a guid iding lig light to cost- effective reserv rvoir monitoring - - PowerPoint PPT Presentation
a guid iding lig light to cost- effective reserv rvoir monitoring - - PowerPoint PPT Presentation
4D Gravity and Subsidence: a guid iding lig light to cost- effective reserv rvoir monitoring Egypt-Norway Technology Days Outline About OCTIO Gravitude The principles of the technology 4D gravity Whole-field subsidence
Outline
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- About OCTIO Gravitude
- The principles of the technology
- 4D gravity
- Whole-field subsidence monitoring
- Case studies: the value of gravity and subsidence
- Concluding remarks
2013 IP and competence transfer
About Octio Gravitude
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- Value of the technology proven in many fields on the NCS
- Gravitude performed 8 surveys in 6 fields since 2012
- Best results to date
- Safe operations with no HSE incidents
- Ormen Lange field (operated by Shell) surveyed since 2012
- Octio has ten years of operational experience
- Highly skilled technical team with diverse background
2012 GRAVITUDE created within Statoil Late 90’s technology developed by Statoil
The surveys in a nutshell
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ROV Primary measurements: gravity and
pressure at the seafloor
Sensor frame with 3 gravimeters and 3 pressure sensors Concrete platform 20’ per measurement Repeated visits
Gravity and subsidence monitoring on the NCS
Field 1st survey # of surveys Seafloor depth (m) Reservoir depth (m) Area (km2) N. stations Comment Troll 1998 6 320 1400 30 x 50 113 Norway’s largest gas field Mikkel 2006 4 230 2500 3 x 12 21 Smaller, deeper reservoir Sleipner 2002 4 80 800 / 2350 4 x 10 50 Gas production + CO2 injection Ormen Lange 2007 5 295-1130 2000 15 x 50 120 Second largest gas field in Norway Challenging oceanography, Shell-operated Statfjord 2012 2 140-200 2750 5 x 25 53 Oil field, subsidence is the main motivation Midgard 2006 4 240-310 2500 10 x 20 60 Deep reservoir Snøhvit / Albatross 2007 2 250-340 2500 20 x 20 86 Gas production + CO2 injection
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Gravity for reservoir monitoring
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- Sensitive to changes of density in the subsurface
- It allows monitoring movements of fluid interfaces. Example:
- 𝜍𝑥𝑏𝑢𝑓𝑠 > 𝜍𝑏𝑡 ⇒ Δ > 0 observed
- Magnitude proportional to the raise of the contact
- Spatial distribution of Δ tells about comparmentalization, permeability, aquifer
strengths
Before production start After production start
gas gas water from aquifers sea sea gravimeter gravimeter
Some applications of gravity
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hydrocarbon water
Unproduced compartments? Acquifer strengths? Volume of gas in place?
Accuracy of gravity at the seafloor
1 µGal means:
- 10-8 m/s2, or 10-9 g, or 100 kg at 0.8 m
- Sub-meter sensitivity in a gas-water contact
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Year 10 000 1 10 100 1000 Satellite altimeter Airborne Shipborne Seafloor Land Borehole Stationary 1998 2002/2005 2006/2007 2009 2013 2015
mGal
Seafloor
Increased recovery
Value of the gravity data
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Infill well planning Well data Planning of production, pipeline use Lateral compart- mentalization Aquifer strength
Gravity
Update actual volume of hydrocarbon reserves Prediction of water breakthrough Reservoir parameters
(e. g. permeability)
Understanding reservoir behavior away from wells Installation of compression facilities Seismic
- At a cost ~15% of that of time-lapse seismic
Subsid idence
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Subsidence
Measured through time-lapse changes in water pressure (after applying tide and environmental corrections)
The value of subsidence data
- Accuracy on subsidence (published values):
- Mikkel 2006-2011 time-lapse: 2.5 - 3.7 mm
- Sleipner 2002-2005 time-lapse: 2.3 mm
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Compressibility, pressure depletion Drilling window for infill wells Geological model Installation safety and integrity Caprock integrity
Reservoir Overburden
Subsidence (or uplift)
Aquifer
Compressibility, permeability Lateral compartmentalization
Survey setup
- Pressure and gravity measured at each of the concrete
platforms (typically 20 minutes)
- Tide gauges deployed during the whole survey at a
subset of stations
- Allow to refer all pressure measurements to normal sea and
atmospheric conditions
- Enables comparison of data from different vintages
- In all:
- No storage issues: < 2 Gb per survey
- Fast turnaround: three months from survey to final report
- Environmental friendly
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Example: Troll field
Field cases
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Troll 2002-2009: subsidence
Pore compressibility:
- Troll West PDO (1991): ~ 80·10-5/bar
- Revised core data (2000): ~ 9·10-5/bar
- Subsidence history-matching: ~ 3·10-5/bar
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Maximum ~1 cm / year
Zero-level stations
http://www.slideshare.net/Statoil/alnes-et-al-gravity-and-subsidence-monitoring
Alnes, H., Stenvold, T. and Eiken, O. [2010] Experiences on Seafloor Gravimetric and Subsidence Monitoring Above Producing Reservoirs, 72nd EAGE Conf. and Exhib., L010.
Corrected for gas takeout
Troll 2002-2009: 4D gravity
- Significant raise of ~2 m of the gas-water contact
- bserved in some stations already in 2002-2005
- Time-lapse seismic lines shot in 2002 and 2006
showed no evidence of the raise yet
- 5-10 m were required for it to be visible over effect of
pressure drop
- Updated aquifer strengths in the reservoir simulation
model
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Oil production Gas production, movement
- f the water front
http://www.slideshare.net/Statoil/alnes-et-al-gravity-and-subsidence-monitoring
Alnes, H., Stenvold, T. and Eiken, O. [2010] Experiences on Seafloor Gravimetric and Subsidence Monitoring Above Producing Reservoirs, 72nd EAGE Conf. Exhib, L010.
Mikkel 2006-2011: 4D gravity
- Initial uncertainties on:
- External aquifers
- Total volume of gas
- The system has low tolerance for water production
due to risk of hydrate formation
- Results show lower water influx than expected
- Aquifer volume reduced by factor 4
- Mikkel contains more gas than expected
- This input enabled:
- Better prediction of water breakthrough
- Better long term planning
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From Vevatne, J. N., et al., [2012] Use of Field-wide Seafloor Time-lapse Gravity in History Matching the Mikkel Gas Condensate Field, 74th EAGE Conference & Exhibition, Extended Abstracts, F040
Data – model discrepancy
Less water than expected More water than expected
Forward-modelled gravity change (µGal)
Midgard 2006-2012: 4D gravity and subsidence
- Uncertainties in the model:
- Aquifer support and drainage patterns
- Fault distribution and compartmentalization
- Learnings from 4D gravity and subsidence: one
segment underproduced, indicating sealing faults
- Reinterpretation of available seismic data
- Updated reservoir model with the sealing fault as the most
likely realization
- A new well target was identified, which is now
number one producing well in all the Åsgard complex
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Ueland, I., et al., [2015] Modnet fram brønn på utradisjonel vis, Origo Statoil ASA, pp. 40-41 September.
Ormen Lange
- Increased recovery involved decisions on:
- Compression facilities
- Infill wells
- Water break-through and
compartmentalization identified as a significant uncertainties
- Feasibility studies for measuring water influx:
- Nearly impossible with 4D seismics
- Would take > 7 years with EM
- Abstract submitted to EAGE 2017 with
Gravitude and Shell authors
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Van den Beukel, A. et al. [2014], Integrated Reservoir Monitoring of the Ormen Lange field: Time lapse seismic, Time lapse gravity and seafloor deformation monitoring, The Biennial Geophysical Seminar, NPF, Kristiansand 2014
Forward-modelled gravity change (µGal), 2 years time-lapse
Outtake Water influx
Dunn et al., A long-term seafloor deformation monitoring campaign at Ormen Lange gas field, first break volume 34, October 2016
Significantly less subsidence than modelled in the south
Measured 2012-2014
Gravitude’s feasibility studies
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Define alternative scenarios reflecting:
- Uncertainties on reservoir model
- Value of the new information
Environment conditions
- Oceanography
- Seafloor quality
Model the strength of 4D gravity and subsidence signals for each alternative scenario Requirements from installation safety on subsidence precision Feasibility report
- Ability to distinguish reservoir scenarios
- Increased safety from subsidence monitoring
- Survey design and cost
Value of the gravity and subsidence data
Optionally
Conclusions
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- 4D gravity - subsidence surveys provide:
- Key information for reservoir management, e.g.
- Movement of fluid contacts
- Identification of non-producing compartments
- Reservoir compaction
- Information for whole-field – not only producing wells
- Improved safety of the field and installations
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Thank you
hugo.ruiz@octio.com