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1 | US DOE Geothermal Office eere.energy.gov Public Service of Colorado Ponnequin Wind Farm Geothermal Technologies Office 2015 Peer Review EGS Reservoir Simulations & Long-term Performance Modeling Project Officer: Lauren Boyd Total Project Funding,: $208,041 May 31, 2015 Principal Investigator: Rob Podogorney Presenter: Mitchell Plummer Idaho National Laboratory EGS This presentation does not contain any proprietary confidential, or otherwise restricted information.

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1 | US DOE Geothermal Office eere.energy.gov

Public Service of Colorado Ponnequin Wind Farm

Geothermal Technologies Office 2015 Peer Review

EGS Reservoir Simulations & Long-term Performance

Modeling

Project Officer: Lauren Boyd

Total Project Funding,: $208,041

May 31, 2015

Principal Investigator: Rob

Podogorney

Presenter: Mitchell Plummer

Idaho National Laboratory

EGS

This presentation does not contain any proprietary

confidential, or otherwise restricted information.

2 | US DOE Geothermal Office eere.energy.gov

Relevance/Impact of Research

• Project objectives

– Interpret RRG-9 pressure/flow response to improve understanding of

reservoir response to stimulation

– Use numerical simulation to test hypotheses about reservoir response to

high-pressure / low-temperature well stimulation

• Challenge: Reservoir creation via well stimulation is the key to EGS

development, but limited data exist regarding geothermal reservoir response to

thermal and high-pressure injections. Analysis of those data is required to

understand impact.

• Impact on EGS development: Demonstrated success of stimulation tests will

provide risk reduction necessary to motivate industry to attempt EGS.

• Innovation: Many existing codes use sequential coupling to solve THMC

problems. Code development in INL’s MOOSE framework attempts to use fully

implicit, fully coupled approach.

• Impact to GTO goals: Reducing risks of EGS development is the first step

toward industry deployment of a targeted 100+ GW of EGS.

• Integration: Analyses support the larger “EGS – Concept Testing and

Development at Raft River” under direction of Joe Moore

3 | US DOE Geothermal Office eere.energy.gov

Scientific / Technical Approach

0 500 1 103

500

1 103

1.5 103

0.01

1

100

1 104

1 106

1 108

1 1010

1 1012

1 1014

Observ ations

Theis superposition f it

Flow rate

Transmissiv ity

Storativ ity

Time (min)

Pre

ssu

re (

ps

i) &

Flo

w (

gpm

)

T (

mD

*m)

& S

/

0 500 1 103

200

400

600

800

1 103

10

100

1 103

1 104

1 105

1 106

Observ ations

Theis superposition f it

Flow rate

Transmissiv ity

Storativ ity

Time (min)

Pre

ssu

re (

ps

i) &

Flo

w (

gpm

)

T (

mD

*m)

& S

/

0 500 1 103

0

200

400

600

800

100

1 103

1 104

1 105

1 106

1 107

1 108

1 109

1 1010

1 1011

1 1012

Observ ations

Theis superposition f it

Flow rate

Transmissiv ity

Storativ ity

Time (min)

Pre

ssu

re (

ps

i) &

Flo

w (

gpm

)

T (

mD

*m)

& S

/

0 500 1 103

1.5 103

0

500

1 103

100

1 103

1 104

1 105

1 106

1 107

Observ ations

Theis superposition f it

Flow rate

Transmissiv ity

Storativ ity

Time (min)

Pre

ssu

re (

ps

i) &

Flo

w (

gpm

)

T (

mD

*m)

& S

/

1. Apply multiple methods of analysis

to provide explanations for

observed response to stimulation

– Standard well hydraulics

diagnostics

– Numerical simulation, using thermo-

hydraulic-mechanics simulations

2. Modify FALCON code to extend

implicitly coupled fracture

mechanics, fluid flow & heat

transfer capabilities

3. Develop simulations to test

hypotheses about reservoir

– What models are consistent or

inconsistent with hydraulic data?

• narrows zone permeability,

• primary fracture extent,

• response at other wells, …

4 | US DOE Geothermal Office eere.energy.gov

Inference from pumping test anlaysis

• Response to lowest pressure injection provides best estimate of

initial permeability and compressibility.

– Transmissivity (permeability x thickness) ~ 2e-14 m3 (9.7e-7 m2/s)

• Slow pressure rise suggests unrealistic compressibility,

– Suggests presence of large fracture that effectively extends wellbore to

several meters radius.

– Consistent with borehole televiewer data and temperature profiles

– Note that dilation-induced changes in permeability would act to steepen

pressure response, apparent lower storativity

0.1 1 10 1000.01

0.1

1

10

100

1 103

1 104

Radius (m)

Fra

ctu

re a

pe

rtur

e (

mm

)

rwell

m

1 10 100 1 103

0.01

0.1

1

10

Radius (m)

Fra

ctu

re a

pe

rtur

e (

mm

)rwell

m

5 | US DOE Geothermal Office eere.energy.gov

2.4e-8 m Pa-1

4.8e-8 m Pa-1

1.2e-7 m Pa-1

2.4e-7 m Pa-1

Diffusivity impact, uncertain S

1-psi response contours, 100 gpm, 2 yr

Diffusivity impact, uncertain S

S0 x2 x5 x10

6 | US DOE Geothermal Office eere.energy.gov

FALCON improvements

– Developed solution method for use of lower-

dimension domains in higher dimension

models (eg. 2D fracture in 3D domain)

– Added reconstructed discontinuous

Galerkin method for high Peclet-number

problems

– Replaced mechanics with tensor mechanics

approach

– Developed well model

– Developing cohesive zone

model for fracturing

approach in finite elements

7 | US DOE Geothermal Office eere.energy.gov

Temperature anomaly analysis

• Small-scale, high-resolution heat

transport simulations to explain

DTS temperature anomalies in

cased portion of RRG-9

• Helped resolved concern that T

anomaly suggested casing leak

4/03 3/15

3/06

3/24

4/11

Bottom of casing

Bottom of casing

8 | US DOE Geothermal Office eere.energy.gov

Injection test analysis on the edge of precision, 2014 SULI student project

Wellhead pressure

Injection rate

Pre

ssu

re [

psi

]

• Plant, wellhead and

calculated bottomhole

pressure out of phase

with flow rate variation

• Hypothesize

uncompensated

temperature effect in

pressure sensor

• New BHP sensor

4/8/15

Time [days]

Flo

w [

gp

m]

• Used DTS data to calculate precise bottom-hole pressure (BHP) (sensor failed)

• Corrected for T-dependent density & hydrostatic head, pressure loss via flow, …

• Wellhead flow and pressure data suggest diurnal fluctuation that could be used

for transient pumping test analysis, but

Reduce residual between observed pressure and modeled pressure and

calculate hydraulic parameters

9 | US DOE Geothermal Office eere.energy.gov

Permeability response to thermal effects

• Numerical simulations of discrete

fracture response to thermal

stimulation demonstrate krel

dependence on unsupported

fracture length & T

• 2D simulations demonstrate how

thermal effects can reproduce

observed long-term evolution of

injectivity

10 | US DOE Geothermal Office eere.energy.gov

Fluid pressure Horizontal displacement field

(& fracture network colored by permeability)

DEM simulations of stress and permeability response

Short

ly a

fter

inje

ction s

tart

S

tea

dy s

tate

T

ime

11 | US DOE Geothermal Office eere.energy.gov

Shear slipping vs. opening?

Displacement vector fields

X

Y

DEM simulations of stress and permeability response

12 | US DOE Geothermal Office eere.energy.gov

Accomplishments, Results and Progress

• Applied pumping test analysis methods to interpret injection test pressure / flow response

• Used numerical simulation of heat transport in a well to test hypotheses about temperature

anomalies in well

• Made numerous improvements to FALCON for geothermal reservoir simulations

• Worked with EGI Ph.D. student to: – Develop FALCON modules that automate importing of FRACMAN-generated fracture networks

– Develop reservoir scale models that can reproduce observed pressure/flow response

• Worked with SULI student to develop a well injection model to simplify point sources in FALCON

• Worked with SULI student to use DTS data to calculate precise bottomhole pressure and

examine diurnal pressure/flow fluctuation

• Used discrete element fracture models, coupled to flow network model, to test hypotheses about

shearing response to thermal and high-pressure stimulation

• Developed discrete fracture THM models, using procedure developed by Rutqvist (1998) to

simulate elastic response of fractures to hydraulic jacking tests

Original Planned Milestone/ Technical

Accomplishment

Actual Milestone/Technical Accomplishment

Date Completed

Quarterly reports

Reports describing model modifications, analyses,

and simulation progress

Quarterly

Peer-reviewed manuscript on well hydraulics and

measurements

Conference proceedings papers February, 2015

13 | US DOE Geothermal Office eere.energy.gov

Accomplishments, Results and Progress

Technical challenges

• Lack of measured response at other wells (pressure, flow, tracer

return)

– Pumping test analysis without observation wells

• Non-uniqueness in fitted models

– eg. Constant flow at constant pressure after ~1.5 days

• Nearby connection to higher permeability zone

• Alteration to spherical flow regime, reflecting pressure diffusion into

adjacent hydrogeologic units

• Fracture opening; proximal drawdown decreases with pressure diffusion

14 | US DOE Geothermal Office eere.energy.gov

Future Directions

• Analyses, for hypothetical EGS and Raft River

case study, provide improved understanding of

reservoir response to well stimulation

• Continuing work focuses on 3D THM models and

large-scale reservoir properties that could

reproduce principle features of the observed

hydraulic response

– Use results of previous analyses to determine

appropriate scale and features of 3D THM model

– Summer, 2015: Work with EGI Ph.D. student, Jacob

Bradford to develop alternative 3-D THM models,

including single fracture zone response to thermal

and high-pressure injection effects

Milestone Status & Expected Completion Date

Peer-reviewed manuscript on well hydraulics

and measurements

May 1, 2015 (delayed from 2/28/15)

Peer-reviewed manuscript on reservoir

modeling

July 31, 2015

• Continue FALCON simulations examining relationship between flow and thermal strain

• Continue DEM simulations exploring fracture distribution effect on stress/strain & flow

15 | US DOE Geothermal Office eere.energy.gov

• Simulations and analyses have supported Raft River stimulation effort

– Design of stepped rate, hydraulic jacking, tests

– Implications of temperature anomalies in cased well section

• Work to date focused on implications of well flow/pressure response

– Calculated hydraulic properties and apparent response to stimulation

– Apparent radial flow regime at <1-day timescale

– Steady-state flow after ~1.5 days suggests fracture opening at 280 psi (~2

Mpa), or nearby high-k zone

– No evidence of proximal impermeable boundary (Narrows zone)

– Exploration of likely temperature-dependent injectivity response is consistent

with range observed in thermal stimulation efforts

• Current work

– Use discrete fracture THM model to simulate near-well fracture response

– Apply THM with mechanics to simulate permeability response to effective

fracture behavior

– Reproduce long-term pressure/flow response with THM models

Summary

Summarize the

key points you

wish the

reviewers and

the audience to

take away from

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