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Record W1639084873

Radar-Bright and Radar-Dark Haloes Around Craters on Lunar Nearside: Implications on Particle-Size Distribution of Ejecta

2008· article· en· W1639084873 on OpenAlexaff
Vikas Gupta, R. R. Ghent

Bibliographic record

VenueLunar and Planetary Science Conference · 2008
Typearticle
Languageen
FieldPhysics and Astronomy
TopicPlanetary Science and Exploration
Canadian institutionsUniversity of Toronto
Fundersnot available
KeywordsEjectaImpact craterRadarGeologyAstrobiologyLunar cratersRegolithSolar SystemRemote sensingGeophysicsPhysicsAstronomyAerospace engineering
DOInot available

Abstract

fetched live from OpenAlex

Introduction: Distinct radar-bright [1, 2] and radar-dark ejecta facies [3] have been observed to form haloes around numerous craters on the lunar nearside during Earth-based radar investigations. These observations provide an opportunity to quantify the block distribution in crater ejecta in order to further understand the physics of ejecta production and ballistic emplacement on an airless body. In this study, we make detailed measurements of the sizes of radarbright and radar-dark ejecta haloes associated with a large number of craters on the lunar nearside, using newly-released Earth-based 70-cm wavelength radar imagery obtained from the Planetary Data System (PDS) archive. The ultimate goal of the study is to understand the particle size distribution in lunar ejecta blankets. This would be a stepping stone for the eventual formulation of models that depict how impact ejecta are produced and emplaced on the Moon. Background: It is important to have a detailed understanding of particle size distribution in lunar ejecta blankets, since it can provide us with information about how particles of various sizes are produced in lunar impacts and eventually emplaced on the surface. Earth-based radar has been used in this study since the strength of the radar returns depends on the degree of scattering by particles on and near the surface. The strong dependence of these radar returns on polarization and wavelength allows for a degree of constraint through a comparison of multiple polarizations and wavelengths. Bright signatures are produced by particles on or near the surface large enough to scatter the radar [e.g. 2], whereas dark responses appear due to a lack of these big blocks [3]. We predict that the percentage of coarse material decreases with distance away from the crater, leaving only the fine-grained material to travel the farthest. The edge of either halo is the point at which we begin to see either an abundance of blocks (bright haloes) or a lack of blocks (dark haloes), and the transition between the two can be either sharp or gradational, thereby indicating two potentially different types of processes involving ejecta production and emplacement. Previous work [3-5] showed that nearly all lunar impacts over two orders of magnitude in size produce block-poor, radar-dark ejecta haloes that had not been previously studied. Is has been demonsrated [4, 5] that for a small number of large craters, the total volume of block-poor ejecta scales with crater size according to the power-law relationship: rH = Arc (1)

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 distilled prediction

Teacher imitation

Not calibrated prevalence, not ground truth. Human validation pending. Learned from the 10,348 direct Codex labels and 10,348 direct Gemma labels. Candidate is the union of thresholded teacher heads; consensus is their intersection. These outputs are machine_predicted_unvalidated and are not human labels or direct frontier model labels.

metaresearch head score (Codex)0.000
metaresearch head score (Gemma)0.000
Version: codex-gemma-dda1882f352aValidation 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 score0.115
Threshold uncertainty score0.580

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0000.000
Science and technology studies0.0010.001
Scholarly communication0.0000.001
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 head0.025
GPT teacher head0.228
Teacher spread0.203 · 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 teacher head, 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
Published2008
Admission routes1
Has abstractyes

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