An entropic network has approximately one thermal energy of elastic cost per mesh volume, giving . At , the supplied mesh size and viscosity give
The intermediate-time plateau in the three-dimensional mean squared displacement is
After the omitted fast initial transient, the log-log sketch is approximately flat for , crosses over near , and grows linearly for . The figure shows the Maxwell compliance prediction over this range.
Figure 1.
Elastic plateau and diffusive growth in the ideal Maxwell microrheology prediction, with the video time scale marked
. Details.
An ordinary 25–30 frame-per-second recording samples intervals of about –, comparable to . It therefore has little access to a clear plateau at lags well below the crossover, even if its positional precision resolves a displacement of a few tenths of a micrometre. Higher frame rates and calibrated localization noise would improve the modulus measurement. The bead radius is only twice the mesh size, so treating the network as a homogeneous continuum is also an approximation.
Under a step stress, the Maxwell spring extends immediately by , while the dashpot adds . Hence , and the microrheology of a Maxwell fluid relation gives
This idealized overdamped relation describes an elastic plateau followed by long-time diffusion. Its nonzero extrapolated intercept is not the actual displacement variance at exactly zero lag, which is zero. Inertia or fast solvent relaxation must resolve the initial rise; those processes were omitted from the ideal spring-dashpot model.
Passive microrheology uses thermal bead motion as a probe of mechanical compliance. The fluctuation-dissipation theorem relates equilibrium displacement fluctuations to the same linear response measured by a small applied force. The stated thermal stress scale has units of energy per bead volume; dividing the mean-square displacement by provides a dimensionless effective strain. With that prescribed analogy,
The displacement is relative to the starting position, and the variance here is the sum over three spatial coordinates. For a Newtonian fluid, substitution gives , exactly the Stokes–Einstein relation .
The continuum interpretation assumes a dilute no-slip spherical probe, thermal equilibrium, linear response and a homogeneous incompressible medium on the bead scale. The stated stress estimate is an effective scale for the analogy; a literal instantaneous stress variance would also require a microscopic or temporal averaging prescription.
The creep compliance is the strain per unit step stress: if , then for . A Newtonian fluid obeys , so under constant stress its initially zero strain grows as . Therefore
For the convention , the complex viscoelastic modulus is . Thus
The storage modulus exceeds the loss modulus for , so the response is predominantly solid-like above the crossover
At low frequency ; at high frequency .
The Maxwell model has a spring of modulus in series with a dashpot of viscosity . Their stresses are equal and strains add, giving . After a step strain , the strain rate is zero for , so with . Initially the spring takes the step, . Hence
A linear viscoelastic fluid responds linearly to small imposed strain histories but retains memory of earlier deformation. For shear strain and a relaxed initial state, Boltzmann superposition gives
Here is the causal relaxation modulus, the stress following a unit step strain. Doubling a sufficiently small strain history doubles the stress, and responses to added histories add. Elasticity stores deformation energy; viscosity dissipates it. Linearity is an amplitude approximation, not an assertion that the material has no relaxation times.
For a microscopic swimmer, the Reynolds number is usually small. Taking , and water-like properties gives . The Stokes equations then balance viscous stress and pressure almost instantaneously, so a swimmer cannot coast appreciably when its propulsive stroke stops.
The scallop theorem rules out a reciprocal opening-and-closing stroke in an otherwise unchanged Newtonian environment: reversing the sequence of shapes reverses the motion, and changing the stroke speed does not prevent cancellation. Organisms therefore use nonreciprocal motion. A sperm-like bending wave travels along a flagellum; a bacterium can rotate a helical flagellar bundle. The unequal parallel and perpendicular drag of a slender filament converts those motions into a net thrust. A freely suspended swimmer is force-free and torque-free overall, so body drag balances thrust and the body counter-rotates against the rotating bundle. Tracking a body and its flagellum together can reveal these opposite rotations. The helical microswimmer with a spherical head makes that force and torque balance quantitative.
DLVO theory combines the attractive Van der Waals force with repulsion between overlapping electrical double layers. A charged colloid attracts counterions; their electrostatic and osmotic response screens its field over the Debye length. Adding salt generally shortens this range and can lower the repulsive aggregation barrier, allowing particles to reach the strongly bound primary minimum. A shallow secondary minimum can instead give weak reversible association. Whether Brownian encounters cause rapid aggregation depends on barrier heights relative to , not just on the sign of the force at one separation.
Adsorbed or grafted polymer layers can provide steric stabilization: overlap costs chain entropy and increases the local osmotic pressure. Nonadsorbing smaller particles or polymers can create a depletion force, because bringing large surfaces together increases the volume accessible to the smaller species. Polymer bridging can be attractive when one chain binds more than one particle. A useful comparison experiment varies salt concentration while monitoring scattered light or aggregation, then repeats with a sterically protected suspension. Charge, solvent quality, polymer coverage and particle size determine which interaction dominates; none is a universal constant of all colloids.
The restoring force in ideal rubber elasticity is mainly entropic: stretching restricts the conformations of network strands. A Gaussian chain of statistical segments of length has extension free energy , so its small-extension spring constant is proportional to . For an affine network with active-strand number density , the shear modulus is approximately . Increasing the cross-link density normally raises and shortens the strands; polymer entanglement can add effective constraints. Dangling ends and loops do not contribute like elastically active bridges, while junction fluctuations reduce the affine-network estimate.
For incompressible uniaxial stretching by ratio , the nominal tensile stress is in the ideal Gaussian-network model. Finite contour length causes stronger stiffening as strands approach full extension; swelling dilutes the active strands and changes their reference conformations. A direct demonstration is to hang a load from a stretched rubber strip and warm it gently: an entropy-dominated network tends to contract under that fixed load. This temperature dependence contrasts with a model based solely on stretching bond energies. The simple formula assumes equilibrium, adequate cross-linking and temperatures away from glass transitions or degradation.
A liquid crystal flows like a liquid while retaining some molecular order. In a nematic liquid crystal, elongated molecules have long-range orientational order but no ordinary positional lattice. The nematic director specifies the preferred axis, with and equivalent for head-tail-symmetric molecules. The nematic order parameter distinguishes an isotropic distribution, , from perfect parallel alignment, . A smectic phase additionally has a periodic layered density modulation, while molecules remain mobile within layers.
The broken rotational symmetry allows birefringence and distinct elastic costs for nematic splay, nematic twist and nematic bend. Under crossed polarizers, rotating a thin aligned sample changes the transmitted intensity because its two optical polarization components acquire different phases. Heating through a nematic-to-isotropic transition removes that orientational birefringence. An electric field can rotate the director if the dielectric anisotropy of a nematic favors alignment, explaining the optical switching principle of a liquid-crystal cell. Molecular shape, temperature, concentration and surface anchoring determine which ordered phase appears.
The mean interface height fluctuation is zero; its root mean square roughness is obtained by summing the mode variances. Replacing the two-dimensional wavevector sum by its continuum density gives the thermal roughness of a tension-dominated interface:
Take with , and with . At ,
The logarithm makes the answer only weakly sensitive to order-one choices of cutoff. Gravity has been omitted as stipulated; the fixed mean height removes the zero wavevector mode.
For the symmetric regular solution model, the dimensionless mixing free energy is . At the thermodynamic critical point, its second and third derivatives in composition vanish. The third derivative gives ; the second then gives . Therefore
This uses the equal-size, composition-symmetric mixture model.
For complete wetting, the meniscus has curvature radius equal to the capillary radius . The Young–Laplace equation gives the supporting pressure difference . Balance it against the hydrostatic pressure . Taking the sap's mass density to be water-like, , gives
This is the height supported by the stipulated capillary-pressure model. The density assumption is needed because the surface tension and capillary diameter alone do not determine a height.
The nearly-free electron model treats a weak periodic potential as a perturbation of plane waves. Near a Bragg plane, states with wavevectors and are nearly degenerate and must be mixed together. Their two-state Hamiltonian is
At the unperturbed crossing, the band gap is . The corresponding standing waves place different charge densities near the ions and between them, giving different potential energies. Far from a crossing, ordinary perturbation theory is adequate; near it, the degenerate two-wave calculation is essential. In three dimensions, gaps at individual zone boundaries do not guarantee a global insulating gap because bands from different directions can overlap.
A partly filled one-dimensional energy band is especially sensitive to a lattice modulation at . At half filling, , so the Peierls distortion alternates the bond lengths and doubles the primitive unit cell. Mixing states at the Fermi points opens a band gap, lowering the energy of occupied states. In the ideal weak-coupling, zero-temperature chain, the electronic gain behaves as while the elastic cost is proportional to , favouring a small distortion. The dimerized tight-binding chain gives an explicit band calculation.
The structural signature is extra diffraction intensity at the modulation wavevector; optical absorption can detect the gap and transport can detect loss of metallic conduction. A dynamic precursor is a Kohn anomaly, with phonon softening near . Inelastic neutron scattering of TTF-TCNQ, using a deuterated sample over –, found an anomaly near developing below about as the transition was approached. This probes a lattice mode coupled to the electronic instability rather than inferring distortion from resistance alone.[ref]
Away from half filling, the modulation need not simply double the lattice. Finite-temperature ordering in real quasi-one-dimensional solids also involves interchain coupling and fluctuations; the ideal isolated-chain argument alone does not establish a finite-temperature transition.

Pinned article: Introduction to the OurBigBook Project

Welcome to the OurBigBook Project! Our goal is to create the perfect publishing platform for STEM subjects, and get university-level students to write the best free STEM tutorials ever.
Everyone is welcome to create an account and play with the site: ourbigbook.com/go/register. We belive that students themselves can write amazing tutorials, but teachers are welcome too. You can write about anything you want, it doesn't have to be STEM or even educational. Silly test content is very welcome and you won't be penalized in any way. Just keep it legal!
We have two killer features:
  1. topics: topics group articles by different users with the same title, e.g. here is the topic for the "Fundamental Theorem of Calculus" ourbigbook.com/go/topic/fundamental-theorem-of-calculus
    Articles of different users are sorted by upvote within each article page. This feature is a bit like:
    • a Wikipedia where each user can have their own version of each article
    • a Q&A website like Stack Overflow, where multiple people can give their views on a given topic, and the best ones are sorted by upvote. Except you don't need to wait for someone to ask first, and any topic goes, no matter how narrow or broad
    This feature makes it possible for readers to find better explanations of any topic created by other writers. And it allows writers to create an explanation in a place that readers might actually find it.
    Figure 1.
    Screenshot of the "Derivative" topic page
    . View it live at: ourbigbook.com/go/topic/derivative
  2. local editing: you can store all your personal knowledge base content locally in a plaintext markup format that can be edited locally and published either:
    This way you can be sure that even if OurBigBook.com were to go down one day (which we have no plans to do as it is quite cheap to host!), your content will still be perfectly readable as a static site.
    Figure 5. . You can also edit articles on the Web editor without installing anything locally.
    Video 3.
    Edit locally and publish demo
    . Source. This shows editing OurBigBook Markup and publishing it using the Visual Studio Code extension.
  3. https://raw.githubusercontent.com/ourbigbook/ourbigbook-media/master/feature/x/hilbert-space-arrow.png
  4. Infinitely deep tables of contents:
    Figure 6.
    Dynamic article tree with infinitely deep table of contents
    .
    Descendant pages can also show up as toplevel e.g.: ourbigbook.com/cirosantilli/chordate-subclade
All our software is open source and hosted at: github.com/ourbigbook/ourbigbook
Further documentation can be found at: docs.ourbigbook.com
Feel free to reach our to us for any help or suggestions: docs.ourbigbook.com/#contact