2002
DOI: 10.1016/s1353-2561(02)00124-x
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The Influence of Salinity on Oil–Mineral Aggregate Formation

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Cited by 74 publications
(51 citation statements)
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“…Because of the intense fluorescence characteristics of aromatic hydrocarbons, UV epi-fluorescence illumination distinguishes between oil droplets and non-fluorescent particles. The fine structure of OMA formed as a result of oil and suspended sediments in shoreline and aquatic environments were characterized using combined phase contrast and UV epifluorescence microscopy [13,[20][21][22]. Ultraviolet epifluorescent microscopy has proved useful for characterizing the fine structure of oil-mineral aggregates.…”
Section: Introductionmentioning
confidence: 99%
“…Because of the intense fluorescence characteristics of aromatic hydrocarbons, UV epi-fluorescence illumination distinguishes between oil droplets and non-fluorescent particles. The fine structure of OMA formed as a result of oil and suspended sediments in shoreline and aquatic environments were characterized using combined phase contrast and UV epifluorescence microscopy [13,[20][21][22]. Ultraviolet epifluorescent microscopy has proved useful for characterizing the fine structure of oil-mineral aggregates.…”
Section: Introductionmentioning
confidence: 99%
“…This natural mechanism contributes to dispersion of spilled oil because it enhances stability of oil droplets in the water column. More recently, it has been suggested that formation of oil mineral aggregates (OMA) may play a major role in the natural cleaning of oiled shorelines and may be the basis for the development of oil spill countermeasure technologies (Bragg, Prince, Harner, & Atlas, 1994;Bragg & Yang, 1993;, 1999J ez equel, Merlin, & Lee, 1999;Kepkay, Bugden, Lee, & Stoffyn-Egli, 2002;Khelifa, Stoffyn-Egli, Hill, & Lee, 2002, 2003a, 2003bLee et al, 2003, Lee, Lunel, Wood, Swannell, & Stoffyn-Egli, 1997Le Floch et al, 2002;Muschenheim & Lee, 2002;Omotoso, Munoz, & Mikula, 2002;Owens, 1999;, 1994Payne, Clayton, & Kirstein, 2003, 1989, 1999Wood, Lunel, Baily, Lee, & Stoffyn-Egli, 1997). Nevertheless, little is known about the influence of water salinity and clay type on OMA formation.…”
Section: Introductionmentioning
confidence: 99%
“…Thus, the size or frequency of phytoplankton blooms, and their sedimentation, may have been elevated compared to non-spill years due to the DWH spill. Additionally, increased nutrient and clay concentrations due to freshwater input , as well as resulting salinity gradients, which are known to enhance the formation of particles (Le Floch et al, 2002;Wetz et al, 2009), may have further enhanced the sedimentation potential. Increased sedimentation rates of diatoms could explain the exceptional deposition rate of material in the six months following the spill .…”
Section: Mossfa: Marine Oil Snow Sedimentation and Flocculent Accumulmentioning
confidence: 99%