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The change in the absorbance upon chlorination (the differential absorbance, AA) of natural organic matter (NOM) that has been concentrated, isolated, and/or fractionated from five sources was explored as a possible indicator of the formation of total organic halogen (TOX) in the samples. The results demonstrate that concentration and isolation of NOM using techniques that are currently in widespread use does not significantly alter the TOX-deltaA272 relationship that applies to the unprocessed NOM. However, when such samples are fractionated, the TOX-deltaA272 relationships for the different fractions are not identical. In particular, when the hydrophobic and hydrophilic neutral fractions of NOM are chlorinated, the amount of TOX formed per unit of A272 destroyed is significantly larger than the corresponding value for other NOM fractions. This observation might reflect the relatively high content of proteins and other amino acid structures that can be disinfection by-product precursors but that absorb little or no light at 272 nm.

This study examined correlations between the differential absorbance at 272nm (deltaA272) and the formation of disinfection by-products (DBPs) in chlorinated water from the Tolt River, a water source for Seattle, WA. The DBPs investigated included chloroform (CHCl3), dichlorobromomethane (CHCl2Br), mono-, di- and trichloroacetic acids (MCAA, DCAA, and TCAA, respectively), chloral hydrate (CH), dichloroacetonitrile (DCAN) and 1,1,1-trichloropropanone (TCP). Whereas the kinetics of DBP formation are complex and are non-linear, the same DBP data represented as a function of deltaA272 are quite simple. Absorbance decreases when the water is chlorinated, i.e., deltaA272 is always negative. The DBP vs. -deltaA272 correlations can almost always be quantified by linear equations, at least above some threshold value of -deltaA272, with R2 values > 0.95. The only DBP that did not follow this trend was CH, for which an exponential relationship better described the data. TCP and DCAN were unstable at pH 7 and 8, but at pH 6 linear correlations between their concentrations and -deltaA272 were as strong as those for the more stable DBPs. The threshold -deltaA272 value is approximately the same for many of the DBPs studied, supporting the hypothesis that individual DBPs are released following the formation of a common intermediate, or at least a small group of similar intermediates. The DBP vs. -deltaA272 correlations may have practical value since they provide an alternative approach for monitoring the formation of individual DBP species on-line, but the generality of the relationships needs to be further examined.

The ability of iron oxide-coated sand (IOCS) to adsorb strontium from synthetic wastes simulating the tank wastes at the Hanford Nuclear Reservation was examined in this study. These wastes have high pH and high ionic strength, containing up to 5.5 M Na+, 3.7 M NO3-, and 1.2 M OH-. The use of IOCS in such applications may be advantageous because it is inexpensive, is nontoxic, and can be prepared from readily available materials. IOCS can selectively remove strontium from solutions, even when they contain overwhelmingly higher concentrations of potentially competing cations such as Ca2+, Al3+, and Cr3+. Sr-EDTA chelates do not adsorb to IOCS. However, the interference caused by EDTA can be substantially overcome by the addition of excess Ca to the solution since Ca displaces Sr from EDTA. The adsorbed Sr can be released, and the IOCS can be regenerated by exposure to dilute acid (pH approximately 3) for short periods. The physical and adsorptive properties of the IOCS remain essentially unaltered over at least several dozens of regeneration cycles, corresponding to treatment of at least 20000 bed volumes of influent. The only byproduct of the regeneration process is a small volume of residual waste containing essentially only strontium and dilute acid.

The influence of heating or boiling on the formation and behavior of disinfection by-products (DBPs) was investigated in DBP-spiked reagent water, municipal tap water, and synthetic water containing chlorinated aquatic humic substances. Thermal cleavage of larger halogenated species leads to both formation of smaller chlorinated molecules (including THMs and HAAs) and dechlorination of organics. In parallel with their formation from larger molecules, THMs can be volatilized, and this latter process dominates the change in their concentration when water is boiled. HAAs are not volatile, but they can be destroyed by chemical reactions at elevated temperatures, with the net effect being loss of trihalogenated HAAs and either formation or loss of less chlorinated HAAs. Although other identifiable DBPs can be generated at slightly elevated temperatures, in most cases their concentrations decline dramatically when the solution is heated.