Swapnil said:
T
* If instead of having f(s) and f(s,t) to be unity, you could have easily made them to be some arbitrary functions and then you would have gotten the area between your curve C and your function f(s) and, similarly, the volume between your surface S and your function f(s,t), right?
Okay, the first thing to understand here is that here we are not concerned about dimensionality. In your first post you were asking about something of the form
\int_C f(x) ds.
But here, our curve C is some arbitrary curve. We don't know if it's in \mathbb{R}, \mathbb{R}^2, \mathbb{R}^{15}, or perhaps some arbitrary manifold! All being a "curve" means is that it can be parameterized using only one parameter (ie. if C is in say, \mathbb{R}^3, then there's some parameterization x=f(t), y=g(t), z=h(t) of C, where t is just a real parameter running over some interval I). This is the essential problem with just saying that line, surface and volume integrals mean the area/surface/volume between the function and the region in question (though this idea certainly has some merit if you're careful with it).
Now, the integrand is just some arbitrary function defined on the same space that C is in (at least that's good enough for our purposes here, though not quite general). So again, if C is in, say, \mathbb{R}^3, then in general your integral will look something like
\int_C f(x,y,z)d\vec{s}.
It's important to understand here that d\vec{s} is not really a differential in the way that you usually think about one. Here d\vec{s} is just a convenient way of writing the "arclength element" of C: if C is parameterized in the way I described above (ie. x=f(t), y=g(t), z=h(t), and assuming that C is smooth [read: x, y, z are differentiable fns of t]), then what we mean by d\vec{s} is actually
\sqrt{(f^\prime(t))^2+(g^\prime(t))^2+(h^\prime(t))^2}dt,
or in other words,
|r^\prime(t)|dt = \big|\frac{d}{dt}<x,y,z>\big|dt,
as jbusc indicated. This is the same thing you derived for the arclength formula back in first year calculus.Next is to talk about how you should think about these. Let's go back to what jbusc was looking at. If (in the situation above), we have f(x,y,z) identically equal to unity, then our integral is
\int_C f(x,y,z)d\vec{s} = \int_C d\vec{s}.
Given what I just explained about d\vec{s}, it should be pretty clear to you that this is just the
arclength of the curve C.
So if f(x,y,z) is arbitrary, what happens? Well, the best way to think about it in my opinion is as a weighting function. If f(x,y,z)=1, then each infinitesimal arclength segment of C is valued equally in the integral and since d\vec{s} is just the arclength element for C, you just get back the arclength when you take the sum. On the other hand, if f(x,y,z) is some nonconstant function, then you are assigning different "weights" to different parts of C.
Surface and volume integrals (and you can go further than that of course, to integrating over arbitrary 4-d hypersurfaces and so on) are basically just higher-dimensional analogs to that. The idea of the integrand as a "weighting function" works for them too.