FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W826218353> ?p ?o ?g. }

• W826218353 endingPage "20" @default.
• W826218353 startingPage "9" @default.
• W826218353 abstract "This research assesses the thermodynamic consistency of recent marine CO2 system measurements in United States coastal waters. As one means of assessment, we compared aragonite saturation states calculated using various combinations of measured parameters. We also compared directly measured and calculated values of total alkalinity and CO2 fugacity. The primary data set consists of state-of-the-art measurements of the keystone parameters of the marine CO2 system: dissolved inorganic carbon (DIC), total alkalinity (TA), CO2 fugacity (fCO2), and pH. This study is the first thermodynamic CO2 system intercomparison based on measurements obtained using purified meta cresol purple as a pH indicator. The data are from 1890 water samples collected during NOAA's West Coast Ocean Acidification Cruise of 2011 (WCOA2011) and NOAA's Gulf of Mexico and East Coast Carbon Cruise of 2012 (GOMECC-2). Calculations of in situ aragonite saturation states (ΩA) near the saturation horizon exhibited differences on the order of ± 10% between predictions based on the (DIC, TA) pair of measurements vs. the (pH, DIC), (fCO2, DIC), or (fCO2, pH) pairs. Differences of this magnitude, which are largely attributable to the imprecision of ΩA calculated from the (DIC, TA) pair, are roughly equivalent to the magnitude of ΩA change projected to occur over the next several decades due to ocean acidification. These observations highlight the importance of including either pH or fCO2 in saturation state calculations. Calculations of TA from (pH, DIC) and (fCO2, DIC) showed that internal consistency could be achieved if minor subtractions of TA (≤ 4 μmol kg− 1) were applied to samples of salinity < 35. The extent of thermodynamic consistency is also exemplified by the small offset between TA calculated from (DIC, pH) and that calculated from (DIC, fCO2): ~ 3 μmol kg− 1, which is similar to the accuracy of the TA measurements. Systematic trends can be detected in the offsets between measured and calculated parameters, but for this high-quality data set the magnitude of methodological improvements required to achieve exact thermodynamic consistency is quite small." @default.
• W826218353 created "2016-06-24" @default.
• W826218353 creator A5019328347 @default.
• W826218353 creator A5026236427 @default.
• W826218353 creator A5059484084 @default.
• W826218353 creator A5062468987 @default.
• W826218353 creator A5075828760 @default.
• W826218353 date "2015-11-01" @default.
• W826218353 modified "2023-10-11" @default.
• W826218353 title "Internal consistency of marine carbonate system measurements and assessments of aragonite saturation state: Insights from two U.S. coastal cruises" @default.
• W826218353 cites W1526060631 @default.
• W826218353 cites W1540137853 @default.
• W826218353 cites W1649510910 @default.
• W826218353 cites W1662180232 @default.
• W826218353 cites W1967525859 @default.
• W826218353 cites W1970231993 @default.
• W826218353 cites W1977870567 @default.
• W826218353 cites W1979260633 @default.
• W826218353 cites W1981451061 @default.
• W826218353 cites W1986635986 @default.
• W826218353 cites W1990250430 @default.
• W826218353 cites W2002308261 @default.
• W826218353 cites W2002573490 @default.
• W826218353 cites W2023508473 @default.
• W826218353 cites W2023633170 @default.
• W826218353 cites W2025878918 @default.
• W826218353 cites W2026653904 @default.
• W826218353 cites W2030087307 @default.
• W826218353 cites W2030604405 @default.
• W826218353 cites W2031854984 @default.
• W826218353 cites W2033233017 @default.
• W826218353 cites W2034735472 @default.
• W826218353 cites W2049078437 @default.
• W826218353 cites W2050103984 @default.
• W826218353 cites W2058270112 @default.
• W826218353 cites W2058809270 @default.
• W826218353 cites W2060128334 @default.
• W826218353 cites W2062323967 @default.
• W826218353 cites W2068375361 @default.
• W826218353 cites W2076025165 @default.
• W826218353 cites W2081006552 @default.
• W826218353 cites W2082344533 @default.
• W826218353 cites W2085167193 @default.
• W826218353 cites W2087524325 @default.
• W826218353 cites W2111645094 @default.
• W826218353 cites W2113297575 @default.
• W826218353 cites W2117052580 @default.
• W826218353 cites W2125776675 @default.
• W826218353 cites W2133305189 @default.
• W826218353 cites W2144920118 @default.
• W826218353 cites W2147331520 @default.
• W826218353 cites W2153455362 @default.
• W826218353 cites W2154356323 @default.
• W826218353 cites W2159816121 @default.
• W826218353 cites W2164586302 @default.
• W826218353 cites W2173001546 @default.
• W826218353 cites W2331859108 @default.
• W826218353 doi "https://doi.org/10.1016/j.marchem.2015.06.022" @default.
• W826218353 hasPublicationYear "2015" @default.
• W826218353 type Work @default.
• W826218353 sameAs 826218353 @default.
• W826218353 citedByCount "44" @default.
• W826218353 countsByYear W8262183532015 @default.
• W826218353 countsByYear W8262183532016 @default.
• W826218353 countsByYear W8262183532017 @default.
• W826218353 countsByYear W8262183532018 @default.
• W826218353 countsByYear W8262183532019 @default.
• W826218353 countsByYear W8262183532020 @default.
• W826218353 countsByYear W8262183532021 @default.
• W826218353 countsByYear W8262183532022 @default.
• W826218353 countsByYear W8262183532023 @default.
• W826218353 crossrefType "journal-article" @default.
• W826218353 hasAuthorship W826218353A5019328347 @default.
• W826218353 hasAuthorship W826218353A5026236427 @default.
• W826218353 hasAuthorship W826218353A5059484084 @default.
• W826218353 hasAuthorship W826218353A5062468987 @default.
• W826218353 hasAuthorship W826218353A5075828760 @default.
• W826218353 hasConcept C111368507 @default.
• W826218353 hasConcept C114614502 @default.
• W826218353 hasConcept C127313418 @default.
• W826218353 hasConcept C129513315 @default.
• W826218353 hasConcept C147789679 @default.
• W826218353 hasConcept C148318117 @default.
• W826218353 hasConcept C178790620 @default.
• W826218353 hasConcept C179104552 @default.
• W826218353 hasConcept C185592680 @default.
• W826218353 hasConcept C197248824 @default.
• W826218353 hasConcept C19829342 @default.
• W826218353 hasConcept C199289684 @default.
• W826218353 hasConcept C2779866092 @default.
• W826218353 hasConcept C2780659211 @default.
• W826218353 hasConcept C2780828025 @default.
• W826218353 hasConcept C33923547 @default.
• W826218353 hasConcept C36574619 @default.
• W826218353 hasConcept C39432304 @default.
• W826218353 hasConcept C45812177 @default.
• W826218353 hasConcept C530467964 @default.
• W826218353 hasConcept C85084404 @default.

• next