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Record W2981329419 · doi:10.4095/299796

Improving the spatial density of a regional hydraulic conductivity dataset with estimates made from domestic water well information

2017· report· en· W2981329419 on OpenAlexaboutno aff
Elizabeth Priebe, Christopher J. Neville, David L. Rudolph

Bibliographic record

Venuenot available
Typereport
Languageen
FieldEngineering
TopicReservoir Engineering and Simulation Methods
Canadian institutionsnot available
Fundersnot available
KeywordsHydraulic conductivityEnvironmental scienceSpatial analysisConductivityData miningHydrology (agriculture)Soil scienceComputer scienceGeographyGeologyRemote sensingGeotechnical engineeringChemistry

Abstract

fetched live from OpenAlex

High-quality hydraulic conductivity data tend to be sparse relative to the large areas under investigation in regional-scale groundwater studies. From the 1960s through the 1990s, the literature is replete with articles discussing the details of augmenting high-quality hydraulic conductivity datasets with values estimated from specific capacity tests. Early publications focused on the development of the fundamental mathematical relation between specific capacity and hydraulic conductivity. Later articles presented approaches claiming improved accuracy of hydraulic conductivity estimates from specific capacity by correcting for additional well losses. However, because the site-specific data required to correct for additional well losses are generally not available, these corrections often led to error. Through the 1990s, many workers abandoned the analytical approach for an empirical one, arguing that correcting for additional well losses introduces significant error into the K estimate. Since the early 2000s, the literature has become largely silent on the topic of augmenting high-quality hydraulic conductivity datasets with K estimates developed from specific capacity. Despite a pause in the literature, integration of the results of high-quality tests within more approximate but spatially extensive datasets is still desired, particularly to support the identification of groundwater resource exploration targets in complex, heterogeneous geological settings. We present a simple and effective approach to synthesize the results from high-quality hydraulic tests with reconnaissance-level hydraulic conductivity estimates made from domestic water well specific capacity tests. Domestic water wells are ubiquitous across Ontario, and although their associated well records do not contain the information required to support rigorous hydraulic test analyses, they do contain the information required to calculate specific capacity. We use the fundamental Theis relation to make hydraulic conductivity estimates from specific capacity tests, assuming that additional well losses account for a relatively small portion of the total observed drawdown. The utility of this approach is demonstrated with data comparisons at three different spatial scales. Each comparison is conducted to evaluate the suitability of augmenting the high-quality data set with lesser quality estimates to answer specific research questions. The results of the comparisons results show good correlation between both sets of hydraulic conductivity estimates, and provide the information required to support careful data integration for improved hydraulic conductivity data coverage.

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)0.001
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: Simulation or modeling · Consensus signal: Simulation or modeling
GenreCandidate signal: Empirical · Consensus signal: none
Teacher disagreement score0.765
Threshold uncertainty score0.998

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0010.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0000.000
Science and technology studies0.0000.000
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 head0.031
GPT teacher head0.283
Teacher spread0.252 · 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 designSimulation or modeling
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
Published2017
Admission routes1
Has abstractyes

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