf -- units
20 SOIL MOVEMENT TABLES Design Differential Soil Movement, y m, Guide Number for Slab Design: Tree Drying Case (Without Moisture Barrier) Depth of Tree Root Zone, ft y m Guide Numbers Measured Equilibrium Suction at Depth, z m pf -- units Movement active zone, z A = 11.5 ft. Movement active zone, z A = 7.5 ft. Movement active zone, z A = 3.5 ft.
21 SOIL MOVEMENT TABLES Design Differential Soil Movement, y m, Guide Number for Slab Design: Tree Drying Case (With Moisture Barrier) Depth of Tree Root Zone, ft y m Guide Numbers Measured Equilibrium Suction at Depth, z m (With 4 ft Deep Moisture Barrier) pf -- units Movement active zone, z A = 11.5 ft. Movement active zone, z A = 7.5 ft.
22 SLAB DEFLECTIONS AND STRESSES EXAMPLE NO. 1 P.T.I. DESIGN MANUAL FLAT SLAB RIBBED SLAB
23
24
25
26
27
28
29
30
31
32
33
34
35
36
37
38
39
40
41
42
43
44
45
46
47
48
49
50
51
52
53
54
55
56
57
58
59
60
61
62
63
64
65
66
67
68
69
70
71 SOIL VOLUME CHANGE CHARTS NATURAL RESOURCES CONSERVATION SERVICE U.S.D.A. DATA BASE (130,000 SAMPLES)
72 EXPANSIVE SOILS ZONES (A. P. COVAR) B-Line PLASTICITY INDEX, % PI = 0.90(LL-8) U-Line Upper Limit of Chart (PI=LL) Any mineral plotting in this zone should be included in ZoneI Montmorillonite 10 VII Halloysites V VI I II PI = 0.85(LL-11) Mixed Minerals PI = 0.81(LL-14) Illites Kaolinites Chlorites LIQUID LIMIT, % PI = 0.73(LL-20) A-Line III IV VIII PI = 0.68(LL-25)
73 EXPANSIVE SOIL VOLUME CHANGE GUIDE NUMBER (A. P. COVAR) ZONE 1
74 EXPANSIVE SOIL VOLUME CHANGE GUIDE NUMBER (A. P. COVAR) ZONE 2
75 EXPANSIVE SOIL VOLUME CHANGE GUIDE NUMBER (A. P. COVAR) ZONE 3
76 EXPANSIVE SOIL VOLUME CHANGE GUIDE NUMBER (A. P. COVAR) ZONE 4
77 EXPANSIVE SOIL VOLUME CHANGE GUIDE NUMBER (A. P. COVAR) ZONE 5
78 EXPANSIVE SOIL VOLUME CHANGE GUIDE NUMBER (A. P. COVAR) ZONE 6
79 EXPANSIVE SOIL VOLUME CHANGE GUIDE NUMBER (A. P. COVAR) ZONE 7
80 EXPANSIVE SOIL VOLUME CHANGE GUIDE NUMBER (A. P. COVAR) ZONE 8
81 VOLUME CHANGE COEFFICIENT, γ h = PERCENT FINE CLAY VOLUME CHANGE GUIDE NUMBER
82 EDGE MOISTURE VARIATION DISTANCE, e m, ft
83 e m (ft), Edge Moisture Variation Distance EDGE MOISTURE VARIATION DISTANCE CENTER LIFT α(cm 2 /sec), Unsaturated Diffusivity Coefficient 0.0E+0 1.0E-3 2.0E-3 3.0E-3 4.0E-3 5.0E-3 6.0E-3 7.0E-3 8.0E-3 VOLUME CHANGE COEFFICIENT (SUCTION COMPRESSION INDEX, γ h ) EDGE LIFT S, Slope of pf--vs--water Content Cuve Percent Passing #200 Sieve (%) LIQUID LIMIT (LL, %) PLASTICITY INDEX (PI, %) -30
84 EFFECT OF VERTICAL MOISTURE BARRIER
85 MOISTURE BARRIER (T = 1.5 ft) Edge Moisture Variation Distance for Moisture Flow, em, ft Depth of Perimeter Beam Below Ground Level or Depth of Vertical Moisture Barrier Below Ground Level, D', FT 6'--5.5' 5' 4.5' 4' 3.5' 3' 2.5' 2' 1.5' 1' D ' T = 1.5 FT Design Value of the Edge Moisture Variation Distance, e' m, ft. T e m '
86 MOISTURE BARRIER (T = 2.0 ft) Edge Moisture Variation Distance for Moisture Flow, em, ft Depth of Perimeter Beam Below Ground Level or Depth of Vertical Moisture Barrier Below Ground Level, D', FT 6' 5.5' 5' 4.5' 4' 3.5' 3' 2.5' 2' 1.5' 1' D ' T T = 2 FT e m ' Design Value of the Edge Moisture Variation Distance, e' m, ft.
87 MOISTURE BARRIER (T = 2.5 ft) Edge Moisture Variation Distance for Moisture Flow, em, ft Depth of Perimeter Beam Below Ground Level or Depth of Vertical Moisture Barrier Below Ground Level, D', FT 6' 5.5' 5' 4.5' 4' 3.5' 3' 2.5' 2' 1.5' 1' D ' T T = 2.5 FT e m ' Design Value of the Edge Moisture Variation Distance, e' m, ft.
88 DESIGN AIDS FOR SLABS ON EXPANSIVE SOILS
4. Soil Consistency (Plasticity) (Das, chapter 4)
4. Soil Consistency (Plasticity) (Das, chapter 4) 1 What is Consistency? Consistency is a term used to describe the degree of firmness of fine-grained soils (silt and clay). The consistency of fine grained
More informationTikrit University. College of Engineering Civil engineering Department SOIL PROPERTES. Soil Mechanics. 3 rd Class Lecture notes Up Copyrights 2016
Tikrit University SOIL PROPERTES College of Engineering Civil engineering Department Soil Mechanics 3 rd Class Lecture notes Up Copyrights 2016 1-Soil Composition -Solids -Water -Air 2-Soil Phases -Dry
More informationGeotechnical 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 informationChapter 1 - Soil Mechanics Review Part A
Chapter 1 - Soil Mechanics Review Part A 1.1 Introduction Geotechnical Engineer is concerned with predicting / controlling Failure/Stability Deformations Influence of water (Seepage etc.) Soil behavour
More informationFOUNDATIONS ON SHRINKING AND SWELLING SOILS (Prediction of Movement, Construction Issues)
FOUNDATIONS ON SHRINKING AND SWELLING SOILS (Prediction of Movement, Construction Issues) by Jean-Louis Briaud, Sangho Moon, Xiong Zhang Department of Civil Engineering, Texas A&M University, College Station,
More informationEffect of Lime on the Compressibility Characteristics of a Highly Plastic Clay
Effect of Lime on the Compressibility Characteristics of a Highly Plastic Clay Abstract İnci Süt-Ünver Ph.D. Candidate Istanbul Technical University Istanbul - Turkey Musaffa Ayşen Lav Prof. Dr. Istanbul
More informationChapter I Basic Characteristics of Soils
Chapter I Basic Characteristics of Soils Outline 1. The Nature of Soils (section 1.1 Craig) 2. Soil Texture (section 1.1 Craig) 3. Grain Size and Grain Size Distribution (section 1.2 Craig) 4. Particle
More informationPREDICTING SOIL SUCTION PROFILES USING PREVAILING WEATHER
PREDICTING SOIL SUCTION PROFILES USING PREVAILING WEATHER Ronald F. Reed, P.E. Member, ASCE rreed@reed-engineering.com Reed Engineering Group, Ltd. 2424 Stutz, Suite 4 Dallas, Texas 723 214-3-6 Abstract
More informationModule 1 GEOTECHNICAL PROPERTIES OF SOIL AND OF REINFORCED SOIL (Lectures 1 to 4)
Module 1 GEOTECHNICAL PROPERTIES OF SOIL AND OF REINFORCED SOIL (Lectures 1 to 4) Topics 1.1 INTRODUCTION 1.2 GRAIN-SIZE DISTRIBUTION Sieve Analysis Hydrometer Analysis 1.3 SIZE LIMITS FOR SOILS 1.4 WEIGHT-VOLUME
More informationBehavior of Expansive Soil Treated by using Different Electrolyte Substances
Behavior of Expansive Soil Treated by using Different Electrolyte Substances Ahmed T. M. Farid Geotechnical Institute Housing and National Building Research Center, (HBRC) Cairo, Egypt atfarid2013@gmail.com
More informationREPORT ON THE ASSESSMENT OF TRENCHING INTHE ROAD RESERVE OF THE ROAD BETWEEN BEAUFORT WEST AND CARNAVON.
Contract Report CSIR/BE/TIE/SKA/59E2214 August 2018 REPORT ON THE ASSESSMENT OF TRENCHING INTHE ROAD RESERVE OF THE ROAD BETWEEN BEAUFORT WEST AND CARNAVON. Authors: Dave Ventura Anele Sambo Michael Roux
More informationEffect on Engineering properties of Black Cotton Soil by Alkali Content Sodium Hydroxide (NaOH)
IJIRST International Journal for Innovative Research in Science & Technology Volume 2 Issue 09 February 2016 ISSN (online): 2349-6010 Effect on Engineering properties of Black Cotton Soil by Alkali Content
More informationSOIL FORMATION SOIL CLASSIFICATION FOR GEOTECHNICAL ENGINEERS. Soil Properties and Classification
SOIL CLASSIFICATION FOR GEOTECHNICAL ENGINEERS Soil Properties and Classification Soil Formation Soil Types Particle Size Analysis and Grading Characteristics Consistency Indices Engineering classification
More informationCHAPTER: 4 PLASTICITY OF SOILS
CHAPTER: 4 PLASTICITY OF SOILS CONTENTS: Plasticity characteristics of soils, Atterberg limits, determination of shrinkage limit, plasticity, liquidity & consistency indexes, thixotropy, activity of soil,
More informationGeology 229 Engineering Geology. Lecture 8. Elementary Soil Mechanics (West, Ch. 7)
Geology 229 Engineering Geology Lecture 8 Elementary Soil Mechanics (West, Ch. 7) Outline of this Lecture 1. Introduction of soil properties 2. Index properties of soils Soil particles Phase relationship
More informationProf. B V S Viswanadham, Department of Civil Engineering, IIT Bombay
05 Clay particle-water interaction & Index properties Electrical nature of clay particles a) Electrical charges i) The two faces of all platy particles have a negative charge. Resulting due to isomorphous
More informationIntroduction 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 informationName Date Class. biota climate decomposition horizon organic matter parent material pore sediment soil topography. Clues
Content Vocabulary Directions: Use the clues and the terms listed below to complete the puzzle. NOTE: There is no empty square in the puzzle between the words of two-word terms. Some words may not be used.
More informationSwell and Shrinkage Strain Prediction Models for Expansive Clays
Boise State University ScholarWorks Civil Engineering Faculty Publications and Presentations Department of Civil Engineering 1-26-2014 Swell and Shrinkage Strain Prediction Models for Expansive Clays Anand
More informationDEFINITION OF EXPANSION POTENTIAL FOR EXPANSIVE SOIL John D. Nelson 1,2, Kuo-Chieh Chao 2 & Daniel D. Overton 2
DEFINITION OF EXPANSION POTENTIAL FOR EXPANSIVE SOIL John D. Nelson 1,2, Kuo-Chieh Chao 2 & Daniel D. Overton 2 1 ) Colorado State University, USA 2 ) Tetra Tech, Inc., USA Abstract: Expansion potential
More informationShear 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 informationCyclic 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 informationSlake Durability of a Deep Red Stratum Sandstone under Different Environments
An Interdisciplinary Response to Mine Water Challenges - Sui, Sun & Wang (eds) 2014 China University of Mining and Technology Press, Xuzhou, ISBN 978-7-5646-2437-8 Slake Durability of a Deep Red Stratum
More informationFarimah MASROURI. Professor in Geotechnical Engineering. LAEGO : Research Center In Geomechanics & Geoenvironmental Engineering
Farimah MASROURI Professor in Geotechnical Engineering LAEGO : Research Center In Geomechanics & Geoenvironmental Engineering Nancy Université France http://www.laego.org 1/29 Nancy 90 min by TGV Paris
More informationA. V T = 1 B. Ms = 1 C. Vs = 1 D. Vv = 1
Geology and Soil Mechanics 55401 /1A (2002-2003) Mark the best answer on the multiple choice answer sheet. 1. Soil mechanics is the application of hydraulics, geology and mechanics to problems relating
More informationGeology and Soil Mechanics /1A ( ) Mark the best answer on the multiple choice answer sheet.
Geology and Soil Mechanics 55401 /1A (2003-2004) Mark the best answer on the multiple choice answer sheet. 1. Soil mechanics is the application of hydraulics, geology and mechanics to problems relating
More informationProject: ITHACA-TOMPKINS REGIONAL AIRPORT EXPANSION Project Location: ITHACA, NY Project Number: 218-34 Key to Soil Symbols and Terms TERMS DESCRIBING CONSISTENCY OR CONDITION COARSE-GRAINED SOILS (major
More informationHardened Concrete. Lecture No. 16
Hardened Concrete Lecture No. 16 Fatigue strength of concrete Modulus of elasticity, Creep Shrinkage of concrete Stress-Strain Plot of Concrete At stress below 30% of ultimate strength, the transition
More informationP.E. Civil Exam Review: GEOMECHANICS. Jerry Vandevelde, P.E.
P.E. Civil Exam Review: GEOMECHANICS Jerry Vandevelde, P.E. gtv@gemeng.com GEOMECHANICS National Council of Examiners for Engineering and Surveying http://www.ncees.org/ 3 STUDY REFERENCES Foundation Engineering;
More informationTeaching Unsaturated Soil Mechanics as Part of the Undergraduate Civil Engineering Curriculum
Teaching Unsaturated Soil Mechanics as Part of the Undergraduate Civil Engineering Curriculum Delwyn G. Fredlund, Visiting Professor Kobe University, Kobe, Japan Sapporo, Hokkaido, Japan February 15, 2005
More informationThis document downloaded from vulcanhammer.net vulcanhammer.info Chet Aero Marine
This document downloaded from vulcanhammer.net vulcanhammer.info Chet Aero Marine Don t forget to visit our companion site http://www.vulcanhammer.org Use subject to the terms and conditions of the respective
More informationUnbound Pavement Applications of Excess Foundry System Sands: Subbase/Base Material
Unbound Pavement Applications of Excess Foundry System Sands: Subbase/Base Material Tuncer B. Edil University of Wisconsin-Madison Recycled Materials Resource Center RMRC Participant Job Description Which
More informationCopyright SOIL STRUCTURE and CLAY MINERALS
SOIL STRUCTURE and CLAY MINERALS Soil Structure Structure of a soil may be defined as the mode of arrangement of soil grains relative to each other and the forces acting between them to hold them in their
More informationConsolidation Properties of NAPL Contaminated Sediments
Consolidation Properties of NAPL Contaminated Sediments M. B. Erten 1, C. S. El Mohtar 2, D. D. Reible 3, R. B. Gilbert 4 1 Graduate Research Assistant, University of Texas at Austin, 1 University Station
More informationUnsaturated Flow (brief lecture)
Physical Hydrogeology Unsaturated Flow (brief lecture) Why study the unsaturated zone? Evapotranspiration Infiltration Toxic Waste Leak Irrigation UNSATURATAED ZONE Aquifer Important to: Agriculture (most
More informationDr. Ravi Kant mittal. CE C361 Soil Mechanics and Foundation Engg. 1
Dr. Ravi Kant mittal Assistant Professor, BITS Pilani E- Mail: ravi.mittal@rediffmai.com ravimittal@bits-pilani.ac.in Mobile: 9887692025 CE C361 Soil Mechanics and Foundation Engg. 1 Contents Soil Formation
More informationTable 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 informationTikrit University College of Engineering Civil engineering Department
Tikrit University SOIL CLASSIFICATION College of Engineering Civil engineering Department Soil Mechanics 3 rd Class Lecture notes Up Copyrights 2016 Classification of soil is the separation of soil into
More informationThis procedure covers the determination of the moment of inertia about the neutral axis.
327 Sample Problems Problem 16.1 The moment of inertia about the neutral axis for the T-beam shown is most nearly (A) 36 in 4 (C) 236 in 4 (B) 136 in 4 (D) 736 in 4 This procedure covers the determination
More informationMass Movements and Hillslopes
Mass Movements and Hillslopes Erosion (or lack of) results from balance between internal resistance of materials & magnitude of external forces acting on them Evolution of landscapes depends largely on
More informationProf. B V S Viswanadham, Department of Civil Engineering, IIT Bombay
06 Index properties Review Clay particle-water interaction Identification of clay minerals Sedimentation analysis Hydrometer analysis 0.995 20-40 Hydrometer is a device which is used to measure the specific
More informationBeam Design - Pine Tree
- Pine Tree 1. Beam Data Load Type: Uniform Dist. Load Support: Simple Beam Beam Type: Sawn Lumber Species: Southern Pine Grade: SP DSS Size: 2 x 8 Design Span (L): 11.83 ft. Clear Span: 11.67 ft. Total
More informationSOIL TYPE INVESTIGATION OF THE DOĞANHİSAR CLAYS, CENTRAL ANATOLIA, TURKEY. İ.İnce* and A. Özdemir
Ozean Journal of Applied Sciences 3(3), 2010 ISSN 1943-2429 2010 Ozean Publication SOIL TYPE INVESTIGATION OF THE DOĞANHİSAR CLAYS, CENTRAL ANATOLIA, TURKEY İ.İnce* and A. Özdemir Department of Geological
More informationBuilding Science. Some Interesting Stuff on Slabs. Water Flow Through Slab. Mechanisms of Flow. buildingscience.com 9/25/09
Water Flow Through Slab Joseph Lstiburek, Ph.D., P.Eng Building Science Some Interesting Stuff on Slabs From under the slab From the edge of the slab From the slab itself presented by www.buildingscience.com
More informationBeam Design - Shed Roof Back Wall Beam-S
Beam Design - Shed Roof Back Wall Beam-S 1. Beam Data Load Type: Uniform Dist. Load Support: Simple Beam Beam Type: Glulam Species: Western Species Grade: 24F-V4 1.8E DF/DF Size: 2.5 x 6 Design Span (L):
More informationClass 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 informationBeam Design - FLOOR JOIST
Beam Design - FLOOR JOIST 1. Beam Data Load Type: Uniform Dist. Load Support: Simple Beam Beam Type: Sawn Lumber Species: Douglas Fir-Larch Grade: DF No.2 Size: 2 x 10 Design Span (L): 11.83 ft. Clear
More informationBeam Design - Trotin Project
Beam Design - Trotin Project 1. Beam Data Load Type: Uniform Dist. Load Support: Simple Beam Beam Type: Glulam Species: Western Species Grade: 24F-V4 1.8E DF/DF Size: 3.125 x 13.5 Design Span (L): 14.98
More information2012 Road School Light Weight Deflectometer (LWD)
2012 Road School Light Weight Deflectometer (LWD) Nayyar Siddiki, M.S., P.E. Office of Geotechnical Services Outline Testing for Compaction NO 53 and chemically modified soils (Special Prov.) Changing
More informationCh. 4 - Clay Minerals, Rock Classification Page 1. Learning Objectives. Wednesday, January 26, 2011
Ch. 4 - Clay Minerals, Rock Classification Page 1 Learning Objectives Ch. 4 - Clay Minerals, Rock Classification Page 2 Symbols Ch. 4 - Clay Minerals, Rock Classification Page 3 Clay Minerals and Structure
More informationQUESTION 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 informationSoil Mechanics Brief Review. Presented by: Gary L. Seider, P.E.
Soil Mechanics Brief Review Presented by: Gary L. Seider, P.E. 1 BASIC ROCK TYPES Igneous Rock (e.g. granite, basalt) Rock formed in place by cooling from magma Generally very stiff/strong and often abrasive
More informationIntroduction to Soil Mechanics Geotechnical Engineering-II
Introduction to Soil Mechanics Geotechnical Engineering-II ground SIVA Dr. Attaullah Shah 1 Soil Formation Soil derives from Latin word Solum having same meanings as our modern world. From Geologist point
More informationOutline. In Situ Stresses. Soil Mechanics. Stresses in Saturated Soil. Seepage Force Capillary Force. Without seepage Upward seepage Downward seepage
Soil Mechanics In Situ Stresses Chih-Ping Lin National Chiao Tung Univ. cplin@mail.nctu.edu.tw Outline Without seepage Upward seepage Downward seepage Seepage Force The total stress at the elevation of
More informationCONSOLIDATION OF SOIL
Lecture-6 Soil consolidation Dr. Attaullah Shah 1 CONSOLIDATION OF SOIL When a soil mass is subjected to a compressive force there is a decrease in volume of soil mass. The reduction in volume of a saturated
More informationPrinciples 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 informationThe Effects of Water Contents on Free Swelling of Expansive Soil
International Journal of Civil & Environmental Engineering IJCEE-IJENS Vol:12 No:6 13 The Effects of Water Contents on Free Swelling of Expansive Agus Tugas Sudjianto 1), M. Cakrawala 1) and Candra Aditya
More informationExpansive soils and practice in foundation engineering
Expansive soils and practice in foundation engineering Jay X. Wang, Ph.D., P.E. Programs of Civil Engineering and Construction Engineering Programs Louisiana Tech University 1 Facts about expansive soils
More informationClay Robinson, PhD, CPSS, PG copyright 2009
Engineering: What's soil got to do with it? Clay Robinson, PhD, CPSS, PG crobinson@wtamu.edu, http://www.wtamu.edu/~crobinson, copyright 2009 Merriam-Webster Online Dictionary soil, noun 1 : firm land
More informationGEOLOGICAL PROCESSES AND MATERIALS SGM210
University of Pretoria GEOLOGICAL PROCESSES AND MATERIALS SGM210 22 April 2014 1 GEOLOGICAL MAPS 1. Dip 2. Strike 3. Faults 2 1 2 FAULTS 3 San Andreas Fault 3 14 18" 26" JJJ' 22 4 (.) 5I cr w o(aigcegroup,
More informationIntegrated Ground Behavior
Integrated Ground Behavior Part A: Particle-level Phenomena & Macroscale Behavior (J. Carlos Santamarina) Georgia Institute of Technology fluid particles microorganisms mineral size shape surface charge
More informationAssessment of accuracy in determining Atterberg limits for four Iraqi local soil laboratories
IOP Conference Series: Materials Science and Engineering PAPER OPEN ACCESS Assessment of accuracy in determining Atterberg limits for four Iraqi local soil laboratories To cite this article: H O Abbas
More informationGG 454 January 18, SOILS (06)
GG 454 January 18, 2002 1 SOILS (06) I Main Topics A Pedologic classification schemes B Engineering classification schemes C Behavior of soils and influence of geologic history II Pedologic classification
More informationSOILS/AGGREGATE TECHNICIAN REVIEW
(8:00 to 4:00) SOILS/GGREGTE TECHNICIN REVIEW Intro TTI Safety Rounding Procedure Thursday RIZ 201 SHTO T 11 RIZ 210 SHTO T 19 RIZ 211 SHTO T 255 RIZ 212 RIZ 233 RIZ 236 RIZ 225 RIZ 245 SHTO T 89 SHTO
More informationMonitoring of Moisture Fluctuations in a Roadway over an Expansive Clay Subgrade
Monitoring of Moisture Fluctuations in a Roadway over an Expansive Clay Subgrade Christian P. Armstrong, M.S., S.M.ASCE 1 and Jorge G. Zornberg, Ph.D., P.E., F.ASCE 2 1 Ph.D. Candidate, Department of Civil
More informationEffect of Suction on the Resilient Modulus of Compacted Fine- Grained Subgrade Soils
THE UNIVERSITY OF WISCONSIN-MADISON Effect of Suction on the Resilient Modulus of Compacted Fine- Grained Subgrade Soils by Auckpath Sawangsuriya, Ph.D. Tuncer B. Edil, Ph.D., P.E. Craig H. Benson, Ph.D.,
More informationFUNDAMENTALS 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 informationTesting of an expansive clay in a centrifuge permeameter
Plaisted, M.D., and Zornberg, J.G. (2010). Testing of an Expansive Clay in a Centrifuge Permeameter. Proceedings of the 7th International Conference on Physical Modelling in Geotechnics (ICPMG 2010), Zurich,
More informationCalculation of 1-D Consolidation Settlement
Calculation of 1-D Consolidation Settlement A general theory for consolidation, incorporating threedimensional flow is complicated and only applicable to a very limited range of problems in geotechnical
More information12 SWAT USER S MANUAL, VERSION 98.1
12 SWAT USER S MANUAL, VERSION 98.1 CANOPY STORAGE. Canopy storage is the water intercepted by vegetative surfaces (the canopy) where it is held and made available for evaporation. When using the curve
More informationChapter (6) Geometric Design of Shallow Foundations
Chapter (6) Geometric Design of Shallow Foundations Introduction As we stated in Chapter 3, foundations are considered to be shallow if if [D (3 4)B]. Shallow foundations have several advantages: minimum
More informationGeoShanghai 2010 International Conference Paving Materials and Pavement Analysis
Particle Shape, Type and Amount of Fines, and Moisture Affecting Resilient Modulus Behavior of Unbound Aggregates Debakanta Mishra 1, Erol Tutumluer 2, M. ASCE, Yuanjie Xiao 3 1 Graduate Research Assistant,
More informationClimate effects on landslides
GEORAMP ONE DAY SYMPOSIUM Climate effects on landslides E. E. Alonso, M. Sondón, N. M. Pinyol Universitat Politècnica de Catalunya October 14th, 2016. UPC, Barcelona Infiltration (evaporation) and slope
More informationSoil Water Atmosphere Plant (SWAP) Model: I. INTRODUCTION AND THEORETICAL BACKGROUND
Soil Water Atmosphere Plant (SWAP) Model: I. INTRODUCTION AND THEORETICAL BACKGROUND Reinder A.Feddes Jos van Dam Joop Kroes Angel Utset, Main processes Rain fall / irrigation Transpiration Soil evaporation
More informationSolution:Example 1. Example 2. Solution: Example 2. clay. Textural Soil Classification System (USDA) CE353 Soil Mechanics Dr.
CE353 Soil Mechanics CE353 Lecture 5 Geotechnical Engineering Laboratory SOIL CLASSIFICATION Lecture 5 SOIL CLASSIFICATION Dr. Talat A Bader Dr. Talat Bader 2 Requirements of a soil Systems Why do we need
More informationDesiccation Cracking of Soils
Desiccation Cracking of Soils Lyesse Laloui Hervé Péron, Tomasz Hueckel, Liangbo Hu Ecole Polytechnique Fédérale de Lausanne Switzerland Duke University, NC USA The consequences of desiccation cracking
More information10 Slope Stability Analysis of a Rock Slope
Slope Stability Analysis of a Rock Slope 10-1 10 Slope Stability Analysis of a Rock Slope 10.1 Problem Statement Limit equilibrium methods are commonly used to evaluate the stability of slopes in rock
More informationSWELLING POTENTIAL OF THE RESIDUAL SOIL, BASED ON PLASTICITY INDEX VALUE AT MUAROSIJUNJUNG, WEST SUMATERA
SWELLING POTENTIAL OF THE RESIDUAL SOIL, BASED ON PLASTICITY INDEX VALUE AT MUAROSIJUNJUNG, WEST SUMATERA Faiq NIRMALA* and Yanwar Yusup RUKMANA Faculty of Geological Engineering, Universitas Padjadjaran,
More informationSection 5.1 Weathering This section describes different types of weathering in rocks.
Section 5.1 Weathering This section describes different types of weathering in rocks. Reading Strategy Building Vocabulary As you read the section, define each vocabulary term. For more information on
More informationB-1 BORE LOCATION PLAN. EXHIBIT Drawn By: 115G BROOKS VETERINARY CLINIC CITY BASE LANDING AND GOLIAD ROAD SAN ANTONIO, TEXAS.
N B-1 SYMBOLS: Exploratory Boring Location Project Mngr: BORE LOCATION PLAN Project No. GK EXHIBIT Drawn By: 115G1063.02 GK Scale: Checked By: 1045 Central Parkway North, Suite 103 San Antonio, Texas 78232
More informationPredicting Erosion Rates of Cohesive Streambanks
Predicting Erosion Rates of Cohesive Streambanks * Donovan M, A Miller, M Baker, A Gellis. 2015. Sediment contributions from floodplains and legacy sediments to Piedmont streams of Baltimore County, Maryland.
More informationParticularity of plasticity characteristics of fine glacial materials (North Chicago area)
J. CONSTANTINESCU, D. CONSTANTINESCU Particularity of plasticity characteristics of fine glacial materials (North Chicago area) Juliana CONSTANTINESCU (1), Damian CONSTANTINESCU (2) (1) Department of Physics,
More informationEvaluating Structural Performance of Base/Subbase Materials at the Louisiana Accelerated Pavement Research Facility
Evaluating Structural Performance of Base/Subbase Materials at the Louisiana Accelerated Pavement Research Facility Zhong Wu, Ph.D., P.E. Zhongjie Zhang, Bill King Louay Mohammad Outline Background Objectives
More informationEvapotranspiration. Rabi H. Mohtar ABE 325
Evapotranspiration Rabi H. Mohtar ABE 325 Introduction What is it? Factors affecting it? Why we need to estimate it? Latent heat of vaporization: Liquid gas o Energy needed o Cooling process Saturation
More informationSOIL CLASSIFICATION CHART COARSE-GRAINED SOILS MORE THAN 50% RETAINED ON NO.200 SIEVE FINE-GRAINED SOILS 50% OR MORE PASSES THE NO.200 SIEVE PRIMARY DIVISIONS GRAVELS MORE THAN 50% OF COARSE FRACTION RETAINED
More informationClays and Clay Minerals
Clays and Clay Minerals Fields of interest for clays Various definitions Acients: Earths in the earth-air-fire-water system Definition of clay depends on discipline: Geologist grain size
More informationBeam Design - Awning
Beam Design - Awning 1. Beam Data Load Type: Uniform Dist. Load Support: Simple Beam Beam Type: Sawn Lumber Species: Douglas Fir-Larch Grade: DF No.2 Size: 4 x 12 Design Span (L): 21.50 ft. Clear Span:
More informationCE 240 Soil Mechanics & Foundations Lecture 5.2. Permeability III (Das, Ch. 6) Summary Soil Index Properties (Das, Ch. 2-6)
CE 40 Soil Mechanics & Foundations Lecture 5. Permeability III (Das, Ch. 6) Summary Soil Index Properties (Das, Ch. -6) Outline of this Lecture 1. Getting the in situ hydraulic conductivity 1.1 pumping
More informationApplication of DCP in Prediction of Resilient Modulus of Subgrade Soils
Application of DCP in Prediction of Resilient Modulus of Subgrade Soils Louay Mohammad, Ph.D. Louisiana Transportation Research Center Louisiana State University 2006 Pavement Performance Seminar April
More informationAssistant Prof., Department of Civil Engineering Bhagwant University,Ajmer,Rajasthan,India ABSTRACT
Study of Index Properties of the Soil 1 Mr Utkarsh Mathur 2 Mr Nitin Kumar 3 Mr Trimurti Narayan Pandey 4 Mr.Amit Choudhary 1 PG Scholar, Department of Civil Engineering Bhagwant University,Ajmer,Rajasthan,India
More informationThis is start of the single grain view
SOIL TEXTURE, PARTICLE SIZE DISTRIBUTION, SPECIFIC SURFACE AND CLAY MINERALS We will assess the physical realm of soil science in a piecewise fashion starting with the physical phases of soil, -- a single
More informationDrying shrinkage of deformable porous media: mechanisms induced by the fluid removal
Drying shrinkage of deformable porous media: mechanisms induced by the fluid removal L.B. Hu 1, H. Péron 2, T. Hueckel 1 and L. Laloui 2 1 Department of Civil and Environmental Engineering, Duke University,
More informationIdentification of Expansive Soils and Assessment of Expansion Potential by Fuzzy Approach
Identification of Expansive Soils and Assessment of Expansion Potential by Fuzzy Approach P. Venkata Subba Reddy Department of Computer Science and Engineering, Sri Venkateswara University, Tirupati, India
More informationCorrelation of unified and AASHTO soil classification systems for soils classification
Journal of Earth Sciences and Geotechnical Engineering, vol. 8, no. 1, 2018, 39-50 ISSN: 1792-9040 (print version), 1792-9660 (online) Scienpress Ltd, 2018 Correlation of unified and AASHTO classification
More informationGLY 363 Seminar : Residual Dolerite Group
GLY 363 Seminar : Residual Dolerite Group 16 1 1 1. Introduction 2. Formation 3. Characteristics 4. Engineering Properties 5. Engineering problems 6. Engineering uses 7. Conclusion 8. References GLY 363
More informationMoulding and Casting Methods 2. Greensand system
MME 345, Lecture 22 Moulding and Casting Methods 2. Greensand system Ref: [1] Heine, Loper & Rosenthal, Principles of Metal Casting, McGraw-Hill, 1976 [2] Beeley, Foundry Technology, Butterworth-Heinemann,
More informationK Design Graphs and Charts for Raft Foundations Spanning Local Depressions
K Design Graphs and Charts for Raft Foundations Spanning Local Depressions The reader is advised to read the text in Chapter 13 before using these charts. The charts and figures are repeated here for quick
More informationINTRINSIC COMPRESSION CHARACTERISTICS OF AN EXPANSIVE CLAY FROM WESTERN AUSTRALIA
Geotec., Const. Mat. & Env., ISSN: 2186-2990, Japan; DOI: http://dx.doi.org/10.21660/2017.29.20455 INTRINSIC COMPRESSION CHARACTERISTICS OF AN EXPANSIVE CLAY FROM WESTERN AUSTRALIA *Farzad Habibbeygi 1,
More informationINTERPRETATION 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 informationNHBRA SOIL LABORATORY SECTION INTERIM REVISED TEST RATES FOR THE MATERIALS LABORATORY
NHBRA SOIL LABORATORY SECTION INTERIM REVISED TEST RATES FOR THE MATERIALS LABORATORY DATE OF REVISION: ) 10th October 2010 S/N TEST DESCRIPTION UNIT RATE REMARKS 1 Sieve Analysis (wet and dry methods
More information