FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2980197852> ?p ?o ?g. }

• W2980197852 endingPage "104953" @default.
• W2980197852 startingPage "104953" @default.
• W2980197852 abstract "In the present study, we combined stable isotopes and anthropogenic tracers to investigate the origin, residence times, and evolution of thermal waters in the Lonquimay-Tolhuaca Volcanic Complex (LTVC) of the southern Chilean Andes. A total of 20 water samples from springs discharging at a broad range of temperatures (8–96 °C) were collected and analyzed for major ion geochemistry, stable isotope ratios (δ2H, δ18O, δ13CTDIC), dissolved chlorofluorocarbons (CFCs) and sulfur hexafluoride (SF6). In addition, we compiled all available data on the isotopic composition of precipitation in the region to derive the local meteoric water line. Coupled with a Rayleigh-fractionation model of precipitation, we provide constraints on the elevation at which infiltration and recharge to the system is produced. δ13CTDIC values are consistent with the bulk of dissolved inorganic carbon being derived from the addition of soil CO2 to an atmospheric source, while magma degassing and boiling processes are evidenced in samples discharging directly on the flanks of volcanoes. The isotopic composition of thermal water, once heated at depth, is further modified by CO2 degassing and carbonate precipitation during ascent. All geothermal samples contain low but detectable concentrations of CFC-11, CFC-12, CFC-113, and SF6, suggesting the addition of only a small fraction (2–22%) of modern meteoric water. The discharge temperature of naturally outflowing springs in the LTVC correlates directly with the age distribution of the water samples. This difference in residence times is attributed to the distinct subsurface circulation pathways of each water type—i.e., the shallow, diffuse flow of cold groundwater vs. the deep, focused circulation of thermal water along fault zones. Conduit flow along high vertical permeability networks allows hydrothermal fluid to remain relatively unmixed with shallow meteoric water during ascent. Data from this study confirm that fault-fracture meshes with different orientations exert a first order control on the residence times, ascent, and mixing rates of thermal waters in this segment of the Andean Cordillera, thus modulating their chemical and isotopic signature. Additionally, our results show that the combined use of conventional hydrogeochemical and isotopic data with environmental tracers, including anthropogenic CFCs and SF6, is a powerful tool to better understand the dynamics of geothermal systems." @default.
• W2980197852 created "2019-10-18" @default.
• W2980197852 creator A5008005563 @default.
• W2980197852 creator A5011104625 @default.
• W2980197852 creator A5024751791 @default.
• W2980197852 creator A5030224049 @default.
• W2980197852 creator A5040535656 @default.
• W2980197852 creator A5089404804 @default.
• W2980197852 date "2021-05-01" @default.
• W2980197852 modified "2023-09-27" @default.
• W2980197852 title "Stable isotope and anthropogenic tracer signature of waters in an Andean geothermal system" @default.
• W2980197852 cites W1494156690 @default.
• W2980197852 cites W1585612743 @default.
• W2980197852 cites W1907316404 @default.
• W2980197852 cites W1965545777 @default.
• W2980197852 cites W1965935874 @default.
• W2980197852 cites W1967328673 @default.
• W2980197852 cites W1972600799 @default.
• W2980197852 cites W1980429770 @default.
• W2980197852 cites W1985949563 @default.
• W2980197852 cites W1987063203 @default.
• W2980197852 cites W1992524555 @default.
• W2980197852 cites W1998061454 @default.
• W2980197852 cites W2000500304 @default.
• W2980197852 cites W2000829620 @default.
• W2980197852 cites W2001987411 @default.
• W2980197852 cites W2005000310 @default.
• W2980197852 cites W2005435672 @default.
• W2980197852 cites W2007557785 @default.
• W2980197852 cites W2012179736 @default.
• W2980197852 cites W2016510161 @default.
• W2980197852 cites W2020555042 @default.
• W2980197852 cites W2024349823 @default.
• W2980197852 cites W2028347198 @default.
• W2980197852 cites W2030179080 @default.
• W2980197852 cites W2030283646 @default.
• W2980197852 cites W2035272526 @default.
• W2980197852 cites W2035967472 @default.
• W2980197852 cites W2040799203 @default.
• W2980197852 cites W2041852140 @default.
• W2980197852 cites W2043787408 @default.
• W2980197852 cites W2046610487 @default.
• W2980197852 cites W2049856409 @default.
• W2980197852 cites W2050910676 @default.
• W2980197852 cites W2051757039 @default.
• W2980197852 cites W2054980195 @default.
• W2980197852 cites W2058179313 @default.
• W2980197852 cites W2060393110 @default.
• W2980197852 cites W2062012791 @default.
• W2980197852 cites W2062197462 @default.
• W2980197852 cites W2067841165 @default.
• W2980197852 cites W2068444673 @default.
• W2980197852 cites W2070022169 @default.
• W2980197852 cites W2073115524 @default.
• W2980197852 cites W2077072904 @default.
• W2980197852 cites W2078544282 @default.
• W2980197852 cites W2085322438 @default.
• W2980197852 cites W2086136946 @default.
• W2980197852 cites W2090063629 @default.
• W2980197852 cites W2091824032 @default.
• W2980197852 cites W2093243001 @default.
• W2980197852 cites W2127938786 @default.
• W2980197852 cites W2131297790 @default.
• W2980197852 cites W2131546880 @default.
• W2980197852 cites W2132814790 @default.
• W2980197852 cites W2132828790 @default.
• W2980197852 cites W2141947981 @default.
• W2980197852 cites W2158100493 @default.
• W2980197852 cites W2160883425 @default.
• W2980197852 cites W2163463585 @default.
• W2980197852 cites W2166848208 @default.
• W2980197852 cites W2169991175 @default.
• W2980197852 cites W2172977821 @default.
• W2980197852 cites W2345413594 @default.
• W2980197852 cites W2349646370 @default.
• W2980197852 cites W2407590321 @default.
• W2980197852 cites W242216452 @default.
• W2980197852 cites W2564840613 @default.
• W2980197852 cites W2579969050 @default.
• W2980197852 cites W2606468197 @default.
• W2980197852 cites W2735282274 @default.
• W2980197852 cites W2757119532 @default.
• W2980197852 cites W2767654972 @default.
• W2980197852 cites W2794469311 @default.
• W2980197852 cites W2804039641 @default.
• W2980197852 doi "https://doi.org/10.1016/j.apgeochem.2021.104953" @default.
• W2980197852 hasPublicationYear "2021" @default.
• W2980197852 type Work @default.
• W2980197852 sameAs 2980197852 @default.
• W2980197852 citedByCount "4" @default.
• W2980197852 countsByYear W29801978522022 @default.
• W2980197852 countsByYear W29801978522023 @default.
• W2980197852 crossrefType "journal-article" @default.
• W2980197852 hasAuthorship W2980197852A5008005563 @default.
• W2980197852 hasAuthorship W2980197852A5011104625 @default.
• W2980197852 hasAuthorship W2980197852A5024751791 @default.
• W2980197852 hasAuthorship W2980197852A5030224049 @default.
• W2980197852 hasAuthorship W2980197852A5040535656 @default.

• next