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Method and apparatus for reducing matrix density effects on porosity measurements during epithermal neutron porosity well logging

机译:降低超热中子孔隙度测井中基质密度对孔隙度测量影响的方法和装置

摘要

The porosity of the subsurface earth formation surrounding a borehole is investigated by measuring the populations of epithermal neutrons at detector locations longitudinally spaced from a neutron source. In this measuring process, a detector is located at a matrix density neutral (MDN) spacing from the neutron source at which effects of the matrix density of the earth formation are significantly reduced. The porosity measurements are determined from neutron counts detected at both the MDN location and other locations to derive formation porosity measurements which have reduced lithology and matrix density effects. Because of these reduced effects, formation porosity values derived do not need to be corrected to account for lithology and matrix density effects. In addition, the formation lithology and matrix density may be obtained.
机译:通过测量与中子源纵向隔开的探测器位置处的超热中子的数量,研究了围绕井眼的地下地层的孔隙度。在此测量过程中,将探测器放置在距中子源的矩阵密度中性点(MDN)处,从而显着降低地球形成的矩阵密度的影响。孔隙率测量值是根据在MDN位置和其他位置检测到的中子计数来确定的,以得出降低了岩性和基质密度影响的地层孔隙率测量值。由于这些降低的影响,不需要校正导出的地层孔隙度值以解决岩性和基质密度的影响。另外,可以获得地层岩性和基质密度。

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