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THE FLORIDA STATE UNIVERSITY ARTS AND SCIENCES ...

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50ºC (36ºF - 122ºF) (Brady & Weil, 2002; Poulin et al., 2006). While there are no studies<br />

reviewed to show the possibility of denitrification above 50ºC (122ºF), it is theoretically<br />

possible where bacteria have evolved to cope with specific environmental conditions.<br />

Researchers assume that reaction rates double for every 10ºC (50ºF) increase in<br />

temperature (Arrhenius rate law). Since groundwater temperature generally reflective of<br />

the average temperature of the region, it may be therefore be difficult to observe a<br />

relationship between temperature and denitrification rates in groundwater in a specific<br />

area.<br />

Nevertheless Robertson et al. (2000, 2008) demonstrate a correlation between water<br />

temperature and denitrification rates in a permeable reactive barrier system.<br />

Denitrification is observed at temperatures as low as 2ºC (36ºF). Robertson et al. (2000)<br />

reported a denitrification rate of 5 mg-N/l/day for a temperature range of 2 ºC (36 ºF) -<br />

5ºC (41ºF) and 15–30 mg-N/l/ day for a temperature range of 10ºC (50ºF) - 20ºC (68ºF).<br />

Pfenning and McMahon (1996) demonstrated that lowering temperatures by 18ºC (65ºF)<br />

result in a 77 % decrease in the rates of denitrification. This shows that there is a direct<br />

correlation between temperature and the rate of denitrification.<br />

Christiansen and Cho (1983) reported that abiotic denitrification of nitrite by soluble<br />

organic matter can occur in frozen soil. At one field site, Cannavo et al. (2004) observed<br />

that, unlike CO2 levels, N2O levels in soil are independent of temperature; the authors<br />

ascribed this to aerobic denitrifying fungi that are much more tolerant of low<br />

temperatures than bacteria.<br />

Changes in the denitrification rate due to seasonal temperature variations may be masked<br />

by deviations in the rate of organic carbon flux. For example, Cannavo et al. (2004)<br />

found that freeze–thaw cycles increase the flux of carbon to the unsaturated zone and can<br />

create anaerobic micro-environments in which denitrification can become established.<br />

The observed increase in the denitrification rate with an increase in temperature varies<br />

8

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