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Determining a formation porosity from neutron logging information

机译:根据中子测井信息确定地层孔隙度

摘要

A method for determining the porosity of a subsurface geological formation traversed by a borehole is provided. The method generally comprises obtaining a means which relates ranges of apparent formation porosity (pa) as determined by a neutron-neutron log, formation fluid salinities, formation total capture cross sections (E), formation matrix and fluid constituents, and true formation porosity (ϕT) according to a predetermined equation. The predetermined equation relates the apparent porosity to a function of a modified migration length which is obtained in a semi-empirical manner (i.e. physics modified by data). The modified migration length includes a slowing down length and a diffusion length, but causes at least the diffusion length to be a function of the slowing down length. The means which relates the apparent porosity to salinity, E, matrix and fluid constituents, and ϕT solves a forward problem. Thus, the inverse problem of determining true porosity may be solved by obtaining determinations of salinity, formation matrix and fluid constituents, E, and ϕa, and using the relating means to provide the true porosity. The provided method properly and separately accounts for the effects of capture cross section and salinity, and can be used to correct the apparent porosity determination of a neutron-neutron tool, regardless of the formation matrix or formation fluid constituents.
机译:提供了一种确定被钻孔横穿的地下地质构造的孔隙率的方法。该方法通常包括获得一种手段,该手段将由中子-中子测井,地层流体盐度,地层总俘获截面(E),地层基质和流体成分以及真实地层孔隙度确定的表观地层孔隙度范围(a)关联起来。 (ϕT)根据预定方程式。预定方程将表观孔隙率与以半经验方式(即,通过数据修改的物理学)获得的修正的迁移长度的函数相关。改变的迁移长度包括减慢长度和扩散长度,但是至少使扩散长度是减慢长度的函数。将表观孔隙率与盐度,E,基质和流体成分以及ϕT相关联的方法解决了一个正向问题。因此,确定真实孔隙度的反问题可以通过获得盐度,地层基质和流体成分E和ϕa的确定,并使用相关手段提供真实孔隙度来解决。所提供的方法适当地和单独地考虑了捕获截面和盐度的影响,并且可以用于校正中子-中子工具的表观孔隙率测定,而与地层基质或地层流体成分无关。

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