Area under the curve using polar coordinates - help

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Discussion Overview

The discussion revolves around the integration of areas using polar coordinates, particularly focusing on the interpretation of negative areas and the behavior of the differential element dθ. Participants explore the relationship between polar coordinates and Cartesian coordinates, questioning how negative values affect area calculations in polar integration.

Discussion Character

  • Exploratory
  • Technical explanation
  • Debate/contested
  • Mathematical reasoning

Main Points Raised

  • One participant explains that in Cartesian coordinates, areas below the x-axis are negative, while areas above are positive, and questions how this translates to polar coordinates.
  • Another participant describes a scenario of integrating around a circle, suggesting that the direction of integration (anticlockwise) affects the sign of dθ, leading to a subtraction of areas on the return path.
  • A participant expresses confusion about how dθ can be negative, questioning if it is related to the direction of integration and seeking clarification on this concept.
  • One participant reiterates their confusion about the negative nature of dθ and its implications for area calculations in polar coordinates.
  • Another participant introduces the concept of surface integrals and the Jacobian determinant, discussing how area elements in polar coordinates can be interpreted as small rectangles.
  • A later reply distinguishes between simple integrals and polar coordinate integrals, suggesting that they can compute areas under curves in different forms, but they may not be directly comparable.

Areas of Agreement / Disagreement

Participants express varying levels of understanding regarding the implications of negative values in polar integration, with some agreeing on the directional influence on dθ while others remain uncertain. The discussion does not reach a consensus on how to interpret these concepts fully.

Contextual Notes

Participants highlight potential confusion regarding the definitions and interpretations of dθ and its relationship to area calculations in polar coordinates. There are unresolved questions about how these concepts relate to traditional Cartesian integration.

fleazo
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Hi, I have a pretty simple question but I'm not certain I know how to phrase it properly. I will try.


When we are integrating using cartesian coordinates to find the area under a curve, area under the x-axis is negative and area above the x-axis is positive. This makes sense when I think of the integral in terms of reimann sums because because we are just summing areas of rectangles using the formula f(t)*(t-a) for some t in the interval we're integrating over. If we have an f(t) under the x axis, that means f(t) is negative, and since dx is "positive", we would get a negative number for the area of the rectangle.


But when thinking of polar coordinates I'm confused. In polar coordinates, θ is like our "x" and r is like our "y". So it seems the analogue to this situation would be when r is negative. But when thinking of this in terms of reimann sums, that doesn't seem like the case. Since the area of a sector of a circle is (1/2)r2θ, if r is negative it just becomes positive when we square it. So the only thing that would make this amount negative is if θ is negative. in the integral, dθ takes the place of θ in this equation. Does dθ ever become "negative"? Do we have to worry about negative area when dealing with integrating using polar coordinates?
 
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Imagine integrating around a circle that does not touch or contain the origin to find its area. Suppose you go anticlockwise around it. On the section that's further from the origin, dθ is positive, and it gives you not just the area of the circle but also the area of the triangle it subtends at the origin; on the return section, it is negative, and subtracts the extra area to leave you with just the area of the circle.
 
wow thank you, that makes perfect sense!


I have one doubt though. How is it that dθ is negative? When I think of dθ, I think of it like a metric, like it's measuring the distance between two points and that it's always positive. So I'm not quite grasping what it is that makes dθ negative. Is it because we are going anti clockwise? If so, why is it that the direction we go has an impact on the sign of dθ?


Thanks again for your explanation
 
fleazo said:
When we are integrating using cartesian coordinates to find the area under a curve, area under the x-axis is negative and area above the x-axis is positive. This makes sense when I think of the integral in terms of reimann sums because because we are just summing areas of rectangles using the formula f(t)*(t-a) for some t in the interval we're integrating over. If we have an f(t) under the x axis, that means f(t) is negative, and since dx is "positive", we would get a negative number for the area of the rectangle.


But when thinking of polar coordinates I'm confused. In polar coordinates, θ is like our "x" and r is like our "y". So it seems the analogue to this situation would be when r is negative. But when thinking of this in terms of reimann sums, that doesn't seem like the case. Since the area of a sector of a circle is (1/2)r2θ, if r is negative it just becomes positive when we square it. So the only thing that would make this amount negative is if θ is negative. in the integral, dθ takes the place of θ in this equation. Does dθ ever become "negative"? Do we have to worry about negative area when dealing with integrating using polar coordinates?
Can you give an example where you would use polars to evaluate the area under a graph?

I generally only use it to evaluate an area within some sort of boundary.
 
Sorry, it was bad wording on my part. That's what i meant, was the interior of say a circle, or a cardioid or something like that.
 
fleazo said:
How is it that dθ is negative?
Remember that θ is an angle measured at the origin. On the 'return' part, although you are still going anticlockwise around the circle, θ is decreasing.
 
You can also think of it in terms of a surface integral. dA=dxdy=rdrdθ. This is calculated through the determinant of the Jacobian. Now, if dxdy is a small rectangle what is rdrdθ?

Well, rdθ is an arc length, therefore you have small convex rectangles. However, because both dr and dθ are infinitesimal in size, you can consider that dθ(r) ~ dθ(r+dr), therefore they degenerate to normal rectangles like in the cartesian case.
 
I think you are mixing together a number of different things.

When you think of an integral in terms of "area under the curve", you think of a "simple" integral (of f(x) on an interval). When you think of polar coordinates, you think either about a contour integral or a planar double integral.

They have somewhat different forms, but all of them can be used to compute "area under the curve", in which case one form can always be transformed into another.
 

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