Enhanced (or Engineered) Geothermal Systems are systems designed to extract heat from the earth for power generation. In hydrothermal systems, naturally occurring hot water or steam reservoirs beneath the surface of the earth are tapped into and the hot water or steam is brought to the surface to generate electricity. Hydrothermal systems require heat, water, and permeability of the underground rock. EGS can be used when rock permeability is low to create man-made reservoirs.
Many aspects of the present disclosure can be better understood with reference to the following drawings. The components in the drawings are not necessarily to scale, with emphasis instead being placed upon clearly illustrating the principles of the disclosure. Moreover, in the drawings, like reference numerals designate corresponding parts throughout the several views.
In accordance with the purpose(s) of the present disclosure, as embodied and broadly described herein, embodiments of the present disclosure, in some aspects, relate to systems and methods for using controlled fractures in geothermal systems. In general, embodiments of the present disclosure provide for methods of cutting slots in subsurface rock, injecting water into the slots, and producing heated water.
Before the present disclosure is described in greater detail, it is to be understood that this disclosure is not limited to particular embodiments described, and as such may, of course, vary. It is also to be understood that the terminology used herein is for the purpose of describing particular embodiments only, and is not intended to be limiting, since the scope of the present disclosure will be limited only by the appended claims.
Disjunctive language such as the phrase “at least one of X, Y, or Z,” unless specifically stated otherwise, is otherwise understood with the context as used in general to present that an item, term, etc., can be either X, Y, or Z, or any combination thereof (e.g., X; Y; Z; X or Y; X or Z; Y or Z; X, Y, or Z; etc.). Thus, such disjunctive language is not generally intended to, and should not, imply that certain embodiments require at least one of X, at least one of Y, or at least one of Z to each be present.
The present disclosure provides for methods of extracting heat from the earth for power generation, using in heating systems, and the like. In addition, the present disclosure provides systems that can extract heat from the earth for power generation, heating systems and the like. The present disclosure uses controlled fractures in a well, where water is flowed through the controlled fracture and the temperature of the water is increased. The heated water is then flowed out of the well and can be used as desired. The present disclosure is advantageous in that heat from the earth can be efficiently acquired using water and the process does not produce emissions.
In some embodiments, the method uses controlled fractures in geothermal systems to transport heat from the earth to water, where the water is then circulated to the surface where the thermal energy can be used. The method includes drilling at least one injection well bore and then cutting a plurality of slots away from the injection well bore to form the controlled fractures. The slots can be connected serially and/or in parallel. The slots are fluidically connected to the injection well bore and the production well bore so that water can flow from the injection well bore to the production well bore. In some embodiments, the injection well bore can be a substantially (e.g., +/−25%) vertical well bore into the earth. In some embodiments, the slots are cut substantially (e.g., +/−45%) perpendicular to the injection well bore. In some embodiments, the slots are cut and connected in series such that a flow-path for water is formed through the slots to flow water from the first slot through the middle slots and to the end slots. In other embodiments, the slots are cut and connected in parallel. In still other embodiments, some slots are cut in serials and others in parallel. The flow-path can be formed between the injection well bore at the first end and the production well bore at the second end. In some embodiments, the slots can be cut away from the injection well bore in multiple directions and feed multiple different production well bores, in series, in parallel, or a combination of in series and parallel. In each embodiment the injection well bore, the one or more slots, and the production well bore are in fluidic communication so that water is flowed into the injection well bore, through the one or more slots, and out of the production well bore.
Each slot can comprise a cut in the earth's surface or subsurface having substantially (e.g., +/−50%) uniform surface area. In an aspect, the width of the slot can be about 1 centimeter to 1 meter. The width of the slot is typically the width of the mechanism used to form the slot. In some embodiments, the slots can be cut using slot-drill technology as shown in
In some embodiments, the slots can be cut in a repeating pattern such as the examples shown in
In some embodiments, the slots can be cut to intercept naturally occurring fractures in the rock. The naturally occurring fractures can be targeted and used to connect some or all of the slots.
In general, water can be injected via the injection well bore and flow from the injection well bore into the plurality of slots and through the slots to the production well bore where it can be extracted. While flowing through the slots, the water can be heated by the surrounding rock and earth. Then the heated water can be flowed out of the production well bore and the thermal energy used accordingly.
More specifically, the present disclosure provides for a system that includes an injection well bore configured to receive a stream of water. The stream of water is flowed through at least a first slot, where the first slot is at an angle with respect to the injection well bore. In some embodiments, the first slot is substantially perpendicular to the injection well bore. The first slot has a first end and a distal end on opposite sides of the first slot. The first end of the first slot being connected to the injection well bore such that the stream of water flows from the injection well bore into the first slot. The system can optionally include a second slot at an angle to the injection well bore. In some embodiments, the second slot is substantially perpendicular to the injection well bore. The second slot can have a first end and a distal end at opposite ends of the second slot. Optionally, the first end of the second slot is connected to the distal end of the first slot such that the stream of water flows from the first slot into the second slot. The system also includes at least one production well bore. The production well bore is connected to the distal end of the second slot such that the stream of water flows from the second slot into the production well bore. Additional slots can be included in series and/or in parallel the injection well, the first slot, the second slot, and the production well bore. Other aspects are provided for in the examples.
Now having described the embodiments of the disclosure, in general, the examples describe some additional embodiments. While embodiments of the present disclosure are described in connection with the example and the corresponding text and figures, there is no intent to limit embodiments of the disclosure to these descriptions. On the contrary, the intent is to cover all alternatives, modifications, and equivalents included within the spirit and scope of embodiments of the present disclosure.
This example seeks to demonstrate a technique to cut fractures mechanically and recover heat efficiently from all parts of hot rocks in the subsurface. Although the technique of cutting rocks using abrasive cables in tension has been proposed and used to cut rock slabs at the surface for years, its feasibility in subsurface conditions is yet to be assessed in the field. Unlike hydraulic fracturing, which is typically used for developing tight rocks, this technique of mechanically cutting fractures (referred to as slot-drilling) offers precise control over the fractures' location, size, orientation, and conductivity. This control of fracture location can be used to design and simulate a configuration of slot-drill fractures that could improve the recovery from tight/shale oil reservoirs by a factor of three. In some cases, there is potential of increasing the thermal recovery from EGS by a factor of two if slot-drill fractures are used instead of hydraulic fracturing.
Although
To obtain results that will inform how to perform slot drilling in the subsurface, an estimation of the strength of the tensioned cable needed to cut the granitic rock outcrop can be performed. This can be compared with the measured force required to create slot-drill fractures in this small-scale field test demonstration. In addition to the measurements of the torque needed to create the small-scale slot-drill fractures, several temperature and pressure sensors will be inserted at several points in the granite slab. These measurements will be used to calibrate the numerical models and provide recommendations on how to perform slot drilling safely and efficiently in the subsurface. Additionally, the thermal energy measurements from this small-scale field test will help validate and calibrate the numerical models. This is important to ensure that the simulated higher thermal recovery efficiency represents what to expect in reality.
This example is to improve the technology-readiness level of the proposed technology to a point where it can be implemented in the subsurface. The specific tasks performed during this project include:
The main impact of the project will be a demonstration of an alternative approach to create fractures, which, unlike hydraulic fracturing, allows precise control over the placement of fractures in a configuration that ensures the efficient recovery of heat from all parts of subsurface hot rocks. The control over the fracture location, size, and orientation will help avoid the risks associated with the uncertainty in hydraulic fracture location. These include the risk of short-circuiting flow and the risk of the injection or production well not intersecting the fractures created from the first horizontal well drilled. This technology could also be designed for use with existing hydraulically fractured EGS to recover heat from parts of the reservoir that have not been stimulated due to the geomechanical and hydraulic properties of the rocks.
A potential risk is the possibility of the slot-drill fractures closing after being cut. However, the roughness of the fracture surface will prevent it from closing completely and the simulations indicate thermal recoveries even at low to moderate fracture conductivity values. These slot-drilled fractures can also be propped as in hydraulic fractures.
This technological invention proposes to improve the efficiency of heat recovery from enhanced (or engineered) geothermal systems (EGS) by using fractures that are mechanically cut into hot dry rocks using the slot-drill technology, which is illustrated in
The reasons why this technology could be the game changer for EGS in ultra-low permeability rocks include:
At this point, only numerical simulation studies have been performed to evaluate the amount of recovery to expect from this technology, and the results appear promising. Current work involves incorporating stochastically generated natural fractures (with different lengths, aperture, conductivity, and orientation) into the matrix, and evaluating the robustness of this technology in such scenarios.
Enhanced geothermal systems (EGS) are typically tight and naturally fractured like unconventional oil and gas (UOG) reservoirs, so the leading technology being evaluated for their commercial development is also multistage fractured horizontal wells (MFHW). The state-of-the-art approach of thermal recovery from EGS involves injecting cold water into a multiply fractured horizontal/deviated well and producing hot water from a parallel well above the injector. The limited control over the hydraulic fracture location, size, and orientation in MFHWs results in low and unpredictable thermal recoveries. To this end, an alternative technology is presented herein that employs unique configurations of mechanically cut fractures to recover heat efficiently from all parts of hot rocks in the subsurface. The precise control over these fractures' location, size, orientation, and conductivity facilitates the design of suitable configurations of intersecting fractures.
This work presents high-resolution numerical studies of thermal recovery from both MFHW and the proposed approach. The results show that the proposed approach can recover significantly more thermal energy than MFHWs. Additionally, the temperature profiles show that precise control over the location of the fractures allows the reliable and efficient recovery of heat from all parts of the EGS, which could be the key to their commercial development.
Enhanced or engineered geothermal systems (EGS) are subsurface heat exchange systems created by fracturing low-matrix permeability hot rocks. The idea is to extract thermal energy economically by circulating cold water through these typically fractured rocks and producing the water after it has been heated via contact with the hot rock in a so-called closed loop. Although early research on EGS development focused on the hydraulic fracturing of vertical wells, several researchers have evaluated the idea of shearing existing joints or natural fractures in these hot rocks. Unfortunately, these approaches have yet to prove commercially viable. The sketch in
Considering the high costs of evaluating different EGS technologies in the field, several researchers have developed coupled heat and fluid flow simulators to simulate the performance of these technologies. Several researchers have designed computer experiments and sensitivity studies using these simulators to evaluate the potential of MFHW in EGS. For instance, some have performed numerical simulation studies that showed that horizontal wells have higher efficiency than vertical hydraulically fractured wells, which indicates the possible success of MFHW in EGS.
Although virtually all published numerical studies of the application of MFHW in EGS assume that the horizontal injection and production wells intersect all the hydraulic fractures, which are planar and bi-wing, this is only an unrealistic idealization. The negligible control over the size and orientation of hydraulic fractures, as well as the non-planarity and non-orthogonality of these fractures, will result in a lower heat recovery in the field compared to the simulated recovery. The expected lower recovery from non-planar and non-orthogonal fractures (compared to planar and orthogonal fractures) is demonstrated in an analogous system for the primary production from unconventional gas reservoirs. These uncertainties in MFHW highlight the need for a controlled fracture system that can be used to recover heat reliably and efficiently from all parts of an EGS.
EGS are typically naturally fractured and have low matrix permeability like UOG reservoirs, so the fractures generally are modeled using similar methods. The effective models represent the fractured reservoir as an effective medium with homogenized or average properties. For example, researchers have homogenized the naturally fractured system into a single-porosity system to simulate an EGS. Other multiple continuum formulations of the effective medium include the dual-porosity, dual-permeability, and multi-continuum models.
Unlike the effective medium models, discrete models individually account for each fracture in fractured reservoirs. These include the discrete fracture model (DFM), embedded discrete fracture model (EDFM) and projection-based embedded discrete fracture model (pEDFM). Although pEDFM was developed to model natural fractures of high and low conductivity, it cannot accurately model low-conductivity fractures that neither lie parallel to any of the spatial (x-, y-, and z-) axes nor cut through the diagonals of the matrix cells. To obtain reference solutions for the EGS systems studied, the fully dimensional (or explicit fracture) model was used, where each natural fracture is meshed in 3D and partitioned into several fracture cells. Although this approach is very computationally expensive, it is the most accurate approach to model fractured reservoirs. The idea is to obtain high-resolution reference solutions, which can be used to validate the application of other fracture models.
The next section presents the proposed approach to recover heat from EGS using controlled fractures, which are mechanically cut into the rock with the slot-drilling technology proposed.
This section presents the design of slot-drill fracture configurations that can lead to improved, reliable, and efficient heat recovery from all parts of an EGS. The slot-drill (SD) technology is based on ideas involving using a chain cutter that is pulled through massive rock outcrops. The EGS approach proposed here involves designing an interconnected system of fractures, which are mechanically cut using the SD technology. The proposed application of this concept to cut fractures in the subsurface involves using a deviated well bore, as shown in
A flexible and tensioned cutting cable (shown as the curved red lines) is then inserted into the wellbore and fixed at the toe of the wellbore. The back-and-forth motion of the tensioned cable could result in the cutting of the slot-drill fracture, shown as the shaded semi-circle in
This configuration is so-called because the pattern contains eight slot-drill fractures and three wells, as shown in
This configuration is so-called because the repeating pattern contains six slot-drill fractures and two wells, as shown in
The doublet configuration with parallel flow is referred to as the “doublet parallel” case, whereas the other doublet configuration is referred to as the “doublet series” case. The former was introduced because our numerical simulation studies reveal that although the thermal recoveries of both cases were approximately equal, the latter required unrealistically high injection pressures to flow fluids through the fracture and obtain the same pressure in the production well. Therefore, all subsequent references to the doublet case in this work refer to the doublet parallel configuration.
Compared to the SD triplet configuration, the SD doublet design is more flexible regarding the number of fractures that can be placed in any given area and requires fewer wells per unit SD fracture and per unit area. For instance, it is easy to see that the same vertical injection well section at the bottom corner of the domain can be used to drill the SD fractures in the next pattern below and to the left of the current pattern shown in
Modelling the coupled flow of fluid and heat in geothermal reservoirs involves solving the equations that govern both the fluid flow and heat flow. The mass conservation equation for single-phase fluid flow in porous media can be written as follows:
where, ϕ is the porosity of the rock, ρf is the fluid density, vf is the Darcy velocity of the fluid, qf is the source or sink, and V is the bulk volume. From the Darcy equation, the Darcy velocity is given as:
where, K is the permeability, μf is the fluid viscosity, z is the depth, and g is the acceleration due to gravity.
The energy conservation equation governs the flow of heat in geothermal reservoirs. It is written as follows:
Here, T is the current temperature of the system, while Cf and Cr are the specific heat capacities of the fluid and rock, respectively. The term Qfhf is the energy source or sink term, and hf is the specific enthalpy, which is given as:
The Hf and Hr terms in equation 3 represent the heat conduction for the fluid and rock, respectively. The equation for heat conduction is given by Fourier's law:
where λf and λr represent the thermal conductivity of the fluid and rock, respectively. Solving the governing mass and energy conservation equations involves discretizing them with respect to time using the implicit or backward Euler scheme. This yields the semi-discrete form of the energy balance equation:
Similarly, the semi-discrete form of the mass-conservation equation is given as:
This work uses the finite-volume discretization with single-point upwind weighting for spatial discretization. The discrete divergence and gradient operators are used to simplify the numerical implementation of the spatial discretization.
These coupled nonlinear equations are linearized using the Newton-Raphson iteration scheme. The linearized system of equations is then solved for the changes in the primary variables (ΔX) at each Newton iteration, using a Bi-Conjugate Gradient Stabilized (BiCG-Stab) linear solver with an Algebraic Multi-Grid (AMG) pre-conditioner. The changes in the primary variables are then added to the previous values of the primary variables (X), and the procedure is repeated until the system converges. Upon convergence, the solution algorithm proceeds to the next time step and repeats this Newton iteration.
To perform the simulation studies presented in this paper, the geothermal and unstructured gridding modules were used in the MATLAB Reservoir Simulation Toolbox (MRST). The stochastic natural fractures simulated were created using the Alghalandis Discrete Fracture Network Engineering code.
This work uses the thermal recovery fraction to facilitate a reasonable comparison between the thermal energy recovered from different simulation cases. The equation for the thermal recovery fraction can be given as follows:
and Qt is the total energy stored in the reservoir, which is given as:
In these equations, Vactive is the active or effective reservoir volume in m3, Vtotal is the total reservoir volume in m3, ρr is the rock density, C, is the specific heat capacity of the rock in J/(kg K), Tr, i is the mean initial reservoir temperature, Tr, a is the mean reservoir temperature at abandonment, and To is the ambient temperature. It is worth noting that equations (10) and (11) implicitly homogenize the entire reservoir and calculate the energy stored from mean reservoir properties. However, in the numerical studies performed in this work, each grid block or cell in the simulation domain has unique temperatures, density, bulk volume, etc. So, the recovery factor is calculated from the summation of the energy stored in each cell at the initial condition and at the end of the simulation. Therefore, the recovery factor (RF) is computed as follows:
where Vgj represents the grain volume in cell j at any pressure and temperature (which is the product of the cell volume and one minus the current porosity of the cell), Vg,ij is the initial value of the grain volume in cell j, and Trj is the current temperature in cell j. The superscript nc in the summation indicates that the equation is evaluated and summed over the total number of cells (nc) in the simulation domain.
Estimating the thermal energy of the produced hot water is essential for evaluating the commercial feasibility of an enhanced geothermal system. The “extractable” thermal energy depends on the produced fluid's amount and temperature. To estimate it, we first compute the extractable energy at the wellhead (Ewh):
where hwh and href are the enthalpies of the fluid at the wellhead and reference conditions, respectively. The symbol mwh represents the mass of hot water extracted from the producer. The mass flow rate can be calculated as follows:
Here, q is the volumetric flow rate at the wellhead in m3/s. Therefore, the cumulative thermal energy (Ecum) can be estimated by integrating the product of the mass flow rate (14) and (hwh−href) over a time interval (dt) in seconds:
This section verifies the extended MRST codes against the TOUGH3 simulator from the Lawrence Berkeley National Lab.
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This section presents the simulation studies of the SDF EGS configurations shown in Section 2.
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The cumulative thermal energy and produced fluid temperature profiles of the two SDF cases are almost identical, but the thermal recovery fraction of the eight SDF triplet is higher than that for the six SDF doublet configuration. To understand this counterintuitive observation, it is worth noting that both cases produce the same total fluid volume at almost identical temperatures, and the fracture volumes for both cases are approximately the same (within 0.28%). However, the triplet case has two producers, while the doublet case has only one producer. The average temperatures (after 50 years of simulated production) are 427 and 421 K for the doublet and triplet cases, respectively.
Although the temperature of the injection well is approximately the same in the two SDF cases, the production well temperature (shown in
A computation of the volume-weighted average temperature for the two SDF cases after 50 years of thermal recovery confirms that the thermal recovery fraction is indeed higher in the eight SDF triplet configuration. This yielded average temperatures of 422 K and 427 K for the eight SDF triplet and six SDF doublet configurations, respectively. The lower value of the eight SDF triplet configuration indicates that more thermal energy has been recovered from the geothermal reservoir. Additionally, this higher recovery fraction is consistent with the fact that the SDF triplet case will incur more drilling and completion costs (involving three wells) than the SDF doublet, which applies only two wells for the same reservoir domain.
To obtain insights into the thermal recovery from the three EGS configurations presented, the temperature profiles (after the simulated 50 years of thermal energy recovery) are presented in
As explained in Section 2.2, the six SDF doublet configuration uses fewer wells per unit SD fracture and provides the flexibility needed to use any number of SD fractures within a given area. In this section, the number of SD fractures (in the same domain presented in the previous section) is increased from six SDFs in the doublet configuration to 14. The idea is to evaluate the corresponding increase in thermal energy recovery as the number of SDF fractures increases. A corresponding MFHW case with the same total fracture area is also provided to facilitate a reasonable comparison with the state-of-the-art approach for thermal recovery from EGS.
To study the effect of natural fractures (NF) on thermal recovery from EGS, ADFNE was used to generate different realizations of natural fractures. This work used the fully dimensional or explicit fracture model, which involves partitioning each fracture into several fracture cells. Although this approach is very computationally expensive, it is the most accurate approach to model fractured reservoirs. The idea is to obtain high-resolution reference solutions, which can be used to validate the application of other fracture models such as discrete fracture models (DFM), embedded discrete fracture models (EDFM), projection-based embedded discrete fracture models (pEDFM) in EGS.
To further investigate the potential of large natural fractures to shortcircuit the desired fluid flow path in SDF EGS, four moderately sized conductive natural fractures were manually placed in the reservoir domain. In
Although the location of the natural fractures is fixed in the subsurface, the flexibility in the SD doublet fracture configurations can be leveraged to design the path of the SDFs so that they improve the thermal recovery instead of decreasing it due to a short-circuiting of the desired flow path. In contrast, the lack of control over the path of propagating hydraulic fractures makes it practically impossible to design MFHWs to take advantage of large natural fractures or faults, even when we know their location and orientation from image logs, and seismic and micro-seismic data. Furthermore, performing a similar study of the role of known large natural fractures on MFHWs is considered unnecessary because there is no technology to guarantee that any modeled hydraulic fracture configurations (that intersect the NFs at specific points) can be created in the subsurface.
This section discusses our numerical studies of the applicability of the proposed model by simulating a system representative of the Utah FORGE project. To this end, we obtained the model parameters from topical reports from the Utah FORGE Phase 2C, and these are summarized in Table 3. The thermal recovery from the representative Utah FORGE subsurface rock is modeled using the proposed SD configuration and the current approach, which is based on two pairs of parallel horizontal/deviated wells.
The images in
The plots of the cumulative thermal energy, produced fluid temperature, and thermal recovery fraction are given in
This paper presents high-resolution numerical simulation studies of the performance of the state-of-the-art MFHW approach to recover heat from EGS compared to our proposed approach that uses slot-drilled fractures. The performance plots and temperature profiles for all the simulated cases show that the proposed approach significantly outperforms the MFHW approach to different degrees, depending on the configuration of the SD fracture system and the model parameters. The proposed technology yields a 50% higher thermal recovery fraction for the representative Utah FORGE field case simulated. Other conclusions based on the various cases simulated can be summarized as follows:
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For completeness, it is worth clarifying that the single-phase formulation used in this work implies that the results are only directly applicable to low-enthalpy geothermal reservoirs. However, we do not expect the conclusions on the performance of the proposed technology relative to the state-of-the-art approach to change due to multiphase flow and the presence of salts and other impurities. Mechanical deformation can lead to a reduction in fracture conductivity over time if the pore pressure decreases considerably, but the continued injection of water during this process, as well as the availability of proppants, make this relatively less important.
This section presents the simulation results for the six SDF doublet series and parallel configurations. The results show that the SDF doublet parallel configuration yields slightly lower cumulative thermal energy and produced fluid temperature than the series configuration. In contrast, the SDF doublet parallel configuration yields a marginally higher thermal recovery fraction than its corresponding series configuration. This SDF series configuration's slightly higher produced fluid temperature could be due to the pressure-volume work, as evidenced by the increase in the injection and near-fracture pressures (up to 1.5 times the initial reservoir pressure). From equation 15, the higher produced fluid temperature in the SDF series configuration results in increased wellhead enthalpy and cumulative thermal energy. Conversely, we observed that the volume-weighted average temperature after 50 years of heat extraction is 428 and 427 K for the SDF doublet series and parallel cases, respectively. The observed higher thermal recovery fraction of the SDF doublet parallel case is consistent with equation 12, which indicates that the case with the lower average temperature yields a higher recovery fraction.
This section presents the result of the extended doublet case with fourteen slot drill fractures. Although the cumulative thermal energy and produced fluid temperature are higher in the series configuration, its thermal recovery fraction is lower. The artificially higher cumulative thermal energy and produced fluid temperature in the series configuration is because the injection pressure increases to two times the initial reservoir temperature in the series configuration. These high-pressure values induce pressure-volume work, resulting in higher cumulative thermal energy and fluid temperature. However, the average temperatures of the 14 SDF doublet series and parallel configurations are 386 and 382 K, respectively, after 50 years of thermal energy production. So, the thermal recovery fraction, as described by equation 12, is still higher in the parallel configuration than in the series configuration.
Although all simulations presented in the manuscript used no-flow and fully insulated boundary conditions, the trend in the results remains unchanged if the temperature is instead maintained constant on the outer faces of the simulation domain. To achieve this, the domain shown in
In addition to the forgoing, the various embodiments of the present disclosure include, but are not limited to, the embodiments set forth in the following clauses.
It should be noted that ratios, concentrations, amounts, and other numerical data may be expressed herein in a range format. It is to be understood that such a range format is used for convenience and brevity, and thus, should be interpreted in a flexible manner to include not only the numerical values explicitly recited as the limits of the range, but also to include all the individual numerical values or sub-ranges encompassed within that range as if each numerical value and sub-range is explicitly recited. To illustrate, a concentration range of “about 0.1% to about 5%” should be interpreted to include not only the explicitly recited concentration of about 0.1 wt % to about 5 wt %, but also include individual concentrations (e.g., 1%, 2%, 3%, and 4%) and the sub-ranges (e.g., 0.5%, 1.1%, 2.2%, 3.3%, and 4.4%) within the indicated range. In an embodiment, “about 0” can refer to 0, 0.001, 0.01, or 0.1. In an embodiment, the term “about” can include traditional rounding according to significant figures of the numerical value. In addition, the phrase “about ‘x’ to ‘y’” includes “about ‘x’ to about ‘y’”.
It should be emphasized that the above-described embodiments of the present disclosure are merely possible examples of implementations, and are set forth only for a clear understanding of the principles of the disclosure. Many variations and modifications may be made to the above-described embodiments of the disclosure without departing substantially from the spirit and principles of the disclosure. All such modifications and variations are intended to be included herein within the scope of this disclosure.
This application claims priority to, and the benefit of, co-pending U.S. provisional application entitled “System and Method for Using Controlled Fractures in Enhanced Geothermal Systems” having Ser. No. 63/443,221, filed Feb. 3, 2023, which is hereby incorporated by reference in its entirety.
Number | Date | Country | |
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63443221 | Feb 2023 | US |