煤物质表层的纳米结构

IF 0.2 Q4 GEOLOGY
V. Portnov, V. Yurov, N. Reva, A. Mausymbaeva, S. Imanbaeva
{"title":"煤物质表层的纳米结构","authors":"V. Portnov, V. Yurov, N. Reva, A. Mausymbaeva, S. Imanbaeva","doi":"10.17721/1728-2713.95.07","DOIUrl":null,"url":null,"abstract":"According to modern concepts, the surface layer of compounds is understood as the ultrathin cover, the properties, structure and composition are different from the crystalline substrate with this layer and this layer is in thermodynamic equilibrium. The surface layer consists of two layers - d(I) with thickness h = d, at which the phase transition occurs, and d(II) with the lower limit h≈10d, at which the physical properties of the crystal begin to manifest themselves. The thickness of the surface layer d(I) is determined by one fundamental parameter, the molar (atomic) volume of the element (Ʊ= M/ρ, M is molar mass (g/mol), ρ is density (g/cm3)). The average statistical structural unit of coal corresponds to higher fullerenes with the number of carbon atoms in the cluster >100, which is the unique feature of the coal substance, which is not a crystalline structure, but a complex polymer with a supramolecular structure. The thickness of the surface layer of the coal substance is two orders of magnitude greater than the thickness of pure metals and is close to the thickness of the surface layer of higher fullerenes C96 (135 nm). The increasing of the coal substance's porosity of 90 % is led to increasing the thickness d(I) of the surface layer by the order of magnitude, that is 2 microns. In this regard, the \"apparent\" change in the radius of a coal particle means a change in its mass, proportional to the release of methane from the solid solution. The dependence of the complete decomposition's time of coal methane is τ0 on the parameter |λ|. The equation which is obtained, includes the ratio of the heat flux introduced into the reservoir volume due to the internal heat release process to the heat flux which is carried away from the volume due to thermal conductivity. If this ratio exceeds a certain critical value of the unity's order, the thermal explosion occurs, leading to the decomposition of coal methane. The size effects in the d(I) layer are determined by the entire group of atoms in the system (collective processes). Such \"quasi-classical\" size effects are observed only in nanoparticles and nanostructures. The d(I) layer for coal matter extends from 151.5 nm (Anthracite) to 214.2 nm (Brown). The dimensional temperature of the carbon nanoparticle at the initial temperature T0 = 300 K will be at least Tm = 872 K. This corresponds to particles of the order of half a micron. Coal particles with the radius of about one micron (or marked half a micron) in the case of decomposition of coal matter are heated to temperatures at which spontaneous combustion of nanoparticles is possible. Hygroscopic moisture in the genetic line of coal has the certain pattern of change and correlates with the thickness of their surface layer.","PeriodicalId":42798,"journal":{"name":"Visnyk of Taras Shevchenko National University of Kyiv-Geology","volume":null,"pages":null},"PeriodicalIF":0.2000,"publicationDate":"2021-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"1","resultStr":"{\"title\":\"NANOSTRUCTURES IN THE SURFACE LAYERS OF COAL MATTER\",\"authors\":\"V. Portnov, V. Yurov, N. Reva, A. Mausymbaeva, S. Imanbaeva\",\"doi\":\"10.17721/1728-2713.95.07\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"According to modern concepts, the surface layer of compounds is understood as the ultrathin cover, the properties, structure and composition are different from the crystalline substrate with this layer and this layer is in thermodynamic equilibrium. The surface layer consists of two layers - d(I) with thickness h = d, at which the phase transition occurs, and d(II) with the lower limit h≈10d, at which the physical properties of the crystal begin to manifest themselves. The thickness of the surface layer d(I) is determined by one fundamental parameter, the molar (atomic) volume of the element (Ʊ= M/ρ, M is molar mass (g/mol), ρ is density (g/cm3)). The average statistical structural unit of coal corresponds to higher fullerenes with the number of carbon atoms in the cluster >100, which is the unique feature of the coal substance, which is not a crystalline structure, but a complex polymer with a supramolecular structure. The thickness of the surface layer of the coal substance is two orders of magnitude greater than the thickness of pure metals and is close to the thickness of the surface layer of higher fullerenes C96 (135 nm). The increasing of the coal substance's porosity of 90 % is led to increasing the thickness d(I) of the surface layer by the order of magnitude, that is 2 microns. In this regard, the \\\"apparent\\\" change in the radius of a coal particle means a change in its mass, proportional to the release of methane from the solid solution. The dependence of the complete decomposition's time of coal methane is τ0 on the parameter |λ|. The equation which is obtained, includes the ratio of the heat flux introduced into the reservoir volume due to the internal heat release process to the heat flux which is carried away from the volume due to thermal conductivity. If this ratio exceeds a certain critical value of the unity's order, the thermal explosion occurs, leading to the decomposition of coal methane. The size effects in the d(I) layer are determined by the entire group of atoms in the system (collective processes). Such \\\"quasi-classical\\\" size effects are observed only in nanoparticles and nanostructures. The d(I) layer for coal matter extends from 151.5 nm (Anthracite) to 214.2 nm (Brown). The dimensional temperature of the carbon nanoparticle at the initial temperature T0 = 300 K will be at least Tm = 872 K. This corresponds to particles of the order of half a micron. Coal particles with the radius of about one micron (or marked half a micron) in the case of decomposition of coal matter are heated to temperatures at which spontaneous combustion of nanoparticles is possible. Hygroscopic moisture in the genetic line of coal has the certain pattern of change and correlates with the thickness of their surface layer.\",\"PeriodicalId\":42798,\"journal\":{\"name\":\"Visnyk of Taras Shevchenko National University of Kyiv-Geology\",\"volume\":null,\"pages\":null},\"PeriodicalIF\":0.2000,\"publicationDate\":\"2021-01-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"1\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Visnyk of Taras Shevchenko National University of Kyiv-Geology\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.17721/1728-2713.95.07\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q4\",\"JCRName\":\"GEOLOGY\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Visnyk of Taras Shevchenko National University of Kyiv-Geology","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.17721/1728-2713.95.07","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q4","JCRName":"GEOLOGY","Score":null,"Total":0}
引用次数: 1

摘要

根据现代概念,化合物的表面层被理解为超薄的覆盖层,其性质、结构和组成与晶体基底不同,该层处于热力学平衡状态。表面层由两层组成,厚度为h = d的d(I)层发生相变,下限为h≈10d的d(II)层开始体现晶体的物理性质。表面层的厚度d(I)由一个基本参数决定,即元素的摩尔(原子)体积(Ʊ= M/ρ, M是摩尔质量(g/mol), ρ是密度(g/cm3))。煤的平均统计结构单元对应于团簇中碳原子数>100的更高的富勒烯,这是煤物质的独特特征,它不是晶体结构,而是具有超分子结构的复杂聚合物。煤物质的表面层厚度比纯金属的厚度大两个数量级,接近于高富勒烯C96的表面层厚度(135 nm)。煤质孔隙率增加90%,导致表层厚度d(I)增加了一个数量级,即2 μ m。在这方面,煤颗粒半径的“表观”变化意味着其质量的变化,与固溶体中甲烷的释放成正比。煤甲烷的完全分解时间τ0与参数|λ|有关。所得到的方程包括由于内部放热过程引入储层体积的热流通量与由于导热性而从体积带走的热流通量之比。如果该比值超过某一单位阶的临界值,就会发生热爆炸,导致煤层气分解。d(I)层的尺寸效应是由系统中的整个原子群(集体过程)决定的。这种“准经典”尺寸效应只在纳米粒子和纳米结构中观察到。煤的d(I)层从151.5 nm(无烟煤)延伸到214.2 nm(褐煤)。在初始温度T0 = 300 K时,纳米碳颗粒的尺寸温度至少为Tm = 872 K。这相当于半微米量级的粒子。在煤质分解的情况下,半径约为1微米(或标记为半微米)的煤颗粒被加热到纳米颗粒可能自燃的温度。煤的成因线吸湿性含水率有一定的变化规律,并与煤的表层厚度有关。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
NANOSTRUCTURES IN THE SURFACE LAYERS OF COAL MATTER
According to modern concepts, the surface layer of compounds is understood as the ultrathin cover, the properties, structure and composition are different from the crystalline substrate with this layer and this layer is in thermodynamic equilibrium. The surface layer consists of two layers - d(I) with thickness h = d, at which the phase transition occurs, and d(II) with the lower limit h≈10d, at which the physical properties of the crystal begin to manifest themselves. The thickness of the surface layer d(I) is determined by one fundamental parameter, the molar (atomic) volume of the element (Ʊ= M/ρ, M is molar mass (g/mol), ρ is density (g/cm3)). The average statistical structural unit of coal corresponds to higher fullerenes with the number of carbon atoms in the cluster >100, which is the unique feature of the coal substance, which is not a crystalline structure, but a complex polymer with a supramolecular structure. The thickness of the surface layer of the coal substance is two orders of magnitude greater than the thickness of pure metals and is close to the thickness of the surface layer of higher fullerenes C96 (135 nm). The increasing of the coal substance's porosity of 90 % is led to increasing the thickness d(I) of the surface layer by the order of magnitude, that is 2 microns. In this regard, the "apparent" change in the radius of a coal particle means a change in its mass, proportional to the release of methane from the solid solution. The dependence of the complete decomposition's time of coal methane is τ0 on the parameter |λ|. The equation which is obtained, includes the ratio of the heat flux introduced into the reservoir volume due to the internal heat release process to the heat flux which is carried away from the volume due to thermal conductivity. If this ratio exceeds a certain critical value of the unity's order, the thermal explosion occurs, leading to the decomposition of coal methane. The size effects in the d(I) layer are determined by the entire group of atoms in the system (collective processes). Such "quasi-classical" size effects are observed only in nanoparticles and nanostructures. The d(I) layer for coal matter extends from 151.5 nm (Anthracite) to 214.2 nm (Brown). The dimensional temperature of the carbon nanoparticle at the initial temperature T0 = 300 K will be at least Tm = 872 K. This corresponds to particles of the order of half a micron. Coal particles with the radius of about one micron (or marked half a micron) in the case of decomposition of coal matter are heated to temperatures at which spontaneous combustion of nanoparticles is possible. Hygroscopic moisture in the genetic line of coal has the certain pattern of change and correlates with the thickness of their surface layer.
求助全文
通过发布文献求助,成功后即可免费获取论文全文。 去求助
来源期刊
自引率
66.70%
发文量
0
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
确定
请完成安全验证×
copy
已复制链接
快去分享给好友吧!
我知道了
右上角分享
点击右上角分享
0
联系我们:info@booksci.cn Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。 Copyright © 2023 布克学术 All rights reserved.
京ICP备2023020795号-1
ghs 京公网安备 11010802042870号
Book学术文献互助
Book学术文献互助群
群 号:481959085
Book学术官方微信