FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W3095811361> ?p ?o ?g. }

• W3095811361 endingPage "101093" @default.
• W3095811361 startingPage "101093" @default.
• W3095811361 abstract "The work investigates the major solute chemistry of groundwater and fluoride enrichment (F−) in the shallow phreatic aquifer of Odisha. The study also interprets the hydrogeochemical processes of solute acquisition and the genetic behavior of groundwater F− contamination. A total of 1105 groundwater samples collected from across the state from different hydro-geomorphic settings have been analyzed for the major solutes and F− content. Groundwater is alkaline in nature (range of pH: 6.6–8.7; ave.: 7.9) predominated by moderately hard to very hard types. Average cation and anion chemistry stand in the orders of Ca2+ > Na+ > Mg2+ > K+ and HCO3− > Cl− > SO42− > CO32− respectively. The average mineralization is low (319 mg/L). The primary water types are Ca-Mg-HCO3 and Ca-Mg-Cl-HCO3, followed by Na-Cl, Ca-Mg-Cl, and Na-Ca-Mg-HCO3-Cl. Silicate-halite dissolution and reverse ion exchange are the significant processes of solute acquisition. Both the geogenic as well as the anthropogenic sources contribute to the groundwater fluoride contamination, etc. The ratio of Na+/Ca2+ > 1.0 comprises Na-HCO3 (Cl) water types with F− > 1.0 mg/L (range 1.0–3.5 mg/L) where the F− bears geogenic source. Positive relations exist between F− and pH, Na+, TDS, and HCO3−. It also reflects a perfect Na-TDS correlation (0.85). The ratio of Na+/Ca2+ < 1.0 segregates the sample population (F− range: 1.0–4.0 mg/L) with the F derived from anthropogenic sources. Such water types include Ca-Mg-HCO3 (Cl) varieties which are recently recharged meteoritic water types. The F− levels exhibit poor and negative correlations with the solutes in groundwater. The Na-TDS relation remains poor (0.12). In contrast, the TDS levels show strong correlations with Ca2+ (0.91), Mg2+ (0.80) and even Cl− (0.91). The majority of the monitoring points with the anthropogenic sources of groundwater F− are clustered in the Hirakud Canal Command area in the western parts of the state, indicating the role of irrigation return flow in the F− contamination." @default.
• W3095811361 created "2020-11-09" @default.
• W3095811361 creator A5021953219 @default.
• W3095811361 creator A5035793491 @default.
• W3095811361 creator A5047577399 @default.
• W3095811361 date "2021-05-01" @default.
• W3095811361 modified "2023-10-14" @default.
• W3095811361 title "Groundwater solute chemistry, hydrogeochemical processes and fluoride contamination in phreatic aquifer of Odisha, India" @default.
• W3095811361 cites W179546942 @default.
• W3095811361 cites W1971381271 @default.
• W3095811361 cites W1971918252 @default.
• W3095811361 cites W1973295190 @default.
• W3095811361 cites W1975505207 @default.
• W3095811361 cites W1994268523 @default.
• W3095811361 cites W2008587428 @default.
• W3095811361 cites W2028542434 @default.
• W3095811361 cites W2028671837 @default.
• W3095811361 cites W2031377162 @default.
• W3095811361 cites W2041196478 @default.
• W3095811361 cites W2045312180 @default.
• W3095811361 cites W2045493271 @default.
• W3095811361 cites W2053472491 @default.
• W3095811361 cites W2053742566 @default.
• W3095811361 cites W2060680089 @default.
• W3095811361 cites W2065318691 @default.
• W3095811361 cites W2072325309 @default.
• W3095811361 cites W2077795175 @default.
• W3095811361 cites W2079762260 @default.
• W3095811361 cites W2085433711 @default.
• W3095811361 cites W2088267958 @default.
• W3095811361 cites W2112149282 @default.
• W3095811361 cites W2129537345 @default.
• W3095811361 cites W2137810729 @default.
• W3095811361 cites W2146216952 @default.
• W3095811361 cites W2168030992 @default.
• W3095811361 cites W2281483701 @default.
• W3095811361 cites W2291324108 @default.
• W3095811361 cites W2308711928 @default.
• W3095811361 cites W2313912183 @default.
• W3095811361 cites W2489469160 @default.
• W3095811361 cites W2517652302 @default.
• W3095811361 cites W2560140501 @default.
• W3095811361 cites W2584421029 @default.
• W3095811361 cites W2748074662 @default.
• W3095811361 cites W2790797106 @default.
• W3095811361 cites W2883377287 @default.
• W3095811361 cites W2885421136 @default.
• W3095811361 cites W2990108932 @default.
• W3095811361 cites W4241839754 @default.
• W3095811361 doi "https://doi.org/10.1016/j.gsf.2020.10.001" @default.
• W3095811361 hasPublicationYear "2021" @default.
• W3095811361 type Work @default.
• W3095811361 sameAs 3095811361 @default.
• W3095811361 citedByCount "19" @default.
• W3095811361 countsByYear W30958113612021 @default.
• W3095811361 countsByYear W30958113612022 @default.
• W3095811361 countsByYear W30958113612023 @default.
• W3095811361 crossrefType "journal-article" @default.
• W3095811361 hasAuthorship W3095811361A5021953219 @default.
• W3095811361 hasAuthorship W3095811361A5035793491 @default.
• W3095811361 hasAuthorship W3095811361A5047577399 @default.
• W3095811361 hasBestOaLocation W30958113611 @default.
• W3095811361 hasConcept C107872376 @default.
• W3095811361 hasConcept C127313418 @default.
• W3095811361 hasConcept C144024400 @default.
• W3095811361 hasConcept C147789679 @default.
• W3095811361 hasConcept C149923435 @default.
• W3095811361 hasConcept C151730666 @default.
• W3095811361 hasConcept C178790620 @default.
• W3095811361 hasConcept C179104552 @default.
• W3095811361 hasConcept C180087314 @default.
• W3095811361 hasConcept C185592680 @default.
• W3095811361 hasConcept C187320778 @default.
• W3095811361 hasConcept C199289684 @default.
• W3095811361 hasConcept C2776277684 @default.
• W3095811361 hasConcept C2777335606 @default.
• W3095811361 hasConcept C2779229104 @default.
• W3095811361 hasConcept C2780828025 @default.
• W3095811361 hasConcept C2781113784 @default.
• W3095811361 hasConcept C2908647359 @default.
• W3095811361 hasConcept C75622301 @default.
• W3095811361 hasConcept C76177295 @default.
• W3095811361 hasConcept C88380143 @default.
• W3095811361 hasConceptScore W3095811361C107872376 @default.
• W3095811361 hasConceptScore W3095811361C127313418 @default.
• W3095811361 hasConceptScore W3095811361C144024400 @default.
• W3095811361 hasConceptScore W3095811361C147789679 @default.
• W3095811361 hasConceptScore W3095811361C149923435 @default.
• W3095811361 hasConceptScore W3095811361C151730666 @default.
• W3095811361 hasConceptScore W3095811361C178790620 @default.
• W3095811361 hasConceptScore W3095811361C179104552 @default.
• W3095811361 hasConceptScore W3095811361C180087314 @default.
• W3095811361 hasConceptScore W3095811361C185592680 @default.
• W3095811361 hasConceptScore W3095811361C187320778 @default.
• W3095811361 hasConceptScore W3095811361C199289684 @default.
• W3095811361 hasConceptScore W3095811361C2776277684 @default.
• W3095811361 hasConceptScore W3095811361C2777335606 @default.
• W3095811361 hasConceptScore W3095811361C2779229104 @default.

• next