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Source rock maturity study by capillary tube interferometer

机译:毛细管干涉仪来源岩石成熟研究

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The mechanism of capillary tube interferometer is expected to be two-beam interference by ray tracing. A computer program to simulate the interference fringe pattern was established. By comparing the simulated fringe pattern and experimental fringe pattern, the refractive index of the liquid can be given when the two fringes coincide best. The results of this method are very near the Abbe refratometer. In the first time, the refractive indices of the low transparent extraction of source rocks were measured by capillary tube interferometer. A curve between the refractive indices of the diluted extraction of source rocks and corresponding vitrinite reflectance Ro was established. When Ro is in the range of 0.36-1.25, the refractive indices of the extraction increase with Ro, or the maturity of the source rocks. Good correlation was observed between the refractive indices and vitrinite reflectance Ro. The refractive index of the extraction of source rock is valuable for determining the degree of maturity of source rock. This technique is promising to measure the refractive indices of low transparent liquids and could be used to estimate the maturity of source rock.
机译:毛细管干涉仪的机理预计通过射线跟踪是双光束干扰。建立了模拟干涉条纹图案的计算机程序。通过比较模拟条纹图案和实验条纹图案,当两个条纹最佳时,可以给出液体的折射率。该方法的结果非常靠近Abbe测压表。在第一次,通过毛细管干涉仪测量源岩的低透明提取的折射率。建立了烃源岩的折射率与相应的vitriinite反射率Ro之间的曲线。当RO在0.36-1.25的范围内时,提取的折射率与RO增加,或源岩的成熟度。在折射率和vitriinite反射率之间观察到良好的相关性。烃源岩提取的折射率对于确定源岩的成熟程度是有价值的。该技术很有希望测量低透明液体的折射率,可用于估计源岩的成熟度。

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