There IS ROTATION in the S wave The Rotation Signal is purely from the S wave There is NO ROTATION in the P Wave Rotational Seismic: SEG Standards Proposal.

Slides:



Advertisements
Similar presentations
Surface Waves and Free Oscillations
Advertisements

Surface Waves and Free Oscillations
Aula Teórica 6 Pressure distribution in “Rigid Body” type flows.
13-1 Physics I Class 13 General Rotational Motion.
Development of an In-Situ Test for Direct Evaluation of the Liquefaction Resistance of Soils K. H. Stokoe, II, E. M. Rathje and B.R. Cox University of.
Rotational Motion Angular Quantities Angular Kinematics Rolling Motion.
March 25, 2002EarthScope CSIT Workshop Data Archiving and IT Issues for PBO Douglas Neuhauser UC Berkeley Seismological Lab Northern California Earthquake.
Attenuating the ice flexural wave on arctic seismic data David C. Henley.
H. Igel1, A. Cochard1, A. Fichtner1, A. Flaws1,2, U. Schreiber3 , B
Measurements using Atom Free Fall
Rotational Dynamics and Static Equilibrium. Torque From experience, we know that the same force will be much more effective at rotating an object such.
Data centres and observablesModern Seismology – Data processing and inversion 1 Data in seismology: networks, instruments, current problems  Seismic networks,
Theoretical aspects of seismic waves and sources Massimo Cocco INGV Earthquakes produce effects to the environment & the society Damages are produced by.
Applied Geophysics An Introduction
14-1 Physics I Class 14 Introduction to Rotational Motion.
Studying Earthquakes. Seismology: the study of earthquakes and seismic waves.
1 Physics 111/121 Mini-Review Notes on Vectors. 2 Right hand rule: - curl fingers from x to y - thumb points along +z.
Esci 411, Advanced Exploration Geophysics (Micro)seismicity John Townend EQC Fellow in Seismic Studies
How and where are earthquake waves detected and recorded? A seismograph is an instrument that records earthquake waves. It is also used to determine the.
Sensing self motion Key points: Why robots need self-sensing Sensors for proprioception in biological systems in robot systems Position sensing Velocity.
Geology 5660/6660 Applied Geophysics 17 Jan 2014 © A.R. Lowry 2014 Read for Wed 22 Jan: Burger (Ch 2.2–2.6) Last time: The Wave Equation; The Seismometer.
Seismic interferometry-by- deconvolution for controlled-source and passive data Kees Wapenaar, Joost van der Neut, Elmer Ruigrok, Deyan Draganov, Juerg.
PEER EARTHQUAKE SCIENCE-ENGINEERING INTERFACE: STRUCTURAL ENGINEERING RESEARCH PERSPECTIVE Allin Cornell Stanford University SCEC WORKSHOP Oakland, CA.
Weighted Stacking of 3-D Converted-wave Data for Birefringent Media Richard Bale.
Copyright © 2010 Pearson Education, Inc. Lecture Outline Chapter 11 Physics, 4 th Edition James S. Walker.
New Trends in AVO Brian Russell and Dan Hampson
The In-flight Calibration of the GOCE Gradiometer Stefano Cesare(1), Giuseppe Catastini(1), Rune Floberghagen(2), Daniel Lamarre(2) (1) Thales Alenia.
Circular Motion Topics Angular Measure Angular Speed and Velocity Uniform Circular Motion and Centripetal Acceleration Angular Acceleration.
Geology 5660/6660 Applied Geophysics Last time: Brief Intro to Seismology & began deriving the Seismic Wave Equation: Four types of seismic waves:  P.
Geophysics/Tectonics
The elastic wave equation Seismology and the Earth’s Deep Interior The Elastic Wave Equation Elastic waves in infinite homogeneous isotropic media Numerical.
IntroductionModern Seismology – Data processing and inversion 1 Modern Seismology Lecture Outline Seismic networks and data centres Mathematical background.
1 Honors Physics 1 Class 15 Fall 2013 Rolling motion Noninertial reference frames Fictitious forces.
Geology 5640/6640 Introduction to Seismology 6 Feb 2015 © A.R. Lowry 2015 Read for Mon 9 Feb: S&W (§2.5) Last time: Polarization & seismic phases…
Seismological Perspectives on Broadband Tilt, Strain, and Rotation Measurement Charles Langston Center for Earthquake Research and Information University.
Summary of seismology component of the course Sources Waves Location Magnitude/Intensity Focal mechanisms Other topics.
The elastic wave equationSeismology and the Earth’s Deep Interior The Elastic Wave Equation  Elastic waves in infinite homogeneous isotropic media 
RECORD PROCESSING CONSIDERATIONS FOR THE EFFECTS OF TILTING AND TRANSIENTS VLADIMIR GRAIZER California Geological Survey.
ESS 303 – Biomechanics Linear Kinematics. Linear VS Angular Linear: in a straight line (from point A to point B) Angular: rotational (from angle A to.
Geometric Transformations Hearn & Baker Chapter 5 Some slides are taken from Robert Thomsons notes.
Abj 4.2.2: Pressure, Pressure Force, and Fluid Motion Without Flow [Q2 and Q3] Area as A Vector Component of Area Vector – Projected Area Net Area.
1 Honors Physics 1 Class 11 Fall 2013 Propagation of Uncertainty Rotational quantities as vectors.
Chapter 8: Rotational Motion Pure rotational motion means the circular movement of a ‘rigid body’ where all points have the same angular motion…this motion.
Tuesday Sept 21st: Vector Calculus Derivatives of a scalar field: gradient, directional derivative, Laplacian Derivatives of a vector field: divergence,
Geology 5640/6640 Introduction to Seismology 2 Feb 2015 © A.R. Lowry 2015 Read for Wed 4 Feb: S&W (§2.4); Last time: The Wave Equation! The.
Transmission coefficients for P and S waves in HardBego stones The point where the incident ray reaching the S critique angle hits the interface The point.
Lecture 5: Introduction to 3D
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.
Near Fault Ground Motions and Fault Rupture Directivity Pulse Norm Abrahamson Pacific Gas & Electric Company.
Physics Formulas. The Components of a Vector Can resolve vector into perpendicular components using a two-dimensional coordinate system:
Geology 5640/6640 Introduction to Seismology 23 Mar 2015 © A.R. Lowry 2015 Last time: Normal Modes Free oscillations are stationary waves that result from.
Chapter 11 – Rotational Dynamics & Static Equilibrium.
Geology 5640/6640 Introduction to Seismology 09 Jan 2015 © A.R. Lowry 2015 Read for Mon 12 Jan: S&W 1-28 Last time: Course overview Discussed: syllabus,
Geology 5660/6660 Applied Geophysics 20 Jan 2016
CREWES 2003 Sponsors Meeting We’ve presented our research results and educational progress in geophysical exploration in partnership with the resource.
Instrumentation Symposium 10/9/2010 Nigbor 1 Instrumentation Selection Strategies Robert Nigbor
Lee M. Liberty Research Professor Boise State University.
1 Introduction to Applied Geophysics & Geophysical Exploration Prof Jeannot Trampert (coordinator) Dr Fred Beekman
Constant Rotation Now that we know how to define the angular position, we can examine rotational motion. Consider the lab equipment using a view from above.
Geophones for Recording EQ’s OVERVIEW Local Events Aftershock Deployments Extend Period for Regional Events Simple Checks to Assure Sensor Works.
Introduction to Seismology
Conor Mow-Lowry Thanks to: Krishna, Jeff, Brian, Jim, Hugh, Robert
Introduction to Seismology
Geodesy & Crustal Deformation
الفصل 1: الحركة الدورانية Rotational Motion
Coupled seismoelectric wave propagation in porous media
Physics I Class 13 Introduction to Rotational Motion.
Elastic Moduli Young’s Modulus Poisson Ratio Bulk Modulus
Effects of Rotation Motions on a Seismogram
Physics I Class 14 Introduction to Rotational Motion.
Presentation transcript:

There IS ROTATION in the S wave The Rotation Signal is purely from the S wave There is NO ROTATION in the P Wave Rotational Seismic: SEG Standards Proposal – Sept., 2013 What is it & why consider standards at this early stage?

Measure Rotation around 3 axes - 3 θ θ-x θ-y θ-z Vector Curl of displacement Record 3- θ Rotation in addition to 3-C or 4-C Measure Rotation around 3 axes - 3 θ θ-x θ-y θ-z Vector Curl of displacement Record 3- θ Rotation in addition to 3-C or 4-C 3-Theta Data – What is it? “Theta Data” is comprised of “Curl Traces”

Earthquake Seismology: William H. K. Lee (USGS) & others Int’l Working Group on Rotational Seismology (IWGRS) BSSA (May, 2009) Sensor technology development - decades: Defense (US and USSR) inertial guidance, etc. Earthquake Seismology: William H. K. Lee (USGS) & others Int’l Working Group on Rotational Seismology (IWGRS) BSSA (May, 2009) Sensor technology development - decades: Defense (US and USSR) inertial guidance, etc. Origins – Where Did Rotational Seismic ‘Come From’? Origins – Where Did Rotational Seismic ‘Come From’?

Typically flat spectral response for angular velocity. MET Tech, ATA Eentec, Rotaphone, FOG, SAGNAC, Sercel, etc. Typically flat spectral response for angular velocity. MET Tech, ATA Eentec, Rotaphone, FOG, SAGNAC, Sercel, etc. Rotational Sensors

Electrokinetic Rotational Sensor Rotational Fluid flow through screen electrodes

Transverse Rotational – TR Mode 6 Components: 3 Linear, 3 Theta

Transverse Linear – TL Mode 6 Components: 3 Linear, 3 Theta

PSV - 3C-Vert., 3C-Radial, 3θ-Trans.

SH - 3C-Trans., 3θ-Vert., 3θ-Radial

Proposing standards before commercialization due to risk of confusion. (analogous to some other industries, such as computer networking) ‘Default’ (Right-Handed coordinates & rotations, positive voltages / numbers) Consider 6-C, or more: 7-C (including Pressure), or 10-C (vector Pressure Gradient) Consider particular relationships with vector linear seismic Proposing standards before commercialization due to risk of confusion. (analogous to some other industries, such as computer networking) ‘Default’ (Right-Handed coordinates & rotations, positive voltages / numbers) Consider 6-C, or more: 7-C (including Pressure), or 10-C (vector Pressure Gradient) Consider particular relationships with vector linear seismic Proposed Rotational Standards

Example of Relationship between Theta and Linear Ordinate and Slope Sampling to double the Effective Spatial Nyquist Example of Relationship between Theta and Linear Ordinate and Slope Sampling to double the Effective Spatial Nyquist

Example of Relationship between Theta and Linear Pressure (P wave only) + TR-Theta (S wave only) AVO for gas sandstone David Aldridge, et. al., Sandia National Lab, Example of Relationship between Theta and Linear Pressure (P wave only) + TR-Theta (S wave only) AVO for gas sandstone David Aldridge, et. al., Sandia National Lab, PP SP PS SS (No Free surface; buried phones)

Example of Relationship between Theta and Linear Igel / Aldridge Point Array Example of Relationship between Theta and Linear Igel / Aldridge Point Array At a single 3-C / 3- Ɵ sensor: transverse linear acceleration S VELOCITY = orthogonal transverse rotational velocity Potential use for shear statics: get shear velocity around each 6-C phone. From 3-C and 3- Ɵ data can determine direction AND velocity of shear wave propagation.

Example of Relationship between Theta and Linear Tilt Correction of Linear using Rotation Example of Relationship between Theta and Linear Tilt Correction of Linear using Rotation If a Horizontal Linear Phone tilts by angle α, then it picks up error: Gravity * sin(α) Micro- or milli-radians of tilt give a potentially significant error compared to weak seismic reflections (C-waves). Consider a worse case: weak C-wave data on horizontal phone at same time as strong ground roll in uncorrelated vibroseis data

Right Handed coordinate system Z-axis point down (note ‘Parity’ issues, e.g. Z-up) Right-Handed rotation (‘Chirality’) Theta-Phones typically angular velocity Positive voltages for RH rotation (‘Polarity’) & Positive numbers for RH rotation Nominal scaling: number “1” = 1.0 μ -radian/sec Consider(?) recommended nomenclature Carefully consider relationships of rotational and linear, … and also future processing Right Handed coordinate system Z-axis point down (note ‘Parity’ issues, e.g. Z-up) Right-Handed rotation (‘Chirality’) Theta-Phones typically angular velocity Positive voltages for RH rotation (‘Polarity’) & Positive numbers for RH rotation Nominal scaling: number “1” = 1.0 μ -radian/sec Consider(?) recommended nomenclature Carefully consider relationships of rotational and linear, … and also future processing Some Suggested Specifics:

Some level of interest in Rotational Standards: 3+ major E&P cos. 2 Geophysical service cos. 2 Rotational sensor manufacturer’s Most companies unaware Small but increasing interest and activity in rotational testing, patent activity, and presentations. Next step - ? Draft Rotational Standards to be developed by 3 to 6+ companies with technical interest / knowledge Some level of interest in Rotational Standards: 3+ major E&P cos. 2 Geophysical service cos. 2 Rotational sensor manufacturer’s Most companies unaware Small but increasing interest and activity in rotational testing, patent activity, and presentations. Next step - ? Draft Rotational Standards to be developed by 3 to 6+ companies with technical interest / knowledge Thank you for your interest !

THETA-DATA: Introduction to rotational seismology and its potential uses THETA-DATA: Introduction to rotational seismology and its potential uses David Aldridge Sandia National Lab Mirko van der Baan U. of Alberta, Edmonton Robert Brune Consultant/Geokinetics Jim Gaiser Geokinetics, now CGG Everhard Muyzert Schlumberger, Cambridge Rotational Seismic: measure & analyze rotational motion at geophones, in addition to linear motion. Potential applications: spatial sampling, micro-seismic, elastic wave,... Rotational Summary 2012 SEG ALSO Various Presentations, particularly Schlumberger, Cambridge at EAGE 2012, 2013 and Stanford SEP