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2.4.7. Texture 7 (Sandy Loam)<br />

The Sandy loam dataset can be divided based on temperature into 18 subsets. The<br />

following temperatures within the sandy loam texture have more that 3 records of data. 2<br />

ºC (n=6), 3 ºC (n=6), 4 ºC (n=6), 5 ºC (n=8), 7 ºC (n=5), 10 ºC (n=10), 11 ºC (n=5), 12 ºC<br />

(n=9), 13 ºC (n=6), 14 ºC (n=6), 15 ºC (n=6), 16 ºC (n=6), 18 ºC (n=11) , 20 ºC (n=16),<br />

22 ºC (n=3), 25 ºC (n=19), 28 ºC (n=31), and 35 ºC (n=21).<br />

The majority of the data, once sub-divided, do not have different values for organic<br />

carbon, and pH. There are only three subsets (7-20, 7-25 and 7-28) with three or more<br />

unique nitrate concentration values. The linear relationship between the denitrification<br />

rate and nitrate concentration is weak for all of the three subsets. The same applies to pH<br />

values, except for 7-15, 7-20, 7-22, 7-25 and 7-28. Except for 7-22 there is no significant<br />

relationship between the denitrification rate and pH. Even with organic carbon values<br />

there are no subsets with three or more organic carbon values except for 7-5, 7-20 and 7-<br />

28, unfortunately there is no significant linear relationship between the denitrification rate<br />

and organic carbon.<br />

The water filled porosity values fortunately do yield more information. With the<br />

exception of 7-15 and 7-22 all of the subsets have three or more unique values. All of the<br />

subsets show improvement in linear relationship between the denitrification rate and<br />

water filled porosity. In general while there is an improvement in the coefficient of<br />

determination the only subsets with a significant improvement are 7-4, 7-7, 7-10, 7-12, 7-<br />

13, 7-14, 7-16 and 7-28 (Figure 2.23 - Figure 2.29)<br />

52

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