Surface diffusivity of cleaved NaCl crystals as a function of humidity : Impedance spectroscopy measurements and implications for crack healing in rock salt. / Koelemeijer, Paula J.; Peach, Colin J.; Spiers, Christopher J.

In: Journal of Geophysical Research: Solid Earth, Vol. 117, No. B1, B01205, 21.01.2012, p. 1-15.

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Surface diffusivity of cleaved NaCl crystals as a function of humidity : Impedance spectroscopy measurements and implications for crack healing in rock salt. / Koelemeijer, Paula J.; Peach, Colin J.; Spiers, Christopher J.

In: Journal of Geophysical Research: Solid Earth, Vol. 117, No. B1, B01205, 21.01.2012, p. 1-15.

Research output: Contribution to journalArticlepeer-review

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Koelemeijer, Paula J. ; Peach, Colin J. ; Spiers, Christopher J. / Surface diffusivity of cleaved NaCl crystals as a function of humidity : Impedance spectroscopy measurements and implications for crack healing in rock salt. In: Journal of Geophysical Research: Solid Earth. 2012 ; Vol. 117, No. B1. pp. 1-15.

BibTeX

@article{810a82cb0bee43c98537f9b54fbdacb3,
title = "Surface diffusivity of cleaved NaCl crystals as a function of humidity: Impedance spectroscopy measurements and implications for crack healing in rock salt",
abstract = "Rock salt offers an attractive host rock for geological storage applications, because of its naturally low permeability and the ability of excavation-induced cracks to heal by fluid-assisted diffusive mass transfer. However, while diffusive transport rates in bulk NaCl solution are rapid and well characterized, such data are not directly applicable to storage conditions where crack walls are coated with thin adsorbed water films. To reliably predict healing times in geological storage applications, data on mass transport rates in adsorbed films are needed. We determined the surface diffusivity in such films for conditions with absolute humidities (AH) ranging from 1 to 18 g/m 3 (relative humidities (RH) of 4%-78%) by measuring the surface impedance of single NaCl crystals. We use the impedance results to calculate the effective surface diffusivity S = DδC using the Nernst-Einstein equation. The S values obtained lie in the range 1 × 10-27 m3 s-1 at very dry conditions to 1 × 10-19 m 3 s-1 for the deliquescence point at 296 K, which is in reasonable agreement with existing values for grain boundary diffusion under wet conditions. Estimates for the diffusivity D made assuming a film thickness δ of 50-90 nm and no major effects of thickness on the solubility C lie in the range of 1 × 10-14 to 8 × 10-12 m 2 s-1 for the highest humidities studied (14-18 g/m 3 AH, 60%-78% RH). For geological storage systems in rock salt, we predict S values between 1 × 10-22 - 8 × 10-18 m3 s-1. These imply crack healing rates 6 to 7 orders of magnitude lower than expected for brine-filled cracks.",
author = "Koelemeijer, {Paula J.} and Peach, {Colin J.} and Spiers, {Christopher J.}",
year = "2012",
month = jan,
day = "21",
doi = "10.1029/2011JB008627",
language = "English",
volume = "117",
pages = "1--15",
journal = "Journal of Geophysical Research: Solid Earth",
issn = "2169-9313",
publisher = "Wiley-Blackwell",
number = "B1",

}

RIS

TY - JOUR

T1 - Surface diffusivity of cleaved NaCl crystals as a function of humidity

T2 - Impedance spectroscopy measurements and implications for crack healing in rock salt

AU - Koelemeijer, Paula J.

AU - Peach, Colin J.

AU - Spiers, Christopher J.

PY - 2012/1/21

Y1 - 2012/1/21

N2 - Rock salt offers an attractive host rock for geological storage applications, because of its naturally low permeability and the ability of excavation-induced cracks to heal by fluid-assisted diffusive mass transfer. However, while diffusive transport rates in bulk NaCl solution are rapid and well characterized, such data are not directly applicable to storage conditions where crack walls are coated with thin adsorbed water films. To reliably predict healing times in geological storage applications, data on mass transport rates in adsorbed films are needed. We determined the surface diffusivity in such films for conditions with absolute humidities (AH) ranging from 1 to 18 g/m 3 (relative humidities (RH) of 4%-78%) by measuring the surface impedance of single NaCl crystals. We use the impedance results to calculate the effective surface diffusivity S = DδC using the Nernst-Einstein equation. The S values obtained lie in the range 1 × 10-27 m3 s-1 at very dry conditions to 1 × 10-19 m 3 s-1 for the deliquescence point at 296 K, which is in reasonable agreement with existing values for grain boundary diffusion under wet conditions. Estimates for the diffusivity D made assuming a film thickness δ of 50-90 nm and no major effects of thickness on the solubility C lie in the range of 1 × 10-14 to 8 × 10-12 m 2 s-1 for the highest humidities studied (14-18 g/m 3 AH, 60%-78% RH). For geological storage systems in rock salt, we predict S values between 1 × 10-22 - 8 × 10-18 m3 s-1. These imply crack healing rates 6 to 7 orders of magnitude lower than expected for brine-filled cracks.

AB - Rock salt offers an attractive host rock for geological storage applications, because of its naturally low permeability and the ability of excavation-induced cracks to heal by fluid-assisted diffusive mass transfer. However, while diffusive transport rates in bulk NaCl solution are rapid and well characterized, such data are not directly applicable to storage conditions where crack walls are coated with thin adsorbed water films. To reliably predict healing times in geological storage applications, data on mass transport rates in adsorbed films are needed. We determined the surface diffusivity in such films for conditions with absolute humidities (AH) ranging from 1 to 18 g/m 3 (relative humidities (RH) of 4%-78%) by measuring the surface impedance of single NaCl crystals. We use the impedance results to calculate the effective surface diffusivity S = DδC using the Nernst-Einstein equation. The S values obtained lie in the range 1 × 10-27 m3 s-1 at very dry conditions to 1 × 10-19 m 3 s-1 for the deliquescence point at 296 K, which is in reasonable agreement with existing values for grain boundary diffusion under wet conditions. Estimates for the diffusivity D made assuming a film thickness δ of 50-90 nm and no major effects of thickness on the solubility C lie in the range of 1 × 10-14 to 8 × 10-12 m 2 s-1 for the highest humidities studied (14-18 g/m 3 AH, 60%-78% RH). For geological storage systems in rock salt, we predict S values between 1 × 10-22 - 8 × 10-18 m3 s-1. These imply crack healing rates 6 to 7 orders of magnitude lower than expected for brine-filled cracks.

UR - http://www.scopus.com/inward/record.url?scp=84856250578&partnerID=8YFLogxK

U2 - 10.1029/2011JB008627

DO - 10.1029/2011JB008627

M3 - Article

AN - SCOPUS:84856250578

VL - 117

SP - 1

EP - 15

JO - Journal of Geophysical Research: Solid Earth

JF - Journal of Geophysical Research: Solid Earth

SN - 2169-9313

IS - B1

M1 - B01205

ER -