Instructed by Sebastien Soulas (Avalon Sciences Ltd, UK)
Sebastien Soulas completed his Master’s degree in Geophysics (specialising in Borehole geophysics) from School and Observatory of Earth Sciences (EOST), Strasbourg France, in 1994. He then spent 12 years working in marine seismic data processing, acquisition, and analysis at various European locations before leading global borehole seismic activities for Maersk Oil in Copenhagen. He worked for BP 8 years and acted as senior Borehole Seismic Technical Expert in Upstream Reservoir Development, managing global borehole seismic operations, including the planning and execution of data acquisition, data processing and VSP data integration with surface seismic. At the beginning of 2019, he joined LYTT as Senior Advisor for Borehole Seismic, a BP tech start-up which develop and deploy high-value applications using DAS and DTS to provide real-time 24/7 subsurface analytics including seismic applications. He played an instrumental role in the design, development, installation, and validation in the industry’s first subsea DAS VSP system using distributed Fiber Optic Sensing (DFOS) for bp in GoM Atlantis field.He joined Avalon Sciences in May 2022 as Global Operations Manager in Somerton and is overseeing field operations, field testing and advise on internal/external technical matters. He also continues to provide support to the R&D team in downhole 3-C optical seismic sensors technology development for active and passive seismic.He has presented numerous technical papers on borehole Geophysics including DAS seismic at EAGE and SEG conferences and workshops promoting data value, technology adoption and integration with surface seismic.
The course is designed for Geologists, Geophysicists and geoscientists who would like to get an understanding of VSP principles and various applications.
Basic understanding of Geology and geophysics including signal processing and geophysical operations (surface and downhole)
Time | Topic | Learning Objectives | Assessment Method/Content | Duration |
08:00 - 08:15 | Course opening | Identify what you will learn during the course | PPT with overarching objectives | 15 mins |
08:15 - 09:30 | VSP basics | General overview, geophysical principles and different VSP geometries | PPT and examples | 75 mins |
09:30 - 10:10 | VSP data acquisition | Surface/downhole equipment and operational considerations | PPT and examples + Q&A | 40 mins |
10:10 - 10:20 | Break |
|
| 10 mins |
10:20 - 11:00 | Velocity survey | Data pre-conditioning for first break picking. Identify limits of absolute T-D based on well geometry and geology | PPT and exercise | 40 mins |
11:00 - 11:45 | VSP modelling | Practical pre-survey design and evaluation, Ray tracing modelling | Software demo and spreadsheet exercise | 45 mins |
11:45 - 12:00 | Wrap up day 1 (morning) | Recap key learnings | Q&A | 15 mins |
13:00 - 13:45 | 1-C VSP processing | Single component Processing sequence | PPT with overarching objectives | 45 mins |
13:45 - 14:15 | High angle wells | Implications with highly deviated wells and non zero offset VSP | PPT, examples and case histories | 30 mins |
14:15 - 14:55 | Lookahead VSP and SWD | Estimate predict ahead of the bit and use of SWD in drilling applications | PPT, examples and case histories | 40 mins |
14:55 - 15:05 | Break |
|
| 10 mins |
15:05 - 15:45 | VSP imaging | How to use VSP for 2D/3D imaging and pros/cons of VSP as an imaging tool | PPT, examples and case histories | 40 mins |
15:45 - 16:45 | Distributed Acoustic Sensing (DAS) | DAS principles and technology for seismic applications. Technology evolution | PPT, examples and case histories | 60 mins |
16:45 - 17:00 | Wrap up/close out | 10 things you should know |
| 15 mins |
Instructed by Leo Eisner (Seismik, Czech Republic)
Leo Eisner obtained his MSc. degree in Physics at the Charles University of Prague and Ph.D. in Geophysics from the California Institute of Technology and his M.S in Geophysics from the Charles University in Prague. He spent six years as a Senior Research Scientist with Cam-bridge Schlumberger Research. He then moved to MicroSeismic, Inc.in 2008 and since 2009 till 2010 he was the Chief Geophysicist. in 2010 he moved to Prague to become Purkyne Fellow at the CzechAcademy of Sciences. He worked in the Academy of Sciences until 2017. He founded and he is currently the President of a consulting company Seismik s.r.o. His papers and extended abstracts cover abroad range of subjects, including the seismic ray method, finite difference methods, seismological investigations of local and regional earthquakes and micro earthquakes induced by hydraulic fracturing, etc. He has lead/advised three Ph.D.s and six MSc. theses.
This newly revised programme explains the principles of microseismic monitoring ranging from single monitoring borehole to surface and near surface networks. The applications cover from conventional to unconventional production, through geothermal energy extraction to CO2 sequestration. We will focus on understanding the measurements made in passive seismic, their use and their uncertainties.
The course will also discuss the latest developments in microseismicity from DAS monitoring systems, source mechanisms, tomography and anisotropy to reservoir simulations. Finally, we will discuss social and scientific aspects of (induced) seismicity related to oil and gas reservoir, hydraulic fracturing and unconventional production.
The course is designed for users and practitioners in microseismic monitoring.
1. Introduction: Definitions, a brief review of microseismicity outside of oil industry: water reservoirs, mining, geothermal, CO2 sequestration. Microseismicity and induced seismicity by reservoir production.Historical review of microseismicity in energy industry with focus on hydraulic fracturing (Basel, Soultz, M-site, Cotton Valley, Barnett,etc). Principles of the hydraulic fracturing and geomechanics. Goal of microseismic monitoring and options to meet them.
2. Earthquake seismology: number of unknowns, differences be-tween active and passive seismic. Receivers - how to select optimal type of sensors to meet our goals. Absolute location, relative location. P- and S-wave polarizations. Frequency content of microseismic data. Finite source. Earthquake magnitudes.
3. Downhole monitoring: single well monitoring technique - S-P wave time + P-wave polarization technique location. Horizontal monitoring borehole. Picking strategies for downhole montoring. Optimal design of downhole monitoring array. Orientation of down-hole geophones. Velocity model building and calibration. Inclined/dual and multi well monitoring.
4. Surface monitoring: P-wave location from surface: depth vs. ori-gin time. Detection uncertainty and signal-to-noise ratio. Frequency content, attenuation and detection. Design of surface monitoring array. Calibration and velocity model building. Relative locations:using S-waves recorded at the surface monitoring array. Case study comparing the downhole and surface locations. Why surface micro-seismic monitoring works, near surface attenuation.
5. Source mechanisms: concept of source mechanism, definition of dip, strike and rake for shear source. Description of shear, tensile, volumetric, CLVD components of source mechanism. Inversion for source mechanisms from single monitoring borehole, multiple monitoring boreholes surface P-wave only data. Radiation pattern of source mechanisms frequently seen in microseismic monitoring.Source mechanisms and stress orientation.
6. Advanced source parametrization: Magnitude: definition and de-termination, seismic energy, b-values and magnitude of completness, physical liminations of b-values, stress drop, source dimensions.
7. Anisotropy: Introduction to anisotropy. Effect of anisotropic media on S-waves: shear wave splitting. Shear wave splitting observed in microseismic data. Inversion of anisotropic media from P- andS-waves using microseismic events, time lapse changes. Anisotropy and surface monitoring of microseismic events.
8. Reservoir simulations: Current use of microseismicity in oil industry and implementation of microseismicity into modeling. Diffusion model for pressure triggering of microseismic events. Non-linear diffusion and mass balance. Discrete Fracture Networks constrained by microseismicity. Reservoir simulations and history matching.
9. Seismicity in the vicinity of energy exploration. History of felt seismicity related to oil and gas industry. Differentiation of natural and induced seismicity. Seismic moment and total injected volume.Blackpool case study as an example of induced seismicity. Oklahoma and DFW seismicity - natural seismicity? Hazard assessment and mitigation. Social aspects related to development of shale gas.
10. Review of recent research effort and case studies in microseismicity. Models of relationship between microseismicity and hydraulic fracturing. Most important things to remember about microseismicity.
Topic | Learning Objectives | Assessment Method/Content | Duration |
Course opening | Definitions, review of microseismicity outside oil and gas industry | PPT with overarching objectives | 60 mins (08:00-09:00) |
Instrumentation and earthquake seismology | General overview, geophysical principles and different VSP geometries | PPT and examples | 60 mins (09:00-10:00) |
Break | 10 mins (10:00-10:10) | ||
Downhole monitoring | Single vertical monitoring borehole, downhole monitoring design, picking strategy, receiver orientation, velocity calibration, Design with DAS monitoring | PPT and exercise | 70 mins (10:10-11:20) |
Shallow borehole monitoring | Surface vertical component monitoring, downhole-surface comparison, borehole noise and optimal depth of shallow borehole receivers | PPT and exercise | 25 mins (11:20-11:45) |
Wrap up morning | Recap key learnings | Q&A | 15 mins (11:45-12:00) |
Source mechanisms | Definition of dip, strike and rake, description of shear, tensile, volumetric, CLVD. Radiation pattern, inversion for source mechanisms, magnitude, seismic energy, b-values and magnitude of completeness | PPT with exercises | 80 mins (13:00-14:20) |
Induced seismicity I | Geomechanical introduction to induced seismicity, volume dependency | PPT, examples and case histories | 40 mins (14:20-15:00) |
Break | 10 mins (15:00-15:10) | ||
Induced seismicity II | Differentiation between natural and induced seismicity, mitigation | PPT, examples and case histories | 40 mins (15:10-15:50) |
Case studies and summary | Published case studies on microseismicity processing and observations, relationship to hydraulic injections | PPT, examples and case histories | 55 mins (15:50-16:45) |
Wrap up/close out | Q&A and wrap up | 15 mins (16:45-17:00) |