2015
DOI: 10.1016/j.desal.2015.01.008
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Changes in feedwater organic matter concentrations based on intake type and pretreatment processes at SWRO facilities, Red Sea, Saudi Arabia

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Cited by 32 publications
(17 citation statements)
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“…Higher salinity sea water with a slightly lower pH occurs in the carbonate sediments directly underlying the nearshore Red Sea bottom as documented by Dehwah and Missimer (). The higher salinity is likely caused by nearshore evaporative concentration which is 2–3 m of evaporation per year and low rates of nearshore circulation (Dehwah et al , ).…”
Section: Methodsmentioning
confidence: 99%
“…Higher salinity sea water with a slightly lower pH occurs in the carbonate sediments directly underlying the nearshore Red Sea bottom as documented by Dehwah and Missimer (). The higher salinity is likely caused by nearshore evaporative concentration which is 2–3 m of evaporation per year and low rates of nearshore circulation (Dehwah et al , ).…”
Section: Methodsmentioning
confidence: 99%
“…The operating costs of SWRO is very dependent on the complexity of the pretreatment system. The lowest pretreatment costs have been found to occur on SWRO systems that use subsurface intakes that have minimal maintenance and require minimal pretreatment (sand filtration only) [6][7][8][9][10]. The average total water treatment costs for a 100,000 m 3 /day permeate capacity SWRO system using an open-ocean intake ranges from about US$0.80 to US$1.00 per m 3 ( Table 1).…”
Section: Comparison Of Total Water Treatment Costs Of Normal Chemistrmentioning
confidence: 99%
“…While it is unlikely that membrane biofouling can ever be eliminated, the rate of biofouling can be controlled by using extensive pretreatment processes [4,5] designed to remove inorganic and organic particulates including algae, fineorganic solids, and bacteria; and semi-dissolved or dissolved organic matter, such as particulate and colloidal transparent exopolymer particles (TEP) and other sticky polysaccharides that occur mostly within the biopolymer fraction of natural organic matter (NOM) [6]. Many of the precursors to biofouling are also known to be effectively removed by using subsurface intakes, such as conventional vertical wells [7][8][9][10][11] and seabed galleries [12,13].…”
Section: Introductionmentioning
confidence: 99%
“…Studies on TEP distribution in relation to other forms of organic matter in the Red Sea have focused mainly on assessing the links between TEP and phytoplankton and bacterial production (Bar-Zeev et al, 2009b) and the impacts of TEP and dissolved forms of NOM on biofouling in seawater desalination plants (Bar-Zeev et al, 2009a;Dehwah et al, 2015a;Dehwah et al, 2015b;Dehwah et al, 2015c;Dehwah and Missimer, 2016;Rachman et al, 2014;Rachman et Biogeosciences Discuss., https://doi.org/10.5194/bg-2019-59 Manuscript under review for journal Biogeosciences Discussion started: 13 March 2019 c Author(s) 2019. CC BY 4.0 License.…”
mentioning
confidence: 99%