Geomechanics for Unconventionals Series, Vol III:

Similar documents
Stress Shadows Explained: What It Is, What It Isn t, And Why You Should Care

2015 Training Course Offerings

Gas Shale Hydraulic Fracturing, Enhancement. Ahmad Ghassemi

If your model can t do this, why run it?

Call for Papers. Hydraulic Fracturing Special Issue

Newton s Wagon. Materials. friends rocks wagon balloon fishing line tape stopwatch measuring tape. Lab Time Part 1

Before beginning, I would like to acknowledge the amazing contributions of Ken Nolte. I suspect that the origins of most of our discussion during

A Better Modeling Approach for Hydraulic Fractures in Unconventional Reservoirs

Abstracts ESG Solutions

Analysis of stress variations with depth in the Permian Basin Spraberry/Dean/Wolfcamp Shale

Reservoir Geomechanics and Faults

Microseismic Monitoring Shale Gas Plays: Advances in the Understanding of Hydraulic Fracturing 20 MAR 16 HANNAH CHITTENDEN

Microseismic Geomechanical Modelling of Asymmetric Upper Montney Hydraulic Fractures

Laws of Force and Motion

This paper was prepared for presentation at the Unconventional Resources Technology Conference held in San Antonio, Texas, USA, 1-3 August 2016.

for any object. Note that we use letter, m g, meaning gravitational

Newton s Laws Student Success Sheets (SSS)

Welcome to Forces an anticipation guide A force is defined as a push or a pull When answering the following true or false statements, offer a

ractical Geomechanics for Unconventional Resources

Hydraulics Prof Dr Arup Kumar Sarma Department of Civil Engineering Indian Institute of Technology, Guwahati

What Can Microseismic Tell Us About Hydraulic Fracturing?

3. A piece of candy is accelerated at 3.0 m/s 2 in the direction shown by a, over a frictionless horizontal surface. The acceleration is caused by 3

Microdeformation: combining direct fracture height measurement with microseismic response Natalia Verkhovtseva, Greg Stanley

Robustness to formation geological heterogeneities of the limited entry technique for multi-stage fracturing of horizontal wells

What Microseismicity Tells Us About Re-fracturing An Engineering Approach to Re-fracturing Design

Title: Application and use of near-wellbore mechanical rock property information to model stimulation and completion operations

DIFFERENTIAL EQUATIONS

Optimized Recovery from Unconventional Reservoirs: How Nanophysics, the Micro-Crack Debate, and Complex Fracture Geometry Impact Operations

2016 Junior Lesson One

Sir Isaac Newton ( ) One of the world s greatest scientists Developed the 3 Laws of Motion

and a contribution from Offshore Europe

Geomechanical Controls on Hydraulic Fracturing in the Bakken Fm, SK

Physics Chapter 4 Newton s Laws of Motion

Conceptual Physics Momentum and Impulse Take Home Exam

THE FIRST SUCSESSFUL MULTI STAGED FRACTURING IN A DEEP VOLCANIC GAS RESERVOIR IN JAPAN

LECTURE 16: Friction

Descriptive Statistics (And a little bit on rounding and significant digits)

Hydraulics Prof. Dr. Arup Kumar Sarma Department of Civil Engineering Indian Institute of Technology, Guwahati

A Better Modeling Approach for Hydraulic Fractures in Unconventional Reservoirs

J.V. Herwanger* (Ikon Science), A. Bottrill (Ikon Science) & P. Popov (Ikon Science)

The Gravity of the Situation. PTYS Mar 2008

Geomechanical controls on fault and fracture distribution with application to structural permeability and hydraulic stimulation

Forces. Unit 2. Why are forces important? In this Unit, you will learn: Key words. Previously PHYSICS 219

3.4 Fuzzy Logic Fuzzy Set Theory Approximate Reasoning Fuzzy Inference Evolutionary Optimization...

Practical Geomechanics

SHALE GAS AND HYDRAULIC FRACTURING

Optimization of Hydrocarbon Production from Unconventional Shale Reservoirs using FEM based fracture simulation. Lectures. J. Will, St.

Laboratory Shear Stimulation and Hydraulic Fracture Characterization Using Acoustic Emission

Fault Reactivation Predictions: Why Getting the In-situ Stresses Right Matters

Newton s Laws of Motion. Chapter 4

PHY131H1F - Class 9. Today, finishing Chapter 5: Kinetic Friction Static Friction Rolling without slipping (intro) Drag

Keys to Successful Multi-Fractured Horizontal Wells In Tight and Unconventional Reservoirs

Test Wed, Feb 8 th 7pm, G20 MING HSIEH Bring your calculator and #2 pencil with a good eraser! 20 Multiple choice questions from:

Chapter: The Laws of Motion

Scientific approach applied to multi-well pad development in Eagle Ford shale

Stuff you asked about:

Technology of Production from Shale

Halliburton Engineering for Success in Developing Shale Assets

Role of lithological layering on spatial variation of natural and induced fractures in hydraulic fracture stimulation

Chapter 4 Homework Packet

Forces. Name and Surname: Class: L E A R N I N G O U T C O M E S. What is a force? How are forces measured? What do forces do?

Geomechanical Analysis of Hydraulic Fracturing Induced Seismicity at Duvernay Field in Western Canadian Sedimentary Basin

Proppant Transport & Screenout Behavior. R.D. Barree

Impact of fracture spacing and mechanical parameter anisotropy on fracture width in horizontal wells in shales

Quadratic Equations Part I

Chapter 4: Newton's Second Law of Motion

SPE DISTINGUISHED LECTURER SERIES is funded principally through a grant of the SPE FOUNDATION

Fractures and fluid flow in petroleum reservoirs

M. Y Soliman, PhD, PE, NAI Ali Rezaei

Newton s Laws Review

FRACTURE REORIENTATION IN HORIZONTAL WELL WITH MULTISTAGE HYDRAULIC FRACTURING

Main Ideas in Class Today

AP Physics 1 Summer Assignment

Experiment 1 Look Out Below!!

Geology geomathematics. Earthquakes log and exponential relationships

Unit 08 Work and Kinetic Energy. Stuff you asked about:

In this lecture we will discuss three topics: conservation of energy, friction, and uniform circular motion.

Physics 9 Monday, February 13, 2012

Integrated Approach to Drilling Project in Unconventional Reservoir Using Reservoir Simulation

Magnetism and Gravity

From Micro to Macro: Application of a Geomechanically Calibrated, Seismically Constrained Reservoir Model to Unconventional Resource Development

Driveway Races Acceleration

Rate Transient Analysis COPYRIGHT. Introduction. This section will cover the following learning objectives:

Motion and Forces. Forces

Passive seismic monitoring in unconventional oil and gas

MAXIMIZING THE RESERVOIR ACCESS WITH COMPLETION OPTIMIZATION AND EFFECTIVENESS. Luciano Fucello, NCS Multistage Fabio Chiarandini, Gaffney & Cline

4 Forces in One Dimension 2 Weight and Drag Force MAINIDEA Write the Main Idea for this section.

An analogy from Calculus: limits

Considerations for Infill Well Development in Low Permeability Reservoirs

Integrating Geomechanics and Reservoir Characterization Examples from Canadian Shale Plays

What is proof? Lesson 1

Name per due date mail box. Friction Lab. Challenge - move your wooden block from start to finish with the least amount of force.

ConcepTest PowerPoints

Investigate the relationship between the extension of a spring and the applied force

Integrating Lab and Numerical Experiments to Investigate Fractured Rock

How Do Objects Move? Describing Motion. Different Kinds of Motion

3 Newton s First Law of Motion Inertia. Forces cause changes in motion.

Now, consider the actual molecules reacting with each other:

A new methodology for estimating field horizontal stress from microseismic focal mechanisms

Exam 1 is Two Weeks away.here are some tips:

Transcription:

Geomechanics for Unconventionals Series, Vol III: Hydraulic Fracturing: Of Magic and Engineering By Dr. Neal B. Nagel Part 1 Several years ago, I attended an industry conference where a well-known rock mechanics researcher made the comment that hydraulic fracturing in shales was magic. Initially, I was not intrigued by the comment since, after all, who among us has not used a bit of hyperbole while making an argument. Take a moment to think of the times you have used always or never to describe the occurrence of something while trying to make a point. However, this researcher said that hydraulic fracturing in shales was magic twice more in the presentation, including the conclusions. Now I was intrigued. I made a presentation about Stress Shadows several weeks ago (I will be a 2016-17 SPE Distinguished Lecturer on the topic) and had two interesting comments from the audience. The first comment, and I am paraphrasing, was we don t see Stress Shadows so they must not be happening. Fair enough, but how would you see Stress Shadows anyway? The second comment came about from my effort to show the effects of Stress Shadows (in this case, on the pattern of microseismicity) where the discussion got into hydraulic fracture modeling and the idea that we do not know the physics of hydraulic fracturing enough to make accurate models. Intriguing to say the least. As many of you know, the first experimental hydraulic fracturing operations, in the Hugoton, were performed in 1947 nearly 70 years ago. Since that time, we have learned a lot about hydraulic fracturing, but the fundamental physics of hydraulic fracturing (HF) have been known for decades. That is: For well stimulation, an HF consists of: 1) generation of the fracture; and 2) filling the fracture with proppant to keep it open to provide a highly conductive pathway for hydrocarbon flow. An HF is created only when the injection rate exceeds the flow capacity of the formation. If the flow capacity of the formation (either into the matrix or natural fractures) is greater than the injection rate, no HF may form at all. In addition, once an HF is propagating, if the leakoff rate (loss of fluid from the hydraulic fracture) into the matrix or natural fractures exceeds the injection rate, the HF will stop propagating and begin to close. Hydraulic energy, in the form of pressurized frac fluid, is controlled only in the well (or to the perforations); past this, the flow path of the omni-directional hydraulic energy is largely controlled by the reservoir and always follows the path of least resistance.

Net pressure the difference between the fluid pressure inside a hydraulic fracture and the minimum principal stress is the primary metric for the amount of work being done to the formation while hydraulic fracturing. Commonly, net pressure is +/- 300 psi or less. The tensile strength of most formations is +/- 10% of the shear strength of the formation (i.e., the tensile strength is +/- 1/10 th that of the UCS value). Since the injected hydraulic energy (pressurized frac fluid) will always find and follow the path of least resistance, hydraulic fractures are commonly formed in tension (not shear) and open against the least principal insitu stress (in a normal faulting environment, this means that the created hydraulic fracture propagates vertically towards the maximum horizontal stress, SHmax, and opens against the minimum horizontal stress, Shmin). However, there are situations where the path of least resistance to fracture propagation is not dominated by the stress state but rather by the mechanical properties of the formation (i.e., ductile formations which are difficult to fail in tension or naturally fractured formations where the natural fractures dominate the hydraulic fracture propagation path). So where does the magic come in? What are the uncertainties in the physics involved (not uncertainty in the data to evaluate the physics, but the physics itself)? Why do we have to see the physics (like Stress Shadows) to believe that they exist? By way of explanation, we could first simply fall back to the human pre-historic tendency to attribute magical powers to things unknown (at the time). Clouds, rain, hail, and fire were all, for example, feared and worshiped by numerous primitive human tribes, yet today the understanding of each of these is taught to children in elementary school. Further, the need to see (or touch or taste or hear or smell) something in order to accept it and understand it is also a basic human tendency. Surely, however, when it comes to hydraulic fracturing we are beyond this. So, finally, we might simply chalk it up to semantics what one person sees as uncertainty in data is another person s uncertainty in physics. Whether it is because of (the fear of) the unknown or because of incorrect terminology, these beliefs have significant negative impacts on both new and experienced personnel within the industry (and, perhaps more critically, society at large). The belief that hydraulic fracturing is magic or we don t understand its physics leads to (incorrectly) a: Lack of trust in numerical predictive models which leads to the belief that we are unable to predict and assess hydraulic fracturing behavior before pumping the job; Resorting to trial-and-error job designs which is both costly and promotes future incorrect actions because the correlation established during the trial-and-error process lacks causation; Lack of advancement in the associated physics why, for example, try a new fluid or process if we can t resort to anything but expensive trial-and-error to show its value; and Lack of focus on critical steps towards improvement why collect more (or more detailed) data if there is no predictive value in it (other than, again, feeding a trial-and-error approach that lacks causation).

It should go without saying that there are many, many folks who do understand hydraulic fracturing and the fundamental physics behind it. And there are many, many folks who can and are engineering their hydraulic fracture stimulations using sound physics and sound numerical tools. However, there are many who are not and these folks can and do influence not only the next generation of engineers and scientists but also society at large which poses a great challenge to the industry. Part 2 In my previous post regarding the magic of hydraulic fracturing, I related several negative effects that are occurring within the oil & gas industry because of the belief that hydraulic fracturing in Unconventionals is (at least partially) beyond our capacity to understand and predict (ergo, the reference story about hydraulic fracturing in shales referred to as magic ). These negative consequences include a lack of trust in numerical predictive models, resorting to trial-and-error stimulation designs, a lack of advancement in the associated physics, and a lack of focus on critical steps towards improvement such as collecting more (or more detailed) data. A critical point that I did not dwell on in the previous post was the issue of physics versus data. Perhaps, again, the issue is one of semantics one person s physics is another person s data. But let s dispel that possibility up front. Recall Newton s Second Law of Motion that states that Force, F, equals Mass, m, multiplied by Acceleration, a (F=ma). The physics of Newton s Second Law is that the sum of the forces acting on a body ( F ) must be equal to the mass of the body ( m ) times the acceleration of the body ( a ). We know and accept that these physics are correct. For example, due to the lower gravity on the moon, astronauts weighed less and were thus able to (and were predicted to be able to) move and jump around even in their bulky spacesuits. Recall, for example, that astronaut Alan Shepard even played golf on the moon in 1971! Perhaps a more concrete example is the common behavior of street and drag racers where, in order to achieve greater acceleration of her car, a driver will strip out all the unnecessary components to reduce the mass of the car. So the physics of Newton s Second Law is the defined relationship between force, mass, and acceleration. In order to predict the force necessary to create an acceleration (per our drag racer example), it is not enough to know the relationship between force, mass, and acceleration. Rather, we need data (i.e., values for the parameters) - along with the physics - to make a prediction. For hydraulic fracturing then, what are the physics and what is the necessary data? Recall some of the fundamental physics from my previous post: Hydraulic fracturing is about creating volume in the formation, that otherwise did not exist, to stuff fluid (and proppant) into. A hydraulic fracture is created only when the injection rate exceeds the flow capacity of the formation. A good analogy is a balloon with a hole in it. If the hole is large enough, no amount of blowing will inflate the balloon. However, if the hole is relatively small and we blow hard enough (a high enough injection rate), the balloon can be inflated. Similarly, if the flow capacity of a formation (either into the matrix or natural fractures) is greater than the injection rate, no hydraulic fracture may form at all. In addition, once a

hydraulic fracture is propagating, if the leakoff rate (loss of fluid from the hydraulic fracture) into the matrix or natural fractures exceeds the injection rate, the hydraulic fracture will stop propagating and begin to close. Hydraulic energy, in the form of pressurized frac fluid, is controlled only in the well (or to the perforations); past this, the flow path of the omni-directional hydraulic energy is largely controlled by the reservoir and always follows the path of least resistance. Furthermore, there is no injection pressure dial on a pump truck only an injection rate control. Consequently, the magnitude of the hydraulic energy (i.e., the magnitude of the pressure) is a result of a given injection rate into a formation with a given capacity to take this rate. In simple terms, ignoring friction outside the hydraulic fracture, the injection pressure is controlled by the injection rate relative to the flow capacity of the formation (and, where the formation flow capacity is greater or easier to create the injection pressure will be less and, conversely, where the formation flow capacity is less or more difficult to create the injection pressure will be higher). The tensile strength of most formations is +/- 10% of the shear strength of the formation (i.e., the tensile strength is +/- 1/10 th that of the Unconfined Compressive Strength, UCS, value). Since the injected hydraulic energy (pressurized frac fluid) will always find and follow the path of least resistance, hydraulic fractures are commonly formed in tension (not shear) and open against the least principal in-situ stress (in a normal faulting environment, this means that the created hydraulic fracture propagates vertically towards the maximum horizontal stress, SHmax, and opens against the minimum horizontal stress, Shmin). However, there are situations where the path of least resistance to fracture propagation is not symmetric around the wellbore and not dominated by the stress state but rather by the mechanical properties of the formation (i.e., ductile formations which are difficult to fail in tension or naturally fractured formations where the natural fractures dominate the hydraulic fracture propagation path). Many commercial hydraulic fracture simulators model a single fracture wing and assume that the other wing is symmetric to the first, which is premised on the path of least resistance for hydraulic fracture propagation (both stress and formation properties) being laterally homogenous away from the wellbore. Many field microseismic data sets have shown this assumption to be incorrect! So the critical physics of hydraulic fracturing are: 1) formation flow capacity and its change as a hydraulic fracture propagates (i.e., leakoff); 2) in-situ stress (magnitudes and directions) and pressure; and 3) formation structure and mechanical properties (both stiffness and strength), where the stress and formation properties determine the energy required to create the hydraulic fracture and the path(s) of least resistance it will take. As another analogy, consider the process of splitting wood for a fire. Hydraulic pressure is not used (at least directly) to split the wood, so the flow capacity issue is moot in this example. What controls the splitting of the wood then? Since no stress is involved, that is moot as well. Which means that what controls the splitting of the wood (i.e., fracturing the wood) is the structure of the wood (like knots in the wood) and the mechanical properties of the wood itself. If we had a homogenous piece of wood

(without knots) and knew the strength of the wood fibers, we could make a pretty accurate prediction of the splitting process (both the energy required as well as the direction of the split). So the physics are relatively simple and all we really need is the data. Largely, this is true about hydraulic fracturing. We know the physics of formation flow (things like Darcy s law), we know the physics of stress and stress orientation, and we know the physics of formation structure (i.e., faults, bedding planes, and natural fractures) and mechanical properties. What we often lack is the data for all these things in a 3D volume (and not the physics )! If we assume for a moment that a numerical simulator exists containing the physics described above (and leaving aside frac fluid/proppant physics), what data is needed: The flow capacity of the matrix of the formation, which includes permeability, porosity, and pressure; The stress field (magnitudes and direction) within the 3D volume that is going to be fractured; Geological structure in 3D, including bedding, faults and fractures; Matrix mechanical properties (stiffness and strength); Structural component (i.e., bedding planes, faults, and natural fractures) mechanical properties (stiffness and strength) and flow components (i.e., aperture and permeability). Is getting all this data easy? Heck no but let s not hide behind we don t know the physics when what we really mean is I can t (or won t) collect all that data! See all the articles in the OFG Geomechanics for Unconventionals Series : I. ge-o-me-chan-ics, A Better Explanation II. Geomechanics And Unconventionals: A Match Made in Heaven or Just (Occasional) Friends III. Hydraulic Fracturing: Of Magic and Engineering IV. The Complexity Paradigm: Shifting Our Understanding in Order to Optimize Completions in Unconventionals V. Stress Shadows Explained: What It Is, What It Isn t, And Why You Should Care VI. Why 100 Mesh in Unconventionals VII. On the Geomechanics of Zipper Fracs VIII. Who Redefined Frac Gradient: And Why? IX. Completion Engineer for a Day X. On The Geomechanics of Refracturing XI. Sand Volume per Unit of Lateral Length: Is There a Geomechanical Justification? XII. It s the Rock Fabric, Stupid!