For the horizontal film, part (a) gives the lubrication theory equation
The length scale is fixed at , so balancing against gives . The draining viscous film on a finite horizontal plate therefore has the long-time similarity solution
An additive shift of the time origin can represent the initial transient without changing the long-time law. The positive profile is even, with and . Substitution yields
To integrate, put and use . Then
For the decreasing branch has , so inversion gives
The negative half of the profile follows by symmetry.
At the edge, . Set in the integral to obtain
Here is the beta function. Thus , and the centre thickness is
For , the implicit integral remaining between and gives
Consequently the edge region of a draining viscous film has
Its slope satisfies up to a constant factor, so it becomes order one at
The local height is then also , violating the shallow geometry required by lubrication theory. A full local flow is needed to turn the fluid over the edge.
The imposed zero thickness is nevertheless a consistent leading outer boundary condition: , so the unresolved edge height is small compared with the film's bulk height. It should not be interpreted as an exact pointwise prediction inside the edge region. Moreover, at the right edge, so the outward volume flux remains finite even as the outer thickness tends to zero. The singular slope is what allows this outer solution to describe drainage.
For an axisymmetric viscous gravity current on a cone, the cylindrical radius at slant distance is . A surface annulus therefore has area . The local downslope volume flux is the same as in part (a), but conservation of mass must account for this growing circumference. Thus
This is a leading thin-film description away from the apex, with and thickness small relative to the local curvature and streamwise length scales.
The original PDF uses the long-time criterion ; the local TeX incorrectly reads . To see why the PDF criterion is the relevant one, scale . In the bulk, the hydrostatic-gradient term relative to direct downslope gravity is
Hence the leading outer evolution, with , is
For a fixed-volume similarity solution, let and . Conservation of mass gives , while the evolution equation gives . Thus , . Writing , , yields
The positive branch satisfies this equation when . It gives
The ideal outer current has zero thickness beyond its front. Its mass integral is
Therefore
The reduced equation is a conservation law after multiplication by . Its front obeys the Rankine-Hugoniot condition, , consistent with the mass-derived front position. The outer profile has a finite jump at the front; the omitted hydrostatic-gradient term resolves a narrow front region. There is also a small apex region where the outer gradient and conical curvature violate the local approximations. Neither region sets the leading conserved-volume scaling above.
Let measure distance normal to the plane, with the wall at and the free surface at . Take density , dynamic viscosity , and gravitational acceleration . In lubrication theory, normal momentum balance gives hydrostatic pressure while inertia and streamwise viscous derivatives are smaller. With negligible surface tension and negligible air shear,
Apply the no-slip boundary condition at , and zero leading tangential stress at . The velocity profiles are
Depth integration gives the volume flux, with :
Combining incompressibility with the wall and surface kinematic conditions gives conservation of mass, . Therefore the two-dimensional version of the gravity-driven thin film on an incline satisfies
Direct downslope gravity supplies the advective term, while gradients of the hydrostatic pressure spread the film along the surface. At this reduces to nonlinear gravitational spreading in a horizontal film.
Take to be the force and couple exerted by the body on the fluid, equivalently the external force and couple needed to maintain its motion. This fixes the sign for a positive hydrodynamic resistance matrix. If one uses the fluid's force on the body, both resultants have the opposite sign.
For two Stokes flows and in the same fluid domain , with zero body force, the Lorentz reciprocal theorem for Stokes flow is
Here points out of the fluid. To see the identity, take the divergence of the difference of the two cross-work fluxes. The stress divergences vanish, while incompressibility and symmetry of the Newtonian fluid stress tensor reduce the remaining terms to . The divergence theorem proves the result.
On the body, the no-slip boundary condition is , and the far-field contribution vanishes for decaying exterior flows. Reciprocity becomes
With and , this is for all pairs, so . The power identity gives
Equality would force zero strain throughout the connected exterior domain, hence a rigid fluid motion. Decay at infinity makes that motion zero, and the no-slip boundary condition then gives . This proves the symmetry and positivity of a rigid-body resistance matrix:
For the helix, assume and use cylindrical unit vectors. Its arclength element and tangent are
Integrating to gives . In a combined axial translation and rotation, . The slender-body force density, or local resistive-force theory, gives
Writing , , its axial and azimuthal components are
The axial couple density is . Integration over arclength gives the axial resistance matrix of a slender helix:
Thus pure translation gives , and pure rotation gives . The mixed coefficients agree, as reciprocity requires, and . The sign of follows the handedness in the parametrization; reversing handedness reverses propulsion.
For the helical microswimmer with a spherical head, the diagram's rotation relation is . Neutral buoyancy and the absence of external forcing make the whole swimmer force-free and torque-free. Neglecting interactions between its parts gives
With , solving this pair gives
The head counterrotates, providing the reaction to the flagellum's rotation. The figure fixes this relative rotation convention; it is duplicated and corrupted in the local TeX.
For a very large head, the coefficient regime is and . Consequently
The large translational resistance makes the microswimmer slow even though the flagellum rotates almost at the motor rate.
For a very small head, and . The appropriate denominator retains the translation-rotation coupling:
Both tend to zero with , while . The motor mainly rotates the low-resistance head, and produces little flagellar motion relative to the fluid.
In the intermediate coefficient regime and , the head supplies a strong rotational reaction with little translational penalty. Then
The head radius has dropped out. To find the optimal pitch of a helical microswimmer, put . The dimensionless speed becomes and has derivative . Hence, for with the chosen handedness,
The angle is measured from the horizontal plane. An intermediate pitch combines axial and transverse tangent directions, allowing anisotropic drag to convert rotation into translation; either extreme removes that coupling.
The geometric head-size regimes quoted in the paper hold with the logarithmic slenderness factor treated as fixed. More precisely, requires , while requires . These coefficient inequalities state the validity of the intermediate approximation when the logarithm is quantitatively important. The many-turn and local-drag assumptions of slender-body theory also remain in force.
Let denote the Taylor polynomial at zero. On , the integrand defining the Hadamard finite-part reciprocal-power distribution is
The first term is odd, so it cancels under symmetric truncation. The Taylor remainder in the second term has absolute value at most . The integral near zero therefore has a finite limit. For , the original terms are integrable: has compact support, and each subtracted power has exponent .
This proves existence and linearity. It also gives the global estimate
Thus
In particular the order of a distribution is bounded by one integer on all compact sets, not merely separately on each of them.
For the recurrence, write the truncated Hadamard finite-part integral as
where parity evaluates all subtraction integrals explicitly:
Set and . On the two truncated intervals, integration by parts gives
There are no boundary contributions at infinity. The coefficients of the subtraction terms satisfy
This is exactly the negative of the boundary term's Taylor polynomial through degree ; the degree- term itself vanishes by parity. Hence
Taking the limit proves the full distributional identity
The same calculation includes . Starting with the distributional derivative of the logarithmic modulus from part (i), induction yields
This identity holds on all of as a distributional identity. It is stronger than matching the ordinary derivatives away from zero, which would leave possible differentiated Dirac delta distributions at zero undetermined.
The space of test functions is . A sequence converges to when all functions eventually have compact support in one compact set and every derivative converges uniformly:
A distribution is a continuous linear functional on this space of test functions. Equivalently, for each compact set , there are and a finite integer such that
The integer is permitted to depend on . The usual weak convergence of distributions is
Thus the convergence convention on the distribution space is its weak dual topology.
For the principal-value reciprocal distribution, the symmetric truncations can be written
The numerator is near zero by the mean value theorem, and the integrand vanishes for large because has compact support. For ,
Consequently the Cauchy principal value defines a distribution of order of a distribution at most one.
The function has local integrability, since , and therefore defines a distribution. For its distributional derivative, remove and use integration by parts on both remaining intervals:
The boundary term is and tends to zero. The omitted integral of tends to zero by local integrability. Hence the distributional derivative of the logarithmic modulus satisfies
Symmetric truncation is essential to this normalization of the principal-value reciprocal distribution.

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