Matches in SemOpenAlex for { <https://semopenalex.org/work/W4283274922> ?p ?o ?g. }
- W4283274922 endingPage "845" @default.
- W4283274922 startingPage "845" @default.
- W4283274922 abstract "Strontium (Sr), hydrogen (H) and oxygen (O) in vent fluids are important for understanding the water–rock interaction and hydrothermal flux in hydrothermal systems. We have analyzed the Sr, H and O isotopic compositions of seawater, vent fluid and hydrothermal plume samples in the Kueishantao hydrothermal field, as well as their calcium (Ca), total sulfur (S), Sr, arsenic (As), stibium (Sb), chlorine (Cl) and manganese (Mn) concentrations for understanding the origin and processes of fluids. The results suggest that most As, Sb and Mn are leached from andesitic rocks into the fluids, and most Ca and Cl remained in the deep reaction zone during the fluid–andesitic rock interaction. The ranges of 87Sr/86Sr, δDV-SMOW and δ18OV-SMOW values in the yellow spring, white spring and plumes are small. The 87Sr/86Sr, δDV-SMOW and δ18OV-SMOW values of fluids and plumes are like those of ambient seawater, indicating that the Sr, H and O of vent fluids and hydrothermal plumes are derived primarily from seawater. This suggests that the interaction of andesite and subseafloor fluid is of short duration and results in the majority of As, Sb and Mn being released into fluids, while most Ca and Cl remained in the deep reaction zone. In addition, there was no significant variation of Sr, H and O isotopic compositions in the upwelling fluid, keeping the similar isotopic compositions of seawater. There are obvious correlations among the pH values, As and Sb concentrations, and H isotopic compositions of the vent fluids and hydrothermal plumes, implying that the As and Sb concentrations and H isotopic compositions can trace the dispersion of plumes in the ambient seawater. According to the Sr concentrations and 87Sr/86Sr values, the water/rock ratios are 3076~8124, which is consistent with the idea that the interaction between fluid and andesite at the subseafloor is of short duration. The hydrothermal flux of Sr discharged from the yellow spring into the seawater is between 2.06 × 104 and 2.26 × 104 mol/yr, and the white spring discharges 1.18 × 104~1.26 × 104 mol/yr Sr if just andesites appear in the reaction zone." @default.
- W4283274922 created "2022-06-23" @default.
- W4283274922 creator A5011881849 @default.
- W4283274922 creator A5025335800 @default.
- W4283274922 creator A5032656306 @default.
- W4283274922 creator A5049317673 @default.
- W4283274922 creator A5091092455 @default.
- W4283274922 creator A5091914620 @default.
- W4283274922 date "2022-06-21" @default.
- W4283274922 modified "2023-09-28" @default.
- W4283274922 title "Strontium, Hydrogen and Oxygen Behavior in Vent Fluids and Plumes from the Kueishantao Hydrothermal Field Offshore Northeast Taiwan: Constrained by Fluid Processes" @default.
- W4283274922 cites W1827152615 @default.
- W4283274922 cites W1964831515 @default.
- W4283274922 cites W1970552011 @default.
- W4283274922 cites W1971927067 @default.
- W4283274922 cites W1972289882 @default.
- W4283274922 cites W1975082598 @default.
- W4283274922 cites W1978854741 @default.
- W4283274922 cites W1979617515 @default.
- W4283274922 cites W1981823920 @default.
- W4283274922 cites W1984446286 @default.
- W4283274922 cites W1990732046 @default.
- W4283274922 cites W1999514717 @default.
- W4283274922 cites W1999898881 @default.
- W4283274922 cites W2001683255 @default.
- W4283274922 cites W2005106227 @default.
- W4283274922 cites W2006949523 @default.
- W4283274922 cites W2010834477 @default.
- W4283274922 cites W2014343207 @default.
- W4283274922 cites W2022476159 @default.
- W4283274922 cites W2026184025 @default.
- W4283274922 cites W2026191004 @default.
- W4283274922 cites W2030666288 @default.
- W4283274922 cites W2036348046 @default.
- W4283274922 cites W2036506737 @default.
- W4283274922 cites W2045466477 @default.
- W4283274922 cites W2050633812 @default.
- W4283274922 cites W2050953969 @default.
- W4283274922 cites W2058382324 @default.
- W4283274922 cites W2058585304 @default.
- W4283274922 cites W2068435319 @default.
- W4283274922 cites W2069126749 @default.
- W4283274922 cites W2073550547 @default.
- W4283274922 cites W2085152057 @default.
- W4283274922 cites W2088305435 @default.
- W4283274922 cites W2091079709 @default.
- W4283274922 cites W2091429053 @default.
- W4283274922 cites W2097622004 @default.
- W4283274922 cites W2118168812 @default.
- W4283274922 cites W2128507582 @default.
- W4283274922 cites W2160980032 @default.
- W4283274922 cites W2176678440 @default.
- W4283274922 cites W2475410347 @default.
- W4283274922 cites W2557452860 @default.
- W4283274922 cites W2767945588 @default.
- W4283274922 cites W2796526633 @default.
- W4283274922 cites W2888380490 @default.
- W4283274922 cites W2985815981 @default.
- W4283274922 cites W4200079629 @default.
- W4283274922 cites W4253092410 @default.
- W4283274922 cites W965761834 @default.
- W4283274922 doi "https://doi.org/10.3390/jmse10070845" @default.
- W4283274922 hasPublicationYear "2022" @default.
- W4283274922 type Work @default.
- W4283274922 citedByCount "2" @default.
- W4283274922 countsByYear W42832749222022 @default.
- W4283274922 countsByYear W42832749222023 @default.
- W4283274922 crossrefType "journal-article" @default.
- W4283274922 hasAuthorship W4283274922A5011881849 @default.
- W4283274922 hasAuthorship W4283274922A5025335800 @default.
- W4283274922 hasAuthorship W4283274922A5032656306 @default.
- W4283274922 hasAuthorship W4283274922A5049317673 @default.
- W4283274922 hasAuthorship W4283274922A5091092455 @default.
- W4283274922 hasAuthorship W4283274922A5091914620 @default.
- W4283274922 hasBestOaLocation W42832749221 @default.
- W4283274922 hasConcept C111368507 @default.
- W4283274922 hasConcept C120806208 @default.
- W4283274922 hasConcept C121332964 @default.
- W4283274922 hasConcept C127313418 @default.
- W4283274922 hasConcept C137581210 @default.
- W4283274922 hasConcept C156622251 @default.
- W4283274922 hasConcept C165205528 @default.
- W4283274922 hasConcept C17409809 @default.
- W4283274922 hasConcept C178790620 @default.
- W4283274922 hasConcept C185592680 @default.
- W4283274922 hasConcept C1898230 @default.
- W4283274922 hasConcept C192241223 @default.
- W4283274922 hasConcept C197248824 @default.
- W4283274922 hasConcept C199289684 @default.
- W4283274922 hasConcept C2775840915 @default.
- W4283274922 hasConcept C36986328 @default.
- W4283274922 hasConcept C518915863 @default.
- W4283274922 hasConcept C97355855 @default.
- W4283274922 hasConceptScore W4283274922C111368507 @default.
- W4283274922 hasConceptScore W4283274922C120806208 @default.
- W4283274922 hasConceptScore W4283274922C121332964 @default.
- W4283274922 hasConceptScore W4283274922C127313418 @default.
- W4283274922 hasConceptScore W4283274922C137581210 @default.