摘要: |
对不同升温速率下加水热模拟残余样品热解生烃动力学特征进行了分析,并就初次生烃时的升温速率对残余 有机质成烃动力学特征的影响进行了研究。结果表明,初次生烃时较慢的升温速率有利于烃类的初次生成,而残余 有机质的二次生烃潜力明显降低,二次生烃时的启动温度增加;初次生烃时较快的升温速率不利于烃类的初次生 成,但残余有机质二次生烃潜力大,再次生烃时的启动温度降低。通过模拟条件与实际地质条件的对比分析认为, 在地质条件下也存在上述规律。在确定不同地区、不同地质时期的构造演化和地温变化情况下,可以对烃源岩的初 次生径量和二次成烃潜力进行合理的分析。 |
关键词: 有机质 升温速率;动力学参数;二次生烃;控制作用 |
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基金项目:大港油田分公司2003 — 2004年项目“构造热事件对有机质热解成烃演化作用研究”. |
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Control role of primary hydrocarbon temperature-increasing velocity of organic matter to the secondary hydrocarbon generation |
GAO Gang1,ZHAO Zhe2,JIANG Zhen-xue1,PANG Xiong-qi1
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(1. School of Resource and Information Technology in China University of Petroleum, Beijing 102249, China ;2. Research Institute of Petroleum Exploration and Development , China National Petroleum Corporation, Beijing 100083, China)
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Abstract: |
By the analysis of hydrocarbon-generating dynamic parameters of residual organic matter in hydropyrolysis of different temperature-increasing velocity, the influences of temperature-increasing velocity of the primary hydrocarbon on dynamic characteristics were researched. At the lower velocity of temperature increase, the hydrocarbons can be formed advantageously ,the secondary hydrocarbon-generating potential of residual organic matter decreases and the beginning temperature of secondary hydrocarbon generation increases. At the higher velocity of temperature increase, the hydrocarbons can be formed disadvantageously, the hydrocarbon-generating potential of residual organic matter elevates and the beginning temperature of secondary hydrocarbon generation descends. The contrast analysis of thermal simulation to actual geological condition shows that this rule exists in geological history. According to the research result of tectonic evolution and paleotemperature variation,the amount and the potential of secondary hydrocarbon generation of residual organic matter can be analyzed rationally. |
Key words: organic matter temperature-increasing velocity dynamic parameter secondary hydrocarbon generation control role |