Converting borehole images into three dimensional structures for numerical modeling and simulation applications

Information

  • Patent Grant
  • 11954800
  • Patent Number
    11,954,800
  • Date Filed
    Tuesday, December 14, 2021
    2 years ago
  • Date Issued
    Tuesday, April 9, 2024
    24 days ago
Abstract
A computer-implemented method, medium, and system for converting borehole images into three dimensional structures for numerical modeling and simulation applications are disclosed. In one computer-implemented method, multiple CT-scan images of a core sample of a rock are received, where the core sample includes a borehole, and the multiple CT-scan images are cross-section images of the core sample at multiple depths of the borehole. A triangulation process is performed on pixels of each CT-scan image and with respect to each of multiple circumferential position angles. Multiple radii of the borehole corresponding to the multiple circumferential position angles are determined for each CT-scan image. Multiple nodal coordinates of 3D numerical model mesh of the borehole are generated based on the multiple radii of the borehole. An advisory on drilling window limits of mud weight is provided based on the multiple nodal coordinates of the 3D numerical model mesh of the borehole.
Description
TECHNICAL FIELD

The present disclosure relates to computer-implemented methods, medium, and systems for converting borehole images into three dimensional structures for numerical modeling and simulation applications.


BACKGROUND

Quantitative description of wellbore failure is conventionally provided using mechanical multi-arm caliper logs, which provide radial measurements at four circumferential angles (0°, 90°, 180°, 270°) in their most common designs. On the other hand, drilling operations and supporting lab-based activities produce a substantial amount of data in the form of images. In the field, imaging tools are routinely run into the wellbore to extract information about the subterranean rock formations being drilled in the form of image logs. These imaging tools have a lot of variations in terms of imaging techniques and the format of produced images. The most common image logs are either resistivity based or ultrasonic-based. In laboratory environments, when rock core samples are tested for the purpose of measuring their mechanical properties and strength, different imaging techniques can be utilized to monitor the progression of failure in the rock matrix.


SUMMARY

The present disclosure involves computer-implemented method, medium, and system for converting borehole images into three dimensional structures for numerical modeling and simulation applications. One example computer-implemented method includes receiving multiple CT-scan images of a core sample of a rock, where the core sample of the rock includes a borehole, and the multiple CT-scan images are cross-section CT-scan images of the core sample of the rock at multiple depths of the borehole. A triangulation process is performed on pixels of each of the multiple CT-scan images for each of the multiple CT-scan images and with respect to each of multiple circumferential position angles. Multiple radii of the borehole corresponding to the multiple circumferential position angles are determined for each of the multiple CT-scan images. Multiple nodal coordinates of 3D numerical model mesh of the borehole are generated based on the multiple radii of the borehole of each of the multiple CT-scan images and using a meshing function. An advisory on drilling window limits of mud weight is provided for avoiding rock failure of a wellbore, based on the multiple nodal coordinates of the 3D numerical model mesh of the borehole.


While generally described as computer-implemented software embodied on tangible media that processes and transforms the respective data, some or all of the aspects may be computer-implemented methods or further included in respective systems or other devices for performing this described functionality. The details of these and other aspects and implementations of the present disclosure are set forth in the accompanying drawings and the description below. Other features, objects, and advantages of the disclosure will be apparent from the description and drawings, and from the claims.





DESCRIPTION OF DRAWINGS


FIG. 1 depicts an environment architecture of an example computer-implemented system that can execute implementations of the present disclosure.



FIG. 2 illustrates an example CT-scan of a bored core sample showing the development of failure zones around the borehole, in accordance with example implementations of this disclosure.



FIG. 3 illustrates example digital image correlation (DIC) images showing the progress of rock failure, in accordance with example implementations of this disclosure.



FIG. 4A, FIG. 4B, FIG. 4C, and FIG. 4D illustrate an example process of triangulation used to calculate the borehole radii from images, in accordance with example implementations of this disclosure.



FIG. 5 illustrates example full radial measurements of a CT-scan of a failed borehole as a result of combining the horizontal and the vertical triangulation readings and the spline smoothing step, in accordance with example implementations of this disclosure.



FIG. 6A, FIG. 6B, and FIG. 6C illustrate two example CT-scans and the superimposed radii measurements, in accordance with example implementations of this disclosure.



FIG. 7 illustrates an example mapping of the location and magnitude of borehole failure points, in accordance with example implementations of this disclosure.



FIG. 8A and FIG. 8B illustrate an example flow chart of a CT-scan borehole interpretation algorithm, in accordance with example implementations of this disclosure.



FIG. 9 illustrates an example of an ultrasonic image log from a depth location of a wellbore showing stress-induced wellbore enlargements, in accordance with example implementations of this disclosure.



FIG. 10A and FIG. 10B illustrate an example flow chart of an algorithm for calibrating ultrasonic image log interpretations using multi-arm caliper measurements, in accordance with example implementations of this disclosure.



FIG. 11A and FIG. 11B illustrate an example flow chart of an algorithm for applying the calibrated ultrasonic image log model, in accordance with example implementations of this disclosure.



FIG. 12 illustrates an example plot of the RGB numbers from an ultrasonic image log showing a correlation between the location of enlargements in the image and the trends in the RGB numbers, in accordance with example implementations of this disclosure.



FIG. 13 illustrates example results of the ultrasonic image log interpretation showing radial measurements in Cartesian and polar coordinates, in accordance with example implementations of this disclosure.



FIG. 14 illustrates example mechanical multi-arm caliper log readings and corresponding resistivity-based image log, in accordance with example implementations of this disclosure.



FIG. 15A, FIG. 15B, and FIG. 15C illustrate an example flow chart of an algorithm for producing interpretations from resistivity image logs, in accordance with example implementations of this disclosure.



FIG. 16 illustrates an example original RGB number of an resistivity image log and the adjusted RGB values to account for the image gaps and other image noise, in accordance with example implementations of this disclosure.



FIG. 17 illustrates example results of the image log interpretations that are calibrated with mechanical caliper log readings in both Cartesian and polar coordinates, in accordance with example implementations of this disclosure.



FIG. 18A, FIG. 18B, and FIG. 18C illustrate an example process of converting the borehole shape interpretations from field and lab images into a mesh nodal coordinate, in accordance with example implementations of this disclosure.



FIG. 19 illustrates an example meshing function ability to reflect different borehole shapes based on CT-scan taken across different cross-sections of the core sample, in accordance with example implementations of this disclosure.



FIG. 20 illustrates an example definition of key-seating and the results of the meshing function, in accordance with example implementations of this disclosure.



FIG. 21 illustrates an example meshing of a static fracture, in accordance with example implementations of this disclosure.



FIG. 22 illustrates example plots of nodal coordinates of a mesh with finite boundary elements and a mesh with infinite boundary elements, in accordance with example implementations of this disclosure.



FIG. 23A, FIG. 23B, and FIG. 23C illustrate an example mesh created for modelling core samples, in accordance with example implementations of this disclosure.



FIG. 24 illustrates example recommendations of mud weights or downhole pressures required to prevent wellbore rock failure based on the output of the initial setup of a numerical model, in accordance with example implementations of this disclosure.



FIG. 25 illustrates an example of updating the wellbore shape and adjusting the structure of the numerical model mesh based on information from logging while drilling wellbore images or from shale shakers images, in accordance with example implementations of this disclosure.



FIG. 26 illustrates an example of updated recommendations of mud weights or downhole pressures required to prevent wellbore rock failure, in accordance with example implementations of this disclosure.



FIG. 27 illustrates example flow charts depicting the distinction between two processes to determine the pre-drilling mud weight and the while-drilling mud weight update, in accordance with example implementations of this disclosure.



FIG. 28 illustrates an example supervised training process that uses a numerical model output as training features and borehole image interpretations as training responses, in accordance with example implementations of this disclosure.



FIG. 29 is a flowchart illustrating an example of a method for implementing a conversion from borehole images into three-dimensional (3D) structures for numerical modeling, in accordance with example implementations of this disclosure.



FIG. 30 is a schematic illustration of example computer systems that can be used to execute implementations of the present disclosure.





DETAILED DESCRIPTION

With the recent advancements in image analysis, there lies a potential to utilize the different forms of available images for extracting valuable information for drilling engineering applications. Different image logs from the field and different images from lab experiments can help inform drilling geomechanics models of the patterns and limits of a borehole rock failure. These images can be used to construct three-dimensional (3D) structures before and after rock failure takes place. These structures can then be converted to 3D meshes, which in turn can be employed within a numerical model, such as a finite element model (FEM), to estimate the stress distribution around the structure. The end result of this process is a more accurate depictions of the drilled structures and a more accurate prediction of the rock failure limits. On the other hand, conventionally quantitative description of wellbore failure may not provide a comprehensive description of the wellbore shape as well as images can, as mechanical multi-arm caliper logs usually only provide radial measurements at four circumferential angles (0°, 90°, 180°, 270°) in their most common designs.


This disclosure describes technologies for implementing a conversion from borehole images into three dimensional structures for numerical modeling and simulation applications. In some implementations, image analysis techniques can provide the ability to quantitatively determine the extent of wellbore wall rock failure from images. The quantitative description of failure from images can be used to provide a node-based classification of rock failure, which can be used to correlate the classification to each separate node in the numerical model mesh. By providing this link to the numerical model, a more accurate mapping of actual failures is now possible. The end result is an integrated FEM and machine learning (ML) model, which is trained based on offset wells data or previous lab experiments to predict the limits for rock failure in new wells or experiments.


In some implementations, image analysis techniques can enable numerical models to reflect the effect of different drilling events as they occur through images produced from logging while drilling (LWD) tools. This can ensure that events that led to changes to the wellbore geometry and shape can be reflected in the model mesh. This while-drilling consideration of changes to the wellbore shape and structure can enable the rock strength limits and probability of failure be updated as drilling progresses.



FIG. 1 depicts an environment architecture of an example computer-implemented system 100 that can execute implementations of the present disclosure. In the depicted example, the example system 100 includes a client device 102, a client device 104, a network 110, and a cloud environment 106 and a cloud environment 108. The cloud environment 106 may include one or more server devices and databases (e.g., processors, memory). In the depicted example, a user 114 interacts with the client device 102, and a user 116 interacts with the client device 104.


In some examples, the client device 102 and/or the client device 104 can communicate with the cloud environment 106 and/or cloud environment 108 over the network 110. The client device 102 can include any appropriate type of computing device, for example, a desktop computer, a laptop computer, a handheld computer, a tablet computer, a personal digital assistant (PDA), a cellular telephone, a network appliance, a camera, a smart phone, an enhanced general packet radio service (EGPRS) mobile phone, a media player, a navigation device, an email device, a game console, or an appropriate combination of any two or more of these devices or other data processing devices. In some implementations, the network 110 can include a large computer network, such as a local area network (LAN), a wide area network (WAN), the Internet, a cellular network, a telephone network (e.g., PSTN) or an appropriate combination thereof connecting any number of communication devices, mobile computing devices, fixed computing devices and server systems.


In some implementations, the cloud environment 106 include at least one server and at least one data store 120. In the example of FIG. 1, the cloud environment 106 is intended to represent various forms of servers including, but not limited to, a web server, an application server, a proxy server, a network server, and/or a server pool. In general, server systems accept requests for application services and provides such services to any number of client devices (e.g., the client device 102 over the network 110).


In accordance with implementations of the present disclosure, and as noted above, the cloud environment 106 can host applications and databases running on host infrastructure. In some instances, the cloud environment 106 can include multiple cluster nodes that can represent physical or virtual machines. A hosted application and/or service can run on VMs hosted on cloud infrastructure. In some instances, one application and/or service can run as multiple application instances on multiple corresponding VMs, where each instance is running on a corresponding VM.


An example algorithm for lab-based imaging for borehole radial measurements is described next.


In some implementations, Lab-based images, for example CT-scans or digital image correlation (DIC) images, can provide information regarding rock failure because they are more easily interpreted than field-based images. Field-based images such as resistivity image logs are taken downhole in challenging environments due to high pressure, temperature, and drilling fluids noise, and the visual clarity of these images may not be high. Therefore, field-based images may not be visually assessed for the extent of rock failure. This may not be the case for lab-based images. In CT-scans, which are one of the forms of lab images with an example shown in FIG. 2, the location and the extent of rock failure around a borehole in a core sample can be determined by visually examining the image. Therefore the bored core CT-scan algorithm can be used to identify the location of failure and determine the magnitude of failure in terms of change to the borehole radius. An example of DIC images capturing the progress of rock failure is shown in FIG. 3.


In some implementations, since the algorithm deals with images, the data points in the image are pixels and the value for each point is the red-green-blue (RGB) color number. The algorithm can differentiate between the borehole and the rock matrix by first adjusting the contrast of the image so that the borehole void is black colored, while the rock matrix is light gray colored. The CT-scan image algorithm can use the concept of triangulation to assess failure as illustrated in FIG. 4A. Through this concept of triangulation, a pixel that is centralized in the borehole can be selected, which can then be used as the first vertex of a triangle. Since the borehole shape in FIG. 4B is not circular, a center cannot be defined. Instead, this vertex is arbitrarily defined as the pixel that satisfies the intersection of the longest horizontal diameter (LX) with the longest vertical diameter (LY) of the non-uniformly shaped borehole as shown in FIG. 4B. From this vertex, horizontal and vertical straight lines are drawn by selecting the pixels from the defined vertex to the borehole wall. Then, a hypotenuse for a right triangle is formed at a specified angle. Next, the length of the hypotenuse is calculated using the Pythagorean theory. This calculated hypotenuse is one radial measurement, which is assigned to the circumferential position of the corresponding pixels. The total number of borehole pixels defining the adjacent and the opposite legs of the right triangle, as shown by the horizontal (HDim) and vertical (VDim) boxes in FIG. 4A, can be used in the Pythagorean theory calculation. This basic calculation is shown below:

Radial Measurement for One Circumferential Position=√{square root over (HDim2+VDim2)}


In some implementations, this pixel-based measurement of length can be converted to an actual measurement of length by using the detected image resolution. This is done by using a reference CT-scan that depicts a uniform borehole with a known diameter. Next, the image pixels that define the borehole void, which are characterized by a black color RGB value, can be filtered out. Then, the total number of pixels in a line that intersects the borehole center can be determined. These values can be used in the followed formula to calculate the actual length of a pixel in mm:







Pixel


Actual


Length



(
mm
)


=


2
×
Borehole


Actual



Radius





(
mm
)



Total


Number


of


Pixels


in


the


LY


Line






In some implementations, the triangulation process is repeated both vertically and horizontally to provide full readings of the borehole radii as shown in FIG. 4C and FIG. 4D respectively. The number of the radii readings produced is dependent on the number of pixels available, i.e. image resolution, in the CT-scan image. Finally, the vertical and the horizontal radii readings are combined and a smoothing such as a spline smoothing can be applied to the curve to remove irregularities at the pixels corners. An example final result is shown in FIG. 5.


In some implementations, the same process can be repeated for two separate CT-scans to determine the extension of the failure zones from one CT-scan to the other. FIG. 6A, FIG. 6B, and FIG. 6C illustrate two CT-scans and the superimposed radii measurements. FIG. 7 shows the re-positioning of the two CT-scans from FIG. 6C to ensure the area of failure extension is accurately identified. FIG. 7 also shows a mapping of the failure extension zone, where the changes of radial measurements from one CT-scans to the other can be quantified at its specific circumferential location.



FIG. 8A and FIG. 8B illustrate an example flow chart describing the CT-scan borehole interpretation algorithm.


An example algorithm for field-based ultrasonic log imaging for borehole radial measurements is described next.


In some implementations, this algorithm converts a specific type of image logs, which is ultrasonic based, into caliper readings that cover the 360° of the wellbore circumference. Instead of relying on mechanical caliper logs, which provide radial measurements at only four circumferential angles (0°, 90°, 180°, 270°) in their most common designs, it now relies on images to produce radial measurements at all circumferential angles. As in the case with CT-scans, the resolution of radial measurements is dependent on the image log resolution.


In some implementations, the ultrasonic image logs are preferred for at least two reasons. First, unlike the resistivity-based image logs, ultrasonic images have no gaps, and therefore, can provide a more comprehensive description of the wellbore state. Second, they are available in logging while drilling (LWD) tools in the form of density-based images, therefore they can be used in a real-time setting or a while-drilling setting to feed new information into numerical models.


In some implementations, a difference in the interpretation process between lab-based images (CT-scans) and field-based image logs is that field-based image logs cannot be solely relied on to produce the interpretation. This is mainly due to the challenging environment in which these images are taken. This is also due to variations in image attributes from one commercial logging tool to the other. Therefore field image logs require more support information and validation than lab-based images. The support information used in this application is mechanical caliper log readings. For each image logging tool, the analysis of its images can be calibrated and validated against mechanical caliper measurements taken from the same interval where the images were produced. This ensures that the quantitative assessment of enlargements and tight spots from an image is validated using the mechanical caliper measurements of the same enlargements and tight spots. Once this process is performed, the calibrated algorithm can be used to interpret images from the same logging tool without running a mechanical caliper log every time an image log is produced.


In some implementations, this process is used for interpreting ultrasonic image logs by converting the RGB color number or values of each pixel to radial measurements. FIG. 9 illustrates an example of an ultrasonic image log. The area highlighted with a box in the middle section of FIG. 9 is the interval that is used to provide an example of an image log interpretation.



FIG. 10A and FIG. 10B illustrate an example algorithm for calibrating an ultrasonic image log interpretation. In some implementations, this algorithm uses data other than the image log itself to perform the calibration process. These data can be the bit size, multi-arm mechanical caliper log measurements, and a definition of the direction of the maximum in-situ stress. The bit size is used to assign physical dimension to an individual pixel size. The maximum in-situ stress direction is employed so that it can be correlated with the direction of wellbore enlargements or breakouts as observed in the image. The multi-arm mechanical caliper log measurements can be used to ascertain the extent of the radial depth of a darkly-colored breakout zone such as the ones shown as black in FIG. 9. They can also be used to ensure correct interpretation of tight spots, which are characterized by bright spots (shown as white in FIG. 9) on the log and a radius that is smaller than that of the bit size. This step determines Bou and Tsp, which are the breakout and the tight spot calibration constants respectively. The next step in the algorithm described in FIG. 10A is to extract the maximum red-color pixel value and the minimum blue-color pixel value. These two values can be used to determine the breakout and tight spot control constants (CBou and CTsp) as follows:








CB

o

u


=


Bit


size


Maximum


red


color


pixel


value



,
and







CT
sp

=



Bit


size


Minimum


blue


color


pixel


value


.






CBou and CTsp can be correlated to the identification of the most darkly colored region (shown as black in FIG. 9) in the image (which represents the deepest breakout) and the most brightly colored region (shown as white in FIG. 9) in the image (which represents the tightest spot in the hole). These constants, along with the calibration constants, can be used to calculate the breakout-exaggerated radii (rBO) and the tight spot exaggerated-radii (rTS) as follows:

rBO=Bou(Bit size−(Redi×CBou))+Bit size, and
rBO=Bou(Bit size−(Redi×CBou))+Bit size,

where Redi and Bluei are the maximum and minimum values for all pixels in a single horizontal line which defines the borehole full circumference. The final step is the calculation of a weighted average between rBO and rTS as follows:

Radius=WBO×rBO+WTS×rTS

where W_BO and W_TS are the average weights, which are determined through a trial and error process that involves matching the weighted average with the actual multi-arm mechanical caliper log measurements as shown in FIG. 8A and FIG. 8B. This calibration algorithm needs to be applied to each unique image logging tool to ensure that the images produced from the tool are correctly interpreted. The same process may potentially need to be repeated for a calibrated tool when it is run in a new environment.


In some implementations, once the calibration algorithm is applied to a certain imaging tool, the image produced by this tool in new hole sections or new wells can be interpreted to produce a full 360° radial measurements by utilizing the algorithm described in FIG. 11A and FIG. 11B.



FIG. 12 and FIG. 13 illustrate the results of the interpretation of the ultrasonic image log in FIG. 9. FIG. 12 illustrates the correlation between the RGB number and the placement of enlargements and tight spots. This correlation can be used along with calibrating values from a mechanical multi-arm caliper log to calculate the radial measurements of the wellbore at different directions. In some implementations, the number of radial measurements produced is dependent on the number of pixels available in the image log (i.e. image resolution). In the example shown in FIG. 12, the image log has resolution of 221 pixels per the 360° degrees around the wellbore, which equates to about one radius measurement for each 1.63° degrees around the circumference of the wellbore. FIG. 13 illustrates the final results of the image log interpretations that are calibrated with mechanical caliper log readings in both Cartesian and polar coordinates. When comparing the ultrasonic image log interval in FIG. 9 to the interpreted radial measurements in FIG. 13, it can be seen that the dark regions in the image that signify the presence of wellbore enlargements are also reflected as radial measurements that are higher than the bit radius.


An example algorithm for field-based resistivity log imaging for borehole radial measurements is described next.


In some implementations, this algorithm converts this type of image logs into caliper readings that cover the 360° of the wellbore. The main difference between sonic-based images and resistivity-based images is that resistivity images normally contain several gaps due to the space between the electrical pads of the resistivity image logging tool. Resistivity based image logs also differ from sonic-based images in the way a breakout (or wellbore enlargement) can be identified. In sonic images, changes in color are sufficient, however, in resistivity images, changes in color alone can be misleading as they can signify laminations, faults, natural, and induced fractures along with breakouts. This means that resistivity logs are efficient indicators of ‘physical features’ within the wellbore, but they are poor indicators of the spatial (specifically, radial) extension of these physical features. Fortunately, there's one distinguishing feature of breakouts in resistivity logs which is the lowered resolution of the image at that breakout orientation. The lower resolution at breakouts is due to the electrical pad of the logging tool being further away from the wellbore wall when the resistivity image measurements are taken. This change in color resolution is exploited in this image interpretation algorithm to identify the orientation of breakouts, still, it's not sufficient to assess the extent of the enlargement. For this issue, provided multi-arm caliper readings are used to correlate the radial extent at every location in the wellbore. The pixels RGB readings are feature scaled using the following formula to yield the needed radii:








Scaled



R

G

B


=


C

A


L
min


+

(




R

G


B

a

d

j



-

R

G


B
min





R

G


B
max


-

R

G


B
min






(


C

A


L
max


-

C

A


L
min



)


)



,





where CALmin and CALmax are minimum and maximum multi-arm mechanical caliper radius readings respectively, which are used for calibration. RGBadj is the adjusted RGB reading for filtering out noise and white gaps in the image. Using this method in interpreting image logs means that the availability of multi-arm caliper data is a necessity when resistivity images are used, which also means this analysis can't be done in real-time. This is to be expected since conventional resistivity-based image logs are not available through LWD in the same manner as density-based images.



FIG. 14 illustrates an example of a resistivity image log along with mechanical caliper log readings. The regions highlighted in the two boxes in the image log to the right are the low-resolution areas that signify the presence of wellbore enlargements. The area highlighted with a box in the mechanical caliper log to the left is the interval from which the image log to the right was taken.



FIG. 15A, FIG. 15B, and FIG. 15C illustrate an example flow chart of the algorithm for interpreting resistivity-based image logs. In some implementations, this algorithm uses data other than the image log itself to perform the interpretations process. These data can be the bit size, multi-arm mechanical caliper log measurements, and a definition of the direction of the maximum in-situ stress. The low-resolution zones can be defined using the circumferential angle ranges (θc1, θc2, θc3, θc4) where 1 and 2 define the starting and final angle of the first zone while 3 and 4 define the rage for the second zone. The RGB values can be adjusted to produce RGBadj for the purpose of filtering out noise and white gaps in the image. This adjustment process can use an upper cutoff value of 0 for each pixel green color value (Gcutoff), a lower value of 50 for each pixel red color value (Rcutoff), and a lower value of 0 for the subtraction of blue from red color values (R−Bcutoff).



FIG. 16 illustrates the original RGB number of the resistivity image log from FIG. 14 and the adjusted RGB values to account for the image gaps and other image noise. FIG. 17 illustrates the final results of the image log interpretations that are calibrated with mechanical caliper log readings in both Cartesian and polar coordinates. When comparing the resistivity image log interval in FIG. 14 to the interpreted radial measurements in FIG. 17, it can be seen that the low resolution regions in the image that signify the presence of wellbore enlargements are also reflected as radial measurements that are higher than the bit radius. Also, when examining the mechanical caliper readings in the interval highlighted in red to the left in FIG. 14, it can be seen that there is an agreement that the wellbore is fully enlarged at different directions.


An example algorithm for converting borehole radial measurements to 3d numerical model mesh is described next.


In some implementations, once the radii measurements of a borehole are produced by the image analyzer algorithms described in the previous sections (for CT-scans, ultrasonic image logs, and resistivity image logs), the meshing function can receive these measurements and calculates the nodal coordinates of the mesh based on them. This can be done by assigning a separate borehole radius measurement to each circumferential angle around the borehole. Then, the coordinates of each single line of nodes associated with each circumferential angle can be calculated with consideration of whether the line of nodes is placed at the center or at the boundary of an element in the mesh. This process is repeated for each radial line of nodes at all the specified vertical layers until the full coordinates describing the borehole or the wellbore and the formations it penetrates is fully calculated. The meshing function can perform this process based on lab images, CT-scans, ultrasonic image logs, and resistivity image logs as shown in FIG. 18A, FIG. 18B, and FIG. 18C.


In some implementations, this meshing function can also reflect the variation of the borehole shape along the axis of the borehole. For core samples, the mesh function reflects the different borehole shapes as described by CT-scans that are taken at different cross-sections of the core. The same goes for field-based images as the mesh can reflect the different shapes of the wellbore as described by the image log across different depths of the wellbore. An illustration of this function based on CT-scans is shown in FIG. 19.


In some implementations, this meshing function can also reflect different wellbore features, and this is specific to field-based (as opposed to lab-based) images. One wellbore feature can be key-seating, which is the enlargement of one side of the wellbore due to having the drillstring rest on that side. The meshing function can reflect the dimensions of the key-seat enlargement on the coordinate of the wellbore. An illustration of an example definition of key-seating and the results of the meshing function are shown in FIG. 20.


In some implementations, this meshing function can also reflect a fracture. The mesh function takes input such as the fracture aperture, length, tortuosity, and placement within the wellbore so that the geometry of the fracture can be reflected. Based on this, the mesh considers the fracture a part of the wellbore, which makes it exposed to the wellbore pressure. This way of meshing a fracture assumes that the fracture is a static feature of the wellbore. While this assumption may not be applicable for fracture propagation problems, it can be applied to other scenarios as it can be used to reflect the effect of drilling induced fractures, natural fractures, lost circulation, and wellbore strengthening on the drilling window. An illustration of an example of meshing of a static fracture is shown in FIG. 21, where the left plot shows the introduction of fractures to a non-uniform wellbore and a depiction of the wellbore pressure acting on both the wellbore wall and the fracture face, and the right plot shows the placement of nodal coordinate for the mesh of fractured non-uniform wellbore.


In some implementations, this meshing function can also reflect the shape of the structure boundaries. When a mesh for a numerical model is created, the type of boundaries being used can be specified, and the type of boundaries being used can be reflected on the nodal coordinates calculated. The mesh function can consider a finite mesh boundary and an infinite mesh boundary. The finite mesh boundary means that the mesh elements at boundary of the structure, which will be subject to the outside stresses, are all fully formed elements. In one example, this fully formed element can be a 20-node brick element. As for the infinite mesh boundary, the mesh nodal coordinates are created for those that consider an infinite element, which can be a 20-node brick element with one of the cube faces removed resulting in a 12-node infinite element. The removed face signifies the infinite extension of the subterranean geologic formation being modeled. The mesh function can reflect this infinite nature of these elements by removing all nodes that would have described the removed face. The difference between these two boundaries as produced by the mesh function is shown in FIG. 22.


In some implementations, the setup for the structure boundaries within the mesh can be altered when modelling core samples in experiments instead of wells in the field. A specialized meshing function can be created to model the core sample that are discussed in the sections for CT-scan image based algorithm. As these core samples have round boundaries on two side and straight slabbed boundaries on the other two sides, the mesh function places finite element in all sides, but in a manner that mimics the core boundary shape. An illustration of the mesh created for these core samples is shown in FIG. 23A, FIG. 23B, and FIG. 23C.


Example applications of the aforementioned numerical models are described next.


In some implementations, one application of the aforementioned numerical models is providing an advisory on the drilling window limits. The numerical model, which is setup based on the image algorithms and the meshing function described in this disclosure, can provide recommendations of the maximum and minimum allowable mud weight for safe and optimal operations. These mud weights can be determined for the purpose of avoiding wellbore rock failure. Although drilling window advisory systems are common in the industry, some are limited as they produce static recommendations or pre-drilling recommendations. Some existing models lack the ability to update drilling window recommendations in response to commonly occurring drilling events in a dynamic and deterministic manner. The numerical models supported by the image algorithms and the meshing function described in this disclosure can consider the influence of commonly occurring drilling events through the input provided from the shale shakers analysis.



FIG. 24 illustrates example pre-drilling recommendations for the drilling window. In some implementations, the drilling window recommendation can be updated based on the input from logging while drilling wellbore images or from the shale shakers image analysis. Through this analysis, the wellbore structure mesh can be updated as shown in FIG. 25. This updated mesh can be inserted into the numerical model described in this disclosure for the purpose of providing the new mud weights limits or downhole pressure required for preventing wellbore failure. An example of the updated output of the model, which relates to recommending mud weights for preventing wellbore rock failure is shown in FIG. 26. Flow charts depicting the distinction between the two processes to determine the pre-drilling mud weight and the while-drilling mud weight update are shown in FIG. 27.


In some implementations, another application of the aforementioned numerical models is improving the accuracy of borehole rock failure prediction. The image analysis algorithms described in this disclosure can be used to overcome simplifying assumptions in some existing drilling geomechanics modeling, and consequently to improve rock failure prediction beyond the use of the conventional failure criteria such as the Mohr-Coulomb, Mogi, and Lade criterion. The use of image analysis algorithms has an advantage over traditional methods, as the use of image logs analysis and re-meshing functions can enable the reflection of the actual shape of the wellbore on the numerical model mesh. Additionally, rather than relying on generalized and conventional failure criteria for predicting rock failure spatially around the wellbore, the numerical model described in this disclosure can use a statistical or a machine learning algorithm that is trained based on the outcome of borehole image logs analysis and the output of the numerical model. The image analysis can set the limits, distribution, and extent of boreholes rock failure for the machine learning algorithm, based on the failure outcome from previous wells or lab experiments.


In some implementations, the supervised training process of the machine learning algorithm can be performed as shown in FIG. 28 using the outcome of the image analysis algorithms. Based on this illustration, relevant information from offset wells can be gathered, which can then be used to model the circular (pre-failure) wellbore in the numerical model as shown in the left-bottom corner in FIG. 28. This can yield the stress distribution at each node in the mesh in the left-bottom corner, which can be represented by different stress invariants and scalar plastic strain. Consequently, this stress distribution can be used to generate an initial prediction of failure based on one of the aforementioned conventional failure criteria. The next step can be interpreting wireline image logs for each wellbore in the offset wells dataset and producing a mesh of the actual failure that had taken place (post-failure wellbore). This step is illustrated in the wellbore in the right bottom corner in FIG. 28. Finally, all data from the available offset wells can be fed into a machine learning algorithm, which can be decision tree based or a neural network, to enhance the prediction of failure. The final trained model can then be used to generate new predictions of failure for new wells. The main advantage here is that the prediction of failure from the trained model can more accurately describe both the circumferential distribution and radial extension of failure zones as opposed to predicting the critical breakout angle, which is produced from conventional modeling approaches and analytical solutions.



FIG. 29 illustrates an example method for implementing a conversion from borehole images into three-dimensional (3D) structures for numerical modeling.


At 2902, a computer system receives multiple CT-scan images of a core sample of a rock, where the core sample of the rock includes a borehole, and the multiple CT-scan images are cross-section CT-scan images of the core sample of the rock at multiple depths of the borehole.


At 2904, the computer system performs, for each of the multiple CT-scan images and with respect to each of multiple circumferential position angles, a triangulation process on pixels of each of the multiple CT-scan images.


At 2906, in response to performing the triangulation process for each of the multiple CT-scan images and with respect to each of the multiple circumferential position angles, the computer system determines, for each of the multiple CT-scan images, multiple radii of the borehole corresponding to the multiple circumferential position angles.


At 2908, the computer system generates, based on the multiple radii of the borehole of each of the multiple CT-scan images and using a meshing function, multiple nodal coordinates of a 3D numerical model mesh of the borehole.


At 2910, the computer system provides, based on the multiple nodal coordinates of the 3D numerical model mesh of the borehole, an advisory on drilling window limits of mud weight for avoiding rock failure of a wellbore, where the core sample is a rock sample from the wellbore.



FIG. 30 illustrates a schematic diagram of an example computing system 3000. The system 3000 can be used for the operations described in association with the implementations described herein. For example, the system 3000 may be included in any or all of the server components discussed herein. The system 3000 includes a processor 3010, a memory 3020, a storage device 3030, and an input/output device 3040. The components 3010, 3020, 3030, and 3040 are interconnected using a system bus 3050. The processor 3010 is capable of processing instructions for execution within the system 3000. In some implementations, the processor 3010 is a single-threaded processor. The processor 3010 is a multi-threaded processor. The processor 3010 is capable of processing instructions stored in the memory 3020 or on the storage device 3030 to display graphical information for a user interface on the input/output device 3040.


The memory 3020 stores information within the system 3000. In some implementations, the memory 3020 is a computer-readable medium. The memory 3020 is a volatile memory unit. The memory 3020 is a non-volatile memory unit. The storage device 3030 is capable of providing mass storage for the system 3000. The storage device 3030 is a computer-readable medium. The storage device 3030 may be a floppy disk device, a hard disk device, an optical disk device, or a tape device. The input/output device 3040 provides input/output operations for the system 3000. The input/output device 3040 includes a keyboard and/or pointing device. The input/output device 3040 includes a display unit for displaying graphical user interfaces.


Certain aspects of the subject matter described here can be implemented as a method. One or more CT-scan images of a core sample of a rock are received. The core sample of the rock includes a borehole, and the one or more CT-scan images are cross-section CT-scan images of the core sample of the rock at one or more depths of the borehole. A triangulation process is performed on pixels of each of the one or more CT-scan images for each of the one or more CT-scan images and with respect to each of one or more circumferential position angles. In response to the triangulation process being performed on pixels of each of the one or more CT-scan images for each of the one or more CT-scan images and with respect to each of one or more circumferential position angles, one or more radii of the borehole corresponding to the one or more circumferential position angles are determined for each of the one or more CT-scan images. One or more nodal coordinates of a three-dimensional (3D) numerical model mesh of the borehole are generated using a meshing function and based on the one or more radii of the borehole of each of the one or more CT-scan images. An advisory on drilling window limits of mud weight for avoiding rock failure of a wellbore is provided based on the one or more nodal coordinates of the 3D numerical model mesh of the borehole. The core sample is a rock sample from the wellbore.


An aspect taken alone or combinable with any other aspect includes the following features. After the one or more CT-scan images are received and before the one or more radii of the borehole corresponding to the one or more circumferential position angles are determined for each of the one or more CT-scan images, a contrast of each of the one or more CT-scan images is adjusted so that borehole void in each of the one or more CT-scan images is of a first color, and rock matrix surrounding the borehole void in each of the one or more CT-scan images is of a second color that is different than the first color.


An aspect taken alone or combinable with any other aspect includes the following features. The determining the one or more radii of the borehole corresponding to the one or more circumferential position angles for each of the one or more CT-scan images includes determining, for each of the one or more CT-scan images, by performing the triangulation process on the pixels of each of the one or more CT-scan images and with respect to one or more horizontal triangulation lines for each of the one or more circumferential position angles, a first plurality of radii of the borehole corresponding to the one or more circumferential position angles; determining, for each of the one or more CT-scan images, by performing the triangulation process on the pixels of each of the one or more CT-scan images and with respect to one or more vertical triangulation lines for each of the one or more circumferential position angles, a second plurality of radii of the borehole corresponding to the one or more circumferential position angles; and determining, for each of the one or more CT-scan images, by combining the first plurality of radii of the borehole and the second plurality of radii of the borehole, the one or more radii of the borehole corresponding to the one or more circumferential position angles.


An aspect taken alone or combinable with any other aspect includes the following features. After the one or more nodal coordinates of the 3D numerical model mesh of the borehole are generated and before the advisory on the drilling window limits of mud weight is provided, a numerical model of the borehole is determined based on the 3D numerical model mesh of the borehole, and a stress distribution around the borehole is determined based on the numerical model of the borehole.


An aspect taken alone or combinable with any other aspect includes the following features. The borehole has a non-uniform shape.


An aspect taken alone or combinable with any other aspect includes the following features. After the one or more of nodal coordinates of the 3D numerical model mesh of the borehole are generated, rock failure prediction of the wellbore is performed based on the one or more nodal coordinates of the 3D numerical model mesh of the borehole.


An aspect taken alone or combinable with any other aspect includes the following features. After the contrast of each of the one or more CT-scan images is adjusted and before the one or more radii of the borehole are determined for each of the one or more CT-scan images, calibrating a size of each of the one or more CT-scan images based on actual pixel size measurement from a reference CT-scan image generated by a device that generates the one or more CT-scan images. The reference CT-scan image includes a CT-scan image of a core sample of a second borehole with uniform shape and a known diameter.


Certain aspects of the subject matter described in this disclosure can be implemented as a non-transitory computer-readable medium storing instructions which, when executed by a hardware-based processor perform operations including the methods described here.


Certain aspects of the subject matter described in this disclosure can be implemented as a computer-implemented system that includes one or more processors including a hardware-based processor, and a memory storage including a non-transitory computer-readable medium storing instructions which, when executed by the one or more processors performs operations including the methods described here.


The features described can be implemented in digital electronic circuitry, or in computer hardware, firmware, software, or in combinations of them. The apparatus can be implemented in a computer program product tangibly embodied in an information carrier (e.g., in a machine-readable storage device, for execution by a programmable processor), and method operations can be performed by a programmable processor executing a program of instructions to perform functions of the described implementations by operating on input data and generating output. The described features can be implemented advantageously in one or more computer programs that are executable on a programmable system including at least one programmable processor coupled to receive data and instructions from, and to transmit data and instructions to, a data storage system, at least one input device, and at least one output device. A computer program is a set of instructions that can be used, directly or indirectly, in a computer to perform a certain activity or bring about a certain result. A computer program can be written in any form of programming language, including compiled or interpreted languages, and it can be deployed in any form, including as a stand-alone program or as a module, component, subroutine, or other unit suitable for use in a computing environment.


Suitable processors for the execution of a program of instructions include, by way of example, both general and special purpose microprocessors, and the sole processor or one of multiple processors of any kind of computer. Generally, a processor will receive instructions and data from a read-only memory or a random access memory or both. Elements of a computer can include a processor for executing instructions and one or more memories for storing instructions and data. Generally, a computer can also include, or be operatively coupled to communicate with, one or more mass storage devices for storing data files; such devices include magnetic disks, such as internal hard disks and removable disks; magneto-optical disks; and optical disks. Storage devices suitable for tangibly embodying computer program instructions and data include all forms of non-volatile memory, including by way of example semiconductor memory devices, such as EPROM, EEPROM, and flash memory devices; magnetic disks such as internal hard disks and removable disks; magneto-optical disks; and CD-ROM and DVD-ROM disks. The processor and the memory can be supplemented by, or incorporated in, ASICs (application-specific integrated circuits).


To provide for interaction with a user, the features can be implemented on a computer having a display device such as a cathode ray tube (CRT) or liquid crystal display (LCD) monitor for displaying information to the user and a keyboard and a pointing device such as a mouse or a trackball by which the user can provide input to the computer.


The features can be implemented in a computer system that includes a back-end component, such as a data server, or that includes a middleware component, such as an application server or an Internet server, or that includes a front-end component, such as a client computer having a graphical user interface or an Internet browser, or any combination of them. The components of the system can be connected by any form or medium of digital data communication such as a communication network. Examples of communication networks include, for example, a LAN, a WAN, and the computers and networks forming the Internet.


The computer system can include clients and servers. A client and server are generally remote from each other and typically interact through a network, such as the described one. The relationship of client and server arises by virtue of computer programs running on the respective computers and having a client-server relationship to each other.


In addition, the logic flows depicted in the figures do not require the particular order shown, or sequential order, to achieve desirable results. In addition, other operations may be provided, or operations may be eliminated, from the described flows, and other components may be added to, or removed from, the described systems. Accordingly, other implementations are within the scope of the following claims.


The preceding figures and accompanying description illustrate example processes and computer-implementable techniques. But system 100 (or its software or other components) contemplates using, implementing, or executing any suitable technique for performing these and other tasks. It will be understood that these processes are for illustration purposes only and that the described or similar techniques may be performed at any appropriate time, including concurrently, individually, or in combination. In addition, many of the operations in these processes may take place simultaneously, concurrently, and/or in different orders than as shown. Moreover, system 100 may use processes with additional operations, fewer operations, and/or different operations, so long as the methods remain appropriate.


In other words, although this disclosure has been described in terms of certain implementations and generally associated methods, alterations and permutations of these implementations and methods will be apparent to those skilled in the art. Accordingly, the above description of example implementations does not define or constrain this disclosure. Other changes, substitutions, and alterations are also possible without departing from the spirit and scope of this disclosure.

Claims
  • 1. A computer-implemented method for three-dimensional (3D) borehole numerical modeling, comprising: receiving a plurality of CT-scan images of a core sample of a rock, wherein the core sample of the rock comprises a borehole, and wherein the plurality of CT-scan images are cross-section CT-scan images of the core sample of the rock at a plurality of depths of the borehole;performing, for each of the plurality of CT-scan images and with respect to each of a plurality of circumferential position angles, a triangulation process on pixels of each of the plurality of CT-scan images;in response to performing, for each of the plurality of CT-scan images and with respect to each of the plurality of circumferential position angles, the triangulation process, determining, for each of the plurality of CT-scan images, a plurality of radii of the borehole corresponding to the plurality of circumferential position angles;generating, based on the plurality of radii of the borehole of each of the plurality of CT-scan images and using a meshing function, a plurality of nodal coordinates of 3D numerical model mesh of the borehole; andproviding, based on the plurality of nodal coordinates of the 3D numerical model mesh of the borehole, an advisory on drilling window limits of mud weight for avoiding rock failure of a wellbore, wherein the core sample is a rock sample from the wellbore.
  • 2. The computer-implemented method according to claim 1, further comprising: after receiving the plurality of CT-scan images and before determining, for each of the plurality of CT-scan images, the plurality of radii of the borehole corresponding to the plurality of circumferential position angles, adjusting a contrast of each of the plurality of CT-scan images so that borehole void in each of the plurality of CT-scan images is of a first color, and rock matrix surrounding the borehole void in each of the plurality of CT-scan images is of a second color that is different than the first color.
  • 3. The computer-implemented method according to claim 2, further comprising: after adjusting the contrast of each of the plurality of CT-scan images and before determining, for each of the plurality of CT-scan images, the plurality of radii of the borehole, calibrating a size of each of the plurality of CT-scan images based on actual pixel size measurement from a reference CT-scan image generated by a device that generates the plurality of CT-scan images, wherein the reference CT-scan image comprises a CT-scan image of a core sample of a second borehole with uniform shape and a known diameter.
  • 4. The computer-implemented method according to claim 1, wherein determining, for each of the plurality of CT-scan images, the plurality of radii of the borehole corresponding to the plurality of circumferential position angles comprises: determining, for each of the plurality of CT-scan images, by performing the triangulation process on the pixels of each of the plurality of CT-scan images and with respect to a plurality of horizontal triangulation lines for each of the plurality of circumferential position angles, a first plurality of radii of the borehole corresponding to the plurality of circumferential position angles;determining, for each of the plurality of CT-scan images, by performing the triangulation process on the pixels of each of the plurality of CT-scan images and with respect to a plurality of vertical triangulation lines for each of the plurality of circumferential position angles, a second plurality of radii of the borehole corresponding to the plurality of circumferential position angles; anddetermining, for each of the plurality of CT-scan images, by combining the first plurality of radii of the borehole and the second plurality of radii of the borehole, the plurality of radii of the borehole corresponding to the plurality of circumferential position angles.
  • 5. The computer-implemented method according to claim 1, further comprising: after generating the plurality of nodal coordinates of the 3D numerical model mesh of the borehole and before providing the advisory on the drilling window limits of mud weight: determining a numerical model of the borehole based on the 3D numerical model mesh of the borehole; anddetermining a stress distribution around the borehole based on the numerical model of the borehole.
  • 6. The computer-implemented method according to claim 5, further comprising: after generating the plurality of nodal coordinates of the 3D numerical model mesh of the borehole: performing rock failure prediction of the wellbore based on the plurality of nodal coordinates of the 3D numerical model mesh of the borehole.
  • 7. The computer-implemented method according to claim 1, wherein the borehole has a non-uniform shape.
  • 8. A non-transitory, computer-readable medium storing one or more instructions executable by a computer system to perform operations for three-dimensional (3D) borehole numerical modeling, the operations comprising: receiving a plurality of CT-scan images of a core sample of a rock, wherein the core sample of the rock comprises a borehole, and wherein the plurality of CT-scan images are cross-section CT-scan images of the core sample of the rock at a plurality of depths of the borehole;performing, for each of the plurality of CT-scan images and with respect to each of a plurality of circumferential position angles, a triangulation process on pixels of each of the plurality of CT-scan images;in response to performing, for each of the plurality of CT-scan images and with respect to each of the plurality of circumferential position angles, the triangulation process, determining, for each of the plurality of CT-scan images, a plurality of radii of the borehole corresponding to the plurality of circumferential position angles;generating, based on the plurality of radii of the borehole of each of the plurality of CT-scan images and using a meshing function, a plurality of nodal coordinates of 3D numerical model mesh of the borehole; andproviding, based on the plurality of nodal coordinates of the 3D numerical model mesh of the borehole, an advisory on drilling window limits of mud weight for avoiding rock failure of a wellbore, wherein the core sample is a rock sample from the wellbore.
  • 9. The non-transitory, computer-readable medium according to claim 8, wherein the operations further comprise: after receiving the plurality of CT-scan images and before determining, for each of the plurality of CT-scan images, the plurality of radii of the borehole corresponding to the plurality of circumferential position angles, adjusting a contrast of each of the plurality of CT-scan images so that borehole void in each of the plurality of CT-scan images is of a first color, and rock matrix surrounding the borehole void in each of the plurality of CT-scan images is of a second color that is different than the first color.
  • 10. The non-transitory, computer-readable medium according to claim 9, wherein the operations further comprise: after adjusting the contrast of each of the plurality of CT-scan images and before determining, for each of the plurality of CT-scan images, the plurality of radii of the borehole, calibrating a size of each of the plurality of CT-scan images based on actual pixel size measurement from a reference CT-scan image generated by a device that generates the plurality of CT-scan images, wherein the reference CT-scan image comprises a CT-scan image of a core sample of a second borehole with uniform shape and a known diameter.
  • 11. The non-transitory, computer-readable medium according to claim 8, wherein determining, for each of the plurality of CT-scan images, the plurality of radii of the borehole corresponding to the plurality of circumferential position angles comprises: determining, for each of the plurality of CT-scan images, by performing the triangulation process on the pixels of each of the plurality of CT-scan images and with respect to a plurality of horizontal triangulation lines for each of the plurality of circumferential position angles, a first plurality of radii of the borehole corresponding to the plurality of circumferential position angles;determining, for each of the plurality of CT-scan images, by performing the triangulation process on the pixels of each of the plurality of CT-scan images and with respect to a plurality of vertical triangulation lines for each of the plurality of circumferential position angles, a second plurality of radii of the borehole corresponding to the plurality of circumferential position angles; anddetermining, for each of the plurality of CT-scan images, by combining the first plurality of radii of the borehole and the second plurality of radii of the borehole, the plurality of radii of the borehole corresponding to the plurality of circumferential position angles.
  • 12. The non-transitory, computer-readable medium according to claim 8, wherein the operations further comprise: after generating the plurality of nodal coordinates of the 3D numerical model mesh of the borehole and before providing the advisory on the drilling window limits of mud weight: determining a numerical model of the borehole based on the 3D numerical model mesh of the borehole; anddetermining a stress distribution around the borehole based on the numerical model of the borehole.
  • 13. The non-transitory, computer-readable medium according to claim 12, wherein the operations further comprise: after generating the plurality of nodal coordinates of the 3D numerical model mesh of the borehole: performing rock failure prediction of the wellbore based on the plurality of nodal coordinates of the 3D numerical model mesh of the borehole.
  • 14. The non-transitory, computer-readable medium according to claim 8, wherein the borehole has a non-uniform shape.
  • 15. A computer-implemented system, comprising: one or more computers; andone or more computer memory devices interoperably coupled with the one or more computers and having tangible, non-transitory, machine-readable media storing one or more instructions that, when executed by the one or more computers, perform one or more operations for three-dimensional (3D) borehole numerical modeling, the one or more operations comprising: receiving a plurality of CT-scan images of a core sample of a rock, wherein the core sample of the rock comprises a borehole, and wherein the plurality of CT-scan images are cross-section CT-scan images of the core sample of the rock at a plurality of depths of the borehole;performing, for each of the plurality of CT-scan images and with respect to each of a plurality of circumferential position angles, a triangulation process on pixels of each of the plurality of CT-scan images;in response to performing, for each of the plurality of CT-scan images and with respect to each of the plurality of circumferential position angles, the triangulation process, determining, for each of the plurality of CT-scan images, a plurality of radii of the borehole corresponding to the plurality of circumferential position angles;generating, based on the plurality of radii of the borehole of each of the plurality of CT-scan images and using a meshing function, a plurality of nodal coordinates of 3D numerical model mesh of the borehole; andproviding, based on the plurality of nodal coordinates of the 3D numerical model mesh of the borehole, an advisory on drilling window limits of mud weight for avoiding rock failure of a wellbore, wherein the core sample is a rock sample from the wellbore.
  • 16. The computer-implemented system according to claim 15, wherein the one or more operations further comprise: after receiving the plurality of CT-scan images and before determining, for each of the plurality of CT-scan images, the plurality of radii of the borehole corresponding to the plurality of circumferential position angles, adjusting a contrast of each of the plurality of CT-scan images so that borehole void in each of the plurality of CT-scan images is of a first color, and rock matrix surrounding the borehole void in each of the plurality of CT-scan images is of a second color that is different than the first color.
  • 17. The computer-implemented system according to claim 15, wherein determining, for each of the plurality of CT-scan images, the plurality of radii of the borehole corresponding to the plurality of circumferential position angles comprises: determining, for each of the plurality of CT-scan images, by performing the triangulation process on the pixels of each of the plurality of CT-scan images and with respect to a plurality of horizontal triangulation lines for each of the plurality of circumferential position angles, a first plurality of radii of the borehole corresponding to the plurality of circumferential position angles;determining, for each of the plurality of CT-scan images, by performing the triangulation process on the pixels of each of the plurality of CT-scan images and with respect to a plurality of vertical triangulation lines for each of the plurality of circumferential position angles, a second plurality of radii of the borehole corresponding to the plurality of circumferential position angles; anddetermining, for each of the plurality of CT-scan images, by combining the first plurality of radii of the borehole and the second plurality of radii of the borehole, the plurality of radii of the borehole corresponding to the plurality of circumferential position angles.
  • 18. The computer-implemented system according to claim 15, wherein the one or more operations further comprise: after generating the plurality of nodal coordinates of the 3D numerical model mesh of the borehole and before providing the advisory on the drilling window limits of mud weight: determining a numerical model of the borehole based on the 3D numerical model mesh of the borehole; anddetermining a stress distribution around the borehole based on the numerical model of the borehole.
  • 19. The computer-implemented system according to claim 15, wherein the borehole has a non-uniform shape.
  • 20. The computer-implemented system according to claim 19, wherein the one or more operations further comprise: after generating the plurality of nodal coordinates of the 3D numerical model mesh of the borehole: performing rock failure prediction of the wellbore based on the plurality of nodal coordinates of the 3D numerical model mesh of the borehole.
US Referenced Citations (231)
Number Name Date Kind
2286673 Douglas Jun 1942 A
2757738 Ritchey Sep 1948 A
2509608 Penfield May 1950 A
2688369 Broyles Sep 1954 A
2719363 Richard et al. Oct 1955 A
2795279 Erich Jun 1957 A
2799641 Gordon Jul 1957 A
2805045 Goodwin Sep 1957 A
2848469 Kroll Aug 1958 A
3016244 Friedrich et al. Jan 1962 A
3103975 Hanson Sep 1963 A
3104711 Haagensen Sep 1963 A
3114875 Haagensen Dec 1963 A
3133592 Tomberlin May 1964 A
3137347 Parker Jun 1964 A
3149672 Joseph et al. Sep 1964 A
3169577 Erich Feb 1965 A
3170519 Haagensen Feb 1965 A
3200106 Dickson Aug 1965 A
3211220 Erich Oct 1965 A
3428125 Parker Feb 1969 A
3522848 New Aug 1970 A
3547192 Claridge et al. Dec 1970 A
3547193 Gill Dec 1970 A
3642066 Gill Feb 1972 A
3696866 Dryden Oct 1972 A
3750768 Suman, Jr. et al. Aug 1973 A
3862662 Kern Jan 1975 A
3874450 Kern Apr 1975 A
3931856 Barnes Jan 1976 A
3946809 Hagedorn Mar 1976 A
3948319 Pritchett Apr 1976 A
4008762 Fisher et al. Feb 1977 A
4010799 Kern et al. Mar 1977 A
4030548 Richardson et al. Jun 1977 A
4081030 Carpenter Mar 1978 A
4084637 Todd Apr 1978 A
4135579 Rowland et al. Jan 1979 A
4140179 Kasevich et al. Feb 1979 A
4140180 Bridges et al. Feb 1979 A
4144935 Bridges et al. Mar 1979 A
4193448 Jearnbey Mar 1980 A
4193451 Dauphine Mar 1980 A
4196329 Rowland et al. Apr 1980 A
4199025 Carpenter Apr 1980 A
4265307 Elkins May 1981 A
RE30738 Bridges et al. Sep 1981 E
4287946 Brieger Sep 1981 A
4301865 Kasevich et al. Nov 1981 A
4320801 Rowland et al. Mar 1982 A
4354559 Johnson Oct 1982 A
4373581 Toellner Feb 1983 A
4396062 Iskander Aug 1983 A
4412585 Bouck Nov 1983 A
4449585 Bridges et al. May 1984 A
4457365 Kasevich et al. Jul 1984 A
4470459 Copland Sep 1984 A
4476926 Bridges et al. Oct 1984 A
4484627 Perkins Nov 1984 A
4485868 Sresty et al. Dec 1984 A
4485869 Sresty et al. Dec 1984 A
4487257 Dauphine Dec 1984 A
4495990 Titus et al. Jan 1985 A
4498535 Bridges Feb 1985 A
4499948 Perkins Feb 1985 A
4508168 Heeren Apr 1985 A
4513815 Rundell et al. Apr 1985 A
4524826 Savage Jun 1985 A
4524827 Bridges et al. Jun 1985 A
4545435 Bridges et al. Oct 1985 A
4553592 Looney et al. Nov 1985 A
4576231 Dowling et al. Mar 1986 A
4583589 Kasevich Apr 1986 A
4589504 Simpson May 1986 A
4592423 Savage et al. Jun 1986 A
4612988 Segalman Sep 1986 A
4620593 Haagensen Nov 1986 A
4660636 Rundell et al. Apr 1987 A
4705108 Little et al. Nov 1987 A
4776410 Perkin et al. Oct 1988 A
4817711 Jearnbey Apr 1989 A
4981036 Curry et al. Jan 1991 A
5055180 Klaila Oct 1991 A
5068819 Misra et al. Nov 1991 A
5082054 Kiamanesh Jan 1992 A
5092056 Deaton Mar 1992 A
5236039 Edelstein et al. Aug 1993 A
5574371 Tabanou et al. Nov 1996 A
5612293 Swartwout et al. Mar 1997 A
5842149 Harell et al. Nov 1998 A
5890540 Pia et al. Apr 1999 A
5899274 Frauenfeld et al. May 1999 A
5947213 Angle Sep 1999 A
6041860 Nazzal et al. Mar 2000 A
6078867 Plumb et al. Jun 2000 A
6164126 Ciglenec et al. Dec 2000 A
6173795 McGarian et al. Jan 2001 B1
6180571 Sifferman et al. Jan 2001 B1
6189611 Kasevich Feb 2001 B1
6413399 Kasevich Jul 2002 B1
6544411 Varandaraj Apr 2003 B2
6678616 Winkler et al. Jan 2004 B1
6814141 Huh et al. Nov 2004 B2
7048051 McQueen May 2006 B2
7091460 Kinzer Aug 2006 B2
7109457 Kinzer Sep 2006 B2
7114562 Fisseler et al. Oct 2006 B2
7115847 Kinzer Oct 2006 B2
7131498 Campo et al. Nov 2006 B2
7279677 Ellis et al. Oct 2007 B2
7312428 Kinzer Dec 2007 B2
7331385 Symington Feb 2008 B2
7445041 O'Brien Nov 2008 B2
7461693 Considine et al. Dec 2008 B2
7484561 Bridges Feb 2009 B2
7562708 Cogliandro et al. Jul 2009 B2
7596481 Zamora Sep 2009 B2
7629497 Pringle Dec 2009 B2
7630872 Xia et al. Dec 2009 B2
7631691 Symington et al. Dec 2009 B2
7677673 Tranquilla et al. Mar 2010 B2
7828057 Kearl et al. Nov 2010 B2
7909096 Clark et al. Mar 2011 B2
8096349 Considine et al. Jan 2012 B2
8210256 Bridges et al. Jul 2012 B2
8457940 Xi et al. Jun 2013 B2
8526171 Wu et al. Sep 2013 B2
8548783 Dean et al. Oct 2013 B2
8678087 Schultz et al. Mar 2014 B2
8824240 Roberts et al. Sep 2014 B2
8925213 Sallwasser Jan 2015 B2
8960215 Cui et al. Feb 2015 B2
8962535 Welton et al. Feb 2015 B2
9217291 Batarseh Dec 2015 B2
9217323 Clark Dec 2015 B2
9353305 Jiang et al. May 2016 B1
9567819 Cavender et al. Feb 2017 B2
9765609 Chemali et al. Sep 2017 B2
9874806 Takahara et al. Jan 2018 B2
10088725 Umezaki Oct 2018 B2
10330915 Rudolf et al. Jun 2019 B2
10334437 Katsman et al. Jun 2019 B2
10400570 Erge et al. Sep 2019 B2
10641079 Aljubran et al. May 2020 B2
10927618 Albahrani et al. Feb 2021 B2
10941644 Aljubran et al. Mar 2021 B2
10982124 AlBahrani et al. Apr 2021 B2
11187068 Batarseh Nov 2021 B2
20030075339 Gano Apr 2003 A1
20040020693 Damhof et al. Feb 2004 A1
20040221985 Hill et al. Nov 2004 A1
20040256103 Batarseh Dec 2004 A1
20050199386 Kinzer Sep 2005 A1
20060076347 Kinzer Apr 2006 A1
20060102625 Kinzer May 2006 A1
20060106541 Hassan et al. May 2006 A1
20060144620 Cooper Jul 2006 A1
20060200328 Guo et al. Sep 2006 A1
20070000662 Symington et al. Jan 2007 A1
20070108202 Kinzer May 2007 A1
20070131591 Pringle Jun 2007 A1
20070137852 Considine et al. Jun 2007 A1
20070137858 Considine et al. Jun 2007 A1
20070153626 Hayes et al. Jul 2007 A1
20070181301 O'Brien Aug 2007 A1
20070187089 Bridges Aug 2007 A1
20070193744 Bridges Aug 2007 A1
20070204994 Wimmersperg Sep 2007 A1
20070261844 Cogliandro et al. Nov 2007 A1
20070289736 Kearl et al. Dec 2007 A1
20080070805 Munoz et al. Mar 2008 A1
20080073079 Tranquilla et al. Mar 2008 A1
20080173443 Symington et al. Jul 2008 A1
20090084554 Williamson et al. Apr 2009 A1
20090209825 Efinger et al. Aug 2009 A1
20090259446 Zhang et al. Oct 2009 A1
20090288820 Barron et al. Nov 2009 A1
20100071957 Huang et al. Mar 2010 A1
20100089583 Xu et al. Apr 2010 A1
20100186955 Saasen et al. Jul 2010 A1
20100282511 Maranuk Nov 2010 A1
20100326659 Schultz et al. Dec 2010 A1
20110011576 Cavender et al. Jan 2011 A1
20110153296 Sadlier et al. Jun 2011 A1
20110168395 Welton et al. Jul 2011 A1
20110312857 Amanullah et al. Dec 2011 A1
20120012319 Dennis Jan 2012 A1
20120075615 Niclass et al. Mar 2012 A1
20120123756 Wang et al. May 2012 A1
20120169841 Chemali et al. Jun 2012 A1
20120181020 Barron et al. Jul 2012 A1
20120273187 Hall Nov 2012 A1
20130008653 Schultz et al. Jan 2013 A1
20130037268 Kleefisch et al. Feb 2013 A1
20130126164 Sweatman et al. May 2013 A1
20130191029 Heck, Sr. Jul 2013 A1
20130213637 Kearl Aug 2013 A1
20130255936 Statoilydro et al. Oct 2013 A1
20130261032 Ladva Oct 2013 A1
20140032192 Zamora et al. Jan 2014 A1
20140034144 Cui et al. Feb 2014 A1
20140083771 Clark Mar 2014 A1
20140090846 Deutch Apr 2014 A1
20140116776 Trent et al. May 2014 A1
20140122035 Dean et al. May 2014 A1
20140151042 Faugerstrom et al. Jun 2014 A1
20140190695 van Zanten et al. Jul 2014 A1
20140231146 Nguyen Aug 2014 A1
20140231147 Bozso et al. Aug 2014 A1
20140278111 Gerrie et al. Sep 2014 A1
20140360778 Batarseh Dec 2014 A1
20150055438 Yan Feb 2015 A1
20150083422 Pritchard Mar 2015 A1
20150101864 May Apr 2015 A1
20150176400 Kulathu Jun 2015 A1
20150191640 Lee et al. Jul 2015 A1
20150267500 Van Dogen Sep 2015 A1
20160053572 Snoswell Feb 2016 A1
20160076357 Hbaeib et al. Mar 2016 A1
20160153240 Braga et al. Jun 2016 A1
20160247316 Whalley et al. Aug 2016 A1
20170044889 Rudolf et al. Feb 2017 A1
20170234104 James Aug 2017 A1
20170342776 Bullock et al. Nov 2017 A1
20180010419 Livescu et al. Jan 2018 A1
20180051548 Liu et al. Feb 2018 A1
20180119535 Shen et al. May 2018 A1
20180266226 Batarseh et al. Sep 2018 A1
20190257973 AlBahrani et al. Aug 2019 A1
20200018159 Ameen Jan 2020 A1
20210156243 Aljubran et al. May 2021 A1
Foreign Referenced Citations (25)
Number Date Country
2669721 Jul 2011 CA
2926192 Apr 2015 CA
101079591 Nov 2007 CN
102493813 Jun 2012 CN
102597419 Jul 2012 CN
103377307 Oct 2013 CN
104295448 Jan 2015 CN
204627586 Sep 2015 CN
105392954 Mar 2016 CN
107462222 Dec 2017 CN
0326720 Aug 1989 EP
2317068 May 2011 EP
2574722 Apr 2013 EP
2737173 Jun 2014 EP
WO 2002068793 Sep 2002 WO
WO 2008146017 Dec 2008 WO
WO 2009020889 Feb 2009 WO
WO 2011038170 Mar 2011 WO
WO 2011083182 Jul 2011 WO
WO 2013189842 Dec 2013 WO
WO 2015095155 Jun 2015 WO
WO 2016178005 Nov 2016 WO
WO 2017011078 Jan 2017 WO
WO 2017082860 May 2017 WO
WO 2018169991 Sep 2018 WO
Non-Patent Literature Citations (17)
Entry
U.S. Appl. No. 12/974,759, filed Dec. 21, 2010, Sadlier et al.
Adham, “Geomechanics model for wellbore stability analysis in Field ‘X’, North Samatra Basin,” retrieved from URL <https://mountainscholar.org/bitstream/handle/11124/170314/Adham_mines_0052N_11059.pdf?sequence=1>, Jan. 1, 2016, 121 pages.
Albukhari et al., “Geomechanical Wellbore Stability Analysis for the Reservoir Section in J-NC186 Oil Field,” retrieved from URL <https://www.onepetro.org/download/conference-paper/ISRM-TUNIROCK-2018-22?id=conference-paper/ISRM-TUNIROCK-2018-22>, retrieved on Oct. 14, 2019, published Mar. 31, 2018, 15 pages.
Al-Haidary, “Wellbore Stability Assessment in a Shale Formation,” retrieved from URL <http://eprints.kfupm.edu.sa/139181/1/Wellbore_Stability_Assessment_in_a_shale_formation_Saleh_AlHaidary.pdf>, retrieved on Oct. 14, 2019, published May 1, 2014, 136 pages.
Alsubaih, “Shale instability of deviated wellbores in southern Iraqi frields,” retrieved from URL <http://scholarsmine.mst.edu/cgi/viewcontent.cgi?article=8544&context=masters_theses>, retrieved on Oct. 14, 2019, published Jan. 1, 2016, 129 pages.
Aminzadeh, “Pattern recognition and imaging processing,” Geophysical Press Limited, 1987, 5 pages, with English Abstract.
Ashby et al., “Coiled Tubing Conveyed Video Camera and Multi-Arm Caliper Liner Damage Diagnostics Post Plug and Perf Frac,” Society of Petroleum Engineers, SPE-172622-MS, Mar. 2015, pp. 12.
Caryotakis, “The klystron: A microwave source of surprising range and endurance.” The American Physical Society, Division of Plasma Physics Conference in Pittsburg, PA, Nov. 1997, 14 pages.
Gemmeke and Ruiter, “3D ultrasound computer tomography for medical imagining,” Nuclear Instruments and Methods in Physics Research A 580, Oct. 1, 2007, 9 pages.
Johnson, “Design and Testing of a Laboratory Ultrasonic Data Acquisition System for Tomography” Thesis for the degree of Master of Science in Mining and Minerals Engineering, Virginia Polytechnic Institute and State University, Dec. 2, 2004, 108 pages.
Kosset, “Wellbore integrity analysis for wellpath optimization and drilling risks reduction: the vaca muerta formation in neuquen basin,” retrieved from URL <https://mountainscholar.org/bitstream/handle/11124/464/Kosset mines_0O52N_1O469.pdf?sequence=1&i sAllowe3=y>, published Jan. 1, 2014, 131 pages.
Lang et al., “Wellbore Stability Modeling and Real-Time Surveillance for Deepwater Drilling to Weak Bedding Planes and Depleted Reservoirs,” Society of Petroleum Engineers (SPE), Mar. 1, 2011, 18 pages.
Li et al., “Pore-pressure and wellbore-stability prediction to increase drilling efficiency,” Journal of Petroleum Technology, Feb. 28, 2012, 4 pages.
Mokhtari et al., “Characterization of Complex Fracture Propagation in Naturally Fractured Formations Using Digital Image Correlation Technique,” Society of Petroleum Engineers (SPE), presented at the SPE Hydraulic Fracturing Technology Conference and Exhibition, The Woodlands, Texas, USA, Jan. 2017, 11 pages.
Ruiter et al., “3D ultrasound computer tomography of the breast: A new era?” European Journal of Radiology 81S1, Sep. 2012, 2 pages.
Tan et al., “Wellbore Stability of Extended Reach Wells in an Oil Filed in Sarawak Basin, South China Sea,” SPE88609, Society of Petroleum Engineers (SPE), SPE Proceedings, XX, XX, Oct. 18, 2004, 11 pages.
Tutuncu et al., “Annual Meeting Selections. Integrated Wellbore-Quality and Risk-Assessment Study Guides Successful Drilling in Amazon Jungle,” Geophysics, Society of Exploration Geophysics, 71:6, Jan. 1, 2006, 7 pages.
Related Publications (1)
Number Date Country
20230186564 A1 Jun 2023 US