A computer program for the simulation of evaporation of natural waters to high concentration
EQL/EVP is a FORTRAN 90 program that simulates the evaporation of dilute waters as well as concentrated brines. The code calculates stepwise the composition of the evaporated solution and the amounts of precipitated minerals. Activity coefficients are based on the Pitzer's interaction model whi...
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Veröffentlicht in: | Computers & geosciences 2001-03, Vol.27 (2), p.191-201 |
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description | EQL/EVP is a FORTRAN 90 program that simulates the evaporation of dilute waters as well as concentrated brines. The code calculates stepwise the composition of the evaporated solution and the amounts of precipitated minerals. Activity coefficients are based on the Pitzer's interaction model which allows calculation to high ionic strength. The Newton–Raphson method is used to solve a set of linear mass-balance and non-linear mass-action equations. The simulation may be carried out in equilibrium mode where minerals are allowed to redissolve into the solution or in fractional crystallization mode where minerals are removed as they precipitate. Temperature dependence of various parameters and mineral solubility products are tentatively included between 0 and 50°C. The code processes all invariant points: those where the activity of water is constrained by several minerals and the invariant end-points. The code may be a useful tool for understanding hydrological and geochemical processes in arid regions. |
doi_str_mv | 10.1016/S0098-3004(00)00100-X |
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The code calculates stepwise the composition of the evaporated solution and the amounts of precipitated minerals. Activity coefficients are based on the Pitzer's interaction model which allows calculation to high ionic strength. The Newton–Raphson method is used to solve a set of linear mass-balance and non-linear mass-action equations. The simulation may be carried out in equilibrium mode where minerals are allowed to redissolve into the solution or in fractional crystallization mode where minerals are removed as they precipitate. Temperature dependence of various parameters and mineral solubility products are tentatively included between 0 and 50°C. The code processes all invariant points: those where the activity of water is constrained by several minerals and the invariant end-points. The code may be a useful tool for understanding hydrological and geochemical processes in arid regions.</description><identifier>ISSN: 0098-3004</identifier><identifier>EISSN: 1873-7803</identifier><identifier>DOI: 10.1016/S0098-3004(00)00100-X</identifier><language>eng</language><publisher>Oxford: Elsevier Ltd</publisher><subject>Brine ; Earth sciences ; Earth, ocean, space ; Evaporation ; Evaporite ; Exact sciences and technology ; Geochemistry ; Hydrology ; Hydrology. 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The code calculates stepwise the composition of the evaporated solution and the amounts of precipitated minerals. Activity coefficients are based on the Pitzer's interaction model which allows calculation to high ionic strength. The Newton–Raphson method is used to solve a set of linear mass-balance and non-linear mass-action equations. The simulation may be carried out in equilibrium mode where minerals are allowed to redissolve into the solution or in fractional crystallization mode where minerals are removed as they precipitate. Temperature dependence of various parameters and mineral solubility products are tentatively included between 0 and 50°C. The code processes all invariant points: those where the activity of water is constrained by several minerals and the invariant end-points. The code may be a useful tool for understanding hydrological and geochemical processes in arid regions.</description><subject>Brine</subject><subject>Earth sciences</subject><subject>Earth, ocean, space</subject><subject>Evaporation</subject><subject>Evaporite</subject><subject>Exact sciences and technology</subject><subject>Geochemistry</subject><subject>Hydrology</subject><subject>Hydrology. Hydrogeology</subject><subject>Invariant point</subject><subject>Mineralogy</subject><subject>Silicates</subject><subject>Simulation</subject><subject>Water geochemistry</subject><issn>0098-3004</issn><issn>1873-7803</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2001</creationdate><recordtype>article</recordtype><recordid>eNqFkM1KxDAURoMoOI4-ghAQRBfVmzbTpiuRwT8YcKHCLIRwJ02dSNvUJFV8e-NUZusqJJzvfjeHkGMGFwxYfvkEUIokA-BnAOcADCBZ7pAJE0WWFAKyXTLZIvvkwPt3AEhTMZuQ12uqbNsPQTvaO_vmsKW1dTSsNfWmHRoMxnbU1lR_Ym_d9tphGBw29Atj1NNg6dq8reOwTukujNwh2aux8fro75ySl9ub5_l9sni8e5hfLxLkKYSk4BrzskyRCVZDHjcWStRKxTcO5aoSiJrplVIccZVlPCsKVVZlpcoZr1U1y6bkdJwbf_AxaB9ka7zSTYOdtoOXaZ7nUUP6L8hiN-epiOBsBJWz3jtdy96ZFt23ZCB_pcuNdPlrVALIjXS5jLmTvwL0CpvaYaeM34ZFwRjkkboaKR2lfBrtpFdGR3GVcVoFWVnzT88PreeXKg</recordid><startdate>20010301</startdate><enddate>20010301</enddate><creator>Risacher, François</creator><creator>Clement, Alain</creator><general>Elsevier Ltd</general><general>Elsevier Science</general><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7UA</scope><scope>C1K</scope><scope>8FD</scope><scope>FR3</scope><scope>KR7</scope></search><sort><creationdate>20010301</creationdate><title>A computer program for the simulation of evaporation of natural waters to high concentration</title><author>Risacher, François ; Clement, Alain</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a420t-74ea6992a181f067808c8fcc699409bd8aae1ebcc4aab334377c9d9dc954fcd53</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2001</creationdate><topic>Brine</topic><topic>Earth sciences</topic><topic>Earth, ocean, space</topic><topic>Evaporation</topic><topic>Evaporite</topic><topic>Exact sciences and technology</topic><topic>Geochemistry</topic><topic>Hydrology</topic><topic>Hydrology. Hydrogeology</topic><topic>Invariant point</topic><topic>Mineralogy</topic><topic>Silicates</topic><topic>Simulation</topic><topic>Water geochemistry</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Risacher, François</creatorcontrib><creatorcontrib>Clement, Alain</creatorcontrib><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>Water Resources Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><collection>Technology Research Database</collection><collection>Engineering Research Database</collection><collection>Civil Engineering Abstracts</collection><jtitle>Computers & geosciences</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Risacher, François</au><au>Clement, Alain</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>A computer program for the simulation of evaporation of natural waters to high concentration</atitle><jtitle>Computers & geosciences</jtitle><date>2001-03-01</date><risdate>2001</risdate><volume>27</volume><issue>2</issue><spage>191</spage><epage>201</epage><pages>191-201</pages><issn>0098-3004</issn><eissn>1873-7803</eissn><abstract>EQL/EVP is a FORTRAN 90 program that simulates the evaporation of dilute waters as well as concentrated brines. The code calculates stepwise the composition of the evaporated solution and the amounts of precipitated minerals. Activity coefficients are based on the Pitzer's interaction model which allows calculation to high ionic strength. The Newton–Raphson method is used to solve a set of linear mass-balance and non-linear mass-action equations. The simulation may be carried out in equilibrium mode where minerals are allowed to redissolve into the solution or in fractional crystallization mode where minerals are removed as they precipitate. Temperature dependence of various parameters and mineral solubility products are tentatively included between 0 and 50°C. The code processes all invariant points: those where the activity of water is constrained by several minerals and the invariant end-points. 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subjects | Brine Earth sciences Earth, ocean, space Evaporation Evaporite Exact sciences and technology Geochemistry Hydrology Hydrology. Hydrogeology Invariant point Mineralogy Silicates Simulation Water geochemistry |
title | A computer program for the simulation of evaporation of natural waters to high concentration |
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