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Xia Yanqing, Luo Binjie, Wang Chunjiang. A Study on Triterpenoids in the Tertisry Wood Brown Coal from Nanning Basin by Means of Pyrolysis[J]. Acta Sedimentologica Sinica, 1996, 14(S1): 100-106.
Citation: Xia Yanqing, Luo Binjie, Wang Chunjiang. A Study on Triterpenoids in the Tertisry Wood Brown Coal from Nanning Basin by Means of Pyrolysis[J]. Acta Sedimentologica Sinica, 1996, 14(S1): 100-106.

A Study on Triterpenoids in the Tertisry Wood Brown Coal from Nanning Basin by Means of Pyrolysis

  • Received Date: 1995-12-07
  • Publish Date: 1996-12-31
  • Pyrolysis was done by two methods, the Y series of experiments showed the process of comprehensive original organic matter evolved and the Z series showed the process of only kerogen evolved. The comprehensive original organic matter was composed of non-kerogen matter and kerogen, so based on the two series of experiments we can study deeply how triterpenoids are generated and how they change.From the result of pyrolysis, this paper showed the differences between the comprehensive original organtic matter generated from both non-kerogen matter and kerogen and from only kerogen, and approached geochemical significance of the triterpenoids.The comprehensive original organic matter generated much more pentacyclic triterpenoids than kerogen did, so most pentacyclic triterpenoids were yielded by the non-kerogen matter.In Z series, there were no 8, 14-secohopanes, it's clear that the kerogen didn't yield 8, 14secohopanes. In Y zeries, when the temperature was 400℃, the pentacyclic triterponoids disappeared but 8, 14-secohopanes remained and were abundant, so the pentacyclic triterpanoids changed into 8, 14-secohopanes in high temperature.Hopanes, hopenes and 8, 14-secohopanes are all able to indicate maturity. At 250℃ hopenes were very abundant, but at 300℃ they disappeared, so they can indicate immaturity.Biohopanes are instable, too, when it was 350℃ they disappeared, so they can indicate lowmaturity. Three hopanes parameters and two 8, 14-secohopane ones were calculated. With the rising of the temperature, the two parameters Ts/Tm and C31αβ22S/22 (S+R) increased slowly in the beginning, but when the temperature exceeded 300℃, the parameters increased quickly;when it changed from 250℃ to 300℃, the parameter C32αβ22S/22 (S+R) remained the same, but when it was higher than 300℃, it increased quickly ; the two 8, 14-secohopanes parameters C278β(H) /So (H) and C288β(H) /8α(H) decreased quickly when it was lower than 300℃, and decreased slowly when it was higher than 300℃. The five Parameters all varied greatly at 300℃, so they are nice maturity indexes.
  • [1] 1.史继扬等.五环三枯烷的物该和演化.沉积学报,1991,9(增刊):26-33.

    2.段毅等.现代沼泽沉积物中五环三枯类的组成特征.沉积学报,1993. 11 (3): 82-87.
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  • Received:  1995-12-07
  • Published:  1996-12-31

A Study on Triterpenoids in the Tertisry Wood Brown Coal from Nanning Basin by Means of Pyrolysis

Abstract: Pyrolysis was done by two methods, the Y series of experiments showed the process of comprehensive original organic matter evolved and the Z series showed the process of only kerogen evolved. The comprehensive original organic matter was composed of non-kerogen matter and kerogen, so based on the two series of experiments we can study deeply how triterpenoids are generated and how they change.From the result of pyrolysis, this paper showed the differences between the comprehensive original organtic matter generated from both non-kerogen matter and kerogen and from only kerogen, and approached geochemical significance of the triterpenoids.The comprehensive original organic matter generated much more pentacyclic triterpenoids than kerogen did, so most pentacyclic triterpenoids were yielded by the non-kerogen matter.In Z series, there were no 8, 14-secohopanes, it's clear that the kerogen didn't yield 8, 14secohopanes. In Y zeries, when the temperature was 400℃, the pentacyclic triterponoids disappeared but 8, 14-secohopanes remained and were abundant, so the pentacyclic triterpanoids changed into 8, 14-secohopanes in high temperature.Hopanes, hopenes and 8, 14-secohopanes are all able to indicate maturity. At 250℃ hopenes were very abundant, but at 300℃ they disappeared, so they can indicate immaturity.Biohopanes are instable, too, when it was 350℃ they disappeared, so they can indicate lowmaturity. Three hopanes parameters and two 8, 14-secohopane ones were calculated. With the rising of the temperature, the two parameters Ts/Tm and C31αβ22S/22 (S+R) increased slowly in the beginning, but when the temperature exceeded 300℃, the parameters increased quickly;when it changed from 250℃ to 300℃, the parameter C32αβ22S/22 (S+R) remained the same, but when it was higher than 300℃, it increased quickly ; the two 8, 14-secohopanes parameters C278β(H) /So (H) and C288β(H) /8α(H) decreased quickly when it was lower than 300℃, and decreased slowly when it was higher than 300℃. The five Parameters all varied greatly at 300℃, so they are nice maturity indexes.

Xia Yanqing, Luo Binjie, Wang Chunjiang. A Study on Triterpenoids in the Tertisry Wood Brown Coal from Nanning Basin by Means of Pyrolysis[J]. Acta Sedimentologica Sinica, 1996, 14(S1): 100-106.
Citation: Xia Yanqing, Luo Binjie, Wang Chunjiang. A Study on Triterpenoids in the Tertisry Wood Brown Coal from Nanning Basin by Means of Pyrolysis[J]. Acta Sedimentologica Sinica, 1996, 14(S1): 100-106.
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