Anomalous wave statistics induced by abrupt depth change,
[arXiv link]
C.T. Bolles, K. Speer, M.N.J. Moore
arXiv and under submission
(2018)


Abstract:
Laboratory experiments reveal that variations in bottom topography can qualitatively alter the distribution of randomized surface waves. A normallydistributed, unidirectional wave field becomes highly skewed and nonGaussian upon encountering an abrupt depth transition. A short distance downstream of the transition, wave statistics conform closely to a gamma distribution, affording simple estimates for skewness, kurtosis, and other statistical properties. Importantly, the exponential decay of the gamma distribution is much slower than Gaussian, signifying that extreme events occur more frequently. Under the conditions considered here, the probability of a rogue wave can increase by a factor of 50 or more. We also report on the surfaceslope statistics and the spectral content of the waves produced in the experiments.


A minimal model for predicting ventilation rates of subterranean caves,
[arXiv link]
K. Khazmutdinova, D. Nof, M. Ye, M.N.J. Moore
arXiv and under submission
(2018)


Abstract:
The ventilation of carbon dioxide within subterranean caves regulates the growth
of speleothems  mineral deposits found in caves that provide important clues about past climate. While previous studies have used internal measurements to predict ventilation rates, such measurements would not be available for the task of climate reconstruction. Here, we develop a parsimonious model to predict ventilation rates from knowledge of outside temperatures and the cave's physical dimensions only. In the model, ventilation arises from buoyancydriven flows created in passageways that connect to the outside. A few key simplifications leads to a system amenable to perturbation analysis, resulting in explicit relationships for how ventilation depends on system parameters. We compare these predictions to timeresolved, insitu measurements of transported cave gases (carbon dioxide and radon). The theory accurately accounts for seasonal and synoptic variations of these gases.


A boundaryintegral framework to simulate viscous erosion of a porous medium,
[JCP link],
[arXiv link]
B.D. Quaife and M.N.J. Moore
Journal of Computational Physics
375, 121 (2018)


Abstract:
We develop numerical methods to simulate the fluidmechanical erosion of many bodies in twodimensional Stokes flow. The broad aim is to simulate the erosion of a porous medium (e.g. groundwater flow) with grainscale resolution. Our fluid solver is based on a secondkind boundary integral formulation of the Stokes equations that is discretized with a spectrallyaccurate Nystrom method and solved with fastmultipoleaccelerated GMRES. The fluid solver provides the surface shear stress which is used to advance solid boundaries. We regularize interface evolution via curvature penalization using the thetaL formulation, which affords numerically stable treatment of stiff terms and therefore permits large time steps. The overall accuracy of our method is spectral in space and secondorder in time. The method is computationally efficient, with the fluid solver requiring O(N) operations per GMRES iteration, a meshindependent number of GMRES iterations, and a onetime O(N^2) computation to compute the shear stress. We benchmark singlebody results against analytical predictions for the limiting morphology and vanishing rate. Multibody simulations reveal the spontaneous formation of channels between bodies of close initial proximity. The channelization is associated with a dramatic reduction in the resistance of the porous medium, much more than would be expected from the reduction in grain size alone.


A fast Chebyshev method for simulating flexiblewing propulsion,
[JCP link],
[arXiv link]
M.N.J. Moore
Journal of Computational Physics
345, 792817 (2017)


Abstract:
We develop a highly efficient numerical method to simulate smallamplitude flapping propulsion by a flexible wing in a nearly inviscid fluid. We allow the wing's elastic modulus and mass density to vary arbitrarily, with an eye towards optimizing these distributions for propulsive performance. The method to determine the wing kinematics is based on Chebyshev collocation of the 1D beam equation as coupled to the surrounding 2D fluid flow. Through smallamplitude analysis of the Euler equations (with trailingedge vortex shedding), the complete hydrodynamics can be represented by a nonlocal operator that acts on the 1D wing kinematics. A class of semianalytical solutions permits fast evaluation of this operator with O(N log N) operations, where N is the number of collocation points on the wing. This is in contrast to the minimum N^2 cost of a direct 2D fluid solver. The coupled wingfluid problem is thus recast as a PDE with nonlocal operator, which we solve using a preconditioned iterative method. These techniques yield a solver of nearoptimal complexity, allowing one to rapidly search the infinitedimensional parameter space of all possible material distributions and even perform optimization over this space.


RiemannHilbert problems for the shapes formed by bodies dissolving, melting, and eroding in fluid flows,
[preprint],
[link]
M.N.J. Moore
Communications on Pure and Applied Mathematics
70(9), 18101831 (2017)


Abstract:
The classical Stefan problem involves the motion of boundaries during phase transition, but this process can be greatly complicated by the presence of a fluid flow. Here, we consider a body undergoing material loss due to either dissolution (from molecular diffusion), melting (from thermodynamic phase change), or erosion (from fluidmechanical stresses) in a fastflowing fluid. In each case, the task of finding the shape formed by the shrinking body can be posed as a singular RiemannHilbert problem. A class of exact solutions captures the rounded surfaces formed during dissolution/melting, as well as the angular features formed during erosion, thus unifying these different physical processes under a common framework. This study, which merges boundarylayer theory, separatedflow theory, and RiemannHilbert analysis, represents a rare instance of an exactly solvable model for highspeed fluid flows with free boundaries.


Torsional spring is the optimal flexibility arrangement for thrust production of a flapping wing,
[pdf],
[link]
M.N.J. Moore
Physics of Fluids (Letters)
27(9), 091701 (2015)


Abstract:
While it is understood that flexibility can improve the propulsive performance of flapping wings and fins, the flexibility distribution leading to optimal performance has not been explored. Using 2D smallamplitude theory and a fast Chebyshev method, we examine how thrust depends on the chordwise distribution of wing stiffness. Through numerical optimization, we find that focusing flexibility at the wing's front, e.g. through a torsional spring, maximizes thrust. A wing with an optimally chosen spring constant typically generates 36% more thrust than a wing of optimal uniform stiffness. These results may relate to material distributions found in nature, such as insect wings, and may apply to the design of biomimetic swimmers and flyers, such as ornithopters.


Shape dynamics and scaling laws for a body dissolving in fluid flow,
[pdf],
[link]
J.M. Huang, M.N.J. Moore, L. Ristroph
Journal of Fluid Mechanics (Rapids)
765, R3 (2015)


Abstract:
While fluid flows are known to promote dissolution of materials, such processes are poorly understood due to the coupled dynamics of the flow and the receding surface. We study this moving boundary problem through experiments in which hard candy bodies dissolve in laminar highspeed water flows. We find that different initial geometries are sculpted into a similar terminal form before ultimately vanishing, suggesting convergence to a stable shapeflow state. A model linking the flow and solute concentration shows how uniform boundarylayer thickness leads to uniform dissolution, allowing us to obtain an analytical expression for the terminal geometry. Newly derived scaling laws predict that the dissolution rate increases with the square root of the flow speed and that the body volume vanishes quadratically in time, both of which are confirmed by experimental measurements.


Analytical results on the role of flexibility in flapping propulsion,
[pdf],
[link]
M.N.J. Moore,
Journal of Fluid Mechanics
757, 599 (2014)


Abstract:
Wing or fin flexibility can dramatically affect the performance of flying and swimming animals. Both laboratory experiments and numerical simulations have been used to study these effects, but analytical results are notably lacking. Here, we develop smallamplitude theory to model a flapping wing that pitches passively due to a combination of wing compliance, inertia, and fluid forces. Remarkably, we obtain a class of exact solutions describing the wing's emergent pitching motions, along with expressions for how thrust and efficiency are modified by compliance. The solutions recover a range of realistic behaviors and shed new light on how flexibility can aid performance, the importance of resonance, and the separate roles played by wing and fluid inertia. The simple, robust estimates afforded by our theory will likely be valuable even in situations where details of the flapping motion and wing geometry differ.


Selfsimilar evolution of a body eroding in a fluid flow,
[pdf],
[link]
M.N.J. Moore, L. Ristroph, S. Childress, J. Zhang, and M.J. Shelley
Physics of Fluids 25(11), 116602 (2013)


Abstract:
Erosion of solid material by flowing fluids plays an important role in shaping landforms, and in this natural context is often dictated by processes of high complexity. Here, we examine the coupled evolution of solid shape and fluid flow within the idealized setting of a cylindrical body held against a fast, unidirectional flow, and eroding under the action of fluid shear stress. Experiments and simulations both show selfsimilar evolution of the body, with an emerging quasitriangular geometry that is an attractor of the shape dynamics. Our fluid erosion model, based on Prandtl boundary layer theory, yields a scaling law that accurately predicts the body's vanishing rate. Further, a class of exact solutions provides a partial prediction for the body's terminal form as one with a leading surface of uniform shear stress. Our simulations show this predicted geometry to emerge robustly from a range of different initial conditions, and allow us to explore its local stability. The sharp, faceted features of the terminal geometry defy the intuition of erosion as a globally smoothing process.


Sculpting of an erodible body by flowing water,
[pdf],
[link]
L. Ristroph, M.N.J. Moore, S. Childress, M.J. Shelley, and J. Zhang
Proceedings of the National Academy of Sciences 109(48), 19606 (2012)


Abstract:
Erosion by flowing fluids carves striking landforms on Earth and also provides important clues to the past and present environments of other worlds. In these processes, solid boundaries both influence and are shaped by the surrounding fluid, but the emergence of morphology as a result of this interaction is not well understood. We study the coevolution of shape and flow in the context of erodible bodies molded from clay and immersed in a fast, unidirec tional water flow. Although commonly viewed as a smoothing process, we find that erosion sculpts pointed and cornerlike features that persist as the solid shrinks. We explain these observations using flow visualization and a fluid mechanical model in which the surface shear stress dictates the rate of material removal. Experiments and simulations show that this interaction ultimately leads to self similarly receding boundaries and a unique front surface character ized by nearly uniform shear stress. This tendency toward confor mity of stress offers a principle for understanding erosion in more complex geometries and flows, such as those present in nature.


A weakcoupling expansion for viscoelastic fluids applied to dynamic settling of a body,
[pdf],
[link]
M.N.J. Moore and M.J. Shelley
Journal of NonNewtonian Fluid Mechanics 183, 25 (2012)


Abstract:
The flow of viscoelastic fluids is an area in which analytical results are difficult to attain, yet can provide invaluable information. We develop a weakcoupling expansion that allows for semianalytical computations of viscoelastic fluid flows coupled to immersed structures. In our method, a leadingorder poly meric stress evolves according to a Newtonian velocity field, and this stress is used to correct the motion of bodies. We apply the method to the transient problem of a sphere settling through a viscoelas tic fluid using the OldroydB model, and recover previous results and observed behavior. The theory pre sented here is in contrast to the retardedmotion, or lowWeissenbergnumber, expansions that have seen much application. One advantage of the weakcoupling method is that it offers information for Weissenberg numbers larger than one. The expansion's limit of validity is closely related to the diluteness criterion of a Boger fluid. We extend the classical settling problem to include an oscillatory bodyforce, and show how the introduction of a second timescale modifies the bodydynamics.


Stratified flows with vertical layering of density: experimental and theoretical study of flow configurations and their stability,
[pdf],
[link]
R. Camassa, R.M. McLaughlin, M.N.J. Moore, and K. Yu
Journal of Fluid Mechanics 690, 571 (2012)


Synopsis:
The vertical motion of bodies through a densitystratified fluid is a problem with important applications in the ocean and atmosphere. Here we create a "strippeddown" flow configuration in order to isolate one feature of vertical motion through stratification  namely the creation of vertical density layers by viscous entrainment. This flow configuration is created in a tabletop experiment by towing a fiber vertically through a stratified corn syrup solution and lubrication theory is used to model the dynamic flow configuration. We find longwave instabilities along the fluid interface for layers that are larger than a critical lengthscale.


Brachistochrones in potential flow and the connection to Darwin's theorem,
[pdf],
[link]
R. Camassa, R.M. McLaughlin, M.N.J. Moore, and A. Vaidya
Physics Letters A 372(45), 6742 (2008)


Synopsis:
Here we characterize the brachistochrone path, or path of shortest time, in potential flow past a body, and we apply our theory to obtain new results related to Darwin's drift volume. Drift volume is related to a body's added mass and has important practical applications. Our theory extends previous infinite and semiinfinite results to finite distances and times, which is an important extension in the context of laboratory experiments. We also discuss an application to a rigid sphere sedimenting through a sharply stratified fluid in order to account for an experimentally observed levitation phenomenon. Further theoretical work related to the potential energy carried by the drift volume is underway.


Other

A weakcoupling expansion applied to the motion of a settling rod in a viscoelastic fluid,
[pdf]
Dustin J. Hill,
Senior honors thesis (2013)


Abstract:
Viscoelastic fluids are fluids that, in addition to having the property of viscosity, also have the property of elasticity. This is often the result of the introduction of a polymeric material to a nonviscoelastic fluid  the presence of these materials greatly affects the behavior of the fluid by introducing additional internal stresses. An example of this  and the focus of this paper  is the dynamics of a settling rod in a viscoelastic fluid. In a Newtonian fluid, a rod settling under gravity adopts a horizontal orientation; whereas, in a viscoelastic fluid, the same rod would adopt a vertical orientation. In this paper, we discuss a number of theoretical and computational models toward the goal of demonstrating the stability of the vertical orientation of the rod in a viscoelastic fluid. The most important of these techniques is the weak coupling expansion. In this technique, we consider the elastic stresses and Newtonian stresses in the fluid to be coupled by a parameter. Considering this to be small, we expand the equations of motion for the rod in terms of it, allowing for an efficient solution of these equations.


