SPE Annual Technical Conference and Exhibition 2011
DOI: 10.2118/147245-ms
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A Novel Approach Based on Dielectric Dispersion Measurements to Evaluate the Quality of Complex Shaly-sand Reservoirs

Abstract: This paper presents a novel approach for the formation evaluation of shaly-sand thin layered reservoirs using dielectric dispersion wireline logging provided by a new generation tool. The study is focused on gas fields in the Mediterranean basin characterized by the presence of very thin inter-laminations (centimeter-scale or even less). In these complex reservoirs, the conventional petrophysical analysis is very challenging due to standard logging tools' vertical resolution limits which prevent the quantitati… Show more

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Cited by 17 publications
(8 citation statements)
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“…The EPT (Electromagnetic Propagation Tool) working at 1.1GHz was reported to provide hydrate saturation in reservoirs in Alaska, and the inversion results had good consistency with other logging methods such as ultrasonic and electrical resistivity tools [13][14][15]. Compared to the electrical resistivity methods, the dielectric method has many advantages such as less prone to water salinity and better vertical resolution, which are desirable for hydrate reservoir evaluation of the sea floor sediments such as salt water invasion and quantitative evaluation of hydrate saturation in thin layers [16,17]. Physical characteristics of unconsolidated porous media containing hydrate crystals are important to natural gas hydrate detection and exploitation from the sea bottom and tundra.…”
Section: Introductionmentioning
confidence: 73%
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“…The EPT (Electromagnetic Propagation Tool) working at 1.1GHz was reported to provide hydrate saturation in reservoirs in Alaska, and the inversion results had good consistency with other logging methods such as ultrasonic and electrical resistivity tools [13][14][15]. Compared to the electrical resistivity methods, the dielectric method has many advantages such as less prone to water salinity and better vertical resolution, which are desirable for hydrate reservoir evaluation of the sea floor sediments such as salt water invasion and quantitative evaluation of hydrate saturation in thin layers [16,17]. Physical characteristics of unconsolidated porous media containing hydrate crystals are important to natural gas hydrate detection and exploitation from the sea bottom and tundra.…”
Section: Introductionmentioning
confidence: 73%
“…Then the three systematic errors were mathematically removed from subsequent permittivity measurements. Гa is derived from the following equation, and it equals the complex reflection coefficient Г * in (15) [ (16) In this study, the compensation was carried out by using 25℃ deionized water, a short circuit kit with gold plated rubber, and air. The permittivity of pure water at standard atmospheric pressure and the temperature of 25℃ was adopted as the referenced permittivity of the 25℃ deionized water [72], and the reflection coefficients with air and deionized water were derived with (15).…”
Section: Inversion Of the Complex Permittivitymentioning
confidence: 99%
“…Numerous dielectric forward models have been developed and used in our work to convert the dielectric measurements into water saturation, water salinity and rock matrix.The models are so-called bimodal, Stroud-Milton-De (SMD), shaly sand, and complex refractive index model (CRIM) (Stroud et al 2006;Feng and Sen. 1985;Seleznev et al 2006;Pirrone et al 2011). Each type of model has inherent strengths and weaknesses based on the assumptions intrinsic to the model.…”
Section: Dielectric Loggingmentioning
confidence: 99%
“…The Schlumberger Array Dielectric Logging Tool (ADT) [4], also known as the Dielectric Scanner, and the Baker Hughes, GE (BHGE) company's Array Dielectric eXplorer Formation Evaluation Service [2] both use multifrequency multi-spacing measurements for formation detection, and the depth of investigation (DOI) can go up to 10 cm, with a resolution of 1 inch (0.0254 cm). They can be used to investigate the properties of formation rock fluids, as well as the dielectric dispersion effect of rock skeletons, and to discern between different geological structures [12][13][14]18].…”
Section: Introductionmentioning
confidence: 99%