FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2024808883> ?p ?o ?g. }

• W2024808883 endingPage "3154" @default.
• W2024808883 startingPage "3146" @default.
• W2024808883 abstract "Water source and lake landscape position can strongly influence the physico-chemical characteristics of flowing waters over space and time. We examined the physico-chemical heterogeneity in surface waters of an alpine stream-lake network (>2600 m a.s.l.) in Switzerland. The catchment comprises two basins interspersed with 26 cirque lakes. The larger lakes in each basin are interconnected by streams that converge in a lowermost lake with an outlet stream. The north basin is primarily fed by precipitation and groundwater, whereas the south basin is fed mostly by glacial melt from rock glaciers. Surface flow of the entire channel network contracted by ∼60% in early autumn, when snowmelt runoff ceased and cold temperatures reduced glacial outputs, particularly in the south basin. Average water temperatures were ∼4 °C cooler in the south basin, and temperatures increased by about 4–6 °C along the longitudinal gradient within each basin. Although overall water conductivity was low (<27 µS cm−1) because of bedrock geology (ortho-gneiss), the south basin had two times higher conductivity values than the north basin. Phosphate-phosphorus levels were below analytical detection limits, but particulate phosphorus was about four times higher in the north basin (seasonal average: 9 µg l−1) than in the south basin (seasonal average: 2 µg l−1). Dissolved nitrogen constituents were around two times higher in the south basin than in the north basin, with highest values averaging > 300 µg l−1 (nitrite + nitrate-nitrogen), whereas particulate nitrogen was approximately nine times greater in the north basin (seasonal average: 97 µg l−1) than in the south basin (seasonal average: 12 µg l−1). Total inorganic carbon was low (usually <0·8 mg l−1), silica was sufficient for algal growth, and particulate organic carbon was 4·5 times higher in the north basin (average: 0·9 mg l−1) than in the south basin (average: 0·2 mg l−1). North-basin streams showed strong seasonality in turbidity, particulate-nitrogen and -phosphorus, and particulate organic carbon, whereas strong seasonality in south-basin streams was observed in conductivity and dissolved nitrogen. Lake position influenced the seasonal dynamics in stream temperatures and nutrients, particularly in the groundwater/precipitation-fed north-basin network. Copyright © 2007 John Wiley & Sons, Ltd." @default.
• W2024808883 created "2016-06-24" @default.
• W2024808883 creator A5017502398 @default.
• W2024808883 creator A5038489971 @default.
• W2024808883 date "2007-01-01" @default.
• W2024808883 modified "2023-10-07" @default.
• W2024808883 title "Hydrological heterogeneity of an alpine stream–lake network in Switzerland" @default.
• W2024808883 cites W1515714986 @default.
• W2024808883 cites W1855584014 @default.
• W2024808883 cites W1964337735 @default.
• W2024808883 cites W1967455176 @default.
• W2024808883 cites W1970400271 @default.
• W2024808883 cites W1982371804 @default.
• W2024808883 cites W1987254762 @default.
• W2024808883 cites W2005930000 @default.
• W2024808883 cites W2007409849 @default.
• W2024808883 cites W2018809356 @default.
• W2024808883 cites W2040235702 @default.
• W2024808883 cites W2041997539 @default.
• W2024808883 cites W2056373757 @default.
• W2024808883 cites W2068960764 @default.
• W2024808883 cites W2083584049 @default.
• W2024808883 cites W2087320225 @default.
• W2024808883 cites W2116544104 @default.
• W2024808883 cites W2118687706 @default.
• W2024808883 cites W2119515210 @default.
• W2024808883 cites W2123616691 @default.
• W2024808883 cites W2133392983 @default.
• W2024808883 cites W2134229141 @default.
• W2024808883 cites W2144832659 @default.
• W2024808883 cites W2159194951 @default.
• W2024808883 cites W2160914961 @default.
• W2024808883 cites W2166703291 @default.
• W2024808883 cites W2172447049 @default.
• W2024808883 cites W2302631465 @default.
• W2024808883 cites W2315543615 @default.
• W2024808883 cites W2320766169 @default.
• W2024808883 cites W2473921138 @default.
• W2024808883 cites W2504072677 @default.
• W2024808883 cites W3012012913 @default.
• W2024808883 cites W3088245905 @default.
• W2024808883 doi "https://doi.org/10.1002/hyp.6536" @default.
• W2024808883 hasPublicationYear "2007" @default.
• W2024808883 type Work @default.
• W2024808883 sameAs 2024808883 @default.
• W2024808883 citedByCount "41" @default.
• W2024808883 countsByYear W20248088832012 @default.
• W2024808883 countsByYear W20248088832013 @default.
• W2024808883 countsByYear W20248088832015 @default.
• W2024808883 countsByYear W20248088832017 @default.
• W2024808883 countsByYear W20248088832019 @default.
• W2024808883 countsByYear W20248088832020 @default.
• W2024808883 countsByYear W20248088832021 @default.
• W2024808883 countsByYear W20248088832022 @default.
• W2024808883 countsByYear W20248088832023 @default.
• W2024808883 crossrefType "journal-article" @default.
• W2024808883 hasAuthorship W2024808883A5017502398 @default.
• W2024808883 hasAuthorship W2024808883A5038489971 @default.
• W2024808883 hasConcept C100834320 @default.
• W2024808883 hasConcept C109007969 @default.
• W2024808883 hasConcept C114793014 @default.
• W2024808883 hasConcept C126645576 @default.
• W2024808883 hasConcept C127313418 @default.
• W2024808883 hasConcept C137527640 @default.
• W2024808883 hasConcept C15739521 @default.
• W2024808883 hasConcept C187320778 @default.
• W2024808883 hasConcept C18903297 @default.
• W2024808883 hasConcept C197046000 @default.
• W2024808883 hasConcept C205649164 @default.
• W2024808883 hasConcept C207318512 @default.
• W2024808883 hasConcept C31258907 @default.
• W2024808883 hasConcept C39432304 @default.
• W2024808883 hasConcept C41008148 @default.
• W2024808883 hasConcept C42090638 @default.
• W2024808883 hasConcept C50477045 @default.
• W2024808883 hasConcept C58640448 @default.
• W2024808883 hasConcept C64649846 @default.
• W2024808883 hasConcept C76886044 @default.
• W2024808883 hasConcept C8625798 @default.
• W2024808883 hasConcept C86803240 @default.
• W2024808883 hasConcept C87717796 @default.
• W2024808883 hasConceptScore W2024808883C100834320 @default.
• W2024808883 hasConceptScore W2024808883C109007969 @default.
• W2024808883 hasConceptScore W2024808883C114793014 @default.
• W2024808883 hasConceptScore W2024808883C126645576 @default.
• W2024808883 hasConceptScore W2024808883C127313418 @default.
• W2024808883 hasConceptScore W2024808883C137527640 @default.
• W2024808883 hasConceptScore W2024808883C15739521 @default.
• W2024808883 hasConceptScore W2024808883C187320778 @default.
• W2024808883 hasConceptScore W2024808883C18903297 @default.
• W2024808883 hasConceptScore W2024808883C197046000 @default.
• W2024808883 hasConceptScore W2024808883C205649164 @default.
• W2024808883 hasConceptScore W2024808883C207318512 @default.
• W2024808883 hasConceptScore W2024808883C31258907 @default.
• W2024808883 hasConceptScore W2024808883C39432304 @default.
• W2024808883 hasConceptScore W2024808883C41008148 @default.
• W2024808883 hasConceptScore W2024808883C42090638 @default.
• W2024808883 hasConceptScore W2024808883C50477045 @default.

• next