Fiber optic distributed sensing methods provide the opportunity to sample strain and temperature variations with detailed sampling along the borehole and in real time. Careful analysis of the data can allow engineers and geoscientists to understand the behavior of reservoir rock, fluids, and pressure systems better, giving quantitative measures for improved management of hydrocarbon production. However, the massive data volumes make rapid analysis difficult, especially because the data are affected by physical processes occurring on a broad range of spatiotemporal scales. For example, during fracturing, acoustic signals will be generated by fracture propagation and by fluid flow, which will take place on different scales.
Measurements from a distributed sensing system may sample all of the processes taking place along a fiber optic cable, but in many cases only a subset of those processes, operating on a subset of spatiotemporal scales, are relevant for the engineering task. Current data processing schemes may be unable to isolate the relevant data features and reduce the data volume.
Current processing schemes applied for analysis of flow or fracturing may emphasize measures applied to signals from individual sensor channels. For example, frequency filtering can enhance either the low frequency strain generated by a propagating fracture system or rapid flow at high frequencies. Other measures may quantify amplitude or phase variation of signals, but all of these approaches may ignore any spatial dependence since they operate on individual channels.
Reference is now made to the following descriptions taken in conjunction with the accompanying drawings, in which:
In the drawings and descriptions that follow, like parts are typically marked throughout the specification and drawings with the same reference numerals, respectively. The drawn figures are not necessarily to scale. Certain features of the disclosure may be shown exaggerated in scale or in somewhat schematic form and some details of certain elements may not be shown in the interest of clarity and conciseness. The present disclosure may be implemented in embodiments of different forms.
Specific embodiments are described in detail and are shown in the drawings, with the understanding that the present disclosure is to be considered an exemplification of the principles of the disclosure, and is not intended to limit the disclosure to that illustrated and described herein. It is to be fully recognized that the different teachings of the embodiments discussed herein may be employed separately or in any suitable combination to produce desired results.
Unless otherwise specified, use of the terms “connect,” “engage,” “couple,” “attach,” or any other like term describing an interaction between elements is not meant to limit the interaction to a direct interaction between the elements and may also include an indirect interaction between the elements described. Unless otherwise specified, use of the terms “up,” “upper,” “upward,” “uphole,” “upstream,” or other like terms shall be construed as generally away from the bottom, terminal end of a well; likewise, use of the terms “down,” “lower,” “downward,” “downhole,” or other like terms shall be construed as generally toward the bottom, terminal end of the well, regardless of the wellbore orientation. Use of any one or more of the foregoing terms shall not be construed as denoting positions along a perfectly vertical axis. In some instances, a part near the end of the well can be horizontal or even slightly directed upwards. Unless otherwise specified, use of the term “subterranean formation” shall be construed as encompassing both areas below exposed earth and areas below earth covered by water such as ocean or fresh water.
Careful analysis of distributed sensing data may allow engineers and geoscientists to better understand the behavior of reservoir rock, fluids, and pressure systems to give quantitative values for effective management of hydrocarbon production. This analysis relies on the ability to sample strain and temperature values along the entire borehole trajectory accurately with fine sampling and space and time.
However, current data processing methods do not provide effective data use because the high-resolution measurements generate extremely large data volumes in a short period of time. A few days of data for a typical hydraulic fracturing monitoring task can easily be several tens of terabytes in size. Permanent fiber installations can be used to repeat measurements over time to assess changes in the reservoir or to detect fluid flow rates and compositions. When oil and gas production lasts for a period of years, the problem may be exacerbated. Therefore, effective data analysis must be fast, and ideally will be able to reduce data volumes.
Additional challenges arise because the data may depend on multiple physical processes such as fluid flow, pressure changes, and fracture mechanics. Different processes may also depend on different material properties and on physical structures (e.g., pipes or fracture geometries) of different size and time scales. For example, consider the case of a fiber optic cable permanently installed in the cement layer outside a well subject to hydraulic fracturing. Common methods create several clusters of perforations in the casing pipe with the goal of generating, ideally, equivalent fracture systems from each. An important application of distributed sensing systems, such as distributed acoustic sensing (DAS), in this context is to attempt to measure the uniformity of the newly formed fracture systems. Once fractures begin to form, they will expand and propagate further into the rock formation over a period of several hours. Fluids are injected into the well to increase pressure and generate fractures, and solid particles (proppant) are also pumped into the well to flow into fractures and hold them open to enhance flow of oil or gas. Fluid and proppant flow can change over intervals on the order of minutes or seconds. In addition, the proppant flow rate often is increased in discrete steps. Thus at least some fluid flow behaviors will change on very short time scales, noting also the fracturing will sometimes propagate episodically in brief bursts.
These complex, multiscale (in space and time) physical systems may lead to another important challenge in data analysis: the measurements from the distributed sensing system are a composite of all the processes taking place in the location of the fiber, but in many cases only a subset of processes affected by a subset of spatiotemporal time scales are important for the task at hand. The data processing scheme may be more effective if it includes a tool that can extract the relevant data features for that task. These engineered features may then be well-suited for use in machine learning (ML) techniques to map them from the feature domain to output quantities providing feedback to guide the engineering tasks (e.g., hydraulic fracture operation designs, hydrocarbon production management, etc.).
In part because the adoption of the distributed sensing technology has accelerated rapidly in recent years, development of methods for extracting useful information from these large datasets is also in its initial stages. As noted above, the application of very low frequency analysis of DAS data for characterizing hydraulic fracture systems was introduced only several years ago. Analysis tends to rely on qualitative descriptions and a couple of data features, namely the time and position on the fiber optic cable where a fracture intersects a monitoring well.
The status of technology development for routine utilization of distributed sensing data to guide hydraulic fracturing programs and hydrocarbon production is therefore rather limited and can be summarized as follows: 1) Some common workflows apply filters or standard measures to try to generate features on signals from individual sensor locations one at a time; and 2) There are some initial developments in formulation of ML algorithms for applying distributed sensing to tasks associated with hydraulic fracturing or fluid flow monitoring.
A rigorous and effective approach to feature engineering for ML algorithms for these tasks that correctly considers both the spatial and temporal signal structures, and the differing spatial and temporal scales of physical phenomena generated fiber signal for relevant applications is not currently available.
Distributed sensing systems may collect densely sampled data measurements of strain and temperature along a fiber optic cable positioned within a wellbore. The collected data measurements can provide important constraints on fracture formation or multiphase fluid flow. Analysis of these data measurements is best done simultaneously to consider both the spatial and temporal variation of the complex physical processes taking place as well as their different physical scales. However, most processing schemes currently used only operate on individual sensor channel signals and the results do not incorporate spatial dependence. Embodiments of the system and method presented herein present a complete processing scheme that includes a method for feature engineering that extracts signals reflecting both spatial and temporal properties of the data, wherein the resulting features are sent to machine learning tools that use these features to generate diagnostics allowing wellbore operators to optimize field operations.
Distributed sensing systems play a vital role in the development and production of hydrocarbon resources by recording mechanical and temperature changes in the subsurface with high spatial and temporal resolution. The sensing architecture relies, in some embodiments, on a fiber optic cable through which a laser pulse is transmitted from an interrogator, and back-scattered energy is analyzed by the interrogator to quantify changes in strain or temperature. Measurement technologies routinely available include distributed acoustic sensing (DAS), distributed strain sensing (DSS) and distributed temperature sensing (DTS). Spatial and temporal sampling vary depending on the specific application, but typical values are 1 min. and 0.001 sec., for example. Advances in related technologies are likely to continue to improve spatial resolution for hydrocarbon production tasks.
In some embodiments, the fiber optic cable may be installed permanently outside a well casing, providing the opportunity to sample borehole conditions at any time during the life of the well. The resulting data may provide insights into fluid flow regimes. The fiber optic cable may be positioned along an entire length of the wellbore, which provides a critical advantage over data from a sparse set of individual instruments, such as, e.g., flow meters, that cannot thoroughly provide both spatial and temporal variations associated with fluid behaviors. Distributed sensing systems such as distributed acoustic sensing (DAS), distributed strain sensing (DSS) and distributed temperature sensing (DTS) data may also be acquired with fiber optic cables installed temporarily via a retrievable wireline or an inexpensive disposable fiber. These installations are well-suited for monitoring hydraulic fracturing programs and are utilized routinely to assess the effectiveness of the design and execution of fracturing. For example, low frequency DAS data detects the mechanical deformation of the reservoir medium around a well equipped with a fiber optic cable, and both DAS and DTS systems help constrain the uniformity of fracture response with position in a stage. The development of more quantitative methods to infer fracture flow and mechanical properties is beginning also and will continue to progress. The datasets are exceptionally large because of the high-resolution spatiotemporal sampling and because they are in many cases measured continuously.
The exceptionally large datasets create a significant challenge in analysis since large data volumes require major computational resources. In addition, resulting measurements and analyses should be provided in a real time or near real time approach to guide decisions optimizing hydrocarbon production or hydraulic fracturing procedures. Machine learning (ML) algorithms provide an option for solving problems analyzing exceptionally large data sets, but may function more quickly with smaller data volumes. Further, embodiments of the methods provided herein may be more effective if input measures are well designed, a process referred to herein as feature engineering. Provide herein are embodiments of data that are preprocessed to extract measures that are closely related to phenomena of interest of a system and method that both reduces distributed sensing data volumes and identifies data features that allow rapid and reliable application of ML and other algorithms to guide decision making in the development of hydrocarbon reservoirs.
Embodiments presented provide a solution that receive complex, densely sampled amounts of DAS, DSS or DTS data and computes a small set of representative signals, referred to hereafter as “modes,” that decompose the complex, densely sampled data into a smaller set of model signals that quantify the behavior of the physical system on different scales in space and time.
Embodiments of the method are data-driven, and generated quantities include a measure of variation of signal strength with distance along the fiber optic cable and frequency parameters that quantify how rapidly the signal varies in time as well as its growth or decay rate. The result is therefore a relatively fast extraction of physically meaningful features that provide greater insight than the complete dataset and in turn facilitate further analysis with ML or other algorithms. Data analysis may provide measures that can be used for any wellbore application utilizing distributed sensing in any stage of reservoir development, and reducing data volumes enable more rapid distribution of the analyzed data. Some embodiments of the method may also be applied to any sensor network, such as sensor arrays, seismometers or tilt meters.
In some embodiments, the interrogator in the signal acquisition system 112C can be directly coupled to the fiber optic cable 113C. Alternatively, the interrogator may be coupled to a fiber stretcher module in the signal acquisition system 112C, wherein the fiber stretcher module is coupled to the fiber optic cable 113C. The signal acquisition system 112C can receive measurement values taken and/or transmitted along the length of the fiber optic cable 113C. In addition, the signal acquisition system 112c can receive measurement values from a bottomhole gauge carrier 114C that can transmit measurements through the fiber optic cable 113C. In some embodiments, the bottomhole gauge carrier 114C can include a pressure temperature gauge and can be inside of, or replaced by, a wireline scanning tool.
Measurement values transmitted through the fiber optic cable 113C can be sent to the signal acquisition system 112C. The interrogator of the signal acquisition system 112C may be electrically connected to a digitizer to convert optically-transmitted measurements into digitized measurements. A computing device 110C can collect the electrically-transmitted measurements from the signal acquisition system 112C using a connector 125C. The computing device may have one or more processors and a memory device to analyze the measurements and graphically represent analysis results on a display device 150C. In addition, the computing device 110C can communicate with components attached to the fiber optic cable 113C. For example, the computing device 110C can send control signals to the bottomhole gauge carrier 114C to modify gauge measurement parameters. Additionally, in some embodiments, at least one processor and memory device can be located downhole for the same purposes. With the fiber optic cable 113C positioned inside a portion of the borehole 103C, the signal acquisition system 112C can obtain information associated with the subterranean formation 102C based on seismic/acoustic disturbances (e.g., seismic disturbances caused by the seismic source 115C).
Distributed fiber optic sensing systems measure light signals from a laser pulse transmitted into the fiber optic cable 113D by an interrogator device. Back-scattered light from that pulse is sampled by the interrogator using one of several techniques that in turn provide measurements of mechanical or temperature changes in the medium in which the fiber is emplaced. The temperature of fluids pumped down a well from the surface may be different temperature from that of in situ fluids in the subsurface, with the difference increasing with depth. Detection of anomalous temperature values can thus be used as a tool to gain insights into the presence or absence of hydrocarbon reservoir fluids within the borehole, which may also helps guide strategies for hydrocarbon production.
Initial use of distributed sensing systems, such as DAS applications included both vertical seismic profiling (VSP) and monitoring of hydraulic fracturing activities. VSP experiments generate seismic waves at the Earth's surface and record waves propagating into the subsurface to infer properties of rock layers, including hydrocarbon reservoirs. Traditional VSP data acquisition recorded signals on a relatively small number of individual sensors (geophones); while this set of sensors can be moved within the borehole, this may lead to long acquisition times, since the surface source of waves must be repeated for each depth range. In contrast, the fiber optic cable may be located along the entire length of the borehole, accelerating data acquisition and reducing costs. The same motivations apply for the monitoring of seismic waves generated in hydraulic fracturing experiments. While VSP experiments use an artificial active source of seismic waves which is controlled by the data acquisition team, hydraulic fracturing monitoring commonly relies on passive using signals generated naturally in the subsurface by the formation of hydraulic fractures in the rock medium around the borehole. These weak signals are generated by shear motion on naturally occurring surfaces around the developing hydraulic fracture system and are called micro seismic events. Data processing schemes estimating the location and fracture processes of these events provide important insights to guide fracture engineers.
The DAS systems, including interrogator and fiber optic cable, in early applications in a wellbore, recorded data with a low signal-to-noise ratio (SNR) compared to the geophones. For this reason, the early DAS systems were limited in their ability to detect the weak seismic signals, thereby reducing their effectiveness in characterizing assessing the response of hydraulic fracture programs. However, several advances have taken place in the last several years to accelerate the routine adoption of DAS data. First, improvements in both interrogators and fiber optic cable technologies have improved the SNR in recorded datasets, creating data quality comparable to traditional geophone data. Furthermore, the DAS system records data with a far greater frequency bandwidth than geophone systems, ranging from around 0.001 Hz to about 10,000 Hz, for example. Micro seismic signals have frequency content around 100 to 200 Hz, but it was discovered that analysis of data at frequencies less than 1 Hz provided significant additional insights. Specifically, the low frequency DAS measures measure deformation of the rock formation caused by a developing hydraulic fracture system, including a direct detection of when and where a fracture system intersects a monitor well with a DAS fiber optic cable. The timing of the intersection quantifies the speed of propagation of the hydraulic fracture system in the subsurface, while the position shows its orientation. These are direct measures of the hydraulic fracture system responsible for movement of hydrocarbons in the reservoir layer, in contrast to the indirect insights provided by micro seismic event analysis. As a result, DAS has recently been applied in the production of oil and gas from unconventional reservoirs where hydraulic fracturing is an essential part of reservoir development.
DSS extracts different measures of the laser signal generated by the interrogator that provides estimates of material deformation, strain, over longer time periods such as days or months where DAS is less effective. Typical implementations measure strain with lower SNR than DAS and the application of low frequency DAS has been commonly used for characterization of fracturing stages lasting several hours. However, there are important potential applications for DSS in the petroleum industry, including long term monitoring of deformation associated with both hydrocarbon production and carbon dioxide geosequestration, where waste carbon dioxide is injected into depleted petroleum reservoirs. More recent DSS technologies offer promise of improved spatial resolution and SNR that may provide important contributions to fracturing applications.
Distributed sensing utilizing fiber optic cables has become an important part of many applications for the petroleum industry. DTS measures temperature fluctuations that can be related to production of hydrocarbons. DAS measures strain (extension, shortening along the fiber optic cable) caused by mechanical deformation; it can detect high frequency seismic waves or low frequency, quasi-static deformation associated with development of hydraulic fracture systems. Vibrations and oscillations associated with fluid flow in boreholes can also be detected. DSS measures longer term strain and can be applied to carbon dioxide sequestration monitoring and other tasks.
Advances in technology leading to faster, more accurate analysis providing quantitative insights into fracturing or fluid flow, for example, may provide significant economic value. In many tasks where real time decisions must be made, such as the implementation and revision of hydraulic fracturing designs, computational speed is especially important, especially in systems receiving large volumes of data generated by distributed sensing systems.
Referring now to
Embodiments of the method and systems presented herein are shown with distributed sensing systems such as sensors along a fiber optic cable or alternatively an array of sensors, but the systems and methods presented herein may also be used with discrete measuring devices of any type.
Some embodiments of the distributed sensing system 300 may include a graphical user interface consistent with other acquisition and processing software currently used, and may provide a report which may be delivered to customers along with other diagnostics and analytic information.
In step 405, data is received from a distributed sensing system. In step 410, as the data is received, feature engineering (e.g., data preprocessed to extract measures that are closely related to an application or behavior of interest) is applied to a sliding time window, delta t (dt), with a predefined length of time. This value of dt will depend on which wellbore application or behavior is of interest, applying larger values for lower frequency phenomena. The increment in the start time of this time window may also be defined according to the behavior or application of interest. For example, processing might utilize data in a time window with length of 10 sec for time points starting at increments of dt=1 sec. For each time window, the modified DMD algorithm may be applied and repeated until all of the steps 415 through 435 are completed for each data set. At a first step 415 of the repeated steps, a singular value decomposition (SVD) may be applied to a data array to output intermediate results describing the data array. SVD results may include the singular values and corresponding left and right matrices U and V, respectively, which are the key quantities for estimation of a mathematical operator predicting a set of signals (modes) depending on position on the fiber and on time that correspond to unique frequency values. At step 420, a mathematical operator is computed for predicting spatiotemporal signal evolution of the data and generate a number of modes. Each mode may be associated with a parameter measuring the growth or decay with time of the mode. Each mode may represent part of the temperature or strain variation of the measured system with a unique spatiotemporal behavior. Because the mode signals may be in general complex-valued functions, one challenge is how to best extract simple values that can be applied in subsequent analysis. Steps 415 and 420 combined represent customization of signal processing such as dynamic mode decomposition, in this embodiment, to extract measures that are physically meaningful and applicable for ML tasks. These steps provide for effective usage in wellbore environments where the fiber data includes a combination of DTS or DAS, different values with distinct numerical ranges.
At step 425, using the mathematical operator, a selected mode of the number of modes is extracted and used as input to subsequent analysis steps, which may, in some embodiments, be a ML implementation that derives quantitative values that can in turn be utilized to guide field operations. A key aspect of this approach is that approximating the original data using a subset of modes may greatly reduce the data volume required for subsequent operations. As a result, operations requiring transmission of data may benefit from accelerated computations.
At step 430, a behavior in the wellbore is quantified based on the selected mode. In some embodiments, the behavior in the wellbore includes temperature variation in the wellbore, strain variation in the wellbore, or pressure in the wellbore. In the illustrated example, the behavior is perforation response in the wellbore. Once the behavior is quantified, at a step 435, the results are sent to an oilfield or wellbore operator to update operational parameters, such as, e.g., fracturing parameters, within the wellbore. At a step 440, the loop of steps 415 through 435 are repeated for each interval of data, incremented by dt, for each different segment of time.
While the method 400 may be applied to comparable problems such as the detection of flow patterns and currents in the ocean, the example embodiment presented in
The computer 800 also includes a controller 825. The controller 825 may perform one or more of the functionalities described herein. In some embodiments, the controller 825 may be coupled with a wellbore system and with a distributed sensing system within the wellbore. The controller 825 may be configured to receive data from a plurality of sensors positioned along various depths of the wellbore. In some embodiments the sensors may be incorporated in a fiber optic cable positioned adjacent one or more casings in the wellbore, either within a production casing, between a production and outer casing, or external the outer casing. Dynamic mode decomposition may be applied to the data for a determined amount of modes. The data may then be analyzed to determine fracture properties within the wellbore. The data analysis results may then be sent to an operator for the wellbore and operational properties of the wellbore may be adjusted. Any one of the previously described functionalities may be partially (or entirely) implemented in hardware and/or on the processor 805. For example, the functionality may be implemented with an application specific integrated circuit, in logic implemented in the processor 805, in a co-processor on a peripheral device or card, etc. Further, realizations may include fewer or additional components not illustrated in
An analysis sequence like that outlined for the previous case may be applied when the monitor well equipped with the fiber optic cable is located at some distance from the treatment well subjected to hydraulic fracturing. While the general steps of the methods are the same, the extraction of a mode feature may be optimized for the very low frequency signals indicative of hydraulic fractures approaching the monitor well. Reduction of data volumes can be greater given these low frequencies. The engineered features (modes) can be applied in subsequent ML tools to identify fractures, predict when they will intersect the monitor well and estimate geometry.
Another embodiment follows the same structure as the first case, except that DTS and DAS data are combined for analysis of perforation cluster uniformity. The computation of modes can utilize a data array combining multiple data types, and ML algorithms routinely do so. When both data types are available and required features are engineered, the invention will provide enhanced insight into fracture response.
Fluid motion will induce strain variations that can be detected by DAS, and the signal will have some dependence on the amounts of oil, gas, and water present. In addition, borehole features such as inflow devices, changes in casing diameter or other instrumentation will generate larger amplitude signals that can be detected by DAS. This embodiment applies the feature extraction step to generate modes measuring the spatial and temporal variation of flow-related strain generated along the borehole and at the features noted previously that may induce turbulence and more complex flow phenomena.
The ML algorithm utilized to estimate values such as flow rate or fluid composition using these engineered features will require supplementary training data. For this application, the ML system will be trained on a combination of laboratory and available numerical simulation results comparable to the field setting. The same feature engineering will be applied to the training data for this purpose.
In another embodiment, the quantification of fluid flow may combine modal features extracted from both DAS and DTS data to identify variations in fluid flow. The incorporation of DTS will allow identification of positions along the fiber where larger volumes of formation fluid enter the borehole.
Aspects disclosed herein include:
Aspect A: A method comprising: receiving data of measurements from a distributed sensing system having sensors distributed along different depths of a wellbore formed in a subsurface formation; and performing signal processing of the data to output a number of modes, wherein each mode includes a subset of the data that quantifies behavior of at least one of a fluid in the subsurface formation and a rock in the subsurface formation on a different combination of locations in the wellbore and timing of the measurements.
Aspect B: a system, comprising: a distributed sensing system having sensors distributed along different depths of a wellbore formed in a subsurface formation; a processor; and a non-transitory computer readable medium having instructions stored thereon that are executable by the processor to cause the processor, receive measurements of data from the distributed sensing system; and perform signal processing of the data to output a number of modes, wherein each mode includes a subset of the data that quantifies behavior of at least one of a fluid in the subsurface formation and a rock in the subsurface formation on a different combination of locations in the wellbore and timing of the measurements.
Aspect C: a non-transitory, computer-readable medium having instructions stored thereon that are executable by a processor to perform operations comprising: receiving data of measurements from a distributed sensing system having sensors distributed along different depths of a wellbore formed in a subsurface formation; and performing signal processing of the data to output a number of modes, wherein each mode includes a subset of the data that quantifies behavior of at least one of a fluid in the subsurface formation and a rock in the subsurface formation on a different combination of locations in the wellbore and timing of the measurements.
Aspects A, B, and C may have one or more of the following additional elements in combination:
Those skilled in the art to which this application relates will appreciate that other and further additions, deletions, substitutions and modifications may be made to the described embodiments.