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Nye data – nye muligheder? Esben Auken, Anders V. Christiansen, Nikolaj Foged and Kurt Sørensen...

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Nye data – nye muligheder? Esben Auken , Anders V. Christiansen, Nikolaj Foged and Kurt Sørensen droGeophysics Group partment of Earth Sciences, University of Aarhus, Denmark w.hgg.au.dk
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Page 1: Nye data – nye muligheder? Esben Auken, Anders V. Christiansen, Nikolaj Foged and Kurt Sørensen HydroGeophysics Group Department of Earth Sciences, University.

Nye data – nye muligheder?

Esben Auken, Anders V. Christiansen, Nikolaj Foged and Kurt Sørensen

HydroGeophysics GroupDepartment of Earth Sciences, University of Aarhus, Denmarkwww.hgg.au.dk

Page 2: Nye data – nye muligheder? Esben Auken, Anders V. Christiansen, Nikolaj Foged and Kurt Sørensen HydroGeophysics Group Department of Earth Sciences, University.

Indhold Hvordan ser x-data ud?

Modelanalyser – motivationen

Problemerne med måling af vinkel – “forurening” af x-signalet

Inversion

Page 3: Nye data – nye muligheder? Esben Auken, Anders V. Christiansen, Nikolaj Foged and Kurt Sørensen HydroGeophysics Group Department of Earth Sciences, University.

Time [s]1e-06 1e-05 1e-04 1e-03 1e-02

dB

/dt

[V/(

m^2

)]

1e-10

1e-09

1e-08

1e-07

1e-06

1e-05

1e-04

Time [s]1e-06 1e-05 1e-04 1e-03 1e-02

dB

/dt

[V/(

m^2

)]

1e-10

1e-09

1e-08

1e-07

1e-06

1e-05

1e-04

Theoretical z-response

100 m 10 m

30 m 20 m

80 m 70 m

10 m

Model z-component data

Page 4: Nye data – nye muligheder? Esben Auken, Anders V. Christiansen, Nikolaj Foged and Kurt Sørensen HydroGeophysics Group Department of Earth Sciences, University.

Time [s]1e-06 1e-05 1e-04 1e-03 1e-02

dB

/dt

[V/(

m^2

)]

1e-10

1e-09

1e-08

1e-07

1e-06

1e-05

1e-04

Theoretical z- and x-response

Late time x ∞ t-3

Late time z ∞ t-2.5

x-component signal level is 5 – 8 times smaller than z-component

x- and z-component

100 m 10 m

30 m 20 m

80 m 70 m

10 m

Model

Page 5: Nye data – nye muligheder? Esben Auken, Anders V. Christiansen, Nikolaj Foged and Kurt Sørensen HydroGeophysics Group Department of Earth Sciences, University.

Model Sensitivity Analysis – model 2 White: z-component alone

Grey: x- and z-component

Black: x- and z-component, x with 60 kHz low-pass filter

Page 6: Nye data – nye muligheder? Esben Auken, Anders V. Christiansen, Nikolaj Foged and Kurt Sørensen HydroGeophysics Group Department of Earth Sciences, University.

Model Sensitivity Analysis – model 1 White: z-component alone

Grey: x- and z-component

Black: x- and z-component, x with 60 kHz low-pass filter

Page 7: Nye data – nye muligheder? Esben Auken, Anders V. Christiansen, Nikolaj Foged and Kurt Sørensen HydroGeophysics Group Department of Earth Sciences, University.

Model Sensitivity Analysis – model 3 White: z-component alone

Grey: x- and z-component

Black: x- and z-component, x with 60 kHz low-pass filter

Page 8: Nye data – nye muligheder? Esben Auken, Anders V. Christiansen, Nikolaj Foged and Kurt Sørensen HydroGeophysics Group Department of Earth Sciences, University.

Location of first gate – 11 or 18 micros? White: z-component alone

Grey: x- and z-component

Black: x- and z-component, x with 60 kHz low-pass filter

Page 9: Nye data – nye muligheder? Esben Auken, Anders V. Christiansen, Nikolaj Foged and Kurt Sørensen HydroGeophysics Group Department of Earth Sciences, University.

The 3 Challenges for exploiting x-data1. Signal to noise level

• Altitude dependency• Natural background noise

2. “Contamination” of the x-data due to tilt of the Tx-frame

3. Timing of the instrumentation and measurement of the tilt

Page 10: Nye data – nye muligheder? Esben Auken, Anders V. Christiansen, Nikolaj Foged and Kurt Sørensen HydroGeophysics Group Department of Earth Sciences, University.

Altitude Dependency

Time [s]1e-06 1e-05 1e-04 1e-03 1e-02

dB

/dt

[V/(

m^2

*s)]

1e-09

1e-08

1e-07

1e-06

1e-05

1e-04

1e-03

1e-02

Time [s]1e-06 1e-05 1e-04 1e-03 1e-02

dB

/dt

[V/(

m^2

*s)]

1e-09

1e-08

1e-07

1e-06

1e-05

1e-04

1e-03

1e-02z-data x-data

Altitude: 1 m

Altitude: 1 m

Page 11: Nye data – nye muligheder? Esben Auken, Anders V. Christiansen, Nikolaj Foged and Kurt Sørensen HydroGeophysics Group Department of Earth Sciences, University.

Time [s]1e-06 1e-05 1e-04 1e-03 1e-02

dB

/dt

[V/(

m^2

*s)]

1e-09

1e-08

1e-07

1e-06

1e-05

1e-04

1e-03

1e-02

Time [s]1e-06 1e-05 1e-04 1e-03 1e-02

dB

/dt

[V/(

m^2

*s)]

1e-09

1e-08

1e-07

1e-06

1e-05

1e-04

1e-03

1e-02

Altitude Dependencyz-data x-data

Altitude: 1 m 18 m

Altitude: 1 m 18 m

Page 12: Nye data – nye muligheder? Esben Auken, Anders V. Christiansen, Nikolaj Foged and Kurt Sørensen HydroGeophysics Group Department of Earth Sciences, University.

Time [s]1e-06 1e-05 1e-04 1e-03 1e-02

dB

/dt

[V/(

m^2

*s)]

1e-09

1e-08

1e-07

1e-06

1e-05

1e-04

1e-03

1e-02

Time [s]1e-06 1e-05 1e-04 1e-03 1e-02

dB

/dt

[V/(

m^2

*s)]

1e-09

1e-08

1e-07

1e-06

1e-05

1e-04

1e-03

1e-02

Altitude Dependencyz-data x-data

Altitude: 1 m 18 m

29 m – operating altitude

Altitude: 1 m 18 m 29 m

Page 13: Nye data – nye muligheder? Esben Auken, Anders V. Christiansen, Nikolaj Foged and Kurt Sørensen HydroGeophysics Group Department of Earth Sciences, University.

The 3 Challenges for Exploiting x-data1. Signal to noise level

• x-signal is 5 – 8 times smaller than z-signal• x-signal decreases faster with altitude compared to the z-

signal• x-noise is 5 – 10 times larger than z-noise

2. “Contamination” of the x-data due to tilt of the Tx-frame

3. Timing of the instrumentation and measurement of the tilt

Page 14: Nye data – nye muligheder? Esben Auken, Anders V. Christiansen, Nikolaj Foged and Kurt Sørensen HydroGeophysics Group Department of Earth Sciences, University.

The 3 Challenges for Exploiting x-data1. Signal to noise level

• x-signal is 5 – 8 times smaller than z-signal• x-signal decreases faster with altitude compared to the z-

signal• x-noise is 5 – 10 times larger than z-noise

2. “Contamination” of the x-data due to tilt of the Tx-frame

3. Timing of the instrumentation and measurement of the tilt

Page 15: Nye data – nye muligheder? Esben Auken, Anders V. Christiansen, Nikolaj Foged and Kurt Sørensen HydroGeophysics Group Department of Earth Sciences, University.

z-component

x-component

Ground

Tx-frame

z-Rx

Ground

x-Rx

Tilt – Normal Situation

Page 16: Nye data – nye muligheder? Esben Auken, Anders V. Christiansen, Nikolaj Foged and Kurt Sørensen HydroGeophysics Group Department of Earth Sciences, University.

Positive Tilt of the Tx-frame

z-response adds signal to the x-response

The x-response caluclated as: Bxtotal = Bx + sin(Tilt) Bz

z-contamination

x-component

GroundGround

Page 17: Nye data – nye muligheder? Esben Auken, Anders V. Christiansen, Nikolaj Foged and Kurt Sørensen HydroGeophysics Group Department of Earth Sciences, University.

GroundGround

”Contaminated” x-response – Positive Tilt

Time [s]1e-06 1e-05 1e-04 1e-03

1.0e-11

1.0e-10

1.0e-09

1.0e-08

1.0e-07

1.0e-06

1.0e-05x-data

Tilt: 0 deg

Page 18: Nye data – nye muligheder? Esben Auken, Anders V. Christiansen, Nikolaj Foged and Kurt Sørensen HydroGeophysics Group Department of Earth Sciences, University.

GroundGround

”Contaminated” x-response – Positive Tilt

Time [s]1e-06 1e-05 1e-04 1e-03

1.0e-11

1.0e-10

1.0e-09

1.0e-08

1.0e-07

1.0e-06

1.0e-05x-data

5 deg

Tilt: 0 deg

Page 19: Nye data – nye muligheder? Esben Auken, Anders V. Christiansen, Nikolaj Foged and Kurt Sørensen HydroGeophysics Group Department of Earth Sciences, University.

GroundGround

”Contaminated” x-response – Positive Tilt

Time [s]1e-06 1e-05 1e-04 1e-03

1.0e-11

1.0e-10

1.0e-09

1.0e-08

1.0e-07

1.0e-06

1.0e-05x-data

10 deg 5 deg

Tilt: 0 deg

9 usefull gates

Page 20: Nye data – nye muligheder? Esben Auken, Anders V. Christiansen, Nikolaj Foged and Kurt Sørensen HydroGeophysics Group Department of Earth Sciences, University.

Negative Tilt of the Tx-frame

z-response subtracts from the x-response

z-contamination

GroundGround

x-component

Page 21: Nye data – nye muligheder? Esben Auken, Anders V. Christiansen, Nikolaj Foged and Kurt Sørensen HydroGeophysics Group Department of Earth Sciences, University.

GroundGround

”Contaminated” x-response – Negative Tilt

Time [s]1e-06 1e-05 1e-04 1e-03

1.0e-11

1.0e-10

1.0e-09

1.0e-08

1.0e-07

1.0e-06

1.0e-05x-data

Tilt: 0 deg

Page 22: Nye data – nye muligheder? Esben Auken, Anders V. Christiansen, Nikolaj Foged and Kurt Sørensen HydroGeophysics Group Department of Earth Sciences, University.

GroundGround

”Contaminated” x-response – Negative Tilt

Time [s]1e-06 1e-05 1e-04 1e-03

1.0e-11

1.0e-10

1.0e-09

1.0e-08

1.0e-07

1.0e-06

1.0e-05x-data

Tilt: 0 deg -5 deg

Page 23: Nye data – nye muligheder? Esben Auken, Anders V. Christiansen, Nikolaj Foged and Kurt Sørensen HydroGeophysics Group Department of Earth Sciences, University.

GroundGround

Time [s]1e-06 1e-05 1e-04 1e-03

1.0e-11

1.0e-10

1.0e-09

1.0e-08

1.0e-07

1.0e-06

1.0e-05

”Contaminated” x-response – Negative Tilt

x-data

Tilt: 0 deg -5 deg -10 deg

3 - 4 usefull gates

Page 24: Nye data – nye muligheder? Esben Auken, Anders V. Christiansen, Nikolaj Foged and Kurt Sørensen HydroGeophysics Group Department of Earth Sciences, University.

The 3 Challenges for Exploiting x-data1. Signal to noise level

• x-signal is 5 – 8 times smaller than z-signal• x-signal decreases faster with altitude compared to the z-signal• x-noise is 5 – 10 times larger than z-noise

2. “Contamination” of the x-data due to tilt of the Tx-frame• The tilt of the frame adds or subtracts signal form the x-

response• Addition of signal is preferred from subtraction of signal • Tilt must treated as an inversion parameter - it can not be

measured with the desired accuracy• Does (probably) not need a priori information for the tilt

3. Timing of the instrumentation and measurement of the tilt

Page 25: Nye data – nye muligheder? Esben Auken, Anders V. Christiansen, Nikolaj Foged and Kurt Sørensen HydroGeophysics Group Department of Earth Sciences, University.

The 3 Challenges for Exploiting x-data1. Signal to noise level

• x-signal is 5 – 8 times smaller than z-signal• x-signal decreases faster with altitude compared to the z-signal• x-noise is 5 – 10 times larger than z-noise

2. “Contamination” of the x-data due to tilt of the Tx-frame• The tilt of the frame adds or subtracts signal form the x-

response• Addition of signal is preferred from subtraction of signal • Tilt must treated as an inversion parameter - it can not be

measured with the desired accuracy• Does (probably) not need a priori information for the tilt

3. Timing of the instrumentation and measurement of the tilt

Page 26: Nye data – nye muligheder? Esben Auken, Anders V. Christiansen, Nikolaj Foged and Kurt Sørensen HydroGeophysics Group Department of Earth Sciences, University.

Timing of the Front Gate

Time [s]1e-06 1e-05 1e-04 1e-03

100.0

1000.0x-data converted to apparent resistivity

Front Gate in 7.8 µs

Front Gate preventing the primary signal to saturate the receiver – opens for the signal just before the first time-gate

Coil Front Gate Receiver

100 m 10 m

30 m 20 m

80 m 70 m

10 m

Model

Page 27: Nye data – nye muligheder? Esben Auken, Anders V. Christiansen, Nikolaj Foged and Kurt Sørensen HydroGeophysics Group Department of Earth Sciences, University.

Time [s]1e-06 1e-05 1e-04 1e-03

100.0

1000.0

Timing of the Front Gate

Front Gate in 8.8 µs

300 nSec shift corresponds to approx. 3 % shift of the first gate

x-data converted to apparent resistivity

Front Gate in 7.8 µs

Coil Front Gate Receiver

100 m 10 m

30 m 20 m

80 m 70 m

10 m

Model

Front Gate preventing the primary signal to saturate the receiver – opens for the signal just before the first time-gate

Page 28: Nye data – nye muligheder? Esben Auken, Anders V. Christiansen, Nikolaj Foged and Kurt Sørensen HydroGeophysics Group Department of Earth Sciences, University.

The 3 Challenges for Exploiting x-data1. Signal to noise level

• x-signal is 5 – 8 times smaller than z-signal• x-signal decreases faster with altitude compared to the z-signal• x-noise is 5 – 10 times larger than z-noise

2. “Contamination” of the x-data due to tilt of the Tx-frame• The tilt of the frame adds or subtracts signal form the x-response• Addition of signal is preferred from subtraction of signal • Tilt must treated as an inversion parameter as it can not be

measured with the desired accuracy• Does probably not need a priori information from the device

3. Timing of the instrumentation and measurement of the tilt• The timing is accurate within 200 nanosec - OK!• Accurate measurement of the tilt while flying

Page 29: Nye data – nye muligheder? Esben Auken, Anders V. Christiansen, Nikolaj Foged and Kurt Sørensen HydroGeophysics Group Department of Earth Sciences, University.

Inversion Methodology LCI – soundings

Profile

TE M soundings - m odelsz z . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . z

Page 30: Nye data – nye muligheder? Esben Auken, Anders V. Christiansen, Nikolaj Foged and Kurt Sørensen HydroGeophysics Group Department of Earth Sciences, University.

Inversion Methodology LCI – soundings

Profile

x x . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . x

TE M soundings - m odelsz z . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . z

Page 31: Nye data – nye muligheder? Esben Auken, Anders V. Christiansen, Nikolaj Foged and Kurt Sørensen HydroGeophysics Group Department of Earth Sciences, University.

Inversion Methodology LCI – soundings

Profile

TE M soundings - m odels

x

z

x . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . x

z . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . z

Page 32: Nye data – nye muligheder? Esben Auken, Anders V. Christiansen, Nikolaj Foged and Kurt Sørensen HydroGeophysics Group Department of Earth Sciences, University.

Inversion Methodology LCI – soundings

n

n+1

n

n+1

n

n+1

d n d

n+1

d n d

n+1

Profile

TEM soundings - m odels

x

z

x . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . x

z . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . z

n+2

n+2

n+2

d n+2

d n+2

x-m odel z-m odel x-m odel

Page 33: Nye data – nye muligheder? Esben Auken, Anders V. Christiansen, Nikolaj Foged and Kurt Sørensen HydroGeophysics Group Department of Earth Sciences, University.

Inversion Methodology Damped least squares scheme, modeling of system

transfer function• Low pass filters, front gate, turn-on and turn-off exponential

ramps• Flight altitude and tilt are constrained parameters

The model is parameterized or smooth 1D

n

n+1

n

n+1

n

n+1

d n d

n+1

d n d

n+1

Profile

TEM soundings - m odels

x

z

x . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . x

z . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . z

n+2

n+2

n+2

d n+2

d n+2

x-m odel z-m odel x-m odel

Page 34: Nye data – nye muligheder? Esben Auken, Anders V. Christiansen, Nikolaj Foged and Kurt Sørensen HydroGeophysics Group Department of Earth Sciences, University.

Data

Page 35: Nye data – nye muligheder? Esben Auken, Anders V. Christiansen, Nikolaj Foged and Kurt Sørensen HydroGeophysics Group Department of Earth Sciences, University.

Diskussion og konklusion x-data tilfører information om den overfladenære geologi

Ved to-moment-system kompenserer x-data for, at første gate er i 16 microsek.

Ved ét-moment-system (første gate i 10 microsek.) tilfører x-data opløslighed i betragetligt omfang.

x-signalet kan anvendes, hvis ikke modstanden er for høj • Kræver at flyvehøjden er omkring 30 m (eller lavere)• Kræver nøjagtig måling af vinkel og kalibrering af

instrumenterne

Giver ikke ekstra arbejde i felten, men giver ekstra processerings- og tolkningsarbejde

Stadigvæk på forskningsstadiet


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