Standard

Relation of SIP relaxation time of sands to salinity, grain size and hydraulic conductivity. / Kemna, A.; Münch, H. M.; Titov, K.; Zimmermann, E.; Vereecken, H.

2005. Работа представлена на 11th European Meeting of Environmental and Engineering Geophysics of the Near Surface Geoscience Division of the EAGE, Near Surface 2005, Palermo, Италия.

Результаты исследований: Материалы конференций › материалы › Рецензирование

Harvard

Kemna, A, Münch, HM, Titov, K, Zimmermann, E & Vereecken, H 2005, 'Relation of SIP relaxation time of sands to salinity, grain size and hydraulic conductivity', Работа представлена на 11th European Meeting of Environmental and Engineering Geophysics of the Near Surface Geoscience Division of the EAGE, Near Surface 2005, Palermo, Италия, 4/09/05 - 7/09/05.

APA

Kemna, A., Münch, H. M., Titov, K., Zimmermann, E., & Vereecken, H. (2005). Relation of SIP relaxation time of sands to salinity, grain size and hydraulic conductivity. Работа представлена на 11th European Meeting of Environmental and Engineering Geophysics of the Near Surface Geoscience Division of the EAGE, Near Surface 2005, Palermo, Италия.

Vancouver

Kemna A, Münch HM, Titov K, Zimmermann E, Vereecken H. Relation of SIP relaxation time of sands to salinity, grain size and hydraulic conductivity. 2005. Работа представлена на 11th European Meeting of Environmental and Engineering Geophysics of the Near Surface Geoscience Division of the EAGE, Near Surface 2005, Palermo, Италия.

Author

Kemna, A. ; Münch, H. M. ; Titov, K. ; Zimmermann, E. ; Vereecken, H. / Relation of SIP relaxation time of sands to salinity, grain size and hydraulic conductivity. Работа представлена на 11th European Meeting of Environmental and Engineering Geophysics of the Near Surface Geoscience Division of the EAGE, Near Surface 2005, Palermo, Италия.

BibTeX

@conference{122523a9af57406daeba05b4c00e44af,
title = "Relation of SIP relaxation time of sands to salinity, grain size and hydraulic conductivity",
abstract = "The spectral induced polarisation (SIP) characteristics of sedimentary rocks contain structural information which potentially can be linked to flow and transport parameters, such as hydraulic conductivity. We examined this connection for pure, saturated sands by measuring SIP spectra of sands with different grain size and pore water electrical conductivity. For each spectrum, relaxation times, chargeabilities and Cole-Cole exponents were determined for identified dispersion ranges under the assumption of superimposed Cole-Cole model responses. We here focus on the results concerning the relaxation time of the observed lowfrequency dispersion. This relaxation time shows a decrease with increasing pore water electrical conductivity, which is supposed to be associated with a decrease of the electrical double layer thickness. With increasing grain diameter an increased relaxation time is observed, in accordance with theory. Importantly, we find a correlation between the lowfrequency relaxation time and the hydraulic conductivity, which is of high practical relevance.",
author = "A. Kemna and M{\"u}nch, {H. M.} and K. Titov and E. Zimmermann and H. Vereecken",
note = "Copyright: Copyright 2014 Elsevier B.V., All rights reserved.; 11th European Meeting of Environmental and Engineering Geophysics of the Near Surface Geoscience Division of the EAGE, Near Surface 2005 ; Conference date: 04-09-2005 Through 07-09-2005",
year = "2005",
language = "English",

}

RIS

TY - CONF

T1 - Relation of SIP relaxation time of sands to salinity, grain size and hydraulic conductivity

AU - Kemna, A.

AU - Münch, H. M.

AU - Titov, K.

AU - Zimmermann, E.

AU - Vereecken, H.

N1 - Copyright: Copyright 2014 Elsevier B.V., All rights reserved.

PY - 2005

Y1 - 2005

N2 - The spectral induced polarisation (SIP) characteristics of sedimentary rocks contain structural information which potentially can be linked to flow and transport parameters, such as hydraulic conductivity. We examined this connection for pure, saturated sands by measuring SIP spectra of sands with different grain size and pore water electrical conductivity. For each spectrum, relaxation times, chargeabilities and Cole-Cole exponents were determined for identified dispersion ranges under the assumption of superimposed Cole-Cole model responses. We here focus on the results concerning the relaxation time of the observed lowfrequency dispersion. This relaxation time shows a decrease with increasing pore water electrical conductivity, which is supposed to be associated with a decrease of the electrical double layer thickness. With increasing grain diameter an increased relaxation time is observed, in accordance with theory. Importantly, we find a correlation between the lowfrequency relaxation time and the hydraulic conductivity, which is of high practical relevance.

AB - The spectral induced polarisation (SIP) characteristics of sedimentary rocks contain structural information which potentially can be linked to flow and transport parameters, such as hydraulic conductivity. We examined this connection for pure, saturated sands by measuring SIP spectra of sands with different grain size and pore water electrical conductivity. For each spectrum, relaxation times, chargeabilities and Cole-Cole exponents were determined for identified dispersion ranges under the assumption of superimposed Cole-Cole model responses. We here focus on the results concerning the relaxation time of the observed lowfrequency dispersion. This relaxation time shows a decrease with increasing pore water electrical conductivity, which is supposed to be associated with a decrease of the electrical double layer thickness. With increasing grain diameter an increased relaxation time is observed, in accordance with theory. Importantly, we find a correlation between the lowfrequency relaxation time and the hydraulic conductivity, which is of high practical relevance.

UR - http://www.scopus.com/inward/record.url?scp=84898663684&partnerID=8YFLogxK

M3 - Paper

AN - SCOPUS:84898663684

T2 - 11th European Meeting of Environmental and Engineering Geophysics of the Near Surface Geoscience Division of the EAGE, Near Surface 2005

Y2 - 4 September 2005 through 7 September 2005

ER -

ID: 75062548