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ORIGINAL RESEARCH article

Front. Chem. , 18 March 2025

Sec. Theoretical and Computational Chemistry

Volume 13 - 2025 | https://doi.org/10.3389/fchem.2025.1543588

This article is part of the Research Topic Design of Extended Networks for Tuning Functionality of Materials View all 3 articles

Predictive modeling of molecular interaction energies using topological and spectral entropies of zeolite AWW

  • 1Department of Mathematics, School of Advanced Sciences, Vellore Institute of Technology, Vellore, India
  • 2Department of Mathematics, Loyola College, Chennai, India

Zeolites are extremely massive mineral crystals with complex frameworks, composed of internal porous structures with channels and cages. Open-framework aluminophosphates (AlPOs) are a significant class of inorganic crystalline compounds known for their diverse properties. Our study focuses on the topological aspects of zeolite frameworks using graph theoretical techniques, providing insights into computational chemistry. In this article, we compute various degree-based topological indices, information entropy, and spectral entropies of zeolite AWW using the bond partitioning approach to assess the complexity of the framework. Additionally, we present the HOMO–LUMO gap measures to evaluate the global chemical descriptors using the eigenvalues of the adjacency matrix of zeolite structures. Furthermore, we developed exponential and polynomial regression models using the obtained information entropy and spectral values to predict various potential energies of the framework. Based on the outcomes of the study, we infer that the information entropies and spectral value have a significant relationship with the potential energies.

1 Introduction

Zeolites are minerals with crystalline structures that have regular frameworks constructed by channels and pores an the molecular level. Zeolite catalysts are employed throughout gasoline production and in the fields of adsorption, ion exchange, heterogeneous catalysis, sensors, and medicine. These crystals are also frequently used in solar energy conversion (Mihaela and Ildiko, 2012). Zeolite frameworks have Si tetrahedral nodes (T-atoms) and T-O-T, a bond referring to the arrangement where T stands for a tetrahedrally coordinated atom, usually silicon (Si) or aluminum (Al), and O stands for oxygen. The oxygen atom acts as a bridge between two tetrahedrally coordinated sites. Replacing Si with Al or other tetrahedral atoms significantly alters the characteristics of zeolites. This changes the framework’s affinity to other cations, allowing for customization of ion-exchange characteristics and adsorption surfaces. The tetrahedral atoms’ three-dimensional geometry forms rings, cages, channels, and pores, resulting in different frameworks (Kapko et al., 2010; Liebau, 1983; Barrer, 1979). Because there were many distinct materials, some with a common framework but differing by the chemical proposition, we needed to categorize all the different crystalline aluminosilicate materials. As a result, the concept of structural variation came into existence (Liebau, 1983; Barrer, 1979).

The aluminophosphate crystalline sieves, denoted as AlPO4n (where n corresponds to distinct structure type), marks the beginning of the era of open-framework aluminophosphates as a significant group of zeolites together with associated microporous materials (Wilson et al., 1982; Richardson et al., 1989). AlPO4n is constructed based on the precise alternation of AlO4 and PO4 tetrahedra through corner exchange to generate a framework that is neutral and has an Al/P ratio of 1. Microporous aluminophosphates were discovered (Yu and Xu, 2006), and the extensive range of framework compositions and potential uses in catalysis, adsorption, and assembly have attracted much curiosity. The rational synthesis of novel materials has become increasingly significant in the field of materials chemistry (Richardson et al., 1989). Zeolite AlPO422 or AWW has an innovative topological structure, which is depicted in Figure 1; it has an equal number of two new polyhedral units that share faces. In this study, the AWW zeolite framework is represented by a PDB file containing Si atoms in tetrahedral coordination linked by O atoms. To model Al and P atoms, specific Si atoms were substituted based on chemical rules, ensuring charge balance and structural consistency. The modified framework, comprising Al, P, and the remaining Si atoms, was used for topological characterization within the AWW topology. Topological measures such as degree and degree sum primarily focus on the contributions of heavier atoms like Al and P, while lighter O atoms act as linkers, indirectly influencing the connectivity. This distinction is significant because the structural and functional properties of zeolite materials largely depend on the ratio of heavy atoms.

Figure 1
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Figure 1. Polyhedral views of the zeolite AWW(2,2,2) framework.

A chemical composition graph is used to demonstrate the basic structure of a chemical compound (Balaban, 1985; Sato, 1991; Chandler, 2019). The vertices represent each of the atoms of the compound, and the edges indicate the bonds that occur among them. A topological index is used to measure the relationship between a chemical compound’s structure and various physical, chemical, or biological characteristics. Degree-based descriptors are extensively used topological descriptors with applications in computational chemistry, whereas topological indices based on neighborhood degree sum are capable of accurately determining most physicochemical parameters (Gutman and Tošović, 2013; Mondal et al., 2019; Ramane et al., 2021; Ullah et al., 2024; Mondal et al., 2021).

Topological descriptors for zeolites were developed to enhance machine learning, optimization, and algorithmic techniques (Krivovichev, 2013; Arockiaraj et al., 2022a; Arockiaraj et al., 2022b; Arockiaraj et al., 2021; Jacob et al., 2023). To better understand the basis for relating the structure and property to the synthesis technique, experimental and computational methods have been closely linked in modern zeolite synthesis. The zeolite framework influences its physicochemical properties such as adsorption, phase transformation, complexity, and chirality of molecules. Recent studies indicate that the topological index quantifies the relationship between zeolite molecular structures and a wide range of physicochemical characteristics (Jacob et al., 2023; Peter and Clement, 2023; Jacob and Clement, 2024; Peter and Clement, 2024; Prabhu et al., 2020).

The complexity of networks can be evaluated using statistical information measures (Bonchev, 1983; Anand and Bianconi, 2009; Mowshowitz, 1968a). Shannon’s information theory was used to develop the universal quantitative measurements of structural and chemical complexity, which are helpful for the investigation of several mineralogical, crystallographic, and chemical processes (Jacob et al., 2023; Dehmer and Mowshowitz, 2011; Krivovichev, 2012; Shannon, 1948). The probability of electrons in molecules and the chemical bonds between molecules have been effectively studied using information theory concepts (Nalewajski, 2006; Nalewajski, 2014). The communication theory for the chemical connection employs the basic information entropy of molecular systems in the atoms-in molecules, orbital, or local levels to ascertain electron probability distributions (Nalewajski, 2006; Nalewajski, 2014; Nalewajski, 2011). The information entropy (IE) method is used to quantitatively evaluate the complexity of zeolite structures and extract structural data from networks with numerous vertices (Krivovichev, 2013). The concept of structural information content based on the partitioning of vertex orbits was originally used to measure the complexity as well as the characteristics of the structure of molecular graphs (Rashevsky, 1960; Mowshowitz, 1968b; Dehmer, 2008).

The model obtained good accuracy and provided information about the connection between the zeolite framework structure and their mechanical stability (Evans and Coudert, 2017). The connections between zeolite frameworks and their characteristics are complicated, making an in-depth experimental investigation for novel zeolites necessary (Burtch et al., 2014). Various density functional theory computational techniques for determining zeolite characteristics have been established (Ranjan et al., 2023; Román-Román and Zicovich-Wilson, 2015; Fischer and Angel, 2017; Balasubramanian, 2023a; Balasubramanian, 2023b). Determining the zeolite lattice energy linked to formation enthalpy can help understand zeolite stability and structure, although computations are expensive but accurate (Román-Román and Zicovich-Wilson, 2015; Fischer and Angel, 2017; Stacey et al., 2023). Machine learning techniques can help determine the characteristics of zeolites by learning from a vast collection of known zeolites and their characteristics. It was demonstrated that some structural descriptors are suitable to characterize the lattice energy of zeolites in a comprehensible manner using a linearized equation, focusing on the intricate connection between structural features (Jacob et al., 2023; Peter and Clement, 2023; Jacob and Clement, 2024; Balestra et al., 2024). Electronic structural calculations help us understand how zeolite structures influence their performance. Long-range and short-range interaction energies significantly affect the geometry of the zeolite framework and their stability of transition states and adsorption behavior. Notably, long-range zeolite electrostatic interactions play a crucial role in describing transition-state structures and in predicting experimentally determined activation energies (Ranjan et al., 2023; Román-Román and Zicovich-Wilson, 2015; Fischer and Angel, 2017; Mansoor et al., 2018).

This article focuses on developing generalized expressions for descriptors such as degree-based and degree-sum-based measures specifically for the AWW zeolite structure, with any arbitrary dimension used to obtain structural data. A detailed analysis of bond information and spectral entropies is presented to evaluate the complexity of the AWW zeolite. Furthermore, we incorporated the exponential regression models that establish relationships between the measured entropies and molecular interaction energies, offering deeper insights into the energy and structural characteristics of zeolite. Global chemical reactivity descriptors and the spectral properties are also calculated using the eigen values of AWW zeolite structures.

2 Computational methods of the molecular topological index

Let G=V(G),E(G) be a simple undirected graph. The number of atoms and bonds between atoms in the graph G is denoted by |V(G)| and |E(G)|, respectively. The degree of an atom uV(G) is given by du, the number of bonds that are adjacent to atoms u and dsu can be described by the sum of the degrees of the neighborhood atoms of u, and it can be expressed as dsu=vNG(u)dv, where NG(u)=vV(G):uvE(G).

For ψ{d,ds}, we define the degree and degree sum-type molecular topological indices (Gutman and Tošović, 2013; Mondal et al., 2019; Ramane et al., 2021; Gutman, 2013; Leszczynski, 2012) with the following expression:

TψG=uvEGTψuv,(1)

where Tψ(uv) is a structural function of the molecular topological index with respect to the edge of molecular graph, for example, Tψ(uv) defined for the first Zagreb M1ψ(uv)=ψu+ψv, second Zagreb M2ψ(uv)=ψuψv, Randić Rψ(uv)=1ψvψu, atom bond connectivity ABCψ(uv) = ψu+ψv2ψuψv, harmonic Hψ(uv) = 2ψu+ψv, sum-connectivity SCψ(uv) = 1ψu+ψv, hyper-Zagreb HMψ(uv) = ψu+ψv2, geometric–arithmetic GAψ(uv) = 2ψuψvψu+ψv, irregularity irrψ(uv) = ψuψv, sigma σψ(uv) = ψuψv2, forgotten Fψ(uv) = ψu+ψv22ψuψv, augmented Zagreb AZψ(uv)ψuψvψu+ψv23, symmetric division degree SDDψ(uv) = ψu+ψv22ψuψvψuψv, and Sombor SOψ(uv)=ψu2+ψv2.

The molecular topological descriptors based on the degree and degree sum are obtained via the atomic valences of the framework’s chemical bonds. Various degree-type topological indices have been developed and employed extensively in molecular modeling of a wide range of zeolite framework characteristics and activities (Arockiaraj et al., 2022a; Jacob et al., 2023; Zhang et al., 2024; Peter and Clement, 2023). Self-powered multiplicative topological indices of chemical structure are derived from the product of edge functions associated with the degrees of end vertices of an edge (Kavitha et al., 2021). These indices have been developed using exponential vertex degree-based descriptors (Rada, 2019). Therefore, one can develop a self-powered multiplicative version of degree and degree sum-based topological indices using the following general form:

Tψŝ*G=uvEGTψuvTψuv.(2)

The edge partition technique is applied to derive the various degree and degree sum-based molecular topological indices. The sizes of the partitions on the basis of end vertex degrees are denoted by d(p,q), and the sizes of the partitions on the basis of end vertex degree sum are denoted by ds(p,q). These quantities are explicitly presented as follows:

d(p,q)=uvE(G):du,dv=(p,q),p,q1

ds(p,q)=uvE(G):dsu,dsv=(p,q),p,q1.

By considering Δ=maxuV(G)ψu and C=(p,q)N×N:1pqΔ2, the generalized form of degree and neighborhood degree sum molecular topological indices Equations 1, 2 can be modified as Equations 36.

TdG=p,qCdp,qTdpq,(3)
TdsG=p,qCdsp,qTdspq,(4)
Tdŝ*G=p,qCTdpqTdpqdp,q,(5)
Tdsŝ*G=p,qCTdspqTdspqdsp,q.(6)

2.1 Bond information entropy

The studies (Krivovichev, 2013; Krivovichev, 2012; Kaußler and Kieslich, 2021; Krivovichev, 2016) used the following equation to determine the quantity of structural Shannon’s information of the crystal structure:

IEG=i=1nρilogρi,(7)

where i represents the number of different crystallographic orbits in the structure and pi is the random choice probability for an atom from the ith crystallographic orbit, in other terms ρi=min, where mi and n are the multiplicity of the crystallographic orbit and the number of atoms in the primitive unit cell, respectively.

Now, Equation 7 will be modified to characterize the structural characteristics of the zeolite framework. The bonds of the zeolite framework are taken into account, and each of them receives a probability value based on the topological indices. The topological information entropy measures for degree type are defined using that molecular topological index T (Bonchev, 1983).

IETG=eEGρrelogρre,

where ρr(e) is the probability function of an edge that is based on the degree which is given by

ρre=TduvuvEGTduv=TduvTdG.

The information entropy measure based on the degree sum molecular topological descriptors is obtained by replacing Td with Tds. As observed in (Kazemi, 2016), the study introduces a new method for calculating graph entropy, utilizing degree-based topological indices as edge weights to evaluate the complexity and uncertainty of a graph’s structure. We could develop and manufacture an extensive range of novel materials with the desired characteristics using the information entropy concept, which was initially applied to inorganic and organic materials (Jacob et al., 2023; Peter and Clement, 2023; Abraham et al., 2022; Rahul et al., 2022; Kalaam et al., 2024), and study the compositional intricacy and structural disorder to change the structural and functional characteristics. Therefore, by using different topological indices, we obtain various entropy values given as follows:

IETψG=logTψG1TψGuvEGTψuvlogTψuv.(8)

By reformulating Equation 8 using self-powered multiplicative degree-based indices, as described in (Kavitha et al., 2021), we could establish a relationship between the self-powered multiplicative indices and the entropy computation typically associated with bond additive indices.

IETψG=logTψG1TψGlogTψŝ*G.(9)

The developed Equations 8, 9 are used to measure the various bond information entropy values of AWW zeolite. Furthermore, the measured information entropy was used to develop the possibility of machine learning of the AWW zeolite structure for studying the properties and activities (Arockiaraj et al., 2022a; Peter and Clement, 2023; Jacob and Clement, 2024; Peter and Clement, 2024).

2.2 Spectral information entropies

To define the spectral entropies for each edge uvE(G), we first construct a symmetric square matrix of order |V(G)| using the degree-based topological index of the graph as defined below (Bozkurt et al., 2010; Ghanbari, 2022; Rodríguez and Sigarreta, 2016):

MTd=0iftheverticesuandvofGarenotadjacentTduviftheverticesuandvofGareadjacent,(10)

where Td(uv) is a structural function of topological indices with respect to an edge, as defined in Section 2. For example, the matrix with respect to the sum connectivity index is defined as follows:

MSCd=0iftheverticesuandvofGarenotadjacent1du+dviftheverticesuandvofGareadjacent.

The study of graph energy obtained from the topological matrix indices offers insights into the structural properties of graphs, with potential applications in chemistry and communication networks (Bozkurt et al., 2010; Ghanbari, 2022; Rodríguez and Sigarreta, 2016; Chen et al., 2014; Hayat et al., 2024; Hui et al., 2022; Kosar et al., 2023). The novelty of this section is that we use the computed eigen values of the topological matrix indices of the zeolite framework to measure the spectral information entropies. Let λ1d,λ2d,λ3d,,λrd be non-zero eigenvalues of the degree-based molecular topological index matrices obtained from Equation 10. Then, in order to compute the spectral entropies, we now modify Equation 7 as follows:

IEMTλdG=i=1r|λid|j=1r|λjd|log|λid|j=1r|λjd|,(11)

where the ratio |λid|j=1r|λjd| is the random choice probability of eigen values. The degree sum-based entropies of the zeolite AWW can be measured using Equation 11 by exchanging Tλds for Tλd.

3 Molecular topological indices of zeolite AWW

The AWW zeolite structures are characterized by using the measurements provided in Section 2. As depicted in Figure 2, the cavities serve as the primary building component for the zeolite AWW molecular communication system, which has 32 vertices and 48 edges connected by eight squares and two octagons, such that some bonds are shared. In order to form a three-dimensional molecular structure, the cavities of AWW are arranged in the j×k×l configuration. This leads to the crystal lattice, which is represented by AWW(j,k,l), as shown in Figure 3, with j,k, and l indicating the number of cavities arranged along the bottom to top, along left to right, and front to back copies, accordingly. Since translational symmetry repeats a single unit cell an infinite number of times to fill the pores and topological indices are numerical values that cannot be generalized in terms of infinity, we have considered point symmetry and not translational symmetry.

Figure 2
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Figure 2. Primary cages in the AWW zeolite material.

Figure 3
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Figure 3. AWW(2,2,2) framework.

Figure 3 depicts the polyhedral structural growth of AWW. Figure 2 shows the primary cavities that are interconnected to generate the AWW(2,2,2) zeolite. Two types of polyhedral structures are considered in Figure 3: the front and back view frameworks. These are generated by connecting the two cavities via a tunnel and sharing all six rings between them. In contrast, the top- and side-view frameworks are directly connected by all eight rings and connected by the tunnels between the cavities. The total number of vertices (T-atoms) and edges (T-O-T bonds) in zeolite AWW(j,k,l) are 8jk(3l+1) and 4[12jkl+2jkjlkl] for j,k,l1.

3.1 Degree-type molecular descriptors of AWW zeolite

We employed the edge partition technique according to the degrees of the end atoms of bonds, and the degree sum of the end atoms of bonds used to generate different degree-based molecular topological descriptors of zeolite AWW(j,k,l) for j,k,l1 is listed below.

Bond degree partitions:

d(3,3)=2[8jk+3(jl+kl)+4(j+k)+2l]

d(3,4)=4[4jk+3(jl+kl)4(j+k)2l]

d(4,4)=2[24jkl12jk11(jl+kl)+4(j+k)+2l]

ds(9,9)=10[j+k+2]

Bond degree-sum partitions (when j,k,l2):

ds(9,10)=4[3j+3k2]

ds(10,10)=2[8jk+jl+kl5(j+k)+6l10]

ds(10,14)=4[jl+kl+j+k+2l6]

ds(10,15)=4[4jk3(j+k)+2]

ds(11,9)=4[j+k2]

ds(11,10)=4(j+k2)(l2)

ds(11,14)=4(j+k2)(l1)

ds(11,15)=4(j+k2)(l1)

ds(14,14)=2[jl+kl+2l4]

ds(14,16)=4l[j+k2]

ds(15,15)=2[8jk+jl+kl5(j+k)2l+2]

ds(15,16)=4[4jk+2(jl+kl)7(j+k)4l+10]

ds(16,16)=2[24jkl28jk19(jl+kl)+23(j+k)+14l18]

Now let us obtain the molecular topological indices using Equation 1, and the estimated bond degree and bond degree sum partition are obtained from the above-listed partitions. The results of the zeolite AWW(j,k,l) are shown in Theorems 3.1, 3.2.

Since the results from Theorem 3.2 are applicable for j,k,l2, we present the neighborhood degree sum-based bond partitions of two-dimensional zeolite AWW, i.e., l=1 and j,k1.

Bond degree-sum partitions (when l=1 and j,k1):

ds(9,9)=10(j+k)+28

ds(14,14)=2(j+k)4

ds(10,10)=4(j+k)+16(j1)(k1)8

ds(10,14)=8(j+k)16

ds(10,15)=4(j+k)+16(j1)(k1)8

ds(14,15)=4(j+k)8

ds(9,10)=16(j+k)32

ds(15,15)=4(j+k)+24(j1)(k1)8

By using the same procedure and the above-listed partitions, we can calculate the neighborhood degree sum-based indices of two-dimensional zeolite AWW.

Theorem 3.1. Let G denote the AWW(j,k,l) zeolite framework, j,k,l1. Then, the degree-form molecular topological descriptors are

1. M1d(G)=384jkl+16jk56jl56kl

2. M2d(G)=768jkl48jk154(jl+kl)+8(j+k)+4l

3. Rd(G)=12jkl+3.95213548685034jk0.0358983848622456(jl+kl)+0.0478645131496611(j+k)+0.0239322565748306l

4. ABCd(G)=29.3938769133981jkl+6.29768379985404jk1.72622689289264(jl+kl)0.0956427709867551(j+k)0.0478213854933776l

5. Hd(G)=14201050jkl+140jk15(jl+kl)+26(j+k)+20l

6. SCd(G)=16.9705627484771jkl+4.09412284133087jk0.793111174158119(jl+kl)+0.0469818803094588(j+k)+0.0234909401547294l

7. HMd(G)=3072jkl176jk604(jl+kl)+16(j+k)+8l

8. GAd(G)=48jkl+7.83589309777259jk4.12308017667056(jl+kl)+0.16410690222741(j+k)+0.0820534511137048l

9. irrd(G)=σd(G)=16jk+12(jl+kl)16(j+k)8l

10. Fd(G)=1536jkl80jk296(jl+kl)

11. SDDd(G)=16120jkl+12jk9(jl+kl)5(j+k)4l

12. AZd(G)=15400010240000jkl2368000jk2689024(jl+kl)+555008(j+k)+584407l

13. SOd(G)=271.529003975634jkl+12.1177490060914jk38.9949493661167(jl+kl)0.804040507106677j0.804040507106677k0.402020253553339l

Theorem 3.2. Let G denote the AWW(j,k,l) zeolite framework, j,k,l2. Then, the degree-sum-form molecular topological descriptors are

1. M1ds(G)=1536jkl96jk308(jl+kl)+16(j+k)+8l

2. M2ds(G)=12288jkl2896jk3594(jl+kl)+696(j+k)+308l24

3. Rds(G)=3jkl+1.50585675513967jk+0.238024998461628(jl+kl)+0.140745376492254(j+k)+0.0476253820709413l+0.0199696427492026

4. ABCds(G)=16.431676725155jkl+5.08922741392934jk0.211371474742995(jl+kl)+0.0995211198551319(j+k)+0.0356164974373255l+0.00466120021924266

5. Hds(G)=3jkl+1.4789247311828jk+0.225964197093229(jl+kl)+0.159886990014324(j+k)+0.0528335105754461l+0.0251943547868845

6. SCds(G)=8.48528137423857jkl+2.67308563317728jk0.0862161391140532(jl+kl)+0.131697210934123(j+k)+0.0427038837370124l+0.0178547409567882

7. HMds(G)=49152jkl11168jk14184(jl+l)+2440(j+k)+1104l64

8. GAds(G)=48jkl+7.66840752524941jk4.15007191255512(jl+kl)+0.2499927179825(j+k)+0.0763565800425527l+0.0332182510198214

9. irrds(G)=96jk+64(jl+kl)88(j+k)64l+32

10. σds(G)=416jk+192(jl+kl)344(j+k)128l+32

11. Fds(G)=24576jkl5376jk6996(jl+kl)+1048(j+k)+488l16

12. SDDds(G)=96jkl+18.7333333333333jk6.78008658008658(jl+kl)2.05894660894661(j+k)0.611255411255411l0.266233766233766

13. AZds(G)=29826.1617777778jkl10244.258617031jk10484.839762917(jl+kl)+3201.8324609039(j+k)+1437.40740464836l261.075052832933

14. SOds(G)=1086.11601590254jkl62.0984297085552jk215.133170624545(jl+kl)+6.72793994101937(j+k)+4.0908228573993l0.0601654666833156

For computing the degree and degree sum-type multiplicative self-powered molecular descriptors of the AWW zeolite, Equations 5, 6 were employed to generate the corresponding indices using the listed bond degree and bond degree sum partitions. For instance, the analytical expression for degree-based self-powered sum connectivity index is

Tdŝ*G=Td33Td33d3,3×Td34Td34d3,4×Td44Td44d4,4Tdŝ*G=1558910783423325225179981368524828jk+3jl+kl+4j+k+2l×779568926258033112589990684262444jk+3jl+kl4j+k2l×390508353708945562949953421312224jkl12jk11jl+kl+4j+k+2l.

Furthermore, the information entropy measures multiplicative self-powered for bond additive degree, and bond additive degree sum topological indices are easily obtained using Equation 9.

4 Determining molecular interaction energies of AWW zeolite through entropy measures

4.1 Degree and degree sum-type information and spectral entropies

This section summarizes the information entropy of AWW zeolite and suggests possible development using the degree, degree sum-based information, and spectral entropies of Equations 8, 11 by assessing the mineral complexity given in Tables 1, 2. It can be very useful for selected dimensions for training in an attempt to analyze the information entropies for larger complex molecules. For all entropy measures, the IETd values are consistently higher than the IETds values, indicating that IETds incorporates more detailed structural aspects of the system, as shown in Table 1. Different entropy measures increase at different rates as j increases. Some information entropy measures are distributed unequally for each layer of AWW zeolite frameworks, except the geometric arithmetic degree and degree sum-based information entropy compared to others. Only the geometric arithmetic information entropy has a significant level of discrimination among all the measured information entropies. Geometric arithmetic entropy is more effective in discriminating the structural complexity because it integrates both local and global structural information, balances contributions across the framework, and is highly sensitive to connectivity variations. On the other hand, the discriminatory power is low for the second Zagreb, harmonic, and forgotten information entropies. This variation indicates that each measure might be sensitive to different aspects of structural complexity in the zeolite. In this study, we exclude the irr and sigma entropies as they are indeterminate with respect to bond additive degree and bond additive degree sum-type entropies.

Table 1
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Table 1. Information entropy measures of AWW(j,k,l) zeolite, when j=k=l.

Table 2
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Table 2. Spectral entropy measures of AWW(j,k,l) zeolite, when j=k=l.

The characteristics of the AWW zeolite structure can be studied using the data provided in Table 1. This allows for the investigation of atomic chemical properties, structural complexity, diversity, similarity, modularity, chirality, and molecular structure information in crystal systems. In addition, in this study, degree spectral entropies were measured to assess the structural complexity of zeolite frameworks. The spectral degree-based entropies have the lowest discriminative values compared to degree and degree sum-based information entropies. This implies that spectral entropy focuses on specific modes or energy distributions within the structure rather than the overall disorder. The zero eigenvalue of the zeolite adjacency matrix is indeterminate in the spectral information entropy calculations from Equation 11 as it causes issues in logarithmic terms. To ensure accuracy, the zero eigenvalue must be excluded or addressed through normalization techniques.

Section 4.2 will address the prediction abilities of our measured bond information and spectral entropies obtained from the AWW zeolite structure.

4.2 Predictive model of various entropies with molecular interaction energies of AWW zeolite

Density functional theory (DFT) has limitations in calculating the molecular interaction energies for large AWW zeolite systems due to its high computational costs, difficulty in capturing long-range interactions, and challenges in modeling non-covalent interactions and strongly correlated electron systems. It also struggles with the flexibility of zeolite frameworks and dynamic effects (Cohen et al., 2012). These issues make DFT impractical for application in large zeolite systems, underscoring the need for predictive models like machine learning to efficiently estimate interaction energies, so there is another computational method to calculate the molecular energies of zeolites: force field method. Force-field methods, in contrast, offer an efficient, cost-effective alternative for studying zeolite structures. These methods allow for scalable simulations of large, complex frameworks and can provide insights into time-dependent behaviors such as adsorption, diffusion, and framework flexibility. Although they rely on parameterized potentials and may struggle with modeling larger zeolite structures, force-field methods, when tailored to specific systems, complement experimental data and fill gaps in case of limited experiments, thus playing a crucial role in advancing our understanding of zeolite properties (Dubbeldam et al., 2019; Jaramillo and Auerbach, 1999).

Determining the properties of zeolites experimentally is challenging due to their structural complexity, which includes intricate pore networks, large unit cells, and diverse atomic environments. These challenges are further compounded by the limited crystallinity, structural defects, and difficulties in synthesizing high-quality samples, all of which impede accurate measurements (Price et al., 2021). The unique crystal structure of the AWW zeolite, characterized by intricate cages and novel configurations, exemplifies this complexity and contributes to the limited availability of experimental data. Additionally, zeolite properties are highly sensitive to environmental factors such as temperature and pressure, complicating the reproducibility. Advanced techniques like X-ray diffraction, neutron diffraction, and nuclear magnetic resonance add to the difficulty, given their high costs and time requirements (Van Vreeswijk and Weckhuysen, 2022).

This subsection investigates the entropies of zeolite AWW using both the bond additive and bond additive sum indices. The results are then correlated with the physical properties of zeolites. For force-field calculations, the Molecular Mechanics 3 (MM3) and Universal Force Field (UFF) approaches are employed within the CRYSTAL computing tools. These tools are essential for analyzing the zeolite’s structural and energetic properties, enabling accurate calculation of molecular interaction energies such as (Ees), total energy (Ete), dispersion (Edse), dihedral (Edhd), two-body (E2b), and three-body (E3b), which are associated with various AWW zeolite structures (Dovesi et al., 2005; Palmer, 2015). Consequently, the following Table 3 presents the experimental data calculated for AWW zeolite structures. With the goal of evaluating the measured information entropy’s predictive ability, data were obtained.

Table 3
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Table 3. Molecular interaction energy properties of AWW(j,k,l), when j=k=l.

A detailed exponential fit analysis was performed between the properties provided in Table 3 and the information entropy values to determine the possible molecular energies and construct models for prediction. The AWW zeolite’s bond degree, degree sum, and spectral information entropy are taken into account for developing the following exponential fit prediction model:

P=x0+y0×ez0×IETψ.(12)

where P represented that the potential energies, x0, y0, and z0 are coefficients that significantly fit the exponential curve, and IETψ information entropies of AWW are listed in Table 4. To test the prediction ability of spectral-based information entropy of the AWW zeolite structure, we substitute IEM(Tλd) with IETψ in Equation 12. The exponential models were developed using Equation 12 to establish relationships between the data presented in Tables 13. The established exponential fit model is a good approximation for modeling the information entropy of the zeolite structure as a function of potential energies because the model attained the coefficient of determination (R2) as 0.99.

Table 4
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Table 4. Significant coefficients for exponential fit of entropies with molecular energies.

The exponential model is chosen for it accurately captures the rapid, non-linear growth of entropy as molecular interaction energies increase in large zeolite frameworks. Unlike polynomial models, the exponential model reflects the exponential increase in the complexity and entropy, providing a more accurate and meaningful representation of their relationship, particularly in complex systems where small energy changes lead to significant increases in entropy.

Table 4 presents the significant coefficients for exponential fit of entropies with molecular energies. The proposed model obtained from Table 4 shows that IEM(M2d) could be utilized for forecasting molecular properties such as E2b, Ees, and Ete. The relationship between information entropy and complexity of zeolite AWW demonstrates that increased entropy results in more intricate and flexible zeolite AWW structure. Figure 4 depicts the exponential fit of the measured bond information, spectral entropies, and molecular energies for the zeolite AWW. The topological indices and information entropies were calculated using MATLAB software, and the statistical OriginLab package was used for evaluating the correlations between experimental data and various information entropies.

Figure 4
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Figure 4. Exponential fitting of bond and spectral information entropy with properties of AWW zeolite.

Table 5 presents a comparison between properties and predicted molecular interaction energies for AWW zeolites. The table also highlights consistent trends across different zeolite frameworks, particularly for larger structures, demonstrating the robustness of entropy-based models in capturing complex molecular interactions and effectively predicting energy properties.

Table 5
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Table 5. Comparison of molecular interaction energy values for AWW zeolite using the force-field method and predictive model AWW(j,k,l) for j=k=l.

4.3 Global chemical reactivity descriptors and spectral properties of AWW zeolite

Assessing global chemical reactivity descriptors such as ionization potential (IP), electron affinity (EA), hardness (η), chemical potential (μ), softness (σ), and electrophilicity index (ω) is challenging for complex materials like zeolites due to the computational and experimental requirements, high resource demands, and the impracticality of DFT and quantum mechanical calculations. Studies use global chemical reactivity descriptors to evaluate the electron-attracting ability, negative of electronegativity, reflects the resistance to electron density changes, and molecule’s tendency (Hemelsoet et al., 2007; Yong et al., 2014; Manda et al., 2024; Gázquez and Sen, 1993; Pearson, 1988; Padmanabhan et al., 2007). The HOMO (highest occupied molecular orbital) and LUMO (lowest unoccupied molecular orbital) energies are closely related to the ionization potential (IP) and electron affinity (EA) in quantum chemistry (Yin et al., 2021). Therefore, using the HOMO and LUMO energies, several important chemical quantum descriptors can be calculated using the given below equations:

IP=EHOMO,(13)
EA=ELUMO,(14)
η=IPEA2,(15)
μ=IP+EA2,(16)
σ=2η.(17)
ω=μ22η.(18)

In this section, we propose the measurement of the global chemical reactivity descriptors using the eigen values of the zeolite graph as the HOMO–LUMO gap. Therefore, we employ the graph-theoretic approach to compute the HOMO–LUMO gap, which involves modeling the zeolite structure as a graph, constructing adjacency, and calculating the eigenvalues of the zeolite matrix. The difference between the maximum negative and minimum positive eigenvalues of the characteristic polynomial gives the HOMO–LUMO gap, which is a key indicator of the molecule’s electronic properties and reactivity (Arockiaraj et al., 2022a; Fowler and Pisański, 2010; Dias and Guirgis, 2002; Aihara, 1999; Bacalis and Zdetsis, 2009; Mushtaq et al., 2022; Ghosh, 2019).

The HOMO–LUMO gap in the zeolite structure reflects their chemical reactivity. A larger HOMO–LUMO gap typically indicates greater stability and lower chemical reactivity as it requires more energy to excite an electron from the HOMO to the LUMO. Conversely, a smaller gap implies higher chemical reactivity as less energy is needed for electronic transitions, facilitating interactions with adsorbates or reactants (Yin et al., 2021). Furthermore, the spectral properties (SP) of chemical structure such as spectral diameter (SD), graph-energy (GE), and spectral entropy (SGE) (Arockiaraj et al., 2022a; Balasubramanian, 2023b; Balasubramanian, 2023c) are computed using the eigen values of characteristic polynomials for the different AWW zeolites listed in Table 6. The global chemical reactivity descriptors are calculated using Equations 1318, and the summarized values in Table 6 are measured using Python code. One can observe from Table 6 that as the AWW zeolite structure increases, the global descriptors such as hardness, chemical potential, and electrophilicity index decrease. On the other hand, the softness of the AWW zeolite structure is increasing.

Table 6
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Table 6. Spectral properties and global reactivity descriptors of zeolite AWW(j,k,l).

Table 7 presents molecular energy properties of various AWW zeolite structures, serving as a benchmark to validate predictive models developed using the measured spectral values of AWW zeolite. It establishes a critical link between computed molecular energies and spectral values, demonstrating the reliability of theoretical calculations in predicting energy properties. The table also highlights how structural variations in zeolites influence energy behavior, emphasizing the practical utility of spectral and entropy-based analyses in evaluating the stability and reactivity.

Table 7
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Table 7. Molecular interaction energies of various AWW zeolites.

The data in Table 8 summarize the significant coefficients of the developed polynomial fit Equation 19. By using the molecular energies and spectral values of zeolite AWW listed in Tables 6, 7, the models demonstrate their effectiveness in predicting potential energies, as evidenced by the high R2 values, which indicate strong relationships.

P=a+bSP+cSP2.(19)

where P, a, b, and c represent the property and coefficients of the models, and SP denotes the spectral properties of the AWW zeolite structures.

Table 8
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Table 8. Significant coefficients for polynomial fit of spectral properties with molecular energies.

Figure 5 highlights the polynomial fitting of spectral values with AWW zeolite properties, demonstrating a strong correlation between spectral entropy and molecular characteristics. The model shows high accuracy, validating the use of spectral properties for predicting molecular energies.

Figure 5
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Figure 5. Polynomial fitting of spectral values with properties of AWW zeolites.

The obtained data, such as the HOMO–LUMO gap and spectral information entropy, directly relate to the applications of AWW zeolites. A smaller HOMO–LUMO gap suggests higher reactivity, enhancing catalytic activity, while spectral information entropy reflects the structural complexity, influencing adsorption capacity through pore connectivity and active site diversity. These comparisons contextualize the findings, linking structural properties to their functional performance in industrial applications.

5 Conclusion

Predicting the characteristics of complicated multicomponent zeolite materials and extremely high-molecular weight systems of molecules is an essential step in the development of QSPR advances in technology. We have developed the degree-sum-based molecular descriptors for zeolite AWW, analyzing three information entropies obtained from topological indices and their spectral aspects. Furthermore, we proposed the exponential regression and polynomial models to predict its potential energies using the computed information measures. The eigenvalue difference approximation of the HOMO–LUMO gap reduces computational demands compared to more complex DFT calculations, enabling faster reactivity predictions in large systems or high-throughput screening. The results of the present investigation illustrate the usefulness and efficacy of the quantitative structure–property relationship approach for the prediction of an extensive variety of properties of the zeolite material.

Data availability statement

The raw data supporting the conclusions of this article will be made available by the authors, without undue reservation.

Author contributions

PP: investigation, methodology, software, validation, and writing–original draft. JC: conceptualization, formal analysis, resources, supervision, validation, and writing–review and editing. MA: formal analysis, supervision, validation, and writing–review and editing. KJ: formal analysis, investigation, methodology, visualization, and writing–original draft.

Funding

The author(s) declare that no financial support was received for the research, authorship, and/or publication of this article.

Conflict of interest

The authors declare that the research was conducted in the absence of any commercial or financial relationships that could be construed as a potential conflict of interest.

The author(s) declared that they were an editorial board member of Frontiers, at the time of submission. This had no impact on the peer review process and the final decision.

Generative AI statement

The author(s) declare that no Generative AI was used in the creation of this manuscript.

Publisher’s note

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Keywords: degree indices, information entropy, eigenvalue, spectral entropy, HOMO–LUMO gap, global reactivity descriptors, AWW zeolite

Citation: Peter P, Clement J, Arockiaraj M and Jacob K (2025) Predictive modeling of molecular interaction energies using topological and spectral entropies of zeolite AWW. Front. Chem. 13:1543588. doi: 10.3389/fchem.2025.1543588

Received: 11 December 2024; Accepted: 04 February 2025;
Published: 18 March 2025.

Edited by:

Eugeny Alexandrov, Samara State Medical University, Russia

Reviewed by:

Adnan Aslam, University of Engineering and Technology, Lahore, Pakistan
Shahid Zaman, University of Sialkot, Pakistan
Muhammad Kamran, Shenzhen University, China

Copyright © 2025 Peter, Clement, Arockiaraj and Jacob. This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) and the copyright owner(s) are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms.

*Correspondence: Joseph Clement, Y2xlbWVudGptYWlsQGdtYWlsLmNvbQ==

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