scholarly journals Electrical anisotropy due to gas hydrate-filled fractures

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.

Geophysics ◽  
2019 ◽  
Vol 84 (4) ◽  
pp. B247-B258 ◽  
Author(s):  
Bo Yang ◽  
Xiangyun Hu ◽  
Wule Lin ◽  
Shuang Liu ◽  
Hui Fang

In China, gas hydrates in onshore permafrost areas have so far only been found in the Juhugeng Mine of the Qilian Mountains. However, their subsurface distribution remains unclear. Electrical resistivity logs have revealed that zones containing gas hydrates have higher resistivity than surrounding zones, which makes electromagnetic methods viable for detecting gas-hydrate deposits. We have deployed a natural-source audio-magnetotelluric (AMT) survey at the Juhugeng Mine. AMT data were collected at 176 sites along five profiles, and resistivity models were derived from 2D inversions after detailed data analysis. After the available geologic and geophysical observations were combined, the inversion results from profile 1 suggested that permafrost near the surface with high resistivity and thickness is essential for underlying gas hydrates to be present. The decrease in resistivity and/or thickness of permafrost due to climate change may lead to gas-hydrate dissociation. The other four AMT transects suggested three prospective gas-hydrate sites. Our results indicate that the AMT survey technique is suitable for exploring gas hydrates in permafrost areas and analyzing the impact of permafrost characteristics on gas-hydrate occurrence.


2013 ◽  
Vol 3 (4) ◽  
pp. 483-487
Author(s):  
S. Soto-Caban ◽  
E. Law

This study uses electrical resistivity measurements of soils and weathered rock to perform a fast and reliable evaluation of field anisotropy. Two test sites at New Concord, Ohio were used for the study. These sites are characterized by different landform and slightly east dipping limestone and siltstone formations of Pennsylvanian age. The measured resistivity ranged from 19 Ω∙m to 100 Ω∙m, and varied with depth, landform, and season. The anisotropy was determined by a comparison of resistance values along the directions of strike and the dip. Measurements showed that the orientation of electrical anisotropy in the shallow ground may vary due to fluid connection, which is determined by the pore geometry in soil and rock, as well as by the direction of fluid movement. Results from this study indicated that a portable electrical resistivity meter is sensitive and reliable enough to be used for shallow ground fluid monitoring.


2020 ◽  
Author(s):  
S Constable ◽  
R Lu ◽  
P Kannberg ◽  
L A Stern ◽  
W L Du Frane ◽  
...  

2020 ◽  
Vol 8 (3) ◽  
pp. SL151-SL158
Author(s):  
Hu Li ◽  
Jun Zhu ◽  
Yanchun Xiong ◽  
Gang Liu ◽  
Yuanshi Tian ◽  
...  

The depth of detection (DOD), which is an important concept in logging data interpretation, describes the detection capability of the borehole measurements. We have extended the definition of DOD for azimuthal information, namely, the geosignal delivered by azimuthal resistivity tools, to resistivity logs in logging-while-drilling (LWD) applications. Instead of using the radial geometric factor, the detection thresholds in predicting a geologic boundary are used to describe the DOD of a measurement. This definition unifies the criteria to evaluate the detectability of different borehole measurements, such as LWD resistivity measurements and geosignals. It also can be generalized to other kinds of well logging methods in LWD applications. Using the proposed definition, we analyze the detection capability of the LWD resistivity measurements in looking-around and looking-ahead applications; they provide more tangible descriptions. In vertical or near-vertical wells, the definition provides an indicator to evaluate the capability and reliability of looking ahead of deep/ultradeep LWD resistivity tools. The investigations on the influence of the DOD on the distance-to-boundary inversion, which can help in developing a robust and accurate inversion scheme, also are presented and discussed.


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.


Author(s):  
W. E. King

A side-entry type, helium-temperature specimen stage that has the capability of in-situ electrical-resistivity measurements has been designed and developed for use in the AEI-EM7 1200-kV electron microscope at Argonne National Laboratory. The electrical-resistivity measurements complement the high-voltage electron microscope (HVEM) to yield a unique opportunity to investigate defect production in metals by electron irradiation over a wide range of defect concentrations.A flow cryostat that uses helium gas as a coolant is employed to attain and maintain any specified temperature between 10 and 300 K. The helium gas coolant eliminates the vibrations that arise from boiling liquid helium and the temperature instabilities due to alternating heat-transfer mechanisms in the two-phase temperature regime (4.215 K). Figure 1 shows a schematic view of the liquid/gaseous helium transfer system. A liquid-gas mixture can be used for fast cooldown. The cold tip of the transfer tube is inserted coincident with the tilt axis of the specimen stage, and the end of the coolant flow tube is positioned without contact within the heat exchanger of the copper specimen block (Fig. 2).


1991 ◽  
Vol 138 (10) ◽  
pp. 3081-3085 ◽  
Author(s):  
W. R. Thurber ◽  
J. R. Lowney ◽  
R. D. Larrabee ◽  
J. R. Ehrstein

2014 ◽  
Vol 447 (1-3) ◽  
pp. 225-232 ◽  
Author(s):  
B. Gómez-Ferrer ◽  
R. Vila ◽  
D. Jiménez-Rey ◽  
C.J. Ortiz ◽  
F. Mota ◽  
...  

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