Integral of a normal distribution

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SUMMARY

The integral of the normal distribution, specifically ∫ e^(-x²) dx from -∞ to +∞, can be evaluated using polar coordinates. By transforming the integral into double integral form, ∫∫ e^(-x² - y²) dx dy, and applying the Jacobian determinant, the correct boundaries for the polar coordinates are established as r from 0 to ∞ and θ from 0 to 2π. Attempting to set r from -∞ to +∞ and θ from 0 to π results in an incorrect answer of zero due to the properties of the Jacobian and the nature of the polar coordinate transformation.

PREREQUISITES
  • Understanding of integral calculus and double integrals
  • Familiarity with polar coordinates and their applications in integration
  • Knowledge of the Jacobian determinant in coordinate transformations
  • Experience with the properties of the normal distribution
NEXT STEPS
  • Study the derivation of the Gaussian integral using polar coordinates
  • Learn about the Jacobian determinant and its role in coordinate transformations
  • Explore advanced integration techniques involving double integrals
  • Investigate the properties of the normal distribution and its applications in statistics
USEFUL FOR

Students and professionals in mathematics, particularly those studying calculus, statistics, or any field requiring a deep understanding of integrals and the normal distribution.

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Homework Statement


(Scroll to bottom for the true question)

Suppose we are to find the integral from -∞ to +∞ of (let’s just say) e-x2dx

Homework Equations


∫∫f(x)g(y)dxdy = (∫f(x)dx)(∫g(y)dy)

The Attempt at a Solution


We can square the integral we want to solve for then use my relevant equation (in reverse) to write the answer to the integral as the square root of this double integral:
∫∫e-(x2+y2)dxdy

Where the x and y boundaries are ±∞

Now we transform into polar coordinates so that the integral becomes:

∫∫e-r2(rdrdθ)

Now we could make the (inner) r integral run from 0 to ∞ and the (outer) θ integral run from 0 to 2π (since these boundaries cover the whole plane) which would give the famous answer.Now my question is about the boundaries of the polar integral... why can’t we have made r run from -∞ to +∞ and θ run from 0 to π? This also seems to cover the plane, but doing this gives an answer of zero. What is the reason this is wrong?

Thanks.

Well actually I just realized the “r” in rdrdθ comes from the absolute value of the ”Jacobian determinant” so it should actually be |r| dr dθ which does give the correct answer.

I’m going to post this anyway since I already typed it out. Maybe someone has more insight to share.
 
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