An electromagnetic modelling tool for the detection of hydrocarbons in thesubsoil

Citation
Jm. Carcione et G. Seriani, An electromagnetic modelling tool for the detection of hydrocarbons in thesubsoil, GEOPHYS PR, 48(2), 2000, pp. 231-256
Citations number
25
Categorie Soggetti
Earth Sciences
Journal title
GEOPHYSICAL PROSPECTING
ISSN journal
00168025 → ACNP
Volume
48
Issue
2
Year of publication
2000
Pages
231 - 256
Database
ISI
SICI code
0016-8025(200003)48:2<231:AEMTFT>2.0.ZU;2-#
Abstract
Electromagnetic geophysical methods, such as ground-penetrating radar (GPR) , have proved to be optimal tools for detecting and mapping near-surface co ntaminants. GPR has the capability of mapping the location of hydrocarbon p ools on the basis of contrasts in the effective permittivity and conductivi ty of the subsoil. At radar frequencies (50 MHz to 1 GHz), hydrocarbons hav e a relative permittivity ranging from 2 to 30, compared with a permittivit y for water of 80. Moreover, their conductivity ranges from zero to 10 mS/m , against values of 200 mS/m and more for salt water. These differences ind icate that water/hydrocarbon interfaces in a porous medium are electromagne tically 'visible'. In order to quantify the hydrocarbon saturation we devel oped a model for the electromagnetic properties of a subsoil composed of sa nd and clay/silt, and partially saturated with air, water and hydrocarbon. A self-similar theory is used for the sandy component and a transversely is otropic constitutive equation for the shaly component, which is assumed to possess a laminated structure. The model is first verified with experimenta l data and then used to obtain the properties of soils partially saturated with methanol and aviation gasoline. Finally, a GPR forward-modelling metho d computes the radargrams of a typical hydrocarbon spill, illustrating the sensitivity of the technique to the type of pore-fluid. The model and the s imulation algorithm provide an interpretation methodology to distinguish di fferent pore-fluids and to quantify their degree of saturation.