FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2051269198> ?p ?o ?g. }

• W2051269198 endingPage "530" @default.
• W2051269198 startingPage "517" @default.
• W2051269198 abstract "Many CO2-rich springs are found in Mesozoic granitoids and surrounding rocks in South Korea. Their presence is locally restricted to three regions: the Kangwon region, the Chungcheong region and the Kyungpook region. Discharge of many CO2-rich springs is mainly related to the geologic structures, i.e., the geologic boundaries, faults and dykes. The sixty-three CO2-rich water samples can be classified into three chemical water types; Ca-HCO3 water, Ca(Na)-HCO3 water, and Na-HCO3 water. Most of the soda waters show a high CO2 concentration (PCO2 0.12 atm to 5.21 atm), a slightly acid pH (4.8 to 6.76), and high ion concentrations. The microscopic observation and the chemical analysis of host rocks at CO2-rich spring sites show that the carbonate minerals are secondary precipitates and interstitial fillings in Cretaceous sedimentary rocks that are the main sources of Ca, Mg, HCO3 and Fe in the CO2-rich waters of the Kyungpook region. The carbonate minerals locally present in the fractures of granite and gneiss would be one of the main sources of abundant Ca, Mg and HCO3 in the CO2-rich water of the Kangwon and the Chungcheong regions. The chemical composition of these CO2-rich springs according to host rocks and discharge regions was compared by using the Box-Whisker diagram. Oxygen and hydrogen isotope data indicates that the CO2-rich waters are of meteoric origin. The carbon isotope data (δ13C -6.6 to -0.9‰) suggest that the carbon of the soda waters is mainly derived from a deep-seated source, but is partly mixed with CO2 derived from carbonate minerals. The formation process of the CO2-rich springs can be summarized as follows. After the CO2 gas derived from the deep-seated source enters the groundwater system along faults or geologic boundaries, the CO2-rich water evolved into three chemical types depending on the aquifer rock types." @default.
• W2051269198 created "2016-06-24" @default.
• W2051269198 creator A5032655474 @default.
• W2051269198 creator A5065629959 @default.
• W2051269198 creator A5070668206 @default.
• W2051269198 date "2005-01-01" @default.
• W2051269198 modified "2023-09-27" @default.
• W2051269198 title "Hydrochemistry and genesis of CO2-rich springs from Mesozoic granitoids and their adjacent rocks in South Korea" @default.
• W2051269198 cites W1553044330 @default.
• W2051269198 cites W1971381271 @default.
• W2051269198 cites W1979203605 @default.
• W2051269198 cites W1981459598 @default.
• W2051269198 cites W2001987411 @default.
• W2051269198 cites W2030369846 @default.
• W2051269198 cites W2041658457 @default.
• W2051269198 cites W2041808565 @default.
• W2051269198 cites W2046977454 @default.
• W2051269198 cites W2051193733 @default.
• W2051269198 cites W2054075985 @default.
• W2051269198 cites W2057858806 @default.
• W2051269198 cites W2072191315 @default.
• W2051269198 cites W2081631371 @default.
• W2051269198 cites W2083394958 @default.
• W2051269198 cites W2085839655 @default.
• W2051269198 cites W2092868748 @default.
• W2051269198 cites W2095365910 @default.
• W2051269198 cites W2142043125 @default.
• W2051269198 cites W2901655032 @default.
• W2051269198 cites W2901876326 @default.
• W2051269198 cites W61186837 @default.
• W2051269198 doi "https://doi.org/10.2343/geochemj.39.517" @default.
• W2051269198 hasPublicationYear "2005" @default.
• W2051269198 type Work @default.
• W2051269198 sameAs 2051269198 @default.
• W2051269198 citedByCount "20" @default.
• W2051269198 countsByYear W20512691982012 @default.
• W2051269198 countsByYear W20512691982013 @default.
• W2051269198 countsByYear W20512691982017 @default.
• W2051269198 countsByYear W20512691982018 @default.
• W2051269198 countsByYear W20512691982019 @default.
• W2051269198 countsByYear W20512691982020 @default.
• W2051269198 countsByYear W20512691982021 @default.
• W2051269198 countsByYear W20512691982022 @default.
• W2051269198 crossrefType "journal-article" @default.
• W2051269198 hasAuthorship W2051269198A5032655474 @default.
• W2051269198 hasAuthorship W2051269198A5065629959 @default.
• W2051269198 hasAuthorship W2051269198A5070668206 @default.
• W2051269198 hasBestOaLocation W20512691981 @default.
• W2051269198 hasConcept C104779481 @default.
• W2051269198 hasConcept C107872376 @default.
• W2051269198 hasConcept C109007969 @default.
• W2051269198 hasConcept C12294951 @default.
• W2051269198 hasConcept C127313418 @default.
• W2051269198 hasConcept C140205800 @default.
• W2051269198 hasConcept C151730666 @default.
• W2051269198 hasConcept C158787203 @default.
• W2051269198 hasConcept C159985019 @default.
• W2051269198 hasConcept C171701179 @default.
• W2051269198 hasConcept C17409809 @default.
• W2051269198 hasConcept C178790620 @default.
• W2051269198 hasConcept C185059815 @default.
• W2051269198 hasConcept C185592680 @default.
• W2051269198 hasConcept C192562407 @default.
• W2051269198 hasConcept C19320362 @default.
• W2051269198 hasConcept C202783661 @default.
• W2051269198 hasConcept C26687426 @default.
• W2051269198 hasConcept C2779002002 @default.
• W2051269198 hasConcept C2780181037 @default.
• W2051269198 hasConcept C2780659211 @default.
• W2051269198 hasConcept C6494504 @default.
• W2051269198 hasConcept C71468253 @default.
• W2051269198 hasConceptScore W2051269198C104779481 @default.
• W2051269198 hasConceptScore W2051269198C107872376 @default.
• W2051269198 hasConceptScore W2051269198C109007969 @default.
• W2051269198 hasConceptScore W2051269198C12294951 @default.
• W2051269198 hasConceptScore W2051269198C127313418 @default.
• W2051269198 hasConceptScore W2051269198C140205800 @default.
• W2051269198 hasConceptScore W2051269198C151730666 @default.
• W2051269198 hasConceptScore W2051269198C158787203 @default.
• W2051269198 hasConceptScore W2051269198C159985019 @default.
• W2051269198 hasConceptScore W2051269198C171701179 @default.
• W2051269198 hasConceptScore W2051269198C17409809 @default.
• W2051269198 hasConceptScore W2051269198C178790620 @default.
• W2051269198 hasConceptScore W2051269198C185059815 @default.
• W2051269198 hasConceptScore W2051269198C185592680 @default.
• W2051269198 hasConceptScore W2051269198C192562407 @default.
• W2051269198 hasConceptScore W2051269198C19320362 @default.
• W2051269198 hasConceptScore W2051269198C202783661 @default.
• W2051269198 hasConceptScore W2051269198C26687426 @default.
• W2051269198 hasConceptScore W2051269198C2779002002 @default.
• W2051269198 hasConceptScore W2051269198C2780181037 @default.
• W2051269198 hasConceptScore W2051269198C2780659211 @default.
• W2051269198 hasConceptScore W2051269198C6494504 @default.
• W2051269198 hasConceptScore W2051269198C71468253 @default.
• W2051269198 hasIssue "6" @default.
• W2051269198 hasLocation W20512691981 @default.
• W2051269198 hasOpenAccess W2051269198 @default.
• W2051269198 hasPrimaryLocation W20512691981 @default.

• next