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Record W4392760130 · doi:10.5194/egusphere-egu24-13586

In-situ Weathering of Alluvial Sediments in the Southern Central Andes Recorded by Ground- and Space-Based Hyperspectral Reflectance

2024· preprint· en· W4392760130 on OpenAlexaff
Henry T. Crawford, Mitch D’Arcy, Andreas Ruby, Taylor Schildgen, Ana Laura Martínez López

Bibliographic record

Venuenot available
Typepreprint
Languageen
FieldComputer Science
TopicGeochemistry and Geologic Mapping
Canadian institutionsUniversity of British Columbia
Fundersnot available
KeywordsWeatheringHyperspectral imagingGeologyAlluviumReflectivityIn situRemote sensingGeomorphologyGeographyMeteorologyOptics

Abstract

fetched live from OpenAlex

Alluvial fans comprise abandoned sedimentary surfaces undergoing physical and chemical weathering. While weathering pathways and kinetics have been described over seconds to decades, few field-based studies have quantified these processes in alluvial deposits over geologic timespans. We examine 14 alluvial-fan surfaces flanking the Sierra del Aconquija, southern Central Andes, which have ages between 3 and 320 ka as determined by cosmogenic nuclide exposure dating. These fans present an opportunity to study the evolution of alluvial sediments across late-Quaternary timescales; including silicate weathering pathways, products, rates, and sensitivity to known past climate changes. We use space- and ground-based hyperspectral reflectance measurements to characterize surface mineralogy, and we test whether in-situ weathering records signals of landform age and regional climatic history. We collect fan-surface reflectance using both a handheld spectroradiometer and the PRISMA hyperspectral satellite sensor. In both datasets, bridging several orders of magnitude in spatial scale, we detect spectral features indicative of changing quantities of primary minerals, clays, and iron oxides. These patterns suggest a gradual increase in absolute weathering with surface age, but at progressively slower rates over time. Superimposed on the long-term weathering kinetics, secondary minerals are generated in amounts and at rates that correlate systematically with ~23 kyr precessional cycles and millennial-scale climate perturbations. We interpret that these alluvial fans are sensitive archives of past weathering, which was more pronounced during episodes of wetter and warmer climate. Furthermore, the surface signals are corroborated by the downward accumulation of iron oxide, as shown in soil profiles from four alluvial fan units which were spectrally scanned from the surface to below the weathering front. Our findings highlight the geomorphological applications of hyperspectral data for (i) quantifying weathering processes over 1-100 kyr timescales; (ii) developing novel chronometers for alluvial sediments; and (iii) recovering new palaeoclimate signals from terrestrial sedimentary archives.

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 score0.044
Threshold uncertainty score0.087

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 communication0.0000.000
Open science0.0000.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0000.000

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 head0.016
GPT teacher head0.240
Teacher spread0.224 · 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
Published2024
Admission routes1
Has abstractyes

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