Thixotropy and Structural Breakdown Properties of Self Consolidating
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Regulatory Guide 3.39 Standard Format & Content of License
NUREG-O010 USNRC REGULATORY J GUIDE SERIES REGULATORY GUIDE 3.39 STANDARD FORMAT AND CONTENT OF LICENSE APPLICATIONS FOR PLUTONIUM PROCESSING 2 AND FUEL FABRICATION PLANTS JANUARY 1976 UNITED STATES NUCLEAR REGULATORY COMMISSION Available from National Technical Information Service Springfield, Virginia 22161 Price: Printed Copy $5.50 ; Microfiche $2.25 U.S. NUCLEAR REGULATORY COMMISSION January 1976 REGULATORY GUIDE OFFICE OF STANDARDS DEVELOPMENT REGULATORY GUIDE 3.39 1 STANDARD FORMAT AND C KEN\ OF LICENSE APPLIC 0O1 .R PLUTONIUM PROCf$ L4('I AND FUEL FABRjATI XP lTS USNRC REGULATORY GUIDES Comments should be sent to the Secretary of the Commission. U.S. Nuclear Regulatory Guides are Issued to describe and make available to the public Regulatory Commission. Washington. D.C. 20555. Attention Docketing and methods ecceptable to the NRC staff of implementing specific parts of the Service Section Commission's regulations, to delineate techniques used by the staff in evelu eting specific problems or postulated accidents. or to provide guidance to appli The guides are issued In the following ten broed divisions cants Regulatory Guides are not substitutes for regulations. and compliance 1 wer Reactors 6. Products with them Is not required. Methods end solutions different from those set 2. out in Research and Test Reactors 7. Transponation the guides will be acceptable if they provide a basis for the findings requisite to 3. Fuels and Materiels Facilities I Occupational Health the issuance or continuance of apermit or license by the Commission 4. Evironmental andSiting 9.Antitrust Review Comments and suggestions for Improvements in these guides are encouraged 5. Materials and Plant Protection 10. -
World Reference Base for Soil Resources 2014 International Soil Classification System for Naming Soils and Creating Legends for Soil Maps
ISSN 0532-0488 WORLD SOIL RESOURCES REPORTS 106 World reference base for soil resources 2014 International soil classification system for naming soils and creating legends for soil maps Update 2015 Cover photographs (left to right): Ekranic Technosol – Austria (©Erika Michéli) Reductaquic Cryosol – Russia (©Maria Gerasimova) Ferralic Nitisol – Australia (©Ben Harms) Pellic Vertisol – Bulgaria (©Erika Michéli) Albic Podzol – Czech Republic (©Erika Michéli) Hypercalcic Kastanozem – Mexico (©Carlos Cruz Gaistardo) Stagnic Luvisol – South Africa (©Márta Fuchs) Copies of FAO publications can be requested from: SALES AND MARKETING GROUP Information Division Food and Agriculture Organization of the United Nations Viale delle Terme di Caracalla 00100 Rome, Italy E-mail: [email protected] Fax: (+39) 06 57053360 Web site: http://www.fao.org WORLD SOIL World reference base RESOURCES REPORTS for soil resources 2014 106 International soil classification system for naming soils and creating legends for soil maps Update 2015 FOOD AND AGRICULTURE ORGANIZATION OF THE UNITED NATIONS Rome, 2015 The designations employed and the presentation of material in this information product do not imply the expression of any opinion whatsoever on the part of the Food and Agriculture Organization of the United Nations (FAO) concerning the legal or development status of any country, territory, city or area or of its authorities, or concerning the delimitation of its frontiers or boundaries. The mention of specific companies or products of manufacturers, whether or not these have been patented, does not imply that these have been endorsed or recommended by FAO in preference to others of a similar nature that are not mentioned. The views expressed in this information product are those of the author(s) and do not necessarily reflect the views or policies of FAO. -
International Society for Soil Mechanics and Geotechnical Engineering
INTERNATIONAL SOCIETY FOR SOIL MECHANICS AND GEOTECHNICAL ENGINEERING This paper was downloaded from the Online Library of the International Society for Soil Mechanics and Geotechnical Engineering (ISSMGE). The library is available here: https://www.issmge.org/publications/online-library This is an open-access database that archives thousands of papers published under the Auspices of the ISSMGE and maintained by the Innovation and Development Committee of ISSMGE. 1/18 Liquefaction of Saturated Sandy Soils Liquéfaction de sols sableux saturés by V. A. F lorin , Professor, Doctor of Technical Sciences, Associate Member of the USSR Academy of Sciences, Institute of Mechanics of the USSR Academy of Sciences, and P. L. I vanov , Docent, Candidate of Technical Sciences, Leningrad Polytechnic Institute. Summary Sommaire The authors give results obtained from theoretical and Le présent rapport contient quelques résultats des études experimental research on the liquefaction of saturated sandy théoriques et expérimentales des phénomènes de liquéfaction soils undertaken by them, in the Laboratory of Soil Mechanics de sols sableux saturés qui ont été effectuées aux Laboratoires of the Institute of Mechanics of the U.S.S.R. Academy of Sciences de Mécanique des sols de l’institut de Mécanique de l’Académie and in the Leningrad Polytechnic Institute. des Sciences de l’U.R.S.S. et de l’institut Polytechnique de Laboratory investigations have been carried out on various Leningrad. kinds of disturbances affecting saturated sandy soils and causing Les auteurs décrivent des études de Laboratoire de la liqué their liquefaction. The authors also give the results of studies faction de sols sableux soumis à diverses influences. -
An Empirical Approach for Tunnel Support Design Through Q and Rmi Systems in Fractured Rock Mass
applied sciences Article An Empirical Approach for Tunnel Support Design through Q and RMi Systems in Fractured Rock Mass Jaekook Lee 1, Hafeezur Rehman 1,2, Abdul Muntaqim Naji 1,3, Jung-Joo Kim 4 and Han-Kyu Yoo 1,* 1 Department of Civil and Environmental Engineering, Hanyang University, 55 Hanyangdaehak-ro, Sangnok-gu, Ansan 426-791, Korea; [email protected] (J.L.); [email protected] (H.R.); [email protected] (A.M.N.) 2 Department of Mining Engineering, Faculty of Engineering, Baluchistan University of Information Technology, Engineering and Management Sciences (BUITEMS), Quetta 87300, Pakistan 3 Department of Geological Engineering, Faculty of Engineering, Baluchistan University of Information Technology, Engineering and Management Sciences (BUITEMS), Quetta 87300, Pakistan 4 Korea Railroad Research Institute, 176 Cheoldobangmulgwan-ro, Uiwang-si, Gyeonggi-do 16105, Korea; [email protected] * Correspondence: [email protected]; Tel.: +82-31-400-5147; Fax: +82-31-409-4104 Received: 26 November 2018; Accepted: 14 December 2018; Published: 18 December 2018 Abstract: Empirical systems for the classification of rock mass are used primarily for preliminary support design in tunneling. When applying the existing acceptable international systems for tunnel preliminary supports in high-stress environments, the tunneling quality index (Q) and the rock mass index (RMi) systems that are preferred over geomechanical classification due to the stress characterization parameters that are incorporated into the two systems. However, these two systems are not appropriate when applied in a location where the rock is jointed and experiencing high stresses. This paper empirically extends the application of the two systems to tunnel support design in excavations in such locations. -
FHWA/TX-07/0-5202-1 Accession No
Technical Report Documentation Page 1. Report No. 2. Government 3. Recipient’s Catalog No. FHWA/TX-07/0-5202-1 Accession No. 4. Title and Subtitle 5. Report Date Determination of Field Suction Values, Hydraulic Properties, August 2005; Revised March 2007 and Shear Strength in High PI Clays 6. Performing Organization Code 7. Author(s) 8. Performing Organization Report No. Jorge G. Zornberg, Jeffrey Kuhn, and Stephen Wright 0-5202-1 9. Performing Organization Name and Address 10. Work Unit No. (TRAIS) Center for Transportation Research 11. Contract or Grant No. The University of Texas at Austin 0-5202 3208 Red River, Suite 200 Austin, TX 78705-2650 12. Sponsoring Agency Name and Address 13. Type of Report and Period Covered Texas Department of Transportation Technical Report Research and Technology Implementation Office September 2004–August 2006 P.O. Box 5080 14. Sponsoring Agency Code Austin, TX 78763-5080 15. Supplementary Notes Project performed in cooperation with the Texas Department of Transportation and the Federal Highway Administration. Project Title: Determination of Field Suction Values in High PI Clays for Various Surface Conditions and Drain Installations 16. Abstract Moisture infiltration into highway embankments constructed by the Texas Department of Transportation (TxDOT) using high Plasticity Index (PI) clays results in changes in shear strength and in flow pattern that leads to recurrent slope failures. In addition, soil cracking over time increases the rate of moisture infiltration. The overall objective of this research is to determine the suction, hydraulic properties, and shear strength of high PI Texas clays. Specifically, two comprehensive experimental programs involving the characterization of unsaturated properties and the shear strength of a high PI clay (Eagle Ford clay) were conducted. -
Evaluation of Soil Dilatancy
The Influence of Grain Shape on Dilatancy Item Type text; Electronic Dissertation Authors Cox, Melissa Reiko Brooke Publisher The University of Arizona. Rights Copyright © is held by the author. Digital access to this material is made possible by the University Libraries, University of Arizona. Further transmission, reproduction or presentation (such as public display or performance) of protected items is prohibited except with permission of the author. Download date 24/09/2021 03:25:54 Link to Item http://hdl.handle.net/10150/195563 THE INFLUENCE OF GRAIN SHAPE ON DILATANCY by MELISSA REIKO BROOKE COX ________________________ A Dissertation Submitted to the Faculty of the DEPARTMENT OF CIVIL ENGINEERING AND ENGINEERING MECHANICS In Partial Fulfillment of the Requirements For the Degree of DOCTOR OF PHILOSOPHY WITH A MAJOR IN CIVIL ENGINEERING In the Graduate College THE UNIVERISTY OF ARIZONA 2 0 0 8 2 THE UNIVERSITY OF ARIZONA GRADUATE COLLEGE As members of the Dissertation Committee, we certify that we have read the dissertation prepared by Melissa Reiko Brooke Cox entitled The Influence of Grain Shape on Dilatancy and recommend that it be accepted as fulfilling the dissertation requirement for the Degree of Doctor of Philosophy ___________________________________________________________________________ Date: October 17, 2008 Muniram Budhu ___________________________________________________________________________ Date: October 17, 2008 Achintya Haldar ___________________________________________________________________________ Date: October 17, 2008 Chandrakant S. Desai ___________________________________________________________________________ Date: October 17, 2008 John M. Kemeny Final approval and acceptance of this dissertation is contingent upon the candidate’s submission of the final copies of the dissertation to the Graduate College. I hereby certify that I have read this dissertation prepared under my direction and recommend that it be accepted as fulfilling the dissertation requirement. -
Slope Stability 101 Basic Concepts and NOT for Final Design Purposes! Slope Stability Analysis Basics
Slope Stability 101 Basic Concepts and NOT for Final Design Purposes! Slope Stability Analysis Basics Shear Strength of Soils Ability of soil to resist sliding on itself on the slope Angle of Repose definition n1. the maximum angle to the horizontal at which rocks, soil, etc, will remain without sliding Shear Strength Parameters and Soils Info Φ angle of internal friction C cohesion (clays are cohesive and sands are non-cohesive) Θ slope angle γ unit weight of soil Internal Angles of Friction Estimates for our use in example Silty sand Φ = 25 degrees Loose sand Φ = 30 degrees Medium to Dense sand Φ = 35 degrees Rock Riprap Φ = 40 degrees Slope Stability Analysis Basics Explore Site Geology Characterize soil shear strength Construct slope stability model Establish seepage and groundwater conditions Select loading condition Locate critical failure surface Iterate until minimum Factor of Safety (FS) is achieved Rules of Thumb and “Easy” Method of Estimating Slope Stability Geology and Soils Information Needed (from site or soils database) Check appropriate loading conditions (seeps, rapid drawdown, fluctuating water levels, flows) Select values to input for Φ and C Locate water table in slope (critical for evaluation!) 2:1 slopes are typically stable for less than 15 foot heights Note whether or not existing slopes are vegetated and stable Plan for a factor of safety (hazards evaluation) FS between 1.4 and 1.5 is typically adequate for our purposes No Flow Slope Stability Analysis FS = tan Φ / tan Θ Where Φ is the effective -
Impact of Thixotropy on Flow Patterns Induced in a Stirred Tank
CORE Metadata, citation and similar papers at core.ac.uk Provided by Open Archive Toulouse Archive Ouverte Impact of thixotropy on flow patterns induced in a stirred tank: Numerical and experimental studies G. Couerbe a, D.F. Fletcher b, C. Xuereb a, M. Poux a,∗ a Universit e´ de Toulouse, Laboratoire de G enie´ Chimique, CNRS/INP/UPS, 5 rue Paulin Talabot, BP 1301, 31106 Toulouse Cedex, France b School of Chemical and Biomolecular Engineering, The University of Sydney, NSW 2006, Australia abstract Agitation of a thixotropic shear•thinning fluid exhibiting a yield stress is investigated both experimentally and via simulations. Steady•state experiments are conducted at three 1 impeller rotation rates (1, 2 and 8 s − ) for a tank stirred with an axial•impeller and flow•field measurements are made using particle image velocimetry (PIV) measurements. Three• dimensional numerical simulations are also performed using the commercial CFD code Keywords: ANSYS CFX10.0. The viscosity of the suspension is determined experimentally and is mod• Thixotropy elled using two shear•dependant laws, one of which takes into account the flow instabilities CFD of such fluids at low shear rates. At the highest impeller speed, the flow exhibits the famil• PIV iar outward pumping action associated with axial•flow impellers. However, as the impeller Stirred tank speed decreases, a cavern is formed around the impeller, the flow generated in the vicin• Impeller ity of the agitator reorganizes and its pumping capacity vanishes. An unusual flow pattern, Mixing where the radial velocity dominates, is observed experimentally at the lowest stirring speed. It is found to result from wall slip effects. -
Thixotropy Vs Wall Slip in Suspensions
Thixotropy vs wall slip in suspensions Wonjae Choi Papers : Dullaert, Mewis : Thixotropy : Build-up and breakdown curves during flow ( JoR, 2005 ) Claimed the first robust stress measurement of the thixotropic system Introduced de-embedding of rheometer’s transfer function from the output data Dullaert, Mewis : A model system for thixotropy studies ( Rheol Acta, 2005 ) Detailed description on the previous ‘robust thixotropic system’ Covered various issues which was problematic for previous researches and was reduced with their new compound Covered wall-slip phenomenon and remedy for it Experiments about thixotropy Difficulties in experiments While there are various models & theories about thixotropy, there are few reliable experimental datasets Primary reason for this is the difficulties involved in measuring thixotropic system with enough accuracy Main objective of this paper Building robust thixotropic system which supports repeatible & reliable measurements Recall : Definition of thixotropy in this paper Change of floc structure resulting in varying viscosity Does not necessarily include viselasticity Why is measurement difficult? Implemental artifacts Wall slip Heterogeneous shear rates Gap size effect Rheometer’s transfer function Memory of floc’s microstructure Evaporation of solvents Particle sedimentation, change in particle’s wetting property, adsorption Plan Wall slip Interparticle attraction & PIB Viscosity control Sedimentation Memory Steady-state Enough pre-treatment Evaporation Non volatile suspension -
Stability Charts for a Tall Tunnel in Undrained Clay
Int. J. of GEOMATE, April, 2016, Vol. 10, No. 2 (Sl. No. 20), pp. 1764-1769 Geotech., Const. Mat. and Env., ISSN: 2186-2982(P), 2186-2990(O), Japan STABILITY CHARTS FOR A TALL TUNNEL IN UNDRAINED CLAY Jim Shiau1, Mathew Sams1 and Jing Chen1 1School of Civil Engineering and Surveying, University of Southern Queensland, Australia ABSTRACT The stability of a plane strain tall rectangular tunnel in undrained clay is investigated in this paper using shear strength reduction technique. The finite difference program FLAC is used to determine the factor of safety for unsupported tall rectangular tunnels. Numerical results are compared with upper and lower bound limit solutions, and the comparison finds a very good agreement with solutions to be within 5% difference. Design charts for tall rectangular tunnels are then presented for a wide range of practical scenarios using dimensionless ratios ~ a similar approach to Taylor’s slope stability chart. A number of typical examples are presented to illustrate the potential usefulness for practicing engineers. Keywords: Stability Analysis, Tall Tunnel, Undrained Clay, Factor of Safety, FLAC, Strength Reduction Method INTRODUCTION C/D and the strength ratio Su/γD. This approach is very similar to the widely used Taylor’s design chart The critical geotechnical aspects for tunnel design for slope stability analysis (Taylor, 1937) [9]. discussed by Peck (1969) in [1] are: stability during construction, ground movements, and the determination of structural forces for the lining design. The focus of this paper is on the design consideration of tunnel stability that was expressed by a stability number initially defined by Broms and Bennermark (1967) [2] in equation 1: = (1) − + Fig. -
Shear Strength Examples.Pdf
444 Chapter 12: Shear Strength of Soil Example 12.2 Following are the results of four drained direct shear tests on an overconsolidated clay: • Diameter of specimen ϭ 50 mm • Height of specimen ϭ 25 mm Normal Shear force at Residual shear Test force, N failure, Speak force, Sresidual no. (N) (N) (N) 1 150 157.5 44.2 2 250 199.9 56.6 3 350 257.6 102.9 4 550 363.4 144.5 © Cengage Learning 2014 t t Determine the relationships for peak shear strength ( f) and residual shear strength ( r). Solution 50 2 Area of the specimen 1A2 ϭ 1p/42 a b ϭ 0.0019634 m2. Now the following 1000 table can be prepared. Residual S shear peak S force, T ϭ residual ؍ Normal Normal Peak shearT S f r Test force, N stress, force, Speak A Sresidual A no. (N) (kN/m2) (N) (kN/m2) (N) (kN/m2) 1 150 76.4 157.5 80.2 44.2 22.5 2 250 127.3 199.9 101.8 56.6 28.8 3 350 178.3 257.6 131.2 102.9 52.4 4 550 280.1 363.4 185.1 144.5 73.6 © Cengage Learning 2014 t t sЈ The variations of f and r with are plotted in Figure 12.19. From the plots, we find that t 2 ϭ ؉ S Peak strength: f (kN/m ) 40 tan 27 t 2 ϭ S Residual strength: r(kN/m ) tan 14.6 (Note: For all overconsolidated clays, the residual shear strength can be expressed as t ϭ sœ fœ r tan r fœ ϭ where r effective residual friction angle.) Copyright 2012 Cengage Learning. -
Cyclic Response of a Sand with Thixotropic Pore Fluid
Cyclic Response of a Sand with Thixotropic Pore Fluid C.S. El Mohtar1, J. Clarke1, A. Bobet1, M. Santagata1, V. Drnevich1 and C. Johnston2 1School of Civil Engineering, Purdue University, West Lafayette, IN 2Department of Agronomy, Purdue University, West Lafayette, IN ABSTRACT Saturated specimens of Ottawa sand prepared with 0%, 3% and 5% bentonite by dry mass of sand are tested under cyclic loading to investigate the effects of bentonite on the cyclic response. For the same skeleton relative density and cyclic stress ratio (CSR), the cyclic tests on the sand-bentonite mixtures show a significant increase of the number of cycles required for liquefaction compared to the clean sand. This is caused , as observed in resonant column tests, by an increase of the elastic threshold due to the presence of bentonite, which delays the generation of excess pore pressure. Such behavior can be explained by the rheological properties of the pore fluid. Oscillatory tests conducted with a rheometer on bentonite slurries show that for shear strains as large as 1% these materials exhibit elastic behavior with a constant shear modulus. Moreover, due to the thixotropic nature of the bentonite slurries, their storage modulus shows a marked increase with time. This observation is consistent with the increase in the liquefaction resistance of the sand-bentonite mixtures with time also observed in cyclic triaxial experiments. INTRODUCTION Liquefaction is an important cause of damage to civil infrastructures during earthquakes. Notable examples are: the collapse