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Thermal Behavior of Oil Shale Pyrolysis under Low-Temperature Co-Current Oxidizing Conditions.

作者信息

Guo Wei, Yang Qinchuan, Zhang Xu, Xu Shaotao, Deng Sunhua, Li Qiang

机构信息

College of Construction Engineering, Jilin University, Changchun 130021, China.

National-Local Joint Engineering Laboratory of In-situ Conversion, Drilling and Exploitation Technology for Oil Shale, Jilin University, Changchun 130021, China.

出版信息

ACS Omega. 2021 Jul 7;6(28):18074-18083. doi: 10.1021/acsomega.1c01875. eCollection 2021 Jul 20.

DOI:10.1021/acsomega.1c01875
PMID:34308041
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC8296611/
Abstract

The thermal behavior of the Huadian oil shale during low-temperature co-current oxidizing pyrolysis was studied by lab-scale experiments under different basic pyrolysis temperatures and input gas flow rates. The results showed that, in the process of oil shale co-current oxidizing pyrolysis, the increasing input gas flow rates under the same basic pyrolysis temperatures can significantly enhance the heat generation of oil shale. Meanwhile, it can be seen from the temperature variation characteristics of oil shale that the heat released by the oxidation reaction of semicoke and oxygen is enough to support the thermal decomposition of organic matter without supplemental heating. Moreover, it can be concluded from the 92.06% effective recovery of shale oil that a high yield of oil without a significant loss can be achieved. Finally, compared with increasing basic pyrolysis temperatures, the increased input gas flow rates have a more obvious effect on improving the effective recovery of shale oil.

摘要
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8495/8296611/2788016804c2/ao1c01875_0008.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8495/8296611/efca00991ee2/ao1c01875_0002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8495/8296611/b6d5a4d37d6a/ao1c01875_0003.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8495/8296611/158c668982f1/ao1c01875_0004.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8495/8296611/70e9ad298e63/ao1c01875_0005.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8495/8296611/75dfb9a2c8f3/ao1c01875_0006.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8495/8296611/d787ac65fa59/ao1c01875_0007.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8495/8296611/2788016804c2/ao1c01875_0008.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8495/8296611/efca00991ee2/ao1c01875_0002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8495/8296611/b6d5a4d37d6a/ao1c01875_0003.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8495/8296611/158c668982f1/ao1c01875_0004.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8495/8296611/70e9ad298e63/ao1c01875_0005.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8495/8296611/75dfb9a2c8f3/ao1c01875_0006.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8495/8296611/d787ac65fa59/ao1c01875_0007.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8495/8296611/2788016804c2/ao1c01875_0008.jpg

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