FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2024883299> ?p ?o ?g. }

• W2024883299 endingPage "1818" @default.
• W2024883299 startingPage "1807" @default.
• W2024883299 abstract "Analyses of the specific products of 35SO42− reduction measurements were made in marine sediments in Denmark. We injected tracer quantities of 35SO42− into cores, incubated the cores, and assayed for 35S-labelled acid volatile sulfides. Additionally, we assayed for 35S-labelled elemental sulfur by extraction with CS2, and for 35S-labelled pyrite by reduction with chromium (II). We separately determined that elemental sulfur which formed in situ and that which formed by oxidation during the acid distillation of acid volatile sulfides. In subtidal sediments in Limfjorden, 35S-labelled elemental sulfur and pyrite make up 14–32% of the reduced sulfur formed in short-term (0–48 hours) 35SO42− reduction experiments, at all depths studied (0–15 cm). Labelled elemental sulfur which formed in situ during the incubations at depths below 1 cm made up a fairly constant 5–11% of the total labelled reduced sulfur, from 0–1 cm, it made up 27%. An additional small amount (1–2% from 1–15 cm and 5% from 0–1 cm) of labelled elemental sulfur was formed during the acid-distillation step in our assay for labelled acid-volatile sulndes. Pyrite contained 4–13% of the total labelled reduced sulfur at all depths. Rates of sulfate reduction in Limfjorden were linear over the period 0–48 hours, and 35S-pyrite made up a nearly constant percentage of the 35S-labelled reduced sulfur formed over this time period. Estimates of sulfate reduction rates for Limfjorden which do not include elemental sulfur and pyrite as products are 19% too low. At Kysing Fjord, estimates of sulfate reduction which do not include elemental sulfur and pyrite are 24% to 32% too low. Thus, while previously published data on sulfate reduction in similar environments are probably low, they are not greatly in error." @default.
• W2024883299 created "2016-06-24" @default.
• W2024883299 creator A5025013215 @default.
• W2024883299 creator A5085453092 @default.
• W2024883299 date "1984-09-01" @default.
• W2024883299 modified "2023-10-09" @default.
• W2024883299 title "Formation of 35S-labelled elemental sulfur and pyrite in coastal marine sediments (Limfjorden and Kysing Fjord, Denmark) during short-term 35SO42? reduction measurements" @default.
• W2024883299 cites W1493164914 @default.
• W2024883299 cites W1586239332 @default.
• W2024883299 cites W1964901884 @default.
• W2024883299 cites W1987194686 @default.
• W2024883299 cites W1997628897 @default.
• W2024883299 cites W1997795848 @default.
• W2024883299 cites W2029474731 @default.
• W2024883299 cites W2030045843 @default.
• W2024883299 cites W2037544128 @default.
• W2024883299 cites W2041141455 @default.
• W2024883299 cites W2042994978 @default.
• W2024883299 cites W2054645658 @default.
• W2024883299 cites W2055209449 @default.
• W2024883299 cites W2069089882 @default.
• W2024883299 cites W2076795037 @default.
• W2024883299 cites W2078775604 @default.
• W2024883299 cites W2082250875 @default.
• W2024883299 cites W2084958576 @default.
• W2024883299 cites W2084961153 @default.
• W2024883299 cites W2090811283 @default.
• W2024883299 cites W2099501892 @default.
• W2024883299 cites W2117185933 @default.
• W2024883299 cites W2122056874 @default.
• W2024883299 cites W2126653649 @default.
• W2024883299 cites W2141697362 @default.
• W2024883299 cites W2155674861 @default.
• W2024883299 cites W2169202959 @default.
• W2024883299 cites W2170977957 @default.
• W2024883299 cites W2313312350 @default.
• W2024883299 cites W2321013126 @default.
• W2024883299 cites W2321712419 @default.
• W2024883299 doi "https://doi.org/10.1016/0016-7037(84)90034-6" @default.
• W2024883299 hasPublicationYear "1984" @default.
• W2024883299 type Work @default.
• W2024883299 sameAs 2024883299 @default.
• W2024883299 citedByCount "213" @default.
• W2024883299 countsByYear W20248832992012 @default.
• W2024883299 countsByYear W20248832992013 @default.
• W2024883299 countsByYear W20248832992014 @default.
• W2024883299 countsByYear W20248832992015 @default.
• W2024883299 countsByYear W20248832992016 @default.
• W2024883299 countsByYear W20248832992017 @default.
• W2024883299 countsByYear W20248832992018 @default.
• W2024883299 countsByYear W20248832992019 @default.
• W2024883299 countsByYear W20248832992020 @default.
• W2024883299 countsByYear W20248832992021 @default.
• W2024883299 countsByYear W20248832992022 @default.
• W2024883299 crossrefType "journal-article" @default.
• W2024883299 hasAuthorship W2024883299A5025013215 @default.
• W2024883299 hasAuthorship W2024883299A5085453092 @default.
• W2024883299 hasConcept C107872376 @default.
• W2024883299 hasConcept C178790620 @default.
• W2024883299 hasConcept C185592680 @default.
• W2024883299 hasConcept C199289684 @default.
• W2024883299 hasConcept C2776062231 @default.
• W2024883299 hasConcept C2778343803 @default.
• W2024883299 hasConcept C2780596425 @default.
• W2024883299 hasConcept C518881349 @default.
• W2024883299 hasConceptScore W2024883299C107872376 @default.
• W2024883299 hasConceptScore W2024883299C178790620 @default.
• W2024883299 hasConceptScore W2024883299C185592680 @default.
• W2024883299 hasConceptScore W2024883299C199289684 @default.
• W2024883299 hasConceptScore W2024883299C2776062231 @default.
• W2024883299 hasConceptScore W2024883299C2778343803 @default.
• W2024883299 hasConceptScore W2024883299C2780596425 @default.
• W2024883299 hasConceptScore W2024883299C518881349 @default.
• W2024883299 hasIssue "9" @default.
• W2024883299 hasLocation W20248832991 @default.
• W2024883299 hasOpenAccess W2024883299 @default.
• W2024883299 hasPrimaryLocation W20248832991 @default.
• W2024883299 hasRelatedWork W1972566244 @default.
• W2024883299 hasRelatedWork W2028359665 @default.
• W2024883299 hasRelatedWork W2029328233 @default.
• W2024883299 hasRelatedWork W2043515955 @default.
• W2024883299 hasRelatedWork W2045102079 @default.
• W2024883299 hasRelatedWork W2064129458 @default.
• W2024883299 hasRelatedWork W2066620874 @default.
• W2024883299 hasRelatedWork W2072844995 @default.
• W2024883299 hasRelatedWork W2075071049 @default.
• W2024883299 hasRelatedWork W4386775769 @default.
• W2024883299 hasVolume "48" @default.
• W2024883299 isParatext "false" @default.
• W2024883299 isRetracted "false" @default.
• W2024883299 magId "2024883299" @default.
• W2024883299 workType "article" @default.