Analysis of Pressure/Flow-Rate Data With the Pressure-History-Recovery Method

1999 ◽  
Vol 2 (04) ◽  
pp. 314-324
Author(s):  
Patrick Gilly ◽  
Roland N. Horne

Summary This study presents a new way to integrate flow rate history and pressure history data in well-test analysis. The method used is an extension of the deconvolution principle to a chosen period of time before the well test. It is based on the recovery of missing parts of the pressure history by taking into account the flow rate history and the available sections of measured pressure history. The method has the advantage of working without making any assumption about the reservoir by using the data itself to define the "model." A real example with 71 pressure points and 70 corresponding flow rate points shows how it is possible to recover the first 20 pressure points correctly considering that only the flow rate history and the last 51 pressure points are known. The main purpose of this procedure is to have an alternative to treat the problem of flow rate variations both before and during the well test. In such a case, neither the usual deconvolution (only applicable for flow rate variations during the well test, when flow rate and pressure are both known), nor the multirate superposition plots (which assume specific reservoir behavior) can be applied properly. In addition, the principle of the method enables us to extend its use to the analysis of well tests with pressure recording errors or missing pressure recording. Examples show that it is possible to make a good analysis of a well test with missing pressure regions when current methods give only parts of the information. Introduction In practical well testing, it is rare to encounter pressure responses generated by only a simple constant step change of rate production. Generally, well tests contain a series of different flow rates or a continuously varying flow rate, and the measured pressure responses are combinations of the pressure transients due to the varying flow rate. Several methods have been developed to perform model recognition when the flow rate pattern is not a perfect drawdown. All these methods integrate, more or less, flow rate data to improve the interpretation. A first set of these methods are those proposed by Horner, 1 Miller et al., 2 and Agarwal3 to treat buildups as drawdowns. With changing flow rate, it is common to resort to the principle of deconvolution (Kuchuk4), thanks to the convenience of the Laplace transform (van Everdingen and Hurst5), when flow rate variations occur during well test, or to handle the convolution with multirate superposition plot techniques (Earlougher 6) when changes of production rate are prior to the pressure recording. However, none of these procedures is completely accurate in handling variations of flow rate both before and during the well test. This paper presents an alternative method to take into account continuously varying flow rate data. This new technique, based on the recovery of missing pressure history (or parts of the pressure history), extends the use of the deconvolution principle to the whole flow rate history. The method is a general procedure, and can be applied to any type of reservoir with any production rate pattern. In fact, the presentation procedure is a simple mathematical treatment using the available data only, that allows us to find an approximation of the missing pressure consistent with the measured pressure and flow rate. After the mathematical background and the description of the method, a simple example, used to demonstrate and refine the algorithm, is presented. Next, a synthetic example shows how the technique can be helpful to solve common well test interpretation problems such as a lack of pressure measurements or obvious pressure recording errors. In such cases, unlike the traditional methods, our procedure enables us to perform a good analysis. Mathematical Preliminaries Dimensionless Variables. Parts of the mathematical treatment of the data require the use of dimensionless variables. Because the permeability, k, is unknown during the procedure, it is impossible to use the usual definitions to calculate the dimensionless variables. Instead, we define characteristic pressure, pref, flow rate, qref, and time, tref from the real data. Thus (1)pD=Δppref; qD=qqref; tD=ttref. We then specify (in consistent units) (2)βp=prefqref=Bμ2πkh (3) and  C D = β p q ref t ref . In oilfield units, Eqs. (2) and (3) must be written: (4)βp=141.2Bμkh, CD=qB24βpqreftref. Laplace Transform. If s is the Laplace variable, the definition of the Laplace transform related to the time, t, is (5)L[f(t)]=f¯(s)=∫0∞e−stf(t)dt. Here, f(t) a continuous function of time, can be either the pressure or the flow rate. Therefore, every variable in the Laplace space has a dimension equal to its dimension in real space multiplied by time. For its part, s has the dimension of reciprocal time. So, the dimensionless variables, in Laplace space, are (6)sD=stref;   p¯D=p¯preftref;   q¯D=q¯qreftref. The integral definition in Eq. (5) can be used for dimensionless variables, but in this case s must be replaced by sD.

1998 ◽  
Vol 1 (03) ◽  
pp. 268-277 ◽  
Author(s):  
M. Onur ◽  
A.C. Reynolds

Abstract In recent years, the numerical Laplace transformation of sampled-data has proven to be useful for well test analysis applications. However, the success of this approach is highly dependent on the algorithms used to transform sampled-data into Laplace space and to perform the numerical inversion. In this work, we investigate several functional approximations (piecewise linear, quadratic, and log-linear) for sampled-data to achieve the "forward" Laplace transformation and present new methods to deal with the "tail" effects associated with transforming sampled-data. New algorithms that provide accurate transformation of sampled-data into Laplace space are provided. The algorithms presented can be applied to generate accurate pressure-derivatives in the time domain. Three different algorithms investigated for the numerical inversion of sampled-data. Applications of the algorithms to convolution, deconvolution, and parameter estimation in Laplace space are also presented. By using the algorithms presented here, it is shown that performing curve-fitting in the Laplace domain without numerical inversion is computationally more efficient than performing it in the time domain. Both synthetic and field examples are considered to illustrate the applicability of the proposed algorithms. Introduction Due to its efficiency, the Stehfest algorithm for the numerical inversion of the Laplace transform is now a well established tool in pressure transient analysis research and applications. Roumboutsos and Stewart showed that convolution and deconvolution in Laplace domain with the aid of the numerical Laplace transformation of measured pressure and/or rate data is more efficient and stable than techniques based on the discretized form of convolution integral in the time domain. Use of the numerical Laplace transformation of tabulated (pressure and/or rate) data has become increasingly popular in recent years for other well testing analysis purposes in a variety of applications; see for example, Refs. 3-10. Guillot and Horne were the first to use piecewise constant and cubic spline interpolations to represent measured flow rate data in Laplace space for the purpose of analyzing pressure tests under variable (downhole or surface) flow rate history by nonlinear regression. Roumboutsos and Stewart were the first to introduce the idea of using the numerical Laplace transformation of measured data for convolution and deconvolution purposes. They presented an algorithm based on piecewise linear interpolation of sampled-data, which can be used to transform measured pressure or rate data into Laplace space. Mendes et al. presented a Laplace domain deconvolution algorithm based on cubic spline interpolation of sampled-data. By considering deconvolution of DST data, they showed that Laplace domain deconvolution is fast and more stable than deconvolution methods based on the discretized forms of the convolution integral in the time domain. However, they noted that noise in pressure and flow rate measurements can also cause instability in Laplace space deconvolution methods, but they did not present any specific results on this issue. Both Corre and Thompson et al. showed that the convolution methods based on a representation of the linear interpolation of the tabulated unit-rate response solution and numerical inversion to the time domain are far more computationally efficient for generating variable rate solutions for complex well/reservoir systems (e.g., partially penetrating wells and horizontal wells) than convolution methods based on the direct use of analytical solutions in Laplace space. Using the numerical Laplace transformation of measured pressure data, Bourgeois and Horne introduced the so-called Laplace pressure and its derivative, and presented Laplace type curves based on these functions for model recognition and parameter estimation purposes. They also deconvolved data using these Laplace pressure functions in the Laplace domain without inversion to the time domain. Wilkinson investigated the applicability of performing nonlinear regression based on the Laplace pressure as suggested in Ref. 7 for parameter estimation purposes.


1986 ◽  
Vol 23 (04) ◽  
pp. 851-858 ◽  
Author(s):  
P. J. Brockwell

The Laplace transform of the extinction time is determined for a general birth and death process with arbitrary catastrophe rate and catastrophe size distribution. It is assumed only that the birth rates satisfyλ0= 0,λj> 0 for eachj> 0, and. Necessary and sufficient conditions for certain extinction of the population are derived. The results are applied to the linear birth and death process (λj=jλ, µj=jμ) with catastrophes of several different types.


Author(s):  
Charles L. Epstein ◽  
Rafe Mazzeo

This chapter describes the construction of a resolvent operator using the Laplace transform of a parametrix for the heat kernel and a perturbative argument. In the equation (μ‎-L) R(μ‎) f = f, R(μ‎) is a right inverse for (μ‎-L). In Hölder spaces, these are the natural elliptic estimates for generalized Kimura diffusions. The chapter first constructs the resolvent kernel using an induction over the maximal codimension of bP, and proves various estimates on it, along with corresponding estimates for the solution operator for the homogeneous Cauchy problem. It then considers holomorphic semi-groups and uses contour integration to construct the solution to the heat equation, concluding with a discussion of Kimura diffusions where all coefficients have the same leading homogeneity.


2005 ◽  
Vol 50 (1-2) ◽  
pp. 179-185 ◽  
Author(s):  
P.G. Massouros ◽  
G.M. Genin

2021 ◽  
Vol 2021 (1) ◽  
Author(s):  
Raheel Kamal ◽  
Kamran ◽  
Gul Rahmat ◽  
Ali Ahmadian ◽  
Noreen Izza Arshad ◽  
...  

AbstractIn this article we propose a hybrid method based on a local meshless method and the Laplace transform for approximating the solution of linear one dimensional partial differential equations in the sense of the Caputo–Fabrizio fractional derivative. In our numerical scheme the Laplace transform is used to avoid the time stepping procedure, and the local meshless method is used to produce sparse differentiation matrices and avoid the ill conditioning issues resulting in global meshless methods. Our numerical method comprises three steps. In the first step we transform the given equation to an equivalent time independent equation. Secondly the reduced equation is solved via a local meshless method. Finally, the solution of the original equation is obtained via the inverse Laplace transform by representing it as a contour integral in the complex left half plane. The contour integral is then approximated using the trapezoidal rule. The stability and convergence of the method are discussed. The efficiency, efficacy, and accuracy of the proposed method are assessed using four different problems. Numerical approximations of these problems are obtained and validated against exact solutions. The obtained results show that the proposed method can solve such types of problems efficiently.


2020 ◽  
Vol 57 (4) ◽  
pp. 1045-1069
Author(s):  
Matija Vidmar

AbstractFor a spectrally negative self-similar Markov process on $[0,\infty)$ with an a.s. finite overall supremum, we provide, in tractable detail, a kind of conditional Wiener–Hopf factorization at the maximum of the absorption time at zero, the conditioning being on the overall supremum and the jump at the overall supremum. In a companion result the Laplace transform of this absorption time (on the event that the process does not go above a given level) is identified under no other assumptions (such as the process admitting a recurrent extension and/or hitting zero continuously), generalizing some existing results in the literature.


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