Data-Driven Analyses of Low Salinity Waterflooding in Carbonates
Abstract
:1. Introduction
2. Methodology
2.1. Data Collection and Cleaning
2.2. Data Analysis Methods
3. Results and Discussion
3.1. Effect of LSW Governing Parameters on Oil Recovery
3.1.1. Linear Multivariable Regression
3.1.2. Nonlinear Multivariable Regression
3.2. Linking Mechanisms to Parameters
4. Conclusions
- •
- Different single parameters (such as salinity, contrast in salinity change, PDI concentration, oil acidity, base number of crude oil, permeability, and temperature) were individually analyzed using linear regression to study their correlation with the incremental oil recovery by LSW flooding. Negligible and weak relationships indicate that a single parameter is not sufficient to explain the performance of LSW injection.
- •
- Among groups of parameters, a set of oil/brine parameters that include AN, alteration in salinity, SO42− and cation concentrations, showed the best, but still weak, correlation. So, linear correlations are insufficient to forecast LSW potential.
- •
- A nonlinear relationship between parameters and RF was observed using ML models. Among the ML models, DT produced the best correlation for brine only parameters; the correlation coefficients for training and testing data were 0.57 and 0.35, respectively. For oil/brine parameters, all models showed strong and very strong relationships. However, ANN and SVM showed unsatisfactory results for testing data due to overfitting. In contrast, less overfitting was achieved by DT, where the correlation coefficients for training and testing data were 0.68 and 0.63, respectively.
- •
- Several mechanisms involved in the LSW process and the LSW effect cannot be explained by a single mechanism. MIE and rock dissolution are the most widely accepted mechanisms in the literature. These mechanisms result in wettability alteration in coreflooding tests in carbonates. Our studies showed that, by analyzing oil/brine parameters, a better understanding of the active mechanisms during LSW can be achieved, and it is possible to predict the mechanism by analyzing parameters such as salinity, ion concentrations, pH, and IFT.
- •
- Future research should be further conducted to confirm these findings by increasing the data set size. In addition, with more experimental data, other parameters should be added to the model to show fluid/fluid interactions.
Author Contributions
Funding
Acknowledgments
Conflicts of Interest
References
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Parameter | Number of Data Points | |
---|---|---|
Secondary Mode | Tertiary Mode | |
Porosity, % | 20 | 112 |
Permeability, mD | 28 | 117 |
Initial water saturation Swi, % | 23 | 116 |
Formation water composition, ppm | 26 | 117 |
Formation water salinity, ppm | 24 | 114 |
Secondary injected brine composition, ppm | 25 | 114 |
Secondary injected brine salinity, ppm | 25 | 116 |
Tertiary injected brine composition, ppm | - | 112 |
Tertiary injected brine salinity, ppm | - | 114 |
Crude oil acid number, mgKOH/g | 7 | 87 |
Crude oil base number, mgKOH/g | 1 | 64 |
Viscosity of oil, cp | 16 | 106 |
Density of oil, cp | 25 | 98 |
Residual oil saturation Sor, % | 7 | 37 |
pH of effluent brine | 0 | 27 |
Test temperature, °C | 8 | 100 |
Secondary recovery factor, %OOIP | 28 | 117 |
Tertiary recovery factor, %OOIP | - | 117 |
IFT, mN/m | 5 | 25 |
Contact angle | 2 | 27 |
Effluent cations concentration, ppm | 3 | 20 |
Effluent SO42− concentration, ppm | 1 | 9 |
Pressure drop, psi | 2 | 60 |
Zeta potential | 9 | 18 |
Parameter | Min | Max | Mean |
---|---|---|---|
Permeability, mD | 0.40 | 200.60 | 32.70 |
Low salinity, ppm | 0 | 193,230 | 22,315 |
SO42− concentration (LS), ppm | 0 | 9222 | 930 |
Cation concentration (LS), ppm | 0.0 | 13,454.5 | 1416.0 |
SO42− concentration (HS), ppm | 0 | 4290 | 534 |
Cation concentration (HS), ppm | 14.34 | 61,480.00 | 15,879.00 |
AN, mgKOH/g | 0.08 | 4.60 | 0.57 |
BN, mgKOH/g | 0.01 | 2.49 | 0.50 |
Temperature, °C | 20 | 250 | 88 |
Models | Number of Simulations | |||||
---|---|---|---|---|---|---|
100 | 1000 | 5000 | ||||
Training R | Testing R | Training R | Testing R | Training R | Testing R | |
SVM | 0.711 | 0.598 | 0.718 | 0.611 | 0.730 | 0.611 |
DT | 0.678 | 0.657 | 0.685 | 0.613 | 0.687 | 0.628 |
ANN | 0.751 | 0.527 | 0.759 | 0.592 | 0.754 | 0.593 |
Number of Layers | Number of Neurons | Results | |
---|---|---|---|
Training R | Testing R | ||
1 | 2 | 0.162 | 0.034 |
1 | 4 | 0.204 | 0.044 |
2 | 2 | 0.150 | 0.017 |
Parameters | Number of Data Points | Correlation Coefficient R | Strength of Relationship * | |
---|---|---|---|---|
Rock | Permeability | 118 | 0.1721 | Negligible |
Brine | Low salinity | 117 | 0.1059 | Negligible |
Change in salinity | 117 | 0.0460 | Negligible | |
Cations | 110 | 0.0290 | Negligible | |
SO42− | 107 | 0.1593 | Negligible | |
Oil | AN | 80 | 0.1848 | Negligible |
BN | 60 | 0.2334 | Weak | |
Temperature | T | 98 | 0.2647 | Weak |
Variable | R | Adjusted R2 | p-Value | No of Data Points | Strength of Relationship * |
---|---|---|---|---|---|
C + DC | 0.088 | −0.0028 | 1.89 × 10−5; 0.39 | 96 | Negligible |
C + DC + DS | 0.095 | −0.0012 | 2.7 × 10−5; 0.39; 0.73 | 96 | Negligible |
C + DC + DS + DTDS | 0.222 | 0.0181 | 0.14; 0.09; 0.05; 0.77 | 96 | Weak |
C + DC + AB | 0.200 | −0.0090 | 0.001; 0.35; 0.23 | 42 | Weak |
C + DC + AB + DTDS | 0.278 | 0.0044 | 0.6; 0.3; 0.21; 0.22 | 42 | Weak |
C + DC + AB + DTDS + DS | 0.290 | −0.0150 | 0.72; 0.31; 0.29; 0.19; 0.60 | 42 | Weak |
Parameters | Number of Data Points | Model | Average R for Training Data | Average R for Testing Data |
---|---|---|---|---|
DC + DS + DTDS | 96 | ANN | 0.20 | 0.04 |
SVM | 0.24 | 0.18 | ||
DT | 0.57 | 0.35 | ||
DC + DS + DTDS + AB | 42 | ANN | 0.75 | 0.59 |
SVM | 0.73 | 0.61 | ||
DT | 0.68 | 0.63 |
Parameters | Model | Strength of Relationship * | |
---|---|---|---|
Training Data | Testing Data | ||
DC + DS + DTDS | ANN | Weak | Negligible |
SVM | Weak | Negligible | |
DT | Strong | Moderate | |
DC + DS + DTDS + AB | ANN | Very strong | Strong |
SVM | Very strong | Strong | |
DT | Strong | Strong |
Paper | Mg2+ | Ca2+ | SO42− | Proposed Mechanism |
---|---|---|---|---|
Austad et al., 2012 | Increase | Increase | Rock dissolution | |
Chandrasekhar et al., 2016 | No change | Increase | Increase | Rock dissolution |
Awolayo et al., 2014 | Decrease | Decrease | MIE | |
Awolayo et al., 2016 | Increase | Decrease | Rock dissolution | |
Gupta et al., 2011 | No change | Increase | Rock dissolution | |
Mohammadkhani et al., 2018 | Increase | Decrease | MIE | |
Vo et al., 2012 | No change | Increase | Rock dissolution | |
Chandreskaer et al., 2018 | Decrease | Decrease | MIE |
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Salimova, R.; Pourafshary, P.; Wang, L. Data-Driven Analyses of Low Salinity Waterflooding in Carbonates. Appl. Sci. 2021, 11, 6651. https://doi.org/10.3390/app11146651
Salimova R, Pourafshary P, Wang L. Data-Driven Analyses of Low Salinity Waterflooding in Carbonates. Applied Sciences. 2021; 11(14):6651. https://doi.org/10.3390/app11146651
Chicago/Turabian StyleSalimova, Rashida, Peyman Pourafshary, and Lei Wang. 2021. "Data-Driven Analyses of Low Salinity Waterflooding in Carbonates" Applied Sciences 11, no. 14: 6651. https://doi.org/10.3390/app11146651
APA StyleSalimova, R., Pourafshary, P., & Wang, L. (2021). Data-Driven Analyses of Low Salinity Waterflooding in Carbonates. Applied Sciences, 11(14), 6651. https://doi.org/10.3390/app11146651