FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2435205893> ?p ?o ?g. }

• W2435205893 endingPage "300" @default.
• W2435205893 startingPage "286" @default.
• W2435205893 abstract "Abstract Conventional graphical techniques, mass balance geochemical modelling, and multivariate statistical methods were jointly applied to hydrogeochemical data of groundwater from the fractured rock aquifer system, and surface water in the Bosumtwi and surrounding areas to reveal evolutionary trends and the characteristics of evolving groundwater in the area. Four clusters distinguished from the Q-mode hierarchical cluster analysis (HCA) comprised three main groundwater associations and one surface water group (lake water). Although both water resources are of low mineralization (TDS  Mg HCO 3 − , evolves to Ca Mg and mixed cations HCO 3 − water types at the lower reaches. The lake water on the other hand is Na HCO 3 − water type. Results from principal component analyses (PCA) and other geochemical interpretations distinguished three sources of variations in the hydrochemistry. Saturation indices of possible reactive mineral phases show groundwater undersaturation relative to albite, anorthite, aragonite, barite, calcite, chlorite, chrysotile, dolomite, gypsum, k-felspar and talc, and supersaturation with respect to gibbsite, kaolinite, Ca-montmorillonite and k-mica in the area. The PCA and other geochemical interpretation identify weathering of feldspars and carbonate mineral dissolution as predominantly influencing the hydrochemistry of the groundwater. Hydrolysis of the aluminosilicates causes the groundwater to reach equilibrium with kaolinite. In addition to dissolution of silicates, the chemical composition of the lake water has been influenced by evaporation and consequent carbonate saturation." @default.
• W2435205893 created "2016-06-24" @default.
• W2435205893 creator A5022595752 @default.
• W2435205893 creator A5031553378 @default.
• W2435205893 creator A5035327967 @default.
• W2435205893 creator A5066282760 @default.
• W2435205893 creator A5072892435 @default.
• W2435205893 creator A5077608896 @default.
• W2435205893 date "2016-09-01" @default.
• W2435205893 modified "2023-09-26" @default.
• W2435205893 title "Determination of the mineral stability field of evolving groundwater in the Lake Bosumtwi impact crater and surrounding areas" @default.
• W2435205893 cites W1966409396 @default.
• W2435205893 cites W1972514904 @default.
• W2435205893 cites W1972804398 @default.
• W2435205893 cites W1980718919 @default.
• W2435205893 cites W1982981402 @default.
• W2435205893 cites W1987575394 @default.
• W2435205893 cites W1996981990 @default.
• W2435205893 cites W2005919559 @default.
• W2435205893 cites W2021004455 @default.
• W2435205893 cites W2030905542 @default.
• W2435205893 cites W2032288892 @default.
• W2435205893 cites W2048348692 @default.
• W2435205893 cites W2054183883 @default.
• W2435205893 cites W2058720760 @default.
• W2435205893 cites W2062917647 @default.
• W2435205893 cites W2072253027 @default.
• W2435205893 cites W2073413073 @default.
• W2435205893 cites W2076892181 @default.
• W2435205893 cites W2080146475 @default.
• W2435205893 cites W2083993551 @default.
• W2435205893 cites W2085868206 @default.
• W2435205893 cites W2087091337 @default.
• W2435205893 cites W2088715049 @default.
• W2435205893 cites W2089711846 @default.
• W2435205893 cites W2137797445 @default.
• W2435205893 cites W2144391541 @default.
• W2435205893 cites W2160172778 @default.
• W2435205893 cites W2161226494 @default.
• W2435205893 cites W2163393486 @default.
• W2435205893 cites W2166581978 @default.
• W2435205893 cites W2223261853 @default.
• W2435205893 cites W4248782425 @default.
• W2435205893 doi "https://doi.org/10.1016/j.jafrearsci.2016.06.007" @default.
• W2435205893 hasPublicationYear "2016" @default.
• W2435205893 type Work @default.
• W2435205893 sameAs 2435205893 @default.
• W2435205893 citedByCount "11" @default.
• W2435205893 countsByYear W24352058932018 @default.
• W2435205893 countsByYear W24352058932020 @default.
• W2435205893 countsByYear W24352058932021 @default.
• W2435205893 countsByYear W24352058932022 @default.
• W2435205893 countsByYear W24352058932023 @default.
• W2435205893 crossrefType "journal-article" @default.
• W2435205893 hasAuthorship W2435205893A5022595752 @default.
• W2435205893 hasAuthorship W2435205893A5031553378 @default.
• W2435205893 hasAuthorship W2435205893A5035327967 @default.
• W2435205893 hasAuthorship W2435205893A5066282760 @default.
• W2435205893 hasAuthorship W2435205893A5072892435 @default.
• W2435205893 hasAuthorship W2435205893A5077608896 @default.
• W2435205893 hasConcept C120806208 @default.
• W2435205893 hasConcept C121332964 @default.
• W2435205893 hasConcept C127313418 @default.
• W2435205893 hasConcept C16674752 @default.
• W2435205893 hasConcept C17409809 @default.
• W2435205893 hasConcept C179537507 @default.
• W2435205893 hasConcept C187320778 @default.
• W2435205893 hasConcept C18903297 @default.
• W2435205893 hasConcept C1965285 @default.
• W2435205893 hasConcept C2776432453 @default.
• W2435205893 hasConcept C2777619642 @default.
• W2435205893 hasConcept C66264921 @default.
• W2435205893 hasConcept C76177295 @default.
• W2435205893 hasConcept C86803240 @default.
• W2435205893 hasConcept C87355193 @default.
• W2435205893 hasConceptScore W2435205893C120806208 @default.
• W2435205893 hasConceptScore W2435205893C121332964 @default.
• W2435205893 hasConceptScore W2435205893C127313418 @default.
• W2435205893 hasConceptScore W2435205893C16674752 @default.
• W2435205893 hasConceptScore W2435205893C17409809 @default.
• W2435205893 hasConceptScore W2435205893C179537507 @default.
• W2435205893 hasConceptScore W2435205893C187320778 @default.
• W2435205893 hasConceptScore W2435205893C18903297 @default.
• W2435205893 hasConceptScore W2435205893C1965285 @default.
• W2435205893 hasConceptScore W2435205893C2776432453 @default.
• W2435205893 hasConceptScore W2435205893C2777619642 @default.
• W2435205893 hasConceptScore W2435205893C66264921 @default.
• W2435205893 hasConceptScore W2435205893C76177295 @default.
• W2435205893 hasConceptScore W2435205893C86803240 @default.
• W2435205893 hasConceptScore W2435205893C87355193 @default.
• W2435205893 hasLocation W24352058931 @default.
• W2435205893 hasOpenAccess W2435205893 @default.
• W2435205893 hasPrimaryLocation W24352058931 @default.
• W2435205893 hasRelatedWork W1981658100 @default.
• W2435205893 hasRelatedWork W1986519218 @default.
• W2435205893 hasRelatedWork W2024458127 @default.
• W2435205893 hasRelatedWork W2036610505 @default.
• W2435205893 hasRelatedWork W204878984 @default.

• next