This invention is related to methods of determining thermophysical properties from solid bodies' (like rocks').
The correct record of the rocks' thermophysical properties, such as thermal conduction, thermal capacity and thermal diffusivity, becomes a top priority during industrial application of thermal production enhancement methods providing prior simulation of the reservoir (oil formation) and borehole heat-mass exchange processes as well as the borehole equipment thermal mode determination.
The proposed method of solid bodies' thermophysical properties non-destructive determination is different from the known methods (e,g., Patent RU 2153664 or Patent RU 2011977) by the possibility to use only one experiment reference standard and enhanced measurement functionalities due to ensuring the measurement accuracy resulting from the reduction of the bias arising in the existing methods because of the samples' surface curvature approximate record.
The purpose of the invention is to expand functionalities due to ensuring volumetric heat capacity measurements and the measurements' accuracy improvement.
The proposed method of solid bodies' thermophysical properties non-destructive determination, including the bodies with non-uniform properties, includes the sample surface heating during the heating unit motion relative to the sample with subsequent determination of excessive temperatures based on which the thermophysical properties like thermal conduction and/or thermal diffusivity are determined. The method may be used for the samples of any shape and ensures wide-range heat conduction measurements (from 0.06 to 250 W/(mK).
The method of solid bodies' thermophysical properties determination consists in the heating the surface of the reference sample—a uniform fixed-dimension sample with the known constant heat conduction and volumetric heat capacity, and the surfaces of the sequentially located solid bodies' samples using a thermal energy source (Popov Yu. A. Some Peculiarities of Rocks' Heat conduction, Universities' Proceedings. Geology and Exploration., No. 4-1984, pp. 72-76.), moving with a constant speed relative to the sample and the solid bodies' samples in question, measurement of excessive temperatures (i.e. the difference between the surface temperature and initial temperature) of the reference sample surfaces at the points on the heating line (the line on the sample surface along which the heating source centre is moving) and determination of the samples' heat conduction based on the measurements of the excessive temperatures of the reference sample and samples in question.
During the standard core measurements (a 30×30 mm cylindrical stick of the rock) and the use of a flat reference sample the excessive temperature measurement results for the reference sample and the samples in question are processed in such a way as using theoretical simulation (the process study using theoretical models—in this case—using a numerical solution) of physical processes accompanying the measurement process the difference of excessive temperatures for the flat and cylindrical surfaces is determined, then a set correction is applied to the measured excessive temperatures.
During standard-core measurements an inverse-factor heat conduction problem is solved (calculation of heat conduction factor or inverse thermal capacity by the temperature values in certain points, James V. Beck, Ben Blackwell, Charles R. St. Clair, Jr/Inverse Heat Conduction Ill-Posed Problems: Wiley Interscience Publication N.Y. 1989.-312 p.) and using the inverse heat conduction problem solution the heat conduction and volumetric heat capacity of the standard core cylindrical samples is determined.
During flat-sample measurements the inverse-factor heat conduction problem is solved and using the inverse-factor heat conduction problem solution heat conduction and volumetric heat capacity of the flat samples is solved.
During the method implementation the samples are located on the desk. The laser user as the thermal energy source is switched on ion the heating mode and moved along the line at a constant speed (2-4 mm/sec). The temperature measurements are held in series on the reference sample and sample-in-question surfaces. Based on the solution to the inverse-factor heat conduction problem for the reference sample the thermal energy distribution law is restored. Based on the inverse-factor heat conduction problem solution the heat conduction factor value or volumetric heat capacity value is restored.
Number | Date | Country | Kind |
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2008138643 | Sep 2008 | RU | national |