For the supplied hillslope values,
The Froude number is below one, but it is not extremely small numerically; the much smaller products actually multiplying inertia and the depth-gradient term justify their leading neglect. Positive flow then satisfies and
In overland flow the source is net rainfall input after infiltration into soil, with evaporation or other local losses included when important. Lateral inflow can also contribute. Negative net input must be limited by water availability once the surface dries.
Manning's uniform-flow law implies the friction slope for positive downstream flow. In a wide rectangular section and , so .
Scale distance with , depth with , velocity with , and time with . Divide momentum by to obtain
The factor compares depth change over with the mean bed drop , rather than with alone. Its product with measures inertial acceleration relative to bed-slope forcing.
Here is downstream distance, the wetted cross-sectional area, the section-averaged downstream velocity, and the lateral water input per channel length and time. Thus is local water storage and the divergence of discharge. Their balance is mass conservation.
The momentum terms and are local and advective acceleration. The bed slope gives the downstream gravitational acceleration . Bed shear stress acting over wetted perimeter produces resisting force per unit mass ; the hydraulic radius is . Finally is the hydrostatic free-surface pressure-gradient term in the chosen bed-following description. The Saint-Venant approximation depth-averages the flow, assumes a long shallow geometry and hydrostatic pressure, and closes the boundary shear through a roughness law.
For quasi-steady enzyme kinetics at low substrate saturation, the quasi-steady-state approximation is controlled here by , rather than by alone. Even with , taking makes and .
After the initial fast layer , the third equation gives
Since , the last equation gives . Starting from , this implies on bounded intervals of the slow time. The quasi-steady second equation then gives . In the first equation,
Matching to the initial substrate value therefore yields . The relation is an outer approximation: it does not replace the initial layer needed to reconcile with . Likewise the smallness of accumulated inactivated enzyme has been justified for bounded slow times, not arbitrarily long times.
The conserved total is under the chosen initial conditions. Substitute into the equations from the previous part. This closes the subsystem for ; product can be recovered afterward by integrating .
Let and . The required nondimensionalization is completed by
Indeed and the free-enzyme fraction is . Substitution and division by the indicated time scale give
For example explains the coefficient in the third equation. The small multiplier on the intermediate-species derivatives identifies their potentially fast adjustment relative to substrate depletion.
Write concentrations as in this calculation. The law of mass action assigns the forward bimolecular rate and the first-order rates . Each species gains the rates of reactions producing it and loses those consuming it:
Adding the equations for all enzyme-bearing species cancels every reaction rate, so . This is conservation of the total enzyme-derived material, including the inactivated form. It does not assert conservation of active enzyme: mechanism-based inhibition transfers some of that conserved material irreversibly into .
For an experiment beginning by mixing unbound enzyme with substrate, take . The enzyme-substrate complexes, inactivated enzyme and product are initially absent. Nonzero pre-existing product could be allowed without changing the dynamics here, since it has no feedback reaction in the specified scheme.
At the crossing the angular frequency is , so the limiting small-amplitude period is
This is the period of the bifurcating infinitesimal oscillation. Finite-amplitude oscillations away from the threshold need not have period exactly .
For a purely imaginary root with , separating real and imaginary parts gives
Thus and , . The first crossing is
For there is no root with nonnegative real part. Indeed, write with . The real equation forces , hence . But the imaginary equation gives , contradicting .
Differentiate the characteristic equation along the root:
The imaginary roots are simple because , and they cross into the unstable half-plane as delay increases.
One can also check the nonlinear Hopf bifurcation directly. With and small amplitude , substitute
The constant and second harmonics at order give the displayed coefficients. Put . At order , absence of resonant first harmonics requires and . Hence
The nonzero coefficient verifies a branch of small periodic solutions for , consistent with the transverse Hopf bifurcation in the delayed logistic equation. This is the delayed logistic Hopf threshold.
Put . Then , so the linearization is . A mode gives the characteristic equation of a delay differential equation
For real , the left side is nonnegative and the right side negative. The two real graphs therefore never meet there, as drawn in the figure. There is no nonoscillatory exponential instability. If stability is lost, the unstable eigenvalues must be a nonreal conjugate pair, producing oscillatory growth; absence of a positive real root alone does not imply stability.
On the attracting right branch, the leading fast balance is , so . On the left branch it is , so . The slow travel times are therefore
Both are positive because . The fast jumps contribute vanishing time as , giving the piecewise linear relaxation-oscillator period
For the illustrated , , the leading period is in the given nondimensional time units.
The nullclines are and . The two outer pieces of have slope ; the middle piece has positive slope
The curve is continuous, with folds and . The unique equilibrium is . Its Jacobian matrix has trace and determinant , so it is unstable. The outer branches attract the fast voltage motion.
Let and . The hypothesis gives . The singular relaxation oscillation follows this route:
  • On the right branch , slowly increases from to .
  • At , the fast voltage jumps from to .
  • On the left branch , slowly decreases from to .
  • At , voltage jumps from to .
The jumps are almost horizontal in the phase plane, because changes negligibly on the fast time. Below , voltage increases; above it, voltage decreases; increases on the right of and decreases on the left. These signs provide a closed trapping region around the indicated route for sufficiently small positive , with the unstable equilibrium excluded, giving a periodic orbit by the planar return-map or Poincaré-Bendixson theorem argument. The continuous piecewise linear field is locally Lipschitz, so solution uniqueness is available at the corners.
The voltage nullcline is and the recovery nullcline is . In the relevant region , so below the voltage curve and above it . Below the recovery curve , while above it .
For small , the outer voltage branches with attract fast voltage motion; the middle branch with repels it. Arrange the intersections so the equilibrium is on that middle branch, with recovery increasing along the high-voltage attracting branch and decreasing along the low-voltage attracting branch. The trajectory then drifts towards a fold, jumps rapidly to the other attracting branch at nearly constant , and repeats. This is a relaxation oscillation.
The local linear stability calculation supports the construction. At an equilibrium,
A sufficiently steep recovery curve gives positive determinant, while gives positive trace. Hence the equilibrium is a repeller. The bounded physical rectangle can be chosen forward invariant, and a small neighborhood of the repeller removed to give a trapping annulus. The Poincaré-Bendixson theorem then supplies a periodic orbit. These conditions can be realized because the recovery function and the applied current control the intersection and its slope; oscillation is possible, not forced for every choice.
For the illustration, , , , , , and . The rectangle has inward-pointing flow, and the displayed numerical trajectory realizes the folded-branch mechanism.
Write . In the physically relevant strip , , the zero-current nullcline satisfies
The left side increases strictly from zero to infinity, so there is exactly one nullcline height for each interior voltage. If is positive at the endpoints, its curve joins to ; when low-voltage activation is idealized as exactly zero, the limiting left branch can lie on .
The signs of the derivatives explain its folds:
At low voltage, potassium's approximately linear contribution dominates and . During rapid sodium activation the last negative term can dominate, giving . Once activation saturates, becomes small and again. This folded conductance-model nullcline has the familiar shape: the curve has descending outer branches and an ascending middle branch in the plane. Equivalently, an intermediate fixed can give three zeros of as voltage rises, with positive, negative and positive at those crossings.
The rapid-activation description permits this folded shape; exact fold positions depend on . The figure supplies an explicit admissible sigmoid example. Its right panel shows as well as the recovery nullcline and an oscillating trajectory.
Put , use proper time , and denote its derivatives by dots. The timelike geodesic equations, away from the Schwarzschild coordinate singularity, are
with normalization . Spherical symmetry permits an equatorial plane, , and the cyclic coordinates give . Normalization then gives .
For and , . Thus
At , , the right side factors as . Set , so and . Integrating the regions and gives, up to angular shifts and time reversal,
The constant , or , is the corresponding circular timelike orbit. The hyperbolic-tangent branch lies at and approaches that orbit from outside as ; the hyperbolic-cotangent branch lies at and approaches it from inside. Near the limit decays exponentially as . Since tends to , the limiting approach also takes infinite proper time. Neither nonconstant branch reaches and joins the circular orbit at a finite angular parameter.
Differentiating the orbit equation gives . A perturbation about obeys , showing that the circular orbit is unstable. The two explicit curves are its separatrix branches, not ordinary small stable oscillations. For the energy is marginally bound, so the outer critical branch is the limiting orbit between scattering and Schwarzschild marginally bound capture from infinity. Time-reversed inner and outer branches describe the corresponding approach or departure from that unstable orbit. These are the Explicit separatrices of the marginally bound Schwarzschild orbit.
Write and restore for the numerical estimate. A stationary clock at radius has . Let radii and denote the upper and lower computers. The metric is stationary and the same two fixed spatial points exchange both signals, so each signal has the same coordinate propagation time. Therefore the interval between reception events equals the interval between emission events in coordinate time: the common delay cancels.
For upper proper running time , the lower computer has run for
In the weak gravitational field near Earth's surface, and
The lower clock runs more slowly, so its remaining work is
Thus about 660 micro-operations remain; the proper-time shortfall is only about seconds.
Successful comparison tests the gravitational dependence of stationary proper-clock rates, specifically the radial variation of and its weak-field gravitational redshift prediction, assuming the computers execute equally per unit proper time. It also checks that this clock effect is independent of the chosen physical clock mechanism. It does not separately verify the Schwarzschild radial metric coefficient: although light propagation uses the null metric, the identical start and finish propagation delays cancel from this particular observable. This is Gravitational redshift measured by a computation counter.
For identical fermions the full wave function is antisymmetric:
In particular it vanishes when the two complete one-particle arguments coincide. Applying this to the position-only model assumes that no independent spin symmetry changes the required spatial parity.
For identical bosons the full wave function is symmetric under the particle exchange operator:
In the given position-only model this is the spatial parity under the particle exchange operator. If additional spin variables are present, the symmetry applies to the complete state including them.
Under the pricing measure, the ex-dividend stock drift is . Thus
A direct replication holds shares and reinvests every dividend into more shares. The share count grows at rate , reaching two shares at expiry, with no external cash input. This payoff contains only the terminal ex-dividend stock value, unlike part (b), which also includes the separately accumulated dividends.
The diffusion associated with the displayed pricing equation is . For , Itô's formula gives
The drift vanishes by the PDE. Under the usual integrability conditions for the payoff and solution, localization and conditional expectation make a true martingale; for polynomial-growth data the lognormal moment bounds provide the needed integrability. Applying the terminal condition yields the Feynman-Kac formula
The printed diffusion contains an additional undefined factor multiplying . If literally retained, its second-order generator coefficient would be , so the requested representation would correspond to that different PDE unless . The formula above uses the volatility specified by the stock model and by part (c).

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