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Wang Kaifa, Li Yiyin, Zhang Huizhi. Preliminary Study of the Thermal Simulation of Spora and Pollen Ⅰ: Generation Rate and Property of Hydrocarbons[J]. Acta Sedimentologica Sinica, 1991, 9(S1): 131-137.
Citation: Wang Kaifa, Li Yiyin, Zhang Huizhi. Preliminary Study of the Thermal Simulation of Spora and Pollen Ⅰ: Generation Rate and Property of Hydrocarbons[J]. Acta Sedimentologica Sinica, 1991, 9(S1): 131-137.

Preliminary Study of the Thermal Simulation of Spora and Pollen Ⅰ: Generation Rate and Property of Hydrocarbons

  • Publish Date: 1991-12-31
  • Thermal transformation of three types of spora and pollen has been conducted to evalute their generation potential of hydrocarbons. Experimental results show that the spora and pollen are source of oil and gas generation. Highest oil and gas generating rate of angiosperm pollen are 170mgHC/g Corgand 150ml/g Corgrespectively, and that of herb pteridopgyte spora are 66. lmgHC/g Corgand 11.4ml/g. 300℃ -400℃ are maturational period of hydrocarbon generation of spora and pollen. The thermal degradation of sporopollenin is the major origin of hydrocarbons generation. Angiosperm pollen is better than herb pteridophte spora in portential of hydrocarbon generation. For same kind of pollen the larger the size of pollen, the better the veins grow, the thicker the outer wall is, the better the generation potential of hydrocarbons. The contain of asphalt of generated by the three types of sporopollen in thermal degration is higher.
  • [1] (1) 傅家漠、刘德汉、盛国英,1990.煤成径地球化学.科学出版社。(2) 戈尔什科妹.1970.石化有机质和石油(沉积矿床有机地化译文集,1984).科学出版社

    (3) 高瑞淇,1986,一种松树花粉的地球化学特证石油地质进展丛书-1,有机地球化学和陆相生油,中国石油学会石油地质委员会编,石油工业出版社

    (4) 黄第藩,1987,未成熟石油成因的初步研究,中国科学院铸州地质研究所牛物.气体地球化学开放研究实验室听报(1987).甘肃科学技术出版社。

    (5) 王开发、吴国、阎家林,1983,地球化学,第4期,380-387页

    (6) 王开发、吴国.1989中国东部第三系含油盆地的抱粉相与抱粉颜色研究、贵州人民出版社

    (7) 徐振泰.1981.石油学报增刊,25-31页

    (8) Brooks. J,1981.沉积有机质的成熟度作Vita油勘探综述.1987,有机质成熟作用研究与矿物燃料勘探,石油工业出版社。

    (9) Erdtman. D.1978.孢粉学手册,科学出版社pp118-167 .

    (10) Brooks. J end G Shaw.1972, Geochemistry of spuropullenm Chemical Geology、Vol 10. No.1 PP.69-87

    (11) Brooks. J.. 1981,Organic maturation studies and fossil fuel explurauun Academm Press

    (12) Combaz. A,1971.Thermal degeration of sporopollenm and genesis of hydrocarbons. In: Sporopollenin Academic Press. London.
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  • Published:  1991-12-31

Preliminary Study of the Thermal Simulation of Spora and Pollen Ⅰ: Generation Rate and Property of Hydrocarbons

Abstract: Thermal transformation of three types of spora and pollen has been conducted to evalute their generation potential of hydrocarbons. Experimental results show that the spora and pollen are source of oil and gas generation. Highest oil and gas generating rate of angiosperm pollen are 170mgHC/g Corgand 150ml/g Corgrespectively, and that of herb pteridopgyte spora are 66. lmgHC/g Corgand 11.4ml/g. 300℃ -400℃ are maturational period of hydrocarbon generation of spora and pollen. The thermal degradation of sporopollenin is the major origin of hydrocarbons generation. Angiosperm pollen is better than herb pteridophte spora in portential of hydrocarbon generation. For same kind of pollen the larger the size of pollen, the better the veins grow, the thicker the outer wall is, the better the generation potential of hydrocarbons. The contain of asphalt of generated by the three types of sporopollen in thermal degration is higher.

Wang Kaifa, Li Yiyin, Zhang Huizhi. Preliminary Study of the Thermal Simulation of Spora and Pollen Ⅰ: Generation Rate and Property of Hydrocarbons[J]. Acta Sedimentologica Sinica, 1991, 9(S1): 131-137.
Citation: Wang Kaifa, Li Yiyin, Zhang Huizhi. Preliminary Study of the Thermal Simulation of Spora and Pollen Ⅰ: Generation Rate and Property of Hydrocarbons[J]. Acta Sedimentologica Sinica, 1991, 9(S1): 131-137.
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