Earthquake Simulation Table

Slides:



Advertisements
Similar presentations
P-wave S-wave Particles oscillate back and forth Wave travels down rod, not particles Particle motion parallel to direction of wave propagation Particles.
Advertisements

Chapter 1- General Properties of Waves Reflection Seismology Geol 4068
An-Najah National University
Properties of Waves Chapter 12 Section 3.
Theoretical aspects of seismic waves and sources Massimo Cocco INGV Earthquakes produce effects to the environment & the society Damages are produced by.
SEISMIC ANALYSIS Stability of a slope can be affected by seismicity in two ways: earthquake and blasting. These seismic motions are capable of inducing.
Chapter 16 Wave Motion.
Lecture-15 1 Lecture #15- Seismic Wave Overview. Lecture-15 2 Seismograms F Seismograms are records of Earth’s motion as a function of time.
Spectral Analysis of Wave Motion Dr. Chih-Peng Yu.
Learning objectives Understand the relationship of earthquakes to faulting Familiarization with earthquake & wave (energy) terminology Understand the.
Ground Motion Parameters Measured by triaxial accelerographs 2 orthogonal horizontal components 1 vertical component Digitized to time step of
Inputs to Signal Generation.vi: -Initial Distance (m) -Velocity (m/s) -Chirp Duration (s) -Sampling Info (Sampling Frequency, Window Size) -Original Signal.
Parameters, pulse parameters, attenuation, and resolution.
Earthquakes An earthquake is shaking or movement of the Earth. They are caused by plate tectonics.
Earthquakes.
Advance Design of RC Structure
Engineering Waves Overview In this lesson, we will learn about: What are waves? What are different types of waves? How do waves travel? How do waves relate.
For this section we start with Hooke’s Law. But we already learned this. (partially)
For this section we start with Hooke’s Law. But we already learned this. (partially)
CP Physics Chapter 12 Waves. Hooke’s Law F spring = kx During the periodic motion At equilibrium, velocity reaches a maximum (b) At maximum displacement,
Unit 2: Tectonic Processes Ms. Thind.  What is an earthquake?  Caused by shifting of the earth’s crust  Occur when plates or rock within the earth.
Graphical Analysis of the Relationship between Circumference and Diameter of a Circle.
Spring Constant, K The constant k is called the spring constant. SI unit of k = N/m.
1& 2. Pattern of earthquake, volcano, and mountain range on the Earth Matches the location of the plate boundaries. Most earthquakes, volcanoes and mountain.
Abdelmageed Elmustafa
Chapter 11 Vibrations and Waves.
HIGH FREQUENCY GROUND MOTION SCALING IN THE YUNNAN REGION W. Winston Chan, Multimax, Inc., Largo, MD W. Winston Chan, Multimax, Inc., Largo, MD Robert.
P – , TOW TANK FOR TETHERED HYDROFOIL TEAM MEMBERS: Hope Alm (ME)Tim Buckner (ME) William Lentlie (ME) Andres Santizo Matheu (ISE) Shauna.
1 Linear Wave Equation The maximum values of the transverse speed and transverse acceleration are v y, max =  A a y, max =  2 A The transverse speed.
1.To arrive at the relationship between displacement, velocity and acceleration for a system in SHM 2.To be able calculate the magnitude & direction of.
Waves. Wave Motion A wave travels along its medium, but the individual particles just move up and down.
BASICS OF DYNAMICS AND ASEISMIC DESIGN
Section 2 Properties of Mechanical Waves. Key Concepts What determines the frequency of a wave? How are frequency, wavelength, and speed related? How.
Measuring Earthquakes
Monday 9/30 QOD ---- on left p12 Write out your answer in a complete sentence. 1)What causes an earthquake to occur?
Get your software working before putting it on the robot!
Earthquakes. Earthquakes Our Definition: a sudden shaking of the ground because of movement within the earth’s crust.
Do Now: Take the waves pre-test – tell me what you already know about waves as we start our new unit.
Government Engineering College, Bhavnagar. Sub:- Geology & Geotechnics.
EaRtHqUaKeS!. More than 700 Earthquakes that are strong enough to cause damage occur every year. Earthquakes are caused by stress applied to rocks from.
Biomechanical Tissue Stimulator Matt Brady (BME/EE) Ankeet Choxi (BME) Misha Kotov (CS) Steven Manuel (ME) Adviser: Dr. V. Prasad Shastri.
Simple Harmonic and non harmonic Motion
Chapter 5:Using Newton’s Laws: Friction, Circular Motion, Drag Forces
Speed, Power, Torque & DC Motors
(plus some seismology)
Seismic Waves Large strain energy released during an earthquake
Earthquakes – Day 1 October 11, 2010.
Waves.
How the ground shakes? Dr. Syed Mohamed Ibrahim M.Tech., Ph.D., by
Chapter 12 The Nature of Waves
Earthquakes A sudden and violent shaking of the ground as a result of movements within the earth's crust or volcanic action.
Circular Motion - Objectives
College Physics, 7th Edition
Describing Motion.
Warmup 1. What is an earthquake’s location on a surface called?
Waves Wave- A self-propagating disturbance.
Waves and Oscillation waves transport _________ along a medium without transporting ________.
Active Figure 15.1  A block attached to a spring moving on a frictionless surface. (a) When the block is displaced to the right of equilibrium (x > 0),
Earthquakes.
Waves transfer energy Wave: A disturbance that propagates
Earthquake Magnitude Ahmed Elgamal
(plus some seismology)
Earth Shakes, Rattles, and Rolls
Chapter 12 - Section 2 Measuring Earthquakes
THE STUDY OF EARTHQUAKES
Acceleration Lab: page 33
Warmup 1. What is an earthquake’s location on a surface called?
Wave Properties.
Earthquake Waves.
Presentation transcript:

Earthquake Simulation Table SDI – Team 02 May 3, 2014

Group Members Tyler Williams, CE Competition Analyst, Researcher Paulina Olmedo, CE Team Leader, Webmaster, Earthquake Researcher Faculty Advisor Dr. Joseph Coe Philip Longo, ME Simulation/Prototype Design, SolidWorks Ilir Marku, CE Earthquake Analyst, Researcher

Preview Design Constraints Seismic Waves Preliminary Design Analysis of parameters Revised Design/ Budget

Abstract The purpose of our project is to design an earthquake shake table to be used by the Temple University Civil and Environmental engineering program for educational purposes and by students that wish to enter the annual EERI seismic design competition. It will have one-dimensional motion, replicating earthquake ground motions. The final goal is for the shake table to replicate an actual earthquake motion that students can test a simple structures on. In order to achieve this we need to acquire actuators and accelerometers to create and record both the motion of the table itself, and the simple structure to be tested. Using the accelerometers, we will be able to solve for the forces that the simulated earthquake motion exerts on the simple structure. This will allow future students to test the structural stability of their designs on a shake table with similar design specifications as the EERI seismic design competition.

Shake Tables

Functional Design Constraints Name Description Peak Acceleration The table will achieve a peak acceleration of 1.5 g’s Design Payload The table will be able to support and successfully test structures up to 11 kg Operation Frequency The shake table will operate at a relative frequency of 1 Hz Peak Velocity The peak velocity of the shake table will be 30 cm/sec Stroke Distance The shake table will have a stroke distance of 15 cm

Non - Functional Design Constraints Type Name Description Economic Cost Less than $500 Performance Power DC motor input Sustainability Reliability Factor of safety > 2.0 Portability Size Table Area:18.0 x18.0 inches Documentation Data Collection LabView MatLab

Determine Wave Parameters Collected Earthquake Records Project Overview Shake Table & Earthquake Research Seismic Wave Research Determine Wave Parameters Collected Earthquake Records Shake Table V.3 Design

Wave Motions Body Waves Surface Waves P - Wave S - Wave Love Wave Rayleigh Wave

P-Wave

S-Wave

Love Wave

Rayleigh Wave

Wave Selection Body Waves vs. Surface Waves We cant replicate body or surface waves We plan to mimic a shearing motion at the surface

Shake Table I.0 The design can only mimic a shear wave once it reaches the surface of the earth Rayleigh and Love Waves are much to complex to mimic even for the most intricate shake tables 2 degrees of motion- too complex, too expensive

Shear Wave Shear waves disrupt the Earths crust by slicing it laterally

Shear Wave Particle Dislocation

Table Wave Properties G Force 1.5 (m/s^2) Acceleration 14.715(m/s^2) Frequency 1(Hz) Stroke Amplitude 7.5(cm)

Frequency vs. Amplitude All seismic waves that travel through a medium have a specific amplitude and frequency The Frequency (1/T) of a surface wave determines the speed at which it propagates The amplitude of a wave determines the amount of displacement between the equilibrium point and the peak of a wave The amplitude is what actually causes the damage during an earthquake as it literally displaces the ground

FFT - Analysis The Fast Fourier Transform (FFT) allows one to analyze data for relative importance For our purposes, it allowed us to take real world acceleration vs. time data from various earthquakes and plot the frequency vs. amplitude This gave us the ability to see at which frequencies an earthquake’s amplitude would be the highest Modeling a wide range of earthquakes allowed us to determine the frequency at which the peak amplitude most often occurs

Frequency vs. FFT Amplitude

Revised Design

Final Design

Drive System Design Circular motion is outputted as linear motion Using a circular disk allowed our team to visualize the displacement our shake table would create Using a circular plate also made frequency calculations, in comparison to motor specs much easier

Materials List Part Name Specifcs Motor 12v DC at 2.4 rpm Bearings 2 at ½” Diameter Aluminum Rails Aluminum Rail Stands 2 at Legth, Height, Width Motor Mount See Final Design Crank arm See Final Desing Top Plate 20in. x 20in. Area Base Plate 24” x 24”

Budget Part Amount Price Motor 1 $44.30 Top Plate $4.86 Base Plate $193.52 Rail Bearing 2 $94.4 Aluminum Rail $128.96 Rail Stand $3.62 Crank Wheel $25.86 Motor Mount $0.4 Crank Arm $0.1 Total $494.06

SDII-Schedule Assemble the Shake Table Write Code using LabView Undergo Testing Adjust Parts as necessary Finish Shake Table

References (2006). Retrieved 2014, from UPSeis: http://www.geo.mtu.edu/UPSeis/waves.html Lam, Nelson. Wilson, John. Chandler, Adrian. Hutchinson, Graham. (2000) Response spectral relationships for rock sites derived from the component attenuation model. Earthquake Engineering And Structural Dynamics Earthquake Engng Struct. Dyn. 2000; 29:1457}1489 Vere-Jones, D. (1995). Forecasting earthquakes and earthquake risk. International Journal of Forecasting, 11(4), 503-538. doi:http://dx.doi.org.libproxy.temple.edu/10.1016/0169- 2070(95)00621-4

Bring Your Child to Work Day

Questions? https://sites.google.com/a/temple.edu/earth-shaker/home