2017
DOI: 10.1016/j.marpolbul.2017.07.042
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Settling of dilbit-derived oil-mineral aggregates (OMAs) & transport parameters for oil spill modelling

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Cited by 24 publications
(20 citation statements)
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“…The results presented above indicate unique differences of floccualtion characteristics between Kaolinite and Bentonite OMAs which may be closely influenced by the OMA structures. Previously, this hasn't been clearly revealed by studying the natural mixture sediment samples directly (e.g., Khelifa et al 2005bKhelifa et al , 2008Sun et al 2010Sun et al , 2013O'Laughlin et al 2017). Kaolinite particles tend to show lower cohesion and the resulting oil-Kaolinite aggregates can be categorized as droplet OMAs.…”
Section: Discussionmentioning
confidence: 99%
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“…The results presented above indicate unique differences of floccualtion characteristics between Kaolinite and Bentonite OMAs which may be closely influenced by the OMA structures. Previously, this hasn't been clearly revealed by studying the natural mixture sediment samples directly (e.g., Khelifa et al 2005bKhelifa et al , 2008Sun et al 2010Sun et al , 2013O'Laughlin et al 2017). Kaolinite particles tend to show lower cohesion and the resulting oil-Kaolinite aggregates can be categorized as droplet OMAs.…”
Section: Discussionmentioning
confidence: 99%
“…The Bentonite aggregates tend to re-shape and absorb or be absorbed by the oil droplets forming large (as large as 900 microns floc has been observed) dense oil-Bentonite aggregates (Figure4b2−4 ). Previous experimental work also indicates that the oil-sediment aggregates formed using natural sediment can be as large as 900 microns(O'Laughlin et al, 2017) and their settling velocity can be variable depending on oil amount trapped in sediment mixture aggregates(Sun et al, 2010). They also suggest that higher sediment concentration may lead to larger flocs with higher settling velocity.…”
mentioning
confidence: 94%
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“…The amount and type of suspended sediment affect not only the amount of oil trapped in OPAs but also the size and type of OPAs that are formed (Cloutier et al, ; Guyomarch et al, ; Omotoso et al, ; Stoffyn‐Egli & Lee, ). For example, O'Laughlin et al () observed that an increase in sediment concentration corresponded to an increase in OPA size and Stoffyn‐Egli and Lee () observed that by varying the sediment type they could produce either droplet, solid, or flake OPAs.…”
Section: Formationmentioning
confidence: 99%