2.2 Artificial Neural Networks
Artificial neural networks are black box models that can perform an estimation using
limited input and output data patterns. In this study, the Generalized Regression
Neural Network (GRNN) method was used to relate the XRD data to the properties of
the crystal structures of zeolites.
The basics of the GRNN can be found in the literature [10,11].
The GRNN method
does not require an iterative training procedure but instead estimates any arbitrary
function between input and output vectors, drawing the function estimate directly
from the training data. This method is consistent, that is, as the training set size be-
comes large, the estimation error approaches zero, with only mild restrictions on the
function. The GRNN is used for estimation of continuous variables, as in standard
regression techniques. It is based on a standard statistical technique called kernel
regression. By definition, the regression of a dependent variable y on an independent
x estimates the most probable value for y, given x and a training set. The regression
method will produce the estimated value of y, which minimizes the mean-squared
error. The GRNN consists of four layers: input layer, pattern layer, summation layer,
and output layer. The first layer is fully connected to the second, pattern layer, where
each unit represents a training pattern and its output is a measure of the distance of
the input from the stored patterns. Each pattern layer unit is connected to the two
neurons in the summation layer: S-summation neuron and D-summation neuron. The
S-summation neuron computes the sum of the weighted outputs of the pattern layer
while the D-summation neuron calculates the unweighted outputs of the pattern neu-
rons. The connection weight between the i
th
neuron in the pattern layer and the S-
summation neuron is y
i
, the target output value corresponding to the i
th
input pattern.
For D-summation neuron, the connection weight is unity. The output layer merely
divides the output of each S-summation neuron by that of each D-summation neuron.
In this method, the spread σ is a smoothing parameter, the optimal value of which is
often determined experimentally [12]. When the spread parameter σ is made large,
the estimated density is forced to be smooth and in the limit becomes a multivariate
Gaussian with covariance σ
2
I. On the other hand, a smaller value of σ allows the
estimated density to assume non-Gaussian shapes, but with the hazard that wild
points may have too great an effect on the estimate. In this study, different spreads
were tried to find the best one that gave the minimum difference between predicted
and experimental values for the utilization of the cross-validation data.
2.3 Method
Zeolites are hydrated microporous crystalline materials. The zeolite framework con-
sists of an assemblage of SiO
4
and AlO
4
tetrahedra, joined together in various regular
arrangements through shared oxygen atoms, to form an open crystal lattice. The mi-
cropore structure is determined by the crystal lattice, which contains pores of molecu-
lar dimensions into which guest molecules can penetrate. The cations (e.g., Na) are
placed in special positions near the Al atoms. The pore size varies for different zeo-
lites, depending on the arrangement of the atoms forming the zeolite crystal structure.
The crystal structure of a material or the arrangement of atoms in a crystal structure
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