泥沙颗粒生长生物膜后起动的实验研究——Ⅱ.起动流速计算
Experimental study of the effect of biofilm formation on sediment incipient motion: Ⅱ.Incipient velocity calculation
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摘要: 泥沙颗粒生长生物膜后,起动流速发生了较大变化。根据生长生物膜后的泥沙起动流速实验数据,考虑天然水体中,生物膜填充于颗粒与颗粒之间形成除水以外新的介质,将生物膜的作用模化为生物膜作用产生的粘连力,再考虑生物膜随时间变化的特性以及基底物理特性的影响等因素,结合泥沙颗粒之间由于薄膜水产生的黏结力、重力等,研究了颗粒在滑动和滚动两种条件下的起动公式。研究表明,滚动和滑动两种条件公式的计算结果基本一致,与实验数据符合良好,能够用来计算不同粒径大小的泥沙颗粒在生物膜生长后的起动流速。Abstract: The sediment incipient motion can be significantly affected by the presence of microbial biofilm growth.Using the experimental incipient velocity data collected under the influence of biofilm colonization,the incipient velocity formulas for the two types of sediments are derived for sliding and rolling motions.The thin water film theory is utilized to describe the coheslve force between sediment partmles and the aClheslve force generated by the biofilm in the formula derivation.Time variation characteristics of the biofilm strength and the feature of the substrate are also taken into the consideration.The result shows that both rolling and sliding formula are able to reproduce the observed incipient Veloci1t1es.The two calculated velocities are basically consistent with each other.