FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W3080551034> ?p ?o ?g. }

• W3080551034 endingPage "758" @default.
• W3080551034 startingPage "758" @default.
• W3080551034 abstract "Regular features of ground and surface waters affected by drainage from mine waste include their acidity and elevated concentrations of dissolved metals, with their attendant negative effects on drinking water quality and aquatic life. One parameter that aids in buffering these waters against acidity and sustains aquatic life is dissolved inorganic carbon (DIC). In this study, the chemical and isotopic (δ13C) composition of primary calcite and DIC (δ13CDIC) in groundwater and surface waters within and downstream, respectively, of abandoned Cu–W–F skarn tailings at Yxsjöberg, Sweden, were used to trace the biogeochemical processes controlling their respective δ13CDIC signatures. In addition, the δ13C signatures of the inorganic (carbonate) fractions of the tailings were used to verify the formation of secondary carbonates within the tailings. Lower average δ13C values of the carbonate fractions (δ13Ccarb = −2.7‰) relative to those of the primary calcite (δ13C = +0.1‰) from the orebodies from which the tailings originated pointed to the precipitation of secondary carbonates. These lower δ13Ccarb signatures were assumed to represent mixed-source C signals involving isotopically light CO2 from the atmosphere, the degradation of organic matter in the upper part of the tailings and HCO3− from calcite dissolution. The groundwater δ13CDIC values (−12.6‰ to −4.4‰) were far lower than the hypothetical range of values (−4.6‰ to +0.7‰) for primary calcite and secondary carbonate dissolution. These signatures were attributed to carbonate (calcite and secondary carbonate) dissolution and the degradation of dissolved organic carbon (DOC) from various organic sources such as peat underneath the tailings and the surrounding forests. Downstream surface water samples collected in May had low δ13CDIC values (−16‰) and high DOC (14 mg C/L) compared to the groundwater samples. These signatures represented the oxidation of the DOC from the wash out of the mires and forests during the snowmelt and spring flood. The DOC and δ13CDIC values of the surface waters from June to September ranged from 6–15 mg·C/L and −25‰ to −8.6‰, respectively. These signatures were interpreted to reflect mixed C sources, including carbonate dehydration by acidity from Fe3+ hydrolysis due to the mixing of groundwater with surface waters and the subsequent diffusive loss of CO2 (g), aquatic photosynthesis, photooxidation, DOC degradation, as well as microbial respiration. Although the 13CDIC signatures of the downstream surface waters seemed to be seasonally controlled and influenced by variable groundwater contributions, the lack of data with respect to DIC concentrations, coupled with multiple potential biogeochemical processes that could influence the DIC pool and 13CDIC values, made it difficult to identify the major regulating process of the 13CDIC signatures. Therefore, other complimentary isotopes and elemental concentrations are recommended in order to decipher the dominant biogeochemical process." @default.
• W3080551034 created "2020-09-01" @default.
• W3080551034 creator A5009293950 @default.
• W3080551034 creator A5063928099 @default.
• W3080551034 creator A5089384490 @default.
• W3080551034 date "2020-08-27" @default.
• W3080551034 modified "2023-09-26" @default.
• W3080551034 title "Biogeochemical Controls on 13CDIC Signatures from Circum-Neutral pH Groundwater in Cu–W–F Skarn Tailings to Acidic Downstream Surface Waters" @default.
• W3080551034 cites W1533703942 @default.
• W3080551034 cites W1579103780 @default.
• W3080551034 cites W166619974 @default.
• W3080551034 cites W1963699922 @default.
• W3080551034 cites W1968026363 @default.
• W3080551034 cites W1976016585 @default.
• W3080551034 cites W1981229895 @default.
• W3080551034 cites W1982652213 @default.
• W3080551034 cites W1998051218 @default.
• W3080551034 cites W2000713353 @default.
• W3080551034 cites W2005435672 @default.
• W3080551034 cites W2022339784 @default.
• W3080551034 cites W2025127061 @default.
• W3080551034 cites W2039569469 @default.
• W3080551034 cites W2043977794 @default.
• W3080551034 cites W2058977923 @default.
• W3080551034 cites W2060051055 @default.
• W3080551034 cites W2078287009 @default.
• W3080551034 cites W2100667474 @default.
• W3080551034 cites W2109993091 @default.
• W3080551034 cites W2113114069 @default.
• W3080551034 cites W2113123546 @default.
• W3080551034 cites W2115380076 @default.
• W3080551034 cites W2119473214 @default.
• W3080551034 cites W2163463585 @default.
• W3080551034 cites W2332387888 @default.
• W3080551034 cites W2739472878 @default.
• W3080551034 cites W2791401146 @default.
• W3080551034 cites W2891374016 @default.
• W3080551034 cites W2898949408 @default.
• W3080551034 cites W2953749677 @default.
• W3080551034 cites W3018352519 @default.
• W3080551034 cites W43061563 @default.
• W3080551034 doi "https://doi.org/10.3390/min10090758" @default.
• W3080551034 hasPublicationYear "2020" @default.
• W3080551034 type Work @default.
• W3080551034 sameAs 3080551034 @default.
• W3080551034 citedByCount "4" @default.
• W3080551034 countsByYear W30805510342022 @default.
• W3080551034 countsByYear W30805510342023 @default.
• W3080551034 crossrefType "journal-article" @default.
• W3080551034 hasAuthorship W3080551034A5009293950 @default.
• W3080551034 hasAuthorship W3080551034A5063928099 @default.
• W3080551034 hasAuthorship W3080551034A5089384490 @default.
• W3080551034 hasBestOaLocation W30805510341 @default.
• W3080551034 hasConcept C107872376 @default.
• W3080551034 hasConcept C127313418 @default.
• W3080551034 hasConcept C147789679 @default.
• W3080551034 hasConcept C178790620 @default.
• W3080551034 hasConcept C185592680 @default.
• W3080551034 hasConcept C187320778 @default.
• W3080551034 hasConcept C199289684 @default.
• W3080551034 hasConcept C2779002002 @default.
• W3080551034 hasConcept C2780191791 @default.
• W3080551034 hasConcept C2780659211 @default.
• W3080551034 hasConcept C36574619 @default.
• W3080551034 hasConcept C48743137 @default.
• W3080551034 hasConcept C5166401 @default.
• W3080551034 hasConcept C71915725 @default.
• W3080551034 hasConcept C76177295 @default.
• W3080551034 hasConceptScore W3080551034C107872376 @default.
• W3080551034 hasConceptScore W3080551034C127313418 @default.
• W3080551034 hasConceptScore W3080551034C147789679 @default.
• W3080551034 hasConceptScore W3080551034C178790620 @default.
• W3080551034 hasConceptScore W3080551034C185592680 @default.
• W3080551034 hasConceptScore W3080551034C187320778 @default.
• W3080551034 hasConceptScore W3080551034C199289684 @default.
• W3080551034 hasConceptScore W3080551034C2779002002 @default.
• W3080551034 hasConceptScore W3080551034C2780191791 @default.
• W3080551034 hasConceptScore W3080551034C2780659211 @default.
• W3080551034 hasConceptScore W3080551034C36574619 @default.
• W3080551034 hasConceptScore W3080551034C48743137 @default.
• W3080551034 hasConceptScore W3080551034C5166401 @default.
• W3080551034 hasConceptScore W3080551034C71915725 @default.
• W3080551034 hasConceptScore W3080551034C76177295 @default.
• W3080551034 hasFunder F4320337753 @default.
• W3080551034 hasIssue "9" @default.
• W3080551034 hasLocation W30805510341 @default.
• W3080551034 hasOpenAccess W3080551034 @default.
• W3080551034 hasPrimaryLocation W30805510341 @default.
• W3080551034 hasRelatedWork W2073361395 @default.
• W3080551034 hasRelatedWork W2379288782 @default.
• W3080551034 hasRelatedWork W2902243426 @default.
• W3080551034 hasRelatedWork W3080551034 @default.
• W3080551034 hasRelatedWork W3092815386 @default.
• W3080551034 hasRelatedWork W3127588597 @default.
• W3080551034 hasRelatedWork W3194833440 @default.
• W3080551034 hasRelatedWork W3201811657 @default.
• W3080551034 hasRelatedWork W4210684782 @default.
• W3080551034 hasRelatedWork W4221072853 @default.

• next