Inter-influence of Temperature-time-reflectivity in the Coal Metamorphism Thermodynamics Equation (CMTE)

Zhang Xuemei; Ma Qinghua; Li Dong; Hao Jingyuan

doi:doi:10.11648/j.ijeee.20210605.16

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Inter-influence of Temperature-time-reflectivity in the Coal Metamorphism Thermodynamics Equation (CMTE)

Zhang Xuemei, Ma Qinghua, Li Dong, Hao Jingyuan

Published in International Journal of Economy, Energy and Environment (Volume 6, Issue 5)

Received: 3 September 2021 Accepted: 15 October 2021 Published: 19 October 2021

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Abstract

The influence and control of time and temperature on coalification are comprehensive. In order to quantitatively analyze the thermal kinetics of coal metamorphosis process by temperature and time, the qualitative analysis of coal metamorphosis thermodynamic equation (CMTE) based on Wu Chonglong was further verified from the mathematical point of view. Wu Chong Long's Coal Metamorphism Thermodynamics Equation (CMTE) is a ternary equation containing coal forming period or metamorphic age (time), metamorphic temperature (temperature) and metamorphic degree (reflectivity). The temperature calculated by fixing time and reflectivity is the lowest theoretical metamorphic temperature. The reflectivity calculated by fixing time and temperature is the maximum theoretical metamorphic degree. The “time-temperature ratio” is defined as the equivalent of extending million years to increasing 1°C temperature regarding coal metamorphism. This ratio is used to compare the impact of extending time or increasing temperature on improving the metamorphic degree and its significance. The results showed that in the same coal forming period, the ratio is decreased with the reflectivity increasing; at the same reflectivity, the ratio decreased with younger coal forming period. At R_o=6.1%, the calculated ratio is 3.67, which means, at R_o=6.1%, increasing 1°C is equaled extending 3.67 million.

Published in	International Journal of Economy, Energy and Environment (Volume 6, Issue 5)
DOI	10.11648/j.ijeee.20210605.16
Page(s)	114-117
Creative Commons	This is an Open Access article, distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution and reproduction in any medium or format, provided the original work is properly cited.
Copyright	Copyright © The Author(s), 2021. Published by Science Publishing Group

Keywords

Coal Metamorphism Thermodynamics Equation, Minimum Metamorphic Temperature, Maximum Metamorphic Degree, Time-temperature Ratio

References

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[2]	Zhang Shuangquan. Coal Chemistry [M]. Xu Zhou: China University of Mining and Technology: 2015.
[3]	Wu Chonglong, Yang Qi, Liu Gang, et al. Principles and methods of thermodynamics for analysis of coal metamorphism [J]. Journal of China Coal Society, 1997, 22 (3): 225-229.
[4]	Yang Qi. A study on coal metamorphism in China [J]. Earth Science-Journal of China University of Geosciences, 1989, 14 (4): 341-345.
[5]	Yang Qi. Superimposed metamorphism of Chinese coal [J]. Earth Science-Journal of China University of Geosciences, 1999, 6 (Z1): 1-8.
[6]	Yang Qi, Wu Chonglong, Tang Dazhen, et al. Coal metamorphism in China [J]. Earth Science-Journal of China University of Geosciences, 1996, 21 (3): 311-319.
[7]	Hood A, Gutjahr C C M, Heacock R H. Organic metamorphism and the generation of petroleum [J]. Bull. AAPG, 1975, 59 (6): 986-996.
[8]	Bostick N H, Cashman S M, McCulloh T H, et al. Gradients of vitrinite reflectance and present temperature in the Los Angeles and Ventura Basins, California. In: Oltz D F, ed. Low temperature metamorphism of kerogen and clay minerals. Los Angeles: Pacific Section, SEPM (Society for Sedimentary Geology), 1979, 65-96.
[9]	Method of determining microscopically the reflectance of vitrinite in coal. GB/T 6948-2008.
[10]	Li Wenhua, Bai Xiangfei, Yang Jinhe, et al. Correspondence between mean maximum reflectance of Vitrinite and classification of bituminous coals [J]. Journal of China Coal Society, 2006, 31 (3): 342-345.
[11]	Classification of coalification degree by vitrinite reflectance. MT/T 1158-2011.
[12]	Xuemei Zhang, Dong Li, Qinghua Ma, et al. Quantitative Calculation of Temperature-Time-Coal Metamorphism [J]. Advances in Geosciences, 2021, 11 (7): 937-946.

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APA Style

Zhang Xuemei, Ma Qinghua, Li Dong, Hao Jingyuan. (2021). Inter-influence of Temperature-time-reflectivity in the Coal Metamorphism Thermodynamics Equation (CMTE). International Journal of Economy, Energy and Environment, 6(5), 114-117. https://doi.org/10.11648/j.ijeee.20210605.16

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ACS Style

Zhang Xuemei; Ma Qinghua; Li Dong; Hao Jingyuan. Inter-influence of Temperature-time-reflectivity in the Coal Metamorphism Thermodynamics Equation (CMTE). Int. J. Econ. Energy Environ. 2021, 6(5), 114-117. doi: 10.11648/j.ijeee.20210605.16

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AMA Style

Zhang Xuemei, Ma Qinghua, Li Dong, Hao Jingyuan. Inter-influence of Temperature-time-reflectivity in the Coal Metamorphism Thermodynamics Equation (CMTE). Int J Econ Energy Environ. 2021;6(5):114-117. doi: 10.11648/j.ijeee.20210605.16

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@article{10.11648/j.ijeee.20210605.16,
  author = {Zhang Xuemei and Ma Qinghua and Li Dong and Hao Jingyuan},
  title = {Inter-influence of Temperature-time-reflectivity in the Coal Metamorphism Thermodynamics Equation (CMTE)},
  journal = {International Journal of Economy, Energy and Environment},
  volume = {6},
  number = {5},
  pages = {114-117},
  doi = {10.11648/j.ijeee.20210605.16},
  url = {https://doi.org/10.11648/j.ijeee.20210605.16},
  eprint = {https://article.sciencepublishinggroup.com/pdf/10.11648.j.ijeee.20210605.16},
  abstract = {The influence and control of time and temperature on coalification are comprehensive. In order to quantitatively analyze the thermal kinetics of coal metamorphosis process by temperature and time, the qualitative analysis of coal metamorphosis thermodynamic equation (CMTE) based on Wu Chonglong was further verified from the mathematical point of view. Wu Chong Long's Coal Metamorphism Thermodynamics Equation (CMTE) is a ternary equation containing coal forming period or metamorphic age (time), metamorphic temperature (temperature) and metamorphic degree (reflectivity). The temperature calculated by fixing time and reflectivity is the lowest theoretical metamorphic temperature. The reflectivity calculated by fixing time and temperature is the maximum theoretical metamorphic degree. The “time-temperature ratio” is defined as the equivalent of extending million years to increasing 1°C temperature regarding coal metamorphism. This ratio is used to compare the impact of extending time or increasing temperature on improving the metamorphic degree and its significance. The results showed that in the same coal forming period, the ratio is decreased with the reflectivity increasing; at the same reflectivity, the ratio decreased with younger coal forming period. At Ro=6.1%, the calculated ratio is 3.67, which means, at Ro=6.1%, increasing 1°C is equaled extending 3.67 million.},
 year = {2021}
}

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TY  - JOUR
T1  - Inter-influence of Temperature-time-reflectivity in the Coal Metamorphism Thermodynamics Equation (CMTE)
AU  - Zhang Xuemei
AU  - Ma Qinghua
AU  - Li Dong
AU  - Hao Jingyuan
Y1  - 2021/10/19
PY  - 2021
N1  - https://doi.org/10.11648/j.ijeee.20210605.16
DO  - 10.11648/j.ijeee.20210605.16
T2  - International Journal of Economy, Energy and Environment
JF  - International Journal of Economy, Energy and Environment
JO  - International Journal of Economy, Energy and Environment
SP  - 114
EP  - 117
PB  - Science Publishing Group
SN  - 2575-5021
UR  - https://doi.org/10.11648/j.ijeee.20210605.16
AB  - The influence and control of time and temperature on coalification are comprehensive. In order to quantitatively analyze the thermal kinetics of coal metamorphosis process by temperature and time, the qualitative analysis of coal metamorphosis thermodynamic equation (CMTE) based on Wu Chonglong was further verified from the mathematical point of view. Wu Chong Long's Coal Metamorphism Thermodynamics Equation (CMTE) is a ternary equation containing coal forming period or metamorphic age (time), metamorphic temperature (temperature) and metamorphic degree (reflectivity). The temperature calculated by fixing time and reflectivity is the lowest theoretical metamorphic temperature. The reflectivity calculated by fixing time and temperature is the maximum theoretical metamorphic degree. The “time-temperature ratio” is defined as the equivalent of extending million years to increasing 1°C temperature regarding coal metamorphism. This ratio is used to compare the impact of extending time or increasing temperature on improving the metamorphic degree and its significance. The results showed that in the same coal forming period, the ratio is decreased with the reflectivity increasing; at the same reflectivity, the ratio decreased with younger coal forming period. At Ro=6.1%, the calculated ratio is 3.67, which means, at Ro=6.1%, increasing 1°C is equaled extending 3.67 million.
VL  - 6
IS  - 5
ER  -

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Author Information

Zhang Xuemei

Energy & Chemical Engineering Research Center, Xi'an Siyuan University, Xi’an, China
Ma Qinghua

Energy & Chemical Engineering Research Center, Xi'an Siyuan University, Xi’an, China
Li Dong

Energy & Chemical Engineering Research Center, Xi'an Siyuan University, Xi’an, China
Hao Jingyuan

Energy & Chemical Engineering Research Center, Xi'an Siyuan University, Xi’an, China

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Plain Text BibTeX RIS

APA Style

Zhang Xuemei, Ma Qinghua, Li Dong, Hao Jingyuan. (2021). Inter-influence of Temperature-time-reflectivity in the Coal Metamorphism Thermodynamics Equation (CMTE). International Journal of Economy, Energy and Environment, 6(5), 114-117. https://doi.org/10.11648/j.ijeee.20210605.16

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ACS Style

Zhang Xuemei; Ma Qinghua; Li Dong; Hao Jingyuan. Inter-influence of Temperature-time-reflectivity in the Coal Metamorphism Thermodynamics Equation (CMTE). Int. J. Econ. Energy Environ. 2021, 6(5), 114-117. doi: 10.11648/j.ijeee.20210605.16

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AMA Style

Zhang Xuemei, Ma Qinghua, Li Dong, Hao Jingyuan. Inter-influence of Temperature-time-reflectivity in the Coal Metamorphism Thermodynamics Equation (CMTE). Int J Econ Energy Environ. 2021;6(5):114-117. doi: 10.11648/j.ijeee.20210605.16

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@article{10.11648/j.ijeee.20210605.16,
  author = {Zhang Xuemei and Ma Qinghua and Li Dong and Hao Jingyuan},
  title = {Inter-influence of Temperature-time-reflectivity in the Coal Metamorphism Thermodynamics Equation (CMTE)},
  journal = {International Journal of Economy, Energy and Environment},
  volume = {6},
  number = {5},
  pages = {114-117},
  doi = {10.11648/j.ijeee.20210605.16},
  url = {https://doi.org/10.11648/j.ijeee.20210605.16},
  eprint = {https://article.sciencepublishinggroup.com/pdf/10.11648.j.ijeee.20210605.16},
  abstract = {The influence and control of time and temperature on coalification are comprehensive. In order to quantitatively analyze the thermal kinetics of coal metamorphosis process by temperature and time, the qualitative analysis of coal metamorphosis thermodynamic equation (CMTE) based on Wu Chonglong was further verified from the mathematical point of view. Wu Chong Long's Coal Metamorphism Thermodynamics Equation (CMTE) is a ternary equation containing coal forming period or metamorphic age (time), metamorphic temperature (temperature) and metamorphic degree (reflectivity). The temperature calculated by fixing time and reflectivity is the lowest theoretical metamorphic temperature. The reflectivity calculated by fixing time and temperature is the maximum theoretical metamorphic degree. The “time-temperature ratio” is defined as the equivalent of extending million years to increasing 1°C temperature regarding coal metamorphism. This ratio is used to compare the impact of extending time or increasing temperature on improving the metamorphic degree and its significance. The results showed that in the same coal forming period, the ratio is decreased with the reflectivity increasing; at the same reflectivity, the ratio decreased with younger coal forming period. At Ro=6.1%, the calculated ratio is 3.67, which means, at Ro=6.1%, increasing 1°C is equaled extending 3.67 million.},
 year = {2021}
}

Copy | Download

TY  - JOUR
T1  - Inter-influence of Temperature-time-reflectivity in the Coal Metamorphism Thermodynamics Equation (CMTE)
AU  - Zhang Xuemei
AU  - Ma Qinghua
AU  - Li Dong
AU  - Hao Jingyuan
Y1  - 2021/10/19
PY  - 2021
N1  - https://doi.org/10.11648/j.ijeee.20210605.16
DO  - 10.11648/j.ijeee.20210605.16
T2  - International Journal of Economy, Energy and Environment
JF  - International Journal of Economy, Energy and Environment
JO  - International Journal of Economy, Energy and Environment
SP  - 114
EP  - 117
PB  - Science Publishing Group
SN  - 2575-5021
UR  - https://doi.org/10.11648/j.ijeee.20210605.16
AB  - The influence and control of time and temperature on coalification are comprehensive. In order to quantitatively analyze the thermal kinetics of coal metamorphosis process by temperature and time, the qualitative analysis of coal metamorphosis thermodynamic equation (CMTE) based on Wu Chonglong was further verified from the mathematical point of view. Wu Chong Long's Coal Metamorphism Thermodynamics Equation (CMTE) is a ternary equation containing coal forming period or metamorphic age (time), metamorphic temperature (temperature) and metamorphic degree (reflectivity). The temperature calculated by fixing time and reflectivity is the lowest theoretical metamorphic temperature. The reflectivity calculated by fixing time and temperature is the maximum theoretical metamorphic degree. The “time-temperature ratio” is defined as the equivalent of extending million years to increasing 1°C temperature regarding coal metamorphism. This ratio is used to compare the impact of extending time or increasing temperature on improving the metamorphic degree and its significance. The results showed that in the same coal forming period, the ratio is decreased with the reflectivity increasing; at the same reflectivity, the ratio decreased with younger coal forming period. At Ro=6.1%, the calculated ratio is 3.67, which means, at Ro=6.1%, increasing 1°C is equaled extending 3.67 million.
VL  - 6
IS  - 5
ER  -

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