Take a piecewise linear path along three coordinate directions, passing through the origin and then :
On the first segment , so its line integral is zero. On the second , so its contribution is also zero. On the last segment and increases from zero to one. Therefore
This gives the requested concrete path dependence with the same ordered endpoints.
For the second vector field, the curl is
It is nonzero, for example at . A differentiable scalar potential would have zero curl of its gradient, so is not conservative. The fact that its curl vanishes on the line does not make it vanish throughout the domain.
The three components of the curl cancel pairwise:
The domain is all of , which is simply connected, so this is consistent with a conservative vector field. To construct its scalar potential, integrate to obtain . Matching gives , hence . Finally forces . Consequently
Every scalar potential differs by a constant on this connected domain. The endpoint values differ by one, agreeing with the line integral in part (a).
The proposed parametric equation traces precisely the same oriented segment, with a different speed. Set , which increases from zero to one, and . Direct substitution gives the line integrals
Thus both values are unchanged. The derivative of vanishes at the initial endpoint for , but the monotone integration by substitution is still valid. This is invariance under reparametrization of one curve, which applies even to a nonconservative vector field; it is not evidence of general path independence.
Parametrize the segment in its stated direction by , . Then , and substitution into the two vector fields gives
Taking each dot product with evaluates the line integrals:
The new cone can be parametrized by
The outward vector area element is . This is ; reversing the order is needed to retain the outward orientation after the exchange of coordinates. Its dot product with is again . Hence
This equality also follows because a rigid rotation takes the first cone into the second and leaves the radial vector field invariant.
On the sphere of radius , the outward unit normal is . Thus everywhere. Multiplying by the surface area gives
The same surface integral follows in spherical coordinates from .
Compute the flux directly using the outward vector area element, as required. Restrict the vector field to the surface parametric equation and take the dot product:
The terms quadratic in cancel. Therefore the surface integral is
This is a direct evaluation of the flux of the position vector through a cone.
The sloping height relation on the cone is . A parametric equation of its curved surface is therefore
Its two tangent vectors are and . Multiplication by and produces the two infinitesimal sides requested in the paper. Their cross product is the vector area element:
Its radial component is positive, so this normal vector points outwards from the solid cone. Taking its norm gives the scalar area element
The parametric equation degenerates at the apex, but that single point contributes no area.

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