Carbon content and sorption coefficients (K
d and K
oc) for all samples, are presented in
Table 1. The K
d values vary from 1.3 to 31.69 L kg
-1 and K
oc values range from 406 to 1 707 L kg
-1. The actual and predicted values (training, validation and testing dataset) are given in
Table 2. In total, 21 out of 36 data values were used randomly in order to train the network. Using the training dataset, a relationship was found between inputs (organic carbon) and measured outputs (K
d and K
oc), and the error of this step was applied for adjusting the weights. Moreover, seven validation values were utilized to control the network correct learning and seven testing values were employed for evaluating the final network performance. Parameters of the best network structure are presented in
Table 3. Each model consisted of one node in the input (organic carbon) and one in the output layer (sorption coefficients). The numbers of nodes in the hidden layer for K
d and K
oc and optimum iteration were 6.6 and 1 000, respectively; while the hyperbolic tangent was the most efficient transfer function. The actual values were plotted against the predicted values for datasets and R
2 values determined (
Figures 2 and 3). The higher the R
2 values (closer to 1) and the lower the ME and RMSE values (closer to zero), the greater the accuracy of the model.
Table 4 shows the appropriate accuracy of ANNs in predicting the sorption coefficients. R
2 and RMSE values for the testing dataset were 0.99 and 0.01 L/kg soil for K
d, and 0.94 and 0.07 L/kg soil for K
oc, respectively. Low ME values (ME = 0.0001 and 0.0059 for K
d and K
OC, respectively), and low RMSE and high R
2 values, showed that ANN is a powerful technique in modeling and predicting variations of K
d and K
oc values of diuron with soil organic carbon content variability. This means that K
d and K
oc values are strongly correlated with soil organic carbon.