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Criteria for Distinguishing Floc Sedimentation and Gel-Like Network Sedimentation of Cohesive Fine-Grained Sediment in a Turbulent Flow

机译:湍流中粘性细粒沉积物的絮凝沉积和凝胶状网络沉积的判别标准

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The study on the criteria used to distinguishfloc sedimentation and gel-like network sedimentation of cohesive fine-grained sedimentin a turbulent flow has rarely been carried out. In this preliminary study, we derivethree criteria to distinguish these two different sedimentation phases by consideringthe comparison of the time that a characteristic floc takes to settle through meandistance between characteristic flocs and the time that it takes to move throughthe same distance under the influence of a turbulent flow. These criteria incorporatephysical and chemical factors that have been verified to have some influences onthe sediment flocculation in some published literatures, and a simple analysis resultis found to be consistent with our qualitative understandings of flocculation phenomenonof cohesive fine-grained sediment.
机译:很少进行用于区分湍流中粘性细粒沉积物的絮凝沉降和凝胶状网络沉降的判据的研究。在此初步研究中,我们通过考虑特征絮凝物通过特征絮凝物之间的平均距离沉降所需的时间与在湍流影响下经过相同距离运动所需的时间的比较,得出三个判别标准,以区分这两个不同的沉积阶段。流。这些标准结合了一些物理和化学因素,在一些已发表的文献中已证实这些因素对沉积物的絮凝有一定影响,并且简单的分析结果与我们对粘性细粒沉积物的絮凝现象的定性认识是一致的。

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