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Saline Groundwater from Coastal Aquifers As a Source for Desalination

机译:来自沿海含水层的盐渍地下水作为海水淡化的来源

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摘要

Reverse osmosis (RO) seawater desalination is currently a widespread means of closing the gap between supply and demand for potable water in arid regions. Currently, one of the main setbacks of RO operation is fouling, which hinders membrane performance and induces pressure loss, thereby reducing system efficiency. An alternative water source is saline groundwater with salinity close to seawater, pumped from beach wells in coastal aquifers which penetrate beneath the freshwater-seawater interface. In this research, we studied the potential use of saline groundwater of the coastal aquifer as feedwater for desalination in comparison to seawater using fieldwork and laboratory approaches. The chemistry, microbiology and physical properties of saline groundwater were characterized and compared with seawater. Additionally, reverse osmosis desalination experiments in a cross-flow system were performed, evaluating the permeate flux, salt rejection and fouling propensities of the different water types. Our results indicated that saline groundwater was significantly favored over seawater as a feed source in terms of chemical composition, microorganism content, silt density, and fouling potential, and exhibited better desalination performance with less flux decline. Saline groundwater may be a better water source for desalination by RO due to lower fouling potential, and reduced pretreatment costs.
机译:目前,反渗透海水淡化技术是缩小干旱地区饮用水供需之间差距的一种广泛手段。当前,RO操作的主要挫折之一是结垢,这会阻碍膜性能并引起压力损失,从而降低系统效率。一种替代的水源是盐度接近海水的盐水,从沿海含水层的海滩井中抽出,这些海水渗透到淡水-海水界面的下方。在这项研究中,我们通过野外考察和实验室方法研究了与地下水相比,沿海含水层的含盐地下水作为海水淡化的潜在用途。表征了盐水的化学,微生物学和物理特性,并与海水进行了比较。此外,在错流系统中进行了反渗透淡化实验,评估了不同水类型的渗透通量,除盐率和结垢倾向。我们的结果表明,就化学成分,微生物含量,淤泥密度和结垢潜力而言,咸水地下水明显优于海水作为饲料来源,并表现出更好的淡化性能和较少的通量下降。由于较低的结垢可能性和降低的预处理成本,盐水可能是RO脱盐的更好水源。

著录项

  • 来源
    《Environmental Science & Technology》 |2016年第4期|1955-1963|共9页
  • 作者单位

    Department of Desalination and Water Treatment, Zuckerberg Institute for Water Research, Jacob Blaustein Institutes for Desert Research, Ben-Gurion University of the Negev, Sede Boqer Campus, Midreshet Ben-Gurion 84990, Israel;

    Department of Geology, Ben-Gurion University of the Negev, Beer-Sheva 84105, Israel;

    Department of Geology, Ben-Gurion University of the Negev, Beer-Sheva 84105, Israel;

    Department of Desalination and Water Treatment, Zuckerberg Institute for Water Research, Jacob Blaustein Institutes for Desert Research, Ben-Gurion University of the Negev, Sede Boqer Campus, Midreshet Ben-Gurion 84990, Israel,Geological Survey of Israel, 30 Malkhei Israel Street, Jerusalem 95501, Israel;

    Israel Oceanographic and Limnological Research, National Institute of Oceanography, Tel-Shikmona 8030, Haifa 31080, Israel;

    Department of Desalination and Water Treatment, Zuckerberg Institute for Water Research, Jacob Blaustein Institutes for Desert Research, Ben-Gurion University of the Negev, Sede Boqer Campus, Midreshet Ben-Gurion 84990, Israel;

    Department of Desalination and Water Treatment, Zuckerberg Institute for Water Research, Jacob Blaustein Institutes for Desert Research, Ben-Gurion University of the Negev, Sede Boqer Campus, Midreshet Ben-Gurion 84990, Israel;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);美国《生物学医学文摘》(MEDLINE);美国《化学文摘》(CA);
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  • 正文语种 eng
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  • 入库时间 2022-08-17 13:58:45

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