Hydroxyl radical formation rates, steady-state concentration,and overall scavenging rate constant were measuredby irradiation of surface lake water samples from Piedmont(NW Italy) and nitrate-rich groundwater samples fromMoldova (NE Romania). Dissolved organic matter (DOM)was the main source and sink of
![](/images/entities/bull.gif)
OH upon lake waterirradiation, with [
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OH] being independent of DOM amount.Water oxidation by photoexcited DOM is a likely
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OHsource in the presence of very low levels of nitrate anddissolved iron. Under different circumstances it is not possibleto exclude other processes, e.g., DOM-enhanced photo-Fenton reactions. Under the hypotheses of no interaction andabsence of mutual screening of radiation, nitrate wouldprevail over DOM as
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OH source for a NO
3-/DOM ratio higherthan 3.3 × 10
-5 (mol NO
3-) (mg C)
-1, DOM prevailing forlower values. Substantial DOM photolability was observedupon irradiation of nitrate-rich groundwater, mainly dueto the elevated
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OH generation rate. For the first time to ourknowledge, evidence was also obtained of the photoformation of potentially toxic and/or mutagenic nitroaromaticcompounds upon irradiation of natural lake water andgroundwater samples, proportionally to the nitrate levels.