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A method of calculating hydrocarbon generation history - hydrogen index method (TTPCI-I_H method)

机译:计算烃生成历史的方法-氢指数法(TTPCI-I_H方法)

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摘要

The traditional TTI-R_o method uses virtinite reflectance as the indicator of the organic matter maturity, and then makes it a dominant parameter during the simulation of organic matter hydrocarbon generation history. However, this method only takes virtinite reflectance as a function of time and temperature, but ignores not only the influence of pressure and catalyst, but also the follow-up generation contradiction. Actually, this method is difficult to correctly describe the organic matter hydrocarbon generation history. By a variety of analysis and comparison, hydrogen index (I_H) is found to be the parameter with the above characteristics. I_H is also the synthetical effect result of time, temperature, pressure and catalyst and their dynamic change. So it is appropriate to use I_H, instead of R_o, as the dominant parameter during the hydrocarbon generation history of organic matter. Then it is possible to establish a method on the basis of the hydrogen index to calculate the hydrocarbon generation history - the comprehensive simulation method of time, temperature, pressure, catalyst and index, called TTPCI-I_H method. And it is successfully applied in hydrocarbon generation history simulation. The actual simulation results in Shengli oilfield show that TTPCI-Ih method is obviously better than TTI-R_o method. Kormation pressure;;organic matter maturity;;hydrocarbon generation history simulafion;;vitrinite reflectance;;hydrogen index;;TTl-R_o method;;TTPCI-I_H method.
机译:传统的TTI-R_o方法使用云母石反射率作为有机物成熟度的指标,然后使其成为模拟有机物烃生成历史的主要参数。然而,该方法仅将白云石反射率作为时间和温度的函数,而不仅忽略了压力和催化剂的影响,而且忽略了后续发生的矛盾。实际上,该方法难以正确地描述有机物烃的生成历史。通过各种分析和比较,发现氢指数(I_H)是具有上述特性的参数。 I_H也是时间,温度,压力和催化剂及其动态变化的综合结果。因此,在有机质生烃历史中,以I_H代替R_o作为主导参数是合适的。然后可以根据氢指数建立一种计算烃生成历史的方法-时间,温度,压力,催化剂和指数的综合模拟方法,称为TTPCI-I_H方法。并成功应用于生烃史模拟。胜利油田的模拟结果表明,TTPCI-Ih法明显优于TTI-R_o法。 K形成压力;有机物成熟度;生烃历史模拟;镜质体反射率;氢指数; TT1-R_o法; TTPCI-I_H法。

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