QUANTITATIVE SEPARATION AND DETERMINATION OF INORGANIC AND ORGANIC FORMS OF TOTAL CARBON AND RADIOCARBON IN NATURAL-WATERS AND APPLICATION AT A RADIOACTIVE-WASTE MANAGEMENT SITE
Rr. Rao et Rwd. Killey, QUANTITATIVE SEPARATION AND DETERMINATION OF INORGANIC AND ORGANIC FORMS OF TOTAL CARBON AND RADIOCARBON IN NATURAL-WATERS AND APPLICATION AT A RADIOACTIVE-WASTE MANAGEMENT SITE, Radiochimica Acta, 65(1), 1994, pp. 63-74
A method for the quantitative separation and measurement of both total
carbon and C-14 in dissolved inorganic carbon (DIC) and dissolved org
anic carbon (DOC) in moderate-volume (up to 1.51) samples is presented
, accompanied by a systematic optimization of process and analytical v
ariables. Inorganic carbon is removed by acidification and gas strippi
ng, while DOC is wet-oxidized using a mixture of potassium persulphate
, potassium dichromate, and perchloric acid and an oxygen sweep while
boiling the sample. This treatment is shown to provide quantitative ox
idation of even refractory compounds (humic acid) at concentrations ab
ove those observed in natural waters. In both cases, the CO2 is trappe
d in NaOH, precipitated as BaCO3, and subsequently re-converted to CO2
and transferred to Carbo-Sorb for liquid scintillation counting. The
study analyzed the effects of CO2 loading, storage time, and Carbo-sor
b/Permafluor E(+) ratios on quenching, sensitivity and efficiency in C
-14 measurements. The high precision and accuracy (each +/-5%), and lo
w detection limits (0.1 and 0.3 mg.l(-1) for DIC and DOC, respectively
and 0.06 Bq.g(-1) of carbon for C-14) provided by the method make it
suitable for radiocarbon speciation studies in natural waters. The met
hod has been applied to measure radiocarbon concentrations in ground a
nd surface waters downgradient of a low level radioactive waste manage
ment site at the Chalk River Laboratories. Radiocarbon releases from t
he waste to groundwater occur in both inorganic and organic forms. App
roximately 20% of the total carbon and 10% of the total C-14 in ground
water are present in organic species; less than 2% of both the (DIC)-C
-14 and (DOC)-C-14 delivered to the wetland by groundwater discharge s
ubsequently leave in surface waters.