Triple integral in spherical coordinates.

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Discussion Overview

The discussion revolves around the use of spherical coordinates in triple integrals, specifically addressing the limits of integration for the angles involved in the volume calculation of a sphere. Participants explore the implications of allowing the angle φ (phi) to range from 0 to 360 degrees, contrasting it with the standard practice of limiting φ to 0 to 180 degrees.

Discussion Character

  • Exploratory, Technical explanation, Debate/contested

Main Points Raised

  • One participant questions the conventional limits of integration for φ in spherical coordinates, suggesting that it could be allowed to run from 0 to 360 degrees.
  • Another participant draws an analogy to Earth's latitude and longitude, explaining that latitude traditionally runs from 90 degrees north to 90 degrees south (180 degrees), while longitude runs 0 to 360 degrees, highlighting potential issues with multiple coordinates for the same point if latitude were allowed to run 360 degrees.
  • A later reply clarifies that allowing φ to exceed 180 degrees would lead to negative values for the projection lengths in the volume element, thus altering the standard volume calculation.
  • Participants discuss the necessity of adjusting the volume element if φ is allowed to exceed 180 degrees, suggesting the use of the absolute value of sin φ to maintain correct volume representation.
  • Several participants express interest in introductory books on calculus and vector calculus, with recommendations provided for specific texts that cover these topics in depth.

Areas of Agreement / Disagreement

Participants do not reach a consensus on the appropriateness of allowing φ to run from 0 to 360 degrees, with some arguing against it due to the implications for the volume element, while others propose it as a valid alternative.

Contextual Notes

The discussion includes assumptions about the geometric interpretation of spherical coordinates and the implications of changing the limits of integration, which remain unresolved. The mathematical steps involved in deriving the volume element are not fully detailed.

Who May Find This Useful

This discussion may be of interest to students and educators in mathematics and physics, particularly those exploring integration techniques in spherical coordinates and the implications of coordinate transformations.

Mohankpvk
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While deriving the volume of sphere formula, I noticed that almost everyone substitute the limits 0 to 360 for the angle (theta) i.e the angle between the positive x-axis and the projection of the radius on the xy plane.Why not 0to 360 for the angle fi (angle between the positive z axis and radius)?
I tried it, but I got 0 as answer.Please explain this.
 
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Think about the Earth using latitude and longitude. Latitude runs from 90 degrees north latitude (the North Pole) to 90 degrees south. So that's 180 degrees. Longitude runs from 0 to 180 East longitude and then from 180 West longitude back to 0. So that's 360 degrees.

If you let latitude run a full 360 degrees, then points on Earth would have multiple coordinates: The point that is 270 degrees south of the North Pole and longitude 0 is the same as the point that is only 90 degrees south of the North Pole and longitude 180.
 
stevendaryl said:
Think about the Earth using latitude and longitude. Latitude runs from 90 degrees north latitude (the North Pole) to 90 degrees south. So that's 180 degrees. Longitude runs from 0 to 180 East longitude and then from 180 West longitude back to 0. So that's 360 degrees.

If you let latitude run a full 360 degrees, then points on Earth would have multiple coordinates: The point that is 270 degrees south of the North Pole and longitude 0 is the same as the point that is only 90 degrees south of the North Pole and longitude 180.
Iam not suggesting to make both latitude and longitude 360.My question is,
why shouldn't we let latitude run 360 and make longitude 180?
Just inverting the system.
 
Mohankpvk said:
Iam not suggesting to make both latitude and longitude 360.My question is,
why shouldn't we let latitude run 360 and make longitude 180?
Just inverting the system.
There is no problem doing that. However, the volume element is then different: you can calculate it using classical geometry or using the Jacobian of your new coordinate system. If you integrate the old volume element using your new coordinate system, what you are integrating will no longer represent volume.
In particular, recall that the ##r\sin \phi ## factor of the volume element ##r^2 \sin\phi \, dr\, d\theta\, d\phi ## comes about geometrically from the length of the projection of the radial position vector of each point onto the xy-plane in order to get the sweeping radii for the lengths of arc ##d\theta ## and ##d\phi ##. If you are now allowing ##\phi ## to have values above 180°, then ##r\sin \phi ## will be a negative number when ##180^{\circ} < \phi < 360^{\circ}##. We do not want those projection lengths to be negative, so that is not the standard volume element anymore.
To get the correct standard volume, you can use the factor ##r|\sin \phi |## instead, which would result in a volume element of ##r^2 |\sin\phi | \, dr\, d\theta\, d\phi ##. However, I think you can see that this is a bit unwieldy.
 
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slider142 said:
There is no problem doing that. However, the volume element is then different: you can calculate it using classical geometry or using the Jacobian of your new coordinate system. If you integrate the old volume element using your new coordinate system, what you are integrating will no longer represent volume.
In particular, recall that the ##r\sin \phi ## factor of the volume element ##r^2 \sin\phi \, dr\, d\theta\, d\phi ## comes about geometrically from the length of the projection of the radial position vector of each point onto the xy-plane in order to get the sweeping radii for the lengths of arc ##d\theta ## and ##d\phi ##. If you are now allowing ##\phi ## to have values above 180°, then ##r\sin \phi ## will be a negative number when ##180^{\circ} < \phi < 360^{\circ}##. We do not want those projection lengths to be negative, so that is not the standard volume element anymore.
To get the correct standard volume, you can use the factor ##r|\sin \phi |## instead, which would result in a volume element of ##r^2 |\sin\phi | \, dr\, d\theta\, d\phi ##. However, I think you can see that this is a bit unwieldy.
Thank you.Nice answer.
Is there any good(and simple,introductory) books for calculus and vector calculus?
 
Mohankpvk said:
Thank you.Nice answer.
Is there any good(and simple,introductory) books for calculus and vector calculus?
Definitely. I do not know many good free books that go in depth the way that introductory books should, so unfortunately you will have to either pay for these texts or find them at a local library.

The best introductory textbook path I know to calculus and vector calculus is to first go through "Calculus" by Spivak, then study the texts "Vector Calculus, Linear Algebra, and Differential Forms" by Hubbard, "Calculus on Manifolds" by Spivak, "Linear Algebra Done Right" by Axler, and "Linear Algebra Done Wrong" by Treil concurrently.

The first is a nice walkthrough introduction of vector calculus that showcases many applications as well as showing details of vital theorems. The second gives an extremely bird's eye view of vector calculus that takes you from the basic component-based vector approach to the modern exterior calculus coordinate-independent approach with proper proofs and rigor. The latter two books help fill out the rigor in your understanding of linear algebra, as much of vector calculus is concerned with reducing nonlinear problems to questions in linear algebra. Knowing how linear algebra works properly is thus an important skill. Hope this helps you out! :-)
 
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slider142 said:
Definitely. I do not know many good free books that go in depth the way that introductory books should, so unfortunately you will have to either pay for these texts or find them at a local library.

The best introductory textbook path I know to calculus and vector calculus is to first go through "Calculus" by Spivak, then study the texts "Vector Calculus, Linear Algebra, and Differential Forms" by Hubbard, "Calculus on Manifolds" by Spivak, "Linear Algebra Done Right" by Axler, and "Linear Algebra Done Wrong" by Treil concurrently.

The first is a nice walkthrough introduction of vector calculus that showcases many applications as well as showing details of vital theorems. The second gives an extremely bird's eye view of vector calculus that takes you from the basic component-based vector approach to the modern exterior calculus coordinate-independent approach with proper proofs and rigor. The latter two books help fill out the rigor in your understanding of linear algebra, as much of vector calculus is concerned with reducing nonlinear problems to questions in linear algebra. Knowing how linear algebra works properly is thus an important skill. Hope this helps you out! :-)
Thank you
 

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