Articles | Volume 18, issue 1
https://doi.org/10.5194/tc-18-489-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/tc-18-489-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Non-destructive multi-sensor core logging allows for rapid imaging and estimation of frozen bulk density and volumetric ice content in permafrost cores
Joel Pumple
CORRESPONDING AUTHOR
Department of Earth and Atmospheric Sciences, University of Alberta, Edmonton, AB, Canada
Alistair Monteath
Department of Earth and Atmospheric Sciences, University of Alberta, Edmonton, AB, Canada
Jordan Harvey
Department of Earth and Atmospheric Sciences, University of Alberta, Edmonton, AB, Canada
Mahya Roustaei
Department of Earth and Atmospheric Sciences, University of Alberta, Edmonton, AB, Canada
Department of Civil Engineering, Geotechnics Laboratory, Ghent University, Technologiepark 68, 9052 Zwijnaarde, Ghent, Belgium
Alejandro Alvarez
Department of Earth and Atmospheric Sciences, University of Alberta, Edmonton, AB, Canada
Casey Buchanan
Department of Earth and Atmospheric Sciences, University of Alberta, Edmonton, AB, Canada
YukonU Research Centre, Yukon University, Whitehorse, YT, Canada
Duane Froese
CORRESPONDING AUTHOR
Department of Earth and Atmospheric Sciences, University of Alberta, Edmonton, AB, Canada
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Cited articles
Andersland, O. B. and Ladanyi, B.: Frozen Ground, An Introduction to Frozen Ground Engineering, 1–22, Springer, Boston, MA, https://doi.org/10.1007/978-1-4757-2290-1_1, 1994.
ASTM D4083-89: Standard test method for description of frozen soils (reapproved 2016), in: ASTM International, PA, USA, https://doi.org/10.1520/d4083, 2016.
Bandara, S., Froese, D. G., St. Louis, V. L., Cooke, C. A., and Calmels, F.: Post Depositional Mercury Mobility in a Permafrost Peatland from Central Yukon, Canada, ACS Earth and Space Chemistry, 3, 770–778, https://doi.org/10.1021/acsearthspacechem.9b00010, 2019.
Calmels, F. and Allard, M.: Ice segregation and gas distribution in permafrost using tomodensitometric analysis, Permafrost Periglac., 15, 367–378, https://doi.org/10.1002/ppp.508, 2004.
CAN/BNQ 2501-500/2017: Geotechnical Site Investigations for Building Foundations in Permafrost Zones, Standards Council of Canada and the Bureau de normalisation du Quebec, 2017.
Carbonneau, A., Allard, M., L'Herault, E., and LeBlanc, A.: High permafrost s in Holocene slope deposits as observed from shallow geophysics and a coring program in Pangnirtung, Nunavut, Canada, in: Proceedings of AGU Fall Meeting 2011: American Geophysical Union, Fall Meeting 2011, 5–9 December 2011, C41C-0419, 2011AGUFM.C41C0419C, 2011.
Darrow, M. M. and Lieblappen, R. M.: Visualizing cation treatment effects on frozen clay soils through μCT scanning, Cold Reg. Sci. Technol., 175, 103085, https://doi.org/10.1016/j.coldregions.2020.103085, 2020.
Evans, H. B.: GRAPE – A device for continuous determination of material density and porosity, in: Proceedings of 6th Annual SPWLA Logging Symposium, 2, Dallas, TX, 4 May 1965, B1–B25, SPWLA-1965-2B, 1965.
Fortin, D., Francus, P., Gebhardt, A. C., Hahn, A., Kliem, P., Lisé-Pronovost, A., Roychowdhury, R., Labrie, J., and St-Onge, G.: Destructive and non-destructive density determination: method comparison and evaluation from the Laguna Potrok Aike sedimentary record, Quaternary Sci. Rev., 71, 147–153, https://doi.org/10.1016/j.quascirev.2012.08.024, 2013.
French, H. M. and Shur, Y.: The principles of cryostratigraphy, Earth-Sci. Rev., 101, 190–206, https://doi.org/10.1016/j.earscirev.2010.04.002, 2010.
Geotek, LTD: Multi-sensor Core Logger manual, Daventry, UK, 2022-09-07, https://www.geotek.co.uk/wp-content/uploads/2022/09/MSCL-S-manual-2022-09-07.pdf (last access: 17 January 2024), 2021.
Gunn, D. E. and Best, A. I.: A new automated nondestructive system for high resolution multi-sensor core logging of open sediment cores, Geo-Mar. Lett., 18, 70–77, https://doi.org/10.1007/s003670050054, 1998.
Heiri, O., Lotter, A. F., and Lemcke, G.: Loss on ignition as a method for estimating organic and carbonate content in sediments: reproducibility and comparability of results, J. Paleolimnol., 25, 101–110, https://doi.org/10.1023/A:1008119611481, 2001.
Hunt, J. E., Wynn, R. B., Masson, D. G., Talling, P. J., and Teagle, D. A. H.: Sedimentological and geochemical evidence for multistage failure of volcanic island landslides: A case study from Icod landslide on north Tenerife, Canary Islands, Geochem. Geophy. Geosy., 12, https://doi.org/10.1029/2011gc003740, 2011.
Jorgenson, M. T., Romanovsky, V., Harden, J., Shur, Y., O'Donnell, J., Schuur, E. A. G., Kanevskiy, M., and Marchenko, S.: Resilience and vulnerability of permafrost to climate change, Can. J. Earth Sci., 40, 1219–1236, https://doi.org/10.1139/X10-060, 2010.
Kazemian, S., Huat, B., Prasad, A., and Barghchi, M.: “A State of Art Review of Peat: Geotechnical Engineering Perspective”, Int. J. Phys. Sci., 6, 1974–1981, https://doi.org/10.5897/IJPS11.396, 2011.
Kokelj, S. V. and Burn, C. R.: Ground ice and soluble cations in near-surface permafrost, Inuvik, Northwest Territories, Canada, Permafrost Periglac., 14, 275–289, https://doi.org/10.1002/ppp.458, 2003.
Kleinberg, R. L. and Griffin, D. D.: NMR measurements of permafrost: unfrozen water assay, pore-scale distribution of ice, and hydraulic permeability of sediments, Cold Reg. Sci. Technol., 42, 63–77, https://doi.org/10.1016/j.coldregions.2004.12.002, 2005.
Kuras, O., Shreeve, J., Smith, N., Graham, J., and Atherton, N.: Enhanced Characterisation of Radiologically Contaminated Sediments at Sellafield by MSCL Core Logging and X-ray Imaging, in: Near Surface Geoscience 2016-22nd European Meeting of Environmental and Engineering Geophysics, European Association of Geoscientists & Engineers, Barcelona, Spain, 4–8 September 2016, Vol. 2016, No. 1, pp. cp-495, https://doi.org/10.3997/2214-4609.201601918, 2016.
Kruse, A. M. and Darrow, M. M.: Adsorbed cation effects on unfrozen water in fine-grained frozen soil measured using pulsed nuclear magnetic resonance, Cold Reg. Sci. Technol., 142, 42–54, https://doi.org/10.1016/j.coldregions.2017.07.006, 2017.
Lenz, J., Grosse, G., Jones, B. M., Walter Anthony, K. M., Bobrov, A., Wulf, S., and Wetterich, S.: Mid-Wisconsin to Holocene Permafrost and Landscape Dynamics based on a Drained Lake Basin Core from the Northern Seward Peninsula, Northwest Alaska, Permafrost Periglac., 27, 56–75, https://doi.org/10.1002/ppp.1848, 2015.
Linell, K. A. and Kaplar, C. W.: Description and classification of frozen soils, U.S. Army Cold Reg. Res. Eng. Lab. Tech. Rep. 140, 1966.
Lin, Z., Gao, Z., Fan, X., Niu, F., Luo, J., Yin, G., and Liu, M.: Factors controlling near surface ground-ice characteristics in a region of warm permafrost, Beiluhe Basin, Qinghai-Tibet Plateau, Geoderma, 376, 114540, https://doi.org/10.1016/j.geoderma.2020.114540, 2020.
Liu, H., Maghoul, P., Shalaby, A., and Thomson, D.: Ultrasonic characterization of frozen soils using a multiphase poromechanical approach, Comput. Geotech., 153, 105068, https://doi.org/10.1016/j.compgeo.2022.105068, 2023.
Motorin, A. S., Bukin, A. V., and Iglovikov, A. V.: Water-physical properties of drained peat soils of northern trans-ural forest-steppe zone, IOP C. Ser. Earth Env., 90, 012053, https://doi.org/10.1088/1755-1315/90/1/012053, 2017.
Murton, J. B. and French, H. M.: Cryostructures in permafrost, Tuktoyaktuk coastlands, western Arctic, Canada, Can. J. Earth Sci., 31, 737–747, https://doi.org/10.1139/e94-067, 1994.
Niessen, F., Magens, D., and Gebhardt, A. C.: Physical properties of the AND-1B Core, ANDRILL McMurdo ice shelf project, Antarctica, Terra Antartica, 14, 155–166, hdl:10013/epic.30000.d001, 2007.
Pihlainen, J. A. and Johnston, G. H.: Guide to a Field description of Permafrost for Engineering Purposes, Associate Committee on Soil and Snow Mechanics, Ottawa, Technical Memorandum No. 79, p. 21, https://doi.org/10.4224/20386268, 1963.
Pumple, J.: Non-destructive multi-sensor core logging and cuboid data, Zenodo [data set], https://doi.org/10.5281/zenodo.10519939, 2023.
Roustaei, M., Pumple, J., Harvey, J., and Froese, D.: Estimating ice and unfrozen water in permafrost samples using industrial computed tomography scanning, in: GeoCalgary 2022, 2–5 October 2022, Calgary, Canada, 2022.
Smol, J. P., Birks, H. J. B., and Last, W. M. (Eds.): Tracking Environmental Change Using Lake Sediments, Dev. Paleoenviron. Res., 1, 137–170, https://doi.org/10.1007/0-306-47671-1, 2001.
Stephani, E., Fortier, D., and Shur, Y.: Applications of cryofacies approach to frozen ground engineering – case study of a road test site along the Alaska highway (Beaver Creek, Yukon, Canada), Joint 63rd Canadian geotechnical conference and 6th Canadian permafrost conference, 12–15 September 2010, Calgary, Alberta, Canada, 546, 476–483, https://doi.org/10.13140/2.1.2467.2961, 2010.
Throop, J., Lewkowicz, A. G., and Smith, S. L.: Climate and ground temperature relations at sites across the continuous and discontinuous permafrost zones, northern Canada, Can. J. Earth Sci., 49, 865–876, https://doi.org/10.1139/e11-075, 2012.
Vardy, M. E., L'Heureux, J.-S., Vanneste, M., Longva, O., Steiner, A., Forsberg, C. F., Haflidason, H., and Brendryen, J.: Multidisciplinary investigation of a shallow near-shore landslide, Finneidfjord, Norway, Near Surf. Geophys., 10, 267–277, https://doi.org/10.3997/1873-2012022, 2012.
Weber, M. E., Niessen, F., Kuhn, G., and Wiedicke, M.: Calibration and application of marine sedimentary physical properties using a multi-sensor core logger, Mar. Geol., 136, 151–172, https://doi.org/10.1016/s0025-3227(96)00071-0, 1997.
Zhou, X., Zhou, J., Kinzelbach, W., and Stauffer, F.: Simultaneous measurement of unfrozen water content and ice content in frozen soil using gamma ray attenuation and TDR, Water Resour. Res., 50, 9630–9655, https://doi.org/10.1002/2014wr015640, 2014.
Short summary
Ice content is a critical variable in the context of thawing permafrost, and permafrost cores provide a means to measure the characteristics of frozen ground; however, these measurements are typically destructive and time intensive. Multi-sensor core logging (MSCL) provides a fast, non-destructive method to image permafrost cores, measure bulk density, and estimate ice content. The use of MSCL will improve existing digital permafrost archives by adding high-quality and reproducible data.
Ice content is a critical variable in the context of thawing permafrost, and permafrost cores...