2003
DOI: 10.1016/s1353-2561(03)00048-3
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Oil/Suspended Particulate Material Interactions and Sedimentation

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Cited by 84 publications
(46 citation statements)
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“…This can be due to the slow deposition rate of small particles (e.g., clay), to which those petroleum hydrocarbons, especially those > C 13 , adsorb due to their low solubility (43). In the open sea, fine suspended particulate matter settles very slowly (<0.01 mm·s −1 ) (44) and thus remains in the surface layers for extended time periods (45,46). However, those particles can be scavenged by marine snow consisting of diatoms, feces, feeding structures, or detritus, therewith cosedimenting rapidly (47,48).…”
Section: Resultsmentioning
confidence: 99%
“…This can be due to the slow deposition rate of small particles (e.g., clay), to which those petroleum hydrocarbons, especially those > C 13 , adsorb due to their low solubility (43). In the open sea, fine suspended particulate matter settles very slowly (<0.01 mm·s −1 ) (44) and thus remains in the surface layers for extended time periods (45,46). However, those particles can be scavenged by marine snow consisting of diatoms, feces, feeding structures, or detritus, therewith cosedimenting rapidly (47,48).…”
Section: Resultsmentioning
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%
“…OMAs vary in buoyancy and can travel in ocean currents, and can thus aid in the proliferation of synthetic dispersants. [11,12] This mechanism could be expected to occur especially in more turbulent, coastal areas, where clay and silica are more abundant and well-mixed.…”
Section: Interpretation Of Cloud Point and Precipitationmentioning
confidence: 99%
“…The various chemical treatments applied to oceanic oil spills contain surfactants and polymers which aim to hasten the breakup of oil slicks into droplets by reducing the surface tension between oil and water. [10] At the same time, the formation of oil-mineralaggregates (OMAs), composed of dispersed oil droplets and clay or silica particles, [11,12] occurs spontaneously through an aggregation method attributable to electrostatic interactions between the particles and polar compounds in oil. [10] The OMAs can be considered as a form of Pickering emulsion, where finely divided oil droplets are stabilized by particles.…”
Section: Introductionmentioning
confidence: 99%