FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2022758813> ?p ?o ?g. }

• W2022758813 endingPage "179" @default.
• W2022758813 startingPage "167" @default.
• W2022758813 abstract "This study is concerned with the geochemical behavior of Cu, Zn, As, Mo, Ba, La and Ce under the reducing conditions of a bank infiltration system. To identify and interpret individual processes laboratory experiments were performed on columns containing sandy sediments of an anoxic pleistocene aquifer from the Ruhr valley (western Germany). The flow rate being the key variable was varied from 0.21 to 0.46 and 0.82 m/d (meters per day), whereas the concentration of the reducing agent (acetate) remained constant. A second experiment lasting 80 weeks was carried out at a flow rate of 0.80 m/d, in order to characterize interactions between the pore water and solid phase. The results of these experiments show that the geochemistry of the trace elements involved can be explained to a large extent by the major redox processes of manganese, iron and sulfate turnover. The trace elements As, Mo, Ce and La were released into the pore water as a result of the reduction of Mn- and Fe-(hydr)oxides within the zone of major redox processes. Cu and Zn were removed from the infiltrating water within the first centimeters of the column by sulfide (co)precipitation, whereas the mobility of Mo was controlled by sulfidic fixation further down the flow path. As a result of the decreasing S2−-concentrations along the flow path, dissolved As(III) was re-oxidized (EH>− 250 mV) and precipitated as As(V) in a barium–arsenate-phase." @default.
• W2022758813 created "2016-06-24" @default.
• W2022758813 creator A5057914911 @default.
• W2022758813 creator A5072496107 @default.
• W2022758813 creator A5083015227 @default.
• W2022758813 creator A5020982070 @default.
• W2022758813 date "2001-11-01" @default.
• W2022758813 modified "2023-09-27" @default.
• W2022758813 title "The influence of redox processes on trace element mobility in a sandy aquifer—an experimental approach" @default.
• W2022758813 cites W140231629 @default.
• W2022758813 cites W1565745832 @default.
• W2022758813 cites W1970520523 @default.
• W2022758813 cites W1979124271 @default.
• W2022758813 cites W1998292078 @default.
• W2022758813 cites W2011020318 @default.
• W2022758813 cites W2012027509 @default.
• W2022758813 cites W2018212785 @default.
• W2022758813 cites W2023753492 @default.
• W2022758813 cites W2026575600 @default.
• W2022758813 cites W2028594681 @default.
• W2022758813 cites W2029997922 @default.
• W2022758813 cites W2035803088 @default.
• W2022758813 cites W2035953899 @default.
• W2022758813 cites W2039407536 @default.
• W2022758813 cites W2043506634 @default.
• W2022758813 cites W2050892975 @default.
• W2022758813 cites W2066102294 @default.
• W2022758813 cites W2066200707 @default.
• W2022758813 cites W2076663769 @default.
• W2022758813 cites W2081706904 @default.
• W2022758813 cites W2091794361 @default.
• W2022758813 cites W2163426744 @default.
• W2022758813 cites W506294680 @default.
• W2022758813 doi "https://doi.org/10.1016/s0375-6742(01)00195-9" @default.
• W2022758813 hasPublicationYear "2001" @default.
• W2022758813 type Work @default.
• W2022758813 sameAs 2022758813 @default.
• W2022758813 citedByCount "27" @default.
• W2022758813 countsByYear W20227588132012 @default.
• W2022758813 countsByYear W20227588132013 @default.
• W2022758813 countsByYear W20227588132014 @default.
• W2022758813 countsByYear W20227588132015 @default.
• W2022758813 countsByYear W20227588132016 @default.
• W2022758813 countsByYear W20227588132017 @default.
• W2022758813 countsByYear W20227588132018 @default.
• W2022758813 countsByYear W20227588132022 @default.
• W2022758813 crossrefType "journal-article" @default.
• W2022758813 hasAuthorship W2022758813A5020982070 @default.
• W2022758813 hasAuthorship W2022758813A5057914911 @default.
• W2022758813 hasAuthorship W2022758813A5072496107 @default.
• W2022758813 hasAuthorship W2022758813A5083015227 @default.
• W2022758813 hasConcept C107872376 @default.
• W2022758813 hasConcept C108970007 @default.
• W2022758813 hasConcept C114614502 @default.
• W2022758813 hasConcept C127313418 @default.
• W2022758813 hasConcept C17409809 @default.
• W2022758813 hasConcept C178790620 @default.
• W2022758813 hasConcept C179104552 @default.
• W2022758813 hasConcept C185592680 @default.
• W2022758813 hasConcept C187320778 @default.
• W2022758813 hasConcept C199289684 @default.
• W2022758813 hasConcept C2778343803 @default.
• W2022758813 hasConcept C2780596425 @default.
• W2022758813 hasConcept C33923547 @default.
• W2022758813 hasConcept C34682378 @default.
• W2022758813 hasConcept C528890316 @default.
• W2022758813 hasConcept C55904794 @default.
• W2022758813 hasConcept C75622301 @default.
• W2022758813 hasConcept C76177295 @default.
• W2022758813 hasConcept C9930424 @default.
• W2022758813 hasConceptScore W2022758813C107872376 @default.
• W2022758813 hasConceptScore W2022758813C108970007 @default.
• W2022758813 hasConceptScore W2022758813C114614502 @default.
• W2022758813 hasConceptScore W2022758813C127313418 @default.
• W2022758813 hasConceptScore W2022758813C17409809 @default.
• W2022758813 hasConceptScore W2022758813C178790620 @default.
• W2022758813 hasConceptScore W2022758813C179104552 @default.
• W2022758813 hasConceptScore W2022758813C185592680 @default.
• W2022758813 hasConceptScore W2022758813C187320778 @default.
• W2022758813 hasConceptScore W2022758813C199289684 @default.
• W2022758813 hasConceptScore W2022758813C2778343803 @default.
• W2022758813 hasConceptScore W2022758813C2780596425 @default.
• W2022758813 hasConceptScore W2022758813C33923547 @default.
• W2022758813 hasConceptScore W2022758813C34682378 @default.
• W2022758813 hasConceptScore W2022758813C528890316 @default.
• W2022758813 hasConceptScore W2022758813C55904794 @default.
• W2022758813 hasConceptScore W2022758813C75622301 @default.
• W2022758813 hasConceptScore W2022758813C76177295 @default.
• W2022758813 hasConceptScore W2022758813C9930424 @default.
• W2022758813 hasIssue "3" @default.
• W2022758813 hasLocation W20227588131 @default.
• W2022758813 hasOpenAccess W2022758813 @default.
• W2022758813 hasPrimaryLocation W20227588131 @default.
• W2022758813 hasRelatedWork W1967634252 @default.
• W2022758813 hasRelatedWork W1969087022 @default.
• W2022758813 hasRelatedWork W1975524802 @default.
• W2022758813 hasRelatedWork W2055208702 @default.
• W2022758813 hasRelatedWork W2057766473 @default.

• next