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Flow pathways in porous media : electrical resistance tomography and dye staining image verification.

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Flow pathways in porous media : electrical resistance tomography and dye staining image verification. / Binley, Andrew M.; Shaw, Ben; Henry-Poulter, Siobhan.
In: Measurement Science and Technology, Vol. 7, No. 3, 03.1996, p. 384-390.

Research output: Contribution to Journal/Magazine › Journal article › peer-review

Harvard

Binley, AM, Shaw, B & Henry-Poulter, S 1996, 'Flow pathways in porous media : electrical resistance tomography and dye staining image verification.', Measurement Science and Technology, vol. 7, no. 3, pp. 384-390. https://doi.org/10.1088/0957-0233/7/3/020

APA

Binley, A. M., Shaw, B., & Henry-Poulter, S. (1996). Flow pathways in porous media : electrical resistance tomography and dye staining image verification. Measurement Science and Technology, 7(3), 384-390. https://doi.org/10.1088/0957-0233/7/3/020

Vancouver

Binley AM, Shaw B, Henry-Poulter S. Flow pathways in porous media : electrical resistance tomography and dye staining image verification. Measurement Science and Technology. 1996 Mar;7(3):384-390. doi: 10.1088/0957-0233/7/3/020

Author

Binley, Andrew M. ; Shaw, Ben ; Henry-Poulter, Siobhan. / Flow pathways in porous media : electrical resistance tomography and dye staining image verification. In: Measurement Science and Technology. 1996 ; Vol. 7, No. 3. pp. 384-390.

Bibtex

@article{3d707c6be00a42a897f91e65930bbc63,
title = "Flow pathways in porous media : electrical resistance tomography and dye staining image verification.",
abstract = "Electrical resistance tomography permits the determination of the spatial distribution of electrical resistivity by non-destructive means. The technique may be applied to the study of flow through porous media by following the changes in resistivity distribution within a soil or rock core as an electrolytic tracer is passed through the specimen. Image reconstruction of the electrical resistance tomography data may be achieved by robust regularized nonlinear inverse methods provided data errors are suitably characterized. The procedure is reported here for a natural (undisturbed) soil core using four planes of 16 electrodes placed around the boundary of the core. The experiment was performed with a dye tracer that provided, by destructive slicing, visual verification of the flow pathways observed with the tomographic imaging.",
author = "Binley, {Andrew M.} and Ben Shaw and Siobhan Henry-Poulter",
year = "1996",
month = mar,
doi = "10.1088/0957-0233/7/3/020",
language = "English",
volume = "7",
pages = "384--390",
journal = "Measurement Science and Technology",
issn = "0957-0233",
publisher = "IOP Publishing Ltd.",
number = "3",

}

RIS

TY - JOUR

T1 - Flow pathways in porous media : electrical resistance tomography and dye staining image verification.

AU - Binley, Andrew M.

AU - Shaw, Ben

AU - Henry-Poulter, Siobhan

PY - 1996/3

Y1 - 1996/3

N2 - Electrical resistance tomography permits the determination of the spatial distribution of electrical resistivity by non-destructive means. The technique may be applied to the study of flow through porous media by following the changes in resistivity distribution within a soil or rock core as an electrolytic tracer is passed through the specimen. Image reconstruction of the electrical resistance tomography data may be achieved by robust regularized nonlinear inverse methods provided data errors are suitably characterized. The procedure is reported here for a natural (undisturbed) soil core using four planes of 16 electrodes placed around the boundary of the core. The experiment was performed with a dye tracer that provided, by destructive slicing, visual verification of the flow pathways observed with the tomographic imaging.

AB - Electrical resistance tomography permits the determination of the spatial distribution of electrical resistivity by non-destructive means. The technique may be applied to the study of flow through porous media by following the changes in resistivity distribution within a soil or rock core as an electrolytic tracer is passed through the specimen. Image reconstruction of the electrical resistance tomography data may be achieved by robust regularized nonlinear inverse methods provided data errors are suitably characterized. The procedure is reported here for a natural (undisturbed) soil core using four planes of 16 electrodes placed around the boundary of the core. The experiment was performed with a dye tracer that provided, by destructive slicing, visual verification of the flow pathways observed with the tomographic imaging.

U2 - 10.1088/0957-0233/7/3/020

DO - 10.1088/0957-0233/7/3/020

M3 - Journal article

VL - 7

SP - 384

EP - 390

JO - Measurement Science and Technology

JF - Measurement Science and Technology

SN - 0957-0233

IS - 3

ER -