2016
DOI: 10.1016/j.desal.2016.05.006
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Kinetics of dolomite dissolution in a packed bed by acidified desalinated water

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Cited by 15 publications
(7 citation statements)
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“…The dissolution of dolomite is a function of pH, moreover, the fractionation of carbonate rocks is also influenced by water pH [ 34 ]. Greiserman [ 35 ] also reported similar observation where the dissolution of dolomite into calcium and magnesium ions were effective in acidic medium. These studies are in line with this current study that, high concentration of magnesium ions in water suggest non-optimal pH and that the availability of magnesium in water especially in groundwater system is influenced by pH.…”
Section: Discussionmentioning
confidence: 73%
“…The dissolution of dolomite is a function of pH, moreover, the fractionation of carbonate rocks is also influenced by water pH [ 34 ]. Greiserman [ 35 ] also reported similar observation where the dissolution of dolomite into calcium and magnesium ions were effective in acidic medium. These studies are in line with this current study that, high concentration of magnesium ions in water suggest non-optimal pH and that the availability of magnesium in water especially in groundwater system is influenced by pH.…”
Section: Discussionmentioning
confidence: 73%
“…Rocks and minerals are commonly used in various applications of environmental engineering. In water technology and protection, these are used as adsorbents and ion exchangers [1-5], filter media [6,7], remineralizing and deacidifying materials [8,9], coagulant aids [7], as well as substrates for the production of inorganic membranes [10][11][12] or sorbents for removal of petroleum substances [13]. In groundwater treatment, the filtration systems are a technical representation of the natural processes that occur between water components and rock material.…”
Section: Introductionmentioning
confidence: 99%
“…However, such application is both costly and in case of MgCl 2(s) the resulting added Cl − concentration surpasses the allowed Cl − threshold. Several processes have been suggested in recent years for supplying Mg 2+ to desalinated water, based on either dissolution of dolomite [5][6][7][8] or selective separation of Mg 2+ from seawater, where it exists at a relatively high concentration (typically above 1350 mg/L). The latter group includes a process for separating Mg 2+ from seawater via selective ion-exchange and transferring the Mg 2+ to the desalinated water by passing a Ca 2+ -rich solution originating from calcite dissolution, through the Mg-saturated resin [9]; nanofiltration-based Mg 2+ separation [10,11]; with or without adsorption of Mg(OH) 2(s) on the surface of Fe 3 O 4 [12] and processes based on diananofiltration as a rinsing method for reducing the NaCl background of the separated Mg-rich solution [13][14][15].…”
Section: Introductionmentioning
confidence: 99%