On Vortex Shedding and Prediction of Vortex-Induced Vibrations of Circular Cylinders
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Causes and Behavior of a Tornadic Fire-Whirlwind
61 §OUTHWJE§T FOJRJE§T & JRANGJE JEXlPJEJREMlE '"'"T § TAT1,o~ 8 e r k e I e y , C a I i f o '{"1'~qiNNT':l E_ ;:;;~"~~~1 ,;i,.,. ..t"; .... ~~ :;~ ·-:-; , r~-.fi... .liCo)iw:;-;sl- Central Reference File II ....·~ 0 ........................................(). 7 ;s_ .·············· ··········· Causes and Behavior of a Tornadic Fire-Whirlwind ARTHUR R.PIRSKO, LEO M.SERGIUS, AND CARL W.HICKERSON ABSTRACT: A destructive whirlwind of tor Normally an early March nadic force was formed in a 600-acre brush fire burning on the lee side o f a ridge brush fire would not be much near Santa Barbara on March 7, 1964. The of a problem for experienced fire whirlwind, formed in a post-frontal unstable air mass, cut a mile long path, firefighters in the Santa Bar- injured 4 people, destroyed 2 houses, a barn, · bara area of the Los Padres and 4 automobiles, and wrecked a 100-tree avocado orchard. National Forest in southern California. But the Polo fire of March 7, 1964, spread several times faster than expected and culminated in a fire -whirl wind of tornadic violence (fig. 1). It represents a classic case of such fire behavior and was unusually well documented by surface and upper air observations. This fire damaged 600 acres of prime watershed land, and the fire -induced tornado injured 4 persons; destroyed 2 homes, a barn, and 3 automobiles; and toppled almost 100 avocado trees. BURNING CONDITIONS FUELS The fire area was predominantly 50-year old ceanothus (Cea nothus sp.) that stood 10 to 15 feet high (fig. 2). Minor amounts of California sagebrush (Artemisia californica) and scrub oak (Quer cus dumosa) were intermixed with the ceanothus. -
Sensitivity Analysis of Non-Linear Steep Waves Using VOF Method
Tenth International Conference on ICCFD10-268 Computational Fluid Dynamics (ICCFD10), Barcelona, Spain, July 9-13, 2018 Sensitivity Analysis of Non-linear Steep Waves using VOF Method A. Khaware*, V. Gupta*, K. Srikanth *, and P. Sharkey ** Corresponding author: [email protected] * ANSYS Software Pvt Ltd, Pune, India. ** ANSYS UK Ltd, Milton Park, UK Abstract: The analysis and prediction of non-linear waves is a crucial part of ocean hydrodynamics. Sea waves are typically non-linear in nature, and whilst models exist to predict their behavior, limits exist in their applicability. In practice, as the waves become increasingly steeper, they approach a point beyond which the wave integrity cannot be maintained, and they 'break'. Understanding the limits of available models as waves approach these break conditions can significantly help to improve the accuracy of their potential impact in the field. Moreover, inaccurate modeling of wave kinematics can result in erroneous hydrodynamic forces being predicted. This paper investigates the sensitivity of non-linear wave modeling from both an analytical and a numerical perspective. Using a Volume of Fluid (VOF) method, coupled with the Open Channel Flow module in ANSYS Fluent, sensitivity studies are performed for a variety of non-linear wave scenarios with high steepness and high relative height. These scenarios are intended to mimic the near-break conditions of the wave. 5th order solitary wave models are applied to shallow wave scenarios with high relative heights, and 5th order Stokes wave models are applied to short gravity waves with high wave steepness. Stokes waves are further applied in the shallow regime at high wave steepness to examine the wave sensitivity under extreme conditions. -
Boxer's Fracture • Knuckle Fracture of the Pinky
Boxer’s Fracture • Knuckle Fracture of the Pinky Introduction Treatment A Boxer’s fracture occurs when the bone at the knuckle Many Boxer’s fractures can be treated by immobi- of the little finger breaks. It can result from a forceful lizing the joint to promote healing. Immobilization can injury during fist fighting or hitting a solid object, such be achieved with a variety of splints, a cast, or taping as a wall. A Boxer’s fracture causes swelling, pain, and techniques. “Buddy-taping” involves taping the little stiffness. Treatment involves realigning the broken bone, finger to the ring finger. when necessary, and providing stabilization while it heals. Surgery Anatomy Surgery is recommended for Boxer’s fractures if large The “knuckle” of the fifth finger (small finger or “pinky”) degrees of angulation or displacement occur, or if the is comprised of the head of the metacarpal bone from joint surface is misaligned. Displacement and angulation the hand, and the base of the finger, called the proximal means that a piece or pieces of the metacarpal bone phalanx. The main function of your little finger is to that has broken have moved out of position. An open contribute to a tight strong grip. reduction and internal fixation (ORIF) surgery allows surgical hardware, such as wires and screws, to be Causes placed in the bone to align the fracture and allow it to A Boxer’s fracture occurs when the neck of the metacarpal heal in the correct position. bone in the little finger breaks. It is commonly caused by punching an immovable object, such as a wall, or Recovery someone’s jaw or head during a fist fight. -
Waves and Structures
WAVES AND STRUCTURES By Dr M C Deo Professor of Civil Engineering Indian Institute of Technology Bombay Powai, Mumbai 400 076 Contact: [email protected]; (+91) 22 2572 2377 (Please refer as follows, if you use any part of this book: Deo M C (2013): Waves and Structures, http://www.civil.iitb.ac.in/~mcdeo/waves.html) (Suggestions to improve/modify contents are welcome) 1 Content Chapter 1: Introduction 4 Chapter 2: Wave Theories 18 Chapter 3: Random Waves 47 Chapter 4: Wave Propagation 80 Chapter 5: Numerical Modeling of Waves 110 Chapter 6: Design Water Depth 115 Chapter 7: Wave Forces on Shore-Based Structures 132 Chapter 8: Wave Force On Small Diameter Members 150 Chapter 9: Maximum Wave Force on the Entire Structure 173 Chapter 10: Wave Forces on Large Diameter Members 187 Chapter 11: Spectral and Statistical Analysis of Wave Forces 209 Chapter 12: Wave Run Up 221 Chapter 13: Pipeline Hydrodynamics 234 Chapter 14: Statics of Floating Bodies 241 Chapter 15: Vibrations 268 Chapter 16: Motions of Freely Floating Bodies 283 Chapter 17: Motion Response of Compliant Structures 315 2 Notations 338 References 342 3 CHAPTER 1 INTRODUCTION 1.1 Introduction The knowledge of magnitude and behavior of ocean waves at site is an essential prerequisite for almost all activities in the ocean including planning, design, construction and operation related to harbor, coastal and structures. The waves of major concern to a harbor engineer are generated by the action of wind. The wind creates a disturbance in the sea which is restored to its calm equilibrium position by the action of gravity and hence resulting waves are called wind generated gravity waves. -
Activity 21: Cleavage and Fracture Maine Geological Survey
Activity 21: Cleavage and Fracture Maine Geological Survey Objectives: Students will recognize the difference between cleavage and fracture; they will become familiar with planes of cleavage, and will use a mineral's "habit of breaking" as an aid to identifying common minerals. Time: This activity is intended to take one-half (1/2) period to discuss cleavage planes and types and one (1) class period to do the activity. Background: Cleavage is the property of a mineral that allows it to break smoothly along specific internal planes (called cleavage planes) when the mineral is struck sharply with a hammer. Fracture is the property of a mineral breaking in a more or less random pattern with no smooth planar surfaces. Since nearly all minerals have an orderly atomic structure, individual mineral grains have internal axes of length, width, and depth, related to the consistent arrangement of the atoms. These axes are reflected in the crystalline pattern in which the mineral grows and are present in the mineral regardless of whether or not the sample shows external crystal faces. The axes' arrangement, size, and the angles at which these axes intersect, all help determine, along with the strength of the molecular bonding in the given mineral, the degree of cleavage the mineral will exhibit. Many minerals, when struck sharply with a hammer, will break smoothly along one or more of these planes. The degree of smoothness of the broken surface and the number of planes along which the mineral breaks are used to describe the cleavage. The possibilities include the following. Number of Planes Degree of Smoothness One Two Three Perfect Good Poor Thus a mineral's cleavage may be described as perfect three plane cleavage, in which case the mineral breaks with almost mirror-like surfaces along the three dimensional axes; the mineral calcite exhibits such cleavage. -
Scaling of Critical Velocity for Bubble Raft Fracture Under Tension Chin
Scaling of critical velocity for bubble raft fracture under tension Chin-Chang Kuo, and Michael Dennin1, a) Department of Physics and Astronomy and Institute for Complex Adaptive Matter, University of California at Irvine, Irvine, CA 92697-4575 (Dated: 9 September 2011) The behavior of materials under tension is a rich area of both fluid and solid mechanics. For simple fluids, the breakup of a liquid as it is pulled apart generally exhibits an instability driven, pinch-off type behavior. In contrast, solid materials typically exhibit various forms of fracture under tension. The interaction of these two distinct failure modes is of particular interest for complex fluids, such as foams, pastes, slurries, etc.. The rheological properties of complex fluids are well-known to combine features of solid and fluid behavior, and it is unclear how this translates to their failure under tension. In this paper, we present experimental results for a model complex fluid, a bubble raft. As expected, the system exhibits both pinch-off and fracture when subjected to elongation under constant velocity. We report on the critical velocity vc below which pinch-off occurs and above which fracture occurs as a function of initial system width W , length L, bubble size R, and fluid viscosity. The fluid viscosity sets the typical time for bubble rearrangements τ. The results for the critical velocity are consistent with a simple scaling law vcτ=L ∼ R=W that is based on the assumption that fracture is nucleated by the failure of local bubble rearrangements to occur rapidly enough. a)Corresponding Author email: [email protected] 1 I. -
Mitigation of Vortex-Induced Vibrations Using Macro
Florida State University Libraries Electronic Theses, Treatises and Dissertations The Graduate School 2012 Mitigation of Vortex-Induced Vibrations in Cables Using Macro-Fiber Composites Gustavo J. Munoz Follow this and additional works at the FSU Digital Library. For more information, please contact [email protected] THE FLORIDA STATE UNIVERSITY FSU-FAMU COLLEGE OF ENGINEERING MITIGATION OF VORTEX-INDUCED VIBRATIONS IN CABLES USING MACRO-FIBER COMPOSITES By GUSTAVO J. MUNOZ A Thesis submitted to the Department of Civil and Environmental Engineering in partial fulfillment of the requirements for the degree of Master of Science Degree Awarded: Spring Semester, 2012 Gustavo J. Munoz defended this thesis on March 30, 2012. The members of the supervisory committee were: Sungmoon Jung Professor Directing Thesis Michelle Rambo-Roddenberry Committee Member Lisa K. Spainhour Committee Member The Graduate School has verified and approved the above-named committee members, and certifies that the [thesis/treatise/dissertation] has been approved in accordance with university requirements ii I dedicate this manuscript to my mother, father and wife. I love you. iii ACKNOWLEDGMENTS This thesis is a combination of efforts in different ways from many special people. To begin, my advisor, Sungmoon Jung has worked tirelessly and constantly in ensuring my complete understanding of the work needed to complete this project. Not only did he guide me through my thesis work, he pushed me to reach further than minimum requirements -- arguing that we should tap into all of our potential. He also taught me and guided me through a very particular way of analytical thought while stimulating me to blossom in my own way of scientific thinking. -
Synoptic Meteorology
Lecture Notes on Synoptic Meteorology For Integrated Meteorological Training Course By Dr. Prakash Khare Scientist E India Meteorological Department Meteorological Training Institute Pashan,Pune-8 186 IMTC SYLLABUS OF SYNOPTIC METEOROLOGY (FOR DIRECT RECRUITED S.A’S OF IMD) Theory (25 Periods) ❖ Scales of weather systems; Network of Observatories; Surface, upper air; special observations (satellite, radar, aircraft etc.); analysis of fields of meteorological elements on synoptic charts; Vertical time / cross sections and their analysis. ❖ Wind and pressure analysis: Isobars on level surface and contours on constant pressure surface. Isotherms, thickness field; examples of geostrophic, gradient and thermal winds: slope of pressure system, streamline and Isotachs analysis. ❖ Western disturbance and its structure and associated weather, Waves in mid-latitude westerlies. ❖ Thunderstorm and severe local storm, synoptic conditions favourable for thunderstorm, concepts of triggering mechanism, conditional instability; Norwesters, dust storm, hail storm. Squall, tornado, microburst/cloudburst, landslide. ❖ Indian summer monsoon; S.W. Monsoon onset: semi permanent systems, Active and break monsoon, Monsoon depressions: MTC; Offshore troughs/vortices. Influence of extra tropical troughs and typhoons in northwest Pacific; withdrawal of S.W. Monsoon, Northeast monsoon, ❖ Tropical Cyclone: Life cycle, vertical and horizontal structure of TC, Its movement and intensification. Weather associated with TC. Easterly wave and its structure and associated weather. ❖ Jet Streams – WMO definition of Jet stream, different jet streams around the globe, Jet streams and weather ❖ Meso-scale meteorology, sea and land breezes, mountain/valley winds, mountain wave. ❖ Short range weather forecasting (Elementary ideas only); persistence, climatology and steering methods, movement and development of synoptic scale systems; Analogue techniques- prediction of individual weather elements, visibility, surface and upper level winds, convective phenomena. -
Distal Radius Fracture
Distal Radius Fracture Osteoporosis, a common condition where bones become brittle, increases the risk of a wrist fracture if you fall. How are distal radius fractures diagnosed? Your provider will take a detailed health history and perform a physical evaluation. X-rays will be taken to confirm a fracture and help determine a treatment plan. Sometimes an MRI or CT scan is needed to get better detail of the fracture or to look for associated What is a distal radius fracture? injuries to soft tissues such as ligaments or Distal radius fracture is the medical term for tendons. a “broken wrist.” To fracture a bone means it is broken. A distal radius fracture occurs What is the treatment for distal when a sudden force causes the radius bone, radius fracture? located on the thumb side of the wrist, to break. The wrist joint includes many bones Treatment depends on the severity of your and joints. The most commonly broken bone fracture. Many factors influence treatment in the wrist is the radius bone. – whether the fracture is displaced or non-displaced, stable or unstable. Other Fractures may be closed or open considerations include age, overall health, (compound). An open fracture means a bone hand dominance, work and leisure activities, fragment has broken through the skin. There prior injuries, arthritis, and any other injuries is a risk of infection with an open fracture. associated with the fracture. Your provider will help determine the best treatment plan What causes a distal radius for your specific injury. fracture? Signs and Symptoms The most common cause of distal radius fracture is a fall onto an outstretched hand, • Swelling and/or bruising at the wrist from either slipping or tripping. -
ECSS 2009 Abstracts by Session
th 5 European Conference on Severe Storms 12 - 16 October 2009 - Landshut - GERMANY ECSS 2009 Abstracts by session ECSS 2009 - 5th European Conference on Severe Storms 12-16 October 2009 - Landshut – GERMANY List of the abstract accepted for presentation at the conference: O – Oral presentation P – Poster presentation Session 08: (Extra-)tropical cyclones: embedded thunderstorms and large-scale wind fields Page Type Abstract Title Author(s) Sensitivities of Mediterranean intense cyclones: analysis O L. Garcies, V. Homar and verification A study of generation of available potential energy in South 247 O A. Vetrov, N. Kalinin cyclones and hazard events over the Ural 249 O Lightning activity in hurricanes C. Price, Y. Yair, M. Asfur O Sting jets in climatological datasets O. Martinez-Alvarado, S. Gray 251 O Cold-season mesoscale convective systems in Germany C. Gatzen, T. Púčik Comparison of two cold-season mesoscale convective 253 P C. Gatzen, T. Púčik, D. Ryva systems Klaus over Basque Country: local characteristics and 255 P S. Gaztelumendi, J. Egaña Euskalmet operational aspects A. Schneidereit, K. Riemann- North-Atlantic extra-tropical cyclone intensities, wind 257 P Campe, R. Blender, K. Fraedrich, fields, and CAPE F. Lunkeit Klaus overview and comparison with other cases affecting 259 P J. Egaña, S. Gaztelumendi Basque country area A numerical study of the windstorm Klaus: role of the sea 261 P surface temperature and domain size N. Tartaglione, R. Caballero 245 246 5th European Conference on Severe Storms 12 - 16 October 2009 - Landshut - GERMANY A STUDY OF GENERATION OF AVAILABLE POTENTIAL ENERGY IN SOUTH CYCLONES AND HAZARD EVENTS OVER THE URAL A.Vetrov1, N. -
THERMODYNAMICS, HEAT TRANSFER, and FLUID FLOW, Module 3 Fluid Flow Blank Fluid Flow TABLE of CONTENTS
Department of Energy Fundamentals Handbook THERMODYNAMICS, HEAT TRANSFER, AND FLUID FLOW, Module 3 Fluid Flow blank Fluid Flow TABLE OF CONTENTS TABLE OF CONTENTS LIST OF FIGURES .................................................. iv LIST OF TABLES ................................................... v REFERENCES ..................................................... vi OBJECTIVES ..................................................... vii CONTINUITY EQUATION ............................................ 1 Introduction .................................................. 1 Properties of Fluids ............................................. 2 Buoyancy .................................................... 2 Compressibility ................................................ 3 Relationship Between Depth and Pressure ............................. 3 Pascal’s Law .................................................. 7 Control Volume ............................................... 8 Volumetric Flow Rate ........................................... 9 Mass Flow Rate ............................................... 9 Conservation of Mass ........................................... 10 Steady-State Flow ............................................. 10 Continuity Equation ............................................ 11 Summary ................................................... 16 LAMINAR AND TURBULENT FLOW ................................... 17 Flow Regimes ................................................ 17 Laminar Flow ............................................... -
POTENTIAL FLOW: in Which the Vorticity Is Zero
Chapter 1 Potential flow: 1.1 General formulation Inviscid and irrotational flows in the limit of high Reynolds number are referred to as ‘potential’ or ‘ideal’ flows. The term ‘inviscid’ refers to flows where viscous forces are small compared to inertial forces, so that the fluid viscosity can be neglected in comparison to fluid inertia. ‘Potential’ or ‘ideal’ flows are a class of inviscid flows in which the vorticity ω, which is the curl of the velocity vector, is zero, i. e. ∂uk ωi = ǫijk = 0 (1.1) ∂xj Since the curl of the velocity is zero, the velocity can be expressed as the gradient of a potential φ, ∂φ ui = (1.2) ∂xi and hence the name ‘potential flow’. Using equation 1.2 for the velocity field, the Navier-Stokes mass and mo- mentum equations can be written in terms of the velocity potential. The mass conservation equation, expressed in terms of the velocity potential, is, 2 ∂ui ∂ φ = 2 = 0 (1.3) ∂xi ∂xi Thus, the mass conservation equation simply states that the velocity potential satisfies the Laplace equation, 2φ = 0. Therefore, for potential flow we can use all the techiques developed∇ for solving the Laplace equation earlier. The momentum conservation equation an inviscid flow is, ∂ui ∂ui 1 ∂p fi + uj = + (1.4) ∂t ∂xj −ρ ∂xi ρ where fi is the body force per unit volume acting on the fluid. The second term on the right side of the above equation can be simplified for an irrotational flow 1 2 CHAPTER 1. POTENTIAL FLOW: in which the vorticity is zero.