Pressure-Anomaly Based Leakage Detection · 2015-09-02 · Pressure-Anomaly Based Leakage Detection...

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Transcript of Pressure-Anomaly Based Leakage Detection · 2015-09-02 · Pressure-Anomaly Based Leakage Detection...

Page 1: Pressure-Anomaly Based Leakage Detection · 2015-09-02 · Pressure-Anomaly Based Leakage Detection JP Nicot, Mehdi Zeidouni, Alex Sun, and K.-Won Chang Bureau of Economic Geology
Page 2: Pressure-Anomaly Based Leakage Detection · 2015-09-02 · Pressure-Anomaly Based Leakage Detection JP Nicot, Mehdi Zeidouni, Alex Sun, and K.-Won Chang Bureau of Economic Geology

Pressure-Anomaly Based Leakage Detection

JP Nicot, Mehdi Zeidouni,Alex Sun, and K.-Won Chang

Bureau of Economic GeologyJackson School of GeosciencesThe University of Texas at Austin

Progress Review of STAR Grant Researchon Carbon Geosequestration

Washington, D.C. – January 7, 2013

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“Expert-Based Development of a Standard in CO2 Sequestration Monitoring Technology”

•STAR R834384 addresses the requirement for a GS project to develop a monitoring plan (UIC Class VI)

• focuses on 5 well-known fields:– Soil gas approaches– Groundwater monitoring and tracers– Pressure and temperature monitoring– Well-based techniques– Seismic techniques

•Above-Zone Monitoring Intervals (AZMI) measurements at Cranfield, MS and other fields

• In-Zone IZ monitoring

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surface

Surface casing

Cemented in

Cement to isolate

Injection zone

AZMI Above Zone Monitoring IntervalTime

Pre

ssur

e

Injection zone

AMZI

Confining = No fluid communication

Using AZMI pressure to assess storage permanence

Courtesy Sue Hovorka

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Pressure Monitoring

CO2 Injection Zone

Above-Zone Monitoring Interval (AZMI) –leakage detection

Within Injection Zone (IZ) reservoir management

Daily injection rate2000

1000

30 m

Metric ton/day

300

310

AZMI

bars

300

350

400

IZ

bars

Tao, Bryant, Meckel, IJGGC accepted ms, available online

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Pressure monitoring subtask

•Presenting results from on-going modeling work:

•Set the stage: how is pressure attenuated, how is it transmitted from IZ to AZMI? (KWC)

•How big is the pressure signal, can we detect it? (MZ)

•Can we locate the leak if there is one? (AS, MZ)

•Optimize location of monitoring wells (AS)

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Role of the ambient rock during CO2injection

– Pressure propagation is governed by ratios of mudrock/sandstone permeability and storativity and relative thickness of formations

– Permeable and compressible surrounding rock reduces pressure propagation within a reservoir

Decrease mudrock permeability

Increase mudrock storativity

Mudrock = ambient rock

sandstone = reservoir

From Chang, Hesse, Nicotin review WRR, 2013

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Pressure diffusion: pumping / CO2 injection

From Chang, Hesse, Nicotin review WRR, 2013

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Development of a leaky well analytical model: Pressure signal magnitude

hm

2rl

hs

hl

AZMI

InjectionZone

kl2rw

r

R

q

r’ r

L

Injection Well Leaky WellAbandoned Well

Observation Well

Zeidouni, JPSE in review

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Analytical solution (single-phaseflow)

0

32

1

00

11

( ) 1( )

D

lD

lDDlD

lD lDD lD lD

D D

K sR

s K sq

sK rK sr

r sK sr s sT r K r

0

1

( )lD DD

mD

D lD lDD D

sq s KP

s sT r K r

Zeidouni, JPSE in review

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Asymptotic solution

2 21 1 ln ln

1 2 2 4 2lDD D

mDD D D D

qRPT t T

21 1 ln1 1/lD D D

D

q C t RT

2 22 3

2 3 4

2 (3)1 6 22 ln 4 2 ln 4 2 ln 4 2 ln 4

DD D D D

C tt t t t

11

2

2 ln1

DTD D

D lD

TT r

Zeidouni, JPSE in review

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Asymptotic solution

2 21 1 ln ln

1 2 2 4 2lDD D

mDD D D D

qRPT t T

21 1 ln1 1/lD D D

D

q C t RT

2 22 3

2 3 4

2 (3)1 6 22 ln 4 2 ln 4 2 ln 4 2 ln 4

DD D D D

C tt t t t

11

2

2 ln1

DTD D

D lD

TT r

Zeidouni, JPSE in review

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Detection type-curves

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Detection type-curves

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Cranfield Example

• D=0.5 (diffusivity ratio), TD=0.28 (transmissivity ratio)• t = 1 yr equivalent to tD=1010 (dimless time)

• P = 0.15 psi ~to PD = 0.0005 (dim pressure threshold)

• = 6 x 10-6 (leakage coefficient)

• and assuming RD = D = 2500

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Detection type-curves

> 6 x 10-6 is detectable

kl > 400 mD is detectable

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Detection type-curves

RD and D < 2500 are detectable

R and < 250 m are detectable

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Similar work on faults:Leaky fault analytical model

Zeidouni, WRR., 2012

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Similar work on faults:Leaky fault analytical model

Zeidouni, WRR., 2012

Multilayer leakage attenuation

Validation ofthe solution

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Inversion of pressure anomaly data:“remediation”

•We observed “pressure anomaly”: can we detect rate and location of source?

Simple homogeneous system

Given observation heads, ordinary least-square method can recover leakage rate history

Sun and Nicot, Adv.W.R., 2012

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Inversion of pressure anomaly data:“remediation”

•We observed “pressure anomaly”: can we detect rate and location of source?

Simple homogeneous system

Given observation heads, ordinary least-square method can recover leakage rate history

Sun and Nicot, Adv.W.R., 2012

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Inversion of pressure anomaly data:“remediation”

•We observed “pressure anomaly”: can we detect rate and location of source?

Simple homogeneous system

Effect of observation errors

OLS TSVD

Sun and Nicot, Adv.W.R., 2012

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Inversion of pressureanomaly data: “remediation”

Multiple leaky wells

Sun and Nicot, Adv.W.R., 2012

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Sun and Nicot, Adv.W.R., 2012

Inversion of pressureanomaly data: “remediation”

Heterogeneous; multiple leaky wells; locations known but rates unknown (could be 0)

Now, heterogeneous K field

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Inversion of pressure anomaly data:“remediation”

ONE leaky well but location not known: simulated annealing

O: Well locations

X: Initial guess

: Actual location

Conclusions:Can detect leakage rates and locations Try different solvers

Sun and Nicot, 2012, Adv. WR

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Leakage source detection:design perspective

Sun, Zeidouni, Nicot et al., accepted ms, Adv.W.R.

0.1 psi = 0.07 m

Earlier signalsLonger tails

Effect of AZMI lnKvariance on SNR

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Leakage source detection:design perspective

An observation point placed closer to potentially leaky

locations may not necessarily always

yield the most reliable signals when aquifer

properties are uncertain.

Sun, Zeidouni, Nicot et al., accepted ms, Adv.W.R.

0.1 psi = 0.07 m

Earlier signalsLonger tails

Effect of AZMI lnKvariance on SNR

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Pressure and temperature

• AZMI temperature changes because:• (1) Leak temperature; (2) Pressure changes (JT cooling); (3)

Dissolution and vaporization (exothermic and endothermic processes)

• CMG-GEM simulations

Zeidouni et al., SPE, ms in progress

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Above-zone temperature pulse

Zeidouni et al., SPE, ms in progressTemperature detection limit = 0.15°C; Pressure detection limit = 0.15 psi).

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• Chang, K.-W. M. A. Hesse, and J.-P. Nicot, 2013, Reduction of lateral pressure propagation due to dissipation into ambient mudrocks during geological carbon dioxide storage, in review WRR

• Sun, A. Y., and Nicot, J. -P., 2012, Inversion of pressure anomaly data for detecting leakage at geologic carbon sequestration sites: Advances in Water Resources, v. 44, p. 20‒29.

• Sun, A.Y., Zeidouni, M., Nicot, J.-P., Lu, Z., and Zhang, D., Assessing leakage detectability at geologic CO2 sequestration sites using the probabilistic collocation method : Advances in Water Resources, accepted

• Sun, A.Y. and others, Optimal CO2 leakage monitoring network design under uncertainty, in preparation

• Zeidouni, M., 2012, Analytical model of leakage through fault to overlying formations, Water Resour. Res., 48, W00N02, doi:10.1029/2012WR012582.

• Zeidouni M. and Pooladi-Darvish M., Inter-aquifer flow through leakage conduits: analytical solutions for leakage rate and pressure change evaluation, in review for Journal of Petroleum Science and Engineering.

• Zeidouni M., Hosseini S.A., and Nicot J.-P., Above-zone temperature variations due to CO2 leakage from the storage aquifer, in preparation for SPE 2013

• Zeidouni M., Hosseini S.A., and Nicot J.-P., Leakage identification through above-zone pressure monitoring, in preparation