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In EDS spectroscopy, x-ray energies are used to identify and quantify the elements present in a sample.

 

An EDS spectrum of the mineral Ilmenite is shown on the right.  The horizontal-axis is X-ray energy (keV), the y-axis is counts.  Because x-rays are ‘characteristic’ of the elements they come from, x-rays emitted from Fe will always have the same energy (and wavelength), and fall at the same position in the spectrum, etc.  X-rays from all the elements present in the sample appear to be counted simultaneously.

X-rays are a part of the electromagnetic spectrum and as such have the properties of waves, and of particles of energy.  These two characteristics of the electromagnetic spectrum are inversely related via this simple expression:

E = 12.4 / λ 

where

    E = energy (keV)

    λ = wavelength (A)

An albite spectrum is shown at the right.  While these spectra were collected with a 100 seconds counting time, mineral identification requires only a few seconds of counting time.  In general, x-ray lines for all the elements with concentration greater then about 2000 ppm can be seen in an EDS spectrum

In addition to the rather high detection limit of about 2000 ppm, EDS suffers from having poor spectral resolution; meaning x-ray lines from different elements may not be resolvable if their energies are similar.  For example, Sr overlaps Si and Ba overlaps Ti.  WDS has much better spectral resolution.  EDS though, is much faster.

Other Mineral Examples Shown Below

EDS spectrum of anorthite

Si

Ca

Al

Anorthite

EDS spectrum of olivine.

Mg

Si

Fe

Olivine

EDS spectrum of orthopyroxene

Mg

Si

Ca

Fe

Orthopyroxene

Ti

EDS spectrum of clinopyroxene

Mg

Si

Ca

Fe

Clinopyroxene

EDS spectrum of albite

Al

Na

Si

EDS spectrum of ilmenite

Mg

Ti

Fe

EDS

(Energy Dispersive Spectroscopy)

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