Effect of Frequency and Temperature on Rock Dielectric Properties

Abstract

The real and imaginary components of dielectric constant were determined for basalt, granite and quartzite in the frequency range 10MHz to 4 GHz. The variation of dielectric permittivity with temperature was determined from room temperature to 450C. No dielectric dispersion or rock relaxation was observed in the frequency range investigated. Hence, the rock relative dielectric constant and relative loss showed mild variation with frequency with no discontinuity or sharp peaks as those previously observed in the low frequency range (up to 2 KHz). The temperature coefficient of the relative dielectric constant was related to the isobarric thermal expansion coefficient of the rock. The relative dielectric loss of basalt and granite followed an Arrhenius exponential increase with temperature suggesting the loss mechanism to be associated with activated particulate diffusion in the rock lattice. Activation energy for the conductance process depended on the temperature range and appeared to be independent of frequency. Quartzite showed an anomalous temperature variation of its conductivity. (Author)

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Document Details

Document Type
Technical Report
Publication Date
Jul 01, 1973
Accession Number
AD0766050

Entities

People

  • Aida S. Khalafalla

Organizations

  • Honeywell International, Inc.

Tags

DTIC Thesaurus Topics

  • Amplifiers
  • Charged Particles
  • Detectors
  • Diagrams
  • Dielectric Permittivity
  • Dielectric Properties
  • Elementary Particles
  • Energy
  • Equations
  • Experimental Data
  • Frequency
  • High Temperature
  • Materials
  • Measurement
  • Standing Waves
  • Thermal Expansion
  • Transmission Lines

Readers

  • Geotechnical Engineering.
  • Materials Science and Engineering.
  • Microwave Engineering.