Patent Publication Number: US-8978461-B2

Title: Apparatus and measuring stress in a subterranean formation

Description:
BACKGROUND 
     Stress within subterranean formations affects the mechanical and fluid properties of those subterranean formations. Accordingly, knowledge of the magnitude and orientation of that stress (the “stress field”) is useful for planning and drilling a wellbore that traverses those subterranean formations. Knowledge of the stress field is also useful for planning and conducting the fracturing of a subterranean formation that contains hydrocarbons. Presently, stress field data is limited to estimates based on limited data and modeling. Any improvements in determining the actual stress field components are valuable for planning, drilling, and producing from a well. 
    
    
     
       BRIEF DESCRIPTION OF THE DRAWINGS 
       For a more detailed description of the embodiments, reference will now be made to the following accompanying drawings: 
         FIG. 1  is a schematic representation of a drilling system including a downhole tool with a stress measurement tool according to the principles disclosed herein; 
         FIG. 2  illustrates a mechanically induced fracture in a formation according to the principles disclosed herein; 
         FIGS. 3A-3C  schematically illustrate a stress measurement tool according to the principles disclosed herein; 
         FIG. 4  schematically illustrates a stress measurement tool according to the principles disclosed herein; 
         FIGS. 5A-5F  illustrate a series of mechanically induced fractures in a formation according to the principles disclosed herein; 
         FIG. 6  illustrates a coordinate system for reference with stress field determinations according to the principles disclosed herein; 
         FIG. 7  schematically illustrates a stress measurement tool according to the principles disclosed herein; 
         FIGS. 8A-8C  illustrate a series of mechanically induced fractures in a formation according to the principles disclosed herein; 
         FIGS. 9A and 9B  illustrate mechanically induced fractures in a formation with pre-existing fractures according to the principles disclosed herein. 
     
    
    
     DETAILED DESCRIPTION OF THE DISCLOSED EMBODIMENTS 
     The present disclosure relates to a stress measurement system for a subterranean formation and includes embodiments of different forms. The drawings and the description below disclose specific embodiments with the understanding that the embodiments are to be considered an exemplification of the principles of the invention, and are not intended to limit the invention to that illustrated and described. Further, it is to be fully recognized that the different teachings of the embodiments discussed below may be employed separately or in any suitable combination to produce desired results. The term “couple,” “couples,” or “coupled” as used herein is intended to mean either an indirect or a direct connection. Thus, if a first device couples to a second device, that connection may be through a direct connection; e.g., by conduction through one or more devices, or through an indirect connection; e.g., by convection or radiation. 
     Referring now to  FIG. 1 , a drilling system  140  including a stress measurement tool  135  according to the principles disclosed herein is depicted. Drilling system  140  further includes a drill string  105  suspended from a rig  110  into a wellbore  115 . Drill string  105  includes a drill pipe  125  that may be made up of a plurality of sections and to which a BHA  120  is coupled. BHA  120  includes a drill bit  130  and may include other components, such as but not limited to a drill sub, a motor, steering assembly, and drill collars. During drilling, drilling fluid, or “drilling mud,” is circulated down through drill string  105  to lubricate and cool drill bit  130  as well as to provide a vehicle for removal of drill cuttings from wellbore  115 . After exiting drill bit  130 , the drilling fluid returns to the surface through an annulus  195  between drill string  105  and wellbore  115 . 
     Embodiments of the stress measurement tool  135  are configured to measure stress and strain during and after mechanically fracturing a wellbore in a selected subterranean formation (hereinafter the “formation”). The mechanical fracturing of the wellbore is performed in a manner that controls the direction in which mechanical force is applied in order to determine direction and magnitude of the stress field for the formation. At least three mechanical fractures are created by the stress measurement tool  135  in different directions. Combined with knowledge of the orientation of the mechanical fractures, the stress and strain measurements may then be used to determine the stress field for the formation, which is discussed in greater detail below. 
       FIG. 2  illustrates a fracture  301  in a formation mechanically induced in accordance with one embodiment.  FIGS. 3A-3C  schematically illustrate a stress pad section  201  of a stress measurement tool for mechanically inducing the fracture  301  shown in  FIG. 2  in accordance with one embodiment. To fracture the formation, two semi-cylindrical pads  202  are forced outward in opposite directions against the wellbore  115 . Force against the wellbore  115  is increased until the fracture  301  is induced by overcoming the formation tensile strength. The fracture  301  occurs substantially perpendicular to the force applied by the semi-cylindrical pads  202 . After the fracture  301  is opened, the semi-cylindrical pads  202  are withdrawn to allow the fracture to close back. The fracture  301  is then reopened by the semi-cylindrical pads  202  while the stress applied by the semi-cylindrical pads  202  is plotted against strain, which can be measured by a strain gauge  215  monitoring the width of a gap  210  between the semi-cylindrical pads  202 . Those having ordinary skill in the art will appreciate that strain in the formation may be measured using various arrangements without departing from the scope of the disclosure. The reopening of the fracture  301  may be repeated using different loading cycles to determine stress magnitudes in the formation. 
     Continuing with  FIGS. 3A-3C , the stress measurement tool includes an upper connection  205  for connecting to the drill string  105 , which may include, for example, coiled tubing, drill pipe, and/or drill collars. The stress measurement tool includes at least one stress pad section  201  with two semi-cylindrical pads  202 . The length of the semi-cylindrical pads  202  is selected according to the diameter of the wellbore in which they will be used. In one embodiment, the semi-cylindrical pads  202  are about three times as long as the diameter of the wellbore. For example, in a 9⅝ inch (24.4 cm) diameter wellbore, the semi-cylindrical pads  202  may be about 30 inches (76.2 cm) long. The semi-cylindrical pads  202  are separated by the gap  210  when outwardly extended, and may be covered by a screen  211  to prevent debris from interfering with the movement of the semi-cylindrical pads  202 . 
       FIG. 3B  is a radial cross-section of the stress pad section  201 . The semi-cylindrical pads  202  are extended and retracted by a spline  221 . If circulation of fluid is desired through the stress measurement tool, a through bore (not shown) may be formed in the spline  221 . The spline  221  is only schematically illustrated because the particular mechanism used is not critical so long as it is capable of providing sufficient outward force to fracture the formation and retracting the semi-cylindrical pads  202  after being pressed into the formation. The semi-cylindrical pads  202  may be constructed to not be entirely rigid in order to conform to the wellbore during fracturing. This may be accomplished through a selection of multiple materials or by having a non-solid structure. For example, an outer portion of the semi-cylindrical pads  202  may be formed from soft metal or high durometer polyurethane. 
       FIG. 3C  is an axial cross-section of the stress pad section  201 . To distribute the force evenly along the semi-cylindrical pads  202 , a series of jacks  230  may be spaced along the stress pad section  201 . The jacks  230  may be actuated, for example, by axial movement of the spline  221 . 
     As discussed above, at least three separate mechanically induced fractures in three directions are necessary to determine the stress field of the formation. Six mechanically induced fractures in six directions allow for determination of the stress field of the formation with fewer assumptions, and, accordingly increased accuracy. The stress measurement tool used to induce the fractures includes at least one stress pad section. A single stress pad section may be used to induce a fracture in a first direction. The single stress pad section may then be moved axially up or down in the wellbore and rotated to a second direction, third direction . . . and sixth direction. Alternatively, each of the fractures may be induced by a different stress pad section simultaneously by using a stress measurement tool that includes three or six stress pad sections oriented in different directions. Simultaneous fracturing saves time relative to sequential fracturing and ensures that the fractures are induced at specific orientations relative to each other. 
     In one embodiment, the stress measurement tool includes six stress pad sections  201  oriented 60 degrees from each other around the stress measurement tool, as schematically shown in  FIG. 4 . Each stress pad section may be oriented more than 60 degrees from the stress pad sections immediately above and below to minimize interference in the direction of the induced fracture from the neighboring induced fractures. Orientations of six stress pad sections  201  and their corresponding induced fractures are illustrated in  FIGS. 5A-5F . In this embodiment, with respect to due north and from the top to the bottom, the stress pad sections  201  are oriented at 0, 60, 120, 30, 90, and 150 degrees. This relative orientation amongst the stress pad sections  201  ensures that a set of stress measurements will be taken every 30 degrees around the wellbore  400 . 
     The stress measurement tool may further include orientation sensors and a gamma ray sensor provided in a sensor module  401  in close proximity to the set of stress pad sections  201 . The orientation sensors may be any systems known in the art for determining orientation of a downhole tool, such as gyroscopes and accelerometers. The orientation sensors allow for the determination of the direction in which each stress pad section  201  is oriented. The gamma ray sensor allows for identification of the basic lithology of the formation being tested to help ensure that the stress measurement tool is placed at the desired location in the wellbore  400  below a casing  410 . 
     The above described apparatus allow for the plotting of stress versus strain while opening a mechanically induced fracture in a formation. As discussed above, a fracture is mechanically induced by applying a stress sufficient to overcome the tensile strength of the formation. The fracture is allowed to close and then is reopened by again applying stress. As stress applied by the semi-cylindrical pads increases, the measured strain will be substantially zero from when the semi-cylindrical pads contact the formation until the fracture reopens, at which point stress and strain will have a proportional relationship. The stress magnitude at this inflection point in the stress versus strain plot is related to the tangential stress component generated at the wellbore by the semi-cylindrical pads. This data for each of the induced fractures can then be used to solve for the stress field of the formation, as detailed mathematically below. 
     With reference to  FIG. 6 , (σ 1 , σ 2 , σ 3 ) is a system of rectangular axes and (X, Y, Z) is another set of rectangular axes whose direction cosines relative to (σ 1 , σ 2 , σ 3 ) coordinate are, respectively, (l 1 , m 1 , n 1 ), (l 2 , m 2 , n 2 ), (l 3 , m 3 , n 3 ). These direction cosines can be expressed in terms of plunge β and trend, α as follows: 
     
       
         
           
               
             
               
                 
                   
                     
                       
                         l 
                         1 
                       
                       = 
                       
                         cos 
                         ⁢ 
                         
                             
                         
                         ⁢ 
                         β 
                         ⁢ 
                         
                             
                         
                         ⁢ 
                         cos 
                         ⁢ 
                         
                             
                         
                         ⁢ 
                         α 
                       
                     
                     , 
                   
                 
                 
                   
                     
                       
                         m 
                         1 
                       
                       = 
                       
                         cos 
                         ⁢ 
                         
                             
                         
                         ⁢ 
                         β 
                         ⁢ 
                         
                             
                         
                         ⁢ 
                         sin 
                         ⁢ 
                         
                             
                         
                         ⁢ 
                         α 
                       
                     
                     , 
                   
                 
                 
                   
                     
                       n 
                       1 
                     
                     = 
                     
                       
                         - 
                         sin 
                       
                       ⁢ 
                       
                           
                       
                       ⁢ 
                       β 
                     
                   
                 
               
               
                 
                   
                     
                       
                         l 
                         2 
                       
                       = 
                       
                         
                           - 
                           sin 
                         
                         ⁢ 
                         
                             
                         
                         ⁢ 
                         α 
                       
                     
                     , 
                   
                 
                 
                   
                     
                       
                         m 
                         2 
                       
                       = 
                       
                         cos 
                         ⁢ 
                         
                             
                         
                         ⁢ 
                         α 
                       
                     
                     , 
                   
                 
                 
                   
                     
                       n 
                       2 
                     
                     = 
                     0 
                   
                 
               
               
                 
                   
                     
                       
                         l 
                         3 
                       
                       = 
                       
                         sin 
                         ⁢ 
                         
                             
                         
                         ⁢ 
                         β 
                         ⁢ 
                         
                             
                         
                         ⁢ 
                         cos 
                         ⁢ 
                         
                             
                         
                         ⁢ 
                         α 
                       
                     
                     , 
                   
                 
                 
                   
                     
                       
                         m 
                         3 
                       
                       = 
                       
                         sin 
                         ⁢ 
                         
                             
                         
                         ⁢ 
                         β 
                         ⁢ 
                         
                             
                         
                         ⁢ 
                         sin 
                         ⁢ 
                         
                             
                         
                         ⁢ 
                         α 
                       
                     
                     , 
                   
                 
                 
                   
                     
                       n 
                       3 
                     
                     = 
                     
                       cos 
                       ⁢ 
                       
                           
                       
                       ⁢ 
                       β 
                     
                   
                 
               
             
             } 
           
         
       
     
     The explicit form of the stress transformation matrices between the two coordinate reference systems are: 
     
       
         
           
             
               [ 
               
                 T 
                 e 
               
               ] 
             
             = 
             
               [ 
               
                 
                   
                     
                       l 
                       1 
                       2 
                     
                   
                   
                     
                       m 
                       1 
                       2 
                     
                   
                   
                     
                       n 
                       1 
                       2 
                     
                   
                   
                     
                       2 
                       ⁢ 
                       
                         m 
                         1 
                       
                       ⁢ 
                       
                         n 
                         1 
                       
                     
                   
                   
                     
                       2 
                       ⁢ 
                       
                         n 
                         1 
                       
                       ⁢ 
                       
                         l 
                         1 
                       
                     
                   
                   
                     
                       2 
                       ⁢ 
                       
                         l 
                         1 
                       
                       ⁢ 
                       
                         m 
                         1 
                       
                     
                   
                 
                 
                   
                     
                       l 
                       2 
                       2 
                     
                   
                   
                     
                       m 
                       2 
                       2 
                     
                   
                   
                     
                       n 
                       2 
                       2 
                     
                   
                   
                     
                       2 
                       ⁢ 
                       
                         m 
                         2 
                       
                       ⁢ 
                       
                         n 
                         2 
                       
                     
                   
                   
                     
                       2 
                       ⁢ 
                       
                         n 
                         2 
                       
                       ⁢ 
                       
                         l 
                         2 
                       
                     
                   
                   
                     
                       2 
                       ⁢ 
                       
                         l 
                         2 
                       
                       ⁢ 
                       
                         m 
                         2 
                       
                     
                   
                 
                 
                   
                     
                       l 
                       3 
                       2 
                     
                   
                   
                     
                       m 
                       3 
                       2 
                     
                   
                   
                     
                       n 
                       3 
                       2 
                     
                   
                   
                     
                       3 
                       ⁢ 
                       
                         m 
                         3 
                       
                       ⁢ 
                       
                         n 
                         3 
                       
                     
                   
                   
                     
                       2 
                       ⁢ 
                       
                         n 
                         3 
                       
                       ⁢ 
                       
                         l 
                         3 
                       
                     
                   
                   
                     
                       2 
                       ⁢ 
                       
                         l 
                         3 
                       
                       ⁢ 
                       
                         m 
                         3 
                       
                     
                   
                 
                 
                   
                     
                       
                         l 
                         2 
                       
                       ⁢ 
                       
                         l 
                         3 
                       
                     
                   
                   
                     
                       
                         m 
                         2 
                       
                       ⁢ 
                       
                         m 
                         3 
                       
                     
                   
                   
                     
                       
                         n 
                         2 
                       
                       ⁢ 
                       
                         m 
                         3 
                       
                     
                   
                   
                     
                       
                         
                           m 
                           2 
                         
                         ⁢ 
                         
                           n 
                           3 
                         
                       
                       + 
                       
                         
                           m 
                           3 
                         
                         ⁢ 
                         
                           n 
                           2 
                         
                       
                     
                   
                   
                     
                       
                         
                           n 
                           2 
                         
                         ⁢ 
                         
                           l 
                           3 
                         
                       
                       + 
                       
                         
                           n 
                           3 
                         
                         ⁢ 
                         
                           l 
                           2 
                         
                       
                     
                   
                   
                     
                       
                         
                           l 
                           2 
                         
                         ⁢ 
                         
                           m 
                           3 
                         
                       
                       + 
                       
                         
                           l 
                           3 
                         
                         ⁢ 
                         
                           m 
                           2 
                         
                       
                     
                   
                 
                 
                   
                     
                       
                         l 
                         3 
                       
                       ⁢ 
                       
                         l 
                         1 
                       
                     
                   
                   
                     
                       
                         m 
                         3 
                       
                       ⁢ 
                       
                         m 
                         1 
                       
                     
                   
                   
                     
                       
                         n 
                         3 
                       
                       ⁢ 
                       
                         n 
                         1 
                       
                     
                   
                   
                     
                       
                         
                           m 
                           1 
                         
                         ⁢ 
                         
                           n 
                           3 
                         
                       
                       + 
                       
                         
                           m 
                           3 
                         
                         ⁢ 
                         
                           n 
                           1 
                         
                       
                     
                   
                   
                     
                       
                         
                           n 
                           1 
                         
                         ⁢ 
                         
                           l 
                           3 
                         
                       
                       + 
                       
                         
                           n 
                           3 
                         
                         ⁢ 
                         
                           l 
                           1 
                         
                       
                     
                   
                   
                     
                       
                         
                           l 
                           1 
                         
                         ⁢ 
                         
                           m 
                           3 
                         
                       
                       + 
                       
                         
                           l 
                           3 
                         
                         ⁢ 
                         
                           m 
                           1 
                         
                       
                     
                   
                 
                 
                   
                     
                       
                         l 
                         1 
                       
                       ⁢ 
                       
                         l 
                         2 
                       
                     
                   
                   
                     
                       
                         m 
                         1 
                       
                       ⁢ 
                       
                         m 
                         2 
                       
                     
                   
                   
                     
                       
                         n 
                         1 
                       
                       ⁢ 
                       
                         n 
                         2 
                       
                     
                   
                   
                     
                       
                         
                           m 
                           1 
                         
                         ⁢ 
                         
                           n 
                           2 
                         
                       
                       + 
                       
                         
                           m 
                           2 
                         
                         ⁢ 
                         
                           n 
                           1 
                         
                       
                     
                   
                   
                     
                       
                         
                           n 
                           1 
                         
                         ⁢ 
                         
                           l 
                           2 
                         
                       
                       + 
                       
                         
                           n 
                           2 
                         
                         ⁢ 
                         
                           l 
                           1 
                         
                       
                     
                   
                   
                     
                       
                         
                           l 
                           1 
                         
                         ⁢ 
                         
                           m 
                           2 
                         
                       
                       + 
                       
                         
                           l 
                           2 
                         
                         ⁢ 
                         
                           m 
                           1 
                         
                       
                     
                   
                 
               
               ] 
             
           
         
       
     
     The tangential stress component at the borehole wall when a fracture is reopened can be expressed as:
 
σ θθ =σ xx +σ yy −2(σ xx −σ yy )cos 2θ−4τ xy  sin 2θ −P   w   =kP   r  
 
     When a fracture is reopened, the tangential stress generated by the in-situ stress regime described above is substantially equal to the tangential stress generated by loading of the stress measurement tool. The reopening pressure P r  may be recorded by observing the stress-strain curve measured by strain sensors. The stress concentration factor k can be calibrated using numerical simulation. Therefore, with six fractures generated by a stress measurement tool, there are six equations to solve for the six unknowns σ 1 , σ 2 , σ 3 , α, β, θ. 
     Although six fractures provide a more accurate stress field determination, three fractures may provide sufficient information for determining a stress field to obtain many of the advantages of the principles disclosed herein.  FIG. 7  illustrates a stress measurement tool for mechanically inducing three or more fractures in accordance with one embodiment. In this embodiment, the stress measurement tool includes three stress pad sections  201  oriented in different directions to mechanically induce the fractures shown in  FIGS. 8A-8C . Orientation sensors and a gamma ray sensor may be provided in a sensor module  401  in close proximity to the set of stress pad sections  201 . In this embodiment, with respect to due north and from the top to the bottom, the stress pad sections  201  are oriented at 0, 60, and 120 degrees. 
     In a simplified form, assuming the vertical stress is one of the principal stress components of the in-situ stress, and with a further simplification of a plain strain assumption, we have the following equation for tangential stress when a fracture is reopened:
 
σ θθ σ 1 +σ 2 −2(σ 1 −σ 2 )cos 2θ− P   w   =kP   r  
 
     There are only three unknowns σ 1 , σ 2  and θ. Therefore, with only three fractures generated, there are three equations to solve for the three unknowns. If additional fractures are desired, the stress measurement tool may be lowered or raised within the wellbore and rotated about 30 degrees to open another set of three fractures to obtain all six of the datasets needed for full analysis without the simplifying assumptions regarding the vertical stress and plain strain. 
     Some formations contain natural fractures. Stress measurement tools in accordance with the principles disclosed herein may be used with such formations. If the existence and orientation of natural fractures in the formation are known in advance, the stress measurement tool may be oriented to put the natural fractures in the compressive stress zone to minimize the influence of the natural fractures on the measurements being taken. Such an alignment is shown in  FIG. 9A  in which the mechanically induced fracture  301  is oriented to avoid opening the natural fracture  900 . Alternatively, the natural fracture  900  may be reopened mechanically by substantially aligning the mechanically induced fracture  301  parallel to the natural fracture  900 , as shown in  FIG. 9B . 
     If the existence and/or orientation of natural fractures are unknown, stress measurement tools in accordance with the principles disclosed herein may be used to determine these formation properties. If a natural fracture is opened by one of the stress pad sections  201 , the plot of stress versus strain during the initial mechanical fracture will more closely resemble the reopening of the fracture instead of the creation of the fracture. 
     Stress measurement tools and stress field determination methods disclosed herein provide direct downhole measurement of the directions and magnitudes of the components of the stress field in a formation under the conditions of downhole temperature and stress that are present at the time of the test. These downhole stress measurements are then used to provide a general solution to the downhole stress measurement problem that is not limited by either hole angle or bed dip. Stress field orientations, magnitudes, and the natural fracture orientation are key parameters needed to plan successful hydraulic fracturing in reservoirs, in designing well orientation, and to predicting the production delivery (flow rates and reserves) of a reservoir. The true stress field is usually not what it is assumed to be, or what it is mathematically simplified to be, when using existing techniques and tools. In the prior art, commonly only the minimum horizontal stress component can be measured to a reasonable degree of accuracy with different inherent assumptions and simplifications. The orientation and magnitude of the maximum horizontal stress component are usually only estimated and rarely directly measured. 
     Direct measurement of the subsurface stress is a key unknown in designing fracture stimulation, in orienting the drilling of wellbores, and in predicting the effectiveness of a hydraulic fracture on both initial production rates and ultimate reservoir recovery. Many different methods are available to estimate these important parameters, but none are designed to measure all of these parameters under in-situ conditions. 
     Stress measurement tools in accordance with the principles disclosed herein can replace the use of downhole formation integrity test (FIT) measurements because the actual values of the stresses would be known from the stress measurement tools. Hydraulic fracturing measurements do not provide as much information as mechanically induced fractures disclosed herein. For example, the orientation and magnitude of the downhole stress system could be determined at multiple depths in the wellbore by setting the stress measurement tool at varying depths for data acquisition. The parameters of the existing natural fracture system in the subsurface are also determinable from the stress measurement tools disclosed herein. 
     Direct measurement and identification of downhole stresses may positively impact many different areas related to the drilling, stimulation, casing, cementing and completion of wells. 
     In fracturing operations, identification of the orientation of natural fractures and the determination of their relationship to the current stress regime is important especially in tight gas and shale reservoirs because the fractures that are oriented preferentially to the current stress state will be the ones that are currently open and that can provide the most effective deliverability of hydrocarbons to the wellbore. Furthermore, a full measurement of the present stress regime will allow the analysis of the relationship between the natural fractures and the geologic time at which they were generated. 
     Identification of the stress state in the subsurface at any point in the wellbore will allow the identification of changes in the stress vertically due to any combination of geologic and lithologic factors. This is currently an unknown that is evaluated by modeling, but that cannot be directly confirmed by the well data. For example, on a tightly folded structure, even in a present-day compressive stress regime, the reservoirs at the top of the folded structure may be in extension with neutral horizontal stress in the middle and strongly compressive stresses at the most tightly folded part of the structure. The identification of the open fractures and their orientation and location on the structure will often determine the success or failure of a well. As another example, the stress state around salt and diapiric shale bodies changes dramatically due to the nature of the mobile rock. This affects the design, drilling, and completion of these wells. 
     The successful artificial fracturing of wells in shale and tight sands is of significant importance to the ability to produce hydrocarbons from such reservoirs. Improved knowledge of the current stress state allows for improvement in the design and stimulation of such wells. In addition to the relationship between fracture orientation and conductivity to the current stress state, the permeability of the reservoir rock itself is anisotropic and is related to the stress field. Identification of this early in the development of a field will allow for the better placement and design of the development wells. 
     Improved knowledge of the stress field can improve the drilling process. The direction in which wells should be drilled to achieve maximum commercial success is related to the stress state and fracture pattern of the formations. The design of the well drilling program is also related to both the rock strength and to the stress state. The interval in which the hole angle is built and the angle of build-up is important in the drilling of successful wells. 
     In overpressured downhole environments, the knowledge of the stress state in the rocks, including pore pressure, is needed to design the drilling plan to allow for safe and efficient construction of the wells to include the casing plan, the mud weight design, the bit selection, the cementing program, the direction that the wells are drilled, the units in which angle build-up will be done, and the rate of hole angle increase, as well as many other factors. The prevention or management of wellbore instability is based on an analysis of the downhole stress conditions. Direct measurement of the downhole stresses may also allow for better identification and analysis of chemical reactions between the rock and the mud or cement system by allowing the separation of the causes of the various effects. Rock strength and stress are also important factors in the selection of the proper bit that will most efficiently drill any specific rock unit in the subsurface. 
     The production from a reservoir may be improved with increased knowledge of the stress field of the formations. Production and depletion of a reservoir of any lithology changes the stress state within and around that reservoir. The results can be either beneficial or deleterious depending on a number of factors. Stress measurement tools disclosed herein may allow the measurement of the change in stress as measured by infill or development or redevelopment wells after the production has begun with a greater accuracy and precision than is currently done. Additionally, casing collapse due to subsurface faulting or the movement of salt or mobile shale can be analyzed and mitigated by the analysis of the stress conditions using the stress measurement tools disclosed herein. 
     Those having ordinary skill in the art will appreciate that the analysis of the stress and strain data obtained by stress measurement tools disclosed herein may occur within electronic components in the stress measurement tool or at the surface. In one embodiment, the stress and strain measurements may be stored on computer readable media in the stress measurement tool and then analyzed when the stress measurement tool is retrieved from the well. In another embodiment, the stress and strain measurements may be communicated from the stress measurement tool to the surface. The data may be communicated to the surface by pressure pulses in well fluid, electronically through wired drill pipe, or through any other downhole telemetry system. 
     While specific embodiments have been shown and described, modifications can be made by one skilled in the art without departing from the spirit or teaching of this invention. The embodiments as described are exemplary only and are not limiting. Many variations and modifications are possible and are within the scope of the invention. Accordingly, the scope of protection is not limited to the embodiments described, but is only limited by the claims that follow, the scope of which shall include all equivalents of the subject matter of the claims.