Engineering Geology and Site Investigation Part 3
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UNIFORM STANDARD SPECIFICATIONS for PUBLIC WORKS CONSTRUCTION
UNIFORM STANDARD SPECIFICATIONS for PUBLIC WORKS CONSTRUCTION SPONSORED and DISTRIBUTED by the 1998 ARIZONA (Includes revisions through 2010) FOREWORD Publication of these Uniform Standard Specifications and Details for Public Works Construction fulfills the goal of a group of agencies who joined forces in 1966 to produce such a set of documents. Subsequently, in the interest of promoting county-wide acceptance and use of these standards and details, the Maricopa Association of Governments accepted their sponsorship and the responsibility of keeping them current and viable. These specifications and details, representing the best professional thinking of representatives of several Public Works Departments, reviewed and refined by members of the construction industry, were written to fulfill the need for uniform rules governing public works construction performed for Maricopa County and the various cities and public agencies in the county. It further fulfills the need for adequate standards by the smaller communities and agencies who could not afford to promulgate such standards for themselves. A uniform set of specifications and details, updated and embracing the most modern materials and construction techniques will redound to the benefit of the public and the private contracting industry. Uniform specifications and details will eliminate conflicts and confusion, lower construction costs, and encourage more competitive bidding by private contractors. The Uniform Standard Specifications and Details for Public Works Construction will be revised periodically and reprinted to reflect advanced thinking and the changing technology of the construction industry. To this end a Specifications and Details Committee has been established as a permanent organization to continually study and recommend changes to the Specifications and Details. -
Slope Stability Reference Guide for National Forests in the United States
United States Department of Slope Stability Reference Guide Agriculture for National Forests Forest Service Engineerlng Staff in the United States Washington, DC Volume I August 1994 While reasonable efforts have been made to assure the accuracy of this publication, in no event will the authors, the editors, or the USDA Forest Service be liable for direct, indirect, incidental, or consequential damages resulting from any defect in, or the use or misuse of, this publications. Cover Photo Ca~tion: EYESEE DEBRIS SLIDE, Klamath National Forest, Region 5, Yreka, CA The photo shows the toe of a massive earth flow which is part of a large landslide complex that occupies about one square mile on the west side of the Klamath River, four air miles NNW of the community of Somes Bar, California. The active debris slide is a classic example of a natural slope failure occurring where an inner gorge cuts the toe of a large slumplearthflow complex. This photo point is located at milepost 9.63 on California State Highway 96. Photo by Gordon Keller, Plumas National Forest, Quincy, CA. The United States Department of Agriculture (USDA) prohibits discrimination in its programs on the basis of race, color, national origin, sex, religion, age, disability, political beliefs and marital or familial status. (Not all prohibited bases apply to all programs.) Persons with disabilities who require alternative means for communication of program informa- tion (Braille, large print, audiotape, etc.) should contact the USDA Mice of Communications at 202-720-5881(voice) or 202-720-7808(TDD). To file a complaint, write the Secretary of Agriculture, U.S. -
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. -
Geotechnical and Pavement Engineering Report Thorp Prairie Road Evaluation and Design Kittitas County, Washington
GEOTECHNICAL AND PAVEMENT GEOTECHNICAL REPORT ElliottENGINEERING Bridge No. 3166 REPORTReplacement Thorp PrairieHWA JobRoad No. Evaluation 1996-143-21 and Design Kittitas County, Washington HWA ProjectPrepared No. for2012-105-21 ABKJ, INC. Prepared for PacifiCleanApril Environmental 4, 2003 LLC February 1, 2013 TABLE OF CONTENTS 1.0 EXECUTIVE SUMMARY ..............................................................................................1 2.0 INTRODUCTION..........................................................................................................1 2.1 GENERAL.......................................................................................................1 2.2 PROJECT UNDERSTANDING............................................................................1 3.0 FIELD AND LABORATORY TESTING............................................................................2 3.1 FALLING WEIGHT DEFLECTOMETER TESTING ...............................................2 3.2 PAVEMENT CORE HOLES ...............................................................................3 3.3 LABORATORY TESTING .................................................................................3 4.0 SITE CONDITIONS ......................................................................................................4 4.1 SITE DESCRIPTION.........................................................................................4 4.2 GENERAL GEOLOGY ......................................................................................4 4.3 PAVEMENT STRUCTURAL -
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 -
An Investigation Into the Volume Changetown Characteristics of Loess Like Soil in Mount Moorosi Village in Lesotho
UNIVERSITY OF CAPE TOWN FACULTY OF ENGINEERING AND THE BUILT ENVIRONMENT Department of Civil Engineering An Investigation into the Volume ChangeTown Characteristics of Loess Like Soil in Mount Moorosi Village in Lesotho Cape Geotechnicalof Engineering Group Author: Monica Damane Supervisor: Assoc. Prof. Denis Kalumba UniversityCo-supervi sor: Mrs. Laxmee Sobhee-Beetul [June 2019] A thesis submitted in partial fulfilment of the requirement for the award of the degree of Master of Science in Engineering Specialising in Geotechnical Engineering at the University of Cape Town The copyright of this thesis vests inTown the author. No quotation from it or information derived from it is to be published without full acknowledgement of the source. The thesis is to be used for private study or non- commercial research purposes Capeonly. of Published by the University of Cape Town (UCT) in terms of the non-exclusive license granted to UCT by the author. University Plagiarism declaration 1. Plagiarism is using another’s work and to pretend that it is one’s own. I know that plagiarism is wrong. 2. I have used the Harvard convention for citation and referencing. Each significant contribution to and quotation in this report from the work or works of the other people have been attributed and has been cited and referenced. 3. This report is my own work. 4. I have not allowed and will not allow anyone to copy my work with the intention of passing it off as his or her own work. Signature: … ………………………………… Date: 17/06/2019 Student Name: Monica Damane (DMNMON001) i Dedication To my grandmother and late parents, for undoubtedly and always believing in me. -
Geotechnical Investigation Report.Docx
GEOTECHNICAL INVESTIGATION FOR THE PROPOSED ALICEDALE RELIEF RISING MAIN PREPARED BY: ISSUED TO: GIBB (PTY) LTD P.O. BOX 63703 Greenacres 6057 July 2016 Form 403.1 {'':lr'\r Stl'a| VERIFICATION PAGE Ce0tc.ltrl.!l & tin!lroDnrcntal Consultdtrts Rev 10/06 GEOTECHNICAL INVESTIGATION FOR THE PROPOSED ALICEDALE RELIED RISING MAIN JOB NO:41650 DATE: Julv 2016 REPORT STATUS: FINAL REPORT CARRIED OUT BY: COMMISSIONED BY: Terratest (Pty) Ltd Gibb (Pty) Ltd P.O. Box 27308 P.O, Box 63703 GREENACRES Greenacres 6057 6057 Tel: (041) 363 4428 Tel: (041) 392 7500 Fax: (041) 3631922 AUTHOR: CLIENT CONTACT PERSONS: Mr. L Parfitt Mr. J Barnard SYNOPSIS: GEOTECHNICAL INVESTIGATION FOR THE PROPOSED ALICEDALE RELIEF RISING MAIN KEY WORDS: Geotechnical, geology @ COPYRIGHT: Terratest (Pty) Ltd. QUALITY VERIFICATION This report has been prepared under the controls established by a quality management system that meets the requirements of lSO9001: 2008 which has been independently certified by DEKRA Certification under certificate number 90906882 Verification Capacity Name Signature Date By Author Geologist Mr L Parfitt July 2016 Checked by Snr Engineering Geologist Mr R Fyvie 4v July 2016 Authorised by Executive Associate Mr R Fyvie ry+ July 2016 GEOTECHNICAL INVESTIGATION FOR THE PROPOSED ALICEDALE RELIEF RISING MAIN CONTENTS 1. INTRODUCTION ................................................................................................ 4 2. TERMS OF REFERENCE .................................................................................. 6 3. DATA BASE ...................................................................................................... -
Core Bits Are Classifi Ed According Figure 1
OCEAN DRILLING PROGRAM www.oceandrilling.org Scientifi c Application Extended Core Barrel (XCB) (see the XCB tool sheet) (both sys- A core bit (Figs. 1, 2) is a drilling Cutting shoe tems use the same BHA), tool with a hole through the center that removes sediment rock and II. Rotary Core Barrel (RCB) (see allows the core pedestal to pass the RCB tool sheet), and through the bit and into the core III. Advanced Diamond Core Barrel barrel. The Ocean Drilling Program (ADCB) (see the ADCB tool (ODP) employs different coring sheet). systems and bits to obtain continu- ous cores in all types of oceanic Bottom-Hole Assembly sediments and igneous basement. Operation The BHA for each coring system Once a coring system is selected is slightly different, but in gen- based on the expected lithology, eral consists of a primary core bit, the engineer determines which outer core barrel (OCB), short type of core bit to use. As coring sub assembly, and drill collars. conditions change, the coring bit The OCB supports the wireline A can be changed in an attempt retrievable inner core barrel, which to improve the recovery and rate Cutting shoe receives and carries the core. Drill of penetration with that coring collars are heavyweight pipes that system. The type of bit used apply weight to the bit on the depends on the expected lithology bottom of the OCB. The BHA is and past bit performance in the run on the drill pipe string, which area or in a similar lithology. Once is rotated at the surface to drive a bit is removed, it is “graded” the bit (except the Motor-Driven (i.e., it is examined to determine Core Barrel [MDCB]) and advance wear on the cutting structure, the BHA (see the BHA tool sheet gauge, bearings, etc., based on for more information). -
Geothermal Study to Explain Man-Made Permafrost in Tailings
Environmental Earth Sciences (2018) 77:288 https://doi.org/10.1007/s12665-018-7465-8 ORIGINAL ARTICLE Geothermal study to explain man‑made permafrost in tailings with raised surface Roger Knutsson1 · Peter Viklander1 · Sven Knutsson1 · Jan Laue1 Received: 5 September 2017 / Accepted: 31 March 2018 © The Author(s) 2018 Abstract Deposition of mine tailings in a cold climate requires precautions as temporary sub-zero temperatures can imply considerable consequences to the storage due to creation of permafrost. The risk of creating man-made permafrost lenses due to tailings deposition exists even in regions with no natural permafrost, as material being frozen during winter might not fully thaw by the following summer. When such frozen layers thaw during later longer warmer periods, excess pore water pressure and large settlements might develop. Such implications close to the dam structure have to be avoided and therefore the risk of generat- ing permafrost should be reduced. This paper describes a geothermal model for one-dimensional heat conduction analysis. The model is able to simulate the temperature profle in tailings where the surface elevation is constantly increased due to deposition. At the tailings surface, the boundary condition is the air temperature changing over time during the year. Air temperatures, tailings deposition schedule and tailings properties are given as input to the model and can easily be changed and applied to specifc facilities. The model can be used for tailings facilities in cold regions, where the efects of tailings deposition on the temperature regime are of interest. Findings can improve tailings management by explaining man-made permafrost generation.