Summary
The paper analyses the behaviour of a probe for direct measurements of temperature increase with depth in boreholes and derives transient characteristics of a gradient probe using the electrothermal analogy.
This is a preview of subscription content, log in via an institution to check access.
Similar content being viewed by others
References
Е. А. Любимова: Проблемы глубинного теплового потока. Наука, М. 1966.
Е. А. Любимова: Геотермические исследования. Наука, М. 1964.
Ф. А. Макаренко: Геотермические исследования и использование тепла земли. Наука, М. 1966.
J. Halousek, K. Příhoda: A Precise Thermistor Thermometer for Use in Geothermics. Travaux Inst. Géophys. Acad. Tchécosl. Sci. No 276, Geofysikální sborník 1967, Academia, Praha 1968.
A. M. Lachenbruch: Crustal Temperature and Heat Flow. J. Geoph. Res., 75 (1970), 3291.
K. Kalliomak, P. Wallin: Measurement of Surface Temperature with a Thermally Compensated Probe. J. of Phys. E. (Sci. Inst.), 4 (1971), 535.
О. А. Геращенко, В. Г. Феодоров: Тепловые и температурные измерения. Наук. Думка, Киев 1962.
K. Hammeke: Messung von Differenz zweier Temperaturen mittles Widerstandsthermometer. Archiv f. tech. Messen, V-212 (1966), 227.
M. Krešl: Řešení teplotního pole pomocí elektrického modelu. Elektrotech. čas., 27 (1976), (at press).
Author information
Authors and Affiliations
Rights and permissions
About this article
Cite this article
Krešl, M. Dynamic properties of the probe for measuring the temperature gradient. Stud Geophys Geod 20, 186–192 (1976). https://doi.org/10.1007/BF01626051
Received:
Published:
Issue Date:
DOI: https://doi.org/10.1007/BF01626051