1 Seismic Stimulation for Enhanced Oil Recovery Steve Pride, Mike Kowalsky, Valeri Korneev LBNL, Earth Sciences Division, Geophysics Department, Berkeley,

Slides:



Advertisements
Similar presentations
Potential impact of faults on CO2 injection into saline aquifers & Geomechanical concerns of CO2 injection into depleted oil reservoirs Quentin Fisher,
Advertisements

Earth Sciences Division, Lawrence Berkeley National Laboratory
(Introduction to) Earthquake Energy Balance
Sticky Water Taiwan Hsieh, Tsung-Lin. Question When a horizontal cylinder is placed in a vertical stream of water, the stream can follow the cylinder's.
Measuring MOTION.
Induced Seismicity Houston Bar Association Environmental Law Section Houston, Texas January 21, 2015 Mark K. Boling Executive Vice President and President,
Using Induced Seismicity to Predict and Monitor Reservoir Permeability Pathways STRM LLC.
Streamflow and Runoff The character, amount, and timing of discharge from a basin tells a lot about flow paths within the basin Therefore, important to.
Chapter 15: Oscillatory motion part 1
SEG San Antonio 09/27/ Interaction of seismic background noise with oscillating pore fluids causes spectral modifications of.
Seismic waves. When an earthquake occurs shockwaves of energy, called seismic waves, are released from the earthquake focus. They shake the Earth and.
© NERC All rights reserved CCS main geological issues Storage capacity Injectivity Containment.
Fluid Dynamics.
Simulation of Flux Emergence from the Convection Zone Fang Fang 1, Ward Manchester IV 1, William Abbett 2 and Bart van der Holst 1 1 Department of Atmospheric,
Groundwater. In the U.S. we use: 400 million gallons of water a day to drink 450 billion gallons of water a day in our homes, agriculture and industry.
1 Next adventure: The Flow of Water in the Vadose Zone The classic solutions for infiltration and evaporation of Green and Ampt, Bruce and Klute, and Gardner.
Chapter 9 Solids and Fluids (c).
8.6A Unbalanced Forces.
Stress, Strain, and Viscosity San Andreas Fault Palmdale.
Introduction to Capillary Pressure Some slides in this section are modified from NExT PERF Short Course Notes, However, many of the slides appears.
Introduction to Effective Permeability and Relative Permeability
Modeling and Measuring Water Saturation in Tight Gas Reservoirs Marcelo A Crotti Inlab S.A. INTERNATIONAL SEMINAR ON TIGHT GAS SANDS August 14th – 15th,
Significant New “Learings” From An Integrated Study Of An Old Field, Foster/South Cowden Field (Grayburg & San Andres), Ector County, Texas DE-FC22-93BC14982.
Hydraulic Drive Systems Hydraulic is derived from Greek word for water and it is the study of water flow. Water from a Nozzle Used to Turn a Turbine.
Erosion By Water and Wind.
8. Permeability (Das, chapter 7)
Science Changing Earth Chapter 2. a fracture in the Earth’s lithosphere fault.
Principal Investigators: Ding Zhu and A. D. Hill
(Calo et al, GJI, 2011). Reservoir-Induced Seismicity Victoria Stevens February 2012.
Significant New “Learnings” From An Integrated Study Of An Old Field, Foster/South Cowden Field (Grayburg & San Andres), Ector County, Texas. Robert C.
R eassessment Review For Unit 9 & 10 To view the presentation property click “Slideshow” and “From Beginning” As you go through the presentationcomplete.
Permeability and Seepage
Presented by: 1. A measure of how easily a fluid (e.g., water) can pass through a porous medium (e.g., soils) 2 Loose soil - easy to flow - high permeability.
Mihailo Jankov, Olav Aursjø, Henning Knutsen, Grunde Løvoll and Knut Jørgen Måløy, UiO Renaud Toussaint, Universite Louis Pasteur de Strasbourg Steve Pride,
Surface Water Chapter 9. Surface water movement: Water Cycle Earths water supply is constantly recycled.
Geometry Group Summer 08 Series Toon Lenaerts, Bart Adams, and Philip Dutre Presented by Michael Su May
SOME NOTES ON MORPHODYNAMIC MODELING OF VENICE LAGOON Gary Parker, Spring, 2004 Venice Lagoon was formed by the action of deposition of mud and sand from.
A positive test charge is used by convention to identify the properties of an electric field. The vector arrow points in the direction of the force that.
ATM 301 Lecture #7 (sections ) Soil Water Movements – Darcy’s Law and Richards Equation.
Chapter 12 Forces and Motion.
CE 3354 Engineering Hydrology Lecture 21: Groundwater Hydrology Concepts – Part 1 1.
Earthquakes & Volcanoes
Two-phase hydrodynamic model for air entrainment at moving contact line Tak Shing Chan and Jacco Snoeijer Physics of Fluids Group Faculty of Science and.
Argentina,
Copyright © 2014 All rights reserved, Government of Newfoundland and Labrador Earth Systems 3209 Unit: 5 Earth’s Resources Reference: Chapters 21; Appendix.
Modeling Subsurface transport of oil-field brine at the USGS OSPER “A” Site, Oklahoma William Herkelrath and Yousif Kharaka U.S. Geological Survey.
UNIVERSITY OF GUYANA FACULTY OF NATURAL SCIENCES DEPART. OF MATH, PHYS & STATS PHY 110 – PHYSICS FOR ENGINEERS LECTURE 14 (THURSDAY, DECEMBER 8, 2011)
Forces Chapter 12, Section 1. Forces Force – a push or a pull that acts on an object Force – a push or a pull that acts on an object A force can cause.
Lawrence Berkeley National Laboratory Earth Sciences Division 1 Cyclotron Road, MS Berkeley, CA D modeling of fault reactivation.
Friday, July 01, 2016 B-Day Objective: YWBAT describe the differences in the states of matter. Drill: Describe the particle arrangement of solids, liquids,
Cabled systems for near-field tsunami early warning: An observation system simulation experiment (OSSE) offshore Portugal A. Babeyko1, M. Nosov2 and.
Groundwater Review Aquifers and Groundwater Porosity
Hasan Nourdeen Martin Blunt 10 Jan 2017
Darcy’s Law and Richards Equation
Dual Mesh Method in Dynamic Upscaling
Unconventional Reservoirs
Next adventure: The Flow of Water in the Vadose Zone
Establishing Patterns Correlation from Time Lapse Seismic
Groundwater & Infiltration
Still talking about things with constant velocities
Groundwater occupies pores or open space within Earth materials
Topic 8 Water Vocabulary
Here are the categories
Modeling Natural Fracture Networks in the Context of Flow Simulations: Teapot Dome, Wy Thomas H. Wilson, Department of Geology and Geography, West Virginia.
1-Dimensional Vertical Motion
Squeezing of a 40% emulsion through
Mechanical Separation
Water Movement In the Ground
Presentation transcript:

1 Seismic Stimulation for Enhanced Oil Recovery Steve Pride, Mike Kowalsky, Valeri Korneev LBNL, Earth Sciences Division, Geophysics Department, Berkeley, CA, USA

2 Todays Talk: The basis of a physical model. A theoretical “stimulation criterion”. Lattice-Boltzmann simulations of seismically stimulated two-phase flow at the pore scale. The Foraker test site for the RPSEA project. Conclusions

3 Context: As much as 60% of the world’s oil is in known reservoirs but is trapped on capillary barriers and is effectively “stuck”. Seismic Stimulation : A seismic wave is to “shake the stuck oil loose” and get it flowing again toward a production well.

4 Increase in Oil Production after Stimulation at Occidental’s Elk Hills Field, California stimulation applied Oil Production (B/day) Oil cut % Oil Production Oil Cut

5 The condition for a stuck oil bubble: The production pressure drop along the bubble is just balanced by a capillary-pressure increase. Beresnev et al. (2005) Pride et al. (2009)

6 The production-gradient force that always acts on the fluids: “ acceleration of grains ” Poroelasticity determines the seismic force acting on the fluids: “ wavelength-scale fluid-pressure gradient” where is the seismic strain rate.

7 The seismic force adds to the production gradient and can overcome the capillary barrier whenever: “stimulation criterion” where Capillary force resisting bubble movement at the barrier (constriction). When the bubble does not become trapped on the barrier.

8 NOTES No green arrow = no applied forcing Single green arrow = production-gradient only Double green arrow = two periods of seismic stress + production-gradient “when stimulation is applied, bubbles coalesce creating a longer stream of oil that flows even in absence of stimulation” Lattice-Boltzmann Movie

9 Snapshots and average oil speed during the four stages of a typical “production run”: a.Oil separates from water without applied forcing. b.Production gradient applied; oil flows some, then gets stuck. c.Two periods of seismic stimulation applied that frees bubbles. d.Stimulation turned off and new steady-flow state emerges. running average

10 Volume of produced oil when no stimulation applied (dependence on )

11 Filled symbols / solid lines = stimulation applied o Open symbols / dashed lines = stimulation not applied. Volume of produced oil is increased when stimulation applied ( wave strain )

12

13 Foraker Field in Osage County, Oklahoma Reservoir is a fractured chert called the “Chat Formation”

Simple Seismic Model at Foraker Seismic Velocity (vertical section) Peak particle acceleration (plan view)

F c = capillary force Used values porosity surface tension permeability contact angle oil bubble length

16 Maps of Stimulation Potential  Created Using: where

Pressure gradient around the 20 wells to be stimulated at the Foraker site. Stimulation Potential The closer to 1, the greater the potential for liberating oil. Characteristic stuck bubble length of h = 10 cm.

18 Conclusions of the modeling to date : Stimulation criterion successfully verified by the 2D Lattice-Boltzmann simulations so far conducted. Need to extend the simulations to 3D and to larger systems. Over a significant and realistic range of seismic amplitudes and reservoir conditions, seismic stimulation seems to work The Foraker test site will be the first field test of the capillary threshold model and one of the most definitive tests to date. The Foraker site is still being monitored for the pre-stimulation well-by-well production statistics. Stimulation is expected to begin by March of 2011.