United States Geological Survey, Great Lakes Science Center, Lake Michigan Ecological Research Station, 1100 North Mineral Springs Road, Porter, Indiana 46304, United States.
Environ Sci Technol. 2012 Feb 21;46(4):2204-11. doi: 10.1021/es203847n. Epub 2012 Feb 1.
Characterization of diel variability of fecal indicator bacteria concentration in nearshore waters is of particular importance for development of water sampling standards and protection of public health. Significant nighttime increase in Escherichia coli (E. coli) concentration in beach water, previously observed at marine sites, has also been identified in summer 2000 from fixed locations in waist- and knee-deep waters at Chicago 63rd Street Beach, an embayed, tideless, freshwater beach with low currents at night (approximately 0.015 m s(-1)). A theoretical model using wave-induced mass transport velocity for advection was developed to assess the contribution of surface waves to the observed nighttime E. coli replenishment in the nearshore water. Using average wave conditions for the summer season of year 2000, the model predicted an amount of E. coli transported from water of intermediate depth, where sediment resuspension occurred intermittently, that would be sufficient to have elevated E. coli concentration in the surf and swash zones as observed. The nighttime replenishment of E. coli in the surf and swash zones revealed here is an important phase in the cycle of diel variations of E. coli concentration in nearshore water. According to previous findings in Ge et al. (Environ. Sci. Technol. 2010, 44, 6731-6737), enhanced current circulation in the embayment during the day tends to displace and deposit material offshore, which partially sets up the system by the early evening for a new period of nighttime onshore movement. This wave-induced mass transport effect, although facilitating a significant base supply of material shoreward, can be perturbed or significantly influenced by high currents (orders of magnitude larger than a typical wave-induced mass transport velocity), current-induced turbulence, and tidal forcing.
描述近岸海域粪便指示菌浓度的昼夜变化特征对于制定水样采集标准和保护公众健康具有重要意义。先前在海洋地点观察到的海滩水中大肠杆菌 (E. coli) 浓度在夜间显著增加,在 2000 年夏季,也在芝加哥 63 街海滩的腰部和膝盖深度的固定位置观察到,该海滩是一个无潮、淡水、夜间水流缓慢(约 0.015 m s(-1)) 的港湾海滩。利用波浪诱导的质量输运速度来评估表面波对近岸水观测到的夜间大肠杆菌补充的贡献,建立了一个理论模型。利用 2000 年夏季的平均波浪条件,该模型预测了从中等水深(间歇性发生沉积物再悬浮的地方)输送的大肠杆菌数量,足以使观测到的冲浪区和冲刷区的大肠杆菌浓度升高。这里揭示的大肠杆菌在冲浪区和冲刷区的夜间补充是近岸水中大肠杆菌浓度昼夜变化循环中的一个重要阶段。根据 Ge 等人的先前发现(Environ. Sci. Technol. 2010, 44, 6731-6737),白天海湾内增强的环流倾向于将物质向外海推移和沉积,这部分通过傍晚为新的夜间向岸运动时段建立系统。这种波浪诱导的质量输运效应虽然有利于大量物质向岸供应,但可能会受到高水流(比典型的波浪诱导质量输运速度大几个数量级)、水流诱导的湍流和潮汐强迫的干扰或显著影响。