2011
DOI: 10.1061/(asce)hy.1943-7900.0000310
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Thin-Layer Gravity Current with Implications for Desalination Brine Disposal

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Cited by 22 publications
(16 citation statements)
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“…Therefore, we completed our first transect after we had completely traversed the pocket of hypoxic waters near platform P2. At that point, we changed our direction of travel and headed southwest toward Oso Bay where hypoxia had been observed previously (Hodges et al 2009). However, as we moved toward Oso Bay, we noticed a low DO gradient in the other direction (i.e., northwest direction toward Nueces Bay).…”
Section: Resultsmentioning
confidence: 99%
“…Therefore, we completed our first transect after we had completely traversed the pocket of hypoxic waters near platform P2. At that point, we changed our direction of travel and headed southwest toward Oso Bay where hypoxia had been observed previously (Hodges et al 2009). However, as we moved toward Oso Bay, we noticed a low DO gradient in the other direction (i.e., northwest direction toward Nueces Bay).…”
Section: Resultsmentioning
confidence: 99%
“…The high weight of concentrated saline stemming from seawater desalination always causes its sinking to the bottom of sea [13,18,22], which prevents mixing with other water bodies and reduces the organic species and qualities and dissolved oxygen level [18,69]. All these factors lead to mortality of benthic organisms [15,22,70], ultimately resulting in degradation to a salt desert status of the ambient water body [13].…”
Section: Seawater Desalination and Environmental Problems Caused By Bmentioning
confidence: 99%
“…The most immediate environmental hazard associated with desalination brine discharges is the formation of so-called 'brine underflows' [4]. This flow is associated is the formation of a thin layer of hypersaline water spreading along the seafloor and becoming depleted in dissolved oxygen.…”
Section: Marine Impacts and Environmental Legislationmentioning
confidence: 99%