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Rdn (kgN ha-1 d-1)<br />

Texture 8 Temperature 25 WFP 90 Nitrate Concentration 320 : Denitrification Rate Vs. Organic Carbon<br />

20<br />

15<br />

10<br />

5<br />

0<br />

S 1.82814<br />

R-Sq 97.9%<br />

2.90<br />

Rdn (kgN ha-1 d-1) = - 506.8 + 174.5 OC (%)<br />

2.92<br />

2.94 2.96<br />

OC (%)<br />

Figure 2.84 8-25-90-320; Denitrification Rate Vs. Organic Carbon.<br />

2.6.9. Texture 9 (Silty Clay)<br />

Texture nine was subdivided into three classes 9-15-25-9 (n=4), 9-25-100-9 (n=4) and 9-<br />

30-100-9 (n=4). There is no significant linear relationship between the denitrification rate<br />

and organic carbon or pH for the 9-15-25-9 and the 9-25-100-9 subset. For the 9-30-100-<br />

9 subset there is no significant relationship between the denitrification rate and pH, the<br />

relationship between Rdn – OC is shown in Figure 2.85.<br />

2.6.10. Texture 10 (Silty Clay Loam)<br />

Texture ten is subdivided into 10-18-100-302 (n=3), 10-25-60-89 (n=3), 10-25-60-288<br />

(n=3), 10-25-60-366 (n=3), 10-25-75-89 (n=3), 10-25-75-228 (n=3), 10-25-75-336 (n=3),<br />

10-25-90-89 (n=3), 10-25-90-228 (n=3), and 10-25-90-366 (n=3).All of the subsets have<br />

only one nitrate concentration value; hence no additional information is acquired. Except<br />

for the first three subsets all of the subsets show a significant linear relationship between<br />

the denitrification rate and organic carbon. (Figure 2.86 -Figure 2.92).<br />

89<br />

2.98<br />

3.00

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