Resistivity Modeling of Array Laterolog Tools: An Application in an Offshore Norway Clastic Reservoir

2005 ◽  
Vol 8 (01) ◽  
pp. 77-87
Author(s):  
M.T. Galli ◽  
M. Gonfalini ◽  
M. Mele ◽  
P. Belik ◽  
O. Faivre ◽  
...  

Summary Resistivity logs, while used extensively in the oil industry for the determination of water-saturation profiles and, consequently, for the quantification of hydrocarbon originally in place (HOIP), are strongly affected by environmental effects such as borehole, shoulder-bed resistivity contrasts, mud-filtrate invasion, dipping beds, and electrical anisotropy. It is well known by log interpreters that the combination of the different effects may strongly affect the estimation of hydrocarbon in place and hydrocarbon reserves. This paper highlights the strong reduction of the uncertainties in water-saturation determination and, consequently, the petrophysical characterization of the reservoir achieved by applying the appropriate 2Dresistivity-modeling and -inversion techniques to two wells of the Norwegian offshore area. Both wells were drilled in a sandstone reservoir, with some thin-bedded intervals, and affected by the presence of anomalous invasion profiles. Introduction Resistivity logs, as directly used for the determination of water-saturation profiles, have always been of focal interest for the oil industry; it is clear that the quality of these measurements, currently used in the net-pay and hydrocarbon-in-place determinations, must be very high. As a consequence, more accurate and flexible resistivity tools have been developed in recent years. We will address the family of array tools, particularly the HRLA,* which makes available a set of five galvanic resistivity measurements at different depths of investigation. Unfortunately, the most common types of environmental noise (borehole effects, shoulder-bed resistivity contrasts, invasion, the presence of dips, and anisotropy) still alter the measured resistivity, thus affecting the estimation of the true resistivity in hydrocarbon-bearing levels. To remove these alterations, we have developed a 2D resistivity modeling and inversion technique that can correct a number of environmental effects simultaneously. This paper presents the results obtained in two wells of the same reservoir in the offshore Norway area, where the sandstone bodies are interbedded with deltaic shales. The values of porosity and permeability are generally very high, and a complete set of data [conventional and special core analysis, conventional wireline logs, microresistivity imaging logs, nuclear magnetic resonance (NMR), and sedimentological analysis from core and images] is available. The 2D modeling provides a better definition of the water saturation in the thinner sandstone bodies of the sequence and in the presence of anomalous invasion profiles. When comparing the resistivity-modeling results with those obtained by standard interpretation techniques, we can see the effectiveness of the developed methodologies (both hardware and software) in improving the reservoir characterization and in maximizing the return of the investments in logging and well-data measurements. The aim of this paper is two-fold: the authors want to show how complex reservoir studies can benefit from the correct integration of heterogeneous geological data, while addressing at the same time the added value of applying a 2D modeling and inversion numerical technique to resistivity measurements to compute accurate water-saturation profiles. One of the most important issues of the formation-evaluation process is the correct estimation of all the petrophysical parameters necessary to determine the hydrocarbon content of the reservoir. This implies the need to compute a saturation profile as correct as possible. Because Sw (and, consequently, Sh)strongly depends on resistivity, porosity, and shale volume, it is of the utmost importance that the uncertainty on these measurements be kept very low. In recent years, the accuracy of resistivity tools has been improved greatly by the introduction of array measurements1,2; unfortunately, the utter complexity of real formations can often lessen the intrinsic advantages of the available logs. The most common environmental noise sources, as listed in many well-knownworks,3–5 are:Thin beds and/or dips.Deep and/or exotic invasion profiles.High resistivity contrasts between mineralized (porous) and tight layers(shoulder effects).Electrical anisotropy (usually related to laminations and grain-size variations). In most cases, their combined effects cannot be removed separately but must be treated as a unique, nonlinear problem. In previous work,6–9 it has been shown how resistivity modeling and inversion techniques can solve these kinds of problems, provided that an appropriate and fast forward model (2D or 3D) is available for all the acquired tools and that a robust and efficient inversion algorithm can be implemented. In the following paragraphs, we will show how the integration of different types of data [geological studies, wireline logs, nuclear magnetic resonance(NMR) measurements, core data], together with the most advanced numerical interpretation techniques, can produce accurate and robust results for many formation-evaluation problems, thus reducing the uncertainty of the estimation of the petrophysical parameters that are relevant in reservoir studies. The importance of geological and petrophysical information in defining a correct formation model was also addressed in a recent paper,10 which shows how this is also useful in constraining the inversion process. For this reason, we will first describe the geological setting of the reservoir and the available data, highlighting the interpretation process and the problems encountered; we will then focus on the methodology used for the evaluation of the correct water-saturation profile from resistivity measurements, demonstrating how this methodology, based on modeling and inversion techniques, can enhance the robustness of the results, as confirmed by different sources of information. Because the field study has not been yet completed, from the reservoir point of view, the conclusions will not be definitive, and the paper will end with a work-in-progress description of future activities. We will, however, be able to state the advantages of the proposed numerical modeling and inversion technique applied to laterolog array measurements, especially when in the presence of data of different qualities.

2021 ◽  
Vol 147 ◽  
pp. 106500
Author(s):  
Marie Antoinette Alhajj ◽  
Sébastien Bourguignon ◽  
Sérgio Palma-Lopes ◽  
Géraldine Villain

Geophysics ◽  
2010 ◽  
Vol 75 (6) ◽  
pp. F173-F185 ◽  
Author(s):  
Ann E. Cook ◽  
Barbara I. Anderson ◽  
Alberto Malinverno ◽  
Stefan Mrozewski ◽  
David S. Goldberg

In 2006, the Indian National Gas Hydrate Program Expedition 01, or NGHP-01, discovered gas hydrate as fill in near-vertical fractures in unconsolidated sediments at several drilling sites on the Indian continental margins. These gas hydrate-filled fractures were identified on logging-while-drilling resistivity images. The gas hydrate-filled fracture intervals coincide with high measured resistivity at the NGHP-01 sites. High measured resistivity translates into high hydrate saturations via Archie’s equation; however, these high saturations contradict lower gas hydrate saturations determined from pressure core and chlorinity measurements. Also, in intervals with near-vertical gas hydrate-filled fractures, there is considerable separation between phase shift and attenuation resistivity logs, with [Formula: see text] resistivity measurements being significantly higher than [Formula: see text] resistivity measurements. We modeled the sensitivity of the propagation resistivity measurements in the gas hydrate-filled fracture intervals at NGHP-01 Sites 5 and 10. Near-vertical hydrate-filled fractures can cause the abnormally high resistivity measurements in vertical holes due to electrical anisotropy. The model suggests the gas hydrate saturations in situ are usually significantly lower than those calculated from Archie’s equation. In addition, these modeled gas hydrate saturations generally agree with the lower gas hydrate saturations obtained from pressure core and chlorinity measurements at NGHP-01 Sites 5 and 10.


2021 ◽  
Author(s):  
Sabyasachi Dash ◽  
◽  
Zoya Heidari ◽  

Conventional resistivity models often overestimate water saturation in organic-rich mudrocks and require extensive calibration efforts. Conventional resistivity-porosity-saturation models assume brine in the formation as the only conductive component contributing to resistivity measurements. Enhanced resistivity models for shaly-sand analysis include clay concentration and clay-bound water as contributors to electrical conductivity. These shaly-sand models, however, consider the existing clay in the rock as dispersed, laminated, or structural, which does not reliably describe the distribution of clay network in organic-rich mudrocks. They also do not incorporate other conductive minerals and organic matter, which can significantly impact the resistivity measurements and lead to uncertainty in water saturation assessment. We recently introduced a method that quantitatively assimilates the type and spatial distribution of all conductive components to improve reserves evaluation in organic-rich mudrocks using electrical resistivity measurements. This paper aims to verify the reliability of the introduced method for the assessment of water/hydrocarbon saturation in the Wolfcamp formation of the Permian Basin. Our recently introduced resistivity model uses pore combination modeling to incorporate conductive (clay, pyrite, kerogen, brine) and non-conductive (grains, hydrocarbon) components in estimating effective resistivity. The inputs to the model are volumetric concentrations of minerals, the conductivity of rock components, and porosity obtained from laboratory measurements or interpretation of well logs. Geometric model parameters are also critical inputs to the model. To simultaneously estimate the geometric model parameters and water saturation, we develop two inversion algorithms (a) to estimate the geometric model parameters as inputs to the new resistivity model and (b) to estimate the water saturation. Rock type, pore structure, and spatial distribution of rock components affect geometric model parameters. Therefore, dividing the formation into reliable petrophysical zones is an essential step in this method. The geometric model parameters are determined for each rock type by minimizing the difference between the measured resistivity and the resistivity, estimated from Pore Combination Modeling. We applied the new rock physics model to two wells drilled in the Permian Basin. The depth interval of interest was located in the Wolfcamp formation. The rock-class-based inversion showed variation in geometric model parameters, which improved the assessment of water saturation. Results demonstrated that the new method improved water saturation estimates by 32.1% and 36.2% compared to Waxman-Smits and Archie's models, respectively, in the Wolfcamp formation. The most considerable improvement was observed in the Middle and Lower Wolfcamp formation, where the average clay concentration was relatively higher than the other zones. Results demonstrated that the proposed method was shown to improve the estimates of hydrocarbon reserves in the Permian Basin by 33%. The hydrocarbon reserves were underestimated by an average of 70000 bbl/acre when water saturation was quantified using Archie's model in the Permian Basin. It should be highlighted that the new method did not require any calibration effort to obtain model parameters for estimating water saturation. This method minimizes the need for extensive calibration efforts for the assessment of hydrocarbon/water saturation in organic-rich mudrocks. By minimizing the need for extensive calibration work, we can reduce the number of core samples acquired. This is the unique contribution of this rock-physics-based workflow.


2021 ◽  
Author(s):  
Ping Zhang ◽  
◽  
Wael Abdallah ◽  
Gong Li Wang ◽  
Shouxiang Mark Ma ◽  
...  

It is desirable to evaluate the possibility of developing a deeper dielectric permittivity based Sw measurement for various petrophysical applications. The low frequency, (< MHz), resistivity-based method for water saturation (Sw) evaluation is the desired method in the industry due to its deepest depth of investigation (DOI, up to 8 ft). However, the method suffers from higher uncertainty when formation water is very fresh or has mixed salinity. Dielectric permittivity and conductivity dispersion have been used to estimate Sw and salinity. The current dielectric dispersion tools, however, have very shallow DOI due to their high measurement frequency up to GHz, which most likely confines the measurements within the near wellbore mud-filtrate invaded zones. In this study, effective medium-model simulations were conducted to study different electromagnetic (EM) induced-polarization effects and their relationships to rock petrophysical properties. Special attention is placed on the complex conductivity at 2 MHz due to its availability in current logging tools. It is known that the complex dielectric saturation interpretation at the MHz range is quite difficult due to lack of fully understood of physics principles on complex dielectric responses, especially when only single frequency signal is used. Therefore, our study is focused on selected key parameters: water-filled porosity, salinity, and grain shape, and their effects on the modeled formation conductivity and permittivity. To simulate field logs, some of the petrophysical parameters mentioned above are generated randomly within expected ranges. Formation conductivity and permittivity are then calculated using our petrophysical model. The calculated results are then mixed with random noises of 10% to make them more realistic like downhole logs. The synthetic conductivity and permittivity logs are used as inputs in a neural network application to explore possible correlations with water-filled porosity. It is found that while the conductivity and permittivity logs are generated from randomly selected petrophysical parameters, they are highly correlated with water-filled porosity. Furthermore, if new conductivity and permittivity logs are generated with different petrophysical parameters, the correlations defined before can be used to predict water-filled porosity in the new datasets. We also found that for freshwater environments, the conductivity has much lower correlation with water-filled porosity than the one derived from the permittivity. However, the correlations are always improved when both conductivity and permittivity were used. This exercise serves as proof of concept, which opens an opportunity for field data applications. Field logs confirm the findings in the model simulations. Two propagation resistivity logs measured at 2 MHz are processed to calculate formation conductivity and permittivity. Using independently estimated water-filled porosity, a model was trained using a neural network for one of the logs. Excellent correlation between formation conductivity and permittivity and water-filled porosity is observed for the trained model. This neural network- generated model can be used to predict water content from other logs collected from different wells with a coefficient of correlation up to 96%. Best practices are provided on the performance of using conductivity and permittivity to predict water-filled porosity. These include how to effectively train the neural network correlation models, general applications of the trained model for logs from different fields. With the established methodology, deep dielectric-based water saturation in freshwater and mixed salinity environments is obtained for enhanced formation evaluation, well placement, and reservoir saturation monitoring.


1967 ◽  
Vol 6 (48) ◽  
pp. 911-915 ◽  
Author(s):  
M. P. Hochstein ◽  
G. F. Risk

The activation energy ϵe1 of polar firn samples determined by D.C. resistivity measurements is a function of temperature and density. In the temperature range −2° C. to −10° C. ϵe1 decreases with decreasing temperature reaching a nearly constant value for temperatures colder than −10°C.; in the temperature range −10°C. to −21°C. ϵe1 was found to decrease with increasing density and to lie between 0.7 eV. and 0.4 eV.


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