FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2048658051> ?p ?o ?g. }

• W2048658051 endingPage "3732" @default.
• W2048658051 startingPage "3721" @default.
• W2048658051 abstract "There is a large body of evidence which indicates that the concentration of many aqueous components in shallow crustal waters is controlled at least in part by mineral-buffering, even at relatively low temperatures. Variations in temperature, pressure, and the total concentration of anionic charge, as reflected by variations in chlorinity and salinity, influence the relative proportions of dissolved cations in saline subsurface fluids. As salinity increases, the concentrations of rock-buffered divalent cations increase at a much greater rate than the concentration of monovalent cations, giving rise to: (1) the observed progression from Na-Cl to Na-Ca-Cl waters with increasing salinity in shallow crustal waters, and (2) nonlinear relations between the concentrations of individual cations and the concentration of chloride. This nonlinear behavior has the potential to induce water-rock reaction and mass transfer. The results of theoretical mass balance calculations performed to simulate the effects of advective-dispersive mixing of fluids of differing chlorinity on mass transfer in rock-buffered systems indicate that reactive transport should occur in any porous medium where there is a chlorinity gradient, even where molecular diffusion is the sole solute transport mechanism. In the hypothetical systems investigated, the calculated rates of fluid-mineral reaction are low during advection and dispersion when cation concentrations are a continuously fixed function of chloride concentration as a result of rock-buffering. A significantly greater degree of mass transfer could occur where mixing of waters of diverse salinity is conservative and cation concentrations are initially a function of physical mixing without reaction. In theory, large volumes of individual mineral phases could be dissolved or precipitated as a result of such mixing, without the need for the flow-through of large volumes of fluid, as fluid-mineral reactions attempt to rebuffer fluid compositions. Rates of mass transfer here would be dependent both on reaction kinetics and on rates of solute transport between reacting phases." @default.
• W2048658051 created "2016-06-24" @default.
• W2048658051 creator A5074863869 @default.
• W2048658051 date "2001-11-01" @default.
• W2048658051 modified "2023-09-24" @default.
• W2048658051 title "Reactive transport involving rock-buffered fluids of varying salinity" @default.
• W2048658051 cites W1969340698 @default.
• W2048658051 cites W1970266532 @default.
• W2048658051 cites W1970999811 @default.
• W2048658051 cites W1974608328 @default.
• W2048658051 cites W1975194082 @default.
• W2048658051 cites W1977091469 @default.
• W2048658051 cites W1981050513 @default.
• W2048658051 cites W1983211517 @default.
• W2048658051 cites W1992595066 @default.
• W2048658051 cites W1994454813 @default.
• W2048658051 cites W1996223327 @default.
• W2048658051 cites W1996892176 @default.
• W2048658051 cites W1998544358 @default.
• W2048658051 cites W2005767181 @default.
• W2048658051 cites W2013590391 @default.
• W2048658051 cites W2018957827 @default.
• W2048658051 cites W2022900900 @default.
• W2048658051 cites W2031557742 @default.
• W2048658051 cites W2045796990 @default.
• W2048658051 cites W2050655165 @default.
• W2048658051 cites W2050815362 @default.
• W2048658051 cites W2051757039 @default.
• W2048658051 cites W2052597986 @default.
• W2048658051 cites W2064796518 @default.
• W2048658051 cites W2068764982 @default.
• W2048658051 cites W2069672475 @default.
• W2048658051 cites W2077795626 @default.
• W2048658051 cites W2090968131 @default.
• W2048658051 cites W2113021229 @default.
• W2048658051 cites W2150861510 @default.
• W2048658051 cites W2332230385 @default.
• W2048658051 doi "https://doi.org/10.1016/s0016-7037(01)00703-7" @default.
• W2048658051 hasPublicationYear "2001" @default.
• W2048658051 type Work @default.
• W2048658051 sameAs 2048658051 @default.
• W2048658051 citedByCount "56" @default.
• W2048658051 countsByYear W20486580512012 @default.
• W2048658051 countsByYear W20486580512013 @default.
• W2048658051 countsByYear W20486580512014 @default.
• W2048658051 countsByYear W20486580512015 @default.
• W2048658051 countsByYear W20486580512016 @default.
• W2048658051 countsByYear W20486580512017 @default.
• W2048658051 countsByYear W20486580512018 @default.
• W2048658051 countsByYear W20486580512019 @default.
• W2048658051 countsByYear W20486580512021 @default.
• W2048658051 countsByYear W20486580512022 @default.
• W2048658051 countsByYear W20486580512023 @default.
• W2048658051 crossrefType "journal-article" @default.
• W2048658051 hasAuthorship W2048658051A5074863869 @default.
• W2048658051 hasConcept C111368507 @default.
• W2048658051 hasConcept C120665830 @default.
• W2048658051 hasConcept C121332964 @default.
• W2048658051 hasConcept C127313418 @default.
• W2048658051 hasConcept C129513315 @default.
• W2048658051 hasConcept C138777275 @default.
• W2048658051 hasConcept C147789679 @default.
• W2048658051 hasConcept C177562468 @default.
• W2048658051 hasConcept C178790620 @default.
• W2048658051 hasConcept C184651966 @default.
• W2048658051 hasConcept C185592680 @default.
• W2048658051 hasConcept C199289684 @default.
• W2048658051 hasConcept C2776371256 @default.
• W2048658051 hasConcept C2778695967 @default.
• W2048658051 hasConcept C43617362 @default.
• W2048658051 hasConcept C5072599 @default.
• W2048658051 hasConcept C51038369 @default.
• W2048658051 hasConcept C62520636 @default.
• W2048658051 hasConcept C69357855 @default.
• W2048658051 hasConcept C74884574 @default.
• W2048658051 hasConcept C97355855 @default.
• W2048658051 hasConceptScore W2048658051C111368507 @default.
• W2048658051 hasConceptScore W2048658051C120665830 @default.
• W2048658051 hasConceptScore W2048658051C121332964 @default.
• W2048658051 hasConceptScore W2048658051C127313418 @default.
• W2048658051 hasConceptScore W2048658051C129513315 @default.
• W2048658051 hasConceptScore W2048658051C138777275 @default.
• W2048658051 hasConceptScore W2048658051C147789679 @default.
• W2048658051 hasConceptScore W2048658051C177562468 @default.
• W2048658051 hasConceptScore W2048658051C178790620 @default.
• W2048658051 hasConceptScore W2048658051C184651966 @default.
• W2048658051 hasConceptScore W2048658051C185592680 @default.
• W2048658051 hasConceptScore W2048658051C199289684 @default.
• W2048658051 hasConceptScore W2048658051C2776371256 @default.
• W2048658051 hasConceptScore W2048658051C2778695967 @default.
• W2048658051 hasConceptScore W2048658051C43617362 @default.
• W2048658051 hasConceptScore W2048658051C5072599 @default.
• W2048658051 hasConceptScore W2048658051C51038369 @default.
• W2048658051 hasConceptScore W2048658051C62520636 @default.
• W2048658051 hasConceptScore W2048658051C69357855 @default.
• W2048658051 hasConceptScore W2048658051C74884574 @default.
• W2048658051 hasConceptScore W2048658051C97355855 @default.
• W2048658051 hasIssue "21" @default.

• next