Direct current (DC) resistivity and induced polarization (IP) monitoring of active layer dynamics at high temporal resol
Publikation: Bidrag til bog/antologi/rapport › Konferencebidrag i proceedings › Forskning › fagfællebedømt
Standard
Direct current (DC) resistivity and induced polarization (IP) monitoring of active layer dynamics at high temporal resol. / Doetsch, J.; Fiandaca, G.; Ingeman-Nielsen, T.; Fiandaca, G.; Christiansen, A. V.; Auken, E.; Elberling, B.
Near Surface Geoscience 2015 - 21st European Meeting of Environmental and Engineering Geophysics. 1. udg. European Association of Geoscientists and Engineers, EAGE, 2015. s. 291-295 (Near Surface Geoscience 2015 - 21st European Meeting of Environmental and Engineering Geophysics).Publikation: Bidrag til bog/antologi/rapport › Konferencebidrag i proceedings › Forskning › fagfællebedømt
Harvard
APA
Vancouver
Author
Bibtex
}
RIS
TY - GEN
T1 - Direct current (DC) resistivity and induced polarization (IP) monitoring of active layer dynamics at high temporal resol
AU - Doetsch, J.
AU - Fiandaca, G.
AU - Ingeman-Nielsen, T.
AU - Fiandaca, G.
AU - Christiansen, A. V.
AU - Auken, E.
AU - Elberling, B.
PY - 2015
Y1 - 2015
N2 - With permafrost thawing and changes in active layer dynamics induced by climate change, interactions between biogeochemical and thermal processes in the ground are of great importance. Here, active layer dynamics have been monitored using direct current (DC) resistivity and induced polarization (IP) measurements at high temporal resolution at a heath tundra site on Disko Island on the west coast of Greenland (69°N). Borehole sediment characteristics and subsurface temperatures supplemented the DCIP measurements. Data acquired during the freezing period of October 2013 - February 2014 clearly image the soil freezing as a strong increase in resistivity. While the freezing horizon generally moves deeper with time, some variations in the freezing depth are observed along the profile. Comparison with depth-specific soil temperature indicates an exponential relationship between resistivity and belowfreezing temperature. Time-lapse inversions of the full-decay IP data indicate a decrease of normalized chargeability with freezing of the ground, which can be the result of a decrease in the total unfrozen water and thus a higher ion concentration in the pore-water. We conclude that DC-IP time-lapse measurements can non-intrusively and reliably image freezing patterns and their lateral variation on a 10-100 m scale that is difficult to sample by point measurements.
AB - With permafrost thawing and changes in active layer dynamics induced by climate change, interactions between biogeochemical and thermal processes in the ground are of great importance. Here, active layer dynamics have been monitored using direct current (DC) resistivity and induced polarization (IP) measurements at high temporal resolution at a heath tundra site on Disko Island on the west coast of Greenland (69°N). Borehole sediment characteristics and subsurface temperatures supplemented the DCIP measurements. Data acquired during the freezing period of October 2013 - February 2014 clearly image the soil freezing as a strong increase in resistivity. While the freezing horizon generally moves deeper with time, some variations in the freezing depth are observed along the profile. Comparison with depth-specific soil temperature indicates an exponential relationship between resistivity and belowfreezing temperature. Time-lapse inversions of the full-decay IP data indicate a decrease of normalized chargeability with freezing of the ground, which can be the result of a decrease in the total unfrozen water and thus a higher ion concentration in the pore-water. We conclude that DC-IP time-lapse measurements can non-intrusively and reliably image freezing patterns and their lateral variation on a 10-100 m scale that is difficult to sample by point measurements.
U2 - 10.3997/2214-4609.201413722
DO - 10.3997/2214-4609.201413722
M3 - Article in proceedings
AN - SCOPUS:84958073382
T3 - Near Surface Geoscience 2015 - 21st European Meeting of Environmental and Engineering Geophysics
SP - 291
EP - 295
BT - Near Surface Geoscience 2015 - 21st European Meeting of Environmental and Engineering Geophysics
PB - European Association of Geoscientists and Engineers, EAGE
T2 - 21st European Meeting of Environmental and Engineering Geophysics, Near Surface Geoscience 2015
Y2 - 6 September 2015 through 10 September 2015
ER -
ID: 260673256