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THE FLORIDA STATE UNIVERSITY ARTS AND SCIENCES ...

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Once again the equations developed based on the restricted variables are better at<br />

predicting the denitrification rate. The improvement is however not sufficient enough for<br />

it to be used with any confidence.<br />

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

Texture ten is divided into two groups, the first group comprises of 55 records and is used<br />

for the development of the equations and the second contains 16 records and is used as an<br />

assessment<br />

Equations for silty clay loam are developed based on the information below, the<br />

coefficient of determination for both equations is 0.28.<br />

R<br />

R<br />

dn<br />

dn<br />

=<br />

=<br />

- 0.17<br />

+ 9.74 ∗ pH + 0.03 Nitrate<br />

- 0.08<br />

- 0.14<br />

∗<br />

∗Temperature<br />

( ° C) + 0..03 ∗ WFP (%) - 1.75 ∗<br />

Concentration<br />

Soil Depth (cm) + 8.53 ∗ Bulk density (gm cm<br />

∗Temperature<br />

( ° C) + 0.03∗<br />

WFP (%) - 2.5 ∗<br />

+ 0.02*<br />

Nitrate Concentration<br />

( μg<br />

N g<br />

-1<br />

soil) - 51.5<br />

(<br />

OC (%)<br />

136<br />

OC (%)<br />

-1<br />

μ g N g soil) ----- Equation 4.16<br />

+ 9.5 ∗<br />

-3<br />

pH<br />

) −<br />

63.<br />

45<br />

Table 4.24 Texture 10, Linear multi-regression using all variables.<br />

----- Equation 4.17<br />

Coefficients Estimate Std.Error t-value Significance<br />

Intercept -63.45 60.63 -1.05<br />

Bulk Density (g cm -3 ) 8.53 41.27 0.21<br />

NO3 - Conc ( µg N g -1 soil) 0.03 0.01 0.89<br />

OC (%) -1.75 4.25 -0.41<br />

pH 9.74 2.89 3.37 **<br />

Soil Depth (cm) -0.09 0.41 -0.21<br />

Temp (ºC) -0.17 0.29 -0.58<br />

WFP (%) 0.03 0.12 0.25<br />

Signif.Codes Signif.Codes Signif.Codes<br />

0.00 '***' 0.00 '**' 0.01<br />

0.01 '*' 0.05 '.' 0.10<br />

0.10 1.00

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