J. J. Thomson's discovery of the negatively charged corpuscle in 1897
is customarily regarded as the discovery of the electron. Thomson, how
ever, did not immediately equate the charge of his corpuscle with the
unitary charge, that is the 'electron', first proposed by Stoney in 18
74. The aim of this paper is to clarify the means by which this identi
fication was eventually made. To do this the work carried out by Thoms
on and his students at the Cavendish Laboratory between 1897 and 1899
has been examined. From this reconstruction it emerges that, following
his work on the mass-to-charge ratio of the corpuscle in 1897, Thomso
n and his school initiated and developed a series of techniques for me
asuring the charge of the ions. These techniques could not be used dir
ectly to measure the charge of the corpuscles because of the condition
s required to produce them. Thomson therefore sought some other phenom
enon that could be interpreted in terms of corpuscles and which allowe
d exploitation of the new charge-measuring techniques. He found such a
phenomenon in the photoelectric effect, which allowed the measurement
of both the charge and the mass-to-charge ratio of the corpuscle to b
e made. These measurements showed the charge of the corpuscle to be cl
ose to that assigned to the 'electron', and the two entities gradually
became equated with each other.