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Nyeste erfaringer med processering af SkyTEM data Esben Auken GeoFysikSamarbejdet Geologisk Institut, Aarhus Universitet

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Page 1: Nyeste erfaringer med processering af SkyTEM data Esben Auken GeoFysikSamarbejdet Geologisk Institut, Aarhus Universitet

Nyeste erfaringer med processering

af SkyTEM data

Esben Auken

GeoFysikSamarbejdetGeologisk Institut, Aarhus Universitet

Page 2: Nyeste erfaringer med processering af SkyTEM data Esben Auken GeoFysikSamarbejdet Geologisk Institut, Aarhus Universitet

Outline What is in the database?

Pitch and roll correction

Data filtering

Summary

Page 3: Nyeste erfaringer med processering af SkyTEM data Esben Auken GeoFysikSamarbejdet Geologisk Institut, Aarhus Universitet

Ensuring Best Possible Data Quality Obtain maximum information about formation

resistivities

5% data reproducibility of SkyTEM data on Lyngby test site

5% repeatability at each take off and landing

Accurate data processing (and inversion) – the basis!

Page 4: Nyeste erfaringer med processering af SkyTEM data Esben Auken GeoFysikSamarbejdet Geologisk Institut, Aarhus Universitet

Data Basis Data types measured by the system

• GPS – 2 per sec.• Pitch and roll of transmitter frame – 1.5 per sec. • Laser altitude – 20 per sec. from two devices• Transmitter current – 1 per dataset• Single decays from 2 or more receiver channels – 40 -120 Mb

per hour

Page 5: Nyeste erfaringer med processering af SkyTEM data Esben Auken GeoFysikSamarbejdet Geologisk Institut, Aarhus Universitet

Outline What is in the database?

Pitch and roll correction

Data filtering

Summery

Page 6: Nyeste erfaringer med processering af SkyTEM data Esben Auken GeoFysikSamarbejdet Geologisk Institut, Aarhus Universitet

Data Processing Voltage data and altitudes corrected with respect to the

pitch and roll of the frame

Manual intervention is necessary for• Altitudes• Culling of distorted data caused by coupling to wires

and fences

Data are not leveled (in the future - might be changed for very early times)

Page 7: Nyeste erfaringer med processering af SkyTEM data Esben Auken GeoFysikSamarbejdet Geologisk Institut, Aarhus Universitet

Altitude and Tilt Correction ”Normal” situation

Tx

R x

G round

1

lTx

R x

G round

1

l

Page 8: Nyeste erfaringer med processering af SkyTEM data Esben Auken GeoFysikSamarbejdet Geologisk Institut, Aarhus Universitet

Altitude and Tilt Correction ”Normal” situation

Tx

R x

G round

1

Tx A lt

l

Page 9: Nyeste erfaringer med processering af SkyTEM data Esben Auken GeoFysikSamarbejdet Geologisk Institut, Aarhus Universitet

Altitude and Tilt Correction ”Normal” situation – modelled in the inversion

Tx

R x

G round

1

Tx A lt R x A lt

l

Page 10: Nyeste erfaringer med processering af SkyTEM data Esben Auken GeoFysikSamarbejdet Geologisk Institut, Aarhus Universitet

Altitude and Tilt Correction ”Field” situation

G round

2

Page 11: Nyeste erfaringer med processering af SkyTEM data Esben Auken GeoFysikSamarbejdet Geologisk Institut, Aarhus Universitet

Altitude and Tilt Correction ”Field” situation

G round

2

Tx A lt

l

Page 12: Nyeste erfaringer med processering af SkyTEM data Esben Auken GeoFysikSamarbejdet Geologisk Institut, Aarhus Universitet

Altitude and Tilt Correction ”Field” situation

G round

2

Tx A lt

Page 13: Nyeste erfaringer med processering af SkyTEM data Esben Auken GeoFysikSamarbejdet Geologisk Institut, Aarhus Universitet

Altitude and Tilt Correction ”Normal” situation – modelled in the inversion

G round

2

Tx A lt R x A lt

R xl cos

Page 14: Nyeste erfaringer med processering af SkyTEM data Esben Auken GeoFysikSamarbejdet Geologisk Institut, Aarhus Universitet

Tilt data 5 min 3.5 line km

Tilt of +/-10° correction of voltage data

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Tilt [D

eg

ree

s]

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-8.0

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Tilt [D

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-8.0

Time

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Tilt [D

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y-tilt +/- 4°x-tilt +/- 8°Filtered

Page 15: Nyeste erfaringer med processering af SkyTEM data Esben Auken GeoFysikSamarbejdet Geologisk Institut, Aarhus Universitet

Altitude Processing

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Altitu

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[m]

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Altitu

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Altitu

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[m]

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Time

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Raw Laser 1Raw Laser 2Removed by filteringFinal – tilt corrected and relocated

Removal of laser reflection from tree tops

Correction of altitudes for tilt – non perpendicular reflections from the ground

Relocation of altitudes to center of Tx and Rx coils

Laser reflections from tree tops

Difference due to high y-tilt

5 min 3.5 line km

Page 16: Nyeste erfaringer med processering af SkyTEM data Esben Auken GeoFysikSamarbejdet Geologisk Institut, Aarhus Universitet

Outline What is in the database?

Pitch and roll correction

Data filtering

Summery

Page 17: Nyeste erfaringer med processering af SkyTEM data Esben Auken GeoFysikSamarbejdet Geologisk Institut, Aarhus Universitet

Time14:29:5014:29:4014:29:3014:29:2014:29:1014:29:0014:28:5014:28:4014:28:3014:28:2014:28:1014:28:00

Log

- N

o U

nit

1e+00

1e+01

1e+02

1e+03

1e+04

1e+05

Box average – Narrow/Wide SkyTEM data example (Airborne TEM)

30s ~ 400m

SkyTEM data, 2 min ~ 1.5 Km

5s ~ 65 m

gate 1 gate 2 gate 3 . . . . . . . gate n

Raw

Page 18: Nyeste erfaringer med processering af SkyTEM data Esben Auken GeoFysikSamarbejdet Geologisk Institut, Aarhus Universitet

Box average – Narrow/Wide

Time14:29:5014:29:4014:29:3014:29:2014:29:1014:29:0014:28:5014:28:4014:28:3014:28:2014:28:1014:28:00

Log

- N

o U

nit

1e+00

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Raw

Time14:29:5014:29:4014:29:3014:29:2014:29:1014:29:0014:28:5014:28:4014:28:3014:28:2014:28:1014:28:00

Log

- N

o U

nit

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Raw

Time14:29:5014:29:4014:29:3014:29:2014:29:1014:29:0014:28:5014:28:4014:28:3014:28:2014:28:1014:28:00

Log

- N

o U

nit

1e+00

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Average

Time14:29:5014:29:4014:29:3014:29:2014:29:1014:29:0014:28:5014:28:4014:28:3014:28:2014:28:1014:28:00

Log

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o U

nit

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Average

30 s

5 s

2 min ~ 1.5 Km

Page 19: Nyeste erfaringer med processering af SkyTEM data Esben Auken GeoFysikSamarbejdet Geologisk Institut, Aarhus Universitet

Time14:29:5014:29:4014:29:3014:29:2014:29:1014:29:0014:28:5014:28:4014:28:3014:28:2014:28:1014:28:00

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o U

nit

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Trapezoid shaped average combines the best from the narrow and the wide box

average

used for SkyTEM data

Trapezoid shaped average

Box shaped average

Page 20: Nyeste erfaringer med processering af SkyTEM data Esben Auken GeoFysikSamarbejdet Geologisk Institut, Aarhus Universitet

Time14:29:5014:29:4014:29:3014:29:2014:29:1014:29:0014:28:5014:28:4014:28:3014:28:2014:28:1014:28:00

Log

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o U

nit

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Average

Trapezoid shaped average

Time14:29:5014:29:4014:29:3014:29:2014:29:1014:29:0014:28:5014:28:4014:28:3014:28:2014:28:1014:28:00

Log

- N

o U

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Average

Time14:29:5014:29:4014:29:3014:29:2014:29:1014:29:0014:28:5014:28:4014:28:3014:28:2014:28:1014:28:00

Log

- N

o U

nit

1e+00

1e+01

1e+02

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Average

Page 21: Nyeste erfaringer med processering af SkyTEM data Esben Auken GeoFysikSamarbejdet Geologisk Institut, Aarhus Universitet

Trapezoid average - Sounding view

Trapezoid averageBox average, medium width

Page 22: Nyeste erfaringer med processering af SkyTEM data Esben Auken GeoFysikSamarbejdet Geologisk Institut, Aarhus Universitet

Trapezoid average - Sounding view

Trapezoid average

Box average, medium width

4 gates culled

Only 2 gates culled

High lateral resolution

Page 23: Nyeste erfaringer med processering af SkyTEM data Esben Auken GeoFysikSamarbejdet Geologisk Institut, Aarhus Universitet

Trapezoid average At each time gate data are median filtered

The standard deviation is calculated from the remaining stack

Page 24: Nyeste erfaringer med processering af SkyTEM data Esben Auken GeoFysikSamarbejdet Geologisk Institut, Aarhus Universitet

Summary Shallow part of model section/early time gates

• maximum lateral resolution is obtain with a narrow data average

• large data stack is not needed because of a high signal to noise ratio

Deep part of model section/late time gates• Wide data average suppress the background noise and

increase penetration depth.• Wide data average does not reduce the lateral resolution

Trapezoid shaped average• maximum lateral resolution • maximum penetration depth

Page 25: Nyeste erfaringer med processering af SkyTEM data Esben Auken GeoFysikSamarbejdet Geologisk Institut, Aarhus Universitet

Example - Sommersted

Page 26: Nyeste erfaringer med processering af SkyTEM data Esben Auken GeoFysikSamarbejdet Geologisk Institut, Aarhus Universitet

Coupling in high resistive areas

Page 27: Nyeste erfaringer med processering af SkyTEM data Esben Auken GeoFysikSamarbejdet Geologisk Institut, Aarhus Universitet
Page 28: Nyeste erfaringer med processering af SkyTEM data Esben Auken GeoFysikSamarbejdet Geologisk Institut, Aarhus Universitet
Page 29: Nyeste erfaringer med processering af SkyTEM data Esben Auken GeoFysikSamarbejdet Geologisk Institut, Aarhus Universitet
Page 30: Nyeste erfaringer med processering af SkyTEM data Esben Auken GeoFysikSamarbejdet Geologisk Institut, Aarhus Universitet
Page 31: Nyeste erfaringer med processering af SkyTEM data Esben Auken GeoFysikSamarbejdet Geologisk Institut, Aarhus Universitet
Page 32: Nyeste erfaringer med processering af SkyTEM data Esben Auken GeoFysikSamarbejdet Geologisk Institut, Aarhus Universitet
Page 33: Nyeste erfaringer med processering af SkyTEM data Esben Auken GeoFysikSamarbejdet Geologisk Institut, Aarhus Universitet
Page 34: Nyeste erfaringer med processering af SkyTEM data Esben Auken GeoFysikSamarbejdet Geologisk Institut, Aarhus Universitet
Page 35: Nyeste erfaringer med processering af SkyTEM data Esben Auken GeoFysikSamarbejdet Geologisk Institut, Aarhus Universitet
Page 36: Nyeste erfaringer med processering af SkyTEM data Esben Auken GeoFysikSamarbejdet Geologisk Institut, Aarhus Universitet

Width?

360 m

540 m

Page 37: Nyeste erfaringer med processering af SkyTEM data Esben Auken GeoFysikSamarbejdet Geologisk Institut, Aarhus Universitet

Coming up in the future New tools for removing data directly from the GIS map

Better automatic filters for detecting coupled data

Major revision when the new multi-moment SkyTEM system is introduced

Page 38: Nyeste erfaringer med processering af SkyTEM data Esben Auken GeoFysikSamarbejdet Geologisk Institut, Aarhus Universitet

Summary Quality of the data processing forms the basis for all

subsequent use of the data

Pitch and roll is used to:• Calculate true altitudes • Perform first order correction for non-true z-receiver and

transmitter

Coupled data are culled in the raw data - before inversion. How much to remove is dependent on the resistivity of the subsurface

Data average using trapezoid shaped filters and pruning