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Electrical properties of partially saturated sandstones.

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Electrical properties of partially saturated sandstones. / Brovelli, A.; Cassiani, G.; Dalla, E. et al.
In: Water Resources Research, Vol. 41, No. 8, 17.08.2005, p. W08411.

Research output: Contribution to Journal/MagazineJournal articlepeer-review

Harvard

Brovelli, A, Cassiani, G, Dalla, E, Bergamini, F, Pitea, D & Binley, AM 2005, 'Electrical properties of partially saturated sandstones.', Water Resources Research, vol. 41, no. 8, pp. W08411. <http://www.agu.org/pubs/crossref/2005/2004WR003628.shtml>

APA

Brovelli, A., Cassiani, G., Dalla, E., Bergamini, F., Pitea, D., & Binley, A. M. (2005). Electrical properties of partially saturated sandstones. Water Resources Research, 41(8), W08411. http://www.agu.org/pubs/crossref/2005/2004WR003628.shtml

Vancouver

Brovelli A, Cassiani G, Dalla E, Bergamini F, Pitea D, Binley AM. Electrical properties of partially saturated sandstones. Water Resources Research. 2005 Aug 17;41(8):W08411.

Author

Brovelli, A. ; Cassiani, G. ; Dalla, E. et al. / Electrical properties of partially saturated sandstones. In: Water Resources Research. 2005 ; Vol. 41, No. 8. pp. W08411.

Bibtex

@article{2523580b32b744aa85a6f7699e844dac,
title = "Electrical properties of partially saturated sandstones.",
abstract = "Electric and electromagnetic geophysical tools are suitable methods for investigating moisture content, transport, and storage properties of the subsoil with noninvasive surveys. Interpretation of field data is still based on empirical or semiempirical equations, which must be calibrated with complex, time-consuming laboratory measurements. In this paper we develop pore-scale models suitable for computing the effective electric conductivity and the effective permittivity of partially saturated porous media on the basis of simple structural parameters (grain size distribution and porosity). We compute the electrical conductivity with three approaches that model the conductivity of the shell of coating clay around solid grains of shaly sandstones using different assumptions. We compare the simulated results with experimental data from Sherwood Sandstone (UK) and discuss the effect of these assumptions on the effective conductivity. Simulations performed using a modeling approach that accounts for interaction between volume and surface conduction show an excellent agreement with experimental data. We also model the effective permittivity of the same porous medium at several saturation values and obtain a good match with laboratory measurements.",
author = "A. Brovelli and G. Cassiani and E. Dalla and F. Bergamini and D. Pitea and Binley, {Andrew M.}",
year = "2005",
month = aug,
day = "17",
language = "English",
volume = "41",
pages = "W08411",
journal = "Water Resources Research",
issn = "0043-1397",
publisher = "AMER GEOPHYSICAL UNION",
number = "8",

}

RIS

TY - JOUR

T1 - Electrical properties of partially saturated sandstones.

AU - Brovelli, A.

AU - Cassiani, G.

AU - Dalla, E.

AU - Bergamini, F.

AU - Pitea, D.

AU - Binley, Andrew M.

PY - 2005/8/17

Y1 - 2005/8/17

N2 - Electric and electromagnetic geophysical tools are suitable methods for investigating moisture content, transport, and storage properties of the subsoil with noninvasive surveys. Interpretation of field data is still based on empirical or semiempirical equations, which must be calibrated with complex, time-consuming laboratory measurements. In this paper we develop pore-scale models suitable for computing the effective electric conductivity and the effective permittivity of partially saturated porous media on the basis of simple structural parameters (grain size distribution and porosity). We compute the electrical conductivity with three approaches that model the conductivity of the shell of coating clay around solid grains of shaly sandstones using different assumptions. We compare the simulated results with experimental data from Sherwood Sandstone (UK) and discuss the effect of these assumptions on the effective conductivity. Simulations performed using a modeling approach that accounts for interaction between volume and surface conduction show an excellent agreement with experimental data. We also model the effective permittivity of the same porous medium at several saturation values and obtain a good match with laboratory measurements.

AB - Electric and electromagnetic geophysical tools are suitable methods for investigating moisture content, transport, and storage properties of the subsoil with noninvasive surveys. Interpretation of field data is still based on empirical or semiempirical equations, which must be calibrated with complex, time-consuming laboratory measurements. In this paper we develop pore-scale models suitable for computing the effective electric conductivity and the effective permittivity of partially saturated porous media on the basis of simple structural parameters (grain size distribution and porosity). We compute the electrical conductivity with three approaches that model the conductivity of the shell of coating clay around solid grains of shaly sandstones using different assumptions. We compare the simulated results with experimental data from Sherwood Sandstone (UK) and discuss the effect of these assumptions on the effective conductivity. Simulations performed using a modeling approach that accounts for interaction between volume and surface conduction show an excellent agreement with experimental data. We also model the effective permittivity of the same porous medium at several saturation values and obtain a good match with laboratory measurements.

M3 - Journal article

VL - 41

SP - W08411

JO - Water Resources Research

JF - Water Resources Research

SN - 0043-1397

IS - 8

ER -