FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2000752316> ?p ?o ?g. }

• W2000752316 endingPage "79" @default.
• W2000752316 startingPage "69" @default.
• W2000752316 abstract "Summary Soil solution was collected to identify seasonal trends in its chemistry and to examine relationships between the concentrations of ions and variables that may control them. Samples were collected fortnightly at 10 cm and 50 cm depth in a blanket peat soil at Moor House–Upper Teesdale National Nature Reserve in the northern Pennine uplands of England. Dissolved organic carbon at 10 cm peaked each summer and correlated most strongly with temperature. At both depths Na + and Cl – were the dominant ions, reflecting the oceanic climate. Over the 3‐year sampling period, concentrations of the principal anions and cations at 10 cm varied little except during the autumns of 1994 and 1995 following unusually dry summers. At these times concentrations of SO 4 2– ‐S increased from < 3 μmol to a maximum of 430 μmol and were balanced by smaller increases in Na + , Mg 2+ , Ca 2+ and H + . The SO 4 2– concentration at 10 cm was most strongly correlated with depth to the water Table 3 weeks prior to sampling. At 50 cm depth in the peat a small increase in SO 4 2– occurred only during the autumn of 1995, and the concentration of SO 4 2– at this depth correlated most strongly with that at 10 cm. At neither depth were there any strong correlations with deposition. The increase in H + concentration associated with the peak in SO 4 2– at 10 cm depth represents a fall in pH from usual values around 4.2 to 3.5. Deposition flux of ions in bulk precipitation at Moor House from weekly samplings 1994 to 1996 in kg ha −1 year −1 . The UK flux is derived from 32 sites of the United Kingdom Precipitation Composition Monitoring Network 1992 to 1994 and the standard deviation (SD) relates to the variation between these sites ( Review Group on Acid Rain, 1997 ) Moor House flux UK flux UK SD H + 0.31 0.26 0.10 Ca 2+ 4.07 3.58 1.86 Mg 2+ 3.37 3.62 2.62 K + 1.54 Fe 2+ 0.73 Al 3+ 0.44 Na + 29.32 25.77 19.27 Cl – 51.14 45.96 32.39 NO 3 – ‐N 4.01 3.20 1.05 NH 4 + ‐N 4.85 3.63 1.74 SO 4 2– ‐S 8.98 7.98 3.09 PO 4 3– ‐P 0.01" @default.
• W2000752316 created "2016-06-24" @default.
• W2000752316 creator A5003119066 @default.
• W2000752316 creator A5003355002 @default.
• W2000752316 creator A5043136882 @default.
• W2000752316 creator A5062159221 @default.
• W2000752316 date "2001-03-01" @default.
• W2000752316 modified "2023-10-18" @default.
• W2000752316 title "Ionic concentrations in a blanket peat bog in northern England and correlations with deposition and climate variables" @default.
• W2000752316 cites W106507986 @default.
• W2000752316 cites W1986121817 @default.
• W2000752316 cites W1987608572 @default.
• W2000752316 cites W2013279517 @default.
• W2000752316 cites W2016252560 @default.
• W2000752316 cites W2041639555 @default.
• W2000752316 cites W2061394944 @default.
• W2000752316 cites W2067794143 @default.
• W2000752316 cites W2086787423 @default.
• W2000752316 cites W2090963808 @default.
• W2000752316 cites W2317110372 @default.
• W2000752316 cites W2320820701 @default.
• W2000752316 cites W2322722878 @default.
• W2000752316 cites W2325397412 @default.
• W2000752316 cites W2335204238 @default.
• W2000752316 cites W4253469695 @default.
• W2000752316 doi "https://doi.org/10.1046/j.1365-2389.2001.t01-1-00350.x" @default.
• W2000752316 hasPublicationYear "2001" @default.
• W2000752316 type Work @default.
• W2000752316 sameAs 2000752316 @default.
• W2000752316 citedByCount "81" @default.
• W2000752316 countsByYear W20007523162012 @default.
• W2000752316 countsByYear W20007523162013 @default.
• W2000752316 countsByYear W20007523162014 @default.
• W2000752316 countsByYear W20007523162015 @default.
• W2000752316 countsByYear W20007523162016 @default.
• W2000752316 countsByYear W20007523162017 @default.
• W2000752316 countsByYear W20007523162018 @default.
• W2000752316 countsByYear W20007523162020 @default.
• W2000752316 countsByYear W20007523162021 @default.
• W2000752316 countsByYear W20007523162022 @default.
• W2000752316 crossrefType "journal-article" @default.
• W2000752316 hasAuthorship W2000752316A5003119066 @default.
• W2000752316 hasAuthorship W2000752316A5003355002 @default.
• W2000752316 hasAuthorship W2000752316A5043136882 @default.
• W2000752316 hasAuthorship W2000752316A5062159221 @default.
• W2000752316 hasConcept C104779481 @default.
• W2000752316 hasConcept C107872376 @default.
• W2000752316 hasConcept C109007969 @default.
• W2000752316 hasConcept C114793014 @default.
• W2000752316 hasConcept C122284674 @default.
• W2000752316 hasConcept C127313418 @default.
• W2000752316 hasConcept C140205800 @default.
• W2000752316 hasConcept C140793950 @default.
• W2000752316 hasConcept C158787203 @default.
• W2000752316 hasConcept C159985019 @default.
• W2000752316 hasConcept C178790620 @default.
• W2000752316 hasConcept C185592680 @default.
• W2000752316 hasConcept C187320778 @default.
• W2000752316 hasConcept C18903297 @default.
• W2000752316 hasConcept C192562407 @default.
• W2000752316 hasConcept C36574619 @default.
• W2000752316 hasConcept C39432304 @default.
• W2000752316 hasConcept C39769621 @default.
• W2000752316 hasConcept C53657456 @default.
• W2000752316 hasConcept C64297162 @default.
• W2000752316 hasConcept C68709404 @default.
• W2000752316 hasConcept C76177295 @default.
• W2000752316 hasConcept C76886044 @default.
• W2000752316 hasConcept C86803240 @default.
• W2000752316 hasConcept C91586092 @default.
• W2000752316 hasConceptScore W2000752316C104779481 @default.
• W2000752316 hasConceptScore W2000752316C107872376 @default.
• W2000752316 hasConceptScore W2000752316C109007969 @default.
• W2000752316 hasConceptScore W2000752316C114793014 @default.
• W2000752316 hasConceptScore W2000752316C122284674 @default.
• W2000752316 hasConceptScore W2000752316C127313418 @default.
• W2000752316 hasConceptScore W2000752316C140205800 @default.
• W2000752316 hasConceptScore W2000752316C140793950 @default.
• W2000752316 hasConceptScore W2000752316C158787203 @default.
• W2000752316 hasConceptScore W2000752316C159985019 @default.
• W2000752316 hasConceptScore W2000752316C178790620 @default.
• W2000752316 hasConceptScore W2000752316C185592680 @default.
• W2000752316 hasConceptScore W2000752316C187320778 @default.
• W2000752316 hasConceptScore W2000752316C18903297 @default.
• W2000752316 hasConceptScore W2000752316C192562407 @default.
• W2000752316 hasConceptScore W2000752316C36574619 @default.
• W2000752316 hasConceptScore W2000752316C39432304 @default.
• W2000752316 hasConceptScore W2000752316C39769621 @default.
• W2000752316 hasConceptScore W2000752316C53657456 @default.
• W2000752316 hasConceptScore W2000752316C64297162 @default.
• W2000752316 hasConceptScore W2000752316C68709404 @default.
• W2000752316 hasConceptScore W2000752316C76177295 @default.
• W2000752316 hasConceptScore W2000752316C76886044 @default.
• W2000752316 hasConceptScore W2000752316C86803240 @default.
• W2000752316 hasConceptScore W2000752316C91586092 @default.
• W2000752316 hasIssue "1" @default.
• W2000752316 hasLocation W20007523161 @default.
• W2000752316 hasOpenAccess W2000752316 @default.

• next