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Record W2485001607 · doi:10.2136/sssabookser5.4.c31

3.4.2 Laboratory Methods

2002· book-chapter· en· W2485001607 on OpenAlexaff
W. D. Reynolds, D. E. Elrick, E.G. Youngs, H.W.G. Booltink, J. Bouma

Bibliographic record

VenueSoil Science Society of America book series · 2002
Typebook-chapter
Languageen
FieldBiochemistry, Genetics and Molecular Biology
TopicElectron Spin Resonance Studies
Canadian institutionsUniversity of GuelphAgriculture and Agri-Food Canada
Fundersnot available
KeywordsComputer science

Abstract

fetched live from OpenAlex

Laboratory measurement of saturated soil water flow parameters is frequently limited to the determination of saturated hydraulic conductivity (Ks). The primary factors affecting Ks in a laboratory environment include the texture and structure of the soil core or column, the temperature of the water, the ionic speciation and concentrations in the water, and the presence of air bubbles in soil pores. The Ks value tends to increase greatly with coarser texture and enhanced structure because of an increase in the number and size of large, highly water-conductive pores. Consequently, coarse-textured and/or structured porous media tend to have larger Ks values than fine-textured and/or structureless porous media. This chapter discusses method for determining Ks such as constant head soil core (Tank) method; falling head soil core (Tank) method; steady flow soil column method and other laboratory methods.

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 categoriesMeta-epidemiology (narrow), Science and technology studies
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Not applicable · Consensus signal: none
GenreCandidate signal: Other · Consensus signal: Other
Teacher disagreement score0.608
Threshold uncertainty score1.000

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 studies0.0000.007
Scholarly communication0.0000.000
Open science0.0010.000
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 head0.011
GPT teacher head0.283
Teacher spread0.272 · 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.

Study designNot applicable
Domainnot available
GenreOther

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

Citations24
Published2002
Admission routes1
Has abstractyes

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