FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1594118889> ?p ?o ?g. }

• W1594118889 abstract "Abstract Watershed characteristics influence the concentrations of dissolved organic carbon (DOC) that affects the levels, fate, partitioning, bioavailability, and toxicity of dissolved metals in aquatic ecosystems. Despite increasing interest in black shales research, there are limited data relating influence of bedrock type upon DOC and dissolved metals in streams whose watersheds are dominated by black shales. Four streams in North-Central Arkansas, USA, were selected for study, three of which (Trace Creek, Begley Creek, and Cove Creek) drain black shales-dominated watersheds. A fourth nearby stream (Mill Creek) that flows over a geologically distinct limestone bedrock, was selected as a reference site to allow comparisons between these watersheds and the assessment of the role of bedrock lithology on DOC and metal concentrations. Spatial and temporal variations in DOC and dissolved metals among stream sites were determined. Streams draining black shales had significantly higher conductivity, and lower pH than the stream draining limestone. Dissolved metal concentrations at all sites were highest in June 2003 and lowest in September 2003, which coincided with a stormflow and a baseflow, respectively. The concentrations of DOC and metals (e.g. Cd, Cu, Hg, Ni, Pb, and Zn) in water collected from Trace, Begley, and Cove creeks were significantly higher than those of Mill Creek. Metals in streams draining black shales whose concentrations approached or exceeded US EPA's surface water criteria included Cr, Cu, Hg, Pb, and Se. A linear regression analysis of DOC with discharge as the predictor variable showed that variations in DOC concentrations were strongly explained by stream discharge with r 2 -values ranged from 0.85 to 0.95, whereas DOC was inversely related to conductivity ( r 2 =0.47–0.89). The study also revealed that bedrock type was a significant predictor of the observed spatial variations in DOC. Streams draining black shale watersheds transported significantly higher ( p" @default.
• W1594118889 created "2016-06-24" @default.
• W1594118889 creator A5004216285 @default.
• W1594118889 creator A5012267584 @default.
• W1594118889 creator A5013265176 @default.
• W1594118889 date "2007-01-01" @default.
• W1594118889 modified "2023-10-14" @default.
• W1594118889 title "Chapter 12 Association of dissolved organic carbon with stream discharge and dissolved metals concentrations in black shale-draining streams" @default.
• W1594118889 cites W107513027 @default.
• W1594118889 cites W1220488938 @default.
• W1594118889 cites W1481249400 @default.
• W1594118889 cites W187511998 @default.
• W1594118889 cites W1926880619 @default.
• W1594118889 cites W1966418918 @default.
• W1594118889 cites W1966699296 @default.
• W1594118889 cites W1967995678 @default.
• W1594118889 cites W1968533694 @default.
• W1594118889 cites W1975010138 @default.
• W1594118889 cites W1978804839 @default.
• W1594118889 cites W1980916768 @default.
• W1594118889 cites W1985702586 @default.
• W1594118889 cites W1987254762 @default.
• W1594118889 cites W1990475289 @default.
• W1594118889 cites W1993971399 @default.
• W1594118889 cites W1998888559 @default.
• W1594118889 cites W2000471560 @default.
• W1594118889 cites W2004481070 @default.
• W1594118889 cites W2005680072 @default.
• W1594118889 cites W2006804649 @default.
• W1594118889 cites W2010269395 @default.
• W1594118889 cites W2014517864 @default.
• W1594118889 cites W2025350765 @default.
• W1594118889 cites W2031740823 @default.
• W1594118889 cites W2036019693 @default.
• W1594118889 cites W2042415195 @default.
• W1594118889 cites W2045407132 @default.
• W1594118889 cites W2053868655 @default.
• W1594118889 cites W2064877977 @default.
• W1594118889 cites W2070020744 @default.
• W1594118889 cites W2075402358 @default.
• W1594118889 cites W2083977666 @default.
• W1594118889 cites W2086944318 @default.
• W1594118889 cites W2087231087 @default.
• W1594118889 cites W2090938025 @default.
• W1594118889 cites W2095549235 @default.
• W1594118889 cites W2097924319 @default.
• W1594118889 cites W2099775165 @default.
• W1594118889 cites W2113735437 @default.
• W1594118889 cites W2136899643 @default.
• W1594118889 cites W2137977740 @default.
• W1594118889 cites W2139159290 @default.
• W1594118889 cites W2147380432 @default.
• W1594118889 cites W2147396432 @default.
• W1594118889 cites W2149701393 @default.
• W1594118889 cites W2150734977 @default.
• W1594118889 cites W2155990140 @default.
• W1594118889 cites W2156811420 @default.
• W1594118889 cites W2159978394 @default.
• W1594118889 cites W2487667528 @default.
• W1594118889 cites W2504717088 @default.
• W1594118889 cites W2512244289 @default.
• W1594118889 cites W2733270882 @default.
• W1594118889 cites W2748461560 @default.
• W1594118889 cites W586358893 @default.
• W1594118889 cites W7524155 @default.
• W1594118889 cites W145453840 @default.
• W1594118889 cites W2108271102 @default.
• W1594118889 cites W2121697486 @default.
• W1594118889 cites W2259110623 @default.
• W1594118889 doi "https://doi.org/10.1016/s1474-8177(07)05012-7" @default.
• W1594118889 hasPublicationYear "2007" @default.
• W1594118889 type Work @default.
• W1594118889 sameAs 1594118889 @default.
• W1594118889 citedByCount "2" @default.
• W1594118889 countsByYear W15941188892020 @default.
• W1594118889 crossrefType "book-chapter" @default.
• W1594118889 hasAuthorship W1594118889A5004216285 @default.
• W1594118889 hasAuthorship W1594118889A5012267584 @default.
• W1594118889 hasAuthorship W1594118889A5013265176 @default.
• W1594118889 hasConcept C107872376 @default.
• W1594118889 hasConcept C114793014 @default.
• W1594118889 hasConcept C127313418 @default.
• W1594118889 hasConcept C137527640 @default.
• W1594118889 hasConcept C158787203 @default.
• W1594118889 hasConcept C168074166 @default.
• W1594118889 hasConcept C178790620 @default.
• W1594118889 hasConcept C185592680 @default.
• W1594118889 hasConcept C187320778 @default.
• W1594118889 hasConcept C2778566039 @default.
• W1594118889 hasConcept C2816523 @default.
• W1594118889 hasConcept C31258907 @default.
• W1594118889 hasConcept C36574619 @default.
• W1594118889 hasConcept C39432304 @default.
• W1594118889 hasConcept C41008148 @default.
• W1594118889 hasConcept C42090638 @default.
• W1594118889 hasConcept C544153396 @default.
• W1594118889 hasConcept C76886044 @default.
• W1594118889 hasConceptScore W1594118889C107872376 @default.
• W1594118889 hasConceptScore W1594118889C114793014 @default.
• W1594118889 hasConceptScore W1594118889C127313418 @default.

• next