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Pattern Formation and Instabilities in Particulate Suspensions 颗粒悬浮液的模式形成和不稳定性
IF 27.7 1区 工程技术 Q1 MECHANICS Pub Date : 2025-10-01 DOI: 10.1146/annurev-fluid-100224-111041
Marc A. Fardin, Thibaut Divoux, Sungyon Lee, Irmgard Bischofberger
Particulate suspensions, consisting of solid particles dispersed in a fluid, exhibit complex flow behaviors influenced by multiple factors, including particle interactions, concentration gradients, and external forces. Suspensions play an important role in diverse processes, from sediment transport to food processing, and display instabilities triggered by shear-driven effects, frictional interactions, and viscous forces. These instabilities can often be understood by identifying the key mechanical quantities that govern the dynamics. Following hydrodynamic tradition, such mechanics can be characterized by dimensionless numbers, which encapsulate the interplay between geometric, kinematic, and mechanical factors. Many of these numbers represent competitions between opposing pairs of mechanical quantities, which we discuss in detail while also considering a few phenomena that require more complex combinations. By emphasizing the underlying mechanical principles, this review provides a perspective for understanding pattern formation and flow instabilities in confined particulate suspensions across different flow geometries.
颗粒悬浮液由分散在流体中的固体颗粒组成,其流动行为受到多种因素的影响,包括颗粒相互作用、浓度梯度和外力。悬浮液在多种过程中发挥着重要作用,从沉积物运输到食品加工,并表现出剪切驱动效应、摩擦相互作用和粘性力引发的不稳定性。这些不稳定性通常可以通过确定控制动力学的关键力学量来理解。按照流体力学的传统,这种力学可以用无因次数来表征,这些无因次数概括了几何、运动学和力学因素之间的相互作用。这些数字中的许多代表了对立的力学量对之间的竞争,我们将详细讨论这一点,同时考虑一些需要更复杂组合的现象。通过强调潜在的力学原理,本综述为理解不同流动几何形状的受限颗粒悬浮液的模式形成和流动不稳定性提供了一个视角。
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引用次数: 0
Filtration in Pore Networks 孔隙网络中的过滤
IF 27.7 1区 工程技术 Q1 MECHANICS Pub Date : 2025-09-30 DOI: 10.1146/annurev-fluid-112723-054759
Linda J. Cummings, Binan Gu, Lou Kondic
In liquid filtration, a particulate-laden feed solution is passed through a porous material (the filter), often a membrane, designed to capture the particulate matter. Usually, the filter has a complex interior structure of interconnected pores, through which the feed passes, and in many cases of interest, it may be reasonable to approximate this interior structure as a network of interconnected tubes. This idea, which dates back about 70 years, greatly simplifies the modeling and simulation of the filtration process. In this article, we review the use of networks as a framework for modeling and investigating filtration, describing the key ideas and milestones. We also discuss some promising areas for future development of this field, particularly concerning the design of next-generation filters.
在液体过滤中,含有颗粒的进料溶液通过多孔材料(过滤器),通常是一层膜,用于捕获颗粒物质。通常,过滤器具有由相互连接的孔隙组成的复杂内部结构,进料通过这些孔隙,在许多感兴趣的情况下,将这种内部结构近似为相互连接的管道网络可能是合理的。这个想法可以追溯到大约70年前,大大简化了过滤过程的建模和模拟。在本文中,我们回顾了网络作为建模和研究过滤的框架的使用,描述了关键思想和里程碑。我们还讨论了该领域未来发展的一些有前途的领域,特别是下一代滤波器的设计。
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引用次数: 0
Urban Fluid Mechanics, Resilience, and Sustainability 城市流体力学,弹性和可持续性
IF 27.7 1区 工程技术 Q1 MECHANICS Pub Date : 2025-09-29 DOI: 10.1146/annurev-fluid-100224-111114
Catherine Gorlé
This review first examines how urban wind flow impacts the sustainability and resilience of cities and identifies the three main challenges in predictive modeling of urban flows: the complexity of the flow physics, the variability and uncertainty in the flow conditions, and the diversity and multiscale nature of urban geometries. To review the complexity of the flow physics, the typical flow patterns observed in canonical urban flows are summarized, and related modeling challenges and opportunities in both wind tunnel experiments and simulations are highlighted. Next, opportunities to predict realistic urban flows by addressing the other challenges are explored through the lens of a modeling framework with uncertainty quantification. The important role of field measurements, supporting the more accurate characterization of uncertainties in the flow conditions, as well as enabling validation with real-world data, is emphasized. The review concludes with two specific examples that demonstrate how integrated use of field measurements and computational models can improve the understanding and modeling of real urban flows to ultimately support sustainable development goals for urban areas.
本文首先考察了城市风如何影响城市的可持续性和弹性,并确定了城市风预测建模的三个主要挑战:流动物理的复杂性、流动条件的可变性和不确定性,以及城市几何形状的多样性和多尺度性质。为了回顾流动物理的复杂性,总结了典型城市流动中观察到的典型流动模式,并强调了风洞实验和模拟中相关建模的挑战和机遇。接下来,通过具有不确定性量化的建模框架,探讨了通过解决其他挑战来预测现实城市流量的机会。强调了现场测量的重要作用,支持更准确地表征流动条件中的不确定性,并能够通过实际数据进行验证。报告最后列举了两个具体的例子,说明实地测量和计算模型的综合使用如何能够提高对实际城市流动的理解和建模,从而最终支持城市地区的可持续发展目标。
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引用次数: 0
Flexible Fibers in Turbulence 湍流中的柔性纤维
IF 27.7 1区 工程技术 Q1 MECHANICS Pub Date : 2025-09-22 DOI: 10.1146/annurev-fluid-112723-050451
Cristian Marchioli, Marco Edoardo Rosti, Gautier Verhille
In this article, we review recent progress in the fundamental understanding of the motion of flexible fibers in a turbulent flow, made through multiscale experiments and simulations. Emphasis is given to problems involving flexible fibers that can be conveniently described with discrete and continuum models closely related to the slender body theory. Current state-of-the-art measurement and simulation methods, including optical techniques, Euler–Lagrange approaches for tracking large swarms of fibers, and recent methodologies for simulating finite-size fibers, are discussed. The capabilities of simulations and experiments are surveyed in connection with the current physical understanding of how flexible fibers interact with the full spectrum of length scales and timescales of turbulence. We review the phenomenological and statistical features of fiber dispersion and spatial distribution. We also discuss the relevant aspects of fiber rotation and deformation, highlighting their connection with mechanisms such as fragmentation and turbulence modulation, which are known to exhibit peculiar features in the case of flexible fibers. We conclude our analysis by providing an outlook on future research direction paths, open methodological issues, and expected advances, in particular those associated with the study of flexible particles in a broader sense.
在本文中,我们回顾了近年来通过多尺度实验和模拟对柔性纤维在湍流中运动的基本认识的进展。重点讨论与细长体理论密切相关的离散和连续模型可以方便地描述的柔性纤维问题。讨论了当前最先进的测量和模拟方法,包括光学技术,欧拉-拉格朗日方法用于跟踪大群光纤,以及模拟有限尺寸光纤的最新方法。模拟和实验的能力与当前对柔性纤维如何与湍流的全长度尺度和时间尺度相互作用的物理理解有关。我们回顾了纤维弥散和空间分布的现象学和统计学特征。我们还讨论了纤维旋转和变形的相关方面,强调了它们与断裂和湍流调制等机制的联系,这些机制已知在柔性纤维的情况下表现出特殊的特征。最后,我们展望了未来的研究方向、方法问题和预期的进展,特别是与更广泛意义上的柔性粒子研究相关的研究。
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引用次数: 0
Aircraft Icing: Modeling and Simulation 飞机结冰:建模与仿真
IF 27.7 1区 工程技术 Q1 MECHANICS Pub Date : 2025-09-18 DOI: 10.1146/annurev-fluid-112723-062537
Alberto Guardone, Tommaso Bellosta, Alessandro Donizetti, Mariachiara Gallia
In-flight ice accretion poses a major safety concern in aviation. It occurs due to the icing from clouds of supercooled water droplets, the accumulation of ice crystals at high altitudes, or snow buildup. Assessing the detrimental effects of ice accretion on aircraft performance and handling qualities is a complex, multidisciplinary task, as it requires modeling the dynamics of the dispersed phase (water droplets, ice crystals, and snowflakes), the particle impact dynamics and its interaction with the aircraft surfaces, the liquid film dynamics, the solidification process, and possibly ice shedding. The ice protection systems must also be modeled. The present review addresses the status of ice accretion models and simulation tools. The intrinsically stochastic nature of ice accretion, combined with substantial operational and modeling uncertainties, makes it challenging to validate these tools against experimental observations and use simulation as a reliable means of compliance for certification in icing conditions, especially for innovative aircraft configurations such as wing-body and advanced urban air mobility vehicles.
飞行中的冰积是航空安全的一个主要问题。它的发生是由于过冷的水滴云结冰,高海拔地区冰晶的积累,或雪的堆积。评估结冰对飞机性能和操纵质量的不利影响是一项复杂的、多学科的任务,因为它需要对分散相(水滴、冰晶和雪花)的动力学、颗粒撞击动力学及其与飞机表面的相互作用、液膜动力学、凝固过程以及可能的冰脱落进行建模。冰防护系统也必须建模。本文综述了冰积累模型和模拟工具的现状。冰积的内在随机性,再加上大量的操作和建模不确定性,使得根据实验观察验证这些工具,并将模拟作为在结冰条件下认证的可靠手段具有挑战性,特别是对于创新的飞机配置,如翼身和先进的城市空中机动车辆。
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引用次数: 0
Secondary Atomization of Droplets at Extreme Conditions 极端条件下液滴的二次雾化
IF 27.7 1区 工程技术 Q1 MECHANICS Pub Date : 2025-08-01 DOI: 10.1146/annurev-fluid-112823-115348
Saini Jatin Rao, Saptarshi Basu
Droplets, which are ubiquitous in nature, are formed through intriguing processes, and one such route is air-assisted atomization or aerobreakup. This review focuses on secondary atomization, particularly the breakup of an individual droplet subjected to high-speed flows. This process involves complex interfacial dynamics with multiscale deformations, ranging from global flattening to local unstable waves. The deformations occur at progressively smaller scales while interacting with the surrounding gas phase, forming a nonlinear cascade. Each local undulation serves as a precursor to a self-similar evolution or subsecondary breakup process that ends with a ligament-mediated mechanism. In practical scenarios, droplets often encounter nonuniform, unsteady, impulsive, or compressible flows, like shock waves, which pose extreme conditions. The spatiotemporal scales of the nonuniformity or unsteadiness of the external flow must be comparable with the drop deformation scales at either global or local levels to influence aerobreakup that cascades across hierarchical deformation scales. The compressible effects at high Mach numbers are interestingly shown to suppress the tendency toward breakup.
液滴在自然界中无处不在,它们是通过有趣的过程形成的,其中一种途径是空气辅助雾化或空气分解。本文综述了二次雾化,特别是单个液滴在高速流动下的破裂。这一过程涉及复杂的界面动力学和多尺度变形,范围从全局变平到局部不稳定波。当与周围的气相相互作用时,变形发生在逐渐变小的尺度上,形成非线性级联。每个局部波动都是自相似进化或亚继发性破裂过程的前兆,该过程以韧带介导的机制结束。在实际情况中,液滴经常遇到不均匀的、不稳定的、脉冲的或可压缩的流动,如激波,这就构成了极端的条件。外部流动的不均匀性或不稳定性的时空尺度必须与全球或局部水平的水滴变形尺度相比较,以影响跨分层变形尺度级联的空气破碎。有趣的是,高马赫数下的可压缩效应抑制了破裂的趋势。
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引用次数: 0
The Dynamics of Sand Dunes 沙丘动力学
IF 27.7 1区 工程技术 Q1 MECHANICS Pub Date : 2025-07-10 DOI: 10.1146/annurev-fluid-112723-062843
Nathalie M. Vriend, Karol A. Bacik
Sand dunes cover 5% of Earth's land surface, and they abundantly populate river bottoms and seabeds. The subtle dynamical interplay between the granular matter and the overlaying fluid leads to rich phenomenology at different scales, from colliding grains through migrating sand dunes to slowly evolving dune fields. In this review, we survey recent developments in the literature on the dynamics of sand dunes and focus in particular on the physics and mathematics. Our discussion is organized around four central paradigms of the field: flat bed instability, single dune migration, dune–dune interactions, and dune field statistics. Besides discussing the key scientific advances, we also highlight the methodological advances in observations, experiments, and simulations that facilitated them. We conclude our review by discussing the social implications of dune dynamics, such as the interaction between dune and infrastructure, and we offer speculation on what research topics related to sand dunes might become important in the next decade.
沙丘覆盖了地球陆地表面的5%,它们大量分布在河底和海床上。颗粒物质与上覆流体之间微妙的动力学相互作用导致了不同尺度上丰富的现象,从颗粒通过迁移沙丘碰撞到缓慢演变的沙丘场。本文综述了沙丘动力学研究的最新进展,重点介绍了沙丘动力学的物理和数学研究。我们的讨论围绕着该领域的四个中心范式:平床不稳定性、单沙丘迁移、沙丘-沙丘相互作用和沙丘场统计。除了讨论关键的科学进展外,我们还强调了促进这些进展的观察、实验和模拟方面的方法进步。最后,我们讨论了沙丘动力学的社会意义,如沙丘与基础设施之间的相互作用,并对未来十年与沙丘相关的研究课题进行了推测。
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引用次数: 0
Electromagnetically Forced Flows in Shallow Electrolyte Layers 浅电解液层中的电磁强迫流动
IF 27.7 1区 工程技术 Q1 MECHANICS Pub Date : 2025-07-02 DOI: 10.1146/annurev-fluid-112723-051243
Sergio Cuevas, Sergey A. Suslov, Aldo Figueroa
Electromagnetically forced flows in shallow electrolyte layers offer a versatile and nonintrusive method for exploring quasi-two-dimensional fluid dynamics. This review focuses on the experimental and theoretical aspects of such flows driven by Lorentz forces generated by the interaction of injected electric currents and the applied magnetic fields. The method is applicable to both liquid metals and electrolytes, with the latter more commonly used due to their wide availability and ease of handling. Experimental aspects of the method and key components of mathematical flow analysis are discussed. Initially developed for geophysical flow modeling, the method has been instrumental in exploring various other physical phenomena including vortex and wake dynamics, spatiotemporal chaos, and mixing processes. The review also addresses the challenges of achieving true two-dimensionality in laboratory settings and discusses the influence of various parameters, such as layer thickness and forcing intensity, on the flow behavior. Future research directions in the field are highlighted.
浅层电解液中的电磁强迫流动为探索准二维流体动力学提供了一种通用的非侵入性方法。本文综述了由注入电流和外加磁场相互作用产生的洛伦兹力驱动的这种流动的实验和理论方面。该方法适用于液态金属和电解质,后者由于其广泛可用和易于处理而更常用。讨论了数学流分析方法的实验方面和关键组成部分。该方法最初是为地球物理流动建模而开发的,在探索其他各种物理现象,包括涡旋和尾流动力学、时空混沌和混合过程中发挥了重要作用。该综述还解决了在实验室环境中实现真正二维的挑战,并讨论了各种参数(如层厚度和强迫强度)对流动行为的影响。展望了该领域未来的研究方向。
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引用次数: 0
Formation and Evolution of Planetary Stagnant Lids and Crusts 行星停滞盖壳的形成与演化
IF 27.7 1区 工程技术 Q1 MECHANICS Pub Date : 2025-06-03 DOI: 10.1146/annurev-fluid-112723-055048
Chloé Michaut, Anne Davaille, Stéphane Labrosse
Earth is the only known planet with plate tectonics, which involves a mobile upper thermal boundary layer. Other terrestrial planets show a one-plate immobile lithosphere, or stagnant lid, that insulates and isolates their interior. Here, we first review the different types of lids that can develop on rocky and icy bodies. As they formed by accretion, involving high-energy impacts, terrestrial planets likely started hot and molten. We examine the process of lid initiation from a magma ocean stage and develop the equations for lid growth. We survey how lateral perturbations in lid and crust thickness can be amplified during their growth and finally discuss the possible processes at the origin of lid rupture and plate generation.
地球是已知的唯一具有板块构造的行星,板块构造涉及一个可移动的上层热边界层。其他类地行星显示出一个板块固定的岩石圈,或静止的盖子,将它们的内部隔离开来。在这里,我们首先回顾不同类型的盖子可以在岩石和冰体上形成。由于它们是由吸积形成的,包括高能撞击,类地行星可能开始时是热的和熔融的。我们研究了岩浆海阶段岩浆盖的形成过程,并建立了岩浆盖生长的方程。我们调查了地壳和地壳厚度的横向扰动如何在它们的生长过程中被放大,最后讨论了地壳和地壳破裂和板块形成的可能起源过程。
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引用次数: 0
Rapidly Rotating Magnetohydrodynamics and the Geodynamo 快速旋转磁流体力学和地球动力
IF 27.7 1区 工程技术 Q1 MECHANICS Pub Date : 2024-10-01 DOI: 10.1146/annurev-fluid-031224-121649
Emmanuel Dormy
The problem of the geodynamo is simple to formulate (Why does the Earth possess a magnetic field?), yet it proves surprisingly hard to address. As with most geophysical flows, the fluid flow of molten iron in the Earth's core is strongly influenced by the Coriolis effect. Because the liquid is electrically conducting, it is also strongly influenced by the Lorentz force. The balance is unusual in that, whereas each of these effects considered separately tends to impede the flow, the magnetic field in the Earth's core relaxes the effect of the rapid rotation and allows the development of a large-scale flow in the core that in turn regenerates the field. This review covers some recent developments regarding the interplay between rotation and magnetic fields and how it affects the flow in the Earth's core.
地球动力问题说起来很简单(地球为什么会有磁场?与大多数地球物理流动一样,地核中熔融铁的流体流动受到科里奥利效应的强烈影响。由于液体是导电的,它也受到洛伦兹力的强烈影响。这种平衡的不寻常之处在于,虽然单独考虑这些效应中的每一种都会阻碍流动,但地核中的磁场会放松快速旋转的影响,使地核中形成大规模流动,进而再生磁场。这篇综述涵盖了有关自转和磁场之间的相互作用及其如何影响地核流动的一些最新进展。
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引用次数: 0
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Annual Review of Fluid Mechanics
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