University of Dundee Newmark Sliding Block
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Newmark Sliding Block Analysis
TRANSPORTATION RESEARCH RECORD 1411 9 Predicting Earthquake-Induced Landslide Displacements Using Newmark's Sliding Block Analysis RANDALL W. }IBSON A principal cause of earthquake damage is landsliding, and the peak ground accelerations (PGA) below which no slope dis ability to predict earthquake-triggered landslide displacements is placement will occur. In cases where the PGA does exceed important for many types of seismic-hazard analysis and for the the yield acceleration, pseudostatic analysis has proved to be design of engineered slopes. Newmark's method for modeling a landslide as a rigid-plastic block sliding on an inclined plane pro vastly overconservative because many slopes experience tran vides a workable means of predicting approximate landslide dis sient earthquake accelerations well above their yield accel placements; this method yields much more useful information erations but experience little or no permanent displacement than pseudostatic analysis and is far more practical than finite (2). The utility of pseudostatic analysis is thus limited because element modeling. Applying Newmark's method requires know it provides only a single numerical threshold below which no ing the yield or critical acceleration of the landslide (above which displacement is predicted and above which total, but unde permanent displacement occurs), which can be determined from the static factor of safety and from the landslide geometry. Earth fined, "failure" is predicted. In fact, pseudostatic analysis tells quake acceleration-time histories can be selected to represent the the user nothing about what will occur when the yield accel shaking conditions of interest, and those parts of the record that eration is exceeded. lie above the critical acceleration are double integrated to deter At the other end of the spectrum, advances in two-dimensional mine the permanent landslide displacement. -
Identification of Maximum Road Friction Coefficient and Optimal Slip Ratio Based on Road Type Recognition
CHINESE JOURNAL OF MECHANICAL ENGINEERING ·1018· Vol. 27,aNo. 5,a2014 DOI: 10.3901/CJME.2014.0725.128, available online at www.springerlink.com; www.cjmenet.com; www.cjmenet.com.cn Identification of Maximum Road Friction Coefficient and Optimal Slip Ratio Based on Road Type Recognition GUAN Hsin, WANG Bo, LU Pingping*, and XU Liang State Key Laboratory of Automotive Simulation and Control, Jilin University, Changchun 130022, China Received November 21, 2013; revised June 9, 2014; accepted July 25, 2014 Abstract: The identification of maximum road friction coefficient and optimal slip ratio is crucial to vehicle dynamics and control. However, it is always not easy to identify the maximum road friction coefficient with high robustness and good adaptability to various vehicle operating conditions. The existing investigations on robust identification of maximum road friction coefficient are unsatisfactory. In this paper, an identification approach based on road type recognition is proposed for the robust identification of maximum road friction coefficient and optimal slip ratio. The instantaneous road friction coefficient is estimated through the recursive least square with a forgetting factor method based on the single wheel model, and the estimated road friction coefficient and slip ratio are grouped in a set of samples in a small time interval before the current time, which are updated with time progressing. The current road type is recognized by comparing the samples of the estimated road friction coefficient with the standard road friction coefficient of each typical road, and the minimum statistical error is used as the recognition principle to improve identification robustness. Once the road type is recognized, the maximum road friction coefficient and optimal slip ratio are determined. -
Borrow Pit Volumes**
EARTHWORK CONSTRUCTION AND LAYOUT **BORROW PIT VOLUMES** When trying to figure out Borrow Pit Problems you need to understand a few things. 1. Water can be added or removed from soil 2. The MASS of the SOLIDS CAN NOT be changed 3. Need to know phase relationships in soil….which I will show you next Phase relationship in Soil This represents the soil that you take from a borrow pit. It is made up of AIR, WATER, and SOLIDS. AIR WATER So if you separated the soil into its components it would look like this. It is referred to as a Soil Phase Diagram. SOIL When looking at a Soil Phase Diagram you think of it two ways, 1. Volume, 2. Mass. Volume Mass Va AIR Ma = 0 Va = Volume Air Ma = Mass Air = 0 V WATER M Vw = Volume Water w w Mw = Mass Water Vs = Volume Solid Ms = Mass Solid Vs SOIL Ms Vt = Volume Total = Va + Vw + Vs Mt = Mass Total = Mw + Ms EARTHWORK CONSTRUCTION AND LAYOUT **BORROW PIT VOLUMES** Basic Terms/Formulas to know – Soil Phase relationship Specific Gravity = the density of the solids divided by the density of Water Moisture Content = Mass of Water divided by the Mass of Solids Void Ratio = Volume of Voids divided by the Volume of Solids Porosity = Volume of Voids divided by the Total Volume, Higher porosity = higher permeability Density of Water = γwater = Mw/Vw Specific Gravity = Gs = γsolids /γwater =M /(V * γ ) English Units = 62.42 pounds per CF(pcf) s s water SI Units = 1,000 g/liter = 1,000kg/m3 Moisture Content (w) = Mw/Ms Porosity (n) = Vv/Vt Vv = Volume of Voids = Vw + Va Vt = Total Volume = Vs +Vw + Va Degree of Saturation -
Soil Plugging of Open-Ended Piles During Impact Driving in Cohesion-Less Soil
Soil Plugging of Open-Ended Piles During Impact Driving in Cohesion-less Soil VICTOR KARLOWSKIS Master of Science Thesis Stockholm, Sweden 2014 © Victor Karlowskis 2014 Master of Science thesis 14/13 Royal Institute of Technology (KTH) Department of Civil and Architectural Engineering Division of Soil and Rock Mechanics ABSTRACT Abstract During impact driving of open-ended piles through cohesion-less soil the internal soil column may mobilize enough internal shaft resistance to prevent new soil from entering the pile. This phenomena, referred to as soil plugging, changes the driving characteristics of the open-ended pile to that of a closed-ended, full displacement pile. If the plugging behavior is not correctly understood, the result is often that unnecessarily powerful and costly hammers are used because of high predicted driving resistance or that the pile plugs unexpectedly such that the hammer cannot achieve further penetration. Today the user is generally required to model the pile response on the basis of a plugged or unplugged pile, indicating a need to be able to evaluate soil plugging prior to performing the drivability analysis and before using the results as basis for decision. This MSc. thesis focuses on soil plugging during impact driving of open-ended piles in cohesion-less soil and aims to contribute to the understanding of this area by evaluating models for predicting soil plugging and driving resistance of open-ended piles. Evaluation was done on the basis of known soil plugging mechanisms and practical aspects of pile driving. Two recently published models, one for predicting the likelihood of plugging and the other for predicting the driving resistance of open-ended piles, were compared to existing models. -
Undergraduate Research on Conceptual Design of a Wind Tunnel for Instructional Purposes
AC 2012-3461: UNDERGRADUATE RESEARCH ON CONCEPTUAL DE- SIGN OF A WIND TUNNEL FOR INSTRUCTIONAL PURPOSES Peter John Arslanian, NASA/Computer Sciences Corporation Peter John Arslanian currently holds an engineering position at Computer Sciences Corporation. He works as a Ground Safety Engineer supporting Sounding Rocket and ANTARES launch vehicles at NASA, Wallops Island, Va. He also acts as an Electrical Engineer supporting testing and validation for NASA’s Low Density Supersonic Decelerator vehicle. Arslanian has received an Undergraduate Degree with Honors in Engineering with an Aerospace Specialization from the University of Maryland, Eastern Shore (UMES) in May 2011. Prior to receiving his undergraduate degree, he worked as an Action Sport Design Engineer for Hydroglas Composites in San Clemente, Calif., from 1994 to 2006, designing personnel watercraft hulls. Arslanian served in the U.S. Navy from 1989 to 1993 as Lead Electronics Technician for the Automatic Carrier Landing System aboard the U.S.S. Independence CV-62, stationed in Yokosuka, Japan. During his enlistment, Arslanian was honored with two South West Asia Service Medals. Dr. Payam Matin, University of Maryland, Eastern Shore Payam Matin is currently an Assistant Professor in the Department of Engineering and Aviation Sciences at the University of Maryland Eastern Shore (UMES). Matin has received his Ph.D. in mechanical engi- neering from Oakland University, Rochester, Mich., in May 2005. He has taught a number of courses in the areas of mechanical engineering and aerospace at UMES. Matin’s research has been mostly in the areas of computational mechanics and experimental mechanics. Matin has published more than 20 peer- reviewed journal and conference papers. -
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 -
Newmark Sliding Block Model for Predicting the Seismic Performance of MARK Vegetated Slopes ⁎ T
Soil Dynamics and Earthquake Engineering 101 (2017) 27–40 Contents lists available at ScienceDirect Soil Dynamics and Earthquake Engineering journal homepage: www.elsevier.com/locate/soildyn Newmark sliding block model for predicting the seismic performance of MARK vegetated slopes ⁎ T. Liang, J.A. Knappett ARTICLE INFO ABSTRACT Keywords: This paper presents a simplified procedure for predicting the seismic slip of a vegetated slope. This is important Analytical modelling for more precise estimation of the hazard associated with seismic landslip of naturally vegetated slopes, and also Centrifuge modelling as a design tool for determining performance improvement when planting is to be used as a protective measure. Dynamics The analysis procedure consists of two main components. Firstly, Discontinuity Layout Optimisation (DLO) Earthquakes analysis is used to determine the critical seismic slope failure mechanism and estimate the corresponding yield Sand acceleration of a given slope. In DLO analysis, a modified rigid perfectly plastic (Mohr–Coulomb) model is Slopes Vegetation employed to approximate small permanent deformations which may accrue in non-associative materials when Ecological Engineering subjected to ground motions with relatively low peak ground acceleration. The contribution of the vegetation to enhancing the yield acceleration is obtained via subtraction of the fallow slope yield acceleration. The second stage of the analysis incorporates the vegetation contribution to the slope's yield acceleration from DLO into modified limit equilibrium equations to further account for the geometric hardening of the slope under in- creasing soil movement. Thereby, the method can predict the permanent settlement at the crest of the slope via a slip-dependent Newmark sliding block approach. -
Diminishing Friction of Joint Surfaces As Initiating Factor for Destabilising Permafrost Rocks?
Geophysical Research Abstracts Vol. 12, EGU2010-3440-1, 2010 EGU General Assembly 2010 © Author(s) 2010 Diminishing friction of joint surfaces as initiating factor for destabilising permafrost rocks? Daniel Funk and Michael Krautblatter Department of Geogrpahy, University of Bonn, Germany ([email protected]) Degrading alpine permafrost due to changing climate conditions causes instabilities in steep rock slopes. Due to a lack in process understanding, the hazard is still difficult to asses in terms of its timing, location, magnitude and frequency. Current research is focused on ice within joints which is considered to be the key-factor. Monitoring of permafrost-induced rock failure comprises monitoring of temperature and moisture in rock-joints. The effect of low temperatures on the strength of intact rock and its mechanical relevance for shear strength has not been considered yet. But this effect is signifcant since compressive and tensile strength is reduced by up to 50% and more when rock thaws (Mellor, 1973). We hypotheisze, that the thawing of permafrost in rocks reduces the shear strength of joints by facilitating the shearing/damaging of asperities due to the drop of the compressive/tensile strength of rock. We think, that decreas- ing surface friction, a neglected factor in stability analysis, is crucial for the onset of destabilisation of permafrost rocks. A potential rock slide within the permafrost zone in the Wetterstein Mountains (Zugspitze, Germany) is the basis for the data we use for the empirical joint model of Barton (1973) to estimate the peak shear strength of the shear plane. Parameters are the JRC (joint roughness coefficient), the JCS (joint compressive strength) and the residual friction angle ('r). -
Slope Stability
SLOPE STABILITY Chapter 15 Omitted parts: Sections 15.13, 15.14,15.15 TOPICS Introduction Types of slope movements Concepts of Slope Stability Analysis Factor of Safety Stability of Infinite Slopes Stability of Finite Slopes with Plane Failure Surface o Culmann’s Method Stability of Finite Slopes with Circular Failure Surface o Mass Method o Method of Slices TOPICS Introduction Types of slope movements Concepts of Slope Stability Analysis Factor of Safety Stability of Infinite Slopes Stability of Finite Slopes with Plane Failure Surface o Culmann’s Method Stability of Finite Slopes with Circular Failure Surface o Mass Method o Method of Slices SLOPE STABILITY What is a Slope? An exposed ground surface that stands at an angle with the horizontal. Why do we need slope stability? In geotechnical engineering, the topic stability of slopes deals with: 1.The engineering design of slopes of man-made slopes in advance (a) Earth dams and embankments, (b) Excavated slopes, (c) Deep-seated failure of foundations and retaining walls. 2. The study of the stability of existing or natural slopes of earthworks and natural slopes. o In any case the ground not being level results in gravity components of the weight tending to move the soil from the high point to a lower level. When the component of gravity is large enough, slope failure can occur, i.e. the soil mass slide downward. o The stability of any soil slope depends on the shear strength of the soil typically expressed by friction angle (f) and cohesion (c). TYPES OF SLOPE Slopes can be categorized into two groups: A. -
Section 6D-1 Embankment Construction
6D-1 Design Manual Chapter 6 - Geotechnical 6D - Embankment Construction Embankment Construction A. General Information Quality embankment construction is required to maintain smooth-riding pavements and to provide slope stability. Proper selection of soil, adequate moisture control, and uniform compaction are required for a quality embankment. Problems resulting from poor embankment construction have occasionally resulted in slope stability problems that encroach on private property and damage drainage structures. Also, pavement roughness can result from non-uniform support. The costs for remediation of such failures are high. Soils available for embankment construction in Iowa generally range from A-4 soils (ML, OL), which are very fine sands and silts that are subject to frost heave, to A-6 and A-7 soils (CL, OH, MH, CG), which predominate across the state. The A-6 and A-7 groups include shrink/swell clayey soils. In general, these soils rate from poor to fair in suitability as subgrade soils. Because of their abundance, economics dictate that these soils must be used on the projects even though they exhibit shrink/swell properties. Because these are marginal soils, it is critical that the embankments be placed with proper compaction and moisture content, and in some cases, stabilization (see Section 6H-1 - Foundation Improvement and Stabilization). Soils for embankment projects are identified during the exploration phase of the construction process. Borings are taken periodically along the proposed route and at potential borrow pits. The soils are tested to determine their engineering properties. Atterberg limits are determined and in-situ moisture and density are compared to standard Proctor values. -
Landslides and the Weathering of Granitic Rocks
Geological Society of America Reviews in Engineering Geology, Volume III © 1977 7 Landslides and the weathering of granitic rocks PHILIP B. DURGIN Pacific Southwest Forest and Range Experiment Station, Forest Service, U.S. Department of Agriculture, Berkeley, California 94701 (stationed at Arcata, California 95521) ABSTRACT decomposition, so they commonly occur as mountainous ero- sional remnants. Nevertheless, granitoids undergo progressive Granitic batholiths around the Pacific Ocean basin provide physical, chemical, and biological weathering that weakens examples of landslide types that characterize progressive stages the rock and prepares it for mass movement. Rainstorms and of weathering. The stages include (1) fresh rock, (2) core- earthquakes then trigger slides at susceptible sites. stones, (3) decomposed granitoid, and (4) saprolite. Fresh The minerals of granitic rock weather according to this granitoid is subject to rockfalls, rockslides, and block glides. sequence: plagioclase feldspar, biotite, potassium feldspar, They are all controlled by factors related to jointing. Smooth muscovite, and quartz. Biotite is a particularly active agent in surfaces of sheeted fresh granite encourage debris avalanches the weathering process of granite. It expands to form hydro- or debris slides in the overlying material. The corestone phase biotite that helps disintegrate the rock into grus (Wahrhaftig, is characterized by unweathered granitic blocks or boulders 1965; Isherwood and Street, 1976). The feldspars break down within decomposed rock. Hazards at this stage are rockfall by hyrolysis and hydration into clays and colloids, which may avalanches and rolling rocks. Decomposed granitoid is rock migrate from the rock. Muscovite and quartz grains weather that has undergone granular disintegration. Its characteristic slowly and usually form the skeleton of saprolite. -
Issue No 14, July/August 2019
FT / PHOTOBOOTH FT / NEWS FT / STEQ Take a look at the best Keep up-to-date with the Recognising Safety, photographs captured by latest news and updates Training, Environment and you on projects, fleet and Quality across the business machinery and employees Aarsleff JULY/AUGUST 2019 ISSUE NO.14 STAFF NEWSLETTER WELCOME Welcome to Aarsleff Ground Engineering’s newsletter. Driven Precast Piling, Bicker, Triton Knoll I would like to open by welcoming Graduate Civil Engineer, order to survive. In this uncertain time, I need everyone Samuel Saul, and placement student Henry Lewis-Borrell to commit to winning projects, delivering them to the high back to Aarsleff after their previous work placements with quality we continue to promote, and all with a strong focus us in 2018. It is great to see the young and upcoming talent on collaboration and communication. joining Aarsleff. And the fact that they are returning to us I know we are excellent at what we do, and don’t just take also says a lot of great things about the culture we have my word on that. We won ‘Civil Engineering Project of the developed here. Year’ for our work at Riverside Rochdale and received a highly …Kevin Hague, Managing Director As I have discussed in previous newsletters and Staff Chat commended for our people development skills in this year’s meetings this year; there are still many uncertainties in East Midlands Celebration Construction Awards. We also the everchanging market, and we are facing a lot more received two highly commended awards for ‘Employer of the competition than we have ever had before.