FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2079897798> ?p ?o ?g. }

• W2079897798 endingPage "46" @default.
• W2079897798 startingPage "32" @default.
• W2079897798 abstract "Geothermal waters originating from three aquifers in northwestern Romania have been analyzed for several physico-chemical parameters namely, pH, temperature, electrical conductivity, total dissolved solids, hardness, redox potential, and chemical oxygen demand. In addition, major dissolved ions and organic matter content and radium and radon occurrence have been analyzed. The three aquifers are the fissured Middle Triassic limestone/dolomite aquifer from Oradea, the Lower Cretaceous limestone aquifer from 1Mai–Felix Spa, and the Lower Pontian (Late Miocene) granular (sand) aquifer from Săcuieni. The first two aquifers belong to the Inner Dacides and the last to the Pannonian Basin. We have examined the relationships between the occurrence of radium and radon in the thermal waters and the hydrochemical and geothermal features of the aquifers, which may impart a secondary control on the activity of these radionuclides. According to their chemistry, the thermal waters were classified as sulfate–bicarbonate–calcium–magnesium (Oradea), bicarbonate–sulfate–calcium–magnesium (Felix–1Mai Spa), and bicarbonate–sodium–chloride (Săcuieni). The activities of radon and radium were higher in Săcuieni (up to 22.88 and 1.40 Bq/L) and Oradea (up to 34.82 and 1.82 Bq/L) than in Felix–1Mai Spa (up to 16.76 and 0.19 Bq/L). The data shows that the thermal processes may control the migration and distribution of radionuclides, and that the mobility of radionuclides may be influenced by several physico-chemical parameters, such as pH, total dissolved solids, and redox potential, or by some chemical processes, such as adsorption on humic acids or partitions into the organic (hydrocarbons) phase. The data illustrate no significant differences between the parameters analyzed from February to July 2009, proving that the production regime of the aquifers has a minor impact on their chemical and physical parameters." @default.
• W2079897798 created "2016-06-24" @default.
• W2079897798 creator A5016134879 @default.
• W2079897798 creator A5026741652 @default.
• W2079897798 creator A5075426328 @default.
• W2079897798 creator A5077906406 @default.
• W2079897798 creator A5089009342 @default.
• W2079897798 date "2012-04-01" @default.
• W2079897798 modified "2023-09-26" @default.
• W2079897798 title "Correlations between radium and radon occurrence and hydrogeochemical features for various geothermal aquifers in Northwestern Romania" @default.
• W2079897798 cites W1968962322 @default.
• W2079897798 cites W1976460796 @default.
• W2079897798 cites W1978595726 @default.
• W2079897798 cites W1990868335 @default.
• W2079897798 cites W1990988214 @default.
• W2079897798 cites W1993750562 @default.
• W2079897798 cites W1994694187 @default.
• W2079897798 cites W1998708595 @default.
• W2079897798 cites W2002395922 @default.
• W2079897798 cites W2003849555 @default.
• W2079897798 cites W2006918716 @default.
• W2079897798 cites W2007015713 @default.
• W2079897798 cites W2007595131 @default.
• W2079897798 cites W2008385258 @default.
• W2079897798 cites W2020372638 @default.
• W2079897798 cites W2021864871 @default.
• W2079897798 cites W2026167163 @default.
• W2079897798 cites W2026878846 @default.
• W2079897798 cites W2030028345 @default.
• W2079897798 cites W2030295205 @default.
• W2079897798 cites W2035705908 @default.
• W2079897798 cites W2037416659 @default.
• W2079897798 cites W2041801027 @default.
• W2079897798 cites W2041933620 @default.
• W2079897798 cites W2047320363 @default.
• W2079897798 cites W2048801364 @default.
• W2079897798 cites W2063863598 @default.
• W2079897798 cites W2066917057 @default.
• W2079897798 cites W2085807999 @default.
• W2079897798 cites W2094860876 @default.
• W2079897798 cites W2114668164 @default.
• W2079897798 cites W2120850670 @default.
• W2079897798 cites W2142043799 @default.
• W2079897798 cites W2159214724 @default.
• W2079897798 cites W2592028969 @default.
• W2079897798 cites W4243898028 @default.
• W2079897798 doi "https://doi.org/10.1016/j.geothermics.2011.12.001" @default.
• W2079897798 hasPublicationYear "2012" @default.
• W2079897798 type Work @default.
• W2079897798 sameAs 2079897798 @default.
• W2079897798 citedByCount "45" @default.
• W2079897798 countsByYear W20798977982013 @default.
• W2079897798 countsByYear W20798977982014 @default.
• W2079897798 countsByYear W20798977982015 @default.
• W2079897798 countsByYear W20798977982016 @default.
• W2079897798 countsByYear W20798977982017 @default.
• W2079897798 countsByYear W20798977982018 @default.
• W2079897798 countsByYear W20798977982019 @default.
• W2079897798 countsByYear W20798977982020 @default.
• W2079897798 countsByYear W20798977982021 @default.
• W2079897798 countsByYear W20798977982022 @default.
• W2079897798 countsByYear W20798977982023 @default.
• W2079897798 crossrefType "journal-article" @default.
• W2079897798 hasAuthorship W2079897798A5016134879 @default.
• W2079897798 hasAuthorship W2079897798A5026741652 @default.
• W2079897798 hasAuthorship W2079897798A5075426328 @default.
• W2079897798 hasAuthorship W2079897798A5077906406 @default.
• W2079897798 hasAuthorship W2079897798A5089009342 @default.
• W2079897798 hasConcept C107872376 @default.
• W2079897798 hasConcept C111766609 @default.
• W2079897798 hasConcept C121332964 @default.
• W2079897798 hasConcept C127313418 @default.
• W2079897798 hasConcept C129360787 @default.
• W2079897798 hasConcept C158973077 @default.
• W2079897798 hasConcept C17409809 @default.
• W2079897798 hasConcept C177322064 @default.
• W2079897798 hasConcept C178790620 @default.
• W2079897798 hasConcept C185592680 @default.
• W2079897798 hasConcept C187320778 @default.
• W2079897798 hasConcept C199289684 @default.
• W2079897798 hasConcept C2778343803 @default.
• W2079897798 hasConcept C39432304 @default.
• W2079897798 hasConcept C545943180 @default.
• W2079897798 hasConcept C550196577 @default.
• W2079897798 hasConcept C62520636 @default.
• W2079897798 hasConcept C75622301 @default.
• W2079897798 hasConcept C76177295 @default.
• W2079897798 hasConcept C8058405 @default.
• W2079897798 hasConcept C87717796 @default.
• W2079897798 hasConceptScore W2079897798C107872376 @default.
• W2079897798 hasConceptScore W2079897798C111766609 @default.
• W2079897798 hasConceptScore W2079897798C121332964 @default.
• W2079897798 hasConceptScore W2079897798C127313418 @default.
• W2079897798 hasConceptScore W2079897798C129360787 @default.
• W2079897798 hasConceptScore W2079897798C158973077 @default.
• W2079897798 hasConceptScore W2079897798C17409809 @default.
• W2079897798 hasConceptScore W2079897798C177322064 @default.
• W2079897798 hasConceptScore W2079897798C178790620 @default.

• next