LAB Exercise #4 - Answers The Traction Vector and Stress Tensor. Introduction. Format of lab. Preparation reading

Similar documents
GG303 Lecture 17 10/25/09 1 MOHR CIRCLE FOR TRACTIONS

GG303 Lab 10 10/26/09 1. Stresses

σn -2α σ1= Maximum Principal Stress -2Θ

(Refer Slide Time: 04:21 min)

CHAPTER ONE FUNCTIONS AND GRAPHS. In everyday life, many quantities depend on one or more changing variables eg:

CHAPTER 4 Stress Transformation

Brittle Deformation. Earth Structure (2 nd Edition), 2004 W.W. Norton & Co, New York Slide show by Ben van der Pluijm

The hitch in all of this is figuring out the two principal angles and which principal stress goes with which principal angle.

Exercise: concepts from chapter 6

The Mohr Stress Diagram. Edvard Munch as a young geologist!

Lecture Notes 5

Linear Motion with Constant Acceleration

GEL 3300 Lab #2: Measuring Strain

Math 121 (Lesieutre); 9.1: Polar coordinates; November 22, 2017

1 Newton s 2nd and 3rd Laws

Force and Stress. Processes in Structural Geology & Tectonics. Ben van der Pluijm. WW Norton+Authors, unless noted otherwise 1/9/ :35 PM

EAS MIDTERM EXAM

EOSC 110 Reading Week Activity, February Visible Geology: Building structural geology skills by exploring 3D models online

Electric Fields and Potentials

Use a highlighter to mark the most important parts, or the parts. you want to remember in the background information.

In other words, we are interested in what is happening to the y values as we get really large x values and as we get really small x values.

9. Stress Transformation

5-Sep-15 PHYS101-2 GRAPHING

Computer simulation of radioactive decay

Electric Fields and Potential

Section 6.2 Notes Page Trigonometric Functions; Unit Circle Approach

Electric Fields and Equipotentials

Structural Geology, GEOL 330 Spring 2012

Here is a sample problem that shows you how to use two different methods to add twodimensional

EXPERIMENT 7: ANGULAR KINEMATICS AND TORQUE (V_3)

Worksheet for Exploration 6.1: An Operational Definition of Work

PHY222 Lab 2 - Electric Fields Mapping the Potential Curves and Field Lines of an Electric Dipole

Physics Lab 202P-9. Magnetic Fields & Electric Current NAME: LAB PARTNERS:

Lab 8 Impulse and Momentum

Tectonics. Lecture 12 Earthquake Faulting GNH7/GG09/GEOL4002 EARTHQUAKE SEISMOLOGY AND EARTHQUAKE HAZARD

CHAPER THREE ANALYSIS OF PLANE STRESS AND STRAIN

Exercise: concepts from chapter 8

! EN! EU! NE! EE.! ij! NN! NU! UE! UN! UU

Experiment 15: Atomic Orbitals, Bond Length, and Molecular Orbitals

ACCESS TO SCIENCE, ENGINEERING AND AGRICULTURE: MATHEMATICS 1 MATH00030 SEMESTER / Functions

Intensity of Light and Heat. The second reason that scientists prefer the word intensity is Well, see for yourself.

Lab #10 Atomic Radius Rubric o Missing 1 out of 4 o Missing 2 out of 4 o Missing 3 out of 4

PHY221 Lab 2 - Experiencing Acceleration: Motion with constant acceleration; Logger Pro fits to displacement-time graphs

Example 2.1. Draw the points with polar coordinates: (i) (3, π) (ii) (2, π/4) (iii) (6, 2π/4) We illustrate all on the following graph:

OBJECTIVE: To understand the relation between electric fields and electric potential, and how conducting objects can influence electric fields.

LAB 2 - ONE DIMENSIONAL MOTION

Since x + we get x² + 2x = 4, or simplifying it, x² = 4. Therefore, x² + = 4 2 = 2. Ans. (C)

Harmonic Motion. Mass on a Spring. Physics 231: General Physics I Lab 6 Mar. 11, Goals:

Math Section 4.3 Unit Circle Trigonometry

Chapter 9: Roots and Irrational Numbers

Using Microsoft Excel

Chapter 9 Ingredients of Multivariable Change: Models, Graphs, Rates

Lab Partner(s) TA Initials (on completion) EXPERIMENT 7: ANGULAR KINEMATICS AND TORQUE

LABORATORY 1: KINEMATICS written by Melissa J. Wafer '95 June 1993

An angle in the Cartesian plane is in standard position if its vertex lies at the origin and its initial arm lies on the positive x-axis.

Physics 6A Lab Experiment 6

Determining strain graphically

PHYSICS 220 LAB #3: STATIC EQUILIBRIUM FORCES

Notes on multivariable calculus

Mathematics Trigonometry: Unit Circle

The choice of origin, axes, and length is completely arbitrary.

Partner s Name: EXPERIMENT MOTION PLOTS & FREE FALL ACCELERATION

DuVal High School Summer Review Packet AP Calculus

Lab 1: Dynamic Simulation Using Simulink and Matlab

Kinematics Lab. 1 Introduction. 2 Equipment. 3 Procedures

Introduction to Computer Tools and Uncertainties

University of Maryland Department of Physics. Spring 2009 Final Exam 20. May (175 points) Post grades on web? (Initial, please) Yes No

Experiment 3 Forces are Vectors

Assignment 1: Molecular Mechanics (PART 1 25 points)

Lesson 6-1: Relations and Functions

Exercise solutions: concepts from chapter 6

Physics E-1ax, Fall 2014 Experiment 3. Experiment 3: Force. 2. Find your center of mass by balancing yourself on two force plates.

Free-Body Diagrams: Introduction

LAB 3: WORK AND ENERGY

PHYSICS 220 LAB #5: WORK AND ENERGY

Name: Date: Partners: LAB 2: ACCELERATED MOTION

Math Lab 10: Differential Equations and Direction Fields Complete before class Wed. Feb. 28; Due noon Thu. Mar. 1 in class

Please read this introductory material carefully; it covers topics you might not yet have seen in class.

Lab 7: STRUCTURAL GEOLOGY FOLDS AND FAULTS

2.1 Definition. Let n be a positive integer. An n-dimensional vector is an ordered list of n real numbers.

You will return this handout to the instructor at the end of the lab period. Experimental verification of Ampere s Law.

Experiment 0 ~ Introduction to Statistics and Excel Tutorial. Introduction to Statistics, Error and Measurement

North Carolina State University

Quiz No. 1: Tuesday Jan. 31. Assignment No. 2, due Thursday Feb 2: Problems 8.4, 8.13, 3.10, 3.28 Conceptual questions: 8.1, 3.6, 3.12, 3.

Chapter 3 Homework Packet. Conceptual Questions

EAS FINAL EXAM

18-Dec-12 PHYS Simple Pendulum. To investigate the fundamental physical properties of a simple pendulum.

Dynamic analysis. 1. Force and stress

Figure 2.1 The Inclined Plane

Lab 6 Forces Part 2. Physics 225 Lab

Part I. PRELAB SECTION To be completed before labs starts:

Is there life outside of Earth? Activity 2: Moving Stars and Their Planets

PHY 221 Lab 2. Acceleration and Uniform Motion

Lab 8 Impulse and Momentum

Motion II. Goals and Introduction

Triangles and Vectors

MATH 32 FALL 2012 FINAL EXAM - PRACTICE EXAM SOLUTIONS

Lab 3 Acceleration. What You Need To Know: Physics 211 Lab

Lab 7: EC-5, Faraday Effect Lab Worksheet

Vectors Part 1: Two Dimensions

Transcription:

LAB Exercise #4 - Answers The Traction Vector and Stress Tensor Due: Thursday, 26 February 2009 (Special Thanks to D.D. Pollard who pioneered this exercise in 1991) Introduction Stress concentrations in the earth lead to the development of structures such as faults, folds, and joints. This problem set is designed to be a tutorial for stress analysis at a point in a rock mass or throughout a region of homogeneous stress. Of course the state of stress can, and generally does vary throughout a deforming rock mass, but these spatial and temporal variations will not be emphasized. Here we will deal only with the stresses acting in two dimensions, that is, in an imaginary plane cutting through a rock mass. The principles you will learn are easily extended to three dimensions. Format of lab We will lead you through the problems step-by-step, and provide many ways for you to check your work. The objective is not just to get the correct answers, but to really understand stress analysis. Show all your work, including visual aids such as figures and printouts from any computer programs you use, so you can go back to your work at any point and understand what you did. Label all figures and diagrams clearly and profusely. Get help if something is not clear to you. For this exercise, you will be doing work both by hand and with Excel. Work through the problems in the given order to minimize confusion. When you are done, you should understand: 1) The difference between the stress tensor at a point and the traction vector acting on some given plane through that point (see Box 7.3, pg. 184 in T&M for a good explanation of the difference between a vector and a tensor); 2) How to calculate the principal stress magnitudes and stress trajectories (are these the principal axes?) at a point; and 3) What the Mohr circle represents and how to plot a Mohr circle given some stress state. Preparation reading Please refer back to Chapter 7 in Twiss and Moores and, if you would like, read Marshak and Mitra pp. 193-199, before you start the problem set. The exercises look very long, but they should go quickly because of all the hints. 19-Feb-2009 Page 1 of 15

Part One (30 pts) 1a (5 pt) Given that the two principal stresses acting in a plane at a point are σ 1 = 60 MPa and σ3= 20 MPa, draw a Mohr circle for this stress state. Use graph paper and be as accurate as you can. For this set of exercises compressive stresses are positive and tensile stresses are negative. Therefore, σ 1 is the maximum compressive stress (or minimum tensile stress if it happens that all normal stresses are tensile and therefore negative), and σ 3 is the minimum compressive stress (or maximum tensile stress). Recall that σ n and σ s are the normal and shear components of the traction vector and plot your Mohr circle with the axes for σ n and σ s arranged as follows: +σ s tensile compressive +σ n 19-Feb-2009 Page 2 of 15

-2 if no label for σ n and σ s -2 if no scale bar or labeling on axis 1b (5 pt) Show where the traction vector components acting on a plane with 2θ = 120 plot on your Mohr circle. Also show where the components acting on a plane with 2θ = 240 plot on your Mohr circle. Remember that the angle 2θ is measured counterclockwise from the positive σ n axis. 1c (6 pts) Assume that this two dimensional stress state describes the traction vectors acting in a horizontal plane in a certain region of the earth's lithosphere and that the two planes given in (1b) are potential fault planes with vertical dips in this same region. Draw a map (3D block diagram would be nice) showing the faults and the principle stresses (assume that σ 1 acts in a north-south direction). Also show the sense of relative motion that the faults would have if they moved (use right-lateral or leftlateral pairs of arrows). The sign conventions shown in problem (2c) may be helpful! On your map be sure to indicate the strike and dip for each fault. Remember that in physical space (your map), θ is measured counterclockwise from σ 1 to the normal for the plane of interest. In stress space, 2θ is measured counterclockwise from (σ 1, 0) on the Mohr circle to the point on the circle that represents the magnitudes of the pair (σ n, σ s ) acting on a given plane. The following sketch illustrates these relationships. -1 if no orientation -1 if gave vertical for dip instead of 90-1 if reversed fault plane strikes -1 for each wrong sense of slip -3 if no strike and dip -1 if didn t scale arrows to magnitude of stresses +σ s (σ n, σ s ) on P 2θ +σ n normal to P P θ σ 1 19-Feb-2009 Page 3 of 15

1d (3 pts) map) What is the angle between σ 1 and each of the fault planes? (Use your For 2θ = 120, fault is 30 E of σ1 For 2θ = 240, fault is 30 W of σ1-1 if didn t specify angle on map or give direction from σ 1 1e (5 pts) Use your Mohr circle to estimate (σ n, σ s ) for each fault plane. Pay attention to sign conventions. σ n = 30; σ s = ±17.3-1 if no negative for 240 shear traction 1f (6 pts) Confirm your results in part (1e) with the following equations for stress resolution: # σ 1 + σ ˆ 3 % # σ ˆ 1 σ ˆ 3 σ n = ˆ $ 2 σ s = # σ ˆ 1 ˆ $ 2 σ 3 & + $ 2 % & sin2θ 2 % & cos2θ 2 19-Feb-2009 Page 4 of 15

σ n = 40 + 20 cos 120 = 40-10 = 30.0 MPa; σ s = 20 sin 120 = 17.3 MPa; σ n = 40 + 20 cos 240 = 40-10 = 30.0 MPa; σ s = 20 sin 240 = -17.3 MPa 19-Feb-2009 Page 5 of 15

Part Two (34 pts) Answer the questions in part 2 of this exercise based on the following three components of the two dimensional stress tensor: σ 11 = 50 MPa σ 13 = σ 31 = -40 Mpa σ 33 = 20 MPa Recall that the first subscript indicates the (normal to the) plane on which the stress acts and the second subscript indicates the direction in which the stress acts. 2a (4 pts) Sketch a picture of this stress state (write down the 2D tensor matrix as well). Draw a square "element" and add arrows for σ 11, σ 33, and σ 13. Make the lengths of your arrows scale (roughly) with the stress magnitudes. Use the following sign conventions: Positive normal stresses are compressive; negative normal stresses are tensile. For example, the stress state σ 11 = +60 MPa ; σ 33 = -30 MPa would be drawn as follows: X 3 X 1 A positive shear stress state is drawn (sign is determined by the direction of the traction acting on the NEGATIVE coordinate face of the square does that make sense?): + X 3 -direction + X 1 -direction 19-Feb-2009 Page 6 of 15

whereas a negative shear stress state is drawn: Negative coordinate faces of square [50-40] [-40 20] -1 if tensor is wrong -1 if arrows aren t scaled -1 for each set of arrows that pointed in wrong direction 2b (3pts) Now add arrows for σ 1 and σ 3 to your sketch in part (2a). You can tell approximately where the principal stresses are located just from looking at your sketch because σ 3 "comes out of the corner that the shear stresses point to." Remember that σ 1 and σ 3 act in directions that are perpendicular to each other. Your sketch gives you the approximate quadrants for σ 1 and σ 3, the exact angles depend on the magnitudes of all three tensor components. You will calculate the exact angles in part (2e). -1 if oriented in wrong direction 2c (5 pts) Construct a Mohr circle diagram for this stress state. Use graph paper and label the points that you use to draw the circle. HINT: To construct the circle, plot (σ n, σ s ) for a plane parallel to 19-Feb-2009 Page 7 of 15

the x-axis and for a plane parallel to the y-axis. These two points will plot on opposite ends of a diameter passing through the center (a point on the σ n axis) of the Mohr circle. After plotting these points, just draw a circle through the two points with the appropriate center and radius. (A compass will come in handy.) -1 if didn t label points -1 if wrong 2 points -1 if axis isn t labeled -1 if no scale 2d (3 pts) Based on your Mohr circle, what are the magnitudes of σ 1 and σ 3 (approximately)? σ1 = 77.7 = 0.5 (50 + 20) + [0.25(50-20) 2 + (-40) 2 ] 0.5 19-Feb-2009 Page 8 of 15

σ2 = -7.7 = 0.5(50 + 20) - [0.25(50-20) 2 = (-40) 2 ] 0.5 The sign conventions for the components of the traction vector acting on a plane, P, are as follows: Note that the tractions are positive when they act in the negative coordinate directions. The coordinates (n, s) are always drawn such that n is positive outward and s is directed to the right when facing in a positive n direction. Look at your sketch in part (2a) to determine the appropriate signs for σ s on planes parallel to the X 1 and X 3 axes. Note the possible difference between the signs of the shear traction vector component and the shear stress tensor component. Clearly, one must be careful to state which component you are talking about. -1 for each wrong sign 2d (6 pts) Compute the principal stress magnitudes using: σ 1 = 1 2 (σ 11 +σ 33 ) + [ 1 4 (σ 11 σ 33 ) 2 +(σ 13 ) 2 ] 1 2 [ ] 1 2 σ 3 = 1 2 (σ 11 +σ 33 ) 1 4 (σ 11 σ 33 ) 2 + (σ 13 ) 2 Show your work. Check to be sure that your results are consistent with your Mohr circle in (2c). 2e (6 pts) Compute the principal stress directions using: Remember that α 1 and α 3 are the angles between the X 1-axis and the directions in which σ 1 and σ 3 act, respectively. 1 & 1 2σ 13 α = tan $ 1 2 % σ σ 11 α = α + 90 3 1 They are measured with a positive sense being counterclockwise. Do not confuse the angle α with the angle θ. See the picture below and refer to the picture on page 3 for clarification of this point. 33 #! " 19-Feb-2009 Page 9 of 15

X 3 σ σ 1 3 α 1 X 1 Be sure that your angles agree with your picture in part (2a); your sketch will help you decide which quadrant is correct for σ 1 and σ 3. The following hint explains how to use the equations to get the correct angles. HINT: Most hand calculators will return an angle between -90 and +90 for the arctan function. Therefore, you may have to add some multiple of 90 to achieve the desired result. You must consider the sign of the numerator and the sign of the denominator in the fraction that is the argument for the arctan function as indicated below: Case 1: if σ 13 is positive and (σ 11 - σ 33 ) is positive, then the arctan is between 0 and 90. Case 2: if σ 13 is positive and (σ 11 - σ 33 ) is negative, then the arctan is between 90 and 180. Case 3: if σ 13 is negative and (σ 11 - σ 33 ) is negative, then the arctan is between 180 and 270. Case 4: if σ 13 is negative and (σ 11 - σ 33 ) is positive, then the arctan is between 270 and 360. This procedure should remind you of the "unit circle" and the definition of the tangent function from your high school math class. You would be surprised to know how many graduate students and professors botch up this calculation! Also, remember the factor of one-half in the formula; once you find the correct arctan, you must divide by two to solve for α 1. Of course with modern computers all of these calculations can be done for you in microseconds, but you must understand the underlying principles and use the correct function!.5 * atan(2*-40)/(50-20).5 * atan(-2.66) 19-Feb-2009 Page 10 of 15

.5*-69.44 Report angle between 270 and 360:.5 * 290.56 α 1 = 145.3 α 3 = 145.28+90 = 235.3-2 if thought α 1 had to be between 270-360 -3 if didn t attempt to put atan part between 270-360 -1 if used wrong α 1 for α 3 calculation 2f Download the excel files from the web site. On a PC, click the right mouse button and choose Save Link to Disk or something similar (varies by browser). On a Mac, click and hold the mouse button until a menu pops up. Choose Save Link to Disk. Double click on the stress folder to open it and shift click on the stress.w, Mohr.c, and Sigma.c files. Open Microsoft Excel. File Open You may need to select All Readable Files from the File Type drop-down menu in order to be able to see the three files listed above (again, the words vary from version to version). Open up all three of the files. The input parameters for this application are the stresses σ 11, σ 33, and σ 13 ; these stresses completely determine the stress state in two dimensions. You can change each of the values for these three input stresses, pressing the "enter" key after each input. Excel then computes the principal stress magnitudes and directions. Excel also draws a Mohr circle in the chart "Mohr.c". CAUTION -- You may have to "grab" the Mohr circle chart by the lower right corner and stretch the plot into a circular shape because the scale changes every time you change the input parameters. Change the input parameters to be σ 11 = 50 MPa, σ 13 = -40 MPa, and σ 33 = 20 MPa. Check to see that Excel's computed principal stress magnitudes, principal stress directions, and Mohr circle agree with your results in parts (a) - (d). To see the Mohr circle chart, pull down the "window" menu and choose "Mohr.c" 2g (7 pts) Assume that this stress state represents the stress tensor components acting in a horizontal plane in some region of the earth and that the X 3-axis is north. If vertical joints (opening mode fractures) formed in this region, what would their strike and dip be? Draw a map showing some of the joints, the principal stresses, and a north arrow. HINT: Assume that the joint faces form perpendicular to the least compressive stress acting in the horizontal plane. Be sure that you understand the difference between the stress tensor at a point and the traction vector acting on some given plane. The Mohr circle is a way of plotting the normal and shear components for traction vectors associated with all possible planes 19-Feb-2009 Page 11 of 15

through a point. In part 3 of this exercise we will study a different way to represent the stress state. 124, 90 dip -2 if wrong strike -2 if not principal stresses -1 if no north orientation Part Three (21 pts) Another representation of the state of stress at a point is found by plotting θ vs. σ n and θ vs. σ s. Pull down the "File" menu and choose the chart "Sigma.c". Study the plots. Now go back to the "stress.w" worksheet and change the input parameters to be σ 11 = 60 MPa, σ 13 = 0 MPa, and σ 33 = 20 MPa. Pull down the window menu and choose "Sigma.c" again. Notice how the plots have changed. Use the chart "Sigma.c" to answer the following questions: 19-Feb-2009 Page 12 of 15

3a (3 pt) What is the magnitude of the shear stress on planes that carry the maximum and minimum normal stresses? zero 3b (3 pt) What is special about the magnitude of the normal stress on planes that carry the maximum shear stress? It is the mean normal stress -2 if said ½ max normal stress -3 if said principal stress 3c (5pts) Get a printout of the chart and show that the planes with maximum shear stress are 45 away from planes of maximum normal stress. Show (with a sketch) how this relationship can also be seen on the Mohr circle. 2θ = 90 on the Mohr circle so θ = 45 3d (5 pts) Show on your plot of σ n that the principal stresses act on planes that are 90 apart and show the value of the mean normal stress. σ m = 40 MPa 3e (5 pts) What are two different ways to completely specify the state of two dimensional stress at a point? What is the minimum amount of information (how many numbers do you need)? 2 principal stresses and α 1 or 3 components of stress tensor Part Four (15 pts) For part 4 of this exercise you are given the following components of the stress tensor: σ 11 = 30 MPa = σ3 19-Feb-2009 Page 13 of 15

σ 13 = 0 MPa σ 33 = 40 MPa = σ1 Suppose that this is the state of stress on a vertical cross-section at some depth in the earth with X 3 pointing upward. 4a (5 pts) Use Excel to find the shear stress and normal stress on planes with normals oriented at 30 and 60 from the X 3-axis. theta (deg): 30 60 sigman MPa: 37.5 32.5 sigmas MPa: 4.3 4.3-2 if switched σn -1 if negative σ3 4b (5 pts) Get a printout of the Mohr circle and show where the stress components acting on these two planes plot on the circle. -3 if points have negative shear traction 4c (5 pts) If these two planes represent potential fault surfaces, which one is more likely to fail? HINT: Assume faulting is a frictional process driven by shear stress and resisted by compressive stress. 19-Feb-2009 Page 14 of 15

The plane oriented at theta = 60 degrees, because there is less normal stress but the same amount of shear stress. It would cross over the coulomb failure envelope sooner than the one on the other side of the circle. -2 if don t say why 19-Feb-2009 Page 15 of 15