skip to main content
OSTI.GOV title logo U.S. Department of Energy
Office of Scientific and Technical Information

Title: Thermal conductivity of the rocks in the Bureau of Mines Standard Rock Suite

Abstract

Thermal conductivities of eight rocks from the Bureau of Mines Standard Rock Suite were measured in air over the temperature range 373 to 533/sup 0/K (100 to 260/sup 0/C). The thermal conductivities of these rocks were measured to furnish standards for future comparisons with host rock from prospective nuclear waste repository sites. The thermal conductivity at a given temperature decreased by as much as 9% after a specimen had been heated to the maximum temperature (533/sup 0/K), but additional heating cycles had no further effect. This decrease was smallest in the igneous rocks and largest in the sedimentary types. Variations due to orientation were within the precision of measurements (+- 5%). In most cases the thermal conductivities were linear with the reciprocal of the temperature and were within 14% of published data obtained by other methods. Measurements were made by a cut-bar comparison method in which the sample was sandwiched between two reference or metering bars made of Pyroceram 9606 glass-ceramic. The apparatus consisted of a Dynatech Model TCFCM-N20 comparative thermal conductivity analyzer controlled by a Hewlett Packard Model 3052A data acquisition system. A program was written to increment and cycle the temperature in steps between predetermined initial and maximummore » values. At each step the thermal conductivity was measured after steady-state conditions were established. The rocks furnished by the Bureau of Mines were quarried in large and fairly homogeneous lots for use by researchers at various laboratories. To investigate any anisotropy, cores were taken from each rock cube perpendicular to each of the cube faces. Samples 2 in. in diameter and approx. 0.75 in. thick were prepared from the cores and were dried in a vacuum oven for at least one month prior to taking measurements.« less

Authors:
;
Publication Date:
Research Org.:
Oak Ridge National Lab., TN (USA)
OSTI Identifier:
5608708
Report Number(s):
ORNL/TM-7052
TRN: 80-004780
DOE Contract Number:
W-7405-ENG-26
Resource Type:
Technical Report
Country of Publication:
United States
Language:
English
Subject:
58 GEOSCIENCES; 12 MANAGEMENT OF RADIOACTIVE AND NON-RADIOACTIVE WASTES FROM NUCLEAR FACILITIES; BASALT; THERMAL CONDUCTIVITY; GRANITES; GRANODIORITES; LIMESTONE; QUARTZITES; SANDSTONES; EXPERIMENTAL DATA; GRAPHS; HEAT TRANSFER; HIGH TEMPERATURE; MEDIUM TEMPERATURE; PYROMETERS; RADIOACTIVE WASTE FACILITIES; ROCKS; STANDARDS; TABLES; US BUREAU OF MINES; CARBONATE ROCKS; DATA; DATA FORMS; ENERGY TRANSFER; IGNEOUS ROCKS; INFORMATION; MEASURING INSTRUMENTS; METAMORPHIC ROCKS; NATIONAL ORGANIZATIONS; NUCLEAR FACILITIES; NUMERICAL DATA; PHYSICAL PROPERTIES; RESERVOIR ROCK; SEDIMENTARY ROCKS; THERMODYNAMIC PROPERTIES; US ORGANIZATIONS; 580300* - Mineralogy, Petrology, & Rock Mechanics- (-1989); 052002 - Nuclear Fuels- Waste Disposal & Storage

Citation Formats

Morgan, M.T., and West, G.A. Thermal conductivity of the rocks in the Bureau of Mines Standard Rock Suite. United States: N. p., 1980. Web. doi:10.2172/5608708.
Morgan, M.T., & West, G.A. Thermal conductivity of the rocks in the Bureau of Mines Standard Rock Suite. United States. doi:10.2172/5608708.
Morgan, M.T., and West, G.A. Tue . "Thermal conductivity of the rocks in the Bureau of Mines Standard Rock Suite". United States. doi:10.2172/5608708. https://www.osti.gov/servlets/purl/5608708.
@article{osti_5608708,
title = {Thermal conductivity of the rocks in the Bureau of Mines Standard Rock Suite},
author = {Morgan, M.T. and West, G.A.},
abstractNote = {Thermal conductivities of eight rocks from the Bureau of Mines Standard Rock Suite were measured in air over the temperature range 373 to 533/sup 0/K (100 to 260/sup 0/C). The thermal conductivities of these rocks were measured to furnish standards for future comparisons with host rock from prospective nuclear waste repository sites. The thermal conductivity at a given temperature decreased by as much as 9% after a specimen had been heated to the maximum temperature (533/sup 0/K), but additional heating cycles had no further effect. This decrease was smallest in the igneous rocks and largest in the sedimentary types. Variations due to orientation were within the precision of measurements (+- 5%). In most cases the thermal conductivities were linear with the reciprocal of the temperature and were within 14% of published data obtained by other methods. Measurements were made by a cut-bar comparison method in which the sample was sandwiched between two reference or metering bars made of Pyroceram 9606 glass-ceramic. The apparatus consisted of a Dynatech Model TCFCM-N20 comparative thermal conductivity analyzer controlled by a Hewlett Packard Model 3052A data acquisition system. A program was written to increment and cycle the temperature in steps between predetermined initial and maximum values. At each step the thermal conductivity was measured after steady-state conditions were established. The rocks furnished by the Bureau of Mines were quarried in large and fairly homogeneous lots for use by researchers at various laboratories. To investigate any anisotropy, cores were taken from each rock cube perpendicular to each of the cube faces. Samples 2 in. in diameter and approx. 0.75 in. thick were prepared from the cores and were dried in a vacuum oven for at least one month prior to taking measurements.},
doi = {10.2172/5608708},
journal = {},
number = ,
volume = ,
place = {United States},
year = {Tue Jan 01 00:00:00 EST 1980},
month = {Tue Jan 01 00:00:00 EST 1980}
}

Technical Report:

Save / Share: