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Handbook of Solvents - George Wypych - ChemTech - Ventech!

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23.1 Natural attenuation <strong>of</strong> chlorinated solvents 1599<br />

Compound<br />

Carbon<br />

tetrachloride<br />

Mean <strong>of</strong> field/in-situ<br />

studies<br />

1 st order rate<br />

coefficients,<br />

day -1<br />

halflives,<br />

day<br />

number<br />

studies<br />

used<br />

for<br />

mean<br />

Recommended 1 st order rate<br />

coefficients<br />

low-end high-end<br />

1 st order rate 1 st order rate<br />

coefficients,<br />

day -1<br />

half-lives<br />

day<br />

coefficients,<br />

day -1<br />

half-lives<br />

day<br />

0.37 1.9 9 0.0037 187 0.13 5<br />

Chlor<strong>of</strong>orm 0.030 23 1 0.0004 1,733 0.03 23<br />

Dichloromethane 0.0064 108 1 0.0064 108 - -<br />

Trichlor<strong>of</strong>luoromethane<br />

- - - 0.00016 4,331 0.0016 433<br />

2, 4-Dichlorophenol 0.014 50 2 0.00055 1,260 0.027 26<br />

Comments<br />

Range not appropriate for nitrate-reducing<br />

conditions. Expect lower<br />

limits to be much less<br />

Only one field study available.<br />

Biodegradation under nitrate-reducing<br />

conditions expected<br />

Rate constant reported from a single<br />

field study under methanogenic conditions<br />

All studies with very low concentrations<br />

<strong>of</strong> this compound<br />

Range may not be appropriate for nitrate<br />

reducing conditions<br />

[From T.H. Wiedemeier, H. S. Rifai, C. J. Newell and J.T. Wilson, Natural Attenuation <strong>of</strong> Fuels and Chlorinated<br />

<strong>Solvents</strong> in the Subsurface. Copyright © 1999 John Wiley & Sons, Inc. Reprinted by permission <strong>of</strong> John<br />

Wiley & Sons, Inc.]<br />

23.1.5 GEOCHEMICAL EVIDENCE OF NATURAL BIOREMEDIATION AT<br />

CHLORINATED SOLVENT SITES<br />

23.1.5.1 Assessing reductive dechlorination at field sites<br />

Assessing biological activity at a field site based on monitoring data can be difficult. However,<br />

there are a number <strong>of</strong> monitoring parameters that can be indicative <strong>of</strong> halorespiration.<br />

First, the presence <strong>of</strong> methane in the groundwater indicates that fermentation is occurring<br />

and that the potential for halorespiration exists. Second, the transformation <strong>of</strong> PCE and TCE<br />

has been studied intensely and many researchers report that <strong>of</strong> the three possible DCE isomers,<br />

1,1-DCE is the least significant intermediate and that cis-1,2-DCE predominates over<br />

trans-1,2-DCE. 103-105 Third, because chlorinated ethenes are 55 to 85% chlorine by mass, the<br />

degradation <strong>of</strong> these compounds releases a large mass <strong>of</strong> chloride. Therefore, elevated chloride<br />

concentrations also indicate reductive dechlorination.<br />

23.1.5.2 Plume classification schemes<br />

Wiedemeier et a1. 106 proposed a classification system for chlorinated solvent plumes based<br />

on the amount and origin <strong>of</strong> fermentation substrates that produce the hydrogen that drives<br />

halorespiration. Three types <strong>of</strong> groundwater environments and associated plume behavior,<br />

Type 1, Type 2, and Type 3, are described below. While the classification system can be<br />

used to represent entire plumes, it can also be used to define different zones within a chlorinated<br />

solvent plume.<br />

23.1.5.2.1 Type 1<br />

For highly chlorinated solvents to biodegrade, anaerobic conditions must prevail within the<br />

contaminant plume. Anaerobic conditions are typical at sites contaminated with fuel hydro-

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