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An elastic solid resists deformation, a viscous liquid resists the rate of deformation, and a viscoelastic material does both; which response wins depends on how fast the material is deformed. Tiny amounts of dissolved polymer change how jets, filaments and films break into droplets, from inkjet printing to coughs and sneezes. To describe such flows we keep Cauchy’s momentum equation and add a polymer stress that depends on the conformation tensor , which measures how stretched the polymers are. In the Oldroyd-B family of models the polymers are stretched by the flow and relax with a single relaxation time . Its limits are a viscous liquid () and a Kelvin–Voigt solid (). The Kelvin–Voigt solid is elastic or purely dissipative depending on its retardation time (solvent viscosity divided by elastic modulus). In dimensionless form, three numbers span the parameter space: the Deborah number (material memory against flow time), the elastocapillary number (elastic against capillary stress) and the solvent Ohnesorge number (viscous against inertio-capillary effects). Both and give a Newtonian liquid.

0) Continuum mechanics across fields

The lecture opened with two images that show the same pattern. In the first, a bubble resting on the surface of a very viscous liquid is punctured at its apex. As the hole opens and the thin film collapses, the film develops a ring of radial wrinkles (Oratis, Bush, Stone & Bird 2020). In the second, a rod pushed into an inflated beach ball produces radial wrinkles in a ring around the rod (Vella, Ajdari, Vaziri & Boudaoud 2011). One material is a liquid and the other a solid, yet they wrinkle in the same way.

In both cases a thin sheet is compressed along the azimuthal direction, and a thin sheet would rather bend out of its plane than shorten within it. For the indented shell, Vella et al. showed that a single dimensionless tension sets the pattern, . Here is the internal pressure, the shell radius, its thickness, its Young’s modulus and its bending stiffness, with the Poisson ratio. Pushed far enough, an unpressurised shell such as a ping-pong ball inverts a cap into a dimple (“mirror buckling”), and the compressive hoop stress that this creates then buckles the shell again (Gomez, Moulton & Vella 2016). The result is a polygon; for unpressurised and weakly pressurised shells, with , it has three vertices at onset (Vella et al. 2011). As increases, the polygons give way smoothly to wrinkles confined to an annulus around the indenter. When , a balance between bending and stretching sets a wrinkle wavelength of order , and the wrinkles occupy a region of size of order . Their number therefore grows as : simulations give , and experiments on an inflated ball agree. Counting the wrinkles thus gives the internal pressure of a shell whose , and are known.

For the viscous bubble, Oratis et al. tilted bubbles sideways and turned them upside down, and showed that gravity is not what drives the collapse: surface tension and the dynamic stress in the compressed liquid film drive both the collapse and the wrinkling.

Continuum mechanics treats both systems with the same momentum balance. Only the constitutive law changes, that is, the relation between stress and deformation. For slow flows, in which inertia is negligible, the governing equations correspond exactly. An incompressible Newtonian liquid, with stress and , obeys the same equations as an incompressible linear elastic solid, with and . Here is the pressure, the identity tensor, the viscosity, the velocity, the strain-rate tensor, the shear modulus, the displacement and the strain. Velocity replaces displacement, strain rate replaces strain, and viscosity replaces the shear modulus (the Stokes–Rayleigh analogy). A viscous sheet can therefore wrinkle like an elastic one, with stresses set by how fast it deforms rather than by how much.

This lecture is about the materials in between, whose stress depends on both the deformation and its rate.

1) Why do we care?

1.1 Elastocapillary jets in inkjet printing

An inkjet printhead fires a drop trailed by a long, slender filament. Ideally the filament retracts into a single drop; if it breaks up instead, it leaves satellite droplets that degrade the print and contaminate the printer. Sen et al. (2021) showed that a minute amount of polymer can prevent this. Aqueous solutions of polyethylene oxide (PEO) at concentrations of about wt%, corresponding to a nozzle-based Deborah number of about (Deborah numbers are defined in §5 and §6), suppress satellite droplets. For given driving conditions there is a window of concentrations: below it satellites still form, and above it the printhead stops jetting. Inside the window the filament retracts faster than the Newtonian Taylor–Culick speed of Lecture 1.5, because polymers stretched during jetting add an elastic tension that pulls the filament back. In the lecture, a video compared water with and PEO solutions.

“Elastocapillary” means that elastic and capillary stresses compete. The elastocapillary number of §6 measures that competition.

1.2 Mist: how sneezes make droplets

Coughs and sneezes are turbulent, multiphase flows that can carry pathogen-bearing droplets of mucosalivary fluid, and how far the contamination reaches is largely set by droplet size. High-speed imaging at the mouths of healthy subjects (Scharfman, Techet, Bush & Bourouiba 2016) showed that the fluid keeps breaking up after it has left the mouth, through a cascade from sheets to bursting bags to ligaments and finally to droplets. The viscoelasticity of the mucosalivary fluid delays this fragmentation: droplet precursors that form along stretched filaments merge, which changes the drop-size distribution further downstream.

1.3 Where do the droplets come from?

Wei & Li (2016) summarise three places where respiratory droplets form (their figure 1):

  • The upper airways (larynx and trachea). Fast airflow destabilises the liquid that lines the airway wall and tears droplets from it.
  • The oral cavity. Saliva in the mouth is atomised by the outgoing air.
  • The bronchioles. Liquid films close the smallest airways during exhalation and rupture when the airways reopen during inhalation.

These sites go with three proposed droplet-size modes: a bronchiolar film-burst mode during normal breathing (diameters up to about ), a laryngeal mode most active during voicing and coughing (about and larger), and an oral mode during speech and coughing (about and larger).

1.4 Coughing as mimicked in the lab

A “cough machine” reproduces the first of these mechanisms (Kant, Pairetti, Saade, Popinet, Zaleski & Lohse 2023). A horizontal channel, cm long with a rectangular cross-section, stands in for the trachea. Its floor is coated with a thin liquid film, and a valve releases a blast of air from a pressurised tank at free-stream speeds of about – m/s. The film is lifted into a sheet that inflates into bag-like structures; holes then open and retract across the bags, and the liquid rims bounding these holes break into droplets. A more viscous film stabilises the bags and produces smaller droplets, with the mean size falling by almost a factor of two over the viscosities studied.

Li, Saade, Zaleski, Sen, Kant & Lohse (2025) replaced the Newtonian film with mucosalivary-mimetic PEO solutions. The viscoelastic films still fragment through bags, but the bags inflate further, so their sheets are thinner before they rupture (and, in the simulations, more uniform), and the droplets are smaller. Their simulations use the Oldroyd-B model that we build in §3.

The lecture contrasted two routes from liquid to droplets: jetting, in which liquid is drawn into a jet or filament that then breaks up (the inkjet filaments of §1.1, or the Worthington jets of Lecture 6), and bag-mediated atomisation of a sheared film, as here. In every example a thin film or filament is stretched and thinned, and its fate depends on whether the liquid resists viscously, elastically or both. To say more we need a constitutive model.

2) How do we model polymeric flows?

2.1 Momentum balance

We keep the Cauchy momentum equation,

with the density and the Cauchy stress tensor. Combined with mass conservation, , this is the equation of Bridge 2.5, without body forces. Gravity is left out here, and surface tension enters through the boundary condition at the interface. We consider incompressible liquids, . The equation holds for any continuum; the material enters only through .

2.2 Splitting the stress

Cartoon of a dilute polymer solution: grey coiled polymer chains dispersed in a blue solvent A dilute polymer solution: flexible polymer coils (grey) dispersed in a Newtonian solvent (blue). The solvent contributes a viscous stress; the coils contribute a stress that depends on how stretched they are.

For a dilute polymer solution we write

The pressure enforces incompressibility. The second term is the viscous stress of the solvent, with solvent viscosity : Newton’s law from Lecture 2. The polymer stress does not depend on the instantaneous strain rate but on the state of the polymers, which is encoded in the conformation tensor . It is convenient to write

for the extra stress, the part of the stress that is not pressure. The diagrams in this lecture write this extra stress as ; here we keep the two apart.

2.3 The conformation tensor: an order parameter for polymer stretch

In the simplest microscopic picture each polymer coil is a dumbbell: two beads joined by an entropic spring, with end-to-end vector . The conformation tensor is the average of , normalised by its value at rest:

At rest the coils are isotropic, , so . The tensor is symmetric and positive definite. Its eigenvectors give the directions along which the polymers are stretched on average, its eigenvalues are the squared stretch ratios along those directions, and is the mean-square stretch. The deviation therefore plays the role of an order parameter: it vanishes in the relaxed, isotropic state and measures how far the flow has pulled the microstructure away from equilibrium.

For linear (Hookean) entropic springs the polymer stress is linear in :

where is the number of polymer chains per unit volume and the thermal energy. This is the same entropic modulus as in Lecture 1.

3) The Oldroyd-B family of models

Spring–dashpot diagram of the Oldroyd-B model: a solvent dashpot of viscosity η_s in parallel with a polymeric dashpot of viscosity η_p in series with a spring of elastic modulus G, pulled by a stress σ, next to the relaxation time λ = η_p/G and the retardation time λ′ = η_s/G Mechanical analogue of the Oldroyd-B model. The solvent (blue) acts as a dashpot of viscosity . The polymers (orange) act as a Maxwell element: a dashpot of “polymeric” viscosity in series with a spring of elastic modulus . The two branches deform together and their stresses add. The two time scales are the relaxation time and the retardation time .

The Oldroyd-B model completes the description with an evolution equation for :

The mechanical analogue has two time scales,

so the polymer viscosity is . The upper-convected derivative is

with and .

Why this derivative? If the polymers were simply carried by the flow, each end-to-end vector would deform like a material line element, . Then , which is exactly . The upper-convected derivative is thus the rate of change of seen by a material element that moves, rotates and stretches with the flow. The evolution equation says that the flow stretches the polymers as it stretches material lines, while the polymers relax back towards their equilibrium coil, , on the single time scale . Oldroyd (1950) showed how to formulate rheological equations of state that do not depend on the motion of the observer; convected derivatives of this kind are the key ingredient, and “liquid B” of that paper is today’s Oldroyd-B model.

In steady simple shear the Oldroyd-B viscosity is , whatever the shear rate, while a first normal stress difference appears (self-check 5). There is no shear thinning. The model therefore suits Boger fluids, dilute and elastic polymer solutions whose shear viscosity hardly changes with shear rate; most of the PEO solutions of Li et al. (2025) behave this way.

Which retardation time?

The lecture defines , the retardation time of the Kelvin–Voigt limit (§4). For finite , eliminating shows that the total extra stress obeys

This is the usual textbook retardation time of the Oldroyd-B model. It reduces to when , which is the limit in which matters below.

4) The limits of the Oldroyd-B family

Diagrams of the two limits of the Oldroyd-B model: for zero relaxation time only the solvent dashpot remains, giving a viscous liquid; for infinite relaxation time a spring sits in parallel with the solvent dashpot, giving a Kelvin–Voigt solid, which becomes an elastic solid for zero retardation time and a dissipative system for infinite retardation time The limits of the Oldroyd-B family. Left: , a viscous liquid with . Right: , a Kelvin–Voigt solid with . It is an elastic solid for and a purely dissipative system for , in which the polymers are deformed () but carry negligible stress. The stresses in the diagram are extra stresses, .

4.1 : viscous liquid

At fixed , means . The dashpot in the polymer branch offers no resistance, the spring is never loaded, and the polymers relax instantly: . What remains is a Newtonian liquid,

For small but finite , write in the evolution equation. Because , the leading order gives , and the polymer stress becomes . The polymers simply add a viscosity , and the liquid is Newtonian with viscosity , as long as is short compared with the local deformation time, .

4.2 : Kelvin–Voigt solid

Now : the dashpot in the polymer branch locks, leaving the spring in parallel with the solvent dashpot. The polymers never relax, , and simply records the deformation. Starting from a relaxed state ( initially),

where the deformation gradient maps a material point at in the relaxed reference state to its current position . The polymer stress is that of a neo-Hookean elastic solid (Snoeijer, Pandey, Herrada & Eggers 2020); for an incompressible material the isotropic part can be absorbed into the pressure. With the solvent in parallel,

which is a Kelvin–Voigt solid. Which of the two parallel branches dominates depends on the retardation time compared with the time over which the material is deformed:

  • (): elastic solid, . Solvent damping is negligible.
  • (): dissipative system, . The polymers are deformed and keeps recording the deformation, but on this time scale the stress they carry is negligible compared with the viscous stress, and the response looks purely viscous.
  • of order one: a genuinely viscoelastic solid.

Not every viscoelastic material flows

For any finite the Oldroyd-B material is a viscoelastic liquid: under a constant stress it eventually flows steadily with viscosity (§5.1). The Kelvin–Voigt limit is a viscoelastic solid: under a constant stress its shear strain saturates at , and it recovers completely when the stress is removed. A time-dependent response does not by itself mean that a material flows at long times.

5) Viscosity + elasticity = viscoelasticity

Three cartoons: a fluid layer sheared between two plates with σ = ηγ̇; a solid bar pulled at both ends with σ = Gγ; a polymer-laden bar both pulled and sheared with σ = ηγ̇ + Gγ Viscosity + elasticity = viscoelasticity. A fluid resists the rate of deformation, a solid resists the deformation itself, and a viscoelastic material does both. The in the image is the shear strain, written in the text.

Strip the model down to one dimension. In simple shear, with shear stress , shear strain and shear rate :

  • Fluid: (Newton). Stress is proportional to the rate of deformation, and the work done is dissipated.
  • Solid: (Hooke, in shear). Stress is proportional to the deformation, and the work done is stored.
  • Viscoelastic: .

The cartoon draws the solid being stretched rather than sheared. For uniaxial stretching of an incompressible material the corresponding coefficients are Young’s modulus for small strains (Lecture 1) and the extensional (Trouton) viscosity .

The combined law is exactly the Kelvin–Voigt limit of §4, with . For the simple shear flow starting from , the condition gives and , so and

This holds at any strain, not only small ones: the neo-Hookean shear stress is linear in . What the one-dimensional picture misses are the normal stresses (self-check 4).

5.1 Two ways to combine a spring and a dashpot

Kelvin–Voigt (parallel), . Apply a constant stress from :

There is no instantaneous jump in strain, because the dashpot cannot move in zero time. The strain creeps towards and stays bounded: a solid. If the stress is removed at , the strain decays back to zero as . Imposing a sudden strain instead requires an impulsive stress at , after which indefinitely: there is no stress relaxation.

Maxwell (series), . The spring and dashpot carry the same stress, and their strains add. After a sudden strain the stress relaxes,

Under a constant stress the strain jumps elastically and then grows without bound, : a liquid. If the stress is removed at , only the elastic part is recovered; the viscous part is permanent.

Oldroyd-B (solvent dashpot in parallel with a Maxwell element). Linearised in simple shear, the model gives with .

Creep of the full model

Under a constant stress applied to relaxed polymers at , the linearised model gives

At first the polymers are unstretched and only the solvent resists, so the material starts to shear at the rate . At long times it flows steadily with viscosity : a viscoelastic liquid. As this becomes the Maxwell response; as at fixed and , it becomes the Kelvin–Voigt response with .

5.2 The time scale decides

The comparison that runs through this lecture is between the relaxation time and the time over which the flow deforms the material, the Deborah number . Deformed slowly (), a Maxwell or Oldroyd-B material flows like a liquid. Deformed quickly (), its polymers respond elastically; the full Oldroyd-B response is then solid-like only if solvent damping is also small, , and otherwise it is a Kelvin–Voigt response with a substantial viscous stress. Reiner (1964) named the number after the prophetess Deborah, whose song says that “the mountains flowed before the Lord”: for a material with a finite relaxation time, whether it looks solid or liquid depends on how long you watch it.

6) Parameter space

Three axes labelled with the Deborah number De, the elastocapillary number Ec and the solvent Ohnesorge number Oh_s, next to the dimensionless Oldroyd-B equations and a box stating that both De = 0 and Ec = 0 represent Newtonian liquids The parameter space of the dimensionless Oldroyd-B model. The in the diagram is the dimensionless extra stress .

For the free-surface flows of Lecture 6, take a length scale (a film thickness, or a bubble or drop radius), the density and the surface tension . Measure time in units of the inertio-capillary time and stress in units of the capillary stress . Three dimensionless numbers remain:

The Deborah number compares the polymer relaxation time with the inertio-capillary time, the elastocapillary number compares the elastic modulus with the capillary stress, and the solvent Ohnesorge number compares viscous with inertio-capillary effects. With tildes marking dimensionless quantities, the model becomes

where is already dimensionless and the upper-convected derivative is now taken with respect to . The momentum equation becomes with no prefactors, and the capillary jump in normal traction across the interface is simply the curvature in units of (the pressure jump also includes any jump in the extra normal stress).

Two combinations recur:

The polymeric Ohnesorge number measures the viscosity the polymers add, and is the retardation time in units of . The limits of §4 now sit in this space:

  • : viscous liquid. At small with finite, the liquid is Newtonian with total Ohnesorge number .
  • : Kelvin–Voigt solid. It is elastic when and dissipative when .
  • : the polymer stress vanishes whatever is, leaving a Newtonian liquid with viscosity . At large this is the dissipative limit of §4 seen from the other side, since .

Two routes to a Newtonian liquid

Both and represent Newtonian liquids, for different reasons. At the polymers relax before the flow can stretch them (). At the flow may stretch them (), but they carry no stress.

Two cautions. First, means no polymer stress at all, but a small nonzero does not guarantee a small polymer stress: in a strong stretching flow the Oldroyd-B conformation tensor can grow without bound, so can become of order one (self-check 7). Second, other flows have other natural time scales; for drop impact, Lecture 6 uses the impact time instead. The logic stays the same: compare the material times and with the flow time, and the modulus with the stress that drives the flow.

Summary

  1. Viscous and elastic sheets obey the same momentum balance and can show the same patterns; only the constitutive law differs, and for slow flows the two are mathematically equivalent.
  2. Small amounts of polymer change how liquids fragment: they suppress satellite droplets in inkjet printing, delay the breakup of sneeze ejecta and make thinner bags and smaller droplets in a cough machine.
  3. Polymeric flows are modelled by adding a polymer stress to the Newtonian stress, where the conformation tensor ( at rest) measures polymer stretch. In the Oldroyd-B model it obeys , with and retardation time .
  4. Limits: gives a viscous liquid; gives a Kelvin–Voigt solid, which is an elastic solid for and a purely dissipative system for . For finite the material is a viscoelastic liquid; the Kelvin–Voigt solid is a viscoelastic solid.
  5. In one dimension, is the Kelvin–Voigt solid. It creeps to without an initial jump, whereas a Maxwell element relaxes stress and flows.
  6. In dimensionless form, , and span the parameter space, with and . Both and give Newtonian liquids.

Self-check questions

  1. Show that and are equivalent. Which conservation law do you need?
  2. Show that if every end-to-end vector deforms like a material line element, , then . Use to show that in the limit .
  3. Expand the Oldroyd-B equation for small to show that , and hence that the polymers add a viscosity .
  4. In the Kelvin–Voigt limit, find all components of for a simple shear of amount , and show that the first normal stress difference is . What does the scalar law miss?
  5. For finite in steady simple shear at rate , show that and , that the shear viscosity is , and that . Does the Oldroyd-B liquid shear-thin?
  6. A constant stress is applied for and then removed. Sketch for a Maxwell element and for a Kelvin–Voigt solid. Which one shows an instantaneous strain jump, and which one recovers completely?
  7. For a wt% PEO solution, Li et al. (2025) report ms, a plateau viscosity of mPa·s (against mPa·s for the solvent), kg/m³ and mN/m, for films of thickness mm. Assuming an Oldroyd-B liquid with mPa·s and mm, estimate , , , , and . Then show that in uniaxial extension at rate , grows exponentially when . Why might the polymers matter in a thinning bag even though ?

References

  1. A. T. Oratis, J. W. M. Bush, H. A. Stone & J. C. Bird, A new wrinkle on liquid sheets: Turning the mechanism of viscous bubble collapse upside down, Science 369, 685–688 (2020). doi:10.1126/science.aba0593
  2. D. Vella, A. Ajdari, A. Vaziri & A. Boudaoud, Wrinkling of pressurized elastic shells, Phys. Rev. Lett. 107, 174301 (2011). doi:10.1103/PhysRevLett.107.174301
  3. M. Gomez, D. E. Moulton & D. Vella, The shallow shell approach to Pogorelov’s problem and the breakdown of ‘mirror buckling’, Proc. R. Soc. A 472, 20150732 (2016). doi:10.1098/rspa.2015.0732
  4. U. Sen, C. Datt, T. Segers, H. Wijshoff, J. H. Snoeijer, M. Versluis & D. Lohse, The retraction of jetted slender viscoelastic liquid filaments, J. Fluid Mech. 929, A25 (2021). doi:10.1017/jfm.2021.855
  5. B. E. Scharfman, A. H. Techet, J. W. M. Bush & L. Bourouiba, Visualization of sneeze ejecta: steps of fluid fragmentation leading to respiratory droplets, Exp. Fluids 57, 24 (2016). doi:10.1007/s00348-015-2078-4
  6. J. Wei & Y. Li, Airborne spread of infectious agents in the indoor environment, Am. J. Infect. Control 44, S102–S108 (2016). doi:10.1016/j.ajic.2016.06.003
  7. P. Kant, C. Pairetti, Y. Saade, S. Popinet, S. Zaleski & D. Lohse, Bag-mediated film atomization in a cough machine, Phys. Rev. Fluids 8, 074802 (2023). doi:10.1103/PhysRevFluids.8.074802
  8. M. Li, Y. Saade, S. Zaleski, U. Sen, P. Kant & D. Lohse, Viscoelasticity reduces the droplet size in mucosalivary film fragmentation during intense respiratory events, Phys. Rev. Fluids 10, 084001 (2025). doi:10.1103/zlgy-36dk; preprint arXiv:2502.05105
  9. J. G. Oldroyd, On the formulation of rheological equations of state, Proc. R. Soc. Lond. A 200, 523–541 (1950). doi:10.1098/rspa.1950.0035
  10. J. H. Snoeijer, A. Pandey, M. A. Herrada & J. Eggers, The relationship between viscoelasticity and elasticity, Proc. R. Soc. A 476, 20200419 (2020). doi:10.1098/rspa.2020.0419
  11. M. Reiner, The Deborah number, Phys. Today 17, 62 (1964). doi:10.1063/1.3051374
  12. A. Morozov & S. E. Spagnolie, Introduction to complex fluids, in Complex Fluids in Biological Systems, ed. S. E. Spagnolie, pp. 3–52 (Springer, New York, 2015). doi:10.1007/978-1-4939-2065-5_1 (further reading)

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