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Apparatus for routine measurements of the thermal conductivity of ice cores

Festa, Crescenzo, Rossi, Aristide·1999·Annals of Glaciology

Abstract

An apparatus is described for measuring the thermal conductivity of ice by the transient hot-wire method. Thermal conductivity A, is determined by tracking the thermal pulse induced in the sample by a heating source consisting of a platinum resistor. A central segment of the same platinum heating resistor acts also as a thermal sensor. A heat pulse transferred to the ice for a period of 40s gives a maximum temperature increment of about 7-14°C. In good experimental conditions, the expected reproducibility of the measurements is within ±3%. The accuracy of the method depends on whether the instrument has been calibrated by reliable standard samples, certified by absolute methods.

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Research works printed but not linked: 12

  1. Ito, 1977, Shotherm QTM measurement of rock specimens. Shotherm Sales Information 111, Chinetsu, 14, 21
  2. Clark, 1966, Handbook of physical constants, 10.1130/MEM97 · DOI
  3. 10.1063/1.1721592 · DOI
  4. Beblo, 1982, Landolt-Börnstein numerical data and functional relationships in science and technology. Vol. lb, 482
  5. Jaeger, 1965, Terrestrial heat flow, 7
  6. 10.1088/0508-3443/15/10/307 · DOI
  7. 10.1088/0508-3443/10/1/306 · DOI · Paper page
  8. 10.1088/0950-7671/40/2/309 · DOI
  9. 10.1071/PH560167 · DOI
  10. 10.1029/JZ064i010p01557 · DOI
  11. Grubbe, 1983, Determination of the vertical component of thermal conductivity by line source methods, Zentralbl. Geol. Paläontol., 1, 49
  12. Carslaw, 1959, Conduction of heat in solids

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Metadata

Authors
Festa, C., & Rossi, A.
Venue
Annals of Glaciology
Published
1999
Volume
29
Pages
151-154
ISSN
  • 0260-3055
  • 1727-5644
Cited by
5
References
0
Language
en

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