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Yin Xiaobo, Lain Liwen, Qian Yibo, Zhu Hui, Qi Houfa, Guan Deshi. Thermo-Analysis of Sedimentary Orgaric Matter under Non-Oxygen Condition[J]. Acta Sedimentologica Sinica, 1996, 14(S1): 143-148.
Citation: Yin Xiaobo, Lain Liwen, Qian Yibo, Zhu Hui, Qi Houfa, Guan Deshi. Thermo-Analysis of Sedimentary Orgaric Matter under Non-Oxygen Condition[J]. Acta Sedimentologica Sinica, 1996, 14(S1): 143-148.

Thermo-Analysis of Sedimentary Orgaric Matter under Non-Oxygen Condition

  • Received Date: 1995-01-18
  • Publish Date: 1996-12-31
  • Non-oxygen thermo-analysis at three different temperatures was Performed for the 19 biogas source rock samples from Ying-Qiong Basin in South China Sea and Qaidam Basin in Qinghai Province. The results showed that the thermo-decomposing temperature was 260-270℃ for polysaccharides (such as cellululose, semi-cellose) and lipid compounds. Also, the thermo-decomposing temperature was lower than 320℃ for most of nucleic acids and proteins.Therefore, the thermo-decomposing value at 330℃ for 1 hr. could be used to estimate the production abundance of biochemical methane.
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    2.阂航.陈美慈,赵华宇等.厌氧傲生物学.浙江大学出版社.1993.

    3.梁家马原,肖趁,周有洪等.生物气模拟实验.生物工程学报.1992. 8 (3): 300-304.

    4.中国科学院兰州地质研究所.青海湖综合考察报告.科学出版社.1979. 219.

    5.Dodama H and Schnitzer M. Thermal analysis of polycylic compounds. Proc. lntl. Clay. Conf. Tokyo.,1969. 1:765.

    6.Priwalw P I.Physical properties of postein and nucleic acid. Proc. Conf. Calorimetry and Thermodynamics. PolishSce, Publ, Waroaw. 1969. 1091.

    7.Speil S. Berkelhamer I. H and Pask J A, et al. Thermal analysis of clay. Bur. Mmes. Tech. Paper. 1945. (664):8.

    8.Steim J M.Arch. Biochem. lliophys. Thermal denatuiation of else-albumin. 1965. 112: 599.
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  • Received:  1995-01-18
  • Published:  1996-12-31

Thermo-Analysis of Sedimentary Orgaric Matter under Non-Oxygen Condition

Abstract: Non-oxygen thermo-analysis at three different temperatures was Performed for the 19 biogas source rock samples from Ying-Qiong Basin in South China Sea and Qaidam Basin in Qinghai Province. The results showed that the thermo-decomposing temperature was 260-270℃ for polysaccharides (such as cellululose, semi-cellose) and lipid compounds. Also, the thermo-decomposing temperature was lower than 320℃ for most of nucleic acids and proteins.Therefore, the thermo-decomposing value at 330℃ for 1 hr. could be used to estimate the production abundance of biochemical methane.

Yin Xiaobo, Lain Liwen, Qian Yibo, Zhu Hui, Qi Houfa, Guan Deshi. Thermo-Analysis of Sedimentary Orgaric Matter under Non-Oxygen Condition[J]. Acta Sedimentologica Sinica, 1996, 14(S1): 143-148.
Citation: Yin Xiaobo, Lain Liwen, Qian Yibo, Zhu Hui, Qi Houfa, Guan Deshi. Thermo-Analysis of Sedimentary Orgaric Matter under Non-Oxygen Condition[J]. Acta Sedimentologica Sinica, 1996, 14(S1): 143-148.
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