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Record W4408467517 · doi:10.5194/egusphere-egu25-18453

A-ERT Insights: Linking resistivity, temperature, and moisture dynamics in two distinctive Antarctic permafrost lithologies

2025· preprint· en· W4408467517 on OpenAlexaff
Michaela Kňažková, Mohammad Farzamian, Filip Hrbáček, Teddi Herring, Christian Hauck

Bibliographic record

Venuenot available
Typepreprint
Languageen
FieldEarth and Planetary Sciences
TopicClimate change and permafrost
Canadian institutionsUniversity of Calgary
Fundersnot available
KeywordsPermafrostLithologyGeologyMoistureElectrical resistivity and conductivityDynamics (music)Earth scienceGeomorphologyPetrologyOceanographyGeographyMeteorology

Abstract

fetched live from OpenAlex

This study investigates the relationship between electrical resistivity, ground temperature, and soil moisture across two contrasting lithologies within the permafrost environment on James Ross Island, located in the north-eastern Antarctic Peninsula. The region is characterized by continuous permafrost and a semi-arid polar continental climate with a mean annual air temperature of approximately -7 °C. The monitoring transect crosses a lithological boundary between a Holocene marine terrace and finer-grained Cretaceous sediments. An automated electrical resistivity tomography (A-ERT) system, utilizing a 4POINTLIGHT_10W (Lippmann) device, was installed near the Czech Antarctic station Johann Gregor Mendel in February 2023. The system performs daily resistivity measurements along a 23-metre transect with 47 electrodes spaced 0.5 m apart, probing depths up to 4.5 meters. Complementary temperature sensors (placed at depths from 5 to 200 cm) and soil moisture sensors (at 5, 35, 55, and 75 cm) provide additional context on thermal and moisture regimes within each of the distinctive lithologies.Approximately two years of data reveal significant lithology-dependent variations in resistivity. Resistivity values are consistently higher in the coarser-grained Holocene marine terrace than in the finer-grained Cretaceous sediments. Overall, resistivity increases rapidly during winter (approximately 1–2 kΩm) and decreases during the thawing phase (approximately 10–100 Ωm), closely following the changes in ground temperature and soil moisture. The thaw front progression is readily observable in resistivity data, highlighting contrasting thermal and hydrological responses between lithologies. These relationships also form the basis for modelling ground temperature across the whole transect using resistivity data, offering a predictive approach to understanding permafrost dynamics.This study demonstrates that A-ERT provides robust, high-resolution insights into the interplay between lithology, thermal regime and soil moisture in permafrost environments, surpassing the spatial limitations of traditional borehole methods and enabling effective long-term monitoring in extreme Antarctic conditions.

Fetched live from OpenAlex and de-inverted. Abstracts are not stored in this database: the inverted indexes are 8.6 GB of the frame’s 9.3 GB of text, and the host has 13 GB free.

How this classification was reachedexpand

Full frame machine prediction

Teacher imitation

Not calibrated prevalence, not ground truth. Human validation pending. The Gemma side is a direct model label for every work in the frame, read from the title-only record. The Codex side is a classifier learned from the 10,348 direct Codex labels and calibrated to design-weighted sample rates; fields without enough sample support carry no Codex call. Candidate is the union of the two sides; consensus is their intersection. These outputs are machine_predicted_unvalidated and are not human labels.

metaresearch head score (Codex)0.000
metaresearch head score (Gemma)0.000
Version: metacan-v3-hybrid-931329e0061cValidation status: machine_predicted_unvalidated
Candidate categoriesnone
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.008
Threshold uncertainty score0.017

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0010.001
Science and technology studies0.0000.000
Scholarly communication0.0010.000
Open science0.0000.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0010.000

Machine scores (provisional)

The two teacher heads of the student model, read on this work. A score orders the frame for review; it never asserts a category, and the validation status ships verbatim with every row.

Baseline scores from an immature model (maturity gate not passed, 7 training rounds). Scores rank; they never assert a category.

Opus teacher head0.027
GPT teacher head0.277
Teacher spread0.251 · how far apart the two teachers sit on this one work
Validation statusscore_only:v0-immature-baseline · verbatim from the scoring run: score_only means the number may rank works, and no category label ships from it

Classification

machine, unvalidated

Machine predicted; a candidate call from one source (direct Gemma or distilled Codex), not a consensus.

The models applied no category: nothing in the taxonomy fit this work.
Study designObservational
Domainnot available
GenreEmpirical

How this classification was reached, model by model and score by score, is at the end of the page under "How this classification was reached".

Quick stats

Citations0
Published2025
Admission routes1
Has abstractyes

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