On-site measurements of water salinity (which can be directly evaluated from the electrical conductivity) in deep-sea sediments is technically the primary source of indirect information on the capacity of the marine deposits of methane hydrates. We show the relation between the salinity (chlorinity) profile and the hydrate volume in pores to be significantly affected by non-Fickian contributions to the diffusion flux—the thermal diffusion and the gravitational segregation—which have been previously ignored in the literature on the subject and the analysis of surveys data. We provide amended relations and utilize them for an analysis of field measurements for a real hydrate deposit.
Denis S. Goldobin 1, 2
@article{CRMECA_2013__341_4-5_386_0, author = {Denis S. Goldobin}, title = {Non-Fickian diffusion affects the relation between the salinity and hydrate capacity profiles in marine sediments}, journal = {Comptes Rendus. M\'ecanique}, pages = {386--392}, publisher = {Elsevier}, volume = {341}, number = {4-5}, year = {2013}, doi = {10.1016/j.crme.2013.01.014}, language = {en}, }
TY - JOUR AU - Denis S. Goldobin TI - Non-Fickian diffusion affects the relation between the salinity and hydrate capacity profiles in marine sediments JO - Comptes Rendus. Mécanique PY - 2013 SP - 386 EP - 392 VL - 341 IS - 4-5 PB - Elsevier DO - 10.1016/j.crme.2013.01.014 LA - en ID - CRMECA_2013__341_4-5_386_0 ER -
Denis S. Goldobin. Non-Fickian diffusion affects the relation between the salinity and hydrate capacity profiles in marine sediments. Comptes Rendus. Mécanique, 10th International Meeting on Thermodiffusion, Volume 341 (2013) no. 4-5, pp. 386-392. doi : 10.1016/j.crme.2013.01.014. https://comptes-rendus.academie-sciences.fr/mecanique/articles/10.1016/j.crme.2013.01.014/
[1] et al. Gas hydrates: Past and future geohazard?, Phil. Trans. R. Soc. A, Volume 368 (2010), pp. 2369-2393
[2] Is the extent of glaciation limited by marine gas hydrates?, Geophys. Res. Lett. (Methane Hydrates in Quaternary Climate Change: The Clathrate Gun Hypothesis), Volume 245 (2006), pp. 65-80
[3] Role of naturally occuring gas hydrates in sediment transport, Am. Assoc. Pet. Geol. Bull., Volume 96 (1999), pp. 3420-3426
[4] Pleistocene slope instability of gas hydrate-laden sediment on the Beaufort sea margin, Mar. Geotechnol., Volume 137 (1998), pp. 191-198
[5] et al. Non-Fickian diffusion and the accumulation of methane bubbles in deep-water sediments, Phys. Rev. E, Volume 84, 2011, p. 056328 | arXiv
[6] Scaling of transport coefficients of porous media under compaction, Europhys. Lett., Volume 95 (2011), p. 64004
[7] A numerical model for the formation of gas hydrate below the seafloor, J. Geophys. Res., Volume 106 (2001), pp. 497-514
[8] A steady state model for marine hydrate formation: Constraints on methane supply from pore water sulfate profiles, J. Geophys. Res., Volume 108 (2003), p. 2495
[9] Sources of methane for marine gas hydrate: Inferences from a comparison of observations and numerical models, Earth Planet. Sci. Lett., Volume 206 (2003), pp. 51-63
[10] Controls on the formation and stability of gas hydrate-related bottom-simulating reflectors (BSRs): A case study from the west Svalbard continental slope, J. Geophys. Res., Volume 4 (2007), pp. 521-544
[11] Proceedings of the Ocean Drilling Program (C.K. Paull; R. Matsumoto; P.J. Wallace; W.P. Dillon, eds.), Scientific Results, vol. 164, Ocean Drilling Program, College Station, TX, 2000
[12] Estimating the amount of hydrate and free gas from surface seismic, SEG Tech. Program Expanded Abstracts, Volume 17 (1998), pp. 566-569
[13] Direct measurement of methane hydrate composition along the hydrate equilibrium boundary, J. Phys. Chem. B, Volume 109 (2005), pp. 9468-9475
[14] Transport Phenomena, Wiley, 2007
[15] Deciphering late lenozoic development of the western Svalbard margin from ODP 986 results, Mar. Geol., Volume 169 (2000), pp. 373-390
[16] Measurements of negative thermal diffusion coefficients observing onset of thermohaline convection, J. Phys. Chem., Volume 20 (1973), pp. 1029-1039
[17] Gas hydrates amount estimated from acoustic logs at the Blake Ridge, sites 994, 995, and 997 (C.K. Paull; R. Matsumoto; P.J. Wallace; W.P. Dillon, eds.), Proceedings of the Ocean Drilling Program, Scientific Results, vol. 164, Ocean Drilling Program, College Station, TX, 2000
Cited by Sources:
Comments - Policy