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EOSC 350 slide 1 The University of British Columbia Geophysical Inversion Facility http://gpg.geosci.xyz EOSC 350 : Environmental, Geotechnical and Exploration Geophysics I September 2016

The University of British Columbia Geophysical … · Summary For Applied Geophysics • Multi-disciplinary: – brings together mathematics, physics, computer science, geology, engineering

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EOSC 350 slide 1

The University of British Columbia Geophysical Inversion Facility

http://gpg.geosci.xyz

EOSC 350 : Environmental, Geotechnical and Exploration

Geophysics I

September 2016

EOSC 350 slide 2

Outline:

• Introduction: Example problems – Environmental, geotechnical, resource exploration

• Geophysical surveys and data images

• Inversion

• Mineral exploration example

• Summary/discussion

EOSC 350 slide 3

Environmental: UXO

• Military proving grounds • Regions of conflict • Avalanche control

http://www.nohowinc.com/ http://www.dma.state.mn.us/

http://www.centennialofflight.gov

EOSC 350 slide 4

Various types of UXO

EOSC 350 slide 5

Environmental: How do we find UXO?

?

EOSC 350 slide 6

Geotechnical: A Canadian potash mining

EOSC 350 slide 7

Geotechnical problem

• Slide: water gushing into the mine

EOSC 350 slide 8

Mineral exploration

• What do we have?

Map of surface geology

EOSC 350 slide 9

?

Mineral exploration

• What do we want? – Subsurface structures and materials

Map of surface geology

Subsurface: Physical Properties and Contrasts

Source Data

Solutions … Geophysics

EOSC 350 slide 11

Geophysics: Sources

• On the ground

• In the air

• Inside the earth

EOSC 350 slide 12

Geophysics: Physical Properties

–Density

–Magnetic susceptibility

–Electrical conductivity

–Chargeability

–Electrical permittivity

–Elastic moduli

Important to have

contrasts in physical

Properties.

EOSC 350 slide 13

Geophysics: Surveys and Data

• On the ground

• In the air

• Inside the earth

SEG Distinguished Lecture slide 14

How do we distinguish bodies?

• Characterize materials by physical properties:

– Density

– Magnetic susceptibility

– Electrical conductivity

– Chargeability

– Electrical permittivity

– Elastic moduli

• If we know the physical properties then we might be able to answer our question…

EOSC 350 slide 15

Physical properties

• UXO: – Electrical conductivity and magnetic susceptibility

• Water (at potash mine): – Electrical conductivity: high if it has dissolved salt

• Minerals: – magnetic susceptibility (at Raglan) – electrical conductivity, – chargeability, – density

EOSC 350 slide 16

Environmental : Magnetic Survey

TM4

Ferrex

nT

-200

-100

0

100

200

Easting (m)

Nor

thin

g (m

)

0 10 20 30 40 50 0

10

20

30

40

50

EOSC 350 slide 17

mortar Popcan Frag 76mm

Operational Task: Dig

EOSC 350 slide 18

100 metres Approximate Scale

3.5 KM of Electrical Resistance Imaging along tunnels

Geotechnical survey data (potash mine)

NTS

UNDERGROUND 2D ERI GOCAD VISUALIZATION VIEW FROM NE

FIGURE 7

PROJECT No. DESIGN CADD CHECK

REVIEW

FILE No. ---- REV. SCALE

TITLE

PROJECT

06OCT03 28SEP04

Max CB/Max

04-1419-007

EOSC 350 slide 19

WEST EAST

143 m 148 m 155 m 159 m 163 m

Ground Penetrating Radar: Drill-holes with no water

Water found

Direct Current Resistivity image: Water found here

Two geophysical surveys along tunnels

EOSC 350 slide 20

Our mineral exploration example • Data: magnetic measurements. • Image: map of anomalies in earth’s field.

Map of surface geology

Image provides some information … but not enough.

Total field aeromagnetics

EOSC 350 slide 21

Getting more from data … • Image provides some information but not enough.

Total field

aeromagnetics

We want a “model” of subsurface materials. Invert the data

EOSC 350 slide 22

What is Inversion?

Goal: Estimate the Earth model that generated the data

Model

?

Data

Airborne, surface or borehole

measurements are data

Inversion processing

EOSC 350 slide 23

Inversion procedure:

• Divide Earth into cells (each with fixed size and unknown value).

• Inversion: find values for cells such that data are explained.

• Use mathematical optimization theory.

• Difficulties: – Solution is non-unique. – Computationally demanding.

Measurements = Data Pre-processing Inversion

Physical property distributions = MODELS

Prior information

3D, and ~ 105 cells

EOSC 350 slide 24

Geophysical inversion is analogous to medical imaging

• We need a 3D image for pinpointing a target or making a final assessment.

Image of a brain based on MRI measurements.

Image of an ore body based on magnetic field measurements.

EOSC 350 slide 25

Viewing an inversion result

• 3D volume can be viewed many ways. Here: – Data on top – Pixels showing material property value:

visible along the slice. – Isosurface:

hide all cells with values less than a chosen value.

EOSC 350 slide 26

Exploration at Raglan: Inversion image

? ?

Invert data => 3D images of property distribution.

Total field aeromagnetic data

EOSC 350 slide 27

Framework for Applied Geophysics: 7 Steps

• Setup: What is the question to be answered?

• What are the diagnostic physical properties?

• Choose survey and design data acquistion.

• Data collection

• Processing of field data

• Interpretation

• Synthesis

EOSC 350 slide 28

Mineral Exploration: The “Cluny” copper/lead/zinc deposit

Physical Properties of the Rocks

Rock unit Conductivity Chargeability Adjacent shale high low

Host volcanic low-moderate low rocks

Mineral zone: - Siltstone containing (Cu, Pb, Zn) - Galena, pyrrhotite, pyrite, sphalerite

moderate high

EOSC 350 slide 29

Electrical survey: concept

DC survey Data: ”pseudosection”

EOSC 350 slide 30

Data set #1: Apparent resistivity, dipole - pole.

Electrical survey: data • Eight survey lines • Two survey configurations.

Easting (m) Easting (m)

mS/m

Easting (m) Easting (m)

mS/m

Data set #2: Apparent conductivity, pole - dipole.

10500 11500 12500

13000

14000

15000

16000

400

450

500

Easting (m)

Nor

thin

g (m

)

Surface topography: Elevation Meters

10 lines surveyed

EOSC 350 slide 31

3D conductivity model from 3D inversion:

Click image to see the AVI movie

EOSC 350 slide 32

IP data: what is being measured?

Source Current (Amps) Measured Voltage (Volts)

Vσ Vs(t)

Vη Measurement is: How easily does material retain charge.

Non-zero area occurs because charges took time to equilibrate.

EOSC 350 slide 33

Apparent chargeability, dipole - pole.

3D induced polarization

10500 11500 12500

13000

14000

15000

16000

400

450

500

Easting (m)

Nor

thin

g (m

)

Surface topography: Elevation Meters

10 lines surveyed

EOSC 350 slide 34

3D conductivity and chargeability: Cluny

Volume rendered resistivity model Volume rendered chargeability model

EOSC 350 slide 35

Summary For Applied Geophysics

• Multi-disciplinary: – brings together mathematics, physics, computer science,

geology, engineering into a single context.

• Requires team work and ability to communicate among different disciplines

• Two communication tools are:

– Expressing problems in terms of physical properties – Images

EOSC 350 slide 36

Framework for Applied Geophysics: 7 Steps

• Setup: What is the question to be answered?

• What are the diagnostic physical properties?

• Choose survey and design data acquistion.

• Data collection

• Processing of field data

• Interpretation

• Synthesis

• Read the paper: “A Geophysical Journey around Ireland” by James Hodgson • Download the TBL and complete it by evaluating one of the case

histories in the paper. This is handed in at the beginning of the next class.

Upcoming events: • Quiz involving “Foundations”

• Team exercise: Physical properties and case histories from

Ireland. EOSC 350

slide 37

Homework