In-class problem For maximum and minimum stresses of 600 and 200 mega-pascals (MPa) oriented as a vertical vector and a horizontal, E-W striking vector.

Slides:



Advertisements
Similar presentations
Stress in any direction
Advertisements

Mohr Circle for stress In 2D space (e.g., on the s1s2 , s1s3, or s2s3 plane), the normal stress (sn) and the shear stress (ss), could be given by equations.
Strain II.
Chapter 3 Rock Mechanics Stress
Geology Resolving stresses on a plane. Outline Resolving stress on a plane Determining maximum shear stress Class problem.
Geology 3120 Powerpoint notes available online at:
PLANE STRESS TRANSFORMATION
Principle and Maximum Shearing Stresses ( )
The stresses that cause deformation
Mohr's Circle - Application
The last of the CIRCULAR GRAPHS which will HAUNT YOU ALL QUARTER January 13, 2005 [Many thanks to H. Bob]
Announcements Next week lab: 1-3 PM Mon. and Tues. with Andrew McCarthy. Please start on lab before class and come prepared with specific questions Cottonwood.
Joints and Shear Fractures
Stress Transformation
Checking Out Stress States With Mohr’s Circle
The Mechanics of the crust
Mechanics of Materials(ME-294)
folded and disturbed layers
APPLICATIONS/ MOHR’S CIRCLE
Borehole Stress Orientation  MIN  MAX Top View Drilling Induced Fracture Borehole Breakout Courtesy of Steve Hansen, Schlumberger.
Coulomb Stress Changes and the Triggering of Earthquakes
This is the trace of the strain tensor. In general the trace of the strain tensor gives area change in 2-D and volume change in 3-D The principal axes.
Problem For the 5 x 3 x -in. angle cross
Chapter 3 Force and Stress. In geology, the force and stress have very specific meaning. Force (F): the mass times acceleration (ma) (Newton’s second.
CHAPTER OBJECTIVES To show how to transform the stress components that are associated with a particular coordinate system into components associated with.
Geology Failure Models
The stresses that cause deformation
Outline Force, vectors Units Normal, shear components Pressure
Triaxial State of Stress at any Critical Point in a Loaded Body
Transformations of Stress and Strain
Brittle Deformation Remember that  is the angle between  3 and a plane.
Failure I. Measuring the Strength of Rocks A cored, fresh cylinder of rock (with no surface irregularities) is axially compressed in a triaxial rig.
1 INTRODUCTION The state of stress on any plane in a strained body is said to be ‘Compound Stress’, if, both Normal and Shear stresses are acting on.
1 Structural Geology Force and Stress - Mohr Diagrams, Mean and Deviatoric Stress, and the Stress Tensor Lecture 6 – Spring 2016.
MOHR'S CIRCLE The formulas developed in the preceding article may be used for any case of plane stress. A visual interpretation of them, devised by the.
Mohr-Coulomb failure Goal: To understand relationship between stress, brittle failure, and frictional faulting and to use this relationship to predict.
CTC / MTC 222 Strength of Materials
CHAPTER OBJECTIVES Derive equations for transforming stress components between coordinate systems of different orientation Use derived equations to.
FOCAL PLANE MECHANISM Dr. N. VENKATANATHAN.
Principal Stresses and Strain and Theories of Failure
Mohr’s Circles GLE/CEE 330 Lecture Notes Soil Mechanics
Presentation on Terminology and different types of Faults
EAG 345 – GEOTECHNICAL ANALYSIS
1. PLANE–STRESS TRANSFORMATION
A graphical method of constructing the shear and normal stress tractions on any plane given two principal stresses. This only works in 2-D. Equations.
LEQ: What are the categories and types of faults, and what type of stress produce each? Key Terms: displacement, strike slip fault, dip slip fault,
Mohr Circle In 2D space (e.g., on the s1s2 , s1s3, or s2s3 plane), the normal stress (sn) and the shear stress (ss), could be given by equations (1) and.
Stress in any direction
Folding and Faulting Chapter 4, Sec. 4.
Transformations of Stress and Strain
STRUCTURAL GEOLOGY LAB. STEREOGRAPHIC PROJECTION Dr. Masdouq Al-Taj
Transformations of Stress and Strain
Let s be the 3x3 stress matrix and let n be a 3x1 unit vector
1. The strike of the plane represented by the great circle trace on the equal area plot at left is: A – S55E B – N25W C – 305 D – 355.
GY403 Structural Geology Laboratory
CHAPTER OBJECTIVES Derive equations for transforming stress components between coordinate systems of different orientation Use derived equations to.
Lithosphere-Earthquakes Unit
Differentiation with Trig – Outcomes
Chapter 3 Force and Stress
Example 7.01 SOLUTION: Find the element orientation for the principal stresses from Determine the principal stresses from Fig For the state of plane.
BI-AXIAL STRESS AND MSS THEORY
Folding and Faulting Chapter 4, Sec. 4.
The Mohr Stress Diagram
Aim: What other details can be discussed about vectors?
Review from LAB #3.
The Traction Vector and Stress Tensor
Mechanics of Materials Engr Lecture 18 - Principal Stresses and Maximum Shear Stress Totally False.
Mechanics of Materials Engr Lecture 20 More Mohr’s Circles
Compound Normal & Shear Stresses
Copyright ©2014 Pearson Education, All Rights Reserved
Presentation transcript:

In-class problem For maximum and minimum stresses of 600 and 200 mega-pascals (MPa) oriented as a vertical vector and a horizontal, E-W striking vector (respectively), determine the normal and shear stresses on a plane oriented North-South, 45 degrees East. It helps to first draw a block diagram. So max stress is oriented vertically and equal to 600 MPA Min stress is horizontal, oriented east-west and = 200 MPa

For max and min stresses of 600, 200 (MPa) oriented as a vertical vector and a horizontal, E-W striking vector (respectively), determine the normal and shear stresses on a plane oriented North-South, 45E. It helps to first draw a block diagram. So max stress is oriented vertically and equal to 600 MPA Min stress is horiz., east-west = 200 Mpa Key: Normal stress = mean stress: 400 MPa; Shear stress 200 MPa

sn = (600 + 200) - (600 - 200) cos 90 2 = 400 ss = (600 - 200) sin 90 For the minimum and maximum principle stresses of 600 and 200 megapascals (MPa) oriented as a vertical vector and a horizontal, E-W striking vector (respectively), determine the normal and shear stresses on a plane oriented North-South, 45 degrees East sn = (600 + 200) - (600 - 200) cos 90 2 = 400 ss = (600 - 200) sin 90 2 = 200

Mean Stress Differential Stress For the stress state in the previous problem, determine the differential stress and mean stress. Start by plotting the solution for normal and shear stresses on the Mohr Stress Diagram. Mean Stress Differential Stress

Determine whether decreasing the dip of the fault will decrease or increase the shear stress acting on it.

Determine whether decreasing the dip of the fault will decrease or increase the shear stress acting on it. It will decrease the shear stress since decreasing the dip of the fault would decrease theta, the angle between the largest principal stress and the normal to the plane the stress is acting on, (the plane is rotating closer to 90 deg. or normal to the maximum stress)

In-class problem 2 Discuss how a change in differential stress might affect whether a rock might be more or less likely to break. It may help by arbitrarily varying the stresses and looking at how they plot on the circle, or by imagining stress on a cube. If the differential stress is decreased (making the stresses closer in value, so the mohr circle shrinks), it would make it less likely to intersect a failure envelope and break. If the differential stress was increased, there would be a bigger difference between the two stresses, the Mohr circle would increase in diameter and more likely to intersect the failure envelope making it more likely to break.

Failure envelope

In-class problem 2 Now discuss whether increasing the mean stress would cause a rock to break more readily. Would this be more or less likely with increasing depth in the crust? Increasing the mean stress would move the circle to the right (increasing normal) stress, resulting in the rock being less likely to break. Given the shape of the envelope, increasing the mean stress will never bring the rock closer to failure (assuming differential stress is not increased as well). Mean stress increases with depth in the crust (and we are assuming differential stress does not increase as well). Intuitively, the difference in stress would have to increase for a rock to break under a higher mean stress.

Draw the stress state where the minimum and maximum stresses are both equal to 600 MPa. The principle stresses are thus equal to the mean stress and differential stress is zero.