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In situ Testing and Soil Properties Correlation PDF

135 Pages·2016·9.58 MB·English
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n situ Testings and Soil Properties Correlations 1000 Nf 500 AVERAGE TREND FOR TICINO SAND TESTED IN ITALIAN 300 CALIBRATION CHAMBERS 200 о < 1— CO 100 CO Ш ш О MONTEREY SAND 50 • ERKSAK SAND о * OTTAWA SAND Ш ) (NGI Ш" a f HOo»SnNDl SOUTHAMPTON UN D ) ( ENEL CRIS V HILTON MINES SAND СИ A TICINO SAND, GOLDER & ASSOCIATES о I I 1 1 -1.0 -0.8 -0.6 -0.4 -0.2 -0.0 -0.2 NORMALIZED STATE PARAMETER * Ул-Г * emax 6 r in conjunction with International Conference on In Situ Measurement of Soil Properties and Case Histories Bali-Indonesia, May 21-24,2007 Iniitu Testing and Soil Properties Correlation P r e f a ce The use of in situ testing has been widely gained popularity to establish general soil profile and to derive soil parameters to be used in design and geotechnicai analysis. The use of CPT, SPT, DMT and PMT for ground improvement control has also been accepted by practical engineers. Nowadays the addition of sensors and testing technology has caused -even positive development in the practice of geotechnicai engineering. The main advantages of the present use of in situ testing derives its favor from the fact that empirical correlation has been so much developed and may be used to accurately estimate the parameters. These publications of correlation are scattered everywhere, in the seminar and conference proceedings, in journals, and research reports. By effort of the graduate students of the Parahyangan Catholic University, they have tried to put all these together to make the most practical and handy application of the in situ testing results. This publication is nothing but the first embryo of the effort. Although many other publications have not been included in this book, we believe that the present collection is advantageous as reference for every geotechnicai engineer. Comprehensive examples rather than simple interpretation has been added in the final chapter to enable further thought towards a more rational application of the empirical correlations. Finally we expect that this book will be beneficial for everyone who use it and for students who want to go deeper into the geotechnicai engineering practice. We apologize for incompleteness of the published correlation which has not been included in the book. In the future this effort will be continued to update with the state of the art so that this book will be more acceptable and more useful. Bandung, May 12, 2001 Paulus P. Rahardio Geotechnics Laboratory Parahyangan Catholic University In SFtli Z001 I Itiiitu Testing and Soil propertie Correlation T A B LE OF C O N T E NT PREFACE CHAPTER 1. IN SITU TESTING DEVICE AND TEST PROCEDURE 1-1 1.1. Vane Shear Test (VST) 1-1 1.2. Bore Hole Shear Test (BST) 1-2 1.3. Standard Penetration Test (SPT) 1-3 1.4. Cone Penetration Test (CPT) 1-4 1.5. DilatometerTest (DMT) 1-6 1.6. Pressuremeter Test (PMT) 1-7 CHAPTER 2. ENGINEERING PROPERTIES OF SOILS 2.1-1 2.1. Soil Classification and Weight Volume Relationship 2.1-1 2.2. Soil Plasticity 2.2-1 2.3. Permeability 2.3-1 2.4. In Situ Stress and State Parameter 2.4-1 2.5. Shear Strength 2.5-1 2.5.2. Undrained Shear Strength of Clays 2.5-4 2.6. Compressibility and Consolidation Characteristics 2.6-1 2.7. Stiffness and Shear Rigidity 2.7-1 2.7.1. Applicability of Strains in Various Construction 2.7-1 2.8. Expansive Soils 2.8-1 CHAPTER 3. USE IN SITU TESTING TO IDENTIFY SOIL TYPES AND SOIL BEHAVIOUR TYPES 3-1 CHAPTER 4. IN SITU TESTING FOR PREDICTION OF DENSITY OF SOILS AND STATE PARAMETERS 4-1 CHAPTER 5. IN SITU TESTING FOR PREDICTION OF IN SITU STRESS AND STRESS HISTORY 5-1 5.1. Prediction of Preconsolidation Pressure or Yield Stress 5-1 5.2. Prediction of Overconsolidation Ratio (OCR) 5-3 5.3. Prediction of Horizontal Stress and K 5-7 0 CHAPTER 6. MEASUREMENT OF SHEAR STRENGTH BY IN SITU TESTINGS 6-1 6.1. Drained Shear Strength of Sand 6-1 6.1.1. Prediction of Ф' by SPT 6-1 6.1.2. Prediction of ф' by CPT 6-4 6.1.3. Prediction off by Dilatometer 6-6 6.2. -Effective Friction Angles of All Soils 6-7 6.3. Undrained Shear Strength of Clays 6-8 6.3.1. Shear Strength of Clays by SPT 6-8 6.3.2. Shear Strength of Clays by CPT 6-8 6.3.3. Shear Strength of Clays by Dilatometer Test 6-11 6.3.4. Shear Strength of Chalk by CPT ^-11 In Situ zooi ii imitu letting and Soil propertie Correlation CHAPTER 7. IN SITU TESTING TO ESTIMATE SOIL STIFFNESS AND SHEAR RIGIDITY 7-1 CHAPTER 8. IN SITU TESTING TO ESTIMATE CONSOLIDATION CHARACTERISTIC 8-1 CHAPTER 9. IN SITU TESTING FOR EVALUATION OF LIQUEFACTION POTENTIAL 9-1 CHAPTER 10. COMPARISON BETWEEN THE RESULTS OF IN SITU TEST 10-1 CHAPTER 11. COMPREHENSIVE EXAMPLE 11-1 11.1. SPT and CPT Interpretation on Clays 11-1 11.2. SPT and CPT Interpretation of Sand Layer 11-6 11.3. CPTU Interpretation in Soft Alluvial Soils 11-11 REFERENCES InSituzooi • " iii CHAPTER 1 1№ШТ№Т^ШЙ@ ВЕЙ AND TEST PROCEDURE Chapter! in Situ Taring Device and Tat Procedure CHAPTER 1 IN SITU TESTING DEVICE AND TEST PROCEDURE 1.1. VANE SHEAR TEST (VST) Device : • Four-bladed rectangular vane (Normally H/D = 2) • Rotating rod • Torque measuring device Test Procedure : Test carried out in a borehole or directly pushing the vane into the ground. It is important that the vane is pushed ahead of disturbance caused by vane housing or drilling operations. The vane rod is then rotated at a rate of 6°/min., while the torque is read at interval of 30 s. After maximum torque isachieved, the^ yane is rotated at higher rate to Obtainг thef remolded-strengthof the^soiis. Measured Parameters: fir, peak • Peak torque (т к) => греак=~ч Fig. 1.1.1 Swedish Vane Borer реа 6Т Г1 • Residual torque (^residual) => Muastmng irii Factors Affecting Results: 1. Disturbance due to vane insertion 2. Blade thickness 3. Rate of rotation -Squortlw 4. Time lapse between insertion of the vane and the beginning of the test 5. Strength anisotropy 6. Type of soils .-Casing 7. Possible friction of the rod and surrounding soils 8. Failure planes around the vanes ■Bdbtwring spacer Corrections for Interpretation: ■Ffietafttfiminoioc <Ь5и Skempton recommended multiplying the vane diameter by 1.05 for interpretation of strength and Bjerrum has used plasticity index to •Vane incorporate field strength to vane shear strength (see chapter 6). Fig. 1.1,2. Details of VST (Ortigao & Collet, 1988) 1.2. BOREHOLE SHEAR TEST (BST> Device: • Shear head • Pressure source • Pulling Yoke • Cabling • Control/measuring unit Test Procedure: Shear head is lowered in a borehole to perform the test. At the required position the two shear plates are expanded until seated in a borehole walls at preselected pressure. Some time is allowed for consolidation to occur. When consolidation is complete the shear head is either pulled upward, or pushed downwards at a steady rate of 2 mm/ min. Thje required forces for shearing are measured, and the shearing stress :,pjs£ted=aga!ns£^he^^aki3^^^ the shear plates may be contracted, the shear head lowered to its original position, rotated 90° and the test repeated. The shear head is then returned to the original position, another seating pressure selected and the test repeated. Tranducers Factors affecting results : • Drainage condition — Deairing Ports • Disturbance and size of drilling hole Porous Stones 100 kPa D_£i Shear Head Fig. 1.2.1. The Iowa Borehole Shear Device (BSH fWineland. 1975^ I. Normal Stress, psi Fig. 1 -? о Typical Results tettezwi- 1-2 -i* Спарил. In Situ Tating Dora and let Procedure 1.3. STANDARD PENETRATION TEST (SPT) Device = • Split spoon sampler $ • Hammer (63.5 kg) • Rods Test Procedure : Automatic 63.5 kg free drop trip hammer ('Monkey! Test carried out in a borehole by lowering the split spoon sampler and driving it using repeated blows Striker plate by the hammer freely dropped at falling height of 762 mm at the top of the borehole. Blow count is Connector to 32mm rods recorded 3 times, each 150 mm penetration and the N value is the sum of the blow count of the last 300 Round 'A' tods mm penetration as blows/300 mm. or square 32mm boring rods Measured Parameters: Spill spoon N blows/30 cm —.—"О*- Standard cutting shoe Corrections for blow count: 60* cone (0( gravel. 0i) and overburden pressure (С ) ы Fig. 1.3.1. Equipment For The Ni(60) «TJ.CN-N Standard Penetration Test Factors Affecting Results: 1. Variations in the test apparatus 2. Disturbance and size of drilling hole 3. Type and consistency or density of soils 4. Confining pressure or overburden pressure 5. Energy 6. Drainage condition 7. Disturbance and size of drilling hole Types of Hammers : 1. Automatic Trip Hammers 2. Slip-Rope-Hammers (pin weight hammer, safety and donut hammer) Fig. 1.3.2. Sections through American SPT slip- rope hammers (a) pin weight hammer (b) safety hammer (c) donut hammer (Riggs, 1986) in Situ zoo) 1-3 flapttn. In Situ feting Device and Tes tProcedure 1.4. CONE PENETRATION TEST fCPT> Device : • Cone D=15 • Friction sleeve • Pore pressure transducer (for piezocone) .D-12.5 .D-30 • Other sensors (if any) • Rods fl • Control/ measuring device E=2p Types of Cone : D-36- • Mechanical cone tei • Electric cone Test Procedure : Test is carried out by mechanically or D-23 «rf hydraulically pushing a cone into the ground at a constant speed (2 cm/s) whilst measuring the tip and shear force, for piezocone, pore pressure is measured along depth of penetration and a d isslpa" ^ -^| Y; an =№=perfcWi^~ara"n"yiTe"q u i red n s C D=32.5 depth by stopping the penetration and measuring the decay of pore water pressure with time. It is recommended that the dissipation be continued to D=35.7; at least 50% degree of dissipation. Measured Parameters : (Dimensions are in mm) Fig. 1.4.1, Begemann Mechanical • Tip resistance, q (kg/cm2) c Friction Cone fMeiah, • Friction resistance, f (kg/cm2) s 1987) • Pore pressure, u (for piezocone) Factors Affecting Results : Water seal Soil seal Type and consistency or density of soils Confining pressure or overburden pressure Verticality Rate of penetration S load cell Calibration of sensors Wear of the cone Temperature changes Water seal^ r Soil seal A rigid pore pressure measuring system and a fully saturated system (for piezocone) Rate of dissipation of pore pressures (for *Г<^ \j > >r4nf*tJ/7 piezocone) X T Location of the filter and axial load on the cone C + S load cell С load cell (for piezocone) Variations in the test apparatus Fig. 1.4.2. Electric Friction Cone (Meigh. 1987) In Situ кип 1-4 Chapter], to Situ Toting Device and Test Procedure Correction for Interpretation : 3 major area of cone design that influence interpretation are : 1. Unequal area effects 2. Piezometer location, size and saturation 3. Accuracy of measurement Additional sensors : In recent year, the CPT or CPTU is supplemented Local side Iriciion. by additional sensors, such-as geophone arrays (seismic cone), lateral stress sensing, pressuremeter module behind cone-penetrometer, electrical resistivity or conductivity for estimating in situ porosity or density and has also been used as an indicator of soil contamination, heat flow measurement, radioisotope measurement, acoustic noise, and other geo-environmental devices. Fig. 1.4.3. Typical Result

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Geotechnics Laboratory Parahyangan Catholic UniversityInternational Conference on In Situ Measurement of Soil Properties and Case Histories Bali-Indonesia, May 21-24 2007Preface The use of in situ testing has been widely gained popularity to establish general soil profile and to derive soil paramete
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