FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4224133073> ?p ?o ?g. }

• W4224133073 abstract "Catchment hydrologists have long puzzled over the question: How can catchments rapidly generate storm flows and pulses of solutes in response to storm events? Conceptual models viewing catchments as composed of discrete source areas generating flow at unique time scales and with unique chemical characteristics have been used to explain the observed changes in flow and water chemistry. Surprisingly, those conceptual models usually do not treat the stream channel as one of the potential source areas. Here, we propose the channel-source hypothesis in which the stream itself should be considered as a potential source with the same rigour as other contributing areas. We pose this in the spirit of the scientific use of the word: a hypothesis is not a proven idea but rather a provisional supposition serving as the basis for further study. We suggest that the channel should be considered as a potential source for dissolved organic carbon (DOC). Channels store substantial amounts of organic matter, and stream ecologists have long studied stream carbon cycling. From those studies, we know that leaching and decomposition can generate DOC from particulate organic carbon (POC). Further, POC is stored in channel ‘dead-zones’—regions of low flow velocity - that can be activated as flow velocity increases, thus releasing accumulated DOC during storms. All catchments are different; there is no reason to assume that channel sources are always important, in every catchment, in every storm. Thus, the channel-source hypothesis does not replace existing conceptual models. Instead, it adds another potential mechanism that may explain DOC dynamics observed in streams. The channel-source hypothesis has substantial implications for catchment studies examining sources of DOC in stream water or using DOC as a tracer to determine the locations of, and proportional contributions of, different source areas for streamflow generation." @default.
• W4224133073 created "2022-04-20" @default.
• W4224133073 creator A5029681358 @default.
• W4224133073 creator A5072370658 @default.
• W4224133073 date "2022-05-01" @default.
• W4224133073 modified "2023-10-12" @default.
• W4224133073 title "The channel‐source hypothesis: Empirical evidence for <scp>in‐channel</scp> sourcing of dissolved organic carbon to explain hysteresis in a headwater mountain stream" @default.
• W4224133073 cites W146626679 @default.
• W4224133073 cites W1489673564 @default.
• W4224133073 cites W1503982519 @default.
• W4224133073 cites W1504735445 @default.
• W4224133073 cites W1576034684 @default.
• W4224133073 cites W1579208789 @default.
• W4224133073 cites W1671483852 @default.
• W4224133073 cites W175157384 @default.
• W4224133073 cites W1930996030 @default.
• W4224133073 cites W1967952455 @default.
• W4224133073 cites W1980433964 @default.
• W4224133073 cites W1987254762 @default.
• W4224133073 cites W1989951096 @default.
• W4224133073 cites W1998250489 @default.
• W4224133073 cites W2007769838 @default.
• W4224133073 cites W2022147869 @default.
• W4224133073 cites W2029587925 @default.
• W4224133073 cites W2029786079 @default.
• W4224133073 cites W2030312177 @default.
• W4224133073 cites W2033794830 @default.
• W4224133073 cites W2052298702 @default.
• W4224133073 cites W2056807694 @default.
• W4224133073 cites W2058185303 @default.
• W4224133073 cites W2066004884 @default.
• W4224133073 cites W2067782836 @default.
• W4224133073 cites W2077038928 @default.
• W4224133073 cites W2096463122 @default.
• W4224133073 cites W2097378496 @default.
• W4224133073 cites W2099748645 @default.
• W4224133073 cites W2113916731 @default.
• W4224133073 cites W2116544104 @default.
• W4224133073 cites W2122203956 @default.
• W4224133073 cites W2135629858 @default.
• W4224133073 cites W2140301216 @default.
• W4224133073 cites W2141924068 @default.
• W4224133073 cites W2143359154 @default.
• W4224133073 cites W2151526862 @default.
• W4224133073 cites W2151650373 @default.
• W4224133073 cites W2151663063 @default.
• W4224133073 cites W2155097344 @default.
• W4224133073 cites W2164540456 @default.
• W4224133073 cites W2165964458 @default.
• W4224133073 cites W2342243088 @default.
• W4224133073 cites W2344106828 @default.
• W4224133073 cites W2530622686 @default.
• W4224133073 cites W2584517279 @default.
• W4224133073 cites W2608239887 @default.
• W4224133073 cites W2611269708 @default.
• W4224133073 cites W2793471833 @default.
• W4224133073 cites W3018782875 @default.
• W4224133073 cites W3157792744 @default.
• W4224133073 cites W4211208946 @default.
• W4224133073 doi "https://doi.org/10.1002/hyp.14570" @default.
• W4224133073 hasPublicationYear "2022" @default.
• W4224133073 type Work @default.
• W4224133073 citedByCount "7" @default.
• W4224133073 countsByYear W42241330732022 @default.
• W4224133073 countsByYear W42241330732023 @default.
• W4224133073 crossrefType "journal-article" @default.
• W4224133073 hasAuthorship W4224133073A5029681358 @default.
• W4224133073 hasAuthorship W4224133073A5072370658 @default.
• W4224133073 hasBestOaLocation W42241330731 @default.
• W4224133073 hasConcept C105306849 @default.
• W4224133073 hasConcept C110872660 @default.
• W4224133073 hasConcept C111368507 @default.
• W4224133073 hasConcept C126645576 @default.
• W4224133073 hasConcept C127162648 @default.
• W4224133073 hasConcept C127313418 @default.
• W4224133073 hasConcept C187320778 @default.
• W4224133073 hasConcept C18903297 @default.
• W4224133073 hasConcept C205649164 @default.
• W4224133073 hasConcept C31258907 @default.
• W4224133073 hasConcept C36574619 @default.
• W4224133073 hasConcept C39432304 @default.
• W4224133073 hasConcept C41008148 @default.
• W4224133073 hasConcept C42090638 @default.
• W4224133073 hasConcept C58640448 @default.
• W4224133073 hasConcept C6939412 @default.
• W4224133073 hasConcept C76886044 @default.
• W4224133073 hasConcept C86803240 @default.
• W4224133073 hasConceptScore W4224133073C105306849 @default.
• W4224133073 hasConceptScore W4224133073C110872660 @default.
• W4224133073 hasConceptScore W4224133073C111368507 @default.
• W4224133073 hasConceptScore W4224133073C126645576 @default.
• W4224133073 hasConceptScore W4224133073C127162648 @default.
• W4224133073 hasConceptScore W4224133073C127313418 @default.
• W4224133073 hasConceptScore W4224133073C187320778 @default.
• W4224133073 hasConceptScore W4224133073C18903297 @default.
• W4224133073 hasConceptScore W4224133073C205649164 @default.
• W4224133073 hasConceptScore W4224133073C31258907 @default.
• W4224133073 hasConceptScore W4224133073C36574619 @default.
• W4224133073 hasConceptScore W4224133073C39432304 @default.
• W4224133073 hasConceptScore W4224133073C41008148 @default.

• next