Water flux and reverse salt flux

dc.authorscopusid23477399300
dc.authorscopusid35795160600
dc.authorscopusid35795402300
dc.authorscopusid57215893742
dc.contributor.authorKoseoglu,H.
dc.contributor.authorGuler,E.
dc.contributor.authorHarman,B.I.
dc.contributor.authorGonulsuz,E.
dc.contributor.otherChemical Engineering
dc.date.accessioned2024-07-05T15:45:18Z
dc.date.available2024-07-05T15:45:18Z
dc.date.issued2018
dc.departmentAtılım Universityen_US
dc.department-tempKoseoglu H., Suleyman Demirel University, Isparta, Turkey; Guler E., Atilim University, Ankara, Turkey; Harman B.I., Suleyman Demirel University, Isparta, Turkey; Gonulsuz E., Suleyman Demirel University, Isparta, Turkeyen_US
dc.description.abstractFollowing the increase in the world population and the demand for economic development, the need for energy has increased day by day. Rapidly increasing global energy consumption is supplied mainly by fossil fuels bearing the risk of exhaustion with decreasing reserves, which now have the effect of carbon emissions and greenhouse gases. These concerns lead humanity to significantly reduce the use of fossil fuels. Salinity gradient energy (SGP), a type of hydroelectric energy, also has a high potential to displace fossil fuels. SGP is less periodic than sources like wind and solar energy. The osmotic pressure gradient energy uses the released energy during mixing of the water currents with different salinity The Gibbs free energy from mixing two solutions of different concentrations is an unnoticed source of energy. Salinity gradient energy, also referred to as osmotic energy or blue energy, can be derived from natural sources such as clean river water, salt water, and desalination of seawater. Various approaches have been developed to capture salinity gradient energy, but the most promising are pressure-retarded osmosis (PRO), reverse electrodialysis (RED) and forward osmosis (FO) processes. In this chapter theoretical approaches derived from the current literature is presented for the deep conceptual understanding of the water flux and reverse salt flux issues. © 2018 Elsevier B.V. All rights reserved.en_US
dc.identifier.citation11
dc.identifier.doi10.1016/B978-0-444-63961-5.00002-X
dc.identifier.endpage86en_US
dc.identifier.isbn978-044463961-5
dc.identifier.isbn978-044463962-2
dc.identifier.scopus2-s2.0-85082291393
dc.identifier.startpage57en_US
dc.identifier.urihttps://doi.org/10.1016/B978-0-444-63961-5.00002-X
dc.identifier.urihttps://hdl.handle.net/20.500.14411/3898
dc.institutionauthorGüler, Enver
dc.language.isoenen_US
dc.publisherElsevieren_US
dc.relation.ispartofMembrane-Based Salinity Gradient Processes for Water Treatment and Power Generationen_US
dc.relation.publicationcategoryKitap Bölümü - Uluslararasıen_US
dc.rightsinfo:eu-repo/semantics/closedAccessen_US
dc.subjectForward osmosisen_US
dc.subjectPressure retarded osmosisen_US
dc.subjectReverse electrodialysisen_US
dc.subjectReverse salt fluxen_US
dc.subjectSalinity gradient energyen_US
dc.subjectWater fluxen_US
dc.titleWater flux and reverse salt fluxen_US
dc.typeBook Parten_US
dspace.entity.typePublication
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