Shear stress

  1. 4.4: Turbulent Shear Stress
  2. Mechanics of Materials: Stress » Mechanics of Slender Structures
  3. Beam Stress & Deflection
  4. Shear Stress Equations and Applications
  5. Difference between shear flow and shear stress


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4.4: Turbulent Shear Stress

[ "article:topic", "showtoc:no", "license:ccbyncsa", "authorname:jsouthard", "turbulent diffusion", "turbulence closure problem", "Reynolds stress", "turbulent shear stress", "program:mitocw", "licenseversion:40", "source@https://ocw.mit.edu/courses/12-090-introduction-to-fluid-motions-sediment-transport-and-current-generated-sedimentary-structures-fall-2006" ] \( \newcommand\): Distribution of total shear stress, turbulent shear stress, and viscous shear stress in a steady and uniform open-channel flow. Because the turbulent shear stress is so much larger than the viscous shear stress except very near the boundary, differences in time- average velocity from layer to layer in turbulent flow are much more effectively ironed out over most of the flow depth than in laminar flow. This accounts for the much gentler velocity gradient \(du/dy\) over most of the flow depth in turbulent flow than in laminar flow; go back and look at Figure near the boundary to the zero velocity at the boundary (remember the no-slip condition) is compressed into a thin layer immediately adjacent to the boundary. Turbulence Closure Problem When the Navier–Stokes equations are written for turbulent flow, and then instantaneous velocities are converted to their mean and fluctuating components, as was done in turbulence closure problem. It is often said to be one of the great unsolved problems in all of physics. (That is a very strong statement.) Various strategies have been devised to circumvent the cl...

Mechanics of Materials: Stress » Mechanics of Slender Structures

Welcome to the Mechanics of Materials. This course builds directly on the fundamentals we learned in Statics – calculating the static equilibrium of various structures under various loads. In statics, we consider the external forces acting on rigid bodies . In reality, all bodies are deformable and those external forces generate internal stresses . Well then, what's a stress? Stress is the measure of an external forceacting over the cross sectional area of an object. Stress has units of force per area: N/m 2(SI) or lb/in 2 (US). The SI units are commonly referred to as Pascals, abbreviated Pa. Since the 1 Pa is inconveniently small compared to the stresses most structures experience, we'll often encounter 10 3 Pa = 1 kPa (kilo Pascal), 10 6 Pa = a MPa (mega Pascal), or 10 9 Pa = GPa (giga Pascal). Okay, how did we arrive at this equation. There are a lot of assumptions behind the scenes. Throughout this course, we will assume that all materials are uniformly at every point of its cross section. The normal stress at a point on a cross section is defined as (with similar equations in the xand ydirections). : Let's look at another example. Consider a bolt that connects two rectangular plates, and a tensile force perpendicular to the bolt. From a free body diagram, we see that the externally applied force exerts a force parallel to the circular cross section of the bolt. This external force results in a shear stress within the bolt. Since the areas of the cube are by definitio...

Beam Stress & Deflection

NOTE: This page relies on JavaScript to format equations for proper display. Please enable JavaScript. Many structures can be approximated as a straight beam or as a collection of straight beams. For this reason, the analysis of stresses and deflections in a beam is an important and useful topic. This section covers shear force and bending moment in beams, shear and moment diagrams, stresses in beams, and a table of common beam deflection formulas. Contents • Constraints and Boundary Conditions For a beam to remain in static equilibrium when external loads are applied to it, the beam must be constrained. Constraints are defined at single points along the beam, and the boundary condition at that point determines the nature of the constraint. The boundary condition indicates whether the beam is fixed (restrained from motion) or free to move in each direction. For a 2-dimensional beam, the directions of interest are the x-direction (axial direction), y-direction (transverse direction), and rotation. For a constraint to exist at a point, the boundary condition must indicate that at least one direction is fixed at that point. Common boundary conditions are shown in the table below. For each boundary condition, the table indicates whether the beam is fixed or free in each direction at the point where the boundary condition is defined. Boundary Condition Direction Axial (X) Transverse (Y) Rotation Free Free Free Free Fixed Fixed Fixed Fixed Pinned Fixed Fixed Free Guided along X ...

Shear Stress Equations and Applications

Shear Stress Equations and Applications Mechanics of Materials Shear Stress Equations and Applications General shear stress: The formula to calculate average shear stress is where τ = the shear stress; F = the force applied; A = the cross-sectional area of material with area perpendicular to the applied force vector; Beam shear : Beam shear is defined as the internal shear stress of a beam caused by the shear force applied to the beam. where V = total shear force at the location in question; Q = statical moment of area; t = thickness in the material perpendicular to the shear; I = Moment of Inertia of the entire cross sectional area. This formula is also known as the Jourawski formula. Semi-monocoque shear: Shear stresses within a semi-monocoque structure may be calculated by idealizing the cross-section of the structure into a set of stringers (carrying only axial loads) and webs (carrying only shear flows). Dividing the shear flow by the thickness of a given portion of the semi-monocoque structure yields the shear stress. Thus, the maximum shear stress will occur either in the web of maximum shear flow or minimum thickness.Also constructions in soil can fail due to shear; e.g., the weight of an earth-filled dam or dike may cause the subsoil to collapse, like a small landslide. Impact shear. The maximum shear stress created in a solid round bar subject to impact is given as the equation: "Jourawski formula" 2 (U G / V ) (1/2) where U = change in kinetic energy; G = shear ...

Difference between shear flow and shear stress

I have been given the following problem in one of my courses. To say that I'm struggling in the course would be an understatement... I'm just wondering what the difference between shear flow and stress is, wouldn't they be the same in each secion? Consider the thin-walled section shown below. The section is fixed on one end, and an axial moment (T=12 kNm) is applied to the free end. The section is 6.9 m long. Do the following: • Determine the shear flow in each section. • What is the maximum shear stress in the section. • Determine the angle of rotation of the free end (G = 26 GPa). Shear flow is a quantity which is used to conveniently solve (usually) torsional problems of thin walled beams (it has other applications also). The concept behind it is, that the stress distribution in a wall of a thin-walled beam can be considered constant (while in a circular cross section is proportional to the distance from the shear center. The relationship between shear flow and shear stress is : $$q= \tau \cdot t$$ where: • $q$ is the shear flow • $\tau$ is the shear stress • $t$ thickness of the thin walled beam. In thin walled sections under torsional moment T, the shear flow $q$ can be calculated by: $$q= \frac$ With just those three concepts, a system of equations can be derived that can be solved (you can easily find examples on the net - if you show your effort, I would gladly expand this section). This write-up repeats the things been taught in the class. Shear flow $f = \tau t$ ...