The Avogadro constant, NA, is a fundamental physical
constant that relates any quantity at the atomic scale to its
corresponding macroscopic scale. Inspired by the kinetic gas
theory Avogadro proposed his hypothesis in 1811, in order to
describe chemical reactions as an atomic process between atoms
or molecules. Starting from his pioneering findings, the
determination of this large number has fascinated generations of
scientists up to this day. The review of methods aimed at
finding a value for NA starts with the calculations made
by Loschmidt (1865; NA ≈72×1023 mol-1) who evaluated the number of molecules in a given gas
volume, derived from estimates of molecular diameters and the
mean free path length. Consideration of Brownian motion led to
some more accurate determinations of NA around the
beginning of the 20th century (Perrin (1908); NA≈6.7×1023 mol-1). Other methods
developed in the following years are based on Millikan's oil
drop experiment (1917, NA≈6.064(6)×1023 mol-1), on the counting of alpha particles emitted from
radium or uranium (Rutherford (1909); NA≈6.16×1023 mol-1) and on investigations of molecular
monolayers on liquids (Nuoy (1924); NA≈6.004×1023 mol-1).
A modern method to derive NA from the density, the relative
atomic mass, and the unit cell length was introduced by Bragg
in 1913. It makes use of the diffraction of x-rays by the
interatomic spacings of a crystal lattice and its periodic
arrangement. The accuracy of this method is extremely affected
by the fact that the lattice scale of the structurally imperfect
lattice can be calibrated only approximately in SI units. Data
of NA were, therefore, found to be in disagreement with
other fundamental constants (Bearden (1931); NA≈6.019(3)×1023 mol-1). A break though was achieved
with perfect crystals of silicon and x-ray interferometry
making available very precise data of atomic distances,
expressed in SI units (Bonse and Hart 1965).
Today, metrology has re-discovered the Avogadro constant and
uses it as one of several possible routes to a re-definition of
the kilogram because the old platinum iridium artefact exhibits
long-term stability problems. This application of the Avogadro
constant presupposes a final measurement uncertainty of about
1×10-8, a challenge for the experimental
determination of the quantities involved, i.e. macroscopic
density, isotopic composition, and unit cell volume of a
silicon crystal. Many years of research work were centred on
the problem of how far the perfection of a real crystal is away
from the ideal state. At present, it is widely accepted that,
in the limits of the desired uncertainty, the lattice parameter,
and thus the unit cell volume of silicon, can be seen as an
invariant quantity when the influence of residual defects, for example
impurities, is taken into account. Up to a relative measurement
uncertainty of a few parts in 107 it has recently been
shown that the molar volume, the ratio of molar mass to
density, is constant, too. The combination of data from several
independent measurements of the unit cell and the molar volumes
has led to a value for the Avogadro constant of
NA = 6.022 1335(30)×1023 mol-1 (De Bièvre et al 2001)
recommended by the national metrology institutes involved in
this research project (Becker 2001).
Prominent examples of the significance of the research work
reviewed here are the use of NA as an input independent of
other data, for the adjustment of a consistent set of
fundamental constants, and the accompanying outstanding
experimental developments acting as spin-offs in the field of
technology to make macroscopic dimensions traceable to the
atomic scale.