CPT-Geoenviron-Guide-2Nd-Edition
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Hydrogeology
Hydrogeology Principles of Groundwater Flow Lecture 3 1 Hydrostatic pressure The total force acting at the bottom of the prism with area A is Dividing both sides by the area, A ,of the prism 1 2 Hydrostatic Pressure Top of the atmosphere Thus a positive suction corresponds to a negative gage pressure. The dimensions of pressure are F/L2, that is Newton per square meter or pascal (Pa), kiloNewton per square meter or kilopascal (kPa) in SI units Point A is in the saturated zone and the gage pressure is positive. Point B is in the unsaturated zone and the gage pressure is negative. This negative pressure is referred to as a suction or tension. 3 Hydraulic Head The law of hydrostatics states that pressure p can be expressed in terms of height of liquid h measured from the water table (assuming that groundwater is at rest or moving horizontally). This height is called the pressure head: For point A the quantity h is positive whereas it is negative for point B. h = Pf /ϒf = Pf /ρg If the medium is saturated, pore pressure, p, can be measured by the pressure head, h = pf /γf in a piezometer, a nonflowing well. The difference between the altitude of the well, H, and the depth to the water inside the well is the total head, h , at the well. i 2 4 Energy in Groundwater • Groundwater possess mechanical energy in the form of kinetic energy, gravitational potential energy and energy of fluid pressure. • Because the amount of energy vary from place-to-place, groundwater is forced to move from one region to another in order to neutralize the energy differences. -
Seismic Pore Water Pressure Generation Models: Numerical Evaluation and Comparison
th The 14 World Conference on Earthquake Engineering October 12-17, 2008, Beijing, China SEISMIC PORE WATER PRESSURE GENERATION MODELS: NUMERICAL EVALUATION AND COMPARISON S. Nabili 1 Y. Jafarian 2 and M.H. Baziar 3 ¹M.Sc, College of Civil Engineering, Iran University of Science and Technology, Tehran, Iran ² Ph.D. Candidates, College of Civil Engineering, Iran University of Science and Technology, Tehran, Iran ³ Professor, College of Civil Engineering, Iran University of Science and Technology, Tehran, Iran ABSTRACT: Researchers have attempted to model excess pore water pressure via numerical modeling, in order to estimate the potential of liquefaction. The attempt of this work is numerical evaluation of excess pore water pressure models using a fully coupled effective stress and uncoupled total stress analysis. For this aim, several cyclic and monotonic element tests and a level ground centrifuge test of VELACS project [1] were utilized. Equivalent linear and non linear numerical models were used to evaluate the excess pore water pressure. Comparing the excess pore pressure buildup time histories of the numerical and experimental models showed that the equivalent linear method can predict better the excess pore water pressure than the non linear approach, but it can not concern the presence of pore pressure in the calculation of the shear strain. KEYWORDS: Excess pore water pressure, effective stress, total stress, equivalent linear, non linear 1. INTRODUCTION Estimation of liquefaction is one of the main objectives in geotechnical engineering. For this purpose, several numerical and experimental methods have been proposed. An important stage to predict the liquefaction is the prediction of excess pore water pressure at a given point. -
Presentation Slides
Center for Accelerating Innovation Advanced Geotechnical Methods in Exploration (A-GaME) Tools for Enhanced, Effective Site Characterization 1 Center for Accelerating Innovation What are the Advanced Geotechnical Methods in Exploration? The A-GaME is a toolbox of underutilized subsurface exploration tools that will assist with: • Assessing risk and variability in site characterization • Optimizing subsurface exploration programs • Maximizing return on investment in project delivery 2 Center for Accelerating Innovation Why do you need to bring your A-GaME? • Because, in up to 50% of major infrastructure projects, schedule or costs will be significantly impacted by geotechnical issues!! • The majority of these issues will be directly or indirectly related to the scope and quality of subsurface investigation and site characterization work. 3 Center for Accelerating Innovation Presenters Silas Nichols Derrick Dasenbrock Ben Rivers Principal Bridge Geomechanics/LRFD Geotechnical Engineer – Engineer Engineer Geotechnical Minnesota DOT FHWA RC FHWA HQ 4 Center for Accelerating Innovation What is “Every Day Counts”(EDC)? State-based model to identify and rapidly deploy proven but underutilized innovations to: shorten the project delivery process enhance roadway safety reduce congestion improve environmental sustainability . EDC Rounds: two year cycles . Initiating 5th Round (2019-2020) - 10 innovations . To date: 4 Rounds, over 40 innovations For more information: https://www.fhwa.dot.gov/innovation/ FAST Act, Sec.1444 5 Center for Accelerating Innovation Implementation Planning Team Practitioners l Geotechnical l Construction l Design l Risk l Geophysics l Site Variability l Public and Private Sectors l Industry Representation – ADSC, AEG, DFI, EEGS, GI and AASHTO COBS, COC, COMP Brian Collins – FHWA-WFL Michelle Mann – NMDOT Derrick Dasenbrock – MNDOT Marc Mastronardi - GDOT Mohammed Elias – FHWA-EFL Mike McVay – Univ. -
Cone Penetration Test for Bearing Capacity Estimation
The 2nd Join Conference of Utsunomiya University and Universitas Padjadjaran, Nov.24,2017 CONE PENETRATION TEST FOR BEARING CAPACITY ESTIMATION AND SOIL PROFILING, CASE STUDY: CONVEYOR BELT CONSTRUCTION IN A COAL MINING CONCESSION AREA IN LOA DURI, EAST KALIMANTAN, INDONESIA Ilham PRASETYA*1, Yuni FAIZAH*1, R. Irvan SOPHIAN1, Febri HIRNAWAN1 1Faculty of Geological Engineering, Universitas Padjadjaran Jln. Raya Bandung-Sumedang Km. 21, 45363, Jatinangor, Sumedang, Jawa Barat, Indonesia *Corresponding Authors: [email protected], [email protected] Abstract Cone Penetration Test (CPT) has been recognized as one of the most extensively used in situ tests. A series of empirical correlations developed over many years allow bearing capacity of a soil layer to be calculated directly from CPT’s data. Moreover, the ratio between end resistance of the cone and side friction of the sleeve has been prove to be useful in identifying the type of penetrated soils. The study was conducted in a coal mining concession area in Loa Duri, east Kalimantan, Indonesia. In this study the Begemann Friction Cone Mechanical Type Penetrometer with maximum push 2 capacity of 250 kg/cm was used to determine bearing layers for foundation of the conveyor belt at six different locations. The friction ratio (Rf) is used to classify the type of soils, and allowable bearing capacity of the bearing layers are calculated using Schmertmann method (1956) and LCPC method (1982). The result shows that the bearing layers in study area comprise of sands, and clay- sand mixture and silt. The allowable bearing capacity of shallow foundations range between 6-16 kg/cm2 whereas that of pile foundations are around 16-23 kg/cm2. -
Pore Pressure Response During Failure in Soils
Pore pressure response during failure in soils EDWIN L. HARP U.S. Geological Survey, 345 Middlefield Road, M.S. 998, Menlo Park, California 94025 WADE G. WELLS II U.S. Forest Service, Forest Fire Laboratory, 4955 Canyon Crest Drive, Riverside, California 92507 JOHN G. SARMIENTO Wahler Associates, P.O. Box 10023, Palo Alto, California 94303 111 45' ABSTRACT Three experiments were performed on natural slopes to investi- gate variations of soil pore-water pressure during induced slope fail- ure. Two sites in the Wasatch Range, Utah, and one site in the San Dimas Experimental Forest of southern California were forced to fail by artificial subsurface irrigation. The sites were instrumented with electronic piezometers and displacement meters to record induced pore pressures and movements of the slopes during failure. Piezome- ter records show a consistent trend of increasing pressure during the early stages of infiltration and abrupt decreases in pressure from 5 to 50 minutes before failure. Displacement meters failed to register the amount of movement, due to location and ineffectual coupling of meter pins to soil. Observations during the experiments indicate that fractures and macropores controlled the flow of water through the slope and that both water-flow paths and permeability within the slopes were not constant in space or time but changed continually during the course of the experiments. INTRODUCTION The mechanism most generally ascribed (for example, Campbell, 1975, p. 18-20) to account for rainfall-induced failure in soils indicates that an increase in the pore-water pressure within the soil mantle results in a reduction of the normal effective stresses within the material. -
Probabilistic Analysis of Immersed Tunnel Settlement Using CPT and MASW
Probabilistic analysis of immersed tunnel settlement using CPT and MASW Bob van Amsterdam January 16, 2019 Version: Final report Probabilistic analysis of immersed tunnel settlement using CPT and MASW Bob van Amsterdam Thesis committee: Prof. Dr. ir. K.G. Gavin Geo-engineering TU Delft Assoc. prof. Dr. ir. W. Broere Geo-engineering TU Delft Ir. K.J. Reinders Hydraulic engineering TU Delft Dr. ir. C. Reale Geo-engineering TU Delft January 16, 2019 Abstract Settlement data of the Kiltunnel and the Heinenoordtunnel show that immersed tunnels in the Netherlands have been experiencing much larger settlement than expected when designing the tunnels causing cracks in the concrete and leakages in the joints. Settlements of 8 - 70 mm have been measured at the Kiltunnel and of 7 - 30 mm at the Heinenoordtunnel while settlements in the range of 0 - 1 mm were expected. Both sites are investigated through non-invasive geophysical site investigation method MASW (Multichannel Analysis of Surface Waves) for each 2.5 meter along the length of the tunnel and invasive site characterisation method CPT’s (Cone Penetration Tests). The settlement of immersed tunnels is similar to that of a shallow foundation. It can be modelled using the Mayne equation which uses the small strain shear stiffness and the degradation of secant stiffness based on the load compared to the ultimate bearing resistance. A way of characterising the site is determining the small strain stiffness directly from the shear wave velocity using the uncertainties in the relationship between shear wave velocity and cone penetration resistance and correlating the cone penetration resistance to this value. -
Eskişehir Teknik Üniversitesi Bilim Ve Teknoloji Dergisi B- Teorik Bilimler
ESKİŞEHİR TEKNİK ÜNİVERSİTESİ BİLİM VE TEKNOLOJİ DERGİSİ B- TEORİK BİLİMLER Eskişehir Technical University Journal of Science and Technology B- Theoritical Sciences 2018, Volume:6 - pp. 183 - 191, DOI: 10.20290/aubtdb.489424 4th INTERNATIONAL CONFERENCE ON EARTHQUAKE ENGINEERING AND SEISMOLOGY BEHAVIOR OF A DENSE NONPLASTIC SILT UNDER CYCLIC LOADING Eyyüb KARAKAN 1, *, Alper SEZER 2, Nazar TANRINIAN 2, Selim ALTUN 2 1 Civil Engineering Department, Faculty of Engineering, Kilis 7 Aralik University, Kilis, Turkey 2 Civil Engineering Department, Faculty of Engineering, Ege University, İzmir, Turkey ABSTRACT Density of granular soils is increased after being subjected to seismic loading, leading to settlements in deeper layers. Foundation systems and shallow buried structures are affected from possible damage due to settlements induced by seismic action. Since studies on liquefaction behavior of silts is limited, it was considered to carry out an experimental study for evaluation of strength behavior of dense silts under cyclic loading conditions. All the tests were performed on specimens at a relative density of 80%, by application of constant level sinusoidal stresses under a frequency of 0.1 Hz. As a consequence, cyclic behavior of a dense silt is experimentally determined and evaluated by application of ten different cyclic stress ratio values. Keywords: Nonplastic silt, Cyclic triaxial tests, Liquefaction 1. INTRODUCTION During seismic excitations, propagation of shear waves cause undrained shear stresses under certain conditions. Formation of undrained shear stresses during shear wave propagation leads to deformations along with increase in pore water pressure. Increasing pore water pressure is accompanied with a decrease in soil rigidity by initiating a vicious circle comprising increasing levels of shear deformation and pore water pressure. -
Table of Common Symbols Used in Hydrogeology
Common Symbols used in GEOL 473/573 A Area [L2] b Saturated thickness of an aquifer [L] d Diameter [L] e void ratio (dimensionless) or e1 is a constant = 2.718281828... f Number of head drops in a flow of net F Force [M L T-2 ] g Acceleration due to gravity [9.81 m/s2] h Hydraulic head [L] (Total hydraulic head; h = ψ + z) ho Initial hydraulic head [L], generally an initial condition or a boundary condition dh/dL Hydraulic gradient [dimensionless] sometimes expressed as i 2 ki Intrinsic permeability [L ] K Hydraulic conductivity [L T-1] -1 Kx, Ky , Kz Hydraulic conductivity in the x, y, or z direction [L T ] L Length from one point to another [L] n Porosity [dimensionless] ne Effective porosity [dimensionless] q Specific discharge [L T-1] (Darcy flux or Darcy velocity) -1 qx, qy, qz Specific discharge in the x, y, or z direction [L T ] Q Flow rate [L3 T-1] (discharge) p Number of stream tubes in a flow of net P Pressure [M L-1T-2] r Radial coordinate [L] rw Radius of well over screened interval [L] Re Reynolds’ number [dimensionless] s Drawdown in an aquifer [L] S Storativity [dimensionless] (Coefficient of storage) -1 Ss Specific storage [L ] Sy Specific yield [dimensionless] t Time [T] T Transmissivity [L2 T-1] or Temperature (degrees) u Theis’ number [dimensionless} or used for fluid pressure (P) in engineering v Pore-water velocity [L T-1] (Average linear velocity) V Volume [L3] 3 VT Total volume of a soil core [L ] 3 Vv Volume voids in a soil core [L ] 3 Vw Volume of water in the voids of a soil core [L ] Vs Volume soilds in a soil -
Geotechnical Investigations for Tunneling
Breakthroughs in Tunneling September 12, 2016 Geotechnical Site Investigations For Tunneling Greg Raines, PE Objective To develop a conceptual model adequate to estimate the range of ground conditions and behavior for excavation, support, and groundwater control. support Typical Phases of Subsurface Investigation Phase 1: Planning Phase – Desk Top Study/Review Phase 2: Preliminary/Feasibility Design – Initial Field Investigations Phase 3: Final Design – Additional/Follow-Up Field Investigations Final Phase: Construction – Continued characterization of site Typical Phases of Subsurface Investigation Phase 1: Planning Phase – Desk Top Study/Review Review: Geologic maps Previous reports/investigations Aerial photos Case histories Develop conceptual geologic/geotechnical model (cross sections), preliminarily identify technical constraints/issues for the project. Plan subsurface investigation program. Identify/Collect Available Geotechnical Data in the Project Area Bridge or control Information can include: structure • Geologic maps • Data from previous reports • Drill hole data • Preliminary mapping Compile available local data into a database for further evaluation. Roads or Residential Canals Area Geologic Profiles – Understand Geologic Setting and Collect Specific Data Bedrock Surface Elevation Maps Aerial Photo / LiDAR Interpretation Aerial Photo Diversion Tunnel Use digital imagery/LiDAR to map local features prior to field mapping. Dam LiDAR Field Geologic Mapping Field Geologic Mapping Structural Data Collection (faults, folds, -
In Situ and Laboratory Evaluation of Liquefaction Resistance of a Fine Sand
Louisiana State University LSU Digital Commons LSU Historical Dissertations and Theses Graduate School 1990 In Situ and Laboratory Evaluation of Liquefaction Resistance of a Fine Sand. Behnam Mahmoodzadegan Louisiana State University and Agricultural & Mechanical College Follow this and additional works at: https://digitalcommons.lsu.edu/gradschool_disstheses Recommended Citation Mahmoodzadegan, Behnam, "In Situ and Laboratory Evaluation of Liquefaction Resistance of a Fine Sand." (1990). LSU Historical Dissertations and Theses. 5075. https://digitalcommons.lsu.edu/gradschool_disstheses/5075 This Dissertation is brought to you for free and open access by the Graduate School at LSU Digital Commons. It has been accepted for inclusion in LSU Historical Dissertations and Theses by an authorized administrator of LSU Digital Commons. For more information, please contact [email protected]. INFORMATION TO USERS This manuscript has been reproduced from the microfilm master. UMI films the text directly from the original or copy submitted. Thus, some thesis and dissertation copies are in typewriter face, while others may be from any type of computer printer. The quality of this reproduction isdependent upon the quality of the copy submitted. Broken or indistinct print, colored or poor quality illustrations and photographs, print bleedthrough, substandard margins, and improper alignment can adversely affect reproduction. In the unlikely event that the author did not send UMI a complete manuscript and there are missing pages, these will be noted. Also, if unauthorized copyright material had to be removed, a note will indicate the deletion. Oversize materials (e.g., maps, drawings, charts) are reproduced by sectioning the original, beginning at the upper left-hand corner and continuing from left to right in equal sections with small overlaps. -
Fugro Cone Penetration Tests
SERVICE FLYER FUGRO CONE PENETRATION TESTS The objective of all site investigations is to obtain data that will ■■ Piezocones (CPTU) can also be used adequately quantify the variability of the geotechnical properties of to assess hydrostatic head, the site. Cone Penetrometer Testing (CPT) provides a rapid and cost consolidation and permeability effective way to achieve this. characteristics ■■ Yields thousands or tens of thousands of data points that can be digitally INTRODUCTION stored and transferred in real time Sufficient data is required to assess the ■■ Provides a continuous (although ■■ Cost-effective method employing rapid impact of soil variability within a time frame indirect) record of ground conditions, probing rates to accredited test such that it can be allowed for within the avoiding the ground disturbance procedures geotechnical design and/or construction. associated with boring and sampling ■■ Data may be used in long-established CPT generates high value data and adapts CPT units can be mobilised as road-going semi-empirical design methods, for readily to the environmental sensitivities of 6x6 trucks or a variety of tracked and example, analysis of foundation many investigations in favourable types of crawler units, ideally suited to traversing bearing capacity, foundation material, generally excluding bedrock, very soft, water logged terrain or entering sites settlement, pile carrying capacity and dense granular fill and strata containing with limited access. Fugro’s development of liquefaction potential cobbles and boulders. -
Darcy's Law and Hydraulic Head
Darcy’s Law and Hydraulic Head 1. Hydraulic Head hh12− QK= A h L p1 h1 h2 h1 and h2 are hydraulic heads associated with hp2 points 1 and 2. Q The hydraulic head, or z1 total head, is a measure z2 of the potential of the datum water fluid at the measurement point. “Potential of a fluid at a specific point is the work required to transform a unit of mass of fluid from an arbitrarily chosen state to the state under consideration.” Three Types of Potentials A. Pressure potential work required to raise the water pressure 1 P 1 P m P W1 = VdP = dP = ∫0 ∫0 m m ρ w ρ w ρw : density of water assumed to be independent of pressure V: volume z = z P = P v = v Current state z = 0 P = 0 v = 0 Reference state B. Elevation potential work required to raise the elevation 1 Z W ==mgdz gz 2 m ∫0 C. Kinetic potential work required to raise the velocity (dz = vdt) 2 11ZZdv vv W ==madz m dz == vdv 3 m ∫∫∫00m dt 02 Total potential: Total [hydraulic] head: P v 2 Φ P v 2 h == ++z Φ= +gz + g ρ g 2g ρw 2 w Unit [L2T-1] Unit [L] 2 Total head or P v hydraulic head: h =++z ρw g 2g Kinetic term pressure elevation [L] head [L] Piezometer P1 P2 ρg ρg h1 h2 z1 z2 datum A fluid moves from where the total head is higher to where it is lower. For an ideal fluid (frictionless and incompressible), the total head would stay constant.