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Analysis

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Analysis

Qualitative Analysis

In simplest terms, qualitative analysis involves the determination of what elements are present in the portion of the sample irradiated by the electron beam. This is accomplished by resolving and identifying the (elements giving rise to) fluorescent characteristic x-rays emitted from the sample. Qualitative analysis has three principal applications: phase identification, identification of elements present for quantitative analysis, and determining proper background offsets for quantitative analysis by WDS. Phase identification is by far the dominant use of qualitative methods, and is an especially valuable tool for characterizing complex, fine-grained materials. This is demonstrated in the following example.

Metallic meteorite

This sample in the image at the left was suspected of being a metallic meteorite, for which the metallic phase characteristically should be an Fe-Ni alloy. This backscattered electron image shows morphologies consistent with quenching (very rapid cooling) of molten material rather than the repetitive exsolution textures (Widmanstätten patterns) that are characteristic of (hexahedral) Ni-Fe meteorites. Qualitative analysis by EDXA shows the individual components to be: (1) Pb-Cu-Sballoys; (2) Fe-As alloy; (3) Fe metal; and (4) Fe-sulfide. Hence, the textures and compositions of the component phases identify this material as more likely being a metallurgical slag than a metallic Ni-Fe meteorite.

Methods and Analysis Time

As in quantitative analysis, there are two techniques for the qualitative resolution of fluorescent x-rays: Energy-Dispersive X-ray Analysis (EDXA) and Wavelength-Dispersive Spectrometry (WDS) (for more information on these methods, see the "Analyzer" section of What is an electron microprobe?).

EDXA is the more commonly used method for simple phase identification, because it is extremely rapid: an entire x-ray spectrum of an unknown can be acquired and displayed in a matter of seconds. Because the relative intensities of x-ray lines displayed in the spectrum are proportional to the abundances of elements in the sample (especially for x-rays arising from similar types of electron transitions), EDXA spectra allow users to estimate the chemical stoichiometry of the sampled compound. This application can be enhanced by semi-quantitative approaches involving rapid standardless analytical methods, which take only a few additional seconds and can provide a reasonable estimate of elemental weight fractions, oxide weight fractions, or atomic proportions. EDXA is especially useful on rough samples, because the detection of x-rays is not as dependent on beam-sample-detector geometry as is the WDS method. Therefore, EDXA can be used very effectively with electron imaging methods to characterize loose grains or unpolished materials. The principal limitation of EDXA as a qualitative tool lies in detecting elements present at trace levels, which produce weak intensities that are commonly very difficult to resolve from the background x-radiation (the "Bremmstrählung", which is white x-radiation produced by the deceleration of electrons of the primary beam).

Qualitative analysis by WDS involves scanning one or more spectrometers along a specified geometric interval, to record the intensities of all x-ray wavelengths reaching the detector. By specifying the range of spectrometer movement(s) and the diffraction element(s) (with particular interplanar spacing), the analyst can accumulate either a complete record of the x-ray spectrum or concentrate on wavelength regions for specified elements. Although a bit more time consuming than EDXA, rapid scans of the spectrometers can acquire a complete x-ray spectrum in about 1 minute. The principal advantages of qualitative analysis by WDS are superior resolution of x-ray lines and higher peak/background intensity ratios compared to EDXA. In conjunction with options for extended counting times and controlling the wavelength regions scanned, these advantages are particularly important in identifying the presence of elements at trace to minor level abundance.

Quantitative Analysis

Analytical Methods and Software

Quantitative analysis can be performed by wavelength-dispersive spectrometry, energy-dispersive analysis, or a combination of both. Most quantitative work is performed via the WDS. The software package controlling microprobe automation is the Probe for EMPA, which was developed by John Donovan. This is an extremely versatile group of programs supporting both individual point (manual mode) analysis or automated analysis of stored point locations for unattended operation. Among many features, this package supports: (a) full asynchronous control of all five WDS; (b) x-ray intensity acquisition modes including simple intensity above mean background and integration of x-ray band areas; (c) background acquisition methods including 2 point, 1 point & slope, or none, with linear or curved background shape models; (d) the use of multiple beam conditions (up to one for each different element); (e) automatic or user-selected order of analysis on each spectrometer; and (f) analysis of up to 40 elements. To this basic package, the Probe for EPMA by John Donovan package provides complete integration of EDXA automation with standard WDS microprobe function and matrix correction procedures.

Elements of interest are usually treated as analytical unknowns, but elements present and not analyzed for can be determined by stoichiometry or difference. If known, the concentrations of any given element(s) can be entered manually, to permit inclusion in the matrix correction calculations. Data reduction methods include PAP and XPP (modified f (r z)) methods, and a ZAF algorithm. Mass absorption coefficients from Heinrich (1986), except for those of the light elements which are from Pouchou and Bastin. Element valences and compound formula stoichiometry can be changed on a point-by-point basis during manual analysis, or after automated analysis can be changed and the results recalculated for all or selected groups of points off-line. For geologists, the software permits the assignment of mineral groups for any chosen point or group(s) of points during manual or automated analysis, permitting analysis and formula calculations (both cations and end-member abundance for many solid solutions) for many different mineral groups with a single analytical file.

Why Use Wavelength Dispersive Spectrometry (WDS)?

Both WDS and EDXA (Energy Dispersive X-ray Analysis) can be used to detect x-rays for analysis, but WDS has superior resolving power for x-ray lines, and yields larger signal/noise ratios. The superior resolution of WDS is demonstrated by comparing EDXA and WDS spectra acquired from benitoite (BaTiSi3O9) in the region of Ba and Ti x-ray emission. The Ti Ka and Ba La 1 peaks show complete overlap by EDXA (left), but are well resolved by WDS (right). Thus, the superior resolution of the WDS makes analysis of element pairs with overlapping emission lines (e.g., Ti & Ba or Ti & V) much more accurate, and larger signal/noise ratios improve minimum levels of detection for minor and trace elements.

Analytical Capabilities

Available diffraction devices in our five WDS permit analysis of elements with Z >= 5 (boron), producing common minimum detection limits (MDL) in the 100-200 ppmrange (elemental basis) using counting times of 30-60 seconds on peak.

Some of the analytical capabilities of the system are demonstrated by the analytical result below from the analysis of a tourmaline group mineral [(Na,Ca)0-1(Fe,Mg,Mn,Al,Li)3Al6(BO3)3Si6O18(O,OH,F)4]. By constraining all of the elements with Z >= 5 in a material, light element components (such as Li, Be, or, in the case below, H2O in the formula) can be deduced with reasonable accuracy by the difference of analytical totals from 100%.

Point

15:

( -13186,-23943, -54),

3 iterations------------BRTUR1-5

Element

Wt%

At%

Ix/Istd

Kratio

Z.A.F. coefficients

Ox%

Cat#

B

3.06

5.59

0.8501

0.0026

0.9304

13.9802

1.0000

9.84

2.77

O

47.68

58.81

 

 

 

 

 

0.00

0.00

F

0.91

0.95

0.0869

0.0021

1.0266

4.2989

1.0001

0.91

0.47

Na

0.70

0.60

0.0780

0.0029

1.0506

2.3362

0.9991

0.95

0.30

Mg

8.75

7.10

0.2968

0.0600

1.0336

1.4201

0.9960

14.52

3.54

Al

15.23

11.14

0.7453

0.0907

1.0687

1.5792

1.0028

28.77

5.54

Si

17.36

12.20

0.4892

0.1781

1.0427

1.0601

0.9997

37.13

6.06

K

0.01

0.01

0.0008

0.0001

1.1135

1.0998

0.9948

0.01

0.00

Ca

2.83

1.39

0.2256

0.0248

1.1034

1.0343

0.9993

3.96

0.69

Ti

0.51

2.10

0.0207

0.0041

1.2187

1.0151

0.9996

0.85

0.10

Mn

0.02

0.01

0.0007

0.0002

1.2627

1.0000

1.0030

0.03

0.00

Fe

0.29

0.10

0.0120

0.0024

1.2460

0.9976

1.0003

0.38

0.05

Sum

97.35

100.00

 

 

 

 

 

97.35

19.52

Standard Materials

Our inventory of standards includes over 300 well-characterized reference materials, for intensity calibrations on most of the elements from B (z = 5) to U (z = 92). These include a large suite of natural and synthetic minerals (silicates, oxides, carbonates, sulfides, phosphates, halides), natural and synthetic glasses, pure elements (metals), element oxides, and metal alloys.

Limits of Detection, Accuracy, and Analysis Time

For most elements with z > 9, minimum detection limits (MDL, at 3-s above mean background) down to 50 ppm on an elemental basis are common, and can be lowered by almost an order of magnitude for many trace components. The MDL are commonly higher for the ultralight elements, with values of 500-1000 ppm common for B (z = 5). Analytical accuracy for major and minor components, determined from counting statistics, is often as low as 0.1% relative to the element concentration. Inverse relationships between analysis time and MDL or accuracy should be noted, such that decreased MDL and increased accuracy are accomplished by the use of longer counting times. Consider that for most elements analyzed using Ka x-ray lines, elemental MDL in the 50-100 ppm range require on the order of 30-60 seconds counting on peak (and an equal time on background). Thus, an analytical routine comprised of 15 elements can commonly be achieved in 3-5 minutes with MDL in this range.

Interference Corrections

Even with the resolving power of the WDS, there still are cases where x-ray line overlap cannot be avoided. To alleviate these uncommon problems, the Probe for EMPA analytical software contains methods for correcting interferences based upon calibration from standard materials.

Interference among first order x-ray lines is more common between pairs of elements with moderate to heavy atomic numbers (Z ³ 12) such as Ti & V or Ti & Ba. The following example shows how the overlap of Ti Kb on V Ka leads to a false V2O5 content of 1.92 wt.% in the analysis of titanite (CaTiSiO5). Correction for this interference removes the fictive V as well as improving the results of other major components by providing correct intensities used in the matrix calculations.

OxideWithout CorrectionWith CorrectionStandard Value
SiO230.6530.6530.65
CaO30.5628.6528.6
TiO240.8540.6240.75
V2O51.9200
Total103.9899.92100

Interference among higher order x-ray lines is especially important for analyzing light elements. Shown below is the effect of correction for third order P Ka on F Ka in an REE-bearing apatite, Ca5(PO4)3(OH,F), which is both a non-biologic mineral and the principal hard component of vertebrate teeth and bone. Lack of correction results in fictive F contents that are greater than the possible stoichiometric occupancy of F in the mineral formula (which is about 3.73 wt.% F).

Oxide/anionWithout CorrectionWith CorrectionStandard Value
CaO54.1954.1454.02
P2O540.8240.8640.88
F5.293.683.53
O=F-2.23-1.55-1.48
Total98.0797.1396.95

Data Manipulation and Output

The Probe for EMPA automation system provides for very flexible treatment of analytical data. From any stored analytical file, the user can select any or all information (raw x-ray intensities, intensities relative to standards, K-ratios, element concentrations, oxide concentrations, atomic proportions, cations, etc.) for output either to hardcopy or text file (pre-formatted for Microsoft Excel). Moreover, the system permits the importation of a new standard (including insertion of a new element and intensity acquisition for points already analyzed), change of valence or formula stoichiometry, and off-line recalculation of analytical results for all or selected points within the file. Additional subroutines exist for sorting the data, in which selected points can be grouped and averaged with user-selectable levels of confidence (sigma) for statistics; the sorted groups of points can be output to hardcopy, Excel-compatible text file, or a new Probe for EMPA analytical file.