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Chapter 2: Acquiring rotations with magnetometers

Shuki

Ronen

Bob

Brune

Kerry

Key

Steven

Constable

  • Current rotational acquisition technology for exploration seismology
  • Rotations from magnetic projections
  • Silver Lake magnetic-rotation survey

Chris Castillo

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Requirements for a seismic sensor

2

  • Durability
  • Reliability
  • Sensitivity
  • Dynamic range (amplitude, frequency)
  • Power consumption
  • Availability / economy
  • …...

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Seismic rotation sensor technologies

3

  • Ring lasers
  • Fiber-Optic Gyroscopes
  • Electrokinetic / Magneto-hydrodynamic
  • Array-derived rotations / Rotaphone

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Seismic rotation sensor technologies

4

  • Ring lasers
  • Fiber-Optic Gyroscopes
  • Electrokinetic / Magneto-hydrodynamic
  • Array-derived rotations / Rotaphone

Geodesy, Gravity waves

Inertial navigation systems

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Array-derived rotations

Current rotational acquisition / Rotations from magnetic projections / Silver Lake magnetic-rotation experiment

5

Hooke’s law:

Free surface:

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Array-derived rotations

Current rotational acquisition / Rotations from magnetic projections / Silver Lake magnetic-rotation experiment

6

d

1

2

Rotations:

Derive rotations without burying the geophones

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Array-derived rotations

Current rotational acquisition / Rotations from magnetic projections / Silver Lake magnetic-rotation experiment

7

Rotations:

1

2

1

2

Aliasing

Noise

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Array-derived rotations / Rotaphone

8

Current rotational acquisition / Rotations from magnetic projections / Silver Lake magnetic-rotation experiment

  • Vertical and horizontal geophones attached to the same frame
  • Rotation is measured by differencing geophone components
  • Requires in-situ cross-calibration between geophone responses before recording data

Noise floor: 4 x 10-9 rad/sec

Dynamic range: 120 dB

Brokesova and Malek, 2016

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Electrokinetic rotation sensor

9

Noise floor: 0.6 x 10-7 rad/sec

Dynamic range: 117 dB

Passband: 0.03 – 50 Hz

Power usage: 12 mA

Weight 1.5 kg

Current rotational acquisition / Rotations from magnetic projections / Silver Lake magnetic-rotation experiment

METR03 (AST LLC, Russia)

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Electrokinetic rotation sensors for exploration seismology

10

Advantages:

  • Field deployable (on land)
  • ~Exploration seismology bandwidth (2-30 Hz)
  • Price

Vertical

Pitch

Challenges:

  • Dynamic range
  • Noise floor (need < 10-8 rad/sec)
  • Availability
  • Durability

Current rotational acquisition / Rotations from magnetic projections / Silver Lake magnetic-rotation experiment

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Current sensor summary

11

Current rotational acquisition / Rotations from magnetic projections / Silver Lake magnetic-rotation experiment

Angela Di Virgilio, 2016

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Seismic rotation sensor technologies

12

  • Ring lasers
  • Fiber-Optic Gyroscopes
  • Electrokinetic / Magneto-hydrodynamic
  • Array-derived rotations / Rotaphone

Current rotational acquisition / Rotations from magnetic projections / Silver Lake magnetic-rotation experiment

  • Induction coil magnetometers?

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Scripps Marine Electromagnetics Lab

13

Induction-coil magnetometers

EM ocean-bottom node

Field deployment

Current rotational acquisition / Rotations from magnetic projections / Silver Lake magnetic-rotation experiment

Controlled source EM survey

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Scripps Marine Electromagnetics Lab

14

Induction-coil magnetometers

EM ocean-bottom node

Field deployment

Current rotational acquisition / Rotations from magnetic projections / Silver Lake magnetic-rotation experiment

Controlled source EM survey

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11 years ago

15

We see seismic shots in ocean-bottom EM data.

Current rotational acquisition / Rotations from magnetic projections / Silver Lake magnetic-rotation experiment

I wonder why?

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April 2009: Earthquake recorded by EM components

16

Current rotational acquisition / Rotations from magnetic projections / Silver Lake magnetic-rotation experiment

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2 years ago, while working on the Kettleman 6C dataset

17

Ohad, could it be that Steve’s EM nodes were recording rotations?

Hmmm…..

Current rotational acquisition / Rotations from magnetic projections / Silver Lake magnetic-rotation experiment

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Faraday’s law

18

Michael Faraday

Induction-coil magnetometer

Current rotational acquisition / Rotations from magnetic projections / Silver Lake magnetic-rotation experiment

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Seismic rotations from induction-coil magnetometers

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Earth’s magnetic field is constant

Seismic waves rotate the ground

Magnetometers rotate

Projections on magnetometers change

Current rotational acquisition / Rotations from magnetic projections / Silver Lake magnetic-rotation experiment

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Seismic rotations from induction-coil magnetometers

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Earth’s magnetic field is constant

Seismic waves rotate the ground

Magnetometers rotate

Projections on magnetometers change

Magnetic projections

Rotations

Current rotational acquisition / Rotations from magnetic projections / Silver Lake magnetic-rotation experiment

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Projection null space

21

Current rotational acquisition / Rotations from magnetic projections / Silver Lake magnetic-rotation experiment

Ambient magnetic field direction

https://en.wikipedia.org/wiki/Euler_angles

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Silver Lake magnetic-rotations experiment

22

Las Vegas

Los Angeles

Silver Lake

Current rotational acquisition / Rotations from magnetic projections / Silver Lake magnetic-rotation experiment

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EM ambient noise floor

23

Betsy gun

Current rotational acquisition / Rotations from magnetic projections / Silver Lake magnetic-rotation experiment

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Shot / Receiver Geometry

24

Current rotational acquisition / Rotations from magnetic projections / Silver Lake magnetic-rotation experiment

+ 1 remote magnetometer station to attenuate magnetotelluric waves

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Rotation sensors, magnetometers and geophones

25

Remote station

Current rotational acquisition / Rotations from magnetic projections / Silver Lake magnetic-rotation experiment

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Remote magnetometer station

26

Remote Hx

Remote Hy

Remote Hz

Current rotational acquisition / Rotations from magnetic projections / Silver Lake magnetic-rotation experiment

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27

Hy

Hx

Hz

Ry

Rx

Rz

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28

Hy

Hx

Hz

Ry

Rx

Rz

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29

Hy

Hx

Hz

Ry

Rx

Rz

V=130 m/s

V=230 m/s

V=1420 m/s

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30

Hy

Hx

Hz

Ry

Rx

Rz

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31

Hy

Hx

Hz

Ry

Rx

Rz

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32

Hy

Hx

Hz

Ry

Rx

Rz

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Converting magnetic projections to rotations

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Hy

Hx

Hz

Ry

Rx

Rz

Quaternion rotation module

Current rotational acquisition / Rotations from magnetic projections / Silver Lake magnetic-rotation experiment

William R. Hamilton,

1844

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Pitch (Ry)

Roll (Rx)

Yaw (Rz)

Rotation sensors

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Pitch (Ry)

Roll (Rx)

Yaw (Rz)

Magnetometers

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Pitch (Ry)

Roll (Rx)

Yaw (Rz)

Magnetometers

Noise from vertical magnetometer

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Pitch (Ry)

Roll (Rx)

Yaw (Rz)

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Projection null space

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Current rotational acquisition / Rotations from magnetic projections / Silver Lake magnetic-rotation experiment

  • Ambient magnetic field direction: Z
  • Can derive rotations around X and Y
  • Can’t derive rotations around Z
  • Non-commutativity of rotations

https://en.wikipedia.org/wiki/Euler_angles

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Pitch (Ry)

Roll (Rx)

Yaw (Rz)

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Summary

40

  1. Robust rotation sensor technology is not (yet) widely available for industry-scale exploration seismology
  2. 3-component magnetometers can be used as 3-component seismic rotation sensors
  3. Need to remove noise from ambient local magnetic fields
  4. Consider null space of projections

Current rotational acquisition / Rotations from magnetic projections / Silver Lake magnetic-rotation experiment

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Prospects

41

  1. 6C earthquakes from existing magnetometer data

Current rotational acquisition / Rotations from magnetic projections / Silver Lake magnetic-rotation experiment

2. 6C ocean-bottom seismic surveys

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  • Steve Constable, Kerry Key, and Scripps students
  • Shuki Ronen
  • The sponsors of the Scripps Marine EM Consortium
  • John Archer, Patryusz Batchelda – Geokinetics
  • Chris Castillo

0

-80

160

80

Acknowledgements

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Spare slides

43

Current rotational acquisition / Rotations from magnetic projections / Silver Lake magnetic-rotation experiment

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What are rotation data�Acquisition and application of 6C data�Recording rotations without rotation sensors�Silver Lake magnetic-rotation survey

Steven Constable, Kerry Key

Rotations from magnetometers

44

Time (sec)

Geophones

Induction-coil magnetometers

mm / s

nanoTesla

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What are rotation data�Acquisition and application of 6C data�Recording rotations without rotation sensors�Silver Lake magnetic-rotation survey

Six-component Earthquake data from combined 3C geophones and 3C magnetometer

45

Is this reliable?�Active seismic field experiment to validate rotations from magnetic

Transverse

Pitch

Radial

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EM ambient noise floor

46

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Ring Lasers

47

Current rotational acquisition / Rotations from magnetic projections / Silver Lake magnetic-rotation experiment

Based on the “Sagnac” effect:

Phase shift of two light beams propagating in opposite directions

Source: Wikipedia

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Ring Lasers

48

Current rotational acquisition / Rotations from magnetic projections / Silver Lake magnetic-rotation experiment

Based on the “Sagnac” effect:

Phase shift of two light beams propagating in opposite directions

  • Earth’s rotation
  • Gravitational waves

Seismic = noise

Source: Wikipedia

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Ring Lasers

49

Current rotational acquisition / Rotations from magnetic projections / Silver Lake magnetic-rotation experiment

Down to 10-13 rad/s at low frequencies

Wetzel, Germany

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Ring Lasers

50

Current rotational acquisition / Rotations from magnetic projections / Silver Lake magnetic-rotation experiment

Angela Di Virgilio, 2016

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Ring Lasers

51

Current rotational acquisition / Rotations from magnetic projections / Silver Lake magnetic-rotation experiment

Angela Di Virgilio, 2016

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Ring Lasers

52

Current rotational acquisition / Rotations from magnetic projections / Silver Lake magnetic-rotation experiment

ROMY:

Tetrahedral ring laser currently under construction near Munich

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Fiber-optic Gyros

53

Current rotational acquisition / Rotations from magnetic projections / Silver Lake magnetic-rotation experiment

Based on the “Sagnac” effect:

Phase shift of two light beams propagating in opposite directions

Need to ensure that polarization of the two light beams is identical

Source: Wikipedia

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Fiber-optic Gyros

54

Current rotational acquisition / Rotations from magnetic projections / Silver Lake magnetic-rotation experiment

iXBlue (France)

20 nrad/s < 0.01 Hz

60 nrad/s 0.01-10 Hz

1 urad/s 10-100 Hz

High power usage: ~8 w

High sensor self-noise

Source: iXBlue

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Magneto-hydrodynamic rotation sensor

55

Current rotational acquisition / Rotations from magnetic projections / Silver Lake magnetic-rotation experiment

Advanced Technology Associates (Albuquerque, New Mexico)

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Magneto-hydrodynamic rotation sensor

56

Current rotational acquisition / Rotations from magnetic projections / Silver Lake magnetic-rotation experiment

Advanced Technology Associates (Albuquerque, New Mexico)

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Magneto-hydrodynamic rotation sensor

57

AST (Moscow)

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Magneto-hydrodynamic rotation sensor

58

AST (Eentec)

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The seismoelectric effect

59

Current rotational acquisition / Rotations from magnetic projections / Silver Lake magnetic-rotation experiment

S. Haines, 2004

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The seismoelectric effect

60

Current rotational acquisition / Rotations from magnetic projections / Silver Lake magnetic-rotation experiment

S. Haines, 2004

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Pride, 1994, seismoelectric effect in porous medium

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Current rotational acquisition / Rotations from magnetic projections / Silver Lake magnetic-rotation experiment

E: Electric field, H: Magnetic field, D: dielectric displacement, B: Magnetic flux density, J: Electric current density, u: particle displacement, w: relative grain/fluid displacement, pf: fluid pressure, tau: bulk stress tensor, G: shear modulus, rho: bulk density

rho_f: pore fluid density, Omega: angular frequency, sigma: electrical conductivity, epsilon: electrical permittivity, mu: magnetic permeability, eta: fluid viscosity, K: hydraulic permeability, L: relation between grain/fluid motion, K_u: undrained bulk modulus, K_s: solid bulk modulus, K_f: fluid bulk modulus, phi: porosity

Current rotational acquisition / Rotations from magnetic projections / Silver Lake magnetic-rotation experiment

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Pride, 1994, seismoelectric effect in porous medium

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Current rotational acquisition / Rotations from magnetic projections / Silver Lake magnetic-rotation experiment

E: Electric field, H: Magnetic field, D: dielectric displacement, B: Magnetic flux density, J: Electric current density, u: particle displacement, w: relative grain/fluid displacement, pf: fluid pressure, tau: bulk stress tensor, G: shear modulus, rho: bulk density

rho_f: pore fluid density, Omega: angular frequency, sigma: electrical conductivity, epsilon: electrical permittivity, mu: magnetic permeability, eta: fluid viscosity, K: hydraulic permeability, L: relation between grain/fluid motion, K_u: undrained bulk modulus, K_s: solid bulk modulus, K_f: fluid bulk modulus, phi: porosity

Current rotational acquisition / Rotations from magnetic projections / Silver Lake magnetic-rotation experiment

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Water table at Silver Lake is ~500 meters down

63

Current rotational acquisition / Rotations from magnetic projections / Silver Lake magnetic-rotation experiment

Vertical geophone frequency content during active shooting at Silver Lake

EM rotations / 6C earthquakes / Seismoelectric effect / EM rotations + seismoelectric field test

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Current rotational acquisition / Rotations from magnetic projections / Silver Lake magnetic-rotation experiment

Bz

By

Bx

Rx

Ry

Rz

Rx

Ry

Rz

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Current rotational acquisition / Rotations from magnetic projections / Silver Lake magnetic-rotation experiment

Bz

By

Bx

Rx

Ry

Rz

Rx

Ry

Rz

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Non-commutativity of rotations

66

Current rotational acquisition / Rotations from magnetic projections / Silver Lake magnetic-rotation experiment

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Current rotational acquisition / Rotations from magnetic projections / Silver Lake magnetic-rotation experiment

Bz

By

Bx

Rx

Ry

Rz

Rx

Ry

Rz

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Current rotational acquisition / Rotations from magnetic projections / Silver Lake magnetic-rotation experiment

Bz

By

Bx

Rx

Ry

Rz

Rx

Ry

Rz