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FR26 · Conformation and stress

Coil–Stretch Transition: Polymers in Shear and Extension

Why does the same polymer solution barely change in shear yet stiffen enormously when stretched? Shear keeps rotating each polymer coil away from the direction it stretches, so the coils lengthen only a little and the viscosity barely moves. Extension has no such rotation. Once the stretching rate exceeds half the coil relaxation rate, the chain unravels until its finite length stops it, and the extensional viscosity can climb a hundredfold above the shear viscosity.

Start shear and planar extension at the same rate. Past a critical rate the extending coils unravel and resist a hundred times harder, while shear barely changes.

Interactive modelCoil–Stretch Transition: Polymers in Shear and Extension
Coil stretch in extension6.45×6.45\times
Coil stretch in shear1.19×1.19\times
Extension over shear viscosity114114
Extension rate Wi\mathrm{Wi}0.80.8
Stress growth after startup
Steady viscosity versus rate
Energy ledger in extension
More numbers and how they are computed
Time shown on the stage
00
Shear rate times relaxation time
00
Transient shear viscosity
00
Transient planar extensional viscosity
00
Shear: normal-stress difference over shear stress
00
Extension stretch at the end of the run
00
Largest share of the finite-extension bound used
00
Smallest conformation eigenvalue in the run
00
Largest mismatch of work minus stored minus dissipated
00
Runge–Kutta steps in both runs
00

Steady curves solve the algebraic steady state by bisection on the spring factor; the Oldroyd-B extension curve ends where no steady state exists. The dashed lines are the same run with an infinitely extensible spring, shown as a reference, not as data.

Physics tutorial

Rotation saves a coil; pure stretching does not

BackgroundA dissolved polymer is a random coil that thermal motion keeps pulling back to its rest size. A flow drags its two ends apart. Which wins depends on how fast the flow stretches compared with how fast the coil relaxes.

Why it mattersShear and planar extension at the same rate stretch fluid elements equally fast at first. In shear the flow also rotates every coil away from the stretching direction; in extension nothing rotates it away.

Start with the essentials

Focus question
Why does the same polymer solution barely change in shear yet stiffen enormously when stretched?
One-sentence intuition
Above Wi=1/2\mathrm{Wi}=1/2 planar extension stretches a linear dumbbell faster than it relaxes, so the stretch grows exponentially. Only the finite length of a real chain stops it, and the extensional viscosity then sits orders of magnitude above the shear viscosity.

Core mathematical model

Conformation tensor and polymer stress

A▽=−fA−Iλ,τp=G (fA−I),f=L2−3L2−tr⁡A\overset{\triangledown}{\mathbf A}=-\frac{f\mathbf A-\mathbf I}{\lambda},\qquad \boldsymbol\tau_p=G\,(f\mathbf A-\mathbf I),\qquad f=\frac{L^2-3}{L^2-\operatorname{tr}\mathbf A}

A\mathbf A is the average end-to-end tensor scaled so that it equals the identity at rest. The upper-convected derivative carries it with the flow. Oldroyd-B is the limit f=1f=1.

Startup of shear, Oldroyd-B

η+(t)=ηs+ηp(1−e−t/λ),N1+(t)=2ηpλγ˙2[1−(1+tλ)e−t/λ]\eta^+(t)=\eta_s+\eta_p\left(1-e^{-t/\lambda}\right),\qquad N_1^+(t)=2\eta_p\lambda\dot\gamma^2\left[1-\left(1+\tfrac{t}{\lambda}\right)e^{-t/\lambda}\right]

Shear viscosity never exceeds its zero-rate value, whatever the rate. The normal-stress difference grows with the square of the rate instead.

Steady planar extension, Oldroyd-B

Axx=11−2Wi,ηP=4ηs+4ηp1−4Wi2A_{xx}=\frac{1}{1-2\mathrm{Wi}},\qquad \eta_P=4\eta_s+\frac{4\eta_p}{1-4\mathrm{Wi}^2}

The steady state exists only below Wi=1/2\mathrm{Wi}=1/2. Above it the startup grows like e(2Wi−1)t/λe^{(2\mathrm{Wi}-1)t/\lambda} without bound.

Energy ledger of the polymer

∫0tτp:∇u dt′=ψ(t)+∫0tG2λ∑i(fai−1)2ai dt′\int_0^t\boldsymbol\tau_p:\nabla\mathbf u\,dt'=\psi(t)+\int_0^t\frac{G}{2\lambda}\sum_i\frac{(f a_i-1)^2}{a_i}\,dt'

Work done on the polymers is either stored as elastic free energy ψ\psi or dissipated; aia_i are the eigenvalues of A\mathbf A. The dissipation is never negative.

Common difficulties

Same rate, same stretch?

Typical misconceptionShear at a given rate stretches polymers as much as extension at that rate.

Better mental modelShear is half stretching and half rotation. The rotation tips a stretched coil toward the flow direction, where the stretching component no longer pulls on it, so the shear stretch saturates while the extension stretch keeps growing.

A diverging viscosity

Typical misconceptionOldroyd-B predicts a real liquid with infinite extensional viscosity.

Better mental modelThe divergence comes from a spring that can stretch forever. A finite chain caps the stretch, which FENE-P captures, and real chains also show hysteresis that neither model contains.

Run the experiment

  1. 01

    Watch both cells

    Play Coils unravel and watch the coils in each cell.

    What to observe: Shear coils tilt and lengthen a little; extension coils keep stretching along the outflow axis, and the stress-growth curve for extension climbs by two orders of magnitude.
  2. 02

    Drag the top plate

    Drag the top-plate handle left until the extension rate reads below one half.

    What to observe: The extension coils stop growing and settle at a modest size, and the steady-viscosity marker slides back below the coil–stretch line.
  3. 03

    Hold the stress instead

    Choose Stress puts on the brakes.

    What to observe: The extension rate starts high, then the growing polymer stress takes over the load and the rate falls toward one half, while shear creeps to a steady rate.

Related experiments and articles

Complex fluids · Reading path

Relaxation, stretching, extension and elastic instability

Articles on this path that use this experiment, followed by the other experiments they suggest.

  1. ArticleFrom a bead-spring dumbbell to the conformation tensor and the Oldroyd-B equation
  2. ArticleWhy extensional flow unravels polymer coils while shear only tumbles them
  3. ArticleHow finite chain length caps stretch and extensional viscosity in the FENE-P model
  4. ArticleHow normal stress along curved streamlines drives elastic instability
  5. LabElastic Instability: Symmetry Breaking in a Four-Roll MillFind curvature and stretching in a four-roll flow
  6. ArticleHow a four-roll flow loses symmetry at its stagnation point, and how much the numerics change it
  7. ArticleReading elastic turbulence: the evidence for chaotic flow without inertia, and what is still open
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