油页岩
烷烃
烯烃
反驳
化学
煤
油页岩气
下降(电信)
阶段(地层学)
燃烧
碳氢化合物
页岩油
化学工程
化石燃料
有机化学
废物管理
催化作用
地质学
工程类
古生物学
电信
计算机科学
作者
Wenzhou Du,Yue Wang,Xuelin Liu,Lulu Sun
出处
期刊:Energies
[MDPI AG]
日期:2018-09-29
卷期号:11 (10): 2594-2594
被引量:14
摘要
Oil shale is a kind of high-combustion heat mineral, and its oxidation in mining and storage are worth studying. To investigate the low-temperature oxidation characteristics of oil shale, the temperature, CO, alkane and alkene gases were analyzed using a temperature-programmed device. The results showed that the temperature of oil shale underwent three oxidation stages, namely a slow low-temperature oxidation stage, a rapid temperature-increasing oxidation stage, and a steady temperature-increasing stage. The higher the air supply rate is, the higher the crossing point temperature is. Similar to coal, CO also underwent three stages, namely a slow low-temperature oxidation stage, a rapid oxidation stage, and a steady increase stage. However, unlike coal, alkane and alkene gases produced by oil shale underwent four stages. They all had a concentration reduction stage with the maximum drop of 24.20%. Statistical classification of inflection temperature of various gases as their concentrations change showed that the temperature of 140 °C is the key temperature for group reactions, and above the temperature of 140 °C, all alkane and alkene gases underwent the rapid concentration increase stage.
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