Difference between revisions of "Surface Resolution"

Revision as of 01:29, 11 April 2007

Surface Resolution Approximation

An important part of topological interferometry is that the surface be retained in the reflected image. Plane wave solutions are most effective when the surface gradually curves and no sharp peaks are present.

Surface Schematic

${\boldsymbol {E}}={\boldsymbol {E_{0}}}e^{i\left({\boldsymbol {k\cdot x}}-\omega t\right)}$

Revision as of 01:27, 11 April 2007 (view source) DemasMa (talk \| contribs) (→‎Surface Resolution Approximation) ← Older edit		Revision as of 01:29, 11 April 2007 (view source) DemasMa (talk \| contribs) (→‎Surface Resolution Approximation) Newer edit →
Line 5:		Line 5:
	[[Image:ResDiagram1.jpg\|thumb\|Surface Schematic]]		[[Image:ResDiagram1.jpg\|thumb\|Surface Schematic]]

−	<math>\boldsymbol{E} = \boldsymbol{E_0} e^{i \boldsymbol{k \cdot x} - \omega t}</math>	+	<math>\boldsymbol{E} = \boldsymbol{E_0} e^{i \left( \boldsymbol{k \cdot x} - \omega t \right)}</math>

Difference between revisions of "Surface Resolution"

Revision as of 01:29, 11 April 2007

Surface Resolution Approximation

Navigation menu

Search