we study the state and evolu on of pressure, stress ...€¦ · geofluids co-directors 2013...

1
and silt content control permeability, compressibility Velocity loading and unloading curve Preparing samples understand mudrock behavior Major current experimental eort is developing ability to measure shear and compressional velocity in mudstones log and seismic We characterize geology, pressure, The Auger Basin is a ‘protected trap’: the shallowest structure is currently leaking; this allows trap integrity at subsidiary structures (Macaroni and Auger). We use direct measurements of salinity and temperature to expelling from vents. Dip image. Red marks oil slick on surface from Radar Ursa Vent We are currently working on modeling salt diapirism Developing a new geomechanical modeling approach that goes beyond current approaches Geomechanical modeling of stress around salt at Mad Dog Elevated horizontal stresses within basins and in front of the salt: 90% to 110% of the overburden. stress, and borehole integrity in salt regimes 0 50 100 150 200 250 300 10 100 1000 10000 S-wave Velocity (m/s) Ver cal Eec ve Stress (kPa) m = 30.4 m = 21.2 13 Graduate Students 4 Post-docs & Research • 4 Sta/Technical Support Jack Germaine Civil and Environmental Engineering, MIT Peter Flemings Professor, Jackson School of Geosciences, U.T. Experimental Field Study Poromechanical Modeling 1. Experimental: (~15,000 psi). 2. Poromechanical Modeling: 3. Field Study: Contacts: p[email protected], [email protected], [email protected] Transferring Online GeoFluids database Deliverables: Online database with experimental results Spread sheets, handbooks Geotechnical Engineers Example 2: Pore Pressure and Trap Integrity in the Auger Basin Vertical effective stress, v (MPa) 20 18 16 14 12 10 8 6 4 2 0 0.2 0.3 0.4 0.5 0.6 Porosity, n 10 -20 10 -16 Vertical permeability, k (m 2 ) 10 -18 59% clay 34% clay 59% clay 34% clay We study the state and evolu on of pressure, stress, deforma on, and uid migra on through experiments, models, and eld study. We are dedicated to producing innova ve concepts that couple geology and uid ow. GeoFluids Co-Directors 2013 Consortium Meeting (Feb 21-22) 89 attendees representing 11 different companies

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Page 1: We study the state and evolu on of pressure, stress ...€¦ · GeoFluids Co-Directors 2013 Consortium Meeting (Feb 21-22) 89 attendees representing 11 different companies. Title:

and silt content control permeability, compressibility

Velocity loading and unloading curve

Preparing samples

understand mudrock behavior

• Major current experimental effort is developing ability to measure shear and compressional velocity in mudstones

log and seismic

We characterize geology, pressure,

The Auger Basin is a ‘protected trap’: the shallowest structure is currently leaking; this allows trap integrity at subsidiary structures (Macaroni and Auger).

We use direct measurements of salinity and temperature to

expelling from vents.

Dip image. Red marks oil slick on surface from Radar

Ursa Vent

We are currently working on modeling salt diapirism

• Developing a new geomechanical modeling approach that goes beyond current approaches

Geomechanical modeling of stress around salt at Mad Dog

• Elevated horizontal stresses within basins and in front of the salt: 90% to 110% of the overburden.

stress, and borehole integrity in salt regimes

0

50

100

150

200

250

300

10 100 1000 10000

S-w

ave

Velo

city

(m/s

)

Ver cal Effec ve Stress (kPa)

m = 30.4

m = 21.2

• 13 Graduate Students• 4 Post-docs & Research

• 4 Staff/Technical Support

Jack Germaine

Civil and Environmental Engineering, MIT

Peter FlemingsProfessor, Jackson School of

Geosciences, U.T.

ExperimentalField StudyPoromechanical Modeling

1. Experimental: (~15,000 psi).2. Poromechanical Modeling:

3. Field Study:

Contacts: [email protected], [email protected], [email protected]

Transferring

Online GeoFluids database

Deliverables:

• Online database with experimental results

• Spread sheets, handbooks

Geotechnical Engineers

Example 2: Pore Pressure and Trap Integrity in the Auger Basin

Vert

ical

effe

ctiv

e st

ress

, ’ v

(MPa

)

20

18

16

14

12

10

8

6

4

2

00.2 0.3 0.4 0.5 0.6

Porosity, n10-20 10-16

Verticalpermeability, k (m2)

10-18

59% clay

34% clay59% clay

34% clay

We study the state and evolu on of pressure, stress, deforma on, and fluid migra on through experiments, models, and field study. We are dedicated to producing innova ve

concepts that couple geology and fluid flow.

GeoFluids Co-Directors

2013 Consortium Meeting (Feb 21-22)89 attendees representing

11 different companies