Добавил:
Опубликованный материал нарушает ваши авторские права? Сообщите нам.
Вуз: Предмет: Файл:
Joseph I. Goldstein, Dale E. Newbury [et al.]. Scanning Electron Microscopy and X-Ray Microanalysis. (2017). (ISBN 978-1-4939-6674-5). (ISBN 978-1-4939-6676-9). (DOI 10.1007978-1-4939-6676-9).pdf
Скачиваний:
20
Добавлен:
11.04.2023
Размер:
68.34 Mб
Скачать

\294 Chapter 19 · Quantitative Analysis: From k-ratio to Composition

19.8\ Ways of Reporting Composition

19.8.1\ Mass Fraction

The most common way to report the composition of a material is in terms of the mass fraction. To understand the mass fraction, consider a block of material containing a mixture of different atoms. Weigh the block. Now imagine separating the block into distinct piles, each pile containing all the atoms from one element in the block. Weigh each of the separated piles. The mass fraction is calculated as the ratio of the mass of pile containing element Z over the total mass of the block. Since each element in the block is represented by a pile and since none of the atoms are lost in the process of dividing the block, the sum of mass fractions equals unity. Of course, we can’t really do this measurement this way for most materials but conceptually we can understand mass fraction as though we can. As a simple example, consider the mineral pyrite, FeS2. The molecular formula combines one gram-mole of Fe (atomic weight A =55.85 g/mole) with two gram moles of S (A =32.07 g/ mole) for a compound molecular weight of 119.99 g/mole. The mass fractions, Cw, of the constituents are thus

Cw,Fe

=55.85 / 119.99 =0.4655

\

(19.8a)

Cw,S

=64.14 / 119.99 = 0.5345

\

(19.8b)

The mass fraction is the fundamental output of electron probe X-ray microanalysis measurements. All other output modes are calculated from the mass fraction.

Weight fraction, mass percent, weight percent are all commonly seen synonyms for mass fractions. Mass fraction or mass percent is the preferred nomenclature because it is independent of local gravity.

19.8.2\ Atomic Fraction

If we perform the same mental experiment as was described in the mass fraction section, but instead of weighing the piles, we instead count the number of atoms in the block and each of the piles. If we then calculate the ratio of the number of atoms of element Z relative to the total number of atoms in

19 the block, this is the atomic fraction, Ca. For the example of FeS2, which contains a total of three atoms in the molecular formula, the atomic fractions are

Ca,Fe

=1 / 3=0.3333

\

(19.9a)

Ca,S

=2 / 3= 0.6667

\

(19.9b)

We can calculate atomic fraction Ca from mass fraction Cw and vice versa using the atomic weights A of the elements.

Ca,i = (Cw,i / Ai )

N

 

Σ(Cw,i / Ai )

(19.10)

 

1

\

 

 

Where N is the number of elements involved in the mixture.

Starting with the atomic fractions, the mass fractions are calculated according to the formula

Cw,i = (Ca,i Ai )

N

Ai )

 

Σ(Ca,i

(19.11)

 

1

 

\

 

 

 

It is appropriate to use the atomic weights as suggested by

the IUPAC (7http://www.ciaaw.org/atomic_weights4.htm). These weights are based on assumed mixes of isotopes as are typically seen in terrestrial samples. Occasionally, when it is known that an element is present in a perturbed isotopic mix, it may be appropriate to use this information to calculate a more accurate atomic weight. Since the atomic fraction depends upon assumed atomic weights, the atomic fraction is less fundamental than the mass fraction.

19.8.3\ Stoichiometry

Stoichiometry is closely related to atomic fraction. Many materials can be described simply in terms of the chemical formula of its most basic constituent unit. For example, silicon and oxygen combine to form a material in which the most basic repeating element consists of SiO2. Stoichiometry can be readily translated into atomic fraction. Since our measurements are imprecise, the stoichiometry rarely works out in clean integral units. However, the measurement is often precise enough to distinguish between two or more valence states.

19.8.4\ Oxide Fractions

Oxide fractions are closely related to stoichiometry. When a material such as a natural mineral is a mixture of oxides, it can make sense to report the composition as a linear sum of the oxide constituents by mass fraction.

.Table 19.1 shows the analysis of NIST SRM470 (K412 glass) with the results reported as oxide fraction, mass fraction, and atomic fraction.

Example Calculations

Calculating the mass fraction from the oxide fraction for Al in K412 glass:

Cw,Al

=

 

2

×26.9815

0.0927

= 0.04906

(19.12)

2

×26.9815 + 3×15.999

 

 

 

 

\

 

 

 

 

 

 

 

Calculating the atomic fraction from the mass fraction:

 

 

 

 

 

0.0491

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

Ca,Al

=

 

 

 

26.9815

 

 

 

 

 

 

0.1166

+

0.0491

+

0.2120

+

0.1090

+

0.0774

+

0.4275

 

 

 

24.305

 

26.9815

28.085

40.078

55.845

15.999

 

\

 

 

 

 

 

 

 

 

 

 

 

 

(19.13)