Phase-evolving inorganic mineral matrices for product-selective pyrolysis of biomass-rich organic solid wastes

Product formation during pyrolysis of biomass-rich organic solid wastes is usually interpreted through temperature, residence time, and reactor configuration, while inorganic mineral matrices are considered less consistently. This review develops an interpretive phase-evolution framework that links the initial mineral assemblage and its condition-dependent transformation to surface functions accessible to pyrolysis vapors and the resulting product responses. Here, product selectivity is used at two distinct levels: partitioning among liquid, gas, and char, and preferential distribution of a defined product family or component within one phase. Relative compositional enrichment is not equated with an increase in absolute yield. Ca-bearing and related alkaline-earth matrices, waste-derived multi-oxide residues, natural minerals, and transition-metal oxides are compared in terms of phase transformation, accessible acid base and redox sites, pore structure, and vapor-solid contact. Representative studies associate Ca-bearing matrices with reported decreases in acidic oxygenates and shifts in gas composition toward H 2 -, CO-, and CH 4 -rich products; these responses are consistent with basic deoxygenation, cracking, and carbonate–oxide chemistry. For N-rich feedstocks, however, nitrogen partitioning among NH 3 /HCN, oil-phase N-containing compounds, and char-N needs to be evaluated independently of deoxygenation. Studies of red mud and steel slag further report oxygenated-vapor restructuring and atmosphere-dependent carbon redistribution within mixed-oxide environments. Natural minerals and transition-metal oxides further show that calcination history and oxide identity affect phenolic, aromatic, and gas-oriented responses. Mineral-assisted pyrolysis should therefore be assessed by phase evolution, accessible surface function, product-family response, matrix lifetime, and spent-solid safety rather than nominal composition or precursor cost alone.

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Publication Details

Journal
Biomass and Bioenergy
Published
2026-09-21
DOI
https://doi.org/10.1016/j.biombioe.2026.110107
Primary Topic
Thermochemical Biomass Conversion Processes
Type
article
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article

Phase-evolving inorganic mineral matrices for product-selective pyrolysis of biomass-rich organic solid wastes

Li‐Wei Chen, Di Liu, Yang Cai, Bin Kuang et al.
Biomass and Bioenergy
Thermochemical Biomass Conversion Processes
article

Phase-evolving inorganic mineral matrices for product-selective pyrolysis of biomass-rich organic solid wastes

Li‐Wei Chen, Di Liu, Yang Cai, Bin Kuang, Dahai Zheng
article en

Abstract

Product formation during pyrolysis of biomass-rich organic solid wastes is usually interpreted through temperature, residence time, and reactor configuration, while inorganic mineral matrices are considered less consistently. This review develops an interpretive phase-evolution framework that links the initial mineral assemblage and its condition-dependent transformation to surface functions accessible to pyrolysis vapors and the resulting product responses. Here, product selectivity is used at two distinct levels: partitioning among liquid, gas, and char, and preferential distribution of a defined product family or component within one phase. Relative compositional enrichment is not equated with an increase in absolute yield. Ca-bearing and related alkaline-earth matrices, waste-derived multi-oxide residues, natural minerals, and transition-metal oxides are compared in terms of phase transformation, accessible acid base and redox sites, pore structure, and vapor-solid contact. Representative studies associate Ca-bearing matrices with reported decreases in acidic oxygenates and shifts in gas composition toward H 2 -, CO-, and CH 4 -rich products; these responses are consistent with basic deoxygenation, cracking, and carbonate–oxide chemistry. For N-rich feedstocks, however, nitrogen partitioning among NH 3 /HCN, oil-phase N-containing compounds, and char-N needs to be evaluated independently of deoxygenation. Studies of red mud and steel slag further report oxygenated-vapor restructuring and atmosphere-dependent carbon redistribution within mixed-oxide environments. Natural minerals and transition-metal oxides further show that calcination history and oxide identity affect phenolic, aromatic, and gas-oriented responses. Mineral-assisted pyrolysis should therefore be assessed by phase evolution, accessible surface function, product-family response, matrix lifetime, and spent-solid safety rather than nominal composition or precursor cost alone.

Biomass and BioenergyVol. 217
Qilu University of Technology (CN), Huzhou Normal University (CN), Huzhou College, Qilu Institute of Technology (CN)
Responsible consumption and production
Openalex Percentile: Top 21%
Thermochemical Biomass Conversion Processes
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