Evolutionary nonlinear chemistry of self-organizing mesophase (liquid crystal) structures of wood: from morphogenesis to regulation of carbon formation (review)

O. Gradov
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Abstract

This work reconstructs the transformation stages of the mesophase (liquid crystal) wood components from their native state to the processes of coke and coal formation. The phytochemical precursors of mesophases (from lignin and polysaccharides, such as cellulose, to lipids) differing in their cell localization are considered separately. Several criteria are listed by which the similarity between the processes of mesophase formation based on the plant raw materials during carbon formation and self-organization in such systems (including the processes proceeding under the thermal pumping) is observed. The role of membrane and membrane-mimetic interfaces in regulation of the above processes is indicated. The applicability of biogeochemical redox criteria (anaerobic, subaerial, aerobic modes) in the analysis of mesophase diagenesis is considered. It is postulated that, due to the specific regulation/feedback, the above factors can lead to the spatial heterogeneity during coal formation, «autocatalytic» effects and the emergence of redox oscillations, accompanied by the localized changes in the properties of mesophases - from those supporting combustion to practically fire retardant. Based on the dependence of the main properties of the corresponding products on the processes of their production and / or formation, as well as their (geo) chemical environment (which is characteristic of supramolecular and colloidal chemistry), it is possible to formulate supramolecular and colloidal chemical approaches to the interpretation of a number of phenomena and mechanisms of the biogenic fossil mesophase formation, which requires consideration in a separate review paper.
木材自组织中间相(液晶)结构的演化非线性化学:从形态发生到碳形成调控(综述)
本研究重建了中间相(液晶)木材组分从其原生状态到焦炭和煤形成过程的转变阶段。中间期的植物化学前体(从木质素和多糖,如纤维素,到脂质)在细胞定位上的不同被分开考虑。列出了几个标准,通过这些标准可以观察到在碳形成过程中基于植物原料的中间相形成过程与这种系统中的自组织过程(包括在热泵下进行的过程)之间的相似性。指出了膜和模拟膜界面在上述过程中的调节作用。探讨了生物地球化学氧化还原标准(厌氧、陆上、好氧模式)在中相成岩作用分析中的适用性。假设,由于特定的调节/反馈,上述因素可能导致煤形成过程中的空间异质性,“自催化”效应和氧化还原振荡的出现,伴随着中间相性质的局部变化-从支持燃烧到实际阻燃。基于相应产物的主要性质对其生产和/或形成过程的依赖性,以及它们的(地球)化学环境(具有超分子和胶体化学的特征),有可能制定超分子和胶体化学方法来解释生物成因化石中间期形成的一些现象和机制,这需要在单独的综述论文中考虑。
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