Edwing Javier Grajales-González, Adri C. T. van Duin, Subram Mani Sarathy
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Methanol conversion increases from 800 to 1000 K to form water and the crucial intermediate surface methoxy species (SMS), whose production diminishes at 1200 K because of the prevalence of the undesired methane. Generally, temperatures above 1200 K can lead to questionable reactions due to entropy effects. Humidity at 800 K modifies the nature of the zeolite acidity from static to dynamic embodied in hydronium ions, which enhances methanol conversion via hydrogen transfer reactions and framework activation, namely, water protonation leaves a negatively charged framework that eventually facilitates the dissociation of protonated methanol in water and an SMS. Cation diffusion was pervasive, and it is hypothesized that this relieves entropic penalties of several relevant reactions. This phenomenon showcases a critical manifestation of dynamic effects that complements experimental and theoretical research mainly conducted by static density functional theory methods. Overall, dynamic effects involving diffusing cations and modification of the zeolite interior by water are complex and call for more extensive investigations.","PeriodicalId":99,"journal":{"name":"Physical Chemistry Chemical Physics","volume":"24 1","pages":""},"PeriodicalIF":2.9000,"publicationDate":"2025-10-08","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Methanol-to-Hydrocarbon Initiation Reactions over a Zeolite Catalyst: Reactive Molecular Dynamics Simulations\",\"authors\":\"Edwing Javier Grajales-González, Adri C. T. van Duin, Subram Mani Sarathy\",\"doi\":\"10.1039/d5cp02704g\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Environmental concerns and energy security drive the need for renewable alternatives to fossil fuels. Methanol is an ideal candidate as it enables the synthesis of olefins and fuels from biomass using zeolite-catalyzed processes, which inspired the concept of \\\"The Methanol Economy\\\" since it implies an oil-dependent scenario. Although MTH industrial units already exist, many fundamental aspects remain unknown. Therefore, in this contribution, we developed a ReaxFF reactive force field to study the dynamic features of MTH processes in an H-ZSM-5 zeolite. Simulations were run from 600 to 1200 K during 1000 ps, using a constant number of molecules, pressure, and temperature (NPT ensemble). Methanol conversion increases from 800 to 1000 K to form water and the crucial intermediate surface methoxy species (SMS), whose production diminishes at 1200 K because of the prevalence of the undesired methane. Generally, temperatures above 1200 K can lead to questionable reactions due to entropy effects. Humidity at 800 K modifies the nature of the zeolite acidity from static to dynamic embodied in hydronium ions, which enhances methanol conversion via hydrogen transfer reactions and framework activation, namely, water protonation leaves a negatively charged framework that eventually facilitates the dissociation of protonated methanol in water and an SMS. Cation diffusion was pervasive, and it is hypothesized that this relieves entropic penalties of several relevant reactions. This phenomenon showcases a critical manifestation of dynamic effects that complements experimental and theoretical research mainly conducted by static density functional theory methods. Overall, dynamic effects involving diffusing cations and modification of the zeolite interior by water are complex and call for more extensive investigations.\",\"PeriodicalId\":99,\"journal\":{\"name\":\"Physical Chemistry Chemical Physics\",\"volume\":\"24 1\",\"pages\":\"\"},\"PeriodicalIF\":2.9000,\"publicationDate\":\"2025-10-08\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Physical Chemistry Chemical Physics\",\"FirstCategoryId\":\"92\",\"ListUrlMain\":\"https://doi.org/10.1039/d5cp02704g\",\"RegionNum\":3,\"RegionCategory\":\"化学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q3\",\"JCRName\":\"CHEMISTRY, PHYSICAL\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Physical Chemistry Chemical Physics","FirstCategoryId":"92","ListUrlMain":"https://doi.org/10.1039/d5cp02704g","RegionNum":3,"RegionCategory":"化学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q3","JCRName":"CHEMISTRY, PHYSICAL","Score":null,"Total":0}
Methanol-to-Hydrocarbon Initiation Reactions over a Zeolite Catalyst: Reactive Molecular Dynamics Simulations
Environmental concerns and energy security drive the need for renewable alternatives to fossil fuels. Methanol is an ideal candidate as it enables the synthesis of olefins and fuels from biomass using zeolite-catalyzed processes, which inspired the concept of "The Methanol Economy" since it implies an oil-dependent scenario. Although MTH industrial units already exist, many fundamental aspects remain unknown. Therefore, in this contribution, we developed a ReaxFF reactive force field to study the dynamic features of MTH processes in an H-ZSM-5 zeolite. Simulations were run from 600 to 1200 K during 1000 ps, using a constant number of molecules, pressure, and temperature (NPT ensemble). Methanol conversion increases from 800 to 1000 K to form water and the crucial intermediate surface methoxy species (SMS), whose production diminishes at 1200 K because of the prevalence of the undesired methane. Generally, temperatures above 1200 K can lead to questionable reactions due to entropy effects. Humidity at 800 K modifies the nature of the zeolite acidity from static to dynamic embodied in hydronium ions, which enhances methanol conversion via hydrogen transfer reactions and framework activation, namely, water protonation leaves a negatively charged framework that eventually facilitates the dissociation of protonated methanol in water and an SMS. Cation diffusion was pervasive, and it is hypothesized that this relieves entropic penalties of several relevant reactions. This phenomenon showcases a critical manifestation of dynamic effects that complements experimental and theoretical research mainly conducted by static density functional theory methods. Overall, dynamic effects involving diffusing cations and modification of the zeolite interior by water are complex and call for more extensive investigations.
期刊介绍:
Physical Chemistry Chemical Physics (PCCP) is an international journal co-owned by 19 physical chemistry and physics societies from around the world. This journal publishes original, cutting-edge research in physical chemistry, chemical physics and biophysical chemistry. To be suitable for publication in PCCP, articles must include significant innovation and/or insight into physical chemistry; this is the most important criterion that reviewers and Editors will judge against when evaluating submissions.
The journal has a broad scope and welcomes contributions spanning experiment, theory, computation and data science. Topical coverage includes spectroscopy, dynamics, kinetics, statistical mechanics, thermodynamics, electrochemistry, catalysis, surface science, quantum mechanics, quantum computing and machine learning. Interdisciplinary research areas such as polymers and soft matter, materials, nanoscience, energy, surfaces/interfaces, and biophysical chemistry are welcomed if they demonstrate significant innovation and/or insight into physical chemistry. Joined experimental/theoretical studies are particularly appreciated when complementary and based on up-to-date approaches.