FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2022134807> ?p ?o ?g. }

• W2022134807 endingPage "1776" @default.
• W2022134807 startingPage "1765" @default.
• W2022134807 abstract "Hydrological, geochemical and environmental isotope data from groundwater wells at Ruprechtov natural analogue site were evaluated to characterize the flow pattern and C chemistry in the system. The results show that water flow in the Tertiary sediments is restricted to 1–2 m thick zones in the so-called clay/lignite horizon with two different infiltration areas in the outcropping granites in the western and south-western part of the investigated area. Generally the flow system is separated from the underlying granite by a kaolin layer up to several tens of metres thick. Differences in stable isotope signatures in the northern part of the site indicate very local connections of both flow systems via fault zones. The observed increase of δ13C values and decrease of 14C activities in dissolved inorganic C during evolution of the groundwater from the infiltration area to the clay/lignite horizon was modelled using simple open- and closed-system models as well as an inverse geochemical model (NETPATH), which included changes in other geochemical parameters. The results from both types of models provided some insights into timescales of groundwater flow, but mainly revealed that additional sources of C are active in the system. These are very likely biodegradation of dissolved and sedimentary organic C (DOC and SOC) as well as the influx of endogenous CO2. The occurrence of microbial degradation of SOC in the clay/lignite layers is indicated by the increase of biogenic DIC, DOC, and phosphate concentrations. The impact of microbial SO4 reduction on this process is confirmed by an increase of δ34S values in dissolved SO42- from the infiltration area to the clay/lignite horizon with an enrichment factor of 11‰. The very low DOC concentrations of 1–5 mg C/L in the clay/lignite horizon with an organic matter content up to 50% C is probably caused by very low availability of organic matter to the processes of degradation and DOC release, demonstrated by extraction experiments with SOC." @default.
• W2022134807 created "2016-06-24" @default.
• W2022134807 creator A5001305317 @default.
• W2022134807 creator A5025440673 @default.
• W2022134807 creator A5030707252 @default.
• W2022134807 creator A5038351189 @default.
• W2022134807 creator A5053011072 @default.
• W2022134807 creator A5059406837 @default.
• W2022134807 creator A5061953677 @default.
• W2022134807 creator A5079553584 @default.
• W2022134807 date "2009-09-01" @default.
• W2022134807 modified "2023-10-17" @default.
• W2022134807 title "Carbon chemistry and groundwater dynamics at natural analogue site Ruprechtov, Czech Republic: Insights from environmental isotopes" @default.
• W2022134807 cites W1984493016 @default.
• W2022134807 cites W1995508857 @default.
• W2022134807 cites W2007003353 @default.
• W2022134807 cites W2008281306 @default.
• W2022134807 cites W2008933537 @default.
• W2022134807 cites W2011744114 @default.
• W2022134807 cites W2014467701 @default.
• W2022134807 cites W2039248536 @default.
• W2022134807 cites W2057164798 @default.
• W2022134807 cites W2057963149 @default.
• W2022134807 cites W2070022169 @default.
• W2022134807 cites W2078928100 @default.
• W2022134807 cites W2083167277 @default.
• W2022134807 cites W2092868748 @default.
• W2022134807 cites W2095107804 @default.
• W2022134807 doi "https://doi.org/10.1016/j.apgeochem.2009.05.007" @default.
• W2022134807 hasPublicationYear "2009" @default.
• W2022134807 type Work @default.
• W2022134807 sameAs 2022134807 @default.
• W2022134807 citedByCount "26" @default.
• W2022134807 countsByYear W20221348072012 @default.
• W2022134807 countsByYear W20221348072013 @default.
• W2022134807 countsByYear W20221348072014 @default.
• W2022134807 countsByYear W20221348072015 @default.
• W2022134807 countsByYear W20221348072016 @default.
• W2022134807 countsByYear W20221348072019 @default.
• W2022134807 countsByYear W20221348072020 @default.
• W2022134807 countsByYear W20221348072022 @default.
• W2022134807 crossrefType "journal-article" @default.
• W2022134807 hasAuthorship W2022134807A5001305317 @default.
• W2022134807 hasAuthorship W2022134807A5025440673 @default.
• W2022134807 hasAuthorship W2022134807A5030707252 @default.
• W2022134807 hasAuthorship W2022134807A5038351189 @default.
• W2022134807 hasAuthorship W2022134807A5053011072 @default.
• W2022134807 hasAuthorship W2022134807A5059406837 @default.
• W2022134807 hasAuthorship W2022134807A5061953677 @default.
• W2022134807 hasAuthorship W2022134807A5079553584 @default.
• W2022134807 hasConcept C107872376 @default.
• W2022134807 hasConcept C111368507 @default.
• W2022134807 hasConcept C121332964 @default.
• W2022134807 hasConcept C127313418 @default.
• W2022134807 hasConcept C131227075 @default.
• W2022134807 hasConcept C153400128 @default.
• W2022134807 hasConcept C158787203 @default.
• W2022134807 hasConcept C159390177 @default.
• W2022134807 hasConcept C169212394 @default.
• W2022134807 hasConcept C17409809 @default.
• W2022134807 hasConcept C185059815 @default.
• W2022134807 hasConcept C185592680 @default.
• W2022134807 hasConcept C187320778 @default.
• W2022134807 hasConcept C199289684 @default.
• W2022134807 hasConcept C36574619 @default.
• W2022134807 hasConcept C6494504 @default.
• W2022134807 hasConcept C75622301 @default.
• W2022134807 hasConcept C76177295 @default.
• W2022134807 hasConcept C76886044 @default.
• W2022134807 hasConcept C97355855 @default.
• W2022134807 hasConceptScore W2022134807C107872376 @default.
• W2022134807 hasConceptScore W2022134807C111368507 @default.
• W2022134807 hasConceptScore W2022134807C121332964 @default.
• W2022134807 hasConceptScore W2022134807C127313418 @default.
• W2022134807 hasConceptScore W2022134807C131227075 @default.
• W2022134807 hasConceptScore W2022134807C153400128 @default.
• W2022134807 hasConceptScore W2022134807C158787203 @default.
• W2022134807 hasConceptScore W2022134807C159390177 @default.
• W2022134807 hasConceptScore W2022134807C169212394 @default.
• W2022134807 hasConceptScore W2022134807C17409809 @default.
• W2022134807 hasConceptScore W2022134807C185059815 @default.
• W2022134807 hasConceptScore W2022134807C185592680 @default.
• W2022134807 hasConceptScore W2022134807C187320778 @default.
• W2022134807 hasConceptScore W2022134807C199289684 @default.
• W2022134807 hasConceptScore W2022134807C36574619 @default.
• W2022134807 hasConceptScore W2022134807C6494504 @default.
• W2022134807 hasConceptScore W2022134807C75622301 @default.
• W2022134807 hasConceptScore W2022134807C76177295 @default.
• W2022134807 hasConceptScore W2022134807C76886044 @default.
• W2022134807 hasConceptScore W2022134807C97355855 @default.
• W2022134807 hasIssue "9" @default.
• W2022134807 hasLocation W20221348071 @default.
• W2022134807 hasOpenAccess W2022134807 @default.
• W2022134807 hasPrimaryLocation W20221348071 @default.
• W2022134807 hasRelatedWork W1573429580 @default.
• W2022134807 hasRelatedWork W2025711010 @default.
• W2022134807 hasRelatedWork W2145150060 @default.
• W2022134807 hasRelatedWork W2147735603 @default.

• next