Application of time-frequency decomposition and seismic attributes for stratigraphic interpretation of thin reservoirs in "Jude Field", Offshore Niger Delta
Precise reservoir characterization has been challenging and demanding due to the in-homogeneity involving sand and shale distribution. The complexity of the subtle structures within thin reservoirs in the deep-water depositional system is another factor. The reservoirs of interest are trapped within an important area noted for exploration activities. Regardless, they can be bypassed considering the complexity that results in poor resolution of the seismic data. Fewer research activities have been carried out within the thinly bedded reservoirs. Spectral Decomposition (Time-Frequency Decomposition) was used for the characterization of the complicated reservoirs to delineate structural changes and stratigraphic information along interpreted horizons. Also, it gains insight into the stratigraphic setting and the complexity of the geology. The transformed results include tuning volumes and a variety of frequency slices. When the fast Fourier algorithm was applied to seismic reflection data, the seismic signal was broken down into its frequency components and allowed visualization of the data at specific frequencies. Stratigraphic and structural features that otherwise would have been overlooked in full bandwidth display were identified. The obtained result revealed concealed and complex geologic features such as multi-complex and meandering channels, subtle faults and lobes. Time-frequency decomposition of seismic data for thinly bedded reservoirs interpreted using high frequency has led to the precise delineation of geologic features of interest. This study will also help in the recovery of more hydrocarbon as bypassed zones and subtle structures are revealed.
Citation: O. A. Oluwadare, M.T. Olowokere, F. Taoili, P.A. Enikanselu, R.M. Abraham-Adejumo. Application of time-frequency decomposition and seismic attributes for stratigraphic interpretation of thin reservoirs in 'Jude Field', Offshore Niger Delta[J]. AIMS Geosciences, 2020, 6(3): 378-396. doi: 10.3934/geosci.2020021
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Abstract
Precise reservoir characterization has been challenging and demanding due to the in-homogeneity involving sand and shale distribution. The complexity of the subtle structures within thin reservoirs in the deep-water depositional system is another factor. The reservoirs of interest are trapped within an important area noted for exploration activities. Regardless, they can be bypassed considering the complexity that results in poor resolution of the seismic data. Fewer research activities have been carried out within the thinly bedded reservoirs. Spectral Decomposition (Time-Frequency Decomposition) was used for the characterization of the complicated reservoirs to delineate structural changes and stratigraphic information along interpreted horizons. Also, it gains insight into the stratigraphic setting and the complexity of the geology. The transformed results include tuning volumes and a variety of frequency slices. When the fast Fourier algorithm was applied to seismic reflection data, the seismic signal was broken down into its frequency components and allowed visualization of the data at specific frequencies. Stratigraphic and structural features that otherwise would have been overlooked in full bandwidth display were identified. The obtained result revealed concealed and complex geologic features such as multi-complex and meandering channels, subtle faults and lobes. Time-frequency decomposition of seismic data for thinly bedded reservoirs interpreted using high frequency has led to the precise delineation of geologic features of interest. This study will also help in the recovery of more hydrocarbon as bypassed zones and subtle structures are revealed.
1.
Introduction
Grey system theory is a method for forecasting and analyzing small sample sequences. It was first put forward by Deng [1,2] and has been widely used in various fields. In order to enhance the adaptability of the prediction model, Deng proposed a single-variable grey prediction model GM(2,1), which stands for one variable and second-order differential equation. However, due to defects in the structure, the prediction effect is not ideal in some cases [21]. In order to improve the prediction accuracy of the model, scholars put forward some improved models based on the classical GM(2,1) model. Shen et al. [3] proposed a method to determine the system parameters using the least square method to reduce error. Zeng et al. [4] proposed a new parameter estimation to GM(2,1) model based on accumulating method which reduces the matrix calculation quantity. A new healthier model was obtained and the serious morbidity problem with a multiple transformation on the initial data was resolved. In [5], two improved models are proposed based on modeling and predicting on non-linear rolling motion by GM(2,1), which are grey cycle extension and grey neural network respectively based on error compensation. Li et al. [6] introduced the GM(2,1) model and its improved algorithm and prediction steps by Matlab. By analyzing the shortcomings of GM(2,1) model, an optimized SOGM(2,1) model was constructed in [7] and applied to the prediction of high-speed roadbed settlement with higher prediction accuracy. In [8], Zhou et al. focused on the two shortcomings of GM(2,1) model and proposed appropriate measures for improvement. Moreover Zhou improved the method, which was used in solving albino equations of the classical GM(2,1) model, to solve the same equations by Laplace transform and improve the prediction accuracy. In [9], based on the GM(2.1) model, the boundary conditions were improved, and the effectiveness of the improved method was verified with grey data.
In [10], Wu et al. first discussed using perturbation theory and the least square method to address a violation of the new information priority principle in grey system theory. Ihis introduced a new grey system model with fractional order accumulation that reflects new information priority better with smaller accumulation orders. In recent years, various grey prediction models based on fractional order accumulation have been proposed in [11,12,13,14,15]. In [12], Wu improved the GM(2,1) using fractional order AGO to achieve an accurate prediction. Based on the GM(2,1) model with fractional order accumulation, Zeng [15] gave two different ways to determine the time response parameters of the fractional order GM(2,1) model, which can be flexibly selected according to the specific results in practical application.
The B-spline method has been widely applied to derive numerical solutions of partial differential equations. In [16], a cubic monotonicity-preserving interpolation spline was proposed to reconstruct the background value. In [17], Chen and Zhu developed a new GM(1,1) model based on C1 monotonicity-preserving rational linear interpolation spline to provide a more reasonable method to calculate the background value. In [18], in order to improve the GM (1,1) model, a formula based on a C1 monotonicitypreserving piecewise rational quadratic interpolation spline for calculating background value was proposed.
In the classical GM2(2,1) model, the corresponding estimated function x(2)(t) has the property of convexity and C∞ continuity. The classical GM2(2,1) model use the piecewise linear polynomial interpolation Lk(t)=(k+1−t)x(2)(k)+(t−k)x(2)(k+1), k=1,2,…,n−1 as an approximate solution of x(2)(t) so as to estimate background values z(2)(k+1) and the derivative values dx(2)(t)dt|t=k+1 and dx(2)(t)dt|t=k. It is well known that the piecewise linear polynomial interpolation has convexity-preserving property, but it just has C0 continuity and only has O(h2) order of convergence. In estimating dx(2)(t)dt|t=1, the classical GM2(2,1) model simply sets x(2)(0)=0, whereas this will cause error in estimating dx(2)(t)dt|t=1.
The main contribution of this work is to use a C1 convexity-preserving rational quadratic interpolation spline given in [19] as approximate solution of x(2)(t) so as to estimate background values z(2)(k+1) and the derivative values dx(2)(t)dt|t=k+1 and dx(2)(t)dt|t=k, k=1,2,…,n−1 and thereby a new GM2(2,1) model is established. The rest of this paper is structured as follows. Section 2 recall the construction of the C1 convexity-preserving interpolation spline given in [19]. In section 3, on the basis of C1 convexity-preserving rational quadratic interpolation spline, a new GM2(2,1) model is constructed in detail. Several numerical examples are given in section 4. The conclusion is given in section 5.
2.
Classical GM2(2,1) model
In this subsection, we recall the classical GM2(2,1) model. Let an original non-negative and uniformly-spaced sequence be
From [10], by using the fractional order accumulation operator, we can also rewrite x(r)(k) as x(r)(k)=k∑i=1(k−i+r−1k−i)x(0)(i),k=1,2,…,n. Here, (mn):=m!(m−n)!n! and (0n):=1,(n+1n):=0. In the following discussion, we mainly focus on r=2.
From Eq (2.1), we can obtain 1-AGO sequence X(1) and 2-AGO sequence X(2) as follows
From Eq (2.2), we can see that the 2-AGO sequence X(2) has convexity property, that is x(1)(k+2)=x(2)(k+2)−x(2)(k+1)≥x(2)(k+1)−x(2)(k)=x(1)(k+1). Suppose that x(2)(t) meets the following second order grey forecasting differential equation
d2x(2)(t)dt2+a1dx(2)(t)dt+a2x(2)(t)=b,
(2.3)
where α=(a1,a2,b)T is the parameter in the model to be estimated.
The corresponding characteristic function of Eq (2.3) is r2+a1r+a2=0. Consider the case that Δ=a21−4a2>0, then the roots of the characteristic function are r1,2=−a1±√Δ2.
Thus, the solution of Eq (2.3) with the initial condition ˜x(2)(1)=x(2)(1),˜x(2)(n)=x(2)(n) is as follows
Therefore, to obtain the prediction model of the original data sequence, we need to identify the effect of α. For this purpose, we do the integral accumulation on both sides of Eq (2.3) in each interval [k,k+1],k=1,2,…,n−1, then we can get
Let background value be z(2)(k+1):=∫k+1kx(2)(t)dt. In order to calculate the background value z(2)(k+1), we need to integrate x(2)(t), which requires the value of α to be given in advance. However, the value of α needs to be determined from the Eq (2.4). Consequently, to estimate the value of α, we must use some methods to estimate the background values z(2)(k+1), k=1,2,⋯,n−1. In the classical GM2(2,1) model, for t∈[k,k+1],k=1,2,…,n−1, we use the piecewise linear polynomial interpolation Lk(t):=(k+1−t)x(2)(k)+(t−k)x(2)(k+1) as an approximate solution of x(2)(t), that is x(2)(t)≈Lk(t) for t∈[k,k+1],k=1,2,…,n−1. Then we get the estimated background values z(2)(k+1), k=1,2,…,n−1 as follows
For dx(2)(t)dt|t=1, by setting x(2)(0)=0, then we get dx(2)(t)dt|t=1≈x(2)(1)−x(2)(0)=x(2)(1).
For each interval [k,k+1], k=1,2,…,n−1, by substituting the estimated background values z(2)(k+1) given in Eq (2.5) and the approximate derivative values dx(2)(t)dt|t=k+1 and dx(2)(t)dt|t=k into Eq (2.4), we have
With the estimated parameter α=(a1,a2,b)T, we further get the solution ˜x(2)(t) of the second order grad forecasting differential equation given in (2.3) with the initial condition ˜x(2)(1)=x(2)(1),˜x(2)(n)=x(2)(n). Finally, we get the following classical GM2(2,1) prediction formula
Given convexity data set {(xk,yk)∈R2}nk=1 with Δ1<Δ2<…<Δn−1, where x1<x2<…<xn and Δk=[yk+1−yk]/[xk+1−xk],k=1,2,…,n−1. For x∈[xk,xk+1], k=1,2,…,n−1, Let hk=xk+1−xk,t=(x−xk)/hk,Ak=Δk−dk,Bk=dk+1−Δk, then the C1 convexity-preserving rational quadratic interpolation spline S(x) developed in [19] is as follows
From Eq (3.1), it is easy to check that S(x+k)=yk,S(x−k+1)=yk+1,S′(x+k)=dk,S′(x−k+1)=dk+1, k=1,2,…,n−1 which implies that S(x)∈C1[x1,xn]. For Δ1<Δ2<…<Δn−1, from [19], we see that S″(x)>0, which means that S(x) has convexity-preserving properties. Furthermore, let f(x)∈C3[x1,xn] be a given convex function with which S(x) is compared and yi=f(xi),i=1,2,…,n, from [19], we have f(x)−S(x)=O(h3), which indicates that interpolant has O(h3) convergence. Since the C1 convexity-preserving rational quadratic interpolation spline S(x) developed in [19] has many merits, in the following we shall use it as approximate solution of x(2)(t) so as to estimate background values z(2)(k+1) and the derivative values dx(2)(t)dt|t=k+1 and dx(2)(t)dt|t=k and a method for estimating dx(2)(t)dt|t=1 will be given.
4.
Establish new GM2(2,1) model
For the original non-negative sequence X(0)={x(0)(1),x(0)(2),…,x(0)(n)}, we first calculate its 1-AGO sequence X(1)={x(1)(1),x(1)(2),…,x(1)(n)}, 2-AGO sequence X(2)={x(2)(1),x(2)(2),…,x(2)(n)}. From the above discussion, the 2-AGO sequence X(2) is a convex data set. The corresponding estimated function x(2)(t) has the property of convexity and C∞ continuity. Thus, we consider to reconstruct x(2)(t) with the C1 convexity-preserving rational quadratic interpolation spline developed in [19]. For the convex 2-AGO sequence data set {(xk,x(2)(k))∈R2}nk=1 with xk=k, for each of the subintervals [k,k+1], by using the C1 convexity-preserving rational quadratic interpolation spline given in (3.1) as approximate solution of x(2)(t), t∈[k,k+1], k=1,2,…,n−1, we have
where the derivative values dk, k=1,2,…,n are given by Eq (4.2).
Then, by substituting the estimated background values z(2)(k+1)=∫k+1kx(2)(t)dt and the estimated the derivative values dx(2)(t)dt|t=k+1 and dx(2)(t)dt|t=k, k=1,2,…,n−1 into the grey differential Eq (2.4) and applying the following least square method to solve Eq (2.4), we get
with dk, k=1,2,…,n are given by Eq (4.2) and z(2)(k+1)=∫k+1kx(2)(t)dtk=1,2,…,n−1 are given by Eq (4.3).
With the estimated parameter α=(a1,a2,b)T given by (4.5), we further solve the second order grad forecasting differential equation given in (2.3) with the initial condition ˜x(2)(1)=x(2)(1),˜x(2)(n)=x(2)(n), whose solution is denoted as ˜x(2)(t). Finally, we get the following new GM2(2,1) grey prediction formula
Summarize the above discussion, we give the following algorithm for establish our new grey prediction equation.
Algorithm 1 New grey prediction model based on a C1 convexity-preserving rational quadratic interpolation spline
Input: original non-negative and uniformly-spaced sequence X(0)={x(0)(1),x(0)(2),…,x(0)(n)}.
Output:grey prediction formula ˜x(0)(k), k=1,2,….
1: Compute the 2-AGO sequence X(2)={x(2)(1),x(2)(2),…,x(2)(n)} by Eq (2.2);
2: Compute the estimated derivative values dk, k=1,2,…,n by Eq (4.2);
3: Compute the estimated background values z(2)(k+1), k=1,2,…,n−1 by Eq (4.3);
4: Compute the estimated model parameter α by Eq (4.5);
5: With the estimated parameter α=(a1,a2,b)T, solve the second order grad forecasting differential equation given in (2.3) with the initial condition ˜x(2)(1)=x(2)(1),˜x(2)(n)=x(2)(n) so as to get ˜x(2)(t).
6: Get the grey prediction formula ˜x(0)(k), k=1,2,… by Eq (4.6).
5.
Numerical examples
We shall give several examples to show that the new GM2(2,1) model based on C1 convexity-preserving rational quadratic interpolation spline has better predict accuracy than the classical GM(2,1) model and GM2(2,1) model, Zeng's GM2(2,1) model given in [15] and Xu and Dang's GM(2,1) model given in [7]. In the following examples, the relative error is computed by
ε=|˜x(0)(k)−x(0)(k)|x(0)(k)×100%,k=1,2,….
Example 1.We take the total water consumption of Beijing from 2003 to 2019 in [20] as an example. We compare our new GM2(2,1) model with the classical GM(2,1) model, the classical GM2(2,1) model and Zeng's GM2(2,1) model given in [15]. We use the data from 2003 to 2015 as the training data and the data from 2016 to 2019 as the testing data. Table 1 gives the numerical results. The results show that the new GM2(2,1) has improved prediction accuracy compared to the classical GM(2,1) model, the classical GM2(2,1) model and Zeng's GM2(2,1) model.
Example 2.We take the precipitation data of Xichang City from 1986 to 1990 in [20] as the second example. We use the data from 1986 to 1989 as the training data and the data in 1990 as the testing data. From the numerical results presented in Table 2, it can be seen that compared with the classical GM(2,1) model, the classical GM2 (2,1) model and Zeng's GM2 (2,1) model given in [15], our new GM2 (2.1) has the best performance.
Example 3.In this example, we consider the historical syphilis incidence data of China from 2000 to 2008 given in [22].We use the data from 2000 to 2005 as the training data and the data from 2006 to 2008 as the testing data. We compare our new GM2(2,1) model with the classical GM(2,1) model, the classical GM2(2,1) model and Zeng's GM2(2,1) model given in [15]. Table 3 gives the numerical results. From the results, compared with the classical GM(2,1) model, the classical GM2(2,1) model and Zeng's GM2(2,1) model, the new GM2(2,1) has better performance.
Example 4.We take the data of inbound tourists (in 10,000 people) in Beijing from 2012 to 2019 as an example. The data comes from the Beijing Statistical Yearbook in Beijing Municipal Bureau of Statistics and Survey Office of the National Bureau of Statistics in Beijing. The unit is 10,000 people. We use the data from 2012 to 2015 as the training data and the data from 2016 to 2019 as the testing data. We compare our new GM2(2,1) model with the classical GM(2,1) model, the classical GM2(2,1) model and Zeng's GM2(2,1) model given in [15]. Table 4 gives the numerical results. From the results, compared with the classical GM(2,1) model, the classical GM2(2,1) model and Zeng's GM2(2,1) model, the new GM2(2,1) has the best prediction accuracy.
Example 5.In this example, we consider the data of tourists staying overnight in Guangzhou (in 10,000 people) from 2010 to 2019, which is from the Guangzhou Statistical Yearbook of Guangzhou Municipal Bureau of Statistics.The data from 2010 to 2015 are taken as the training data and the data from 2016 to 2019 are used as the testing data. Best prediction accuracy using our new GM2(2,1) model can be founded from the numerical results presented in Table 5, compared with the classical GM(2,1) model, the classical GM2 (2,1) model and Xu and Dang's GM(2,1) model given in [7].
Example 6.We take the data on China's foreign exchange reserves (in trillion dollars) from 2010 to 2021. The data is from the China Statistical Yearbook of National Bureau of Statistics of China. We use the data from 2010 to 2018 as the training data and the data from 2019 to 2021 as the testing data. We compare our new GM2(2,1) model with the classical GM(2,1) model, the classical GM2(2,1) model and Xu and Dang's GM(2,1) model given in [7]. Table 6 gives the numerical results. From the results, compared with the classical GM(2,1) model, the classical GM2(2,1) model and Xu and Dang's GM(2,1) model, the new GM2(2,1) has the best prediction accuracy.
Example 7.We take the data of inbound tourists (in 10,000 people) in Zaozhuang from 2005 to 2019 as an example. The data comes from the Ministry of Culture And Tourism of the People's Republic of China. The unit is 10,000 people. We use the data from 2005 to 2017 as the training data and the data from 2018 to 2019 as the testing data. We compare the new GM2(2,1) model with the classical GM(2,1) model, the classical GM2(2,1) model and the OFOPGM model given in [23]. Table 7 gives the numerical results. From the results, the new GM2(2,1) model has better prediction accuracy.
According to the results of the above numerical examples1–6, the prediction accuracy of our new GM2(2,1) model is improved for all the numerical examples compared to the classical GM(2,1) model, the classical GM2(2,1) model, Zeng's GM2(2,1) model given in [15], Xu and Dang's GM(2,1) model given in [7] and the OFOPGM model given in [23]. There are different degrees of improvement for different data features. Based on the above data characteristics, we make the conclusion that the more convexity the original datas presents the higher the prediction accuracy of the new GM2(2,1) model, the better the actual prediction effect.
6.
Conclusions
Using the C1 convexity-preserving rational quadratic interpolation spline developed in [19] to estimate the background values and derivative values, we established a new GM2(2,1) model. Numerical examples show that the new GM2(2,1) model can improve the forecasting quality, especially in prediction reliability and this model performs better when the original data are presented with convexity in time series. There is a limitation in the new method: The computations concerning the background values and derivative values take more time than the methods included in classical GM2(2,1) model. Future work will concentrate on applying C1 convexity-preserving rational quadratic interpolation spline to establish a new GMr(2,1) model with fractional r.
Use of AI tools declaration
The author declares he has not used Artificial Intelligence (AI) tools in the creation of this article.
Acknowledgments
The research is supported by the National Natural Science Foundation of China (No. 61802129).
Conflict of interest
The author declares no conflict of interest.
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O. A. Oluwadare, M.T. Olowokere, F. Taoili, P.A. Enikanselu, R.M. Abraham-Adejumo. Application of time-frequency decomposition and seismic attributes for stratigraphic interpretation of thin reservoirs in 'Jude Field', Offshore Niger Delta[J]. AIMS Geosciences, 2020, 6(3): 378-396. doi: 10.3934/geosci.2020021
O. A. Oluwadare, M.T. Olowokere, F. Taoili, P.A. Enikanselu, R.M. Abraham-Adejumo. Application of time-frequency decomposition and seismic attributes for stratigraphic interpretation of thin reservoirs in "Jude Field", Offshore Niger Delta[J]. AIMS Geosciences, 2020, 6(3): 378-396. doi: 10.3934/geosci.2020021
Figure 1. Map of Niger Delta showing the location of study and oil production sites [21]
Figure 2. Stratigraphic column showing the three formations of the Niger Delta [17,22]
Figure 3. Flow Chart of Methodology
Figure 4. Seismic to well tie in Well 001
Figure 5. Time Structural Map of Horizon 1
Figure 6. Depth Structural Map for Horizon 1
Figure 7. Variance Attribute enhancing structures the faults and fold
Figure 8. Selected Thin Horizons used for Interpretation
Figure 9. Amplitude spectrum of horizon 1 showing peaks of the frequencies
Figure 10. (a): The original 3D seismic data. (b): Enhanced Seismic data with continuous reflections and structures
Figure 11. Lobes and meandering channels across the field
Figure 12. (a): Time slice of frequency range at 12 Hz plotted against Red showing the thickest part of the channel in Map view. (b): Time slice of frequency range at 24 Hz plotted against Green showing the thick part of the channel in Map view. (c): Time slice of frequency range at 46 Hz plotted against blue showing the thinnest part of the channel in Map view
Figure 13. Workflow of the Spectral Decomposition of the horizons at a different frequency range of 12 Hz (low), 24 Hz (medium) and 46 Hz (High). The frequency responses are blended showing contrast in frequency and amplitude
Figure 14. Time-slice of RGB colour blend for the frequencies showing subtle geologic features such as meandering channels and faults for horizon 2
Figure 15. (a): Time-slice showing unconformity with Stratigraphic Contact. (b): Time-slice of RGB Blend showing unconformity with Stratigraphic Contact
Figure 16. Seismic section of the stratigraphic contact showing unconformity
Figure 17. Time-slice showing interpreted horizon 2 within the anticlinal fold
Figure 18. Direct Hydrocarbon Indicator of High Amplitude