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Texture 7 Temperature 28 : Denitrification Rate Vs. Water Filled Porosity<br />

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

16<br />

14<br />

12<br />

10<br />

8<br />

6<br />

4<br />

2<br />

0<br />

S 2.55833<br />

R-Sq 73.2%<br />

20<br />

Rdn (kgN ha-1 d-1) = 0.9599 + 0.08688 WFP (%)<br />

40<br />

60<br />

80<br />

WFP (%)<br />

Figure 2.29 7-28; Denitrification Rate Vs. Water filled Porosity<br />

2.4.8. Texture 8 (Silt Loam)<br />

The silty loam database was subdivided into the following subsets: 8-3 (n=9), 8-4<br />

(n=9),8-6 (n=10),8-7 (n=11), 8-8 (n=10),8-9 (n=10),8-10 (n=27), 8-12 (n=6), 8-13 (n=13)<br />

,8-14 (n=18), 8-15 (n=9),8-17 (n=8), 8-18 (n=4), 8-20 (n=48), 8-21 (n=4) and 8-25<br />

(n=59). Of these subsets only the subsets 8-10,8-13,8-14,8-15,8-20 and 8-2 have three or<br />

more unique organic carbon values, unfortunately there is no subset that provides a<br />

significant linear correlation between the denitrification rate and organic carbon. The<br />

only subsets with three or more unique WFP values are 8-13, 8-15, 8-17, 8-20 and 8-25.<br />

The only subset with a significant correlation is 8-17, between Rdn and WFP (Figure<br />

2.30).<br />

There are six subsets with three or more unique pH values; they are 8-10, 8-12, 8-13, 8-<br />

14, 8-15 and 8-25. None of these subsets have a significant linear correlation between the<br />

pH and denitrification rate.<br />

All of the subsets except for 8-7, 8-8 and 8-21 have three or more unique nitrate<br />

concentration values. The subsets that yield a significant correlation are 8-4 and 8-15.<br />

56<br />

100<br />

120<br />

140

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