Multi-scale studies on the effects of fluid and bed variability on particle entrainment and transport

流体和床层变化对颗粒夹带和运输影响的多尺度研究

• 批准号: 0756480
• 负责人: Kimberly Hill
• 金额: $ 29.59万
• 依托单位: University of Minnesota-Twin Cities
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2008
• 资助国家: 美国
• 起止时间: 2008-07-01 至 2014-06-30
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=0756480&HistoricalAwards=false
• 关键词: Multi; scale; studies; effects; fluid

CBET-0756480HillThe ability to predict and understand particle entrainment and transport via the impelling force of moving fluid is important for engineering and natural applications including stream restoration and brownout conditions for helicopters. Most models predicting particle entrainment are empirically or semi-empirically based on temporally and/or spatially averaged velocity and/or shear stress of the fluid. As such, while these models work reasonably well for relatively simple fluid flow (through channels), under unsteady conditions (for example, due to existence of ripples in the bed or unsteady flow) these models are significantly less successful for flows heavily laden with particles. Further, even for statistically steady conditions, they fail to capture the physical essence of particle transport, adding to the prediction uncertainty. Experimental evidence suggests discrepancies in particle entrainment/transport models and physical measurements are due largely to the neglected effects of turbulence fluctuations on particle movement. A model relating locally-averaged turbulent fluctuations with locally-averaged particle transport could be of great value to parameterize particle entrainment, such as those available in large-eddy simulations. This research focuses on flow-driven particle transport where particle-particle interactions are important, specifically bedload transport in river channels. The central goal of this research is to better understand bedload transport from first principles. Ultimately, this might serve as a framework for particle entrainment in a wider range of flow-driven particle transport, such as wind-blown sand. The broader impacts involve the development of experiments and interactive online modules for middle-school, high-school and college students and related materials for K-12 teachers. These will be developed in particular for the National Center for Earth-surface Dynamics? (NCED) gidakiimanaaniwigamig (Our Earth Lodge) summer camps and after-school programming held at the Fond du Lac Tribal and Community College. Additionally, the PIs will incorporate the fundamentals behind the new model of particle transport into fluid mechanics and sediment transport courses they teach as well as the NCED post-baccalaureate Stream Restoration Certificate Program.

CBET-0756480希尔通过运动流体的推动力预测和理解颗粒夹带和运输的能力对于工程和自然应用非常重要，包括直升机的气流恢复和灯火管制条件。大多数预测颗粒夹带的模型是基于流体的时间和/或空间平均速度和/或剪切应力的经验或半经验的。因此，虽然这些模型对于相对简单的流体流动（通过通道）相当好地工作，但是在不稳定条件下（例如，由于床中存在波纹或不稳定流动），这些模型对于大量负载颗粒的流动明显不太成功。此外，即使在统计稳定的条件下，它们也无法捕捉粒子输运的物理本质，增加了预测的不确定性。实验证据表明，颗粒夹带/运输模型和物理测量的差异主要是由于被忽视的湍流波动对颗粒运动的影响。局部平均湍流波动与局部平均颗粒输运相关的模型对于参数化颗粒夹带可能具有很大价值，例如大涡模拟中可用的那些。本研究的重点是流动驱动的颗粒输运，颗粒之间的相互作用是很重要的，特别是在河道推移质输运。这项研究的中心目标是从第一原理更好地理解推移质输运。最终，这可能作为一个框架，颗粒夹带在更广泛的流动驱动的颗粒运输，如风吹沙。更广泛的影响包括为初中、高中和大学学生开发实验和互动在线模块，以及为K-12教师开发相关材料。这些将特别为国家地球表面动力学中心开发。在丰迪拉克部落和社区学院举办的gidakiimanananiwigamig（我们的地球小屋）夏令营和课后方案。此外，PI将把粒子输运新模型背后的基本原理纳入他们教授的流体力学和沉积物输运课程以及NCED学士学位后河流恢复证书课程。