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Record W2604289400

Historical changes in the geomorphology of the Ottawa River (NW Ohio, U.S.A.) due to urbanization and land clearance

2010· article· en· W2604289400 on OpenAlexaboutno aff
Laura D. Webb

Bibliographic record

VenueOhioLink ETD Center (Ohio Library and Information Network) · 2010
Typearticle
Languageen
FieldSocial Sciences
TopicArchaeology and Natural History
Canadian institutionsnot available
FundersU.S. Geological Survey
KeywordsUrbanizationGeographyHydrology (agriculture)Land useGeomorphologyGeologyPhysical geographyArchaeologyCivil engineeringEngineering
DOInot available

Abstract

fetched live from OpenAlex

In northwestern Ohio, the impact of humans on natural systems extends back hundreds of years as manifested by complete reorganization of fluvial systems.This study addressed historical changes in the geomorphology the Ottawa River using vibracores, trenches, textural and geochemical analyses, and 14 C and blue light optically stimulated luminescence (blue OSL) dating.The total section thickness from trenching and vibracoring is approximately 4.5-m.The oldest sediment in the cores is interbedded massive sands and silts >1.5-m thick.These deposits represent a point bar succession that is likely post-glacial in origin.Overlying the sand is 75-cm thick interval of peats and organic-rich carbonaceous muds interbedded with thin sand horizons.Several 14 C analyses from this interval have calibrated ages of 4889 +/-178 YBP, 4731 +/-306 YBP, and 4547 +/-326 YBP.These deposits are interpreted as hydromorphic paleosols and overbank flood deposits that formed following the rise of Lake Erie.An interval 33-cm to 68-cm thick overlies the paleosols and consists of alternating massive or cross-bedded sands interbedded with discontinuous silts.One blue OSL date from these sands produced an age of 231 +/-15 YBP, which approaches the age of land clearance in northwest Ohio (early-1800s).This interval is interpreted as channel and channel margin deposits.Further up section, a cross-bedded sand layer, dated at -4 +/-5 YBP and -9 +/-5 YBP, corresponds with a major flood that occurred in this region during 1959.Overlying this historic iii flood layer are approximately 1.6-m of silty floodplain deposits that accumulated during a period of rapid population growth and construction upstream of the study area.The implications are that the Ottawa River flowed through riparian wetlands and had low banks prior to land clearance, and that excessive sediment loads dating from the agricultural period and suburbanization boom are responsible for 1.6-m of vertical floodplain aggradation.Following this period, the landscape was re-vegetated thereby decreasing the sediment discharge.As a result, the Ottawa River incised into previously stored sediment which produced the existing stream morphology of an entrenched channel flowing between terrace-like 2.3-m tall streambanks that are still inundated annually.allowing me to use their vibracorer.Thank you to the Geological Society of America, the

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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 score0.519
Threshold uncertainty score0.968

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 studies0.0010.001
Scholarly communication0.0010.000
Open science0.0000.001
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 head0.007
GPT teacher head0.203
Teacher spread0.196 · 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

Citations2
Published2010
Admission routes1
Has abstractyes

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