Matches in SemOpenAlex for { <https://semopenalex.org/work/W2382316268> ?p ?o ?g. }
Showing items 1 to 79 of
79
with 100 items per page.
- W2382316268 abstract "After sampling and analyzing carbon isotope(δ13CDIC) and oxygen isotope(δ18O) in subterranean river and large karst springs in Guilin,Guangxi Zhuang Autonomous Region,southwest China,we found:(a) the carbon isotopic(δ13CDIC) values in subterranean river ranged from –15.99‰ to –12.29‰,with a mean value of(–14.03± 1.15)‰;and oxygen isotope(δ18O) values ranged from –6.63‰ to –5.64‰,with a mean value of(–6.24±0.24)‰;the carbon isotopic(δ13CDIC) values in large karst springs ranged from –15.26‰ to –9.22‰,with a mean value of(–12.05±1.57)‰;and oxygen isotope(δ18O) values ranged from –6.97‰ to –3.19‰,with a mean value of(–5.68±0.97)‰;(b) the carbon isotopic(δ13CDIC) and oxygen isotope(δ18O) values in subterranean river were generally lower than those in large karst springs;(c) the water circulation caused the isotopic differences in difference types of water.In subterranean river,water is in the form of conduit flow,with a fast rate of cycle and a short time of water-rock interaction.Therefore,little heavy carbon isotope(δ13CDIC) came from carbonatite rock to the water,with a short time of distillation process,so the carbon isotope(δ13CDIC) is light.In contrast,water in large karst springs is fissure flow,with a slow circulation rate and a long water-rock time,which lead more heavy HUANG Qi-bo et al.: Carbon and oxygen isotopes in karst water in Guilin carbon isotope came from carbonatite rock to the water,furthermore,its distillation process time is longer,so the carbon isotope(δ13CDIC) is heavy.δ13CDIC valued with the same situation as Sr/Ca,it could reflect the run-off condition of groundwater to some degree." @default.
- W2382316268 created "2016-06-24" @default.
- W2382316268 creator A5074118187 @default.
- W2382316268 date "2013-01-01" @default.
- W2382316268 modified "2023-09-25" @default.
- W2382316268 title "The characteristic and significance of carbon isotope (δ~(13)C_(DIC)) and oxygen isotope (δ~(18)O) value in different type of karst water in Guilin" @default.
- W2382316268 hasPublicationYear "2013" @default.
- W2382316268 type Work @default.
- W2382316268 sameAs 2382316268 @default.
- W2382316268 citedByCount "0" @default.
- W2382316268 crossrefType "journal-article" @default.
- W2382316268 hasAuthorship W2382316268A5074118187 @default.
- W2382316268 hasConcept C104779481 @default.
- W2382316268 hasConcept C107872376 @default.
- W2382316268 hasConcept C121332964 @default.
- W2382316268 hasConcept C127313418 @default.
- W2382316268 hasConcept C140205800 @default.
- W2382316268 hasConcept C151730666 @default.
- W2382316268 hasConcept C158787203 @default.
- W2382316268 hasConcept C159985019 @default.
- W2382316268 hasConcept C17409809 @default.
- W2382316268 hasConcept C182348080 @default.
- W2382316268 hasConcept C185059815 @default.
- W2382316268 hasConcept C185592680 @default.
- W2382316268 hasConcept C187320778 @default.
- W2382316268 hasConcept C192562407 @default.
- W2382316268 hasConcept C22117777 @default.
- W2382316268 hasConcept C62520636 @default.
- W2382316268 hasConcept C69384203 @default.
- W2382316268 hasConcept C71468253 @default.
- W2382316268 hasConcept C76462348 @default.
- W2382316268 hasConcept C76886044 @default.
- W2382316268 hasConceptScore W2382316268C104779481 @default.
- W2382316268 hasConceptScore W2382316268C107872376 @default.
- W2382316268 hasConceptScore W2382316268C121332964 @default.
- W2382316268 hasConceptScore W2382316268C127313418 @default.
- W2382316268 hasConceptScore W2382316268C140205800 @default.
- W2382316268 hasConceptScore W2382316268C151730666 @default.
- W2382316268 hasConceptScore W2382316268C158787203 @default.
- W2382316268 hasConceptScore W2382316268C159985019 @default.
- W2382316268 hasConceptScore W2382316268C17409809 @default.
- W2382316268 hasConceptScore W2382316268C182348080 @default.
- W2382316268 hasConceptScore W2382316268C185059815 @default.
- W2382316268 hasConceptScore W2382316268C185592680 @default.
- W2382316268 hasConceptScore W2382316268C187320778 @default.
- W2382316268 hasConceptScore W2382316268C192562407 @default.
- W2382316268 hasConceptScore W2382316268C22117777 @default.
- W2382316268 hasConceptScore W2382316268C62520636 @default.
- W2382316268 hasConceptScore W2382316268C69384203 @default.
- W2382316268 hasConceptScore W2382316268C71468253 @default.
- W2382316268 hasConceptScore W2382316268C76462348 @default.
- W2382316268 hasConceptScore W2382316268C76886044 @default.
- W2382316268 hasLocation W23823162681 @default.
- W2382316268 hasOpenAccess W2382316268 @default.
- W2382316268 hasPrimaryLocation W23823162681 @default.
- W2382316268 hasRelatedWork W1971587256 @default.
- W2382316268 hasRelatedWork W1973871485 @default.
- W2382316268 hasRelatedWork W1978096088 @default.
- W2382316268 hasRelatedWork W1987259353 @default.
- W2382316268 hasRelatedWork W1987867521 @default.
- W2382316268 hasRelatedWork W1988748362 @default.
- W2382316268 hasRelatedWork W2023802966 @default.
- W2382316268 hasRelatedWork W2024905997 @default.
- W2382316268 hasRelatedWork W2056400575 @default.
- W2382316268 hasRelatedWork W2347529655 @default.
- W2382316268 hasRelatedWork W2350076405 @default.
- W2382316268 hasRelatedWork W2360751924 @default.
- W2382316268 hasRelatedWork W2361760029 @default.
- W2382316268 hasRelatedWork W2375315227 @default.
- W2382316268 hasRelatedWork W2376365415 @default.
- W2382316268 hasRelatedWork W2418525279 @default.
- W2382316268 hasRelatedWork W2436410850 @default.
- W2382316268 hasRelatedWork W2733235710 @default.
- W2382316268 hasRelatedWork W2953757382 @default.
- W2382316268 hasRelatedWork W3133213728 @default.
- W2382316268 isParatext "false" @default.
- W2382316268 isRetracted "false" @default.
- W2382316268 magId "2382316268" @default.
- W2382316268 workType "article" @default.