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Feasibility study of artifacts on the neutron logging curve near the boundary of layers

机译:层边界附近中子测井曲线的可行性研究

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The neutron borehole probe equipped with a neutron source and a system of neutron detectors is commonly used to determine porosity of geological formations. Transport of neutrons through media relies on their interaction with atomic nuclei, mainly with the process of scattering and absorption. Curves recorded by detectors for a given geological layer bordered by a medium with other neutron properties form the so-called anomalies. The course of the anomaly mainly depends on neutron properties of the bordering media and also on the measurement geometry, borehole properties, etc. The paper focuses mainly on an influence of neutron properties of bordered rock media on the course of the anomaly curve, especially near the media boundaries. In some cases of bordering media, characterized by specific neutron properties, the course of anomalies can be significantly disturbed, forming specific artifacts. The paper explains that the presence of artifacts is closely related to the properties of bordered media for both fast and thermal neutrons, i.e., the slowing down length of fast neutrons and the absorption cross section of thermal neutrons. Artifacts can be the cause of misinterpretation of the neutron rock porosity probe measurement. All considerations presented in this paper are based on results obtained from MC calculations performed using MCNP5 code (MCNP Team in X-5 Monte Carlo Team, MCNP a general Monte Carlo N-particle transport code version 5. Los Alamos National Laboratory LA-UR-03-1987, 2008).
机译:配备有中子源和中子探测器系统的中子钻孔探针通常用于确定地质形成的孔隙率。通过媒体运输中子依赖于它们与原子核的相互作用,主要是散射和吸收过程。由探测器记录的曲线对于由具有其他中子特性的介质接近的给定地质层的曲线形成所谓的异常。异常的过程主要取决于边界介质的中子特性,以及在测量几何形状,钻孔特性等上。本文主要侧重于与边界岩石介质在异常曲线过程中的中子特性的影响,特别是附近媒体边界。在一些趋向介质的情况下,特征在于特定的中子特性,异常过程可以显着受到干扰,形成特定的伪像。本文解释说,伪影的存在与快速和热中子的边界介质的性质密切相关,即快速中子的减速和热中子的吸收横截面。文物可以是中子岩孔隙率探头测量误解的原因。本文提出的所有考虑因素都是基于使用MC计算的结果使用MCNP5代码(MCNP团队,X-5 Monte Carlo Team,MCNP一般蒙特卡洛N-Pillet Rode版本5. Los Alamos National La-Ur- 03-1987,2008)。

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