scholarly journals Innovative CO2 Injection Strategies in Carbonates and Advanced Modeling for Numerical Investigation

Fluids ◽  
2019 ◽  
Vol 4 (1) ◽  
pp. 52 ◽  
Author(s):  
José Carlos de Dios ◽  
Yann Le Gallo ◽  
Juan Andrés Marín

Carbon sequestration in deep saline aquifers was recently developed at the industrial scale. CO2 injection experiences in carbonates are quite limited, most of them coming from projects carried out in porous mediums in the USA and Canada. Hontomín (Spain) is the actual on-shore injection pilot in Europe, being a naturally fractured carbonate reservoir where innovative CO2 injection strategies are being performed within the ENOS Project. CO2 migration through the fracture network existing on site produces hydrodynamic, mechanical and geochemical effectsdifferent from those caused by the injection in mediums with a high matrix permeability. The interpretation of these effects is required to design safe and efficient injection strategies in these formations. For this, it is necessary to determine the evolution of pressure, temperature and flow rate during the injection, as well as the period of pressure recovery during the fall-off phase. The first results from the not-continuous injections (8–24 h) conducted at Hontomín reveal the injection of liquid CO2 (density value of 0.828 t/m3) and the fluid transmissivity through the fractures. Taking into account the evolution of the pressure and flow rate showed variations of up to 23% and 30% respectively, which means that the relevant changes of injectivity took place. The results were modeled with a compositional dual media model which accounts for both temperature effects and multiphase flow hysteresis because alternative brine and CO2 injections were conducted. Advanced modeling shows the lateral extension of CO2 and the temperature disturbance away from the well.

Author(s):  
J. Carlos de Dios ◽  
Yann Le Gallo ◽  
Juan A. Marín

CO2 geological storage in deep saline aquifers was recently developed at industrial scale mainly in sandstone formations. Experiences on CO2 injections in carbonates aquifers for permanent trapping are quite limited, mostly from US projects such as AEP Mountaineer, Michigan and Williston Basin. The behavior of fractures in carbonates plays a key role in those reservoirs in which porous matrix permeability is very poor, which drives the CO2 plume migration through the fracture network where hydromechanics and geochemical effects take place due to injection. Hontomín (Spain) is the actual on-shore injection pilot in Europe (EP Resolution of 14 January 2014), whose reservoir is comprised of fractured carbonates. Existing experiences from field scale tests conducted on site have supported to better understand the behavior of this type of reservoirs for CO2 geological storage. Innovative CO2 injection strategies are being carried out in ENOS Project (EU H2020 Programme, http://www.enos-project.eu). First results based on field tests conducted at Hontomín, and the advanced modelling developed so far will be analyzed and discussed in this article, as well as, the description of future works. The evolution of operating parameters such as flow rate, pressure and recovery term during the tests confirm the CO2 migration through the fractures.


Geosciences ◽  
2018 ◽  
Vol 8 (9) ◽  
pp. 354 ◽  
Author(s):  
Yann Le Gallo ◽  
José de Dios

Investigation into geological storage of CO2 is underway at Hontomín (Spain). The storage reservoir is a deep saline aquifer formed by naturally fractured carbonates with low matrix permeability. Understanding the processes that are involved in CO2 migration within these formations is key to ensure safe operation and reliable plume prediction. A geological model encompassing the whole storage complex was established based upon newly-drilled and legacy wells. The matrix characteristics were mainly obtained from the newly drilled wells with a complete suite of log acquisitions, laboratory works and hydraulic tests. The model major improvement is the integration of the natural fractures. Following a methodology that was developed for naturally fractured hydrocarbon reservoirs, the advanced characterization workflow identified the main sets of fractures and their main characteristics, such as apertures, orientations, and dips. Two main sets of fracture are identified based upon their mean orientation: North-South and East-West with different fracture density for each the facies. The flow capacity of the fracture sets are calibrated on interpreted injection tests by matching their permeability and aperture at the Discrete Fracture Network scale and are subsequently upscaled to the geological model scale. A key new feature of the model is estimated permeability anisotropy induced by the fracture sets.


2021 ◽  
Vol 9 ◽  
Author(s):  
B. B. T. Wassing ◽  
T. Candela ◽  
S. Osinga ◽  
E. Peters ◽  
L. Buijze ◽  
...  

This paper describes and deploys a workflow to assess the evolution of seismicity associated to injection of cold fluids close to a fault. We employ a coupled numerical thermo-hydro-mechanical simulator to simulate the evolution of pressures, temperatures and stress on the fault. Adopting rate-and-state seismicity theory we assess induced seismicity rates from stressing rates at the fault. Seismicity rates are then used to derive the time-dependent frequency-magnitude distribution of seismic events. We model the seismic response of a fault in a highly fractured and a sparsely fractured carbonate reservoir. Injection of fluids into the reservoir causes cooling of the reservoir, thermal compaction and thermal stresses. The evolution of seismicity during injection is non-stationary: we observe an ongoing increase of the fault area that is critically stressed as the cooling front propagates from the injection well into the reservoir. During later stages, models show the development of an aseismic area surrounded by an expanding ring of high seismicity rates at the edge of the cooling zone. This ring can be related to the “passage” of the cooling front. We show the seismic response of the fault, in terms of the timing of elevated seismicity and seismic moment release, depends on the fracture density, as it affects the temperature decrease in the rock volume and thermo-elastic stress change on the fault. The dense fracture network results in a steeper thermal front which promotes stress arching, and leads to locally and temporarily high Coulomb stressing and seismicity rates. We derive frequency-magnitude distributions and seismic moment release for a low-stress subsurface and a tectonically active area with initially critically stressed faults. The evolution of seismicity in the low-stress environment depends on the dimensions of the fault area that is perturbed by the stress changes. The probability of larger earthquakes and the associated seismic risk are thus reduced in low-stress environments. For both stress environments, the total seismic moment release is largest for the densely spaced fracture network. Also, it occurs at an earlier stage of the injection period: the release is more gradually spread in time and space for the widely spaced fracture network.


2020 ◽  
Vol 8 (4) ◽  
pp. SP109-SP133 ◽  
Author(s):  
Heloise Bloxsom Lynn ◽  
Bill Goodway

A 3D P-P high-fold full-azimuth full-offset reflection survey was acquired and processed to characterize a naturally fractured carbonate reservoir. The reservoir is a thick carbonate, which will flow commercial oil with a sufficient fracture network. Extensive calibration data include (1) a horizontal borehole’s resistivity image log, (2) the first 24 months cumulative oil produced, by stage, as known from chemical frac tracer data, (3) pre- and postfrac job instantaneous shut-in pressures, (4) microseismic, and (5) wireline log data. We used the cumulative oil production to document the spatially varying amount of aligned vertical porosity (aligned compliance or fracture porosity) connected to the stage borehole location. The stages of high oil production exhibited, for the fracture-perpendicular azimuth, the more positive amplitude variation with angle (AVA) gradients, and dimmer near-angle (6°–15° angles of incidence) amplitudes, compared to the fracture-parallel azimuth. The azimuthal variation of the AVA gradient fit the cos 2θ curve well, indicating the presence of one set of vertical aligned fractures dominating the azimuthal amplitude signature. In a similar fashion, the azimuthal variation of the mathematical intercept, physically the near-angle amplitudes, also fit the cos 2θ curve well. We have constructed crossplots of the azimuthal near-angle amplitude versus the AVA gradient on a bin-by-bin basis: we observed a straight line at bins with elevated oil production (elevated fracture density). A straight line crossplot of the (AVA gradient, mathematical intercept) is the signature of change of the (sensed) porosity, as long as the lithology and pore fluid are held constant. In accord with industry knowledge, we found that porosity affects the P impedance and thus the near-angle amplitudes: the aligned porosity yields azimuthal P impedance (measured at the 6°–15° angles of incidence). Legacy high-fold 3D P-P surveys rich in the 6°–20° angles of incidence should be considered for reprocessing and reinterpretation using these techniques.


2006 ◽  
Vol 9 (02) ◽  
pp. 173-185 ◽  
Author(s):  
Salem E. Salem ◽  
Maged El Deeb ◽  
Medhat K. Abdou ◽  
Steef J. Linthorst ◽  
Asnul Bahar ◽  
...  

Summary This paper presents the methodology, implementation, and results of the dynamic modeling of a naturally fractured carbonate reservoir, which consists of a fracture swarm system and high matrix permeability. The focus of this paper is on the description of the dynamic single-media model that was used to history match the production. The challenges in properly quantifying the separate effects of matrix and fracture within the framework of a single-media model become the major objective of the study. A brief description of the static model (which consists of the development of matrix and fracture models, as well as the method to integrate them) is also presented. Both matrix and fracture systems play an important role in the production mechanism of the reservoir. History matching for 20 years of production was done successfully in a single-media model through an iterative process between static and dynamic models to ensure the consistency between the two models. Different sets of relative permeability curves (for matrix and fracture systems) were generated to properly simulate the fluid movement in the reservoir. The results indicate an excellent history match that is also followed by the success in the blind tests of newly drilled wells. Significant improvement was obtained compared to the previous model in simulating water production that comes from the aquifer to the wells through a complex fracture network. The results were achieved through various sensitivity analyses of fracture conductivity and by fine-tuning relative permeability curves that are based on the eight rock types defined for the reservoir. In conclusion, the single-media model used in this study can successfully simulate the behavior of a naturally fractured reservoir. The model has shown that it can produce excellent results in a very practical way. The methodology described in this paper is suitable for other naturally fractured reservoirs, especially in the Middle East area, where a significant difference between core-derived permeability and well-test-derived permeability exists. Introduction This paper presents the methodology, implementation, and results of the dynamic modeling of a naturally fractured carbonate reservoir of an oil field in the Middle East. The study is part of the field's Reservoir Management and Long Term Development Plan (LTDP). The overall objective of the study is to obtain a representative model that can be used to improve the reliability of the predictions of future performance for the reservoir. The specific objective is to match the 20 years of production history and to predict field future performance with three flow-simulation models that represent the Low (pessimistic), Medium (most-likely), and High (optimistic) cases. The dynamic model (or flow-simulation model) is based on a static model that was generated through a detailed integrated reservoir characterization study (Al-Deeb et al. 2002; Bahar et al. 2001, 2003a, 2003b; Charfeddine et al. 2002; Ates et al. 2003). The study included the integration of various data/information from the geology, geophysics, and engineering disciplines using a stochastic approach. The static model was developed in a fine-scale grid system of 4.2 million cells that has been upscaled into a coarse-scale grid system of 181,000 cells. The upscaling was performed through a grid optimization process using the streamline simulation to maintain a high level of heterogeneity in the reservoir as much as possible (Ates et al. 2003). The main characteristic of this reservoir is the presence of a complex fracture network within the highly heterogeneous matrix system. Additionally, the reservoir is characterized by the presence of Sucrosic Dolomite rock (mainly in the south part of the Middle reservoir unit) that significantly enhances matrix permeability further. Matrix permeability ranges from 0.01 md to 12 Darcy, with the average in excess of 100 md. The fractures are described as fracture corridor systems (or fracture swarms) that show two major trends, namely N40E and N70E. Fracture swarms/subseismic faults are structural features extending laterally over several hundred meters (and, sometimes, over several kilometers). This network was assumed to be extended fully in the vertical direction. It is assumed that there are very few fractures outside the fracture swarms. The flow-simulation model used for the dynamic modeling is the single-media model. Besides having the advantage of being computationally efficient, it is believed that a single-medium model is adequate for this reservoir because it does not consist of a diffuse fracture system but, rather, fracture swarms, as described in the previous paragraph. Three major stages of dynamic modeling, namely Stage 1 (original model), Stage 2 (calibrated model), and Stage 3 (final model), are presented in this paper (Fig. 1). The progress at each stage is evaluated with a newly developed scoring system. With this system, an objective tool is used to monitor the progress of the history matching. The score achieved at each stage for the Medium case is also shown in Fig. 1. The history matching of the three realizations (Low, Medium, and High) has been done in the following manner. First, the Medium case is run until it reaches a certain point, at which significant understanding of the model has been obtained. In this study, this point refers to the condition in which approximately 75% of history matching of the medium case has been achieved. At this point, lessons learned from the Medium case are applied to the other two cases. Ultimately, the overall goal of the study is to have the tool for a better prediction of future performance. The prediction run is currently ongoing. The topic of future performance is beyond the scope of this paper.


SPE Journal ◽  
2016 ◽  
Vol 21 (01) ◽  
pp. 112-120 ◽  
Author(s):  
Øyvind Eide ◽  
Martin A. Fernø ◽  
Zachary Alcorn ◽  
Arne Graue

Summary This work demonstrates that diffusion may be a viable oil-recovery mechanism in fractured reservoirs during injection of carbon dioxide (CO2) for enhanced oil recovery, depending on the CO2 distribution within the fracture network and distance between fractures. High oil recovery was observed during miscible, supercritical CO2 injection (RF = 86% original oil in place) in the laboratory with a fractured chalk core plug with a large permeability contrast. Dynamic 3D fluid saturations from computed-tomography (CT) imaging made it possible to study the local oil displacement in the vicinity of the fracture, and to calculate an effective diffusion coefficient with analytical methods. The obtained diffusion coefficient varies between 0.83 and 1.2 ×10−9m2/s, depending on the method used for calculation. A numerical sensitivity analysis, with a validated numerical model that reproduced the experiments, showed that the rate of oil production during CO2 injection declined exponentially with increasing diffusion lengths from the CO2-filled fracture and oil-filled matrix. In a numerical upscaling effort, with the experimentally achieved diffusion coefficient, oil-recovery rates and local flow were studied in an inverted five-spot pattern in a heavily fractured carbonate reservoir.


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