首页> 外文会议>International Symposium of the Society of Core Analysts >NMR T1-T2 Response of Moveable and Non-Moveable Fluids in Conventional and Unconventional Rocks.
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NMR T1-T2 Response of Moveable and Non-Moveable Fluids in Conventional and Unconventional Rocks.

机译:常规和非传统岩石中可移动和不可移动流体的NMR T1-T2响应。

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Recent publications have shown that liquid rich shales can also contain a significant proportion of high viscosity hydrocarbons that are not producible in tight rocks such as shales [1],[2]. NMR theory of fluid relaxation suggests that the ratio of T1/T2 can be used to differentiate low viscosity fluids(moveable)and highly viscous fluids. In the present study we have investigated the NMR response of moveable and non-moveable fluids in conventional and unconventional reservoir rocks using T1-T2 correlation maps obtained with a TE = 100μsec. Berea sandstone,Lyons sandstone,and Bossier tight sands were saturated at 3000 psi with 2.5% KCl brine. The corresponding T1-T2 maps show that T1/T2= 1.5. In two Wolfcamp shale samples from an oil producing well,we observed for the”native”state a NMR signal with a T1/T2 ratio of 1.3. An increase in amplitude of the”native”state NMR signal was observed after the shale samples imbibed 2.5% KCl brine for 24h. However,the imbibition of dodecane for 24h by the shale samples gave rise to a NMR signal with a T1/T2 ratio of 3 for one shale sample and 2.5 for the other sample. These experiments show that moveable brine in rocks has a T1/T2 ratio close to 1.5 while the T1/T2 ratio for moveable oil is close to 3. The study of non-moveable hydrocarbons was conducted on solid bitumen and wax. In their bulk solid state,solid bitumen and wax have T1/T2 ratios of 20 and 400,respectively. However,these ratios decreased and approached a value of 2 to 3 after the hydrocarbons were liquefied. Liquid wax was also introduced in a Berea sandstone sample,and allowed to solidify within the rock. The NMR T1-T2 map of Berea saturated with solid wax show a T1/T2 ratio of 400. These results imply that non-moveable hydrocarbons are not affected by surface relaxivity and have T1-T2 ratios higher than moveable hydrocarbons.
机译:最近的出版物表明,富含液体富源的HALES还可以含有大量的高粘度烃,其在紧密岩石中不生产,例如SHALES [1],[2]。流体弛豫的NMR理论表明T1 / T2的比率可用于区分低粘度流体(可移动)和高粘度流体。在本研究中,我们研究了使用用TE =100μSEC获得的T1-T2相关图在传统和非传统的储层岩石中的可移动和不可移动流体的NMR响应。 Berea Sandstone,Lyons Sandstone和Bossier紧身砂岩饱和在3000 psi,2.5%Kcl盐水。相应的T1-T2图显示T1 / T2 = 1.5。在两种Wolfcamp页岩样品中,来自产生的油井,我们观察到“天然”状态为NMR信号,T1 / T2比为1.3。在页岩样品中吸收2.5%KCl盐水24小时后观察到“天然”状态NMR信号的幅度的增加。然而,由页岩样品的十二烷的吸入24h,使得对于另一个样品的Sale样品和2.5的T1 / T2比为3的NMR信号。这些实验表明,岩石中的可移动盐水的T1 / T2比率接近1.5,而可移动油的T1 / T2比率接近3.在固体沥青和蜡上进行不可移动烃的研究。在其堆积固态中,固体沥青和蜡分别具有20和400的T1 / T2比。然而,在碳氢化合物液化后,这些比率降低并接近2〜3的值。液体蜡也被引入Berea砂岩样品中,并在岩石内固化。用固体蜡饱和的Berea的NMR T1-T2映射显示出400的T1 / T2比率。这些结果意味着不可移动的烃不受表面松弛率的影响,并且具有比可移动烃高的T1-T2比率。

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