Paleogeochemical deposits in northern Chile are a rich source of naturally
occurring sodium nitrate (Chile saltpeter). These ores are mined to isolate
NaNO3 (16-0-0) for use as fertilizer. Coincidentally, these very same depo
sits are a natural source of perchlorate anion (ClO4-). At sufficiently hig
h concentrations, perchlorate interferes with iodide uptake in the thyroid
gland and has been used medicinally for this purpose. In 1997, perchlorate
contamination was discovered in a number of US water supplies, including La
ke Mead and the Colorado River. Subsequently, the Environmental Protection
Agency added this species to the Contaminant Candidate List for drinking wa
ter and will begin assessing occurrence via the Unregulated Contaminants Mo
nitoring Rule in 2001. Effective risk assessment requires characterizing po
ssible sources, including fertilizer. Samples were analyzed by ion chromato
graphy and confirmed by complexation electrospray ionization mass spectrome
try. within a lot, distribution of perchlorate is nearly homogeneous, presu
mably due to the manufacturing process. Two different lots we analyzed diff
ered by 15%, containing an average of either 1.5 or 1.8 mg g(-1). Inadequat
e sample size can lead to incorrect estimations; 100-g samples gave suffici
ently consistent and reproducible results. At present, information on natur
al attenuation, plant uptake, use/application, and dilution is too limited
to evaluate the significance of these findings, and further research is nee
ded in these areas. Published by Elsevier Science Ltd.