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Investigations of Rheological Flow Properties Based on Lab Data of Fluid Mud Samples and an Extended Model Approach

机译:基于流体泥浆样品实验室数据的流变流动性能研究及扩展模型方法

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Fluid mud parameters like mass concentration, yield point and apparent viscosities are derived by means of fluid mud sampling along the tidal reach of river Ems and subsequent lab analysis regarding suspended sediment concentration, bulk density and rheological parameters. Equilibrium flow curves were obtained for every sample by means of constant-rate analysis with a high resolution lab rheometer. Comparisons of samples from different locations show good correlation between fluid mud mass concentration and yield point. A reliable method for yield point detection based on creep and recovery rheometer tests and a semi graphical approach was found to deliver the best results. In order to reproduce the large spread of viscosities occurring in reality, the Toorman model was extended by means of an empirical fit with respect to suspended sediment mass concentration. The comparison shows a good correlation between model results and measured constant-rate-test data. Also the thixotropic behavior due to weakening and strengthening as a result of disintegration and build-up of the internal floc structure is reproduced.
机译:通过沿河流EMS的潮汐进程和关于悬浮沉积物浓度,堆积密度和流变参数的随后的实验室分析,通过流体泥浆抽样来源的流体泥浆参数。通过用高分辨率实验室流变仪通过恒定速率分析获得平衡流动曲线。来自不同位置的样品的比较显示出流体泥浆质量浓度和屈服点之间的良好相关性。发现基于蠕变和回收流变仪测试的屈服点检测的可靠方法和半图形方法来提供最佳效果。为了再现实际上发生的粘度的大扩散,通过关于悬浮沉积物质量浓度的经验性拟合来延伸Toorman模型。比较显示了模型结果与测量的恒定速率测试数据之间的良好相关性。还转载了由于崩解和加强由于崩解和内部絮凝结构的积聚而导致的触变行为。

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