Articles | Volume 11, issue 6
https://doi.org/10.5194/tc-11-2943-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/tc-11-2943-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| Highlight paper
| 
14 Dec 2017
Research article | Highlight paper |
| 14 Dec 2017
In situ nuclear magnetic resonance response of permafrost and active layer soil in boreal and tundra ecosystems
Crustal Geophysics and Geochemistry Science Center, US Geological Survey, Denver, CO 80225, USA
now at: Hydrogeophysics Group, Aarhus University, 8000 Aarhus, Denmark
Trevor P. Irons
Department of Civil and Environmental Engineering, Energy and Geoscience Institute, University of Utah, Salt Lake City, UT 84112, USA
Burke J. Minsley
Crustal Geophysics and Geochemistry Science Center, US Geological Survey, Denver, CO 80225, USA
Neal J. Pastick
Stinger Ghaffarian Technologies, Inc., Sioux Falls, SD 57198, USA
Department of Forest Resources, University of Minnesota Twin Cities, St. Paul, MN 55108, USA
Dana R. N. Brown
Institute of Arctic Biology, University of Alaska Fairbanks, Fairbanks, AK 99775, USA
Bruce K. Wylie
Earth Resources Observation and Science Center, US Geological Survey, Sioux Falls, SD 57198, USA
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Cited
21 citations as recorded by crossref.
- Vegetation influence on the soil hydrological regime in permafrost regions of the Qinghai-Tibet Plateau, China F. Niu et al. 10.1016/j.geoderma.2019.113892
- Rapid and Gradual Permafrost Thaw: A Tale of Two Sites B. Minsley et al. 10.1029/2022GL100285
- Quantifying Dynamic Water Storage in Unsaturated Bedrock with Borehole Nuclear Magnetic Resonance L. Schmidt & D. Rempe 10.1029/2020GL089600
- Improved estimation of ice and water contents in alpine permafrost through constrained petrophysical joint inversion: The Hoher Sonnblick case study M. Steiner et al. 10.1190/geo2020-0592.1
- Linking Critical Zone With Watershed Science: The Example of the Heihe River Basin X. Li et al. 10.1029/2022EF002966
- Development of perennial thaw zones in boreal hillslopes enhances potential mobilization of permafrost carbon M. Walvoord et al. 10.1088/1748-9326/aaf0cc
- The effects of temperature on shallow borehole NMR measurements in permafrost T. Sullivan & A. Parsekian 10.1016/j.coldregions.2023.103850
- Borehole nuclear magnetic resonance as a promising 3D mapping tool in peatland studies S. Reza Mashhadi et al. 10.1016/j.geoderma.2024.116814
- Surface nuclear magnetic resonance observations of permafrost thaw below floating, bedfast, and transitional ice lakes A. Parsekian et al. 10.1190/geo2018-0563.1
- Seasonal Subsurface Thaw Dynamics of an Aufeis Feature Inferred From Geophysical Methods N. Terry et al. 10.1029/2019JF005345
- A critical mini-review on the low-field nuclear magnetic resonance investigation of pore coupling effects in near-surface environments F. Soto Bravo & C. Zhang 10.3389/frwa.2023.1059128
- Miscellaneous methods for determination of unfrozen water content in frozen soils S. Feng et al. 10.1016/j.jhydrol.2024.130802
- The effect of magnetic susceptibility and magnetic field strength on porosity estimates determined from low-field nuclear magnetic resonance K. Keating et al. 10.1016/j.jappgeo.2020.104096
- Wildfire‐Initiated Talik Development Exceeds Current Thaw Projections: Observations and Models From Alaska's Continuous Permafrost Zone D. Rey et al. 10.1029/2020GL087565
- Evaluation of slim-hole NMR logging for hydrogeologic insights into dolostone and sandstone aquifers P. Pehme et al. 10.1016/j.jhydrol.2022.127809
- Investigations on the freezing characteristic and flexural mechanical properties of frozen loess C. Xu et al. 10.1016/j.coldregions.2023.104060
- Reliable noise measure in time-gated NMR data T. Irons et al. 10.1093/gji/ggy318
- Characterization of thermal conductivity of seasonally frozen turfy soil from Northeastern China Y. He et al. 10.1007/s10064-022-02977-5
- Characterization of unfrozen water in highly organic turfy soil during freeze–thaw by nuclear magnetic resonance Y. He et al. 10.1016/j.enggeo.2022.106937
- Combined Geophysical Measurements Provide Evidence for Unfrozen Water in Permafrost in the Adventdalen Valley in Svalbard K. Keating et al. 10.1029/2017GL076508
- The Biophysical Role of Water and Ice Within Permafrost Nearing Collapse: Insights From Novel Geophysical Observations S. James et al. 10.1029/2021JF006104
19 citations as recorded by crossref.
- Vegetation influence on the soil hydrological regime in permafrost regions of the Qinghai-Tibet Plateau, China F. Niu et al. 10.1016/j.geoderma.2019.113892
- Rapid and Gradual Permafrost Thaw: A Tale of Two Sites B. Minsley et al. 10.1029/2022GL100285
- Quantifying Dynamic Water Storage in Unsaturated Bedrock with Borehole Nuclear Magnetic Resonance L. Schmidt & D. Rempe 10.1029/2020GL089600
- Improved estimation of ice and water contents in alpine permafrost through constrained petrophysical joint inversion: The Hoher Sonnblick case study M. Steiner et al. 10.1190/geo2020-0592.1
- Linking Critical Zone With Watershed Science: The Example of the Heihe River Basin X. Li et al. 10.1029/2022EF002966
- Development of perennial thaw zones in boreal hillslopes enhances potential mobilization of permafrost carbon M. Walvoord et al. 10.1088/1748-9326/aaf0cc
- The effects of temperature on shallow borehole NMR measurements in permafrost T. Sullivan & A. Parsekian 10.1016/j.coldregions.2023.103850
- Borehole nuclear magnetic resonance as a promising 3D mapping tool in peatland studies S. Reza Mashhadi et al. 10.1016/j.geoderma.2024.116814
- Surface nuclear magnetic resonance observations of permafrost thaw below floating, bedfast, and transitional ice lakes A. Parsekian et al. 10.1190/geo2018-0563.1
- Seasonal Subsurface Thaw Dynamics of an Aufeis Feature Inferred From Geophysical Methods N. Terry et al. 10.1029/2019JF005345
- A critical mini-review on the low-field nuclear magnetic resonance investigation of pore coupling effects in near-surface environments F. Soto Bravo & C. Zhang 10.3389/frwa.2023.1059128
- Miscellaneous methods for determination of unfrozen water content in frozen soils S. Feng et al. 10.1016/j.jhydrol.2024.130802
- The effect of magnetic susceptibility and magnetic field strength on porosity estimates determined from low-field nuclear magnetic resonance K. Keating et al. 10.1016/j.jappgeo.2020.104096
- Wildfire‐Initiated Talik Development Exceeds Current Thaw Projections: Observations and Models From Alaska's Continuous Permafrost Zone D. Rey et al. 10.1029/2020GL087565
- Evaluation of slim-hole NMR logging for hydrogeologic insights into dolostone and sandstone aquifers P. Pehme et al. 10.1016/j.jhydrol.2022.127809
- Investigations on the freezing characteristic and flexural mechanical properties of frozen loess C. Xu et al. 10.1016/j.coldregions.2023.104060
- Reliable noise measure in time-gated NMR data T. Irons et al. 10.1093/gji/ggy318
- Characterization of thermal conductivity of seasonally frozen turfy soil from Northeastern China Y. He et al. 10.1007/s10064-022-02977-5
- Characterization of unfrozen water in highly organic turfy soil during freeze–thaw by nuclear magnetic resonance Y. He et al. 10.1016/j.enggeo.2022.106937
2 citations as recorded by crossref.
- Combined Geophysical Measurements Provide Evidence for Unfrozen Water in Permafrost in the Adventdalen Valley in Svalbard K. Keating et al. 10.1029/2017GL076508
- The Biophysical Role of Water and Ice Within Permafrost Nearing Collapse: Insights From Novel Geophysical Observations S. James et al. 10.1029/2021JF006104
Latest update: 25 Apr 2024
Short summary
Geophysical methods have wide applications to permafrost studies. We show that borehole nuclear magnetic resonance is a valuable geophysical tool to rapidly characterize the liquid water content and unfrozen pore space in warm permafrost through simulation and field study. This technique is also sensitive to the ice nucleation process in situ. This method, which is applicable in a variety of soil types, can be used for single observations or for time-lapse monitoring of permafrost changes.
Geophysical methods have wide applications to permafrost studies. We show that borehole nuclear...
