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High-Frequency (400 MHz) T2 Measurements Using a Custom-Built NMR Probe, Eagle Ford Shale, Gonzales and La Salle Counties, Texas

机译:使用自定义内置的NMR探头,鹰福特页岩,歌剧院和La Salle县,高频(400 MHz)T2测量。德克萨斯州

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Nuclear magnetic resonance (NMR) has become an increasingly important tool for estimating porosity, permeability, and fluid characteristics in oil and gas reservoirs since its introduction in the 1950s. While NMR has become common practice in conventional reservoirs, its application is still relatively new to unconventional reservoirs such as the Eagle Ford Shale. Porosity and permeability estimates prove challenging in these exceptionally tight rocks where organic porosity and bound fluids are routinely below the detection limit and/or resolution of low-frequency (2 MHz or less) NMR. In response, a custom-built NMR probe has been constructed, capable of measuring 0.75-inch diameter, 0.45-inch length core plugs at a 400 MHz Larmor frequency. The NMR probe was validated by comparing high-frequency (400 MHz) data acquired in-house to low-frequency (2 MHz) data measured at a commercial laboratory. Twelve core plugs (0.75-inch diameter, 1-inch length) were cut from two Eagle Ford Shale subsurface cores located in Gonzales and La Salle counties, Texas. Low-frequency T2 distributions were measured twice: first after drying core plug samples in a vacuum oven and again after spontaneous imbibition with various brine solutions (deionized water, 8 wt.% KCl, or 17.9 wt.% KCl) for one week. For high-frequency NMR measurements, samples were trimmed to 0.45-inch lengths to fit inside the newly-built NMR probe, creating two sub-samples for each of the original core plugs. T2 distributions were first acquired “as-is” (e.g., without drying or saturation) then again after drying and spontaneous imbibition with the same brine solutions used in the low-frequency study. Qualitatively, high-frequency T2 distributions resemble low-frequency measurements; however, the absolute T2 values are routinely higher by one order of magnitude. The difference may be caused by data acquisition, data processing, enhanced fluid relaxation, magnetic field inhomogeneities, or some combination thereof. The project provides a proof-of-concept that T2 relaxation times can be measured in “conventional-sized” core plugs using 400 MHz NMR. Although limited in its outcomes, the study delivers promising results and elicits future research into utilizing high-frequency NMR spectroscopy as a petrophysical tool for unconventional reservoirs.
机译:核磁共振(NMR)已成为估算石油和燃气藏的孔隙,渗透率和流体特性的越来越重要的工具,自20世纪50年代引入以来。虽然NMR在传统的水库中成为常见的做法,但其应用仍然对非传统的储层仍然相对较新,例如Eagle Ford Sheale。孔隙率和渗透性估计在这些异常紧的岩石中证明了有机孔隙率和结合流体在低频(2MHz或更低)NMR的检测极限和/或分辨率下方有机孔隙率和结合流体。作为响应,已经构造了一种定制的NMR探头,能够测量0.75英寸直径,0.45英寸长度的核心插头,在400 MHz的大频频率下。通过将内部内部的高频(400MHz)数据与商业实验室测量的低频(2MHz)数据进行比较来验证NMR探针。从位于德克萨斯州冈萨雷斯和La Salle Counties的两只Eagle Ford页岩地下核心中切断了十二个芯插塞(0.75英寸直径,1英寸)。测量低频T2分布两次:首先在真空烘箱中干燥核心插头样品后,再次用各种盐水溶液(去离子水,8重量%KCl,或17.9重量%KCl)再次进行自发性吸收。对于高频NMR测量,将样品修剪至0.45英寸长度,以适合新建的NMR探针,为每个原始核心插头创建两个子样本。首先在干燥和具有在低频研究中使用的相同盐水溶液的干燥和自发性吸收后再次获得“AS-IS”(例如,不干燥或饱和)。定性,高频T2分布类似于低频测量;然而,绝对T2值常规较高一个幅度。差异可能是由数据采集,数据处理,增强的流体松弛,磁场不均匀的或其一些组合引起的。该项目提供了概念证据,即使用400 MHz NMR的“常规”核心插头可以测量T2弛豫时间。虽然其结果有限,但该研究提供了有前途的结果,并引发了未来的研究,以利用高频NMR光谱作为非传统水库的岩石物理工具。

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