The most common oxidative destruction technique used is the Standard Fenton reaction, in which Fe(II) reacts with hydrogen peroxide to form Fe(III), a hydroxide ion, and a hydroxyl radical. This hydroxyl radical then reacts with TCE to form carbon dioxide and organic acids. The Standard Fenton reaction requires highly corrosive reaction conditions, and thus has limitations for in situ applications: it requires a low pH and hydroxyl radicals are rapidly consumed by hydroxyl scavengers found in the subsurface.
These problems are alleviated through the Chelate-Modified Fenton reaction, which includes the addition of a nontoxic chelate (L) such as citrate or gluconic acid. The chelate allows the reaction to take place at near neutral pH and control hydrogen peroxide consumption by binding to Fe(II), forming an FeL complex. This increases the H2O2:Fe(II) ratio greatly, therefore accelerating the rate of superoxide radical anion formation, aiding in DNAPL destruction. The chelate also binds to Fe(III), preventing its precipitation as ferric hydroxide and thus prevents problems associated with injection well plugging. It is also possible to generate both H2O2 and chelate (gluconic acid) through enzymatic reactions. Experimentation has shown that increasing the chelate:Fe(II) molar ratio reduces the amount of hydrogen peroxide used to degrade TCE. Our experimental results have also shown that > 90% dechlorination (through chloride ion and TCE analysis) can be achieved. This project is funded by DOE-KRCEE and by NIEHS.