in 39 countries benefit from artifically fluoridated
water. A further 40 million benefit from water supplies
which are naturally fluoridated. The fluoridation of
toothpastes and public water supplies has been ac-
knowledged as a major public health success in the
prevention of dental caries. The addition of fluoride to
water supplies and to oral health products has helped
to bring about a remarkable decline in dental caries
levels since the 1960s. In this paper the occurrence of
fluoride in nature, the history of the discovery of its
effects on the dentition, its use in the prevention of
dental caries, and the risks associated with ingestion of
excess fluoride will be considered.
Fluoride in Nature
0003 Fluorine is a naturally occurring element, apparently
ubiquitous in nature. Number nine on the periodic
table of the elements, it is a halogen gas. It ranks 13th
among the elements in order of abundance in the
earth’s crust. Fluorine is the most electronegative
and reactive of all elements. It is a pale yellow, corro-
sive gas, which reacts with practically all organic and
inorganic substances. The element was isolated in
1886 by Ferdinand Frederic Henri Moisson who
used an apparatus constructed from platinum. He
won the Nobel Prize for chemistry in 1906. Fluorine
occurs chiefly in fluorspar (or fluorite, calcium
difluoride, CaF
2
), cryolite (Na
2
AlF
6
), and in many
other minerals. Ionic fluoride, also referred to as in-
organic or free fluoride, is the biologically important
form of the mineral.
0004 Fluoride is found in fresh water, sea water, and earth
and in foods. Fluoride is present in both groundwater
and surface water. The level of fluoride in groundwater
varies from less than 0.1 mg l
1
to more than 25 mg l
1
according to the geological, chemical, and physical
characteristics of the water-supplying area. The fluor-
ide concentration in fresh surface water is generally
low, ranging from 0.01 to 0.03 mg l
1
. In sea water,
fluoride is found at approximately 1.5 ppm. Marine
plants and animals are therefore constantly exposed to
large amounts of fluoride. Fluoride in soils is derived
primarily from the geologic parent material. Samples of
nonindustrially contaminated soils from Germany,
Greece, Finland, Japan, Morocco, New Zealand,
Sweden, the USA and former USSR have been reported
as containing from 30 to 500 ppm fluoride. Soils near
fluorite and other types of mineralization may show
levels up to more than 5000 ppm.
0005 The normal accumulation of soil fluoride in plants
is small. However, a few species of plants are known
to accumulate high levels of fluoride, for example tea.
The concentration of fluoride in dried tea leaves
varies widely (approximately 4–400 ppm) while
those of brewed tea range from 1 to 6 ppm depending
on the amount of dry tea used, the fluoride concen-
tration of the water, and the brewing time. High levels
of fluoride are also found in fish: early reported con-
centrations range from 0.6 to 2.7 ppm. These samples
may have contained bones. With its high affinity for
calcium, most absorbed fluoride is deposited in bones
therefore fish bones are a source of concentrated
fluoride levels. More recent studies which excluded
bone fragments from fish reported a range of fluoride
values from 0.05 to 0.17 ppm. Other dietary constitu-
ents which contain fluoride are fluoridated water and
infant formulas and beverages reconstituted with
fluoridated water. Most other foods have fluoride
concentrations well below 0.05 ppm.
History of Water Fluoridation
0006In 1901 a letter in the US Public Health Report from
JM Eager of the US Public Health Service, stationed in
Naples, Italy, reported the occurrence of ‘a dental
pecularity’ known locally as denti di chiae. Denti di
chiae were called after Prof Stefano Chiae, a cele-
brated Neapolitan who first described the appearance
of a condition which was later to become known as
dental fluorosis.
0007A similar condition, known as Colarado brown stain,
was observed in Colorado Springs, USA, in 1901 by a
dentist, Fredrick McKay. The condition manifested itself
as a stain of varying intensity from fine white patches to
a disfiguring brown mottling. Some 87% of the popula-
tion in the area were affected. In 1916, McKay, with the
help of GV Black, a prominent figure in dentistry at the
time, published a thorough description of the condition,
describing its appearance as mottled enamel. By the
1920s McKay had suspected drinking water as the
source of the problem. In Oakley, Idaho, where mottling
was severe, McKay noticed that children living on the
outskirts of town who drank from a private spring had
no mottling. He advised the town to change to this
supply, which they did in 1925. Children born in the
town subsequently had no mottling.
0008In 1931 new methods of spectrographic analysis
led to the discovery of fluoride in the water supplies
of areas where mottled enamel was endemic. The
condition then became known as dental fluorosis.
0009In 1928 McKay published the observation that, in
areas where mottled enamel was found, the preva-
lence of dental caries appeared lower than would be
expected. In 1933 Ainsworth in England showed
that dental mottling in Maldon in Essex was associ-
ated with a high level of fluoride in its water (4.5–5.5
ppm). He also noted that the prevalence of caries in
permanent teeth amongst the children in the area was
lower than that for England and Wales as a whole.
DENTAL DISEASE/Fluoride in the Prevention of Dental Decay 1755