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Formation density measurement utilizing pulsed neutrons

机译:利用脉冲中子测量地层密度

摘要

A device for measuring the density of a formation uses a high-energy pulsed neutron source which induces gamma rays in the formation, and determines a gamma diffusion length of the formation based on the attenuation of gamma rays produced by inelastic scattering of fast neutrons. The borehole tool houses the neutron source along with a near gamma ray detector and a far gamma ray detector. The gamma ray detectors are located at different distances from the fast neutron source and spaced sufficiently from the fast neutron source such that dependence of inelastic gamma counts on fast neutron transport and gamma production of the formation is substantially reduced. Gamma ray events can be sorted and counted in time- and energy-dependent bins. The present invention has several advantages over gamma-gamma logging, including deeper penetration of gamma, and is also superior over systems which measure, e.g., hydrogen-based porosity.
机译:用于测量地层密度的设备使用高能脉冲中子源,该中子源在地层中感应出伽马射线,并根据快速中子的非弹性散射产生的伽马射线的衰减来确定地层的伽马扩散长度。钻孔工具容纳中子源以及近伽马射线探测器和远伽马射线探测器。伽马射线探测器与快速中子源的距离不同,并且与快速中子源的距离足够远,从而大大减少了非弹性伽马计数对快速中子传输和地层伽马产生的依赖性。伽马射线事件可以在与时间和能量有关的箱中进行分类和计数。本发明相对于γ-γ测井具有若干优点,包括更深的γ渗透,并且也优于例如测量基于氢的孔隙度的系统。

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