A. Vengosh et al., BORON ISOTOPE APPLICATION FOR TRACING SOURCES OF CONTAMINATION IN GROUNDWATER, Environmental science & technology, 28(11), 1994, pp. 1968-1974
Boron isotope composition and concentration of sewage effluent and pri
stine and contaminated groundwater from the Coastal Plain aquifer of I
srael have been determined. The application of boron compounds, especi
ally sodium perborate as a bleaching agent in detergents, leads to an
enrichment of boron in wastewaters. Anthropogenic boron in wastewater
is isotopically distinct from natural boron in groundwater and thus ca
n be utilized to identify the source of contamination. It is shown tha
t delta(11)B (where delta(11)B = [((B-11/B-10)(sample)/(B-11/B-10)(NBS
951))-1] X 1000) values of raw and treated sewage effluents from the
Dan Region Sewage Reclamation Project (delta(11)B = 5.3-12.9 parts per
thousand) overlap those of natural nonmarine sodium berate minerals (
-0.9 parts per thousand to +10.2 parts per thousand) but differ signif
icantly from those of regional uncontaminated groundwater (similar to
30 parts per thousand) and seawater (39 parts per thousand). Groundwat
er contaminated by recharge of treated sewage yields a high B/Cl ratio
with a distinctive anthropogenic isotopic signature (7-25 parts per t
housand). Elemental B and delta(11)B variations reflect both mixing wi
th regional groundwater and boron isotopic fractionation associated wi
th boron removal by adsorption onto clay minerals. The distinctive iso
topic signature of anthropogenic boron can be recognized, however, in
most samples and differs significantly from those of natural sources o
f contamination in the Coastal Plain aquifer of Israel, such as marine
-derived saline groundwater (35-60 parts per thousand). This enables u
tilization of the boron isotope composition of groundwater as a tracer
for identification and quantification of contaminants in groundwater.