共查询到19条相似文献,搜索用时 170 毫秒
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不同变质煤热解和气化中燃料氮的转化规律 总被引:1,自引:0,他引:1
利用水平管式炉对不同变质程度煤进行了热解和气化实验,并利用傅里叶红外气体分析仪对热解和气化过程中主要含氮产物的释放规律进行了研究.结果发现,煤的变质程度对煤热解和气化过程中HCN的释放具有重要影响,而对NH3的释放影响较小.对于低变质程度煤来说,挥发分含量较高,而挥发分的深度裂解是HCN产生的主要来源.因此,低变质程度煤热解过程中转化为HCN的燃料氮份额高于高变质程度煤;对于不同变质程度煤在热解过程中转化为NH3的燃料氮份额则大致相当.对不同变质程度煤在CO2气氛条件下气化反应过程中含氮产物生成规律的研究发现,焦炭氮几乎全部转化为NO;转化为NH3的燃料氮份额有所增加;除印尼褐煤外,转化为HCN的燃料氮份额也有所增加;此外,对CO2气化过程中NO的生成机理进行分析,认为焦炭氮的直接氧化可能是NO产生的主要来源. 相似文献
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含钠煤热解过程中NH_3的形成和释放 总被引:1,自引:0,他引:1
以3种煤及其相应的不同含量的加钠煤作为研究对象,考察了外加金属钠在热解过程中影响NH3生成与释放的主要因素。结果表明:外加钠在热解过程中对NH3释放的作用较大程度上取决于煤的变质程度,变质程度越低的煤影响越明显。在不同温度范围内,Na的负载量不同,对NH3的释放所起的作用也不相同。在600~800℃温度范围内,2%的钠负载量对小龙潭和神东煤NH3的形成起促进作用。当温度达到900℃时,随着添加剂量的增加,钠对NH3的形成表现为抑制趋势。 相似文献
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煤中氮在热解过程中释放规律的数学模拟 总被引:1,自引:1,他引:1
以化学渗透模型(CPD)为基础构建煤的结构,以实验数据为基础,通过对煤中氮在热解阶段反应历程的描述,以及对NOx的主要前驱体HCN和NH3生成的动力学表达,建立了煤热解阶段氮释放的模型,将模型的计算结果与五种煤在管式固定床反应器中热解阶段形成HCN和NHx的测定结果进行比较,研究发现:模型能够相对准确的预测HCN形成(误差在20%以内),但由于没有考虑惰质组的影响,对部分煤NHx的模拟误差较大(甚至超过50%),模型也表达出在快速热解条件下随温度升高,HCN和NHx的生成量增加;随煤阶增加,HCN生成量减少;随惰质组含量增加,NHx的生成量增加的释放规律。 相似文献
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矿物质对煤转化过程中含氮物迁移的影响 总被引:2,自引:1,他引:2
综述了煤本身所固有的矿物质和外来添加物在煤热解、气化过程中的作用,主要针对煤中氮的形态变化和迁移规律进行了讨论.煤中的含氮物在热解气化过程中以HCN、NH3 N2等形式释放于气相产物之中,还是以大分子杂环化合物形式残留于煤焦和焦油之中,煤中固有的矿物质和添加剂对其在各形态间的分配比例具有较大影响.含Fe、Ca等金属元素的化合物是对含氮物迁移转化存在明显作用的代表性物质,同时对Fe、Ca在煤氮催化转化生成N2中的可能机理和在氮氧化物形成之前进行其前驱体的抑制进行了分析. 相似文献
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煤及其模型化合物快速热解过程中HCN和NH3逸出规律的研究 总被引:2,自引:0,他引:2
利用高频热解装置对褐煤、烟煤和无烟煤三种不同煤阶的煤及模型化合物吡咯、吡啶进行了热解实验,分别考察了煤热解终温为1200℃,平均升温速率为2.7,8.0,11.9,17.1,22.9℃·s-1和不同热解终温(600~1200℃)下煤及吡咯、吡啶快速热解过程中HCN和NH3的生成规律,并且对煤热解过程中HCN和NH3逸出... 相似文献
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《Fuel Processing Technology》2005,86(7):739-756
Pyrolysis of 11 coals with carbon contents of 77–93 wt.% (daf) and corresponding demineralized samples has been studied in a fixed bed quartz reactor with a heating rate of 20 K/min to examine rank, demineralization, temperature and inherent mineral species dependences of nitrogen distribution. Nitrogen mass balances fall within 92.5–104.6%. The results indicate that the chars derived from the coals with higher rank show larger nitrogen retention. Demineralization suppresses volatile nitrogen emission during coal pyrolysis, especially for low rank coals. Coal-N conversion to tar-N reaches the asymptotic values at 600 °C. HCN yields are lower than NH3 yields during coal pyrolysis. The trends in HCN and NH3 emissions are very similar and the yields reach the asymptotic value at about 1200 °C. N2 starts emitting at 600 °C, and as the temperature increases the conversion increases linearly with a corresponding reverse change of char-N. With the catalysts added, N2 formation is prompted with the sequence of Fe>Ca>K>Ti≫Na≫Si≈Al, meanwhile, char-N decreases correspondingly. Fe, Ca, K, Na, Si and Al increase coal-N conversion to NH3 with the sequence of Fe>Ca>K≈Na≫Si≈Al in the pyrolysis. Na addition prompts HCN formation; however, the presence of Ti and Ca decrease the HCN yields with small value. The other catalysts have no notable influence on HCN emission in the pyrolysis. Demineralization and Ti addition increase coal-N conversion to tar-N slightly whereas K, Ca, Mg, Na, Si and Al additions decrease tar-N yield weakly, other catalysts hardly influence tar nitrogen emission. N2 emits mainly from char-N with slight contribution of volatile nitrogen. The mechanism of different N-containing species formation and catalysts influence in the pyrolysis is also discussed in the paper. 相似文献
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《Fuel》2005,84(2-3):271-277
Three coal macerals with high purities were separated from Pingshuo gas coal. The formation rules of HCN and NH3 during macerals pyrolysis and gasification were investigated. Experiments were carried out in a tubular quartz reactor at atmospheric pressure. The reactor allowed coal particles to be heated up rapidly and held for a prespecified period of time at a peak temperature. The amount of HCN and NH3 were quantified by ion chromatography. The influence of temperature and macerals type on the formation rules of HCN and NH3 was discussed. Results showed that the formation of HCN was mainly due to the thermal cracking of volatile, and NH3 formed both from the thermal cracking of volatile and the cracking of nascent char. The HCN yield increased with an increase in pyrolysis temperature. For three coal macerals (liptinite, vitrinite and inertinite), the yield of HCN depended not only on their volatile contents but also nitrogen-containing functional groups, in which more pyrrole-type nitrogens would form more amount of HCN at lower temperature. The yield of NH3 depended on the ability of forming ‘H’ radical. Under the experiment condition in this study, inertinite could convert more nitrogen into NH3 than vitrinite and liptinite. The yield of HCN during gasification was almost the same as that during pyrolysis, the yield of NH3 during gasification was little higher than that during pyrolysis. 相似文献
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利用微型流化床反应装置,结合快速过程质谱仪,在850~940℃操作温度下,研究了三种不同粒度分布烟煤和无烟煤在热解、气化和燃烧反应条件下四种主要气态氮产物HCN、NH3、NO和NO2的释放规律。结果表明,微型流化床可以实时检测挥发分氮和焦炭氮的动态释放序和类型,热解、气化和燃烧反应气氛的改变主要影响HCN和NH3的释放量。热解产物的气态氮主要是来自于挥发分,燃烧反应的HCN和NH3的释放量与温度有明显关系,而气化反应的各类气态氮释放量随温度变化波动不大。煤颗粒尺寸和温度变化对烟煤和无烟煤中各类气态氮释放量产生影响比较复杂,其中NH3的释放特性是区分挥发分N释放和半焦N释放的重要特征。 相似文献
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The present review focuses on elucidating the chemistry of nitrogen release during coal pyrolysis, in particular, on making clear catalytic roles of inherent Ca and Fe ions in not only the partitioning of volatile-N to tar-N, HCN, NH3 and N2 but also the conversion of char-N to N2. 相似文献
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The formation of HCN and NH3 during the pyrolysis of a biomass (bagasse) and a set of rank-ordered coal samples has been studied in a novel reactor. The reactor has some features of both a drop-tube reactor and a fixed-bed reactor: the reactor allows the coal/biomass particles to be heated up rapidly as well as to be held for a pre-specified period of time at peak temperature. The experimental results obtained suggest that a considerable amount of the nitrogen in the nascent char could be converted into HCN and NH3 if the char is held at high temperatures for long time. The formation of NH3 from the thermal cracking of char was seen to last for more than an hour even at temperatures as high as 700–900°C. The formation of HCN went to completion much more rapidly than that of NH3. Compared with the results in the literature from the pyrolysis of coals in a fluidised-bed reactor, the reactor configuration used in this study allows the effects of fuel rank to be studied on an unbiased basis towards the type of fuel. The yields of HCN and NH3 from the present study decrease with increasing rank. The experimental results suggest that the differences in reactor configurations used by various researchers would account at least partially for some of the discrepancies in the literature regarding the formation of HCN and NH3 during the pyrolysis of coals. 相似文献
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提出一种简化的Solomon热解模型, 用于模拟煤粉燃烧NO生成数值模拟中HCN的释放.用纯双流体模型、k-ε-kp两相湍流模型、EBU-Arrhenius燃烧模型、六热流辐射模型、双方程热解模型、简化的Solomon热解模型以及NO生成湍流反应二阶矩代数模型对旋流煤粉燃烧器内两相流动、煤粉燃烧、HCN释放以及NO生成进行了数值模拟.模拟结果与文献中实验结果的对比表明,基于简化Solomon热解模型的HCN释放模型预报结果比基于双方程热解模型的HCN释放模型预报结果好. 相似文献
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《Fuel Processing Technology》2006,87(4):355-362
Experiments have been carried out to investigate the emissions of nitrogen species including NO and its precursors during temperature-programmed coal combustion by TG/EGA method. Experimental results show that the conversion ratio of fuel nitrogen to NO is the highest, followed by that of fuel nitrogen to HCN and the conversion ratio to NH3 is negligibly small. Nitrogen is retained in the char and released mainly as NO at the later stages of coal combustion. HCN and NO are both primary products from coal char oxidation. Coal rank, heating rate, indigenous minerals and external additives are the major influential factors of the nitrogen species release. Higher rank coals with higher fuel ratio have higher NO releases. HCN release decreases as fuel ratio increases for most coals. The fuel nitrogen conversion to NO increases and the fuel nitrogen conversion to HCN decreases with the increase of heating rate, which may imply that the char nitrogen prefers to react with oxygen to form NO instead of HCN while coal char is combusted at higher temperatures. Different metallic additives show different effects on nitrogen species emission and the effects of indigenous minerals on nitrogen release can be qualitatively estimated by ash analyses. 相似文献