Direct differentiation gives with , so is a conservative vector field and its integral depends only on the endpoints. In contrast,
is nonzero, for example at . Thus is not conservative. Both earlier paths lie in the surface , where the two fields happen to coincide. This illustrates why coinciding path integrals need not imply a conservative field.
For , the velocity is . Because throughout this path, both fields again agree pointwise, now as . Thus
These equal values alone do not establish path independence for either field on all of space.
On the straight path , , both fields restrict to . Dotting with gives
The trace is unchanged by transposition and is cyclic under a product. With and ,
Thus . In components this is the vanishing contraction of a symmetric tensor with an antisymmetric tensor.
For , the required right-hand matrix has twice the first row of , the same second row, and twice the third row. Left multiplication scales rows, so
Equivalently, right multiply the given equation by to obtain the same answer.
The determinant is , so for the inverse matrix is
The specified equations use , with right-hand side . Multiplying by gives
In particular the parameter in the inverse formula must be set to four, not left arbitrary for this numerical system.
The cumulative distribution function must tend to one at infinity, so . Differentiation gives the probability density function for and zero for ; there is no atom at zero. This is an exponential distribution of rate one. Its first two moments are and , so
For , the natural logarithm satisfies . Squaring therefore decreases its value, while . Pointwise comparison gives , so
As a check, integration by parts gives , and , consistent with this order.
Figure 1.
Pointwise ordering of the three logarithmic integrands
. Original plot on . The natural logarithm rises from zero to one, so its square lies below it, and twice the logarithm lies above it. Integrating preserves the strict order. Details.
The partial fraction decomposition is . Since both endpoints are positive, integration gives
Orient the three faces outward from the tetrahedron. The two coordinate-plane faces have normals parallel to or , so their flux of the curl is zero. On the inclined face , its upward vector area is , with , . Thus the direct surface integral is
This surface induces the counterclockwise boundary viewed from above, where and . At , . On , take , giving integral . On , take , giving . On , and the integral vanishes. Therefore
Both sides have been calculated directly, verifying the Stokes theorem with consistent orientations.

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