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Title: Electrical and Seismic Response of Saline Permafrost Soil during Freeze - Thaw Transition: Supporting Data

Abstract

These data were collected during a repeat freeze-thaw cycle on a saline permafrost portion of a core to understand mechanical and geophysical property changes over time. The core used for the experiment was collected from the NGEE-Arctic Site 0 transect site located in the Barrow Environmental Observatory (BEO) in Barrow, Alaska. This region features polygonal ground, and the core was collected in the center of a flat centered polygon. The saline permafrost portion of the core was at the bottom 260-280 cm below ground surface.Data files include: Electrical signal change during freeze-thaw-refreeze cycle at 1 Hz; Spectral data - Complex resistivity data during Freeze-thaw of the saline permafrost core; Seismic data; and CT cross sections of the core sample from approximately the same location: (A, D) before the test (thawed), (B, E) after the test (frozen), and (C, F) after deep freeze (frozen). The Next-Generation Ecosystem Experiments: Arctic (NGEE Arctic), was a 10-year research effort (2012-2022) to reduce uncertainty in Earth System Models by developing a predictive understanding of carbon-rich Arctic ecosystems and feedbacks to climate. NGEE Arctic was supported by the Department of Energy?s Office of Biological and Environmental Research.The NGEE Arctic project had two field research sites: 1) locatedmore » within the Arctic polygonal tundra coastal region on the Barrow Environmental Observatory (BEO) and the North Slope near Utqiagvik (Barrow), Alaska and 2) multiple areas on the discontinuous permafrost region of the Seward Peninsula north of Nome, Alaska.Through observations, experiments, and synthesis with existing datasets, NGEE Arctic provided an enhanced knowledge base for multi-scale modeling and contributed to improved process representation at global pan-Arctic scales within the Department of Energy?s Earth system Model (the Energy Exascale Earth System Model, or E3SM), and specifically within the E3SM Land Model component (ELM).« less

Authors:
ORCiD logo ; ; ; ;
Publication Date:
Other Number(s):
NGA119
ngee_F40BA8D6A5E0E7F810CBE19CDC47FAC02017_08_08_141517834
DOE Contract Number:  
DE-AC05-00OR22725
Research Org.:
Next Generation Ecosystems Experiment - Arctic, Oak Ridge National Laboratory (ORNL), Oak Ridge, TN (US); NGEE Arctic, Oak Ridge National Laboratory (ORNL), Oak Ridge, TN (United States)
Sponsoring Org.:
USDOE Office of Science (SC), Biological and Environmental Research (BER)
Collaborations:
ORNL
Subject:
54 Environmental Sciences
Keywords:
unfrozen water content; seismic property; Induced polarization; electrical resistivity; Geophysics; Barrow, Alaska; Utqiagvik, Alaska; Barrow Environmental Observatory
OSTI Identifier:
1374172
DOI:
https://doi.org/10.5440/1374172

Citation Formats

Wu, Yuxin, Nakagawa, Seiji, Kneafsey, Tim, Dafflon, Baptiste, and Hubbard, Susan. Electrical and Seismic Response of Saline Permafrost Soil during Freeze - Thaw Transition: Supporting Data. United States: N. p., 2021. Web. doi:10.5440/1374172.
Wu, Yuxin, Nakagawa, Seiji, Kneafsey, Tim, Dafflon, Baptiste, & Hubbard, Susan. Electrical and Seismic Response of Saline Permafrost Soil during Freeze - Thaw Transition: Supporting Data. United States. doi:https://doi.org/10.5440/1374172
Wu, Yuxin, Nakagawa, Seiji, Kneafsey, Tim, Dafflon, Baptiste, and Hubbard, Susan. 2021. "Electrical and Seismic Response of Saline Permafrost Soil during Freeze - Thaw Transition: Supporting Data". United States. doi:https://doi.org/10.5440/1374172. https://www.osti.gov/servlets/purl/1374172. Pub date:Fri May 07 00:00:00 EDT 2021
@article{osti_1374172,
title = {Electrical and Seismic Response of Saline Permafrost Soil during Freeze - Thaw Transition: Supporting Data},
author = {Wu, Yuxin and Nakagawa, Seiji and Kneafsey, Tim and Dafflon, Baptiste and Hubbard, Susan},
abstractNote = {These data were collected during a repeat freeze-thaw cycle on a saline permafrost portion of a core to understand mechanical and geophysical property changes over time. The core used for the experiment was collected from the NGEE-Arctic Site 0 transect site located in the Barrow Environmental Observatory (BEO) in Barrow, Alaska. This region features polygonal ground, and the core was collected in the center of a flat centered polygon. The saline permafrost portion of the core was at the bottom 260-280 cm below ground surface.Data files include: Electrical signal change during freeze-thaw-refreeze cycle at 1 Hz; Spectral data - Complex resistivity data during Freeze-thaw of the saline permafrost core; Seismic data; and CT cross sections of the core sample from approximately the same location: (A, D) before the test (thawed), (B, E) after the test (frozen), and (C, F) after deep freeze (frozen). The Next-Generation Ecosystem Experiments: Arctic (NGEE Arctic), was a 10-year research effort (2012-2022) to reduce uncertainty in Earth System Models by developing a predictive understanding of carbon-rich Arctic ecosystems and feedbacks to climate. NGEE Arctic was supported by the Department of Energy?s Office of Biological and Environmental Research.The NGEE Arctic project had two field research sites: 1) located within the Arctic polygonal tundra coastal region on the Barrow Environmental Observatory (BEO) and the North Slope near Utqiagvik (Barrow), Alaska and 2) multiple areas on the discontinuous permafrost region of the Seward Peninsula north of Nome, Alaska.Through observations, experiments, and synthesis with existing datasets, NGEE Arctic provided an enhanced knowledge base for multi-scale modeling and contributed to improved process representation at global pan-Arctic scales within the Department of Energy?s Earth system Model (the Energy Exascale Earth System Model, or E3SM), and specifically within the E3SM Land Model component (ELM).},
doi = {10.5440/1374172},
journal = {},
number = ,
volume = ,
place = {United States},
year = {Fri May 07 00:00:00 EDT 2021},
month = {Fri May 07 00:00:00 EDT 2021}
}