scholarly journals A Joint Inversion Approach of Capacitive and Resistive Measurements for the Estimation of Water Saturation Profiles in Concrete Structures

2020 ◽  
Author(s):  
M. Alhajj ◽  
G. Villain ◽  
S. Bourguignon ◽  
S. Lopes

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


2016 ◽  
Vol 19 (04) ◽  
pp. 713-730
Author(s):  
Sushil Shetty ◽  
Lin Liang ◽  
Tarek M Habashy ◽  
Vanessa Simoes ◽  
Austin J Boyd ◽  
...  


Proceedings ◽  
2018 ◽  
Vol 2 (8) ◽  
pp. 524
Author(s):  
Abdallah Accary ◽  
Laurent Daudeville ◽  
Yann Malecot

The objective of this study is to measure the interstitial pore pressure into saturated concrete under hundreds of megapascals of confinement. This study is carried out within a more general context aiming to understand the behavior of concrete structures under impact. It is well known that the water saturation in massive concrete structures evolves from quasi-dry state at the surface to reach a quasi-saturated state at the core. Since the response of these structures under impact is highly linked to the state of saturation into the material, it is suspected that the pore pressure plays a major effect. This paper presents a new testing technique developed to measure the concrete pore pressure at high confining pressure. This latter is generated by means of a high capacity GIGA press. The new concept consists in implementing a pressure sensor into a water collecting cap. This cap is designed specially to collect water from concrete subjected to mechanical confinement pressure. Experimental results show that concrete pore pressure can reach values of the order of the confining pressure.



Geophysics ◽  
2011 ◽  
Vol 76 (6) ◽  
pp. F395-F406 ◽  
Author(s):  
Adam Smiarowski ◽  
James Macnae ◽  
Glen Bann

Our research introduced a method to monitor saturation in the near surface. In agricultural settings, methods measuring electrical conductivity can provide useful information about soil type, moisture content, and salinity extent. Electrical conductivity meters have been used in a number of studies to determine soil properties in a qualitative sense. We examined the range of structures in which the use of low-induction number instruments can be used successfully to determine layered-earth electrical conductivity. We used an inversion routine which employs a Bayesian modification to the ridge-regression technique with a priori conductivity assumptions typical of agricultural areas. We performed joint inversion of horizontal and vertical dipole configurations at two coil separations for layer over half-space models with electrical properties of silt, loam, clay, and saline waters. Generally, the inversion code resolved layer thickness to better than 25% and electrical conductivity to better than 20% if the layer is less than 3-m thick. We then inverted field measurements acquired in salt-scalded areas in the Yass River Valley, New South Wales, Australia, to determine a layer over a half-space. With Kennedy’s formulation concerning the relationship between porosity, water saturation and electrical conductivity, we used the field results to predict autumn water saturation for the top layer to be 13% and the bottom layer to be 15%. In the spring, we used the field results to predict saturation of 50% for the top layer and 51% for the bottom layer, leading to a seasonal variation in soil saturation of approximately 36%. Predicted saturation was spatially consistent across the traverse line, suggesting that the developed methodology was successful.



Geophysics ◽  
2006 ◽  
Vol 71 (3) ◽  
pp. C1-C13 ◽  
Author(s):  
G. Michael Hoversten ◽  
Florence Cassassuce ◽  
Erika Gasperikova ◽  
Gregory A. Newman ◽  
Jinsong Chen ◽  
...  

Accurately estimating reservoir parameters from geophysical data is vitally important in hydrocarbon exploration and production. We have developed a new joint-inversion algorithm to estimate reservoir parameters directly, using both seismic amplitude variation with angle of incidence (AVA) data and marine controlled-source electromagnetic (CSEM) data. Reservoir parameters are linked to geophysical parameters through a rock-properties model. Errors in the parameters of the rock-properties model introduce errors of comparable size in the reservoir-parameter estimates produced by joint inversion. Tests of joint inversion on synthetic 1D models demonstrate improved fluid saturation and porosity estimates for joint AVA-CSEM data inversion (compared with estimates from AVA or CSEM inversion alone). A comparison of inversions of AVA data, CSEM data, and joint AVA-CSEM data over the North Sea Troll field, at a location for which we have well control, shows that the joint inversion produces estimates of gas saturation, oil saturation, and porosity that are closest (as measured by the rms difference, the [Formula: see text] norm of the difference, and net values over the interval) to the logged values. However, CSEM-only inversion provides the closest estimates of water saturation.



Geophysics ◽  
2014 ◽  
Vol 79 (3) ◽  
pp. D145-D159 ◽  
Author(s):  
Olabode Ijasan ◽  
Carlos Torres-Verdín ◽  
William E. Preeg ◽  
John Rasmus ◽  
Edward Stockhausen

A recently introduced interpretation workflow has confirmed that inversion-based interpretation is more reliable than conventional well-log analysis in high-angle (HA) and horizontal (HZ) wells because the former accounts for well trajectory and shoulder-bed effects on well logs. Synthetic examples show that the inversion workflow could improve the estimation of hydrocarbon volumes by 15% and 10% in HA and HZ intervals, respectively. Using field examples of thinly interbedded calcite-cemented siltstone formations, we document results of the joint petrophysical inversion of logging-while-drilling multisector nuclear (neutron porosity, density, natural gamma ray, photoelectric factor) and multiarray propagation resistivity measurement for improved formation evaluation in HA/HZ wells. Under the assumption of multilayer formation petrophysical models, the inversion approach estimates formation properties by numerically reproducing the available measurements. Subsequently, inversion-derived hydrocarbon pore volume is calculated for assessment of reservoir pay. Application of the joint inversion-based interpretation in challenging field examples highlights petrophysical characteristics such as capillary trends or water saturation variations in a hydrocarbon column influenced by reservoir quality and formation electrical anisotropy which otherwise remain inconspicuous with conventional and quick-look interpretation of well-logs.



Geophysics ◽  
2020 ◽  
Vol 85 (3) ◽  
pp. MR107-MR115
Author(s):  
Tongcheng Han ◽  
Shengbiao Liu ◽  
Denghui Xu ◽  
Li-Yun Fu

Successful joint inversion of seismic and electromagnetic survey data to estimate parameters and improve the characterization of the earth’s subsurface relies on the understanding of the cross-property relations between the elastic and electrical properties. Pressure-dependent cross-property relationships of rocks with varying degrees of fluid saturation remain poorly understood even though such conditions are encountered frequently. We investigate this problem by designing and undertaking dedicated laboratory experiments to simultaneously measure the elastic velocity and electrical resistivity in two Berea sandstone samples subject to varying confining pressure and water saturation, using a state-of-the-art joint elastic-electrical measurement system. P- and S-wave velocities are found to increase exponentially with increasing confining pressure at each water saturation, whereas electrical conductivity can either increase or decrease with confining pressure depending on the degree of water saturation. More interestingly, the elastic and electrical properties of the two samples are shown to be systematically correlated as functions of water saturation and the applied confining pressure. The correlations reveal the natural link between the elastic and electrical properties in the two porous sandstones with partial water saturation, and they help to better indicate the fluid flow within compliant pores in addition to the known flow between stiff and compliant pores. The results will form the theoretical basis for the successful joint interpretation of seismic and electromagnetic survey data acquired from partially saturated porous rocks in the subsurface of the earth.



Geophysics ◽  
2012 ◽  
Vol 77 (1) ◽  
pp. R65-R80 ◽  
Author(s):  
Jinsong Chen ◽  
G. Michael Hoversten

Joint inversion of seismic AVA and CSEM data requires rock-physics relationships to link seismic attributes to electric properties. Ideally, we can connect them through reservoir parameters (e.g., porosity and water saturation) by developing physical-based models, such as Gassmann’s equations and Archie’s law, using nearby borehole logs. This could be difficult in the exploration stage because information available is typically insufficient for choosing suitable rock-physics models and for subsequently obtaining reliable estimates of the associated parameters. The use of improper rock-physics models and the inaccuracy of the estimates of model parameters may cause misleading inversion results. Conversely, it is easy to derive statistical relationships among seismic and electric attributes and reservoir parameters from distant borehole logs. In this study, we developed a Bayesian model to jointly invert seismic AVA and CSEM data for reservoir parameters using statistical rock-physics models; the spatial dependence of geophysical and reservoir parameters were carried out by lithotypes through Markov random fields. We applied the developed model to a synthetic case that simulates a CO2 monitoring application. We derived statistical rock-physics relations from borehole logs at one location and estimated seismic P- and S-wave velocity ratio, acoustic impedance, density, electric resistivity, lithotypes, porosity, and water saturation at three different locations by conditioning to seismic AVA and CSEM data. Comparison of the inversion results with their corresponding true values showed that the correlation-based statistical rock-physics models provide significant information for improving the joint inversion results.



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.



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