FIELD: measuring technique.
SUBSTANCE: coefficient of open porosity Kpo of core is measured. Then total curve of spin-grating relaxation (SGR) is measured automatically received from threshold fluid in sample. Measured curve is subject to component-analytical mathematical processing and correspond group/phase contents of residual water in rock-selector is measured by means of relaxation/volumetric transparency from component values of relaxation times. Coefficient of total residual water content Kwa of core is determined by summing products of component/part saturations Wi with phase/group content of residual water Kwai in it from relation Kwa=nixWixKwai, where ni is number of component/group/phases in collector. After that coefficient of effective porosity Kpoef of rock/collector is measured automatically by means of specific values of open porosity coefficients Kpo and residual water saturation Kwa for sample of core from relation of Kpoef=Kpo(1-Kwa).
EFFECT: reduced time for measurements; improved precision; higher truth of results.
19 cl, 1 dwg
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Authors
Dates
2007-06-27—Published
2005-12-23—Filed