Guide to Site Investigation (2017 Version)
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Geotechnical Investigations
GEOTECHNICAL INVESTIGATIONS GUIDELINES VERSION 1.2 3 UNOPS Geotechnical Investigations Version 1.2 - 2018 Version for digital distribution. If printed, spiral binding is recommended. © UNOPS 2018 Published and maintained by the Infrastructure and Project Management Group All rights reserved. The reproduction of any materials from this publication must be accompanied by a reference to the title and a website location of this publication. The designations employed and the presentation of the material in this publication do not imply the expression of any opinion whatsoever on the part of UNOPS concerning the legal status of any country, territory, city or area or of its authorities, or concerning the delimitation of its frontiers or boundaries. All reasonable precautions have been taken by UNOPS to verify the information contained in this publication. However, the published material is being distributed without warranty of any kind, either expressed or implied. The responsibility for the interpretation and use of the material lies with the reader. In no event shall UNOPS be liable for damages arising from its use. This publication may be reproduced for personal use but may not otherwise be reproduced or, stored in a retrieval system or transmitted, in any form or by any means, electronic, photocopying, recording or otherwise, without prior written permission of UNOPS. Trademarks ISO® is a registered trademark of the International Organization for Standardization. Credits: Cover page photo: © Lesterman / Shutterstock.com Contact For more information or for providing feedback, contact: [email protected] UNOPS | Geotechnical Investigations Version 1.2 | December 2018 4 Acknowledgments PROJECT TEAM REVIEWERS AND CONTRIBUTORS The UNOPS Geotechnical The project team wishes to thank, on behalf of UNOPS, the following people who Investigations Guidelines is a provided valuable feedback during the different stages of development of this product of collective hard work and publication in its current revision. -
Caulmert Limited
CAULMERT LIMITED Engineering, Environmental & Planning Consultancy Services Corby Materials Recycling Facility Viridor Waste Management Ltd Concrete Slab for Glass Storage, Handling and Transfer Factual Ground Investigation Report Prepared by: Caulmert Limited 8 St Georges Court, Dairyhouse Lane, Altrincham, Cheshire, WA14 5UA Tel: 0161 9286886 Email: [email protected] Web: www.caulmert.com Doc ref: 2010.7.VWM.DEO.PAC.B0 Issue date: April 2015 APPROVAL RECORD Site: Corby Materials Recycling Facility Client: Viridor Waste Management Ltd Project Title: Concrete Slab for Glass Storage, Handling and Transfer Document Title: Factual Ground Investigation Report Document Ref: 2010.7.VWM.DEO.PAC.B0 Report Status: DRAFT Project Director: Allan Smith Project Manager: Chris Newton Caulmert Limited: 8 St Georges Court, Dairy House Lane, Altrincham, Cheshire, WA14 5UA Tel: 0161 9286886 Author Dominic Ostafijczuk Date April 2015 Reviewer Paul Clayden Date April 2015 Approved Chris Newton Date April 2015 DISCLAIMER This report has been prepared by Caulmert Limited with all reasonable skill, care and diligence in accordance with the instruction of the above named client and within the terms and conditions of the Contract with the Client. The report is for the sole use of the above named Client and Caulmert Limited shall not be held responsible for any use of the report or its content for any purpose other than that for which it was prepared and provided to the Client. Caulmert Limited accepts no responsibility of whatever nature to any third parties who may have been made aware of or have acted in the knowledge of the report or its contents. No part of this document may be copied or reproduced without the prior written approval of Caulmert Limited. -
2017 Classification of Soils and Rocks for The
PIANC WG Report n° 144 - 2017 ABRIDGED FIELD VERSION CLASSIFICATION OF SOILS AND ROCKS FOR THE MARITIME DREDGING PROCESS The World Association for Waterborne Transport Infrastructure PIANC The World Association for Waterborne Transport Infrastructure PIANC REPORT N° 144 MARITIME NAVIGATION COMMISSION CLASSIFICATION OF SOILS AND ROCKS FOR THE MARITIME DREDGING PROCESS - ABRIDGED FIELD VERSION - 2017 PIANC has Technical Commissions concerned with inland waterways and ports (InCom), coastal and ocean waterways (including ports and harbours) (MarCom), environmental aspects (EnviCom) and sport and pleasure navigation (RecCom). This report has been produced by an international Working Group convened by the Maritime Navigation Commission (MarCom). Members of the Working Group represent several countries and are acknowledged experts in their profession. The objective of this report is to provide information and recommendations on good practice. Conformity is not obligatory and engineering judgement should be used in its application, especially in special circumstances. This report should be seen as an expert guidance and state-of-the-art on this particular subject. PIANC disclaims all responsibil- PIANC REPORT N° 144 ity in the event that this report should be presented as an official standard. MARITIME NAVIGATION COMMISSION PIANC Secrétariat Général Boulevard du Roi Albert II 20, B 3 B-1000 Bruxelles Belgique http://www.pianc.org VAT BE 408-287-945 ISBN 978-2-87223-247-5 © All rights reserved TABLE OF CONTENTS Part 1: Introduction and Outline -
Final Report ~ Fhwa-Ok-13-09 Odot Sp&R Item Number 2227
APPLIED APPROACH SLAB SETTLEMENT RESEARCH, DESIGN/CONSTRUCTION FINAL REPORT ~ FHWA-OK-13-09 ODOT SP&R ITEM NUMBER 2227 Submitted to: John R. Bowman, P.E. Planning & Research Division Engineer Oklahoma Department of Transportation Submitted by: Gerald A. Miller, Kianoosh Hatami, Amy B. Cerato, Colin Osborne School of Civil Engineering and Environmental Science University of Oklahoma August 2013 TECHNICAL REPORT DOCUMENTATION PAGE 1. REPORT NO. 2. GOVERNMENT ACCESSION NO. 3. RECIPIENT’S CATALOG NO. FHWA-OK-13-09 4. TITLE AND SUBTITLE 5. REPORT DATE Applied Approach Slab Settlement Research, August 2013 Design/Construction 6. PERFORMING ORGANIZATION CODE 7. AUTHOR(S) 8. PERFORMING ORGANIZATION REPORT Gerald A. Miller, Kianoosh Hatami, Amy Cerato, Colin Osborne 9. PERFORMING ORGANIZATION NAME AND ADDRESS 10. WORK UNIT NO. University of Oklahoma School of Civil Engineering and Environmental 11. CONTRACT OR GRANT NO. Science ODOT SP&R Item Number 2227 202 West Boyd Street, Room 334 Norman, OK 73019 12. SPONSORING AGENCY NAME AND ADDRESS 13. TYPE OF REPORT AND PERIOD COVERED Oklahoma Department of Transportation Final Report Planning and Research Division From September 2010 – December 2012 200 N.E. 21st Street, Room 3A7 14. SPONSORING AGENCY CODE Oklahoma City, OK 73105 15. SUPPLEMENTARY NOTES Click here to enter text. 16. ABSTRACT Approach embankment settlement is a pervasive problem in Oklahoma and many other states. The bump and/or abrupt slope change poses a danger to traffic and can cause increased dynamic loads on the bridge. Frequent and costly maintenance may be needed or extensive repair and reconstruction may be required in extreme cases. Research critically investigated the design and construction methods in Oklahoma to reveal causes and solutions to the bridge approach settlement problem. -
Tunnels in Swelling Ground
Marco Barla Tunnels in Swelling Ground SIMULATION OF 3D STRESS PATHS BY TRIAXIAL LABORATORY TESTING Dottorato di Ricerca in Ingegneria Geotecnica Politecnico di Torino Politecnico di Milano Università degli Studi di Genova Università degli Studi di Padova Dottorato di Ricerca in Ingegneria Geotecnica (XII ciclo) Politecnico di Torino Politecnico di Milano Università degli Studi di Genova Università degli Studi di Padova November 1999 TUNNELS IN SWELLING GROUND SIMULATION OF 3D STRESS PATHS BY TRIAXIAL LABORATORY TESTING ………………………. Marco Barla Author ……………………….………. ………...….…………… ....…….………………… Prof. Michele Jamiolkowski Prof. Giovanni Barla Prof. Diego Lo Presti Supervisors ……………………….. Prof. Renato Lancellotta Head of the Ph.D. Programme in Geotechnical Engineering “Peace cannot be kept by force, it can only be achieved by understanding.” Albert Einstein SAN DONATO TUNNEL (FLORENCE, ITALY), 1986 SARMENTO TUNNEL (SINNI, ITALY), 1997 ABSTRACT I Abstract The present thesis is to contribute to the understanding of the swelling behaviour of tunnels with a major interest being placed on the stress and deformation response in the near vicinity of the advancing face, i.e. in three dimensional conditions. Following the introduction of the most recent developments, mostly based on contributions of the International Society for Rock Mechanics, the research examines the stress distribution around a circular tunnel by means of numerical methods. According to different stress conditions and stress-strain laws for the ground, the stress history of typical points around the tunnel (sidewalls, crown and invert) is described with the stress path method (Lambe 1967). This allows one to evidence how the three dimensional analyses results are necessary to describe the ground behaviour. In particular, it can be observed that the excavation is accompanied by a continuous variation of the mean normal stress even for an isotropic initial state of stress. -
Nash Flood Wall
A1 N RAILWAY EMBANKMENT EXISTING DRAINAGE DITCH AT 0.35m TOE OF RAILWAY EMBANKMENT 8.000mAOD FALL EXPOSED CONCRETE WALL SURFACE TO HAVE A FAIR WORKED FINISH REINFORCED CONCRETE PLEASE REFER TO FLOOD WALL KEY PLAN A ARBORICULTURAL DRAWINGS SCALE 1:10,000 FOR DETAILS OF TREE REMOVAL FLOOD SIDE DRY SIDE AND TPZ'S IF APPROPRIATE (APPROX. NORTH FACING) GENERAL NOTES: 0.5m DIAMETER PIPE RIP RAP STONE LAYER TO BE THROUGH WALL TO MAINTAIN INSTALLED ON SOUTHERN 2.7m 1. THIS DRAWING IS TO BE READ IN CONJUNCTION WITH ALL FLOOD SIDE OF RETAINING DRAINAGE DITCH SIDE OF RETAINING WALL WALL FOR EROSION CONTROL OTHER DRAWINGS, SPECIFICATIONS AND CONTRACT B DOCUMENTS. NOTIFY THE PROJECT MANAGER OF ANY DISCREPANCIES. 5M WORKING SPACE TO REAR 5.65mAOD 2. ALL DIMENSIONS IN MILLMETERS AND ALL LEVELS IN METERS ABOVE ORDNANCE DATUM UNLESS NOTED OTHERWISE. B 3. DO NOT SCALE FROM DRAWING. Trial Pit PROPOSED EARTHWORK RAMPING AROUND TOE OF WALL TO SCREEN 5.000mAOD 0.4m VISUAL APPEARANCE C RIP RAP STONE LAYER TO BE INSTALLED 500mm Ø OPENING IN RETAINING \\global\europe\Cardiff\Jobs\274000\274580-00\4 Internal Project Data\4-30 Drawings\4-31 Issue drawings\274580-ARP-XX-XX-DR-CX-3400.dwg ON THE SOUTHERN SIDE OF THE OPENING WALL AT THIS LOCATION TO 1.2m 1.3m TO PROVIDE EROSION CONTROL MAINTAIN FLOW IN DRAINAGE DITCH Trial Pit C SECTIONS LEGEND: Trial Pit SECTION B-B EXISTING GROUND LEVELS (WALL SECTION) 1:25 FLOOD WALL UPSTAND A FLOOD WALL FOUNDATION Post PLAN LEGEND: RAISED SLUDGE 10M WORKING SPACE TO FRONT OF WALL PLANNING APPLICATION BOUNDARY BEDS FOR CABIN, ACCESS PARKING, TURNING AND MATERIALS STORAGE PROPOSED GROUND RAISING TIE INTO EXISTING EMBANKMENT FLOOD SIDE DRY SIDE (APPROX. -
Slope Stability
Slope stability Causes of instability Mechanics of slopes Analysis of translational slip Analysis of rotational slip Site investigation Remedial measures Soil or rock masses with sloping surfaces, either natural or constructed, are subject to forces associated with gravity and seepage which cause instability. Resistance to failure is derived mainly from a combination of slope geometry and the shear strength of the soil or rock itself. The different types of instability can be characterised by spatial considerations, particle size and speed of movement. One of the simplest methods of classification is that proposed by Varnes in 1978: I. Falls II. Topples III. Slides rotational and translational IV. Lateral spreads V. Flows in Bedrock and in Soils VI. Complex Falls In which the mass in motion travels most of the distance through the air. Falls include: free fall, movement by leaps and bounds, and rolling of fragments of bedrock or soil. Topples Toppling occurs as movement due to forces that cause an over-turning moment about a pivot point below the centre of gravity of the unit. If unchecked it will result in a fall or slide. The potential for toppling can be identified using the graphical construction on a stereonet. The stereonet allows the spatial distribution of discontinuities to be presented alongside the slope surface. On a stereoplot toppling is indicated by a concentration of poles "in front" of the slope's great circle and within ± 30º of the direction of true dip. Lateral Spreads Lateral spreads are disturbed lateral extension movements in a fractured mass. Two subgroups are identified: A. -
The Glacial Origins of Relict 'Pingos'
Annals of Glaciology The glacial origins of relict ‘pingos’, Wales, UK Neil Ross1 , Peter Brabham2 and Charles Harris2 1School of Geography, Politics and Sociology, Newcastle University, Newcastle upon Tyne, UK and 2School of Earth and Ocean Sciences, Cardiff University, Cardiff, UK Paper Abstract Cite this article: Ross N, Brabham P, Harris C Ramparted depressions (doughnut-shaped debris-cored ridges with peat- and/or sediment-filled (2020). The glacial origins of relict ‘pingos’, central basins) are commonly perceived to represent the relict collapsed forms of permafrost – Wales, UK. Annals of Glaciology 1 13. https:// ground-ice mounds (i.e. pingos or lithalsas). In Wales, UK, ramparted depressions of Late doi.org/10.1017/aog.2019.40 Pleistocene age have been widely attributed to permafrost-related processes. However, a variety Received: 28 June 2019 of alternative glacial origins for these enigmatic landforms are also consistent with the available geo- Revised: 6 November 2019 logical and geomorphological evidence, although previous studies have barely considered such Accepted: 7 November 2019 alternative processes of formation. From detailed geophysical, sedimentological and remote-sensing Key words: studies at two field sites, we demonstrate that: (i) the wastage of stagnating glacier ice is a viable alter- glacial geology; permafrost; pingo; near native explanation for the formation of ramparted depressions in Wales; (ii) the glacial geomorph- surface geophysics; stagnant ice; Quaternary ology and geology of these landforms is analogous -
Evaluation of Shear Strength in Cohesive Soils with Special Reference to Swedish Practice and Experience
Information 3 Evaluatian of shear strength in cohesive soils with special reference to Swedish practice and experience ROLF LARSSON ULF BERGDAHL LEIF ERIKSSON STATENS GEOTEKNISKA INSTITUT EVALUATlON OF SHEAR STRENGTH IN COHE8 IVE SOILS WITH SPECIAL REFERENCE TO SWE DISH PRACTICE AND EXPERIENCE In this publication, information is given on how different test results and empirical experience can be weighted and combined to give the best possible estimation of the shear strength proper ties in cohesive soils. The procedure described has evolved during the continuing work at SGI as research results and practical experience from the Institute as weil as others have been obtained and taken into con sideration. The publication describes how the Institute cur rently proceeds in the evaluation of shear strength in cohesive soils. The intention has aiso been to bring about a more unified and objective proce dure t han that has been used up to now. Valuable views on this work have been given by colleagues in and outside the Institute. Linköping November 1984 Rolf Larsson Ulf Bergdahl Leif Eriksson CONTENTS INTRODUCTION 2 DEFINITIONs AND SYMBOLS 3 UNDRAINED SHEAR STRENGTH IN NORMALLY CONSOLIDATED 4 AND SLIGHTLY OVERCONSOLIDATED SOILS eorrection of values of undrained shear strength 4 obtained by vane shear tests and fall cone tests Estimatian of shear strength values on the basis 5 of Hansbo's relation Estimatian of corrected shear strengths on the 6 basis of results from other soundings Estimatian of corrected shear strengths on the 6 basis -
1.6 Consolidation Test
Engineering Properties of Soils 1-24 1.6 Consolidation Test 1.6.1 General - Consolidation can be defined as a dissipation process of excess pore pressure induced by applied load or change of boundary conditions. - It is a time dependent behavior of soil deformation. ⇒ Significant in saturated clayey soils. ⇒ Factors on consolidation time 1) Degree of saturation 2) Coefficient of permeability of soil 3) Viscosity and compressibility of the pore fluid 4) Length of path the expelled pore fluid must take to find equilibrium. 5) Compressibility of soils - Consolidation test determines parameters for the time dependent behavior of soils. 1) The amount of deformation ⇒ (Primary) Consolidation settlement (+ Secondary compression settlement) 2) Rate of consolidation (i.e. Consolidation time) SNU Geotechnical and Geoenvironmental Engineering Lab. Engineering Properties of Soils 1-25 - Idealized stages in primary consolidation - Consolidation theory follows Darcy’s law. v = ki = k(Δh/L) ⇒ Δt = L/v = L/{ k(Δh/L)} = L2/(kΔh) ⇒ Doubling L requires 4 times for consolidation. ⇒ Consolidation rate is getting slower with decreasing Δh. SNU Geotechnical and Geoenvironmental Engineering Lab. Engineering Properties of Soils 1-26 1.6.2 Consolidation Test - Simulates 1-dimensional state (flow and deformation) ⇒ Using a circular metal ring confining the sample. ⇒ (Possible to measure the pore pressure during consolidation and to perform the permeability tests in the oedometer.) SNU Geotechnical and Geoenvironmental Engineering Lab. Engineering Properties of Soils 1-27 - Sample size : 20 – 40 mm thickness(H) and 45 – 113 mm diameter(D). D/H > 2.5 and D < {(Tube sample) - 6mm.} (Commonly used sample size : D = 63.5mm, H= 25.4mm) - Ring-to-soil friction problems: ⇒ Should be reduced by limiting sample thickness, spraying the inner ring wall with tefron powder or using a tefron-lined ring. -
Geotechnical Characterization of Structurally Complex Formations: Advanced Laboratory Testing
Geotechnical Characterization of Structurally Complex Formations: Advanced Laboratory Testing Mariacristina Bonini Research Assistant Politecnico di Torino (Italy) e-mail: [email protected] ABSTRACT This paper focuses on specific issues of advanced laboratory testing of Structurally Complex Formations. The former introductory paper on this subject showed that standard laboratory testing may clarify a few aspects related to swelling potential, water content and hydraulic conductivity and determination of the strength parameters by means of triaxial tests. It is was soon evident that further research was required to characterize the relationship between the behavior of the natural and reconstituted soil and to improve comprehension of the role which structure played in the setting up of the testing procedure and interpretation of results. The outcomes of this survey are described in the following. KEYWORDS: Structurally Complex Formations; Reconstituted Specimens; Advanced Laboratory Testing; Oedometer Tests; Triaxial Tests. INTRODUCTION The rock materials considered in this study pertain to the Raticosa and Osteria tunnels, pertaining to the Italian High Speed Railway project between Bologna and Florence. The tunnels were partly excavated through the Chaotic Complex Tectonised Clay Shales (CCTCS) formation, soft rocks with complex structure subjected to time-dependent behavior. The laboratory specimens obtained from cubic samples taken at the tunnel face were subjected to a number of standard laboratory tests (e.g. classification, physical properties, mineralogical composition, swelling behavior, hydraulic conductivity, triaxial testing) devoted to interpret the complex mechanical behavior of the CCTCS Formation. An introductory paper (Bonini 2012) collected the results of the standard laboratory testing (Bonini 2003) which evidenced the presence of a structure made of clay fragments of various shapes and sizes, spaced by a net of fissures and planes of different roughness and orientation. -
Ocean Drilling Program Scientific Results Volume
Rea, D.K., Basov, I.A., Scholl, D.W., and Allan, J.F. (Eds.), 1995 Proceedings of the Ocean Drilling Program, Scientific Results, Vol. 145 36. SUBMARINE SLOPE STABILITY ANALYSIS ON THE DETROIT SEAMOUNT, SITE 8831 John A. Roberts,2 Anne K. Rutledge,3 and Aarno T. Kotilainen4 ABSTRACT Diatom- and clay-rich sediments sampled from the Detroit Seamount were tested to determine the parameters required for slope stability analysis. Consolidation tests performed show that the sediments are apparently overconsolidated in the upper 24 m of the section and become normally consolidated at greater depths. Triaxial testing shows that the major sediment types (clays and diatom oozes) cannot be distinguished on the basis of normalized strength parameters. The results of a slope stability analysis using the infinite slope theory indicate that the sediments are unstable when subjected to earthquake ground accelerations in excess of 7% to 8% of gravity on the flanks and 10% to 11 % on the top of the seamount. Examination of stress path plots show that most of the samples tested exhibit a nondisintegrative nature, that would be expected to produce slump blocks or slides. INTRODUCTION Consolidation Tests The study of the stability of submarine slopes has increased in One-dimensional consolidation tests were performed using Soil interest to marine geologists over the past 20 yr, as the extent of down- Testing Inc. oedometers at Texas A&M University. The samples (cut to slope mass movement processes has become clear. Very large slope a size of 6.35 cm diameter by 2.54 cm high) were laterally constrained failures have been documented from around the world (e.g., Lewis, while being incrementally loaded up to 800 kPa and then rebounded to 1971;Embley, 1976; Masson et al., 1992).