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Title: The Effect of Brine on the Electrical Properties of Methane Hydrate

Abstract

Gas hydrates possess lower electrical conductivity (inverse of resistivity) than either seawater or ice, but higher than clastic silts and sands, such that electromagnetic methods can be employed to help identify their natural formation in marine and permafrost environments. Controlled laboratory studies offer a means to isolate and quantify the effects of changing individual components within gas-hydrate-bearing systems, in turn yielding insight into the behavior of natural systems. Here we investigate the electrical properties of polycrystalline methane hydrate with ≥25% gas-filled porosity and in mixture with brine. Initially, pure methane hydrate was synthesized from H2O ice and CH4 gas while undergoing electrical impedance measurement, then partially dissociated to assess the effects of pure pore water accumulation on electrical conductivity. Methane hydrate + brine mixtures were then formed by either adding NaCl (0.25–2.5 wt %) to high-purity ice or by using frozen seawater as a reactant. Conductivity was obtained from impedance measurements made in situ throughout synthesis while temperature cycled between +15 °C and -25 °C. Several possible conduction mechanisms were subsequently determined using equivalent circuit modeling. Samples with low NaCl concentration show a doping/impurity effect and a log linear conductivity response as a function of temperature. For higher salt contentmore » samples, conductivity increases exponentially with temperature and the log linear relationship no longer holds; instead, we observe phase changes within the samples that follow NaCl–H2O–CH4 phase equilibrium predictions. Final samples were quenched in liquid nitrogen and imaged by cryogenic scanning electron microscopy (cryo-SEM) to assess grain-scale characteristics.« less

Authors:
ORCiD logo [1]; ORCiD logo [2]; ORCiD logo [1];  [2];  [1]; ORCiD logo [3]
  1. Lawrence Livermore National Lab. (LLNL), Livermore, CA (United States)
  2. U.S. Geological Survey, Menlo Park, CA (United States)
  3. The Scripps Research Inst., La Jolla, CA (United States)
Publication Date:
Research Org.:
Lawrence Livermore National Laboratory (LLNL), Livermore, CA (United States); Univ. of California, San Diego, CA (United States)
Sponsoring Org.:
USDOE National Nuclear Security Administration (NNSA); USDOE Office of Fossil Energy (FE)
OSTI Identifier:
1601946
Alternate Identifier(s):
OSTI ID: 1573282; OSTI ID: 1735361
Report Number(s):
LLNL-JRNL-777845
Journal ID: ISSN 2169-9313; 965649
Grant/Contract Number:  
AC52-07NA27344; FE0028972; FE0026382
Resource Type:
Accepted Manuscript
Journal Name:
Journal of Geophysical Research. Solid Earth
Additional Journal Information:
Journal Volume: 124; Journal Issue: 11; Journal ID: ISSN 2169-9313
Publisher:
American Geophysical Union
Country of Publication:
United States
Language:
English
Subject:
58 GEOSCIENCES; methane hydrate; impedance spectroscopy; resistivity conductivity; hydrohalite; brine; NaCl; gas hydrate; electrical conductivity

Citation Formats

Lu, R., Stern, L. A., Du Frane, W. L., Pinkston, J. C., Roberts, J. J., and Constable, S. The Effect of Brine on the Electrical Properties of Methane Hydrate. United States: N. p., 2019. Web. doi:10.1029/2019JB018364.
Lu, R., Stern, L. A., Du Frane, W. L., Pinkston, J. C., Roberts, J. J., & Constable, S. The Effect of Brine on the Electrical Properties of Methane Hydrate. United States. https://doi.org/10.1029/2019JB018364
Lu, R., Stern, L. A., Du Frane, W. L., Pinkston, J. C., Roberts, J. J., and Constable, S. Wed . "The Effect of Brine on the Electrical Properties of Methane Hydrate". United States. https://doi.org/10.1029/2019JB018364. https://www.osti.gov/servlets/purl/1601946.
@article{osti_1601946,
title = {The Effect of Brine on the Electrical Properties of Methane Hydrate},
author = {Lu, R. and Stern, L. A. and Du Frane, W. L. and Pinkston, J. C. and Roberts, J. J. and Constable, S.},
abstractNote = {Gas hydrates possess lower electrical conductivity (inverse of resistivity) than either seawater or ice, but higher than clastic silts and sands, such that electromagnetic methods can be employed to help identify their natural formation in marine and permafrost environments. Controlled laboratory studies offer a means to isolate and quantify the effects of changing individual components within gas-hydrate-bearing systems, in turn yielding insight into the behavior of natural systems. Here we investigate the electrical properties of polycrystalline methane hydrate with ≥25% gas-filled porosity and in mixture with brine. Initially, pure methane hydrate was synthesized from H2O ice and CH4 gas while undergoing electrical impedance measurement, then partially dissociated to assess the effects of pure pore water accumulation on electrical conductivity. Methane hydrate + brine mixtures were then formed by either adding NaCl (0.25–2.5 wt %) to high-purity ice or by using frozen seawater as a reactant. Conductivity was obtained from impedance measurements made in situ throughout synthesis while temperature cycled between +15 °C and -25 °C. Several possible conduction mechanisms were subsequently determined using equivalent circuit modeling. Samples with low NaCl concentration show a doping/impurity effect and a log linear conductivity response as a function of temperature. For higher salt content samples, conductivity increases exponentially with temperature and the log linear relationship no longer holds; instead, we observe phase changes within the samples that follow NaCl–H2O–CH4 phase equilibrium predictions. Final samples were quenched in liquid nitrogen and imaged by cryogenic scanning electron microscopy (cryo-SEM) to assess grain-scale characteristics.},
doi = {10.1029/2019JB018364},
journal = {Journal of Geophysical Research. Solid Earth},
number = 11,
volume = 124,
place = {United States},
year = {Wed Oct 16 00:00:00 EDT 2019},
month = {Wed Oct 16 00:00:00 EDT 2019}
}

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Cited by: 12 works
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Figures / Tables:

Table 1 Table 1: Sample conditions of NaCl-Hydrate (NH) and Seawater-Hydrate (SH) during synthesis

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