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Formation of oil-particle aggregates: Impacts of mixing energy and duration

机译:油颗粒聚集体的形成:混合能量和持续时间的影响

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Spilled oil slicks are likely to break into droplets offshore due to wave energy. The fate and transport of such droplets are affected by suspended particles in local marine environment, through forming oil particle aggregates (OPAs). OPA formation is affected by various factors, including the mixing energy and duration. To evaluate these two factors, lab experiments of OPA formation were conducted using kaolinite at two hydrophobicities in baffled flasks, as represented by the contact angle of 28.8° and 37.7° (original and modified kaolinite). Two mixing energies (energy dissipation rates of 0.05 and 0.5 W/kg) and four durations (10 min, 30 min, 3 h, and 24 h) were considered. Penetration to the oil droplets was observed at 3-5 urn and 5-7 μm for the original and modified kaolinite by con-focal microscopy, respectively. At lower mixing energy, volume median diameter d50 of oil droplets increased from 45 μm to 60 μm after 24 h mixing by original kaolinite; for modified kaolinite, d50 decreased from 40 μm to 25 μm after 24 h mixing. The trapped oil amount in negatively buoyant OPAs decreased from 35% (3 h mixing) to 17% (24 h mixing) by original kaolinite; and from 18% to 12% after 24 h mixing by modified kaolinite. Results indicated that the negatively buoyant OPAs formed with original kaolinite at low mixing energy reaggregated after 24 h. At higher mixing energy, d50 decreased from 45 μm to 17 μm after 24 h mixing for both kaolinites. And the trapped oil amount in negatively buoyant OPAs increased to 72% and 49% after 24 h mixing for original and modified kaolinite, respectively. At higher mixing energy, the OPAs formed within 10 min and reached equilibrium at 3 h by original kaolinite. For modified kaolinite, the OPAs continued to form through 24 h.
机译:由于波能量,溢出的油烟可能会破坏海上滴落。通过形成油颗粒聚集体(OPA),通过局部海洋环境中悬浮颗粒的悬浮颗粒的悬浮颗粒的命运和运输受到悬浮颗粒的影响。 OPA形成受各种因素的影响,包括混合能量和持续时间。为了评估这两个因素,在两个疏动烧瓶中的两个疏水性在两个疏水性上使用高岭石对OPA形成的实验室进行,如接触角为28.8°和37.7°(原始和改性高岭石)所示。考虑两个混合能量(0.05和0.5W / kg)和4个持续时间(10分钟,30分钟,3小时和24小时)。通过对局部显微镜分别在3-5瓮和5-7μm下观察到油滴的渗透,并通过Con-ocalmar显微镜检查原始和改性高岭石。在较低的混合能量下,通过原始高岭石混合24小时后,油滴的体积中值D50从45μm达到60μm增加;对于改性高岭石,24小时混合后D50从40μm降低至25μm。由于原始高岭石,带负浮力蛋白的捕获的油量从35%(3小时混合)减少到17%(24小时混合);通过改性高岭石24小时混合后,24小时后的18%至12%。结果表明,在24小时后,用原始高岭石形成的负浮力孔径在低混合能量中重新聚集。在较高的混合能量下,在24小时后,D50在对高岭土混合后从45μm至17μm降低。对于原始和改性高岭石分别在24小时混合后,带负浮力蛋白的捕获的油量增加到72%和49%。在更高的混合能量下,孔的孔在10分钟内形成,并通过原始高岭石在3小时内达到平衡。对于改良的高岭石,OPA继续形成24小时。

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