With the aim of determining the contribution of water to the backgroun
d of natural radiation in Spain, the Rn-222 concentration levels were
measured in domestic drinking water from a large part of the country,
The water analyzed, both surface and groundwater, was collected in two
areas of very distinct geological characteristics, pre-selected for t
he likelihood of their containing high levels of 222Rn. This water was
measured using a coaxial detector of high purity Ge, The overall resu
lts demonstrate a log-normal distribution of Rn-222 levels, with a geo
metric and arithmetic means of 10 and 381 Bq L(-1), respectively, and
a range between detection limit of 2 Bq L(-1) and a maximum of 31,000
Bq L(-1). The Rn-222 concentrations measured in surface mater are gene
rally below the detection limit, Significant differences have been fou
nd depending on the geological characteristics of the area of referenc
e, although the very distinct concentration levels of Rn-222 found in
samples of similar lithology imply the influence of more complex facto
rs in the solution of Rn-222 in water. Due to the relationship between
radon and Ra-226, the concentration of the latter was measured in the
same water using radiochemical separation and a scintillation ZnS(Ag)
detector, No significant correlation between Ra-226 and Rn-222 concen
trations has been observed unless measurements carried out in a high b
ackground radiation region are considered separately.