FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2003962015> ?p ?o ?g. }

• W2003962015 endingPage "470" @default.
• W2003962015 startingPage "461" @default.
• W2003962015 abstract "Chemical and sulphur isotopic analyses are presented of fissure-waters and pore-waters in the deep confined zone of a dual porosity carbonate aquifer. Some of the fissure-waters show good evidence for bacterial sulphate reduction, with low concentrations of sulphide present which is strongly to moderately depleted in 34S relative to sulphate. The sulphur geochemistry is best interpreted as mixing between: (i) a reduced water with sulphide ∼60‰ depleted in 34S relative to sulphate; and (ii) a sulphate-rich water from up-dip in the aquifer. In addition, sulphide oxidation occurs where sufficiently oxidizing water is drawn in by abstractions. The large isotope fractionation factor associated with the sulphidic waters is probably the result of redox cycling of sulphur with little net reduction, rather than a true kinetic fractionation factor. By contrast, pore-waters in the “sulphate reducing zone” show little or no evidence for the effects of sulphate reduction, despite the fact that the pore-waters represent a significant reservoir of sulphate for reduction. Some pore-waters have been modified recognizably by diffusional exchange with the fissure-waters, but the aquifer matrix has not been colonized by sulphate reducing bacteria, probably because porethroats in the limestone are too small for bacteria to pass. Physical exclusion of bacteria from the aquifer matrix and limited diffusional exchange are likely to exert fundamental controls on bacterial redox processes in dual porosity aquifer systems and other systems with low permeability due to small pore interconnections." @default.
• W2003962015 created "2016-06-24" @default.
• W2003962015 creator A5009998695 @default.
• W2003962015 creator A5016698717 @default.
• W2003962015 creator A5027905158 @default.
• W2003962015 creator A5037656255 @default.
• W2003962015 creator A5045201846 @default.
• W2003962015 creator A5059687464 @default.
• W2003962015 date "2000-09-01" @default.
• W2003962015 modified "2023-09-27" @default.
• W2003962015 title "Controls on bacterial sulphate reduction in a dual porosity aquifer system: the Lincolnshire Limestone aquifer, England" @default.
• W2003962015 cites W1965324922 @default.
• W2003962015 cites W1987425824 @default.
• W2003962015 cites W2000256856 @default.
• W2003962015 cites W2001608739 @default.
• W2003962015 cites W2005121896 @default.
• W2003962015 cites W2010170309 @default.
• W2003962015 cites W2014124919 @default.
• W2003962015 cites W2014467701 @default.
• W2003962015 cites W2025037466 @default.
• W2003962015 cites W2038934923 @default.
• W2003962015 cites W2040101795 @default.
• W2003962015 cites W2050352449 @default.
• W2003962015 cites W2059016533 @default.
• W2003962015 cites W2061391409 @default.
• W2003962015 cites W2076520478 @default.
• W2003962015 cites W2079476794 @default.
• W2003962015 cites W2081779148 @default.
• W2003962015 cites W2106402447 @default.
• W2003962015 cites W2128504181 @default.
• W2003962015 cites W2151810171 @default.
• W2003962015 cites W2168610019 @default.
• W2003962015 doi "https://doi.org/10.1016/s0009-2541(00)00222-9" @default.
• W2003962015 hasPublicationYear "2000" @default.
• W2003962015 type Work @default.
• W2003962015 sameAs 2003962015 @default.
• W2003962015 citedByCount "49" @default.
• W2003962015 countsByYear W20039620152012 @default.
• W2003962015 countsByYear W20039620152013 @default.
• W2003962015 countsByYear W20039620152014 @default.
• W2003962015 countsByYear W20039620152016 @default.
• W2003962015 countsByYear W20039620152017 @default.
• W2003962015 countsByYear W20039620152018 @default.
• W2003962015 countsByYear W20039620152019 @default.
• W2003962015 countsByYear W20039620152020 @default.
• W2003962015 countsByYear W20039620152021 @default.
• W2003962015 crossrefType "journal-article" @default.
• W2003962015 hasAuthorship W2003962015A5009998695 @default.
• W2003962015 hasAuthorship W2003962015A5016698717 @default.
• W2003962015 hasAuthorship W2003962015A5027905158 @default.
• W2003962015 hasAuthorship W2003962015A5037656255 @default.
• W2003962015 hasAuthorship W2003962015A5045201846 @default.
• W2003962015 hasAuthorship W2003962015A5059687464 @default.
• W2003962015 hasConcept C102579867 @default.
• W2003962015 hasConcept C107872376 @default.
• W2003962015 hasConcept C127313418 @default.
• W2003962015 hasConcept C151730666 @default.
• W2003962015 hasConcept C156622251 @default.
• W2003962015 hasConcept C165205528 @default.
• W2003962015 hasConcept C17409809 @default.
• W2003962015 hasConcept C178790620 @default.
• W2003962015 hasConcept C179104552 @default.
• W2003962015 hasConcept C185592680 @default.
• W2003962015 hasConcept C187320778 @default.
• W2003962015 hasConcept C194356953 @default.
• W2003962015 hasConcept C199289684 @default.
• W2003962015 hasConcept C2776152364 @default.
• W2003962015 hasConcept C2780416900 @default.
• W2003962015 hasConcept C2780659211 @default.
• W2003962015 hasConcept C518881349 @default.
• W2003962015 hasConcept C523546767 @default.
• W2003962015 hasConcept C55904794 @default.
• W2003962015 hasConcept C6648577 @default.
• W2003962015 hasConcept C75622301 @default.
• W2003962015 hasConcept C76177295 @default.
• W2003962015 hasConceptScore W2003962015C102579867 @default.
• W2003962015 hasConceptScore W2003962015C107872376 @default.
• W2003962015 hasConceptScore W2003962015C127313418 @default.
• W2003962015 hasConceptScore W2003962015C151730666 @default.
• W2003962015 hasConceptScore W2003962015C156622251 @default.
• W2003962015 hasConceptScore W2003962015C165205528 @default.
• W2003962015 hasConceptScore W2003962015C17409809 @default.
• W2003962015 hasConceptScore W2003962015C178790620 @default.
• W2003962015 hasConceptScore W2003962015C179104552 @default.
• W2003962015 hasConceptScore W2003962015C185592680 @default.
• W2003962015 hasConceptScore W2003962015C187320778 @default.
• W2003962015 hasConceptScore W2003962015C194356953 @default.
• W2003962015 hasConceptScore W2003962015C199289684 @default.
• W2003962015 hasConceptScore W2003962015C2776152364 @default.
• W2003962015 hasConceptScore W2003962015C2780416900 @default.
• W2003962015 hasConceptScore W2003962015C2780659211 @default.
• W2003962015 hasConceptScore W2003962015C518881349 @default.
• W2003962015 hasConceptScore W2003962015C523546767 @default.
• W2003962015 hasConceptScore W2003962015C55904794 @default.
• W2003962015 hasConceptScore W2003962015C6648577 @default.
• W2003962015 hasConceptScore W2003962015C75622301 @default.
• W2003962015 hasConceptScore W2003962015C76177295 @default.
• W2003962015 hasIssue "3-4" @default.

• next