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Record W1549829134 · doi:10.5772/24275

Fine Sediment Deposition at Forest Road Crossings: An Overview and Effective Monitoring Protocol

2011· book-chapter· en· W1549829134 on OpenAlexaff
Forrest John, L. Silva Ellen

Bibliographic record

VenueInTech eBooks · 2011
Typebook-chapter
Languageen
FieldEnvironmental Science
TopicHydrology and Sediment Transport Processes
Canadian institutionsUniversity of Northern British Columbia
FundersMinistry of Environment
KeywordsEnvironmental scienceSedimentHydrology (agriculture)STREAMSBiotaWatershedSurface runoffGeologyEcologyGeomorphology

Abstract

fetched live from OpenAlex

Fine sediment (< 2mm) is an integral component of naturally functioning streams but can become a pollutant when development activities increase stream concentrations beyond that of the natural regime or when the sediments carry contaminants. Watershed development activities including urbanization, agriculture, and forestry can influence fine sediment quantity, quality, and its transport and storage regime by altering the natural timing and volume of water and sediment delivered to the stream channel. These development activities increase water and fine sediment delivery to streams by removing vegetation cover, disturbing soils, and connecting these disturbed areas to streams through roads, ditch lines, and/or simplified ground surfaces that enhance runoff (Bilby et al., 1989; Corner et al., 1996; Keutzweiser and Capell, 2001). Although development activities can affect the transport of larger particle sizes (e.g. gravels and cobbles), fine sediments from sand to clay are emphasized here as they have a significant impact on instream biota but also because they can impair the effectiveness of potable water supply treatment and increase its costs (Gadgil, 1998). In addition, fine sediments are a transport vector for hydrophobic contaminants (Babek et al., 2008; Taylor and Owens, 2009). This chapter provides 1) an overview of the effect that forestry generated fine sediment has on receiving stream biota and 2) an effective protocol for measuring fine sediment levels at forest road stream crossings. The routing and downstream accumulation of sediment from these stream crossing point sources is a management concern because it will affect stream biota and streambed composition at each of its temporary in-stream storage areas. This sedimentary cumulative watershed effect (CWE) is one of the most detrimental consequences of forest harvesting activities on a watershed. However, the CWE is difficult to assess because its effect is dependent upon the grain size being introduced, the number and size of streams that transport it, and the original sedimentary state of the streambed it encounters (Bunte and MacDonald, 1999). Further, while it may be possible to determine the change in fine sediment levels at a single point in the stream, it is difficult to determine which upstream land use activity instigated the change. Bunte and MacDonald (1999) suggest that to manage a watershed for cumulative sediment effects it is necessary to monitor for a minimum of 5 10 years pre-and-post harvesting because sediment transport is highly variable. However, this type of program is often considered cost prohibitive and of a longer reporting timeline than that required by many resource management programs.

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), Insufficient payload (model declined to judge)
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Bench or experimental · Consensus signal: none
GenreCandidate signal: Other · Consensus signal: none
Teacher disagreement score0.798
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 studies0.0000.000
Scholarly communication0.0000.000
Open science0.0000.000
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 head0.027
GPT teacher head0.275
Teacher spread0.249 · 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 designBench or experimental
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

Citations2
Published2011
Admission routes1
Has abstractyes

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