首页> 外国专利> THERMAL NEUTRON POROSITY FROM NEUTRON SLOWING-DOWN LENGTH, FORMATION THERMAL NEUTRON CAPTURE CROSS SECTION, AND BULK DENSITY

THERMAL NEUTRON POROSITY FROM NEUTRON SLOWING-DOWN LENGTH, FORMATION THERMAL NEUTRON CAPTURE CROSS SECTION, AND BULK DENSITY

机译:中子减速长度引起的中子热孔隙率,形成中子俘获截面的热中子和堆积密度

摘要

A method for determining at least one formation property calculated from neutron measurements acquired with a downhole tool includes emitting neutrons from a source in the tool into the formation, detecting neutrons with at least one detector in the downhole tool, calculating a first slowing-down length (L1) based on the detected neutrons, and deriving a second slowing-down length (L2) based on the first slowing-down length (L1). Further steps include deriving a correlation function for relating slowing-down lengths from a first tool to slowing-down lengths associated with a different source, wherein the correlation function depends on formation properties such as bulk density; and applying the correlation function to the slowing-down length of the first tool to derive the slowing-down length of the second tool. A method for determining a thermal neutron formation porosity based on a slowing-down length from epithermal neutron measurements from an electronic neutron source includes converting the slowing-down length into a computed neutron slowing-down length from thermal neutron measurements from a chemical neutron source, wherein the converting uses a correlation function that depends on formation bulk density; deriving a thermal neutron countrate ratio based on the computed neutron slowing-down length, wherein the deriving uses a function that depends on the formation bulk density and formation sigma; and computing the thermal neutron formation porosity from the thermal neutron countrate ratio.
机译:一种用于确定由井下工具获取的中子测量值计算出的至少一个地层特性的方法,包括:将中子从工具中的源发射到地层中;使用井下工具中的至少一个检测器检测中子;计算第一减速长度(L1)基于检测到的中子,并基于第一减速长度(L1)得出第二减速长度(L2)。进一步的步骤包括从第一工具获得用于将减慢长度与与不同源相关联的减慢长度相关的相关函数,其中,所述相关函数取决于诸如堆积密度之类的地层特性;以及将相关函数应用于第一工具的减慢长度,以推导第二工具的减慢长度。一种基于来自电子中子源的超热中子测量值的减慢长度来确定热中子形成孔隙度的方法,该方法包括将减慢长度转换成根据来自化学中子源的热中子测量值计算出的中子减慢长度,其中转换使用取决于地层堆积密度的相关函数;根据计算出的中子减速长度推导热中子计数率,其中推导使用取决于地层堆密度和地层西格玛的函数;根据热中子计数率计算热中子形成孔隙率。

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