Determination of the diameter of the thermal field disturbance zone around the borehole
Authors:
Abstract
At present, materials of thermal measurements in wells are widely used to determine the geothermal gradient, temperature of formation water and rocks in their natural conditions of occurrence. However, these materials do not always have proper accuracy. One of the main reasons causing the appearance of errors in determining the temperature of rocks and formation water is the violation of the natural thermal field of the Earth by the borehole, i.e., violation of the stationary thermal regime of the area.
Область исследования:
Mining
Funding:
None
References
- Dakhnov V. N. Interpretation of the Results of Geophysical Investigations of Well Sections. Gostoptekhizdat, 1955.
- Dakhnov V. N. and Diakonov D. I. Thermal Studies of Well Sections. Gostoptekhizdat, 1952.
- Russell W. L. Fundamentals of Petroleum Geology. Gostoptekhizdat, 1958.
- Frolov N. M. Geothermal Conditions of the Moldavian SSR. PH of the AS USSR, 1958.
- Cheremensky G. A. Results of Geothermal Research in Siberia. Problems of Geothermia and Practical Use of Earth's Heat. V. 1. PH of the AS of the USSR, 1959.
- ChudnovskyA. F. Heat exchange in dispersed media. GITTL, 1954.
- Van der Held und Van der Drunen F. Physics, 1949, No. 15, p. 865-881.
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