Difference between revisions of "Electric QuadrupoleMoment Forest NuclPhys I"
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because | because | ||
− | <math>\vec{E} = \int \ | + | <math>\vec{E} = \int \rho (\vec{r^'}) \frac{(\vec{r} - \vec{r^'})}{|r - r^'|^3} d^3r^' = - \vec{\nabla} \int \frac{\rho (r^')}{|\vec{r} - \vec{r^'}|}</math> |
\vec{E} = -\vec{\nabla} \Psi (r) | \vec{E} = -\vec{\nabla} \Psi (r) | ||
− | <math>\Psi (r) = \int \frac{\ | + | <math>\Psi (r) = \int \frac{\rho (r^')}{|\vec{r} - \vec{r^'}|}</math> |
[[Forest_NucPhys_I]] | [[Forest_NucPhys_I]] |
Revision as of 04:43, 7 April 2009
Electric Quadrupole Moment of a Nucleus
Pages 104-111
As in the dipole calculation we assume that the object is in a state such that its maximum total angular momentum is along the z-axis.
or
then
From definition of quadrupole moment for a single charged object/particle.
The origin of this comes from electron-statics.
You expand the electric potential in terms of spherical harmonics.
because
\vec{E} = -\vec{\nabla} \Psi (r)