FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2183670054> ?p ?o ?g. }

• W2183670054 abstract "Aquifer fluid compositions have been assessed from analytical data on water and steam samples collected at the wellhead from 28 production wells in eight geothermal areas from five countries (Hveragerdi, Krafla, Namafjall, and Nesjavellir in Iceland; Kizildere in Turkey; Momotombo in Nicaragua; Olkaria in Kenya and Zunil in Guatemala). The state of mineral saturation of the aquifer water with respect to the following minerals was studied: anhydrite, calcite, clinochlore-daphnite, clinozoisiteepidote, grossular, low-albite, microcline (the stable K-feldspar at low temperatures), prehnite, pyrite, pyrrhotite, quartz, wairakite and wollastonite. The aquifer water is close to equilibrium with calcite, quartz, low-albite and microcline. Most of the water is relatively close to wollastonite saturation. The same applies to clinozoisite, prehnite and wairakite although the scatter of the data points is larger than for the previously listed minerals. The waters are saturated or undersaturated with respect to anhydrite and grossular. Oversaturation is indicated for the clinochlore component of chlorite and the epidote component of the epidote solid solution. In the first instance this may be the consequence of the activity of the clinochlore component in the chlorite, but in the latter case faulty thermodynamic data on epidote. The results for all ferrous bearing minerals (daphnite, pyrite and pyrrhotite) indicate undersaturation that increases with increasing temperature. This is most likely an artifact due to faulty data on Fe-ion hydrolysis constants. The results indicate the Kizildere aquifer water is strongly undersaturated with respect to all Ca-bearing minerals. The cause of this apparent undersaturation is precipitation of calcite from the water as it boils, causing wellhead samples to be lower in Ca than the aquifer water. Assessment of calcite and amorphous silica scaling tendencies for selected well waters indicates that waste fluid disposal at Kizildere is most feasible at the lowest possible temperature if scaling is to be minimized or avoided. Similarly, injection temperatures of about 150 and 200/C are optimal for Zunil and Nesjavellir, respectively." @default.
• W2183670054 created "2016-06-24" @default.
• W2183670054 creator A5017442765 @default.
• W2183670054 date "2001-01-01" @default.
• W2183670054 modified "2023-09-26" @default.
• W2183670054 title "AQUIFER CHEMISTRY AND MINERAL SATURATION IN SELECTED HIGH TEMPERATURE GEOTHERMAL AREAS" @default.
• W2183670054 cites W1995679645 @default.
• W2183670054 cites W1998704893 @default.
• W2183670054 cites W2005609972 @default.
• W2183670054 cites W2010230437 @default.
• W2183670054 cites W2010901956 @default.
• W2183670054 cites W2014583614 @default.
• W2183670054 cites W2018335072 @default.
• W2183670054 cites W2020629882 @default.
• W2183670054 cites W2031717627 @default.
• W2183670054 cites W2038865080 @default.
• W2183670054 cites W2051757039 @default.
• W2183670054 cites W2054371902 @default.
• W2183670054 cites W2056891847 @default.
• W2183670054 cites W2068656183 @default.
• W2183670054 cites W2068714502 @default.
• W2183670054 cites W2068764982 @default.
• W2183670054 cites W2072951499 @default.
• W2183670054 cites W2073594514 @default.
• W2183670054 cites W2077868379 @default.
• W2183670054 cites W2081477890 @default.
• W2183670054 cites W2084013960 @default.
• W2183670054 cites W2084266569 @default.
• W2183670054 cites W2090968131 @default.
• W2183670054 cites W2132198234 @default.
• W2183670054 cites W2558209344 @default.
• W2183670054 cites W2474686189 @default.
• W2183670054 hasPublicationYear "2001" @default.
• W2183670054 type Work @default.
• W2183670054 sameAs 2183670054 @default.
• W2183670054 citedByCount "1" @default.
• W2183670054 crossrefType "journal-article" @default.
• W2183670054 hasAuthorship W2183670054A5017442765 @default.
• W2183670054 hasConcept C127313418 @default.
• W2183670054 hasConcept C151730666 @default.
• W2183670054 hasConcept C17409809 @default.
• W2183670054 hasConcept C187320778 @default.
• W2183670054 hasConcept C199289684 @default.
• W2183670054 hasConcept C26687426 @default.
• W2183670054 hasConcept C2775859737 @default.
• W2183670054 hasConcept C2776008383 @default.
• W2183670054 hasConcept C2776044767 @default.
• W2183670054 hasConcept C2776062231 @default.
• W2183670054 hasConcept C2777163820 @default.
• W2183670054 hasConcept C2777844515 @default.
• W2183670054 hasConcept C2778357522 @default.
• W2183670054 hasConcept C2779229104 @default.
• W2183670054 hasConcept C2779870107 @default.
• W2183670054 hasConcept C2780191791 @default.
• W2183670054 hasConcept C75622301 @default.
• W2183670054 hasConcept C76177295 @default.
• W2183670054 hasConceptScore W2183670054C127313418 @default.
• W2183670054 hasConceptScore W2183670054C151730666 @default.
• W2183670054 hasConceptScore W2183670054C17409809 @default.
• W2183670054 hasConceptScore W2183670054C187320778 @default.
• W2183670054 hasConceptScore W2183670054C199289684 @default.
• W2183670054 hasConceptScore W2183670054C26687426 @default.
• W2183670054 hasConceptScore W2183670054C2775859737 @default.
• W2183670054 hasConceptScore W2183670054C2776008383 @default.
• W2183670054 hasConceptScore W2183670054C2776044767 @default.
• W2183670054 hasConceptScore W2183670054C2776062231 @default.
• W2183670054 hasConceptScore W2183670054C2777163820 @default.
• W2183670054 hasConceptScore W2183670054C2777844515 @default.
• W2183670054 hasConceptScore W2183670054C2778357522 @default.
• W2183670054 hasConceptScore W2183670054C2779229104 @default.
• W2183670054 hasConceptScore W2183670054C2779870107 @default.
• W2183670054 hasConceptScore W2183670054C2780191791 @default.
• W2183670054 hasConceptScore W2183670054C75622301 @default.
• W2183670054 hasConceptScore W2183670054C76177295 @default.
• W2183670054 hasLocation W21836700541 @default.
• W2183670054 hasOpenAccess W2183670054 @default.
• W2183670054 hasPrimaryLocation W21836700541 @default.
• W2183670054 hasRelatedWork W1533043850 @default.
• W2183670054 hasRelatedWork W1973081591 @default.
• W2183670054 hasRelatedWork W1995838521 @default.
• W2183670054 hasRelatedWork W2000110378 @default.
• W2183670054 hasRelatedWork W2006256852 @default.
• W2183670054 hasRelatedWork W2009486714 @default.
• W2183670054 hasRelatedWork W2032294533 @default.
• W2183670054 hasRelatedWork W2054009376 @default.
• W2183670054 hasRelatedWork W2068764982 @default.
• W2183670054 hasRelatedWork W2070156572 @default.
• W2183670054 hasRelatedWork W2074769848 @default.
• W2183670054 hasRelatedWork W2091754171 @default.
• W2183670054 hasRelatedWork W2129483939 @default.
• W2183670054 hasRelatedWork W2165771317 @default.
• W2183670054 hasRelatedWork W2182659835 @default.
• W2183670054 hasRelatedWork W2321042444 @default.
• W2183670054 hasRelatedWork W2483451748 @default.
• W2183670054 hasRelatedWork W2603652250 @default.
• W2183670054 hasRelatedWork W2772622420 @default.
• W2183670054 hasRelatedWork W3015609199 @default.
• W2183670054 isParatext "false" @default.
• W2183670054 isRetracted "false" @default.
• W2183670054 magId "2183670054" @default.

• next