A laboratory study on the kinetics of the formation of oil-suspended particulate matter aggregates using the NIST-1941b sediment

被引:58
作者
Sun, Juan [1 ,2 ,3 ]
Khelifa, Ali [3 ]
Zheng, Xilai [2 ]
Wang, Zhendi [3 ]
So, Lily L. [4 ]
Wong, Sharon [5 ]
Yang, Chun [3 ]
Fieldhouse, Benjamin [3 ]
机构
[1] China Univ Petr Qingdao, Coll Chem & Chem Engn, Qingdao 266555, Shandong, Peoples R China
[2] Ocean Univ China Qingdao, Coll Environm Sci & Engn, Qingdao 266100, Shandong, Peoples R China
[3] Environm Canada, Sci & Technol Branch, ESTS, Ottawa, ON K1A 0H3, Canada
[4] Univ Waterloo, Fac Engn, Waterloo, ON N2L 3G1, Canada
[5] Univ Ottawa, Dept Chem, Ottawa, ON, Canada
关键词
Oil dispersion; Oil-mineral aggregate; Oil-sediment interaction; Oil spill; Oil-suspended particulate matter aggregate; Oil sedimentation; MINERAL PARTICLES; SALINITY; SIZE;
D O I
10.1016/j.marpolbul.2010.06.044
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The formation of oil-suspended particulate matter aggregates (OSAs) results from the heteroaggregation between dispersed oil droplets and suspended particulate matter present in coastal waters. This process has been recognized by the oil spill remediation community to enhance natural cleansing of oiled shorelines and oil dispersion in the water column. While several studies have been conducted on the formation and characteristics of OSAs, few studies have addressed the kinetics of OSA formation. Operationally, this has left decision-makers lacking information on the time scale of this process and its significance to oil dispersion in real spills. A laboratory study was conducted to investigate the kinetics of OSA formation as a function of mixing energy and the sediment-to-oil ratio using the standard reference material 1941b. Results showed that formation of OSAs increased exponentially with the mixing time and reached a maximum within 4 h. When the shaking rate increased from 2.0 to 2.3 Hz, the maximum oil trapping efficiency increased from 20% to 42% and the required shaking time decreased from 3.7 to 0.7 h. (C) 2010 Elsevier Ltd. All rights reserved.
引用
收藏
页码:1701 / 1707
页数:7
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